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    Into Dutch Soils

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    Into Dutch Soils | 01

    A swif overview o how he Duch manage heir soils:a source o inspiraion or your own pracice

    Into Dutch Soils

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    The text

    This bookle provides an overview o 35 years o Duch soil

    policy developmen, beginning wih a descripion o how i

    all began: he geological and hisorical developmen o he

    Neherlands. I considers quesions like: Why does a poriono he Duch populaion live below sea level? And how have

    he aciviies o he Duch over ime affeced he soil

    qualiy?

    Soil legislaion provides he legal ramework or curren

    land use in he Neherlands. Amongs many more, i defines

    liabiliy and enables susainable land managemen. I

    relaes o a large number o oher legislaive fields,

    specifically wih respec o oher environmenal compar-

    mens like groundwaer, surace waer and sedimens. These

    marices are only menioned shorly in his bookle.

    In addiion, a large array o echnical guidelines and

    approaches has been developed over he years. These

    insrumens play a major role in daily pracice. The key

    elemens are inroduced in his bookle.

    This 2ndediion o his bookle was writen or he Minisry

    o Inrasrucure and he Environmen by Frank Lam and

    Linda Maring o Delares wih a conribuion o Frank

    Swarjes o RIVM.

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    The photos

    The phoos in his bookle show he Duch in direc conac

    wih heir soil and represen everyday aciviies like

    agriculure, he consrucion o underground inrasrucure,

    recreaion, children playing, spors, soil remediaion,building aciviies, he developmen o man-made

    environmen, invesigaion o soil qualiy and archaeology.

    Table of contents

    Hisory o he Duch dela 05Duch soil: ypes and qualiy 11

    Developing a soil policy 15

    Skech o he legislaive ramework 21

    Fuure developmens in soil policy 25

    Many paries involved 29

    Decisions o he 33

    Liabiliy: who pays he bill? 37

    Soil uncions and ambiions 41

    Knowing he soil qualiy 45

    Waer and sedimens 49

    Technical guidelines 53

    Risk assessmen 57

    The Duch soil qualiy sandards 61

    Invesigaing he soil qualiy 67

    Soluions 71

    Index 75

    Duch soil on he inerne 79

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    The Neherlands is a ypical dela area, wih

    wo major rivers, he Rhine and he Meuse,

    flowing ino he Norh Sea.

    The Neherlands as we know i oday

    developed predominanly during he

    Holocene, approximaely he las 10,000

    years, when he ice shees o he las ice age

    meled and rereaed o he norh. As a

    consequence, beween 10,000 and 5,000

    years ago, he sea level rose by some 35

    meres. For he las 5,000 years he sea level

    has risen by only a ew meres. This risingsea level caused he wesern par o he

    Neherlands o become largely covered by

    he sea some 5,000 years ago.

    Beore ocusing on he way he Duch deal

    wih heir soil, le us firs go back in hisory

    and look a he developmen o he

    Neherlands as we now know i. The rivers

    were able o move reely over he land,

    deposiing clay, sand and gravel during

    seasonal floods wihin a wide floodplain.

    Swamps developed in he coasal area and

    he slighly higher-lying easern par o he

    Neherlands was covered by woods and high

    moorlands.

    Early inhabians were huner-gaherers,

    bu progressively hey setled and became

    armers, clearing he woods or armland.The wesern par o he Neherlands

    gradually evolved due o deposiion o sand

    and clay and he developmen o pea in he

    coasal area, wih he sea becoming a

    diminishing influence on he coasal area.

    The presence of the Romans in the

    Netherlands between 12 B.C. and 450

    A.D. saw their roads and buildings bring

    subsanial progress o he Neherlands. The

    River Rhine ormed a naural norhern

    border o he Roman Empire.

    The lae Middle Ages (1050 - 1500 A.D.)

    specifically saw exploiaion o he pea

    swamps and moorlands. Diches were dug o

    drain he swamps and dikes were build along

    he rivers and he coas. This allowed

    permanen occupaion o he wesern pars

    o he counry. Social and organisaionalsrucures sared o develop, resuling in he

    worlds very firs democraically chosen orm

    o adminisraion, waer auhoriies. These

    waer auhoriies were responsible

    or he waer managemen o he lower

    regions.

    History of the Dutch delta

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    The exensive pea cover o he wesern par

    o he Neherlands proved o be a valuable

    source o energy. This was o growing

    imporance a he end o he Middle Ages as

    he period known as he Litle Ice Age

    sared when he Neherlands suffered longand cold winers. Having a large source o

    pea available or heaing purposes, urher

    economic and social developmen was

    possible, despie he climaic condiions a

    ha ime, resuling in booming economic

    developmen during he 17h cenury, or

    he golden cenury as i became known in

    he Neherlands.

    During his period, he Duch flee made he

    counry a major miliary power ha

    dominaed he world rade. Wih demand

    or big sailing ships or world rade, he ciy

    o Amserdam, wih is naural harbour,

    sared o play a major role. Unil hen oher

    ciies in he Neherlands, like Urech, had

    been o ar greaer poliical and economicimporance. However, in conras o

    Amserdam, hose ciies had no direc

    connecion o he sea. The ciy o

    Amserdam, which had slowly developed

    during he cenuries beore, now became an

    imporan economic power as he base o

    Duch rade merchans. The quickly growing

    populaion uelled he demand or more

    ood and energy, a need ha obviously

    coninued afer he booming 17h cenury.

    Areas in he ormer coasal zone wih rich

    pea deposis were excavaed urher andurher. Where he pea was hick, his

    resuled in shallow lakes. In oher places,

    naural lakes were surrounded by dikes and

    wih he use o windmills he waer was

    pumped ou. This resuled in new land

    below sea level, he amous Duch polders.

    The level o he groundwaer in hese areas

    ofen lies jus a ew decimeres below he

    soil surace. In he pas, armers hereore

    welcomed (household) wase o raise he

    soil level o heir land. In some areas, his

    has resuled in widely disribued diffuse

    conaminaion o he arable land and

    grassland.

    Unil less hen 100 years ago, waer was amajor roue or ransporaion. Boas could

    carry ar more reigh han could be

    ranspored over land. Having pleny o

    waer in he wesern par o he

    Neherlands, he economic developmen in

    his area was given a urher boos and a

    nework o villages and ciies developed,

    housing more and more people in he lower

    pars o he Neherlands.

    Bu he densiy o populaion and indusry

    ook is oll on he soil qualiy, a siuaion

    ha is cerainly no unique o heNeherlands. Similar processes have

    occurred in oher (densely) populaed areas

    around he world.

    Obviously, waer is sill a hrea, no only

    rom he sea bu also rom he rivers. Dunes

    along he Norh Sea coas and dikes around

    lakes and rivers proec he low areas o he

    Neherlands agains he waer. The las ime

    large floods encroached upon par o he

    Neherlands was in 1953. A norh-weserly

    sorm coincided wih a spring ide o raise

    he sea level o a record heigh, which

    proved oo much or many o he dikes,

    specifically in he province o Zeeland. More

    han 1,800 people died and some 100,000

    people became homeless as a resul o hisbreach. This promped a major upgrading o

    he Duch sea deences, he so-called Dela

    Works.

    The very firs inhabians o he Neherlands

    had o cope wih he omnipresen waer;

    his need or proecion agains he sea and

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    The Neherlands below and above sea level

    (Actueel Hoogtebestand Nederland)

    Some facts and figures

    The River Rhineis 1,320 km long. From its source in

    the Swiss Alps, it passes through France and Germany

    with a catchment area o 185,000 km2and an average

    o 2,200 m3/s o water flows through the Netherlands.

    The River Meuseis 925 km long and originates in

    France, passing through Belgium beore arriving in the

    Netherlands. Its catchment covers an area o 36,000

    km2and the average flow rate is 230 m3/s.

    The North Seais a relatively shallow coastal area o

    the Atlantic Ocean. It covers the area between theUnited Kingdom, the Netherlands, northwest

    Germany, Denmark and the southern part o Norway;

    its total area is 575,000 km2with an average depth o

    just 95 m.

    The royal kingdom o the Netherlandscovers 41,526

    km2and is inhabited by 16.9 million people. The

    coastline is 451 km long. Most o the land surace is

    flat, except or some remnant lateral moraine o thelast ice age in the central part, and a hilly area in the

    south east. The highest point in the Netherlands is

    323 m, right on the border with Germany and

    Belgium. The lowest point is 6.76 m below sea level.

    In all some 40% o the land area lies below sea level.

    Elevation level of the Netherlands

    Below sea level

    Above sea level

    Cities

    Rivers

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    rivers over he cenuries has become rooed

    in he Duch who, despie hese risks, value

    he soil beneah heir ee!

    Nowadays, he Neherlands is a densely

    populaed counry, averaging almos 500people per km2, a figure ha rises o almos

    1,300 inhabians per km2in is mos

    densely populaed province o Zuid-

    Holland! And alhough an increasing

    amoun o agriculural land is gradually

    becoming urbanised, redevelopmen o ha

    urban area is ineviable i spaial develop-

    men is o keep in line wih growing needs.

    Tha he Duch should be conroned wiha soil legacy was inescapable.

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    The concept of defining soil quality with legislative

    reference values was so new, that it was even

    implemented in a number of other countries

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    Dutch soil: types and quality

    The descripion o he ormaion o he

    Neherlands during he pas 10,000 years in

    he previous chaper provides a ramework

    or he soil ypes presen. These soil ypes

    are srongly relaed o he aliude o hesoil hroughou is ormaion.

