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    Using

    SOILT XONOMY

    to Identify Hydric Soils

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    Soil Taxonomy is

    A basic system of soil classification formaking and interpreting soil surveys.

    Objective:To develop a hierarchical classificationthat reflects the relationships between

    different soils, and between soils and thefactors responsible for their character.

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    Soil Taxonomy

    Procedure:

    Soils are classified on the basis of:

    Soil properties observed in the field (e.g.,soil horizons, texture, color, pH)and

    Soil properties inferred from the

    combined data of soil science and otherdisciplines (e.g., soil temperature andmoisture regimes inferred from soil science andmeteorology).

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    Soil Taxonomy

    Series

    Family

    Sub Group

    Great Group

    Sub OrderFirst sign of wetness

    Order12 Orders

    Entisol

    Fluvent

    Ustic

    Fine-loamy, mixed, frigid

    Korchea

    Mollic

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    Fine-loamy,

    mixed

    (calcareous),frigid,

    Mollic

    Ustifluvent

    Korchea

    Series

    Not Hydric

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    Soil Taxonomy

    Nature of

    Number Differentiating

    Category of Taxa Characteristics

    Order 12 Soil-forming processes

    as indicated by

    presence or

    absence of majordiagnostic horizons

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    Soil Orders

    Alfisols

    Andisols

    AridisolsEntisols

    Gelisols

    Histosols

    Inceptisols

    Mollisols

    OxisolsSpodosols

    Ultisols

    Vertisols

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    Taxonomic Names

    Soil Order

    Alfisols

    Andisols

    Aridisols

    Entisols

    Gelisols

    Histosols

    Inceptisols

    MollisolsOxisols

    Spodosols

    Ultisols

    Vertisols

    Names Ends in:

    -Alf

    -And

    -Id

    -Ent

    -El

    -Ist

    -Ept

    -Oll-Ox

    -Od

    -Ult

    -Ert

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    Entisol Suborders

    Aquents

    (L. Aqua, Water)

    Wet Entisols

    Fluvents

    (L. Fluvius, River)

    Floodplain Soils

    Orthents

    (Gr. Orthos, True)

    The Common Ones

    Psamments

    (Gr. Psammons, Sand)

    Sandy Soils

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    Entisol Great Groups

    Suborder

    Aquents

    (Wet Entisols)

    Great Group

    Cryaquents - cold

    Fluvaquents - flood plainHydraquents - water

    Psammaquents - sand

    Epiaquents - perched

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    Entisol Great Groups

    SuborderFluvents

    (Floodplain soils)

    Great GroupCryofluvents

    Torrifluvents - Torrid

    (hot and dry)Tropofluvents

    Udifluvents - Humid

    (not dry in most years)

    Ustifluvents - Semi-arid(between Udic-Aridic)

    Xerofluvents - Semi-arid

    (moist cold winter - dry

    warm summer;Mediterranean climate)

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    Soil Taxonomy

    Suborder

    Psamments

    (Sandy Soils)

    Great Group

    Cryopsamments

    Quartzipsamments -Quartz

    Torripsamments

    Udipsamments

    UstipsammentsXeropsamments

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    Soil Taxonomy -How to interpret the formative elements

    Sub group - Great group, Suborder, Order

    4 3 2 1

    for example -

    Vertic Udifluvent

    4 - Vertic sub group - invert, shrink-swell, high clay

    3 - Udi(c) great group - humid

    2 - Fluv(ic) suborder - floodplain

    1 - Ent(isol) order - little soil development

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    Aquic Soil Moisture Regimes

    Typic SubgroupAquic Suborder____ ___aq___

    wettest

    Aeric Subgroup

    Aquic SuborderAeric ___aq___

    better aerated

    Aquic SubgroupAquic ______

    driest

    From Mausbach 1992

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    Subgroups

    4 3 2 1

    Typic Fluvaquents

    4 1 2

    Typical Entisols with aquic moisture

    3

    regimes that occur on floodplains.

    1. Order 3. Great Group

    2. Suborder 4. Subgroup

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    Subgroups

    4 3 2 1

    Mollic Fluvaquents

    1 2

    Entisols with aquic moisture regimes that

    3

    occur on floodplains, and that have thick,

    4dark surface layers.

