unconventional hydrocarbonsin poland – dissapointmentor a ......shale gas prospecting in poland -...

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www.pgi.gov.pl Polish Geological Institute National Research Institute Unconventional hydrocarbons in Poland – dissapointment or a lesson for future? GRZEGORZ PIEŃKOWSKI Polish Geological Institute National Research Institute

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  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Unconventionalhydrocarbons in Poland –dissapointment ora lesson for future?

    GRZEGORZ PIEŃKOWSKI Polish Geological InstituteNational Research Institute

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    EU and Poland - energy security – high ratio of

    hydrocarbons dependency

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Polish present energy mix

    Source: EU Commission, EnergyStatistics, update: Jun-15

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Poland’s Energy Policy 2050 –

    Aug’15 draft

    Main goals• Improvement of Poland’s energy security• Growth of economy’s competitiveness and energy

    efficiency• Minimalisation of the energy sector environmental

    impact

    3 Scenarios:• Sustainable• Alternative – nuclear• Alternative – natural gas + Renewables

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Unconventional hydrocarbons

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Conventional and unconventional hydrocarbons - the same kind of

    source rock – hydrocarbons migration makes the difference

    conventional

    unconventional

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Main screening criteria for gas/oil plays

    in siliciclastic source rocks - “shale gas/oil”• Presence of conventional hydrocarbons in the basin• Present day Total Organic Carbon (TOC) contents > 2.0 %• Gas saturation and presure caused by hydrocarbon generation• Net thickness of hydrocarbon bearing interval > 15 meters• Preferably marine organic matter• Right thermal maturity („thermometer” Ro > 1.1 %, < 3.5 %)• High silica/carbonate contents, low clay mineral contents – high

    brittleness

    • Low burial depth (

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    European onshore resources and the Polish Basin – on this

    map from 2012 still marked as a whole of a „high potential”

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Short geological introduction - Upper Ordovician – Lower Silurian (c. 430 – 450 Mya) – our main (geological) time of interest in Poland

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Polish Basin as a part of trans-European

    Caledonian basinCaledonian foredeep basin extends beyond Poland

    (Oczlon, 2007)

    Baltic Basin

    Lublin Basin

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Big hopes, then greatdisparities in estimations

    Polish shale belt (although generally thick) is far from being uniform in terms of shale gasproperties – this resulted in these dramatically different estimations, (still based on

    archival materials!)

    Although still limited, (70 wells, of which just 12 hydraulically fractured), the new data allowed better understanding of the shale play in Poland – and actually may tell us what

    we can expect elsewhere in Europe

    150 Bcm a year! Same amount as Europe importsfrom Gasprom! Thatstirred imagination and entry into Poland of ExxonMobil and other giants.

    Recovery factors based on multiple analogous North American shale plays !!!

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Shale gas prospecting in Poland - list of completed bor eholes with well stimulation indicated(for 01.01.2015 r.)

    Kind of well stimulationNumber of vertical

    boreholesNumber of boreholes with

    horizontal sectionsTotal

    Hydraulic fracturing 13 12 25

    Only microfracturing / DFIT* 4 0 4

    No hydraulic fracturing 37 4 41

    Total 54 16 70

    DFIT – Diagnostic Fracture Injection Test

    This nubmber is highest in Europe, but very low when comparedto American figures

    Still on the way towards first success…

    24500 m3/day (achieved in one borehole), and 11.000 to 15.000 in few others -it is not enough to keep a big company in Poland – to mee t the global standards, they would expect at least three times more…

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    14

    Shale gas/oil prone – 700 m

    Eifel Tower

    Ordovician

    Lower Silurian

    Hydraulic fracturing – 2894 – 2907 m

    PGNiG Lubocino 1 welland main geological targets

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    THERE IS NO THICK, UNIFORM, HYDROCARBON – RICH, SHALE BELT ACROSS POLAND - ALTHOUGH AT A

    FIRST GLANCE IT SEEMED TO BE THE CASE…

    IN QUEST FOR SWEET SPOTS

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    After: Ottmann & Bohacs

    WHAT IS SWEET SPOT?