    Saring a he Norh Sea coas in he wes,

    we firs encouner a coasal dune area

    whose sands are marine in origin and

    deposied by onshore winds. This is a

    relaively narrow zone, bu o grea

    significance or sea deences. The dunes no

    only proec he low counry rom flooding,

    bu also provide a barrier beween he sal

    waer o he Norh Sea and he resh

    groundwaer inland.

    Jus eas o hese dunes is a zone wih

    surace marine clays ha covers boh he

    wesern and norhern par o he

    Neherlands. Furher inland is he ormer

    coasal swamp region. Given he significan

    excavaion o pea deposis hroughou he

    cenuries, he pea is no longer as wide-spread as i used o be. Wha ofen remains

    here a he surace is he marine clay which

    was originally a he base o he pea.

    In he cenral par o he Neherlands a zone

    wih river deposis can be ound. The main

    soil ype here is river clay. Away rom his

    cenral area, in he somewha higher

    regions o he norh, eas and souh, sandy

    soils occur, while in he norhern par o he

    counry boulder clay is ound. These

    deposis were ormed during he las ew ice

    ages, when he climae in he Neherlands

    was much colder and he large norhern ice

    shee occasionally reached halway ino he

    counry.

    Soils in he Neherlands, specifically in he

    clay areas, are rich and a grea source orcrop producion. Indeed, agriculure is an

    imporan aciviy in he Neherlands.

    Wih he indusrial revoluion a he end o

    he 19hcenury, he Neherlands changed

    rom a predominanly agriculural o an

    indusrialised sociey. As an agriculural

    sociey, he Duch predominanly lived in

    harmony wih he soil bu indusrialisaion

    made demands on he soil wih which i

    could no cope. The sel-susaining armer

    o he pas became a ciizen who no longer

    undersood he needs and capabiliies o

    he soil and ormer agriculural land

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    increasingly became urbanised and

    indusrialised.

    Public awareness o soil conaminaion

    sared in 1979 afer he soil in some major

    areas was ound o be conaminaed, as inhe residenial area o Lekkerkerk, which

    came as a shock o he public in he

    Neherlands. Given ha he exen o he

    problem had been underesimaed or quie

    a number o years, he governmen realised

    ha legislaion would be necessary o deal

    wih i. Forunaely, he governmen had

    sared o develop soil legislaion some

    years earlier, which resuled in he firsInerim Soil Remediaion Ac, passed in

    1983.

    Once he firs (ew) chemical dump sies had

    been ound, a broadly embraced eeling

    emerged among he Duch ha hey had o

    ake care o heir soil. Coincidence or no,

    his fited righ in wih a general growing

    environmenal awareness in he

    Neherlands, expressed in a srong

    environmenal movemen during he 1980s

    and 1990s.

    Expecing a firs only a limied number o

    conaminaed sies, i was assumed ha

    hese problems could be compleely solved

    in jus a decade. However, he appearance o

    more and more conaminaed sies, mainly

    local polluion bu occasionally also

    regionally ound diffuse conaminaion,

    raised he ear among expers o wheherany clean, unpollued, areas were lef in he

    Neherlands. We now know ha he

    majoriy o he rural and naural areas o he

    Neherlands are indeed sill unpollued.

    The quesion wheher he soil is

    conaminaed or no leads by definiion o

    he need or a ramework o esablish such

    a judgemen. For his he Duch Minisryo he Environmen developed he A, B

    and C values firs published in 1983 as par

    o he Inerim Soil Remediaion Ac.

    The concep o defining soil qualiy wih

    legislaive reerence values was so new ha

    he lis no only atraced grea ineres rom

    counries all over he world, i was even

    implemened in a number o oher

    counries. Since hen changes have been

    made o boh he numerical values, he

    erms used, and he role and uncion o

    hese erms. This is considered laer in his

    bookle (see he chaper The Duch soil

    qualiy sandards).

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    Soil ypes in he Neherlands

    (Brus et.al. Environmental Pollution 157 (2009), 2043 - 2052)

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    Developing a soil policy

    Wih he discovery o he firs major

    pollued sies in he lae 1970s, he Duch

    governmen realised ha i was due ime o

    develop a soil conaminaion policy.

    Bearing in mind ha a he ime only asmall number o conaminaed sies had

    been expeced, i was assumed ha hese

    problems could be compleely solved. The

    iniial policy approach, hereore, was ha

    all conaminaion should be eliminaed.

    Consequenly, a remediaed sie would be fi

    or all possible uure uncions, ranging

    rom heavy indusry o a domesic vegeable

    garden.

    Considering he urgency o dealing wih

    serious soil polluion, such as direcly under

    domesic housing, he firs Inerim Soil

    Remediaion Ac passed in 1983. I inro-

    duced he concep o a muliuncional

    soil wih he objecive o allowing every

    kind o reuse afer remediaion.

    In addiion, he Soil Proecion Ac came

    ino effec on 1 January 1987 wih he aim oprevening soil conaminaion. For

    siuaions where new soil conaminaion

    neverheless developed, he polluer pays

    principle was inroduced. The person or

    organisaion ha causes he soil conamin-

    aion is liable or is remediaion (see also

    he chaper Liabiliy: who pays he bill?).

    Since hen his principle has been embraced

    as a unding mechanism or soil reme-

    diaion in a large number o counries.

    In he Naional Environmenal Policy Plans

    o 1989 and 1993, he aim was sill o

    remediae all sies wih serious soil

    conaminaion beore 2010. However,

    acknowledging he discovery o more and

    more pollued sies, he Naional Environ-

    menal Policy Plan o 1997 amended he

    ambiions by saing ha all sies wih soilpolluion should be known beore 2005 and

    ha all sies wih serious risks shall be

    conrolled prior o 2030.

    As or new soil conaminaion, he principle

    o a muliuncional soil remained, as i

    does oday. However, or soil ha was

    conaminaed prior o 1 January 1987, he

    concep o a muliuncional soil was

    abandoned. In view o experiences over

    previous years, i was eviden ha he

    demands o he muliuncional soil

    concep or hisorical soil polluion ofen

    canno be me. Addiionally, echnological

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    developmens in he remediaion field

    inroduced a whole series o new mehods

    o deal wih a conaminaion. Consequenly,

    dig and dump was no longer he only

    possible soluion.

    For immobile conaminans he aim was oesablish a soil qualiy ha is fi or is uure

    land use. The new uncion o he soil,

    hereore, deermines he exen o which

    remediaion is necessary. For mobile

    conaminans he remediaion measures

    should be deermined by cos effeciveness,

    which migh imply he reamen o

    conaminaion over a longer period raher

    han rying o solve he problem wihin aew weeks or monhs.

    In 1994 he A,B and C values or he

    appraisal o he soil and groundwaer

    qualiy were replaced by a new se o

    risk-based acion values. The lowes level

    (Targe values) defines he qualiy o

    unpollued soils while he highes level

    (Inervenion values) defines when

    remediaion becomes necessary.

    On 1 January 1995, soil remediaion was

    included in he Soil Proecion Ac, hereby

    ending he Inerim Soil Remediaion Ac.

    In he ourh Naional Environmenal Policy

    Plan, published in 2001, he Duchgovernmen saes is inenion o end he

    ranser o environmenal coss o uure

    generaions. This policy saemen

    underlined he ambiion o 1997: in 2030 all

    sies wih serious soil polluion should be

    under conrol. In 2002 legislaion acually

    incorporaed he principles se by he

    Naional Environmenal Policy Plan o 1997

    wih respec o specific local circumsances.These circumsances mus deermine he

    remediaion measures necessary in order o

    obain a cos-effecive remediaion. I

    incorporaes a risk-based approach; he

    highes risk is given op prioriy.

    On 1 January 2006 a new Soil Proecion Ac

    came ino effec. I incorporaed he

    amended legislaion wih respec o

    uncional remediaion and inroduced a

    crierion or urgen remediaion.

    Finally, on 1 July 2008, he Soil Qualiy

    Decree and is accompanying Soil Qualiy

    Regulaion came ino effec. I was

    developed in ligh o idenified problems

    wihin exising legislaion. These were:

    1. he qualiy o he acual aciviies,

    2. he managemen o (slighly) pollued

    sies and,

    3. he environmenal sae use obuilding maerials.

    Consequenly, he Soil Qualiy Decree was

    developed rom a differen perspecive. No

    longer a sricly environmenal perspecive

    governs soil policy. Nowadays a balance is

    esablished beween he proecion o he

    soil and is use or economic and social

    purposes.

    Thereore he Soil Qualiy Decree consiss o

    hree pars. The firs par deals wih qualiy

    assurance whereby requiremens are se

    wih respec o he regisraion and

    assurance o he aciviies perormed by

    people and organisaions, boh in he field

    and in he laboraory. To pu i simply, i

    provides an answer o he quesion o

    wheher he repored aciviies have indeed

    been perormed in line wih regulaions and

    he acceped work procedures (like naional

    sandards). I helps o se a balance beween

    he coss and qualiy o he work in a highly

    compeiive marke.

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    The second par is he resul o he

    incorporaion o he Building Maerials

    Decree which originally became effecive on

    1 July 1999. Wih he esablishmen o he

    Soil Qualiy Decree, he Building Maerials

    Decree is no longer a sandalone decree.Alhough he Soil Qualiy Decree brough

    some changes, is conens are comparable

    wih he ormer Building Maerials Decree.

    I aims o regulae he environmenally sae

    use and reuse o sony building maerials.

