Official Series Description


Lab Data Summary

Aggregate lab data for the WALLKILL soil series. This aggregation is based on all pedons with a current taxon name of WALLKILL, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to WALLKILL were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
108A82IL0110581982IL011058Wallkill2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.5047442,-89.6207192
111BWB76091976IN169009Wallkill3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.037575,-85.9401333
111BJY79021979IN075002Wallkill1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5446472,-85.1170889
111BWL80171980IN183017Wallkill1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1594083,-85.5860583
111DBE80361980IN007036Wallkill2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6128917,-87.3389056
111DMY80291980IN107029Wallkill3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0372722,-87.0357444
144A84P0766S1984NY071003Wallkill6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3367609,-74.4523794
144A84P0767S1984NY071004Wallkill6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3370387,-74.4559906
98NW86021986IN111002Wallkill3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.0361583,-87.3729556

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the WALLKILL soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the WALLKILL series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

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Select annual climate data summaries for the WALLKILL series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the WALLKILL series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

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There are insufficient data to create the 3D mountains figure.

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Click the image to view it full size.

Competing Series

Soil series competing with WALLKILL share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

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Select annual climate data summaries for the WALLKILL series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the WALLKILL series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

There are insufficient data to create the 3D mountains figure.

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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with WALLKILL, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database .

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. NY-2012-02-16-06 | Wyoming County - April 1974

    Typical pattern of soils in association 13 (Soil Survey of Wyoming County, New York; April 1974).

  2. WI-2012-03-22-02 | Buffalo County - March 1962

    Soil associations and relief in Buffalo County. 1. Silty soils of the rolling limestone uplands and Steep stony and rocky land: Dubuque, Fayette, Steep stony and rocky land. 2. Loamy soils of the rolling to hilly sandstone uplands: Gale, Hixton. 3. Sandy soils of the rolling to hilly sandstone uplands: Boone, Hixton. 4. Sandy soils of stream terraces: Sparta, Plainfield. 5. Silty soils of stream terraces: Bertrand, Richwood. 6. Loamy terrace soils underlain by sand on stream terraces: Meridian, Tell. 7. Wet organic and mineral soils of bottom lands: Peat and Muck, Ettrick, Wallkill. 8. Soils of overflow bottom lands: Loamy alluvial lands, Marsh (Soil Survey of Bayfield County, WI; 1961).

Map Units

Map units containing WALLKILL as a major component. Limited to 250 records.