    = Pressure

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Going West for dry gas - with deeper burial, higher temperatures and

    pressures – however, the depth of target intervals is also increasing…

    Oil proneGas prone

    Lublin Basin Batlic basin

    Lublin Basin

    Batlic basin

    Maturity map

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    SCREENING OF AN ORDOVICIAN TARGET BASED ON EXISTING WELLS WITH A HIGHER AVERAGE ORGANIC MATTER (TOC) – HIGHER TOC ALONE IS NOT ENOUGH

    Compiled by Adam Wójcicki

    ? offshore

    GoodAverage

    IN EACH TARGET INTERVAL:

    Thickness - potential volume of gas-in-place+ Composition of bulk rock (carbonate, quartz, total clay) –

    brittleness, susceptibility to hydraulic fracturing+ Total organic carbon (TOC) – generation of hydrocarbons____________________________________________________= POTENTIAL SWEET SPOT (however, you have to be lucky to have all these delights occurring together in one place)

    After all, the depth of potential sweet spot is alsoimportant – the deeper, the higher the cost

    1

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    A problem: high clay content

    Smectite group of clay minerals is particularly unwanted , as theseminerals swell in contact with water, clogging the fract ures

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    HOW TO BREAK POLISH SHALES?

    (a hint: more detailedgeological investigations )

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Prehaps, let’s find the spots where the Mother Nature di d the job? In places, tectonized zones can be the most productive one s! A hintfrom China (Fuling field)

    After: GUO Tonglou, ZHANG Hanrong

    Naturally formed fracturesat the crest of anticline = hydrocarbon pathway to wellbore – enhancement of gas flow into the well

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    AT FIRST, VERY CAREFUL GEOLOGICAL RESEARCHRegional seismic section, Baltic Basin, Silurian sequence and teconics (Krzywiec et al., 2013)

    Lublin Basin is more intensively tectonised – also Carboni ferous may be attractive

    Diminishing thickness, less organic carbon, but morecarbonate or silica content – better brittleness

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    In search for sweetspots – combination of different parameters, paleoceanography, enhanced geological maping

    Higher brittlenessMore organic carbon

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    More effective fracturing, adjusted to local geology - one fracturing linking

    two formations – chance to exploit at once separated gas-bearing intervals

    (BNK Gapowo well)

    Thin organic-rich shale, gas bearing interval

    Thin organic-rich shale, gas bearing interval

    10-15 m(toothin)

    10-15 m(toothin)

    Barren marlstoneswell

    This situation may be quite common in geological reality - application of thismethod needs a very high pecision in the well guidance and sometimesheavier hydraulical pressures applied. If separating rock represents non-permeable sandstone, combination of shale and tight gas may occur

    Sasino Fm.

    Jantar Mb.

    Prabuty Fm.

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Breaking clay-rich shales - massive fracturing (example from China)

    Liquid CO2 fracturing? Is it real solution for clayey s hales?

    OrdosBasin, Gao Ruimin, YanchangPetroleum

    However, it is likely that the applicable technologies have already been captured, and the possible innovations will not bring dramatic progress

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    CONCLUSIONS FOR EUROPE

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    North America vs Poland – and Europe – note the sheer s caleof American basins and shale reservoir properties

    Polish BasinMain American basins

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Polish Silurian shales represents a wide spectrum - other shales

    in Europe are within this spectrum (after D. Jarvie, 2012)

    Polish Silurian

    German Lower Jurassic

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    We expect that shale play geology in Poland will be similar to other European basins

    • Hydrocarbons in the Paleozoic basins of Central Europe werecommonly generated during Variscan time, rising uncertainty

    as for gas retention

    • Thermal maturity often is not high enough for dry gas, andconsiderable parts of the analyzed basins might have liquids

    and oil potential

    • European Paleozoic basins with shale gas/oil potential are oftentectonically deformed, causing technological challenges - but in some

    places tectonical deformations can help

    • In Poland (and elsewhere in Europe) thickness of TOC rich layer (and net pay) is often low

    • In Poland (and often in other basins) clay mineral content is relatively high, while brittle mineral content is low

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Productivity - American success, European reality

    A range to be expected in Polish (and European) basins?