    As such i provides an imporan field o

    applicaion or secondary building maerials

    like slags, ha would oherwise have had o

    be disposed o in he absence o environ-menally sae reuse regulaion.

    The hird par deals wih soil and dredged

    sludge. I ses soil qualiy crieria or

    differen soil uncions ha apply boh o

    he soil in-siu as well as o soil or dredged

    sludge ha will be applied on land. Seting

    soil uncion crieria aims o incorporae

    he soil qualiy as a crierion in sie

    redevelopmen and spaial planning. I

    provides a sound basis or susainable land

    managemen.

    Togeher wih he Soil Qualiy Decree also

    he financial means were made available o

    ulfil is policy goals.

    The Soil Qualiy Regulaion, which provides

    a echnical and pracical ranslaion o heSoil Qualiy Decree, conains an enirely

    new sysem o regulaory values or soil and

    dredged sludge, replacing he se o Targe

    and Inervenion values published in 2000.

    This se is now defined rom he perspecive

    o soil (re)use. As he Soil Qualiy Decree

    does no include legislaion wih respec o

    groundwaer, i does no change he Targe

    and Inervenion values or groundwaer sein 2000.

    Despie he ac ha he Soil Qualiy Decree

    does no include Inervenion values, hese

    sill exis. A parly updaed se o

    Inervenion values was published in 2013

    as hey coninue o be he crierion or he

    remediaion o conaminaed sies.

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    0

    100000

    200.000

    300.000

    400.000

    500.000

    600.000

    700.000

    19801989

    19972004

    20052007

    20092013

    Numbe

    rofsites

    Development of estimated workload

    425.000

    250.000255.000

    330.000

    615000

    35.000

    4.200

    Need for (urgent)

    remediation

    Potentially (seriously)

    contaminated

    205.000

    Estimated workload

    Since 1980, several investigations on the number o contam-

    inated sites were undertaken in the Netherlands, but many

    uncertainties remained. In 1998, the government decided on

    a new thorough investigation, based on the evaluation oenvironmental permits, knowledge o activities that are a

    threat to soil quality, and aerial photographs. This resulted in

    a number o 615,000 potentially contaminated sites in 2004,

    o which a workload o 425,000 potentially seriously con-

    taminated sites remained afer first screening. Further local

    site investigations had to reveal the scale o contamination

    and the possible need or remediation.

    Afer urther evaluation and soil remediation, the workload

    was adjusted downwards several times. In 2013 the remain-

    ing workload o potentially seriously contaminated sites was

    estimated at 250,000 sites. Approximately 1,600 o these

    sites need urgent remediation, because o human health

    risks (9%), risks rom transport o contaminants in ground-

    water (70%), ecological risks (8%) or combinations o those

    risks (13%).

    For the remaining sites o the workload, the soil contamina-

    tion is expected not to represent actual risks. Thereore, sus-tainable land management is sufficient and remediation can

    take place at a convenient moment in time, or example,

    when building activities or other soil-related activities take

    place. The number o remediated sites in The Netherlands

    rom 1980 until 2013 is approximately 30,000.

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    Sketch of the

    legislative frameworkThe previous chaper provided an overview

    o he developmens in Duch soil policy

    and he legislaion ha was derived rom i.

    This legislaion is no auonomous; i is

    embedded in more general environmenallegislaion. There is also legislaion or

    closely relaed environmenal comparmens

    like surace waer, groundwaer and wase.

    The overarching environmenal legislaion is

    provided in he Environmenal Managemen

    Ac ha firs came ino effec in 1993. The ac

    ses general regulaions or waer, air, soil and

    wase as well as he ramework or specificlegislaion. Wihin ha ramework, i allows

    he definiion o environmenal qualiy

    demands, including he se o regulaory

    values or soil and dredged sludge as

    incorporaed in he Soil Qualiy Regulaion.

    Furhermore, he Environmenal

    Managemen Ac provides he basis o

    enorce environmenal legislaion.

    Provinces, waer auhoriies, municipaliies

    and he naional governmen along wih isinspecion services ulfil differen asks in

    enorcing he environmenal legislaion.

    Due o he decenralisaion, he municipali-

    ies have an imporan role in enorcing he

    Soil Qualiy Decree. The governmen is

    empowered o impose a fine or o sop

    aciviies when he rules o he Soil Qualiy

    Decree are violaed.

    For a lo o aciviies in which soil is involved,

    a permi is necessary. And as he municipaliy

    is he compeen auhoriy, boh or

    providing hese permis as well as or

    enorcing he law, a conflic o ineress

    migh occur, paricularly in siuaions where

    he municipaliy isel develops hese

    aciviies. In order o ensure he auonomy o

    he legislaion enorcer, he EnvironmenalManagemen Ac demands he enorcers o

    adop ormal organisaional auonomy.

    Alhough in he Neherlands a major disposal

    roue or wase is incineraion, or par o he

    wase his is simply impossible.

    Consequenly, parial disposal o he wase in

    landfills is unavoidable. I he landfill is no

    equipped wih proper soil proecionmeasures, he wase maerial migh ge ino

    conac wih soil and groundwaer. This

    underlines he need or environmenal

    legislaion or wase and landfills. In his

    legislaive field he influence o overarching

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    European legislaion on Duch legislaion, in

    his case he Environmenal Managemen

    Ac, is clear, and he European Landfill

    Direcive ses he condiions.

    In 2006 he Themaic Sraegy or SoilProecion was published by he European

    Commission, he ocus poins o which have

    been aken in consideraion when develop-

    ing he Soil Qualiy Decree.

    Consrucion producs migh have adverse

    effecs on soil qualiy hrough he emission

    o hazardous subsances, somehing already

    ormally recognised in Duch legislaion wihhe publicaion o he Building Maerials

    Decree in 1999. In he European field his has

    also been recognised, resuling in he

    implemenaion o environmenal qualiy

    crieria in he Consrucion Producs

    Direcive and laer (2013) in he Consrucion

    Producs Regulaion. Again, when incorpor-

    aing he Building Maerials Decree in he

    Soil Qualiy Decree, accoun was aken ohese European developmens. This is

    imporan, since consrucion producs are

    quie ofen expored and impored so hey

    should mee he naional requiremens,

    irrespecive o wheher hey are produced

    inside or ouside he Neherlands. Having he

    same requiremens hroughou Europe, and

    using he same mehods o deermine he

    environmenal impac o hese producs, is

    vial o Duch and European indusry.

    I has already been menioned ha apar

    rom he Soil Qualiy Decree, here is also a

    Soil Qualiy Regulaion. In ac, having a

    regulaion in addiion o he decree is a

    general principle in Duch Environmenal

    legislaion. For he whole legislaive package,

    a comparison could be made wih a pyramid.

    On op here is he EnvironmenalManagemen Ac. A second layer is ormed by

    decrees or differen comparmens, o which

    he Soil Qualiy Decree is one. The hird layer

    conains a regulaion or each o hese

    decrees ha provides more echnical and

    pracical rules wih respec o he imple-

    menaion o ha decree. The regulaion

    isel reers o a whole series o proocols,

    sandards as well as cerificaion andaccrediaion schemes. These documens can

    be seen as he ourh and las layer o he

    pyramid. The documens in his las layer are

    no direcly published by he governmen bu

    are developed and mainained by naional

    insiues like he Neherlands

    Sandardisaion Insiue (NEN) and he

    Foundaion Inrasrucure or Qualiy

    Assurance o Soil Managemen (SIKB). Laer

    in his bookle he role o hese bodies will

    be described in more deail (see he chaperTechnical guidelines).

    When i comes o remediaion, he unding

    o he coss is a key acor. Nowadays, since

    he remediaion o he majoriy o sies is due

    o changes in he sies use, spaial planning

    has become an imporan acor.

    However, using he possibiliies ha are

    offered by he financial provisions in he SoilRemediaion Decree, he governmen also

    subsidises he soil remediaion o specific

    indusries. An imporan provision herein is

    an agreemen beween he governmen and

    he umbrella organisaion or a specific ype

    o indusry wih respec o he remediaion o

    conaminaed soils.

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    Overview of curren Duch soil legislaion, ogeher wih relaed European Direcives

    Remediation

    Prevention and sustainable land management

    Environmental Management Act

    Soillegislation

    Wastelegislation

    Water quality

    legislation

    Air quality

    legislation

    Compulsory Soil

    Investigation atIndustrial Sites Degree

    Soil QualityDecree

    Soil QualityRegulation

    Quality

    Assurance

    Construction

    productsRegulation

    Landfill ofwaste Directive

    Soil Protection Act

    Discharge(Soil Protection)

    Decree

    Household WaterDischarge Decree

    Landfill(Soil Protection)

    Decree

    Infiltration(Soil Protection)

    Decree

    Exemptions Decreefor Landfilling outside

    Installations

    Cases of non-duty

    to report SoilRemediation Decree

    Designation

    Competent AuthoritiesSoil Protection Decree

    Soil Clean-upAssessment

    Regulation 2006

    Uniform

    RemediationDecree

    UniformRemediation

    Regulation

    Financial Provisions

    Soil RemediationDecree

    Registration Limitations(Soil Protection Act)

    Regulation

    Soil RemediationCircular 2009

    Sewage sludgeDirective

    Water Act

    Water

    Framework

    Directive

    Groundwater

    Directive

    Industrial

    Emissions

    Directive

    Environmental

    Liability

    DirectiveBuilding

    materials

    Soil and

    Dredgedsludge

    2018 Environment and Planning Act

    European

    Directivesand Regulation

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    Future developmentsin soil policy

    A he momen he Duch environmenal

    regulaion and legislaion is being rans-

    ormed wih he objecive o aciliae

    spaial developmen by simpliying and

    combining many exising acs and decrees.As a consequence mos o he

    Environmenal Managemen Ac (in oal 15

    exising laws) will be inegraed in he

    Environmen and Planning Ac.