Map Unit Name Symbol Map Unit Area (ac) Map Unit Key National Map Unit Symbol Soil Survey Area Publication Date Map Scale
Wallkill silty clay loam, wetW464918211716739kil05919661:20000
Wallkill silt loam, 0 to 2 percent slopes, frequently flooded3292A5781769635y4hil10519911:15840
Wallkill silty clay loamWc4421647565jfqin00319651:15840
Wallkill silt loam, 0 to 2 percent slopesWa42616475530kc5in00319651:15840
Wallkill-Urban land complexYubA1434045432zy5fin00319651:15840
Wallkill variant silty clay loamWa6811646545jbfin00719851:15840
Wallkill silty clay, 0 to 2 percent slopes, frequently floodedWa38662380530kc6in00919831:15840
Wallkill silt loamWd2601652445jygin01519871:15840
Wallkill silt loamWa3771623645fykin02319781:20000
Wallkill silt loam, 0 to 2 percent slopesWa221516034830kc5in03319801:15840
Wallkill silt loam, 0 to 2 percent slopesWa126216259830kc5in04919841:15840
Wallkill silt loam, undrainedWa1581628165gf4in05319851:15840
Wallkill silty clay, 0 to 2 percent slopes, frequently floodedWa27621065130kc6in07519831:15840
Wallkill silt loam, undrainedWb3861645145j5xin08319791:15840
Wallkill silt loam, clayey substratum, drainedWc3091645155j5yin08319791:15840
Wallkill silt loam, 0 to 2 percent slopesWa77116092630kc5in08519851:20000
Wallkill silt loam, 0 to 2 percent slopesWa24827263830kc5in08719781:20000
Milford-Palms-Wallkill complexMt198327247494jhin08919671:15840
Wallkill silt loamWa154927250694kjin08919671:15840
Wallkill silt loamWa63727270694rzin09119791:15840
Wallkill complexWa1161621285fpyin09519651:15840
Wallkill silt loamWa2661630765gpjin10719841:15840
Wallkill variant mucky silty clayWc6761638005hfwin11119901:15840
Wallkill loam, potholeWa3961637975hfsin11119901:15840
Wallkill silt loam, 0 to 2 percent slopesWa100527258130kc5in11319741:15840
Wallkill silt loamWa6791607015d6xin12719781:15840
Wallkill silt loam, undrainedWa10171613205dvwin13519841:15840
Wallkill silt loam, 0 to 2 percent slopesWa70716024730kc5in15119791:20000
Wallkill silt loam, coprogenous earth substratumWb5441643625j10in15719901:15840
Wallkill silt loam, 0 to 2 percent slopesWc80516123830kc5in16919801:15840
Wallkill variant silty clay loamWe3161631805gswin17119871:15840
Wallkill silt loam, coprogenous earth substratum, drainedWa1411612825dtnin17919881:15840
Wallkill silt loam, undrainedWd1111612835dtpin17919881:15840
Wallkill silty clay loamWa22041618295fd9in18319851:15840
Wallkill loamWa24518640767z4mi03719741:15840
Wallkill silt loamWa30218690768h8mi04919671:20000
Wallkill silt loam46321886606b9tmi05919911:15840
Wallkill soilsWa6918821369vdmi06719651:15840
Wallkill silt loam3158918713268qjmi08119841:15840
Kokomo, Barry, and Wallkill loams, overwashed, 0 to 3 percent slopesKgA35021885066b4vmi09119571:20000
Wallkill loam, overwashed, 0 to 3 percent slopesWaA5301885766b73mi09119571:20000
Wallkill silt loamWa7901927466gkmmi13919671:15840
Wallkill loam, 0 to 2 percent slopesWaA05391884186b20mi15119551:15840
Wallkill loamWa6118785869gymi15519671:12000
Wallkill loam, 0 to 2 percent slopes116A325081146b20mi15719841:15840
Wallkill mucky silt loam, 0 to 3 percent slopes, frequently floodedWaakAt183813402w9dsnj01320031:12000
Wallkill silt loam, 0 to 3 percent slopes, frequently floodedWaahAt1164808435w47knj03720021:24000
Wallkill silt loam, 0 to 2 percent slopesWaA6182677805bmp8ny04920181:24000
Wallkill silt loam, 0 to 2 percent slopes, frequently flooded7A159031056382y9v0ny05120191:24000
Wallkill silt loamWa7292926439tj3ny05319751:15840
Wallkill silt loam9824042935099vf1ny06519931:24000
Wallkill silt loamWa20452939899vxjny07119761:15840
Wallkill silt loamWa1622941599w30ny07519731:15840
Wallkill mucky peat, 0 to 3 percent slopes, frequently pondedWkA2225070932q6hfny08520141:12000
Wallkill silt loamWk3462946709wmhny09719761:15840
Wallkill soilsWk5532947809wr1ny09919661:15840
Wallkill silt loamWk14172954389xf8ny12119691:20000
Wallkill silt loamWb2892882069nwzoh00519761:15840
Wallkill silty clay loamWa3114625317grxoh01119791:15840
Wallkill silt loamWa10011714865rftoh02119661:15840
Wallkill silt loam, occasionally floodedWb5514138051jg5moh02119661:15840
Wallkill silt loam, occasionally floodedWc2581717875rrjoh02319971:15840
Wallkill silt loamWb1261686025nfsoh03319751:15840
Wallkill silt loam, lacustrine substratum, occasionally floodedWc36709034rst2oh03319751:15840
Wallkill silt loamWb6971685325ncjoh03719841:15840
Wallkill silt loam, pondedWc2522876009n8foh05519791:15840
Wallkill silt loam, frequently floodedWa2471689705ntnoh06519871:15840
Wallkill silt loamWb216112311r2m6oh06519871:15840
Wallkill silt loamWa916769991t91roh07519891:15840
Wallkill silt loam, lacustrine substratum, occasionally floodedWa1841680075mtloh07719881:15840
Wallkill silt loam, clayey substratum, frequently floodedWa3551710895r10oh08919861:15840
Wallkill silt loamWa14471711735r3qoh09119771:15840
Wallkill silty clay loamWb515931861qgv3oh09119771:15840
Wallkill silt loamWa214028081j2qwoh09719781:15840
Wallkill silt loamWc3472883959p32oh10319741:15840
Wallkill silt loamWa711695445pf5oh10919731:15840
Wallkill silt loamWc2412885059p6moh13319731:15840
Wallkill silt loamWc691708155qr5oh13919711:15840
Wallkill silