Soil Physical Chemical Quality 08

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    Hailin Zhang

    Department of Plant and Soil Sciences

    Oklahoma State University

    Soil Physical and Chemical

    Quality and Management inOrganic Production

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    What makes up soils?

    Water

    25%

    Air

    25%

    OM2%

    Mineral

    48%

    SandSiltClay

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    Soil Is a Living Body

    US

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    Soil Properties

    Physical

    TextureStructure

    Chemical

    Fertility

    pH

    Soluble salts

    Biological

    Microorganism population-life in the soil

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    Clay

    Silty ClaySandy Clay

    % Sand

    LoamySand

    SandyClay Loam

    Sandy

    LoamSand

    Silt

    Loam

    Clay Loam

    Loam

    Silty ClayLoam

    Silt

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    Water holding capacity andmovement

    NRCS

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    Improving Soil PhysicalCondition

    Adding organic material

    Adding gypsum for alkali soils

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    pH and Buffer Index

    Soil pH is a measure of the acidityand alkalinity of the soil;

    Nutrient availability is related to pH;Crops can only grow well in certain

    pH ranges;

    Liming is the most economical andeffective method to raise soil pH

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    pH valuedefinesrelative

    acidity orbasicity

    9.0

    8.0

    7.0

    6.0

    5.0

    4.0

    Very strong

    Strong

    Medium

    Moderate

    Slight

    Slight

    MediumStrong

    Basic

    Acid

    Pure wate

    Mostproductivesoils

    VinegarLemon juic

    Ammoniacleaner

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    Apply limewell ahead of planting to

    correct soil acidity

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    N Ca

    P Mg

    K S

    16

    Essential

    Elements

    C H O

    B Cl Cu Fe

    Mn Mo Zn

    Essential Plant Nutrients

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    Negatively Charged Colloids

    Attract Cations

    K+

    Ca++

    Na+

    Ca++

    H+

    Mg++

    -

    --

    -

    --

    ---

    Soil Colloid

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    Clay and Organic Matter Have

    Greatest Influence on CECClay

    10-150meq/100g

    Organic matter

    200-400meq/100g

    Organic matter has a higher CEC

    (cation exchange capacity)

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    Nutrient balance is the key forsuccess

    Rightnutrients

    Impropernutrients

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    Soil Soluble Salts Affect Plant Growth

    Normal

    EC (mmhos/cm)0 4 8 12 16

    15

    ESP%

    Saline

    Sodic

    Increased salt hazard

    30

    Saline-Sodic

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    Over Fertilization

    Salts build up in thesoil

    Alters soil pH

    Unbalanced growth More vegetative, less

    reproductive growth

    More disease and

    less winter hardy

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    Soil Tests Serve

    Two Basic Functions

    Provide a starting point fordeveloping fertilizer and limingprogram

    Monitor nutrient level to keep thefertilizer program on track

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    OSU Cooperative Extension

    Soil Probe

    Get a Useful Sample

    Clean Bucket

    Right Depth(plow layer or 6inches

    15-20 cores

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    Soil Tests at OSU

    RoutinepHBuffer IndexNitrogen

    PhosphorusPotassium

    Secondary NutrientsSulfurMagnesiumCalcium

    MicronutrientsIronZincBoron

    Soil Organic Matter, Soil Texture, Soil SalinityCompost, Animal Manure, Irrigation Water

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    Summary

    Soil properties are important for plant growth There are 16 essential plant nutrients

    Soil testing is important for successfulorganic production

    An representative sample is needed toensure reliable test results

    Balanced fertilizer program is critical

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    Soil, Water and Forage AnalyticalLaboratory

    http://www.soiltesting.okstate.edu

    http://www.soiltesting.okstate.edu/http://www.soiltesting.okstate.edu/