    Expecaions are ha he Environmen and

    Planning Ac will be empowered in 2018.

    Currenly, he major responsibiliy or soil is

    being decenralised. Wih a covenan(2010-2015) beween he sae governmen,

    provinces, municipaliies and waer

    auhoriies, ambiions were ormulaed

    concerning remediaion and susainable

    use o he subsurace. Arrangemens were

    made o reach hese goals ogeher. Wih

    he covenan, he major responsibiliy or

    soil is decenralised. A succeeding covenan

    is now being prepared and will be effecive

    in 2016. One o he ambiions o he newcovenan is o involve he privae secor in

    he new arrangemens.

    The ransiion in soil regulaion can be

    divided in wo main sreams:

    1. Taking charge of the remediation

    operation

    In he firs covenan period, many siesare invesigaed and remediaed,

    including mos o he urgen sies. The

    nex sep is he managemen phase,

    aimed a conaminaions ha canno be

    excavaed, and ha have a risk o spread.

    This phase ocuses on innovaive

    managemen o hese sies, e.g. on he

    applicaion o differen in-siu echniques

    and area based managemen o conam-

    inaed groundwaer. The link wih spaialdevelopmen is vial o he uure o soil

    remediaion in he Neherlands, as new

    ways o soil usage will iniiae addiional

    unding or remediaion aciviies,

    especially i hese can be combined wih

    anoher land use, e.g. aquier hermal

    energy sorage (ATES). Soil remediaion

    unrelaed o spaial developmen is

    becoming redundan and is replaced byarea based susainable soil managemen.

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    2. Using the possibilities of the

    subsurface

    Objecive o he amendmens is o ocus

    on he susainable use o he subsurace.

    This means ha he use o he subsurace

    canno be seen separaed rom spaialdevelopmens and socieal challenges

    such as climae change, susainable

    energy, (ground)waer managemen and

    economic developmens. The covenan

    addresses differen uncions o he

    subsurace. Themes such as susainable

    use o resources (eg. sraegic ground-

    waer resources) and energy (shale gas,

    effecs o gas winning, soil energy) areopics o ineres.

    Because no all aspecs can be arranged on

    he local or regional level, sraegies are

    being prepared on he spaial planning o

    he subsurace. In 2012 his was done or

    subsurace pipes. In 2013 he naional

    governmen sared, in cooperaion wih

    local and regional governmens, hepreparaion o a naional sraegy or he

    subsurace STRONG. In STRONG decisions

    will be made wih respec o spaial

    planning wih a naional ineres. I also

    should help local or regional governmens

    o make decisions on spaial planning, boh

    in urban and rural areas. The STRONG is

    planned o be ready in 2015. A sraegy or

    shale gas (also expeced 2015) will be an

    inegral par o STRONG.

    The envisaged ransiions will involve

    differen governmenal organisaions as

    well as privae paries and research

    organisaions. This collaboraion aims o

    come o agreemen on he use o he

    subsurace, he generaion o knowledge

    and he necessary financial arrangemens.

    Final objecive is he implemenaion osusainable use and managemen o he

    subsurace in daily pracice.

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    Many parties involved

    During he process o ideniying and

    remediaing a conaminaed sie, he

    number o involved paries easily goes up o

    16. This underlines he need o good

    communicaion. An example:

    The owner o he (poenially) pollued sie

    is obviously he firs pary ha is involved. I

    migh be ha or a specific ype o indusry

    (e.g. drycleaners, uel-filling saions), an

    umbrella associaion is delegaed o deal

    wih he specific soil problems o he secor.

    I so, i will obviously be involved.

    A consulan will be conraced o perorm

    an invesigaion o he sie alhough he

    acual fieldwork will be delegaed o

    sampling specialiss. The resuling samples

    will hen be ranspored o a specialised

    environmenal laboraory. The resuls o he

    lab analyses will go o he consulan who

    will use i o wrie a repor or he person or

    organisaion ha conraced he consulan.

    I here is serious soil conaminaion due ohe exen and concenraions ound, a

    Main Invesigaion will be necessary. A his

    sage a leas he compeen auhoriy will

    be inormed.

    While he same consulancy firm may

    perorm he Main invesigaion, ofen

    anoher consulancy firm is conraced.

    The compeen auhoriy mus be inormed

    abou wha was ound as well, o ake a

    ormal decision wih respec o he

    remediaion o he sie, i necessary. For he

    developmen o a Remediaion Plan a

    consulan will be conraced again, hough

    his is rarely he same consulan as involved

    in he invesigaion phase. The Remediaion

    Plan will be announced in a local news

    paper by he compeen auhoriy, in ordero inorm neighbouring residens.

    The compeen auhoriy will ake a ormal

    decision wih respec o how he sie will be

    remediaed. Then a conracor (or a

    combinaion o conracors ) will be

    involved in he acual remediaion. The

    remediaion mehod applied will deermine

    i groundwaer needs o be reaed on sieand i pollued soil will be excavaed. I he

    later, he echnical and financial easibiliy

    o cleaning ha soil will deermine wheher

    he soil is cleaned or aken o a landfill.

    Slighly pollued soils migh be reused on

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    sie, or are ranspored o a soil recycling

    aciliy or applicaion elsewhere. Landfilling

    is only allowed afer a check by a govern-

    men agency.

    During he remediaion, a consulan will

    ensure ha he environmenal goals o he

    remediaion are acually me. Cerainly

    during he remediaion phase, neighbouring

    residens will have o be inormed abou he

    remediaion and is progress.

    In order o define he final siuaion

    ollowing remediaion, an evaluaion repor

    will be produced. The resul o he remedi-

    aion will have o be approved by hecompeen auhoriy. I any pos-remedi-

    aion care is necessary, his will also require

    a specific decision by he compeen

    auhoriies.

    In pracice, he consulans are in charge o

    all pracical work and consequenly hey bear

    a large degree o responsibiliy. This is

    recognised in he Soil Qualiy Decree inwhich qualiy assurance is an inegral par.

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    Decisions of thecompetent authority

    The compeen auhoriy plays a vial ormal

    role in he appraisal and remediaion o

    conaminaed sies. The Soil Proecion Ac

    designaed he larger Duch municipaliies

    and he provinces as compeen auhoriy.A he various sages o dealing wih a

    conaminaed sie, a ormalised process will

    lead o a ormal decision o he compeen

    auhoriy.

    Depending on he complexiy o he local

    siuaion, wo differen processes exis.

    In a complex siuaion, boh he MainInvesigaion (see he chaper Invesigaing

    he soil qualiy) as well as he developmen

    o a Remediaion Plan sars wih a ormal

    noificaion o he compeen auhoriy.

    Based on his, he compeen auhoriy will

    provide a draf decision which, or a period

    o six weeks, will be available or commens

    by people and/or organisaions ha have an

    ineres in he specific sie. A ormal

    decision will be aken by he compeenauhoriy 15 weeks afer receip o he

    noificaion. Ineresed paries can sill

    appeal o he Sae Council agains he

    ormal decision.

    Afer he remediaion is finished, he com-

    peen auhoriy mus receive he evaluaion

    repor. For pos-remediaion care, he same

    applies o he repor on he pos-

    remediaion care programme. Based onhe repor(s), he compeen auhoriy will

    come o a final decision, eigh weeks afer

    an evaluaion repor and six monhs or a

    pos-remediaion care programme. Again,

    paries wih an ineres in he specific sie

    can appeal wihin six weeks. I he appeal is

    rejeced, a final appeal can sill be made o

    he Sae Council.

    The previous procedure akes a considerableamoun o ime. This is accepable or

    complex siuaions bu or less complex

    siuaions i could hinder urher develop-

    mens on he sie. In ac, he procedure

    could ake more ime han he sie

    invesigaion and remediaion isel. For

    less complex siuaions, hereore,

    a naional uniorm regulaion has been

    provided by he naional governmenwhereby he compeen auhoriy needs o

    be noified o he ac ha remediaion will

    ollow he simplified procedure. A sandard

    orm is available or his noificaion.

    The compeen auhoriy should decide

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    wihin five weeks i he simplified procedure

    can indeed be ollowed. There is no possibil-

    iy o appeal agains his decision. I he

    compeen auhoriy does no respond wihin

    five weeks, he simplified procedure is

    implicily acceped.

    Afer remediaion is compleed, a sandard

    evaluaion orm is provided o he compeen

    auhoriy, based on which a ormal decision

    on he accepance o he remediaion resul

    should be made wihin eigh weeks. Paries

    involved have he righ o appeal o he Sae

    Council.

    The compeen auhoriy no only has a role

    in he remediaion par o he Soil Proecion

    Ac, i also has a specific role when i comes

    o prevenion o soil polluion.

    Environmenal permis demand proecive

    measures whenever aciviies migh pose a

    hrea o he soil qualiy. Obviously his

    relaes o he European IPPC direcive

    (inegraed polluion prevenion andconrol).

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    Although the polluterpays principle is still

    valid, for practical and

    juridical reasons this

    principle cant always

    be followed, while

    stimulation of theremediation process

    also triggers continued

    governmental

    funding.

