aagw2010 june 10 larisa golovko back to basics soil ec as a proxy to map other soil properties

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  • 8/9/2019 Aagw2010 June 10 Larisa Golovko Back to Basics Soil Ec as a Proxy to Map Other Soil Properties

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    Larisa Golovko 1

    Anatoly Pozdnyakov 2

    Landviser, LLC

    1 RiceTec, Inc - Houston, TX USA2 Moscow State University, College of Soil Science Moscow,

    RUSSIA

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    just dirtall soils are the samesubstrate for plantsI just add water and fertilizer, use prime seeds myyields will be high

    2

    Those opinions are very shallow!

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    Parent material (geology)Climate (temperatureand precipitation)TopographyVegetationTime

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    If we can map and understand soils, we can understandthe basics of any agro-ecosystem!

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    Prime land11%

    Too dry28%

    Too humid10%

    Chemicallyimbalanced

    23%

    Too shallow22%

    Permanently

    frozen6%

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    Water quality?Soil quality?Soil horizons?Groundwater depth?

    EC/ER is a good RS indicator of soil and waterquality, especially salinity levels and GW depth!

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    Fits in shirt pocketRuns all season from standard9V battery

    Measures EC/ER in soil, water,food samples as well as in thefield soils from 2 cm to ~10 mdepth

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    Probes can be made to anysize/configuration frommaterials available in anylocal hardware store:

    Nails/screwsIsolated wiresbanana- plugsPVC pipes,

    plastic or wood

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    Chemical properties: saltcontent, CEC, humuscontent, etc.

    Intrusions of highresistivity: stones and oil

    Physical properties: bulkdensity, water content,temperature, texture

    Water movement; soilfreezing-melting, soilcompaction or mixing

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    Spatial variabilityTemporal variability

    Many samples areneeded tocharacterize asingle field.

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    management practiceswater table depthssoil propertiesevapotranspiration rates

    rainfallssalinity levels ofgroundwaterhydrogeological conditions

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    18

    0

    20

    4060

    80

    100

    120140

    1 10 100 1000 10000AB/2 cm

    E R ,

    O h m

    m

    Water

    table

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    Good soil EC in top 30 cm < 1.5 dS/m measured inflooded or mud conditions

    EC of irrigation water

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    25

    35

    45

    55

    65

    75

    85

    95

    C o c

    o d r i

    e

    T r e n a

    s s e

    J u p i t e

    r

    C y p r

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    C L X

    L 7 3

    0

    X P 7 2

    3

    R U

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    1 3 7

    R U

    0 5 0 1

    1 0 2

    R U

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    C h e

    n i e

    r e

    % o

    f h e a l t h y p l a n t s

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