    1. Order 3. Great Group

    2. Suborder 4. Subgroup

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    Subgroups

    4 3 2 1

    Aeric Fluvaquents1 3 2

    Entisols, occurring on floodplains, with an aquic

    moisture regime that are not so wet. Better

    4aerated in the upper part of the soil.

    1. Order 3. Great Group

    2. Suborder 4. Subgroup

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    Soil Taxonomy

    Nature of

    Number Differentiating

    Category of Taxa Characteristics

    Series 15,000+ A series may have virtually the

    full range that is permitted in a

    family in several properties, but

    in one or more properties the

    range is restricted, such as:- Kind and arrangement of

    horizons

    - Color

    - Texture

    - Structure

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    Soil Taxonomy- Predicting

    Problem Hydric Soils

    Formative

    Element

    Soil

    Order

    Why a Problem

    Alf Alfisols Gray / White (high value / low chroma)horizon below A, not always indicative of

    wetness.

    And Andisols Fe immobilized, redox. features are often

    deeper than depth to water table. Some

    Andisols have thick, dark colored surfacelayers.

    Ent Entisols Recent depositional events exceed rate of

    typical hydric morphology formation. Also

    many sandy soils are Entisols.

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    Problem Orders, cont.

    Oll Mollisols Dark colored surface layers "mask" redox features.

    Check colors below mollic, allow surface layers to

    dry then look for redox (NTCHS Indicator F6).

    Od Spodosols Sandy surface layers, no redox features evident inupper part. (Use organic layers, dark surface, and

    stripped matrix indicators).

    Ult Ultisols Some have gray / white (high value / low chroma)

    horizon below A, not necessarily indicative of

    wetness.Ert Vertisols High shrink-swell clays, surface hydrology. Many

    Vertisols also have dark-colored surface layers.

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    Problem Great Groups

    Alb Albic horizon Gray / White (high value / low chroma)

    horizon below A, not necessarily indicative

    of wetness

    Calci,

    calc

    Presence of a

    calcic horizon

    Gray / White (high value / low chroma)

    horizon below A, not necessarily indicative

    of wetness

    Dur Presence of a

    Duripan

    (dense layer)

    Subsoil may be brownish color.

    Perched water table situation.

    Epi Perched

    water table

    Subsoil may be brownish color.

    Fluv Floodplain Surface hydrology, recent deposition

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    Great Groups, cont.

    Fragi Presence of a

    Fragipan (dense layer)

    Subsoil may be brownish

    color, perched water table.

    Gloss Presence of a Glossic

    horizon

    Multi-colored horizon below

    A horizon.

    Melan High organic content Dark colors may mask

    redox features.

    Psamm Sandy texture No, or low Fe content, also

    low OM.

    Sal Presence of a Salic

    horizon

    High pH, low OM; no, or few

    redox features.

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    Typic Haplosaprists

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    Torry Series

    Hydric

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    Terric Haplosaprists

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    Tawas

    Series

    Hydric

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    Lithic Cryofolists

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    Ricker

    Series

    Not Hydric

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    Aquic Paleudalfs

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    Katy

    Series

    Not Hydric

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    Aquic Glossudalfs

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    Withee

    Series

    Not Hydric

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    Typic Aquisalids

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    Unknown Series

    Hydric

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    Aquic

    Quartzipsamments

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    Unknown

    Series

    Not Hydric

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    Oxyaquic Dystrudepts

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    Paxton Series

    Not Hydric

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    Typic Humaquepts

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    Birdsall Series

    Hydric

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    Vertic Argiaquolls

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    Parnell Series

    Hydric

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    Argiaquic Argialbolls

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    Tonka Series

    Hydric

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    Aeric Calciaquolls

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    Hamerly Series

    Not Hydric

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    Aquic Haplorthods

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    Sunapee Series

    Not Hydric

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    Aeric Alaquods

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    Leon Series

    Non-hydric phase

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    Typic Endoaqults

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    Othello Series

    Hydric

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    Typic Umbraqults

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    Series Unknown

    Hydric

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    Chromic Epiaquerts

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    Sharkey Series

    Hydric

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    Summary

    Interpretation of Soil Taxonomic names inSoil Survey manuscripts provides another

    tool for identifying hydric soils.Most useful off-site as part of preliminary

    analysis

    Also useful to identify potential problemhydric soils