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    Liability: who pays the bill?

    As menioned beore, he polluer pays

    principle has already been embedded in

    Duch soil legislaion since 1987 when

    liabiliy became he key erm in recovering

    he cos o soil remediaion. Despie ha,he need persiss or soil remediaion

    unding rom he naional governmen.

    According o jurisprudence, i is generally

    assumed ha beore 1975 people or

    companies could no have been aware o

    he ac ha aciviies migh conaminae

    he soil. Consequenly, all remediaion coss

    or a conaminaion caused beore ha daeare, in principle, covered by he naional

    governmen. This does however no

    compleely exclude conribuions rom

    companies in respec o conaminaion

    caused prior o 1975. I he polluer had

    already been aware o he severe danger o

    conaminaing subsances, and puting

    hese subsances direcly or indirecly ino

    he soil could already have been seen as a

    culpable ac, he polluer pays principle issill valid.

    Generally speaking, prior o 1975, an exper

    working wih chemicals could no have

    been aware o he adverse effecs hese

    chemicals could have on he soil qualiy.

    There were jus oo ew scienific publica-

    ions abou soil conaminaion.

    Since 1975, hese publicaions sared oemerge more requenly, so an exper

    should have aken noe and measures o

    proec he soil. I no, a company employ-

    ing such expers is regarded as liable or he

    soil polluion i caused.

    The availabiliy o exper inormaion,

    however, sill does no imply he availabiliy

    o common knowledge abou soil conam-

    inaion. This changed wih he publicaion

    o he Soil Proecion Ac in 1987. Thepresens o legislaion implied ha, a leas

    in legal erms, everybody in he Neherlands

    should be aware o he need o proec he

    soil agains conaminaion.

    During he grey area beween 1975 and

    1987, i is acceped ha non-expers were

    sill unaware o exising soil conaminaion.

    For propery and premises, or example,achieved beween 1975 and 1987 where he

    buyer was unaware o (he risk o ) soil

    conaminaion, he governmen may sill

    und he remediaion.

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    In order o simulae he remediaion o

    indusrial sies and o achieve ha all sies

    wih serious risks are conrolled prior o

    2030, here are our differen financial

    regulaions under he Financial Provisions

    Soil Remediaion Decree. Apar rom

    simulaing he acual remediaion, hese

    also aim o preven bankrupcy o oherwise

    financially sound companies due o he

    coss o soil remediaion. The governmenal

    financial suppor under hese regulaions

    can go up o 70% o he remediaion coss.

    Wha is he cos or soil remediaion in he

    Neherlands? In recen years, he naionalgovernmen has spen around 150 million

    euros a year on soil remediaion. In

    addiion, he annual marke urnover in

    recen years is he same as governmen

    spending, which means oal annual

    expendiure o around 300 million euros!

    Apar rom soil remediaion coss, here are

    also coss involved in he susainable landmanagemen or clean or slighly pollued

    soils and sedimens.

    Coss relaed o he acual use or reuse o

    soil maerial will be covered by he pary

    responsible or is use or reuse: he coss o

    he soil isel, he machinery necessary o

    relocae he soil maerial and coss relaed

    o sampling and analysis o he soil. In

    addiion o ha here are coss relaed o

    he developmen and use o Soil Qualiy

    Maps (see he chaper Knowing he soil

    qualiy).

    These coss are parly covered by boh

    municipaliies and by spaial redevelop-

    men iniiaives. These coss are hereore

    an inegral par o oher processes and less

    well known. Neverheless, he expendiure

    is probably comparable o ha o soilremediaion.

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    S il f i d bi i

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    Soil functions and ambitions

    The Soil Qualiy Decree generically defines

    wha he Duch wan o achieve wih respec

    o heir soils as well as provides opporuni-

    ies or local auhoriies o deviae rom

    hese general principles. The local auhoriy

    is encouraged o ormulae is own soil

    qualiy aims in a Soil Ambiion ha may

    relae o all he soil he compeen auhoriy

    is responsible or, or may be limied o a

    local spaial developmen. The Soil

    Ambiion direcly relaes o he curren and/

    or uure uncion o he soil: he land use.

    The compeen auhoriy - he municipal-

    iy, he province or he waer auhoriy - isresponsible or he ormal accepance o

    he Soil Ambiion. However, while a

    propery developer may also ake he

    iniiaive o define a local Soil Ambiion or

    he area he is planning o (re)develop, he

    compeen auhoriy sill has o ormally

    accep i.

    The Soil Ambiion is ormulaed in a local

    Soil Managemen policy documen which

    concreises he local Soil Ambiion.

    Apar rom he chemical qualiy, he soil is

    also defined in erms o is physical propery

    and ecological properies, he geological,

    archaeological and culurally hisoric value,

    he soil hreas (e.g. erosion, depleion,

    salinisaion) and he use o he soil or oher

    purposes (e.g. mining, producion odrinking waer, sorage capaciy). I is up o

    he compeen auhoriy o define he erms

    o local relevance, all o which mus be

    aken ino accoun when developing a local

    Soil Ambiion. This should be done in close

    cooperaion wih responsible paries like

    anoher uni wihin he communiys civil

    service, or he waer auhoriy, or example.

    The curren soil qualiy can be mainained

    or enhanced. Taking he opion o main-

    aining he soil qualiy, local deerioraion is

    allowed, somehing ha migh prove

    necessary in order o obain sufficien

    flexibiliy in he local soil managemen.

    Oherwise he soil qualiy could be an

    obsacle or urher spaial developmen. In

    ac, when defining he Soil Ambiion, he

    compeen auhoriies should consideruure spaial developmens. This makes he

    relaionship beween he soil uncion and

    he soil qualiy angible - i uses he

    opporuniies he soil presens.

    When a municipaliy decides o implemen

    S il A bi i ll h il i hi h

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    a Soil Ambiion or all he soil wihin he

    municipal borders, i is advised o

    co-develop his Soil Ambiion wih he

    neighbouring municipaliies, he province

    and he waer auhoriy. This collaboraive

    procedure will resul in more opions o

    reuse soil and sedimen simply because iallows he soil o also be reused in one o

    he neighbouring municipaliies.

    The curren or uure soil uncion (e.g.

    agriculure, residence, indusry) deermines

    wha kind o soil qualiy is necessary. In is

    urn, he prevailing soil qualiy will

    deermine which uncions are possible.

    I he combinaion o soil uncion and soil

    qualiy does no fi, measures have o be

    aken. In shor: he soil should be fi or is

    use.

    I has be come possible o define he Soil

    Ambiion due o he acquisiion o a

    subsanial amoun o soil qualiy daa over

    he years. The Duch now know heir localsoil qualiy.

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    Knowing the soil quality

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    Knowing the soil quality

    The whole concep o susainable land

    managemen or clean and slighly pollued

    soils is based on an exensive knowledge

    abou he soil qualiy. Duch soil has already

    been invesigaed or hree decades, no only

    a conaminaed sies bu also a unconam-

    inaed sies. Theoreically, his implies ha

    here is a huge amoun o soil daa available.

    In pracice, however, his is misleading since

    older daa end no o be digially available

    and soil daa are considered o be valid or a

    period o only five years. Neverheless, mos

    o he soil daa ha are valid are indeed

    digially available.

    As already menioned, all poenial conam-

    inaed sies were idenified in 2005. This

    resuled in a naionwide map ha is publicly

    accessible hrough inerne. I allows

    anyone, boh he lay and proessional public,

    o ocus on a specific sie in he Neherlands

    and obain is conaminaion saus. One can

    simply find ou wheher a sie is suspeced o

    soil conaminaion, is under invesigaion or

    has been remediaed. The naionwide map

    does no provide acual soil qualiy daa. For

    his inormaion, one has o conac he

    municipal auhoriies. Obviously, as his map

    ocuses exclusively on (poenially) conam-

    inaed sies, i does no provide soil qualiy

    inormaion on he major par o he

    Neherlands.

    More deailed inormaion on he soil

    qualiy is conained in he Soil Qualiy Maps

    primarily produced and mainained by he

    municipal auhoriies. These Soil Qualiy

    Maps are an essenial par o he local soil

    managemen aim ha is par o he local

    Soil Ambiion (see he chaper Soil

    uncions and ambiions). These Soil

    Qualiy Maps are based on he available soil

    daa and may perain o he whole, or par,

    o he municipal area. For example,

    agriculural land may be excluded i

    insufficien soil qualiy daa are available.

    The Soil Qualiy Maps provide generalised

    soil qualiy inormaion or specified zones

    wihin municipal borders. These zones

    end o be disinguished by he municipal-

    iys developmen hisory. Even in heabsence o soil qualiy daa, a disincion

    in soil qualiy may be expeced beween an

    area developed beween 1900 and 1940 and

    an area developed, or insance, only in

    1990.

    The generalised soil qualiy is based on daa A naional guideline is available or he provides soil qualiy sandards (see he

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    The generalised soil qualiy is based on daa

    available wihin each zone, excluding

    pollued sies wihin hese zones.