    Top 3 plays= 66%

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Polish Geological InstituteNational Research Institute

    Dr. Monika KonieczyńskaDr. Małgorzata Woźnicka

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    NOISEGASES & DUSTS

    PRESSURERESPONSE

    WASTESWATER

    SOIL

    Geological conditions

    LANDSCAPE

    The aim of the research32

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Geological conditions

    1

    2

    Level of HydraulicFracturing

    Silu

    rian

    Sea

    ling

    Com

    plex

    ZechsteinSealing Complex1000

    2000

    3000

    m bgl

    Pomerania Region

    Lublin Region

    1387 m

    Level of HydraulicFracturing

    857 m

    840 m

    Level of HydraulicFracturing

    1000

    2000

    1000

    2000

    33

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Seismometric survey

    Syczyn

    Zawada

    Gapowo

    No quakes caused by rock cracking downholeregistered on ground surface during boreholesstimulation.

    Some vibrations generated by high-volumes pumpsoperations did not exceed values considered assave by Polish construction standards and did notaffect building stability or work conditions inbuildings.

    Institute of Geophysics, Polish Academy of Sciences

    Central Mining Institute

    34

    Łebień

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Air emissions

    Test siteSO2 NOx Methane

    C2-C12hydrocarbons

    VOC BTEX Benzen

    [µg/m3]

    Value of reference averaged for 1 h

    350 200 nr 3000 nn 850 30

    Lubocino 169 (t) 109 (t) 10108 (t) 7620 (t) 11177 (t) 23,5 (t) 6,0 (t)

    Stare Miasto 815 (f) 105 (f) 1300 (f) 2900 (f) 5500 (f) 485 (f)

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Technological fluidsComponent

    Fracturing fluid Flowback

    mg/l

    Ba 0,0000963 – 2,02 0,00128 – 59,50

    Ca 0,0018 – 3,15 0,23 – 199,56

    Cs 0,0008 – 0,17 0,00161– 54,57

    K 0,0822 – 289,28 1,67 – 86,68

    Na 0,0782 – 36,29 0,84 – 601,65

    Se 0,0904 – 1,40 0,0419 – 40,58

    Sr 0,000894 – 0,89 0,00088 – 23,45

    Ag 0,0008 – 0,0119 0,0113 – 0,0304

    Al 0,000849 – 0,9 0,0152 – 2,36

    As 0,00876 – 0,12 0,00552 – 1,1

    Cd 0,000974 – 0,000144 0,0077 – 0,012

    S 0,00673 – 21,71 0,43 – 120,36

    RadioactivityFracturing fluid Flowback

    Bq/kg

    40 K

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Groundwater reserves versus water consumption for fracturing purposes

    Test site

    Available

    groundwater

    resources

    Reserve

    groundwater

    resources Fracturing water

    withdrawal

    %

    of available

    groundwater

    resources used for

    fracturing purposes

    %of reserve

    groundwaterresources used for

    fracturing purposes (as of 2012)

    103 m3/year 103 m3/year 103 m3 % %

    Lubocino 110 650 56 161 7.967 0.007 0.014

    Stare Miasto 111 930 103 737 3.212 0.003 0.00319

    Syczyn 79 034 66 476 37.849 0.05 0.057

    Wysin 119 951 107 375 No fracturing

    Zawada 256 792 213 472 1.284 0.0005 0.0006

    Łebień 208 828 190 539 17.322 0.008 0.009

    Gapowo 110 650 56 161 25.360 0.023 0.045

    37

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Conclusions

    • Shale gas exploration activities generate mainly short time impact (noise) on the environment, also easy to minimaze, providing that all HSE standards

    and best operation practice with special regard to local conditions are

    implemented.