    The main role o hese Soil Qualiy Maps is

    o enable he reuse o soil wihou he need

    or analysis. As such, i significanly reduceshe coss associaed wih soil reuse and

    gains ime as here is no need o wai or he

    resuls o analyses. The local Soil Ambiion

    will deermine he zones rom which soil

    could be expored o oher zones, and

    which zones can impor soil. The general-

    ised soil qualiy o he zone is he deermin-

    ing acor here. I he Soil Ambiion is

    predominanly defined rom an environ-

    menal proecion perspecive, he resul

    will limi he possibiliies o exchange soil

    beween zones. This will mean ha more

    soil invesigaions will be necessary han or

    a Soil Ambiion ha ries o maximise he

    spaial developmens. So, even wih a raher

    sric environmenal proecion objecive,

    he Soil Ambiion does no rule ou all hesoil ranspor beween zones. I jus implies

    ha soil los require esing (ar) more ofen

    prior o reuse in order o deermine wheher

    he qualiy o a specific soil lo allows i o

    be reused a he designaed locaion.

    A naional guideline is available or he

    developmen o Soil Qualiy Maps.

    Soil qualiy inormaion can also be obained

    hrough naional and provincial invenories.

    This inormaion concerns he acquisiion o

    daa on a naionwide or province-wide scaleor he purpose o knowing he general soil

    qualiy in he Neherlands and he changes

    herein over ime.

    Finally, inormaion on he Duch soil

    qualiy has been obained rom a naion-

    wide invesigaion o he background

    concenraions. This paricular sudy is o

    imporance as i provides he basis or he

    background values ha are now par o he

    se o legislaive soil qualiy sandards (see

    he chaper The Duch soil qualiy

    sandards). The 100 locaions hroughou

    he Neherlands or his naionwide sudy

    were seleced on he basis o inormaion

    on curren land use and using a saisical

    sampling design. Composie samples wereaken a hese locaions o represen he soil

    qualiy o he op soil (0 - 10 cm) and on an

    undisurbed deph (50 - 100 cm). All

    composie samples were analysed or all 252

    subsances or which Duch legislaion

    provides soil qualiy sandards (see he

    chaper The Duch soil qualiy sandards).

    The analysis o such a large amoun o

    subsances in 200 soil samples had never

    been perormed beore in he Neherlands.

    For he firs ime, naionwide conclusions

    could be drawn wih respec o hebackground concenraions.

    Deailed soil qualiy inormaion is obviously

    no available or all 252 subsances. The Soil

    Qualiy Maps, in principle, only cover he

    subsances or which he Background value is

    requenly exceeded. The definiion o his

    sandard se o subsances is based on

    combining:

    The Background values derived rom he

    disribuion o background

    concenraions.

    An exensive daabase o soil qualiy

    measuremens or non-suspec soils as

    perormed by he environmenal

    laboraories.

    The policy decision ha no more han 5%o he rouine measuremens o non-

    suspec soils migh exceed he

    Background values.

    I here is a larger han 5% chance ha a

    rouine measuremen o a non-suspec soil

    exceeds a Background value, rouine esing Contaminated sites that need urgent remediation, 2013

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    exceeds a Background value, rouine esing

    o ha subsance is necessary.

    Accordingly, he sandard se o subsances

    comprises barium, cadmium, cobal,

    copper, mercury, lead, molybdenum, nickel,

    zinc, sum-PCBs, sum-PAHs and mineral oil.In addiion o hese subsances, he

    percenage clay and organic mater also

    needs o be deermined in each sample.

    Contaminated sites that need urgent remediation, 2013

    1

    10

    50

    100

    Number of sites

    per municipality

    Total number of sites: 1643

    Conaminaed sies suspeced o need urgen

    remediaion (2013) for he individual municipaliies.

    (RIVM)

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    Water and sediments

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    Water and sediments

    Like he close relaion beween soil and

    groundwaer in he Neherlands, ground-

    waer is an inegral par o he Duch

    regulaions or soil.

    The chemical equilibrium beween soil and

    waer implies ha he qualiy o he soil

    deermines he qualiy o he groundwaer

    and, when presen, he surace waer.

    Specifically or he wesern par o he

    Neherlands, here is a close relaionship

    beween he groundwaer and soil. Ofen

    he sauraed zone is (ar) less han a mere

    away rom he soil surace, implying hawhere he soil is conaminaed, he

    groundwaer will also be conaminaed.

    Groundwaer in he Neherlands is he main

    supply o drinking waer, ogeher wih

    waer rom he rivers. Surace waer is also

    direcly used or crop irrigaion and

    drinking waer or catle, and serves an

    imporan ecological and recreaional role.

    To some exen he conaminaion o

    groundwaer and surace waer poses a

    bigger hrea o human healh han soil

    conaminaion. The risk o direc conac

    wih conaminans, eiher hrough skin

    conac or ingesion, is much greaer or

    waer han or soil. Alhough he concenra-

    ions in waer are ar less han in soil, his

    highlighs he imporance o proecing he

    groundwaer and surace waer qualiy.

    Soil qualiy is ofen defined in erms o he

    concenraions o chemical subsances like

    heavy meals, mineral oil and PAHs. And

    depending on he solubiliy, hese sub-

    sances also govern he groundwaer and

    surace waer qualiy. In addiion o hese

    subsances, nuriens are o specific

    relevance o groundwaer and surace waer

    qualiy.

    For example in he souhern par o he

    Neherlands, inensive catle breeding on

    sandy soils has resuled in exensive

    nirificaion o he groundwaer. An

    overload o nuriens in he surace waer

    causes europhicaion. Algae can make he

    surace waer less atracive or recreaional

    purposes, and some algae even pose a direcrisk o human healh. Consequenly,

    measures have been aken o diminish he

    release o nuriens ino groundwaer and

    surace waer.

    Being a dela area, sedimens are deposied

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    in he Neherlands. In order o allow a

    sufficien waer flow, hese sedimens need

    o be dredged on a regular basis. Subsances

    dissolved in he surace waer will ofen end

    up in he sedimens. Where surace waer

    serves o drain he surrounding land,seepage o groundwaer will also influence

    he sedimen qualiy, which ofen alls shor

    o he desired level.

    However, as long as he qualiy o he

    sedimens are comparable o he qualiy o

    he soil on he adjacen land, he dredged

    sedimens can be disribued here. This is

    imporan as he sedimen hen conribues

    o elevaing he land ha would oherwise

    sink slowly below he waer level o he

    polder. Would i no be possible o use he

    sedimens on he adjacen land, he waer

    level o he polder would need o be

    adjused downwards. In pea areas, he soils

    would hen coninue o setle, resuling

    again in he need or urher adjusmen ohe waer level. Ulimaely, ha would cause

    severe problems wih he inrasrucure and

    buildings in he polder.

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    Technical guidelines

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    Technical guidelines

    In he pas, prior o he Soil Qualiy Decree,

    he aims or he soil were prety much

    defined by he naional governmen. Since

    he early 1980s, he predominanly

    pioneering naure o soil remediaion

    business has changed ino a proessionalsecor. Wih he developmen o he Soil

    Qualiy Decree his proessionalism has

    been acknowledged. The main responsibil-

    iy or mainaining soil qualiy shifed rom

    naional governmen o he municipal

    auhoriies. A he same ime, he develop-

    men and mainenance o echnical

    guidelines are now primarily a responsibil-

    iy o he organisaions ha acually use

    hese echnical guidelines. As such, he role

    o he consulans who operae in his field

    has become more dominan.

    Consulans help he communiies o

    develop heir Soil Ambiion (see he chaper

    Soil uncions and ambiions) and ake

    care o he developmen and mainenance

    o he sandards and proocols necessary o

    perorm he work. In developing hesedocumens, he consulans generically

    define he qualiy ha should be realised. A

    he same ime, heir day-o-day perorm-

    ance has o comply wih he qualiy

    demands o hese documens.

    Obviously, he echnical definiion o he

    aspired qualiy is no he ask o a single

    consulan. Here he modus operandi o he

    Neherlands Sandardisaion Insiue (NEN)

    seps in. This implies ha he developmen

    o sandards, proocols and guidelines is a

    process ha involves all paries concerned:

    he legislaor, he regulaor, provinces,

    waer auhoriies, municipaliies, indusry,

    consulancy firms, environmenal labora-

    ories and ohers.

    A large se o sandards, proocols andguidelines is available or defining he

    echnical qualiy o he work. Almos all he

    seps o he process are ormalised by hese

    documens, or which here are hree main

    caegories:

    1. guidelines published by or on behal o

    he naional governmen;

    2. sandards published by he Neherlands

    Sandardisaion Insiue (NEN);

    3. cerificaion and accrediaion schemes

    published by he Foundaion

    Inrasrucure or Qualiy Assurance o

    Soil Managemen (SIKB).

    Apar rom naional developmens, he

    N h l d S d di i I i l

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    Neherlands Sandardisaion Insiue also

    operaes specifically a an inernaional

    level, parly wihin he European Commitee

    or Sandardisaion (CEN) and parly wihin

    he Inernaional Organisaion or

    Sandardisaion (ISO). On boh levels aTechnical Commitee deals wih he

    developmen o sandards or soil characer-

    isaion. Boh commitees, CEN/TC 345 and

    ISO/TC 190, are chaired by he Neherlands.

    ISO/TC 190 has published some 160

    sandards, covering erminology, codifica-

    ion, sampling, chemical, biological and

    physical mehods as well as soil and sieassessmen. These sandards are available

    or worldwide use hrough he naional

    sandards insiues.

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    Risk assessment

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    Risk assessment

    Human exposure modelling is he basis o

    human healh risk assessmen in many

    counries. Two human exposure models

    have been developed in he Neherlands.

    The CSOIL model deermines exposure o

    conaminaed erresrial soils, while heSEDISOIL model deermines exposure o

    conaminaed sedimens. These models

    recognise hree elemens:

    conaminan disribuion over he soil or

    sedimen phases;

    conaminan ranser rom (he differen

    phases o ) he soil and sedimen ino

    so-called conac media;

    direc and indirec exposure o humans.

    A human exposure calculaion combined

    wih oxicological reerence values resuls in

    he risk characerisaion, ha is, he risk

    appraisal o he conaminaed sie. I is

    imporan o define he imerame or which

    he risk assessmen is applicable, since

    acors ha influence human healh risks will

    change over ime. Moreover, calculaed

    exposure and criical exposure (oxicologicalreerence value) should be consisen wih

    regard o he duraion and oxicologically

    relevan exposure period in he lieime o

    he exposed populaion. Equaions or all

    relevan exposure pahways have been

    included in he CSOIL exposure model. The

    main exposure pahways are:

    exposure hrough soil ingesion afer

    hand - mouh conac (mainly relevan or

    immobile conaminans);

    exposure hrough crop consumpion

    (mainly relevan or mobile

    conaminans);

    exposure hrough inhalaion o indoor

    air (mainly relevan or volaile

    conaminans).

    Addiionally, exposure hrough he

    inhalaion o soil paricles, dermal upake

    via soil maerial, groundwaer consumpionand inhalaion o air during showering may

    in specific siuaions conribue o he

    exposure o paricular conaminans.

    Exposure hrough soil ingesion is

    calculaed according o soil ingesion inake

    raes or children and aduls. For sie-

    specific applicaions, he acual bioavailab-

    iliy in he human body is deermined in he

    Neherlands using he in-viro IVD model or

    he Unified Barge Model. Plan-soil

    concenraion relaionships are used or

    assessing exposure hrough crop consump-

    ion. For sie-specific applicaions a

    our-iered approach is used, including

    based on acual risks o human healh, he

    soil ecosysem and ood saey as well as risks

    sie-specific assessmen o ecological risks on

    he basis o hree lines o evidence: soil

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    our iered approach is used, including

    calculaions o he accumulaion o

    conaminans in vegeables and a measure-

    men proocol. The VOLASOIL model has

    been developed o assess he risk hrough

    vapour inrusion in case o soil or ground-waer conaminaion wih volaile conamin-

    ans. This model enables he sie-specific

    indoor air concenraion o be indicaively

    assessed as a uncion o ype and posiion-

    ing o he conaminans, building and soil

    characerisics, and groundwaer deph.

    The SEDISOIL exposure model includes he

    relevan exposure pahways or sedimenssuch as exposure hrough fish consumpion,

    dermal upake when swimming and he

    ingesion o waer and pariculae mater

    during swimming.

    By law, he web-based Sanscri decision

    suppor sysem is used in he Neherlands o

    decide on he urgency o remediaion. The

    Risk Toolbox (RTB) is available o develop

    susainable soil qualiy objecives in case o

    slighly conaminaed soil. Boh insrumens

    suppor sie-specific risk-based decisions and

    risk-based land managemen. Decisions are

    soil ecosysem and ood saey as well as risks

    arising rom conaminan ranspor. For each

    o he proecion arges a iered approach is

    ollowed. In each progressive ier he

    assessmen becomes less conservaive, is

    based on more sie-specific inormaion and,hence, is more complex, ime-consuming

    and ofen more expensive. When unaccep-

    able risks in a specific ier canno be

    excluded, an assessmen in he ollowing ier

    has o be perormed. The underlying

    principle is: simple when possible and

    complex when necessary.

    The human healh risk assessmen module inboh decision suppor sysems is based on

    he CSOIL exposure model. I is generally

    recognised ha sie-specific risk assessmen

    requires an inelligen combinaion beween

    exposure calculaions and measuremens in

    conac media. Thereore, his module offers

    he possibiliy or measuremens in conac

    media like indoor air, vegeables and indoor

    dus. In specific cases, he possibiliy o

    biomonioring exiss, e.g. measuring lead in

    blood or arsenic in oe nails.

    Soil ecosysem risks are derived using he

    iered TRIAD approach ha enables he

    he basis o hree lines o evidence: soil

    chemisry, oxiciy and ecology. The our-ier

    approach o assess he risks due o conamin-

    an ranspor in groundwaer is as ollows:

    Tier 0 is a qualiaive analyses o possible risk

    due o groundwaer ranspor. Tier 1 involvesa simple generic conaminan ranspor

    calculaion based on a conservaive scenario.

    In Tier 2, a more complex sie-specific

    calculaion is perormed. Finally, in Tier 3,

    monioring aciviies can be perormed and

    complex numerical models can be used.

    Furhermore, leaching is aken ino accoun

    in his ier, and special atenion is given o

    Toal Peroleum Hydrocarbons (TPH), arequenly occurring conaminan in

    groundwaer.

    Distribution over soil fractions

    representativeSOIL CONTENT

    Contaminated sites that needUrgent remediation, 2013Total number of sites: 1643

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    chemistry

    toxicity ecology

    risk

    The TRIAD approach for scienifically based and efficien sie-specific ecological risk assessmen

    Transfer processes

    Indirect exposure

    ingestion, inhalationdermal uptakeSOIL

    intake DRINKINGWATER, dermal

    contact, inhalationSHOWERING

    uptake by /deposition onVEGETATION

    consumptionofVEGETATION

    Direct exposure

    SOIL AIRconcentration

    transport toSURFACESOIL

    dilution inINDOOR and

    OUTDOOR AIR

    inhalation, dermaluptake AIR

    PORE WATERconcentration

    transport toGROUNDWATER

    transport toDRINKING WATER

    permeation intoDRINKINGWATER

    CSOIL model to quantifyexposure to contaminated terrestrial soils

    9%

    8%

    21%

    70%

    2%8%

    Human health risks only

    Total number of sites: 1643

    Combination of human health risks and risks fromcontaminant transport in groundwater

    Combination of human health risksand ecological risks

    Combination of human health risks, transportin groundwater and ecological risks

    Risks from contaminant transportin groundwater only

    Combination of transport of contaminantsin groundwater and ecological risks

    Ecological risks only

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    The Dutch soil quality standards

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    Reerence has been made earlier in his

    bookle o he ac ha Duch soil qualiy

    sandards have been developed over he

    years in a number o sages (see he chaper

    Developing a soil policy).

    The firs se o soil qualiy sandards or soiland groundwaer, published in 1983 as par

    o he Inerim Soil Remediaion Ac, were

    he A, B and C values or soil and ground-

    waer. Concenraions below he A value

    implied ha here was no soil conamina-

    ion. Exceeding he C value (serious soil

    conaminaion) implied ha remediaion

    was necessary. The B value was he rigger

    or a Main Invesigaion: i suggesed ha i

    concenraions above he B value were

    ound, serious soil conaminaion migh be

    presen. The A, B and C values were defined

    or a lis o subsances ha were hough o

    be o relevance wih respec o he occur-

    rence o soil conaminaion and, o some

    exen, his mirrors he conaminaed sies

    encounered a ha ime in he

    Neherlands. The A values relaed o he

    background concenraion, while he Cvalues were primarily derived based on

    exper judgmen.

    In 1994, hese hree values were replaced by

    a se o wo values, he Targe value and

    Inervenion value or soil and groundwa-

    er. The Targe value had a similar uncion

    as he A value. The role o he Inervenion

    value was comparable o he C value:

    exceeding means a serious soil conamina-

    ion, or which remediaion is necessary.

    However, exceeding he Inervenion value

    does no imply an immediae remediaion.

    I mean ha he urgency o remediaion

    has o be deermined. In pracice, remedi-

    aion akes place or urgen cases o soil

    remediaion, in paricular cases ha are

    urgen on he basis o human healh risks.

    Oher sies wih serious soil conaminaiongenerally can be remediaed a a convenien

    momen in ime, or example, when

    building aciviies or oher soil-relaed

    aciviies ake place a he sie.

    A major difference was he scienific basis o

    he Targe and Inervenion values; hey

    were derived applying risk assessmen. The

    Targe values are based on ecological risks

    and background concenraions and he

    Inervenion values are based on human

    healh and ecological risks. Alhough here

    was no longer a ormal inermediae (B)

    value, in pracice such an inermediae value

    q y

    was sill used o deermine he need or a

    Main Invesigaion. For his, he average o

    logical componen o he Inervenion value

    is missing.

    were inroduced ha define wheher

    slighly conaminaed soil is fi or a specific

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    Targe and Inervenion value was used.

    Moreover, a volume crierion was inro-

    duced in 1994. I implied ha a single excess

    o he Inervenion value in one soil sampleis no sufficien o declare conaminaion o

    be serious. This requires a volume o a leas

    25 m3or soil or 100 m3or waer-sauraed

    soil volume or groundwaer exceeding he

    Inervenion value.

    As menioned earlier, by now he Targe

    values have been replaced by he

    Background values derived rom he naionwide sudy o he background concenra-

    ions or 252 subsances. The number is he

    resul o he sum o all individually lised

    subsances and he subsances ha are par

    o a lised sum parameer. An example is he

    lised sum-PAHs (Polycyclic Aromaic

    Hydrocarbons), or which 10 specific PAHs

    compounds need o be analysed.

    The lis includes so-called indicaive levels

    o serious risk or 32 subsances, as

    alernaive or an Inervenion value, or

    which a sandardised measuremen or

    analysis proocol is lacking or he ecooxico-

    The risk-based Inervenion values were

    revised a several sages; he laes revision

    is rom 2013. In 2008, an Inervenion value

    or asbesos has been included in he lis,solely based on human healh risks. I is

    obvious ha he exposure o asbesos in soil

    is quie differen compared o oher

    subsances since he inhalaion o asbesos

    fibres is he only relevan exposure pahway.