    • The study showed no negative impact of exploration on the surface and groundwater quality in the observed period of time.

    • No indirect impact on water-dependent ecosystems was detected.

    • Gas and dust emissions from drilling equipment are not significant, GHG emissions not measured, difficult to estimate.

    • Flowback chemical characteristics is site-specific and depend both on frack fluid composition and local geochemistry of stimulated formation

    38

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Recommendations:• Special concern should be put on waste management, as high quantities of

    drilling wastes, flowback and produced water might pose hazards to natural

    environment on site and elsewhere.

    • Ensuring safety of the environment and sufficient public perception and safety in production areas will require an adequate control of technical

    operations and the establishment of uniform monitoring system. Further exploratory/production operations should be preceded by:

    • site specific water supply study (incl. alternative water sources)

    • baseline status of surface and groundwater (quality and quantity),

    • background concentrations of methane in groundwater,

    • baseline concentrations of methane in soil gas.

    39

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    General public opinion support

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    WHAT ABOUT OTHER UNCONVENTIONAL

    RESOURCES?

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    OTHER UNCONVENTIONAL HYDROCARBONS IN POLAND – TIGHT GAS

    Tight gas

    Coal Bed Methane

    CONVENTIONAL TIGHT GAS

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Tight gas, Poland: undiscovered (risked) GIP values for the reservoir formations of Rotliegend, Carboniferous and Cambrian; given in Tcf.

    Reservoir formation Depth[m] b.s.l. Minimum [Tcf] Best estimate [Tcf] Maximum [Tcf]

    I – Permian (Rotliegend)sandstones

    5500-6000or 5100-6000

    3.57or 7.62

    12.18or 28.66

    31.21or 81.47

    II – Carboniferoussandstones

    1800-3500 15.99 40.22 99.62

    III – Cambrian sandstones 2800-3100 0.60 1.34 2.82

    TOTAL-

    20.16÷24.22 53.94÷70.42 133.65÷183.91

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    CBM (Coal Bed Methane) – the first coal hydraulic fracturingoperation in a working coal mine (Wesoła, Poland)

    Recoverable resources in Poland – c. 170 billion m3 (bcm)Current emission of CH4 – 660 million m

    3/year, 190 million m3 – captured

    Safety – 64 casualties since 2000 Climate impact - 660 million m3 of CH4 = approximately 15,5 billion m

    3 of CO2

  • www.pgi.gov.pl

    Polish Geological Institute

    National Research Institute

    Final conclusions:EU is still in early exploration phase. Poland and currently England are the only two countries in Europe having scenario of possible economic growth, based on shale gas production. We cannot simply adapt neither U.S. (exceptionally good geological conditions, different regulatory framework, environmental issues), nor (subsidised) Chinese shale gas exploration experiences, as a model for Europe (although, in terms of geology China is more compatible).

    HOWEVER:

    Today’s pessimism about shale gas in Poland reflects (in a reversed sense) the early frenzy- and is just as overblown

    Currently, we can map more accurately early commercial potential of the Polish shales, there is alsoa progress in gas output results, so we are on a learning curve. There is still no substitute for ‘learning-by-doing’, i.e. the knowledge that comes from drilling and completing wells.

    Higher amounts of condensate/oil than anticipated, whereas natural gas production is lower than had been hoped. Importantly, wet gas (higher content of natural gas liquids) is economically attractive

    Forget about 150 bcm/year – as originally hoped for. But even 5 bcm/year might be important (itwould be a 1/3 of current annual consumption in Poland). Tight gas and CBM can provide additionalproduction, and conventional accumulations can be associated with unconventional plays. Many hitherto reports are strongly oriented to think in a way of production from conventional gas reserves –which is a misleading approach. In a sense, Polish experience can serve as a hugedemonstration project for the rest of Europe. No long- lasting impact of hydraulic fracturing on environment has been observed.