    Thereore, an alernaive procedure was

    ollowed, using measured concenraions in

    soil and air a differen aciviies and soil

    and weaher condiions. Moreover,differences in carcinogenic poenial

    beween differen ypes o asbesos were

    aken ino accoun.

    The publicaion o he Soil Qualiy Decree in

    2008 resuled in a drasic change in soil

    qualiy assessmen. The perspecive o he

    new decree is differen rom he pas as

    (re)use o slighly conaminaed soil became

    an imporan objecive. Inervenion values

    are sill used o define wheher remediaion

    is necessary. Bu hrough he Soil Qualiy

    Decree wo addiional soil qualiy sandards

    land use. These soil qualiy sandards, called

    Maximal values or residenial land use and

    Maximal values or indusrial land use,

    relae he accepable qualiy o he soil o is

    uncion. The Maximal values, which areavailable or soil only (no or groundwa-

    er), have been derived based on human

    healh risks, ecological risks and risks or

    agriculural producion.

    Maximal values have been published or 101

    subsances in he Duch soil qualiy

    regulaion (laes version 2012).

    The Background values now in place werederived rom he sudy o naional back-

    ground concenraions in he Neherlands

    (see he chaper Knowing he soil qualiy).

    In principle, he Background values were se

    a he 95 percenile o he disribuion o

    background concenraions in he op soil

    in relaively undisurbed areas. For

    subsances or which he Background

    concenraions were lower han he

    analyical deecion limi, he Background

    values were se equal o he deecion limi.

    This is applicable or a large group o

    organic subsances.

    | Rijkswaterstaat

    Back

    ground

    valu

    e

    Residence

    Industry

    Inte

    rvention

    valu

    e

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    Sustainable land management Site remediation

    Contaminant concentration

    Nature and agriculture Residential areas Industrial areas Remediation

    Soil qualiy sandards expressed for he sandard soil in mg/kg dry mater for he sandard se of subsances.

    Substance ) Background value

    Maximum value

    for residential

    land use

    Maximum value

    function class

    Industry Intervention value )

    barium - - - - )

    cadmium . . .

    cobalt

    copper

    mercury . . . / )

    lead

    molybdenum .

    nickel

    zinc

    sum-PCBs . . .

    sum-PAHs . .

    mineral oil

    Illusraive overview of he Duch Soil Qualiy Sandards

    1. In addiion o he concenraion o hese

    subsances, he percenage o clay andorganic mater should be deermined.

    2. Inervenion values as included in he

    Duch Soil Proecion Ac.

    3. The values or barium have been wihdrawn

    as he inervenion value is lower han he

    naural occurring concenraions. When

    here is a higher value han he background

    value, caused by an anropogenic source,

    hen he compeen auhoriy can assess

    his value using he ormer inervenion

    value o 625 mg/kg d.m.

    4. For inorganic and organic mercury

    respecively.

    As menioned earlier, some major

    differences are ound among he soil

    i h il i h

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    properies o he op soil in he

    Neherlands. There are large differences in

    he racion o clay beween sand and clay

    soils as well as in he organic mater conen

    o, or example, pea and sand. Boh hefine racion and he organic mater srongly

    influence he availabiliy o subsances in

    soil. To accoun or hese differences, he

    soil qualiy sandards are normalized

    according o wha is called he sandard

    soil wih an organic mater conen o 10%

    and 25% clay, using pracical soil properies

    conversion equaions.

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    Investigating the soil quality

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    Prior o invesigaing he soil qualiy o a

    sie, i is imporan o ideniy he moive

    or he invesigaion. Differen moives are

    possible and migh rigger an invesigaion.

    Obvious moives or an invesigaion are

    presen or pas aciviies on he sie hahave a srong likelihood o causing soil

    conaminaion. (Re)developmen or

    residenial purposes also riggers an

    invesigaion in he Neherlands o preven

    building on a seriously conaminaed sie.

    Ye anoher reason could be a propery

    ransacion beween wo (privae) paries,

    whereby he poenial new owner wans o

    exclude he risk o acquiring a conaminaedsie. A logical decision since Duch law

    prescribes ha he new owner will be liable

    or he remediaion coss in he even o

    conaminaion.

    Knowing why he sie requires invesigaion

    already provides imporan clues o he kind

    o soil invesigaion ha is necessary.

    Soil invesigaion always sars wih a

    Preliminary Invesigaion. I consiss o adesk sudy and a sie inspecion. The

    purpose o he Preliminary Invesigaion is

    o esablish wheher he sie migh be

    conaminaed on he basis o hisorical

    inormaion: pas and presen aciviies on

    he sie as well as he sies geological and

    hydrological siuaion. Obviously, i he sie

    has a long hisory, i migh prove very hard

    or even impossible o obain all he relevaninormaion, a ac ha should be aken

    ino consideraion when defining he

    invesigaion sraegy.

    Based on he obained inormaion a

    concepual model o he sies conamina-

    ion siuaion is defined. For his a limied

    number o basic assumpions wih respec

    o he poenial conaminaion is used. I

    conaminaion is expeced, he spaialdisribuion over he sie is eiher homo-

    geneous or heerogeneous.

    I a homogeneous disribuion is expeced,

    he suspeced deph will be idenified. For

    simple siuaions, he conaminaion level

    will be more or less sable over he

    conaminaed surace. However, even

    significan variaion in conaminaion levels

    can occur. The homogeneous characer insuch a siuaion is he expeced consan

    level o variabiliy. For example, a sies

    where he soil plain has been elevaed in he

    pas using old harbour sludge, he concen-

    g g q y

    raions can vary significanly rom poin o

    poin ye he conaminaion level o he

    whole layer sill appears o be predicable

    assumpions o he concepual sie model.

    This underlines he imporance o he

    assumpions ha are he basis or he

    Where conaminaion had been expeced

    and acually ound, here will be a need or

    urher delineaion o ha conaminaion

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    whole layer sill appears o be predicable.

    A heerogeneous disribuion can be

    expeced as a resul o some kind o spillage

    in he pas. Depending on how long he sie

    has been in use, and how many differenaciviies have been perormed, he posiion

    o he resuling ho spos may be known or

    no.

    All hese assumpions ogeher resul in a

    firs version o he concepual sie model.

    The imporance o his invesigaion phase

    is widely acceped, as all subsequen

    invesigaions will, in principle, be based onhese resuls. Consequenly, a sufficien

    amoun o effor (and hus money) should

    be spen on he Preliminary Invesigaion.

    The concepual sie model obained

    provides he inpu or wha needs o be

    done in erms o sie invesigaion in he

    nex phase, he Exploraory Invesigaion.

    During he Exploraory Invesigaion he firs

    acual sampling occurs, is main purposebeing o check wheher he assumpions o

    he concepual sie model are correc. I is a

    limied, cos-effecive sampling exercise

    wherein he sampling sraegy is linked o

    assumpions ha are he basis or he

    concepual sie model. During he

    Exploraory Invesigaion o a heerogeneous

    conaminaion a a known posiion, he

    sampling will ocus on ha posiion only. Ihe inormaion on he posiion is incorrec,

    he conaminaion may be missed.

    Once he samples have been aken and he

    analyical resuls are available, i is up o he

    consulan o redefine he concepual sie

    model. Inormaion rom he Exploraory

    Invesigaion is added o ha o he

    Preliminary Invesigaion o generae asomewha more deailed concepual sie

    model.

    The resul o he Exploraory Invesigaion

    will deermine i addiional sampling is

    necessary. Where no conaminaion had

    been expeced, and i, indeed, no conamina-

    ion has been ound, here will be no reason

    or urher invesigaions. Again, his sresses

    he imporance o well-ounded assumpionsobained rom a horough Preliminary

    Invesigaion. I, despie he assumpions,

    conaminaion is ound, urher inves-

    igaion o he sie will be required.

    urher delineaion o ha conaminaion

    in he Main Invesigaion.

    To assess he risks o he conaminaion,

    apar rom knowledge o he conaminaionisel, inormaion mus also be gahered

    abou he geological and hydrological

    siuaion. This knowledge will also prove

    essenial when remediaion will be

    necessary.

    In he Main Invesigaion he concepual

    sie model needs o be redefined unil

    sufficien knowledge o he conaminaionsiuaion is obained. Sufficien knowledge

    will depend, amongs ohers, on he spaial

    disribuion o he conaminans, he (geo)

    hydrology, he remediaion mehod applied

    as well as he uure use o he sie. Given

    hese variable boundary condiions, i is less

    simple o provide angible insrucions or

    he Main Invesigaion. I also implies ha

    he Main Invesigaion, cerainly in morecomplex siuaions, canno be perormed in

    a single phase. Afer each phase i mus be

    judged i he concepual sie model is

    sufficienly defined in ligh o he conam-

    inaion, he associaed risks and is

    poenial uure remediaion.

    Preliminary Investigation

    contaminationsuspected?

    yes no

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    I more han 25 m3soil or 100 m3groundwa-

    er appears o be pollued above he

    Inervenion value, i is reerred o as

    serious soil polluion. This means ha heuncional properies o he soil or

    humans, plans or animals migh be

    seriously impaired. Thereore, i mus be

    invesigaed wheher he risks o humans

    and/or he environmen are accepable or

    no. The sie-specific risks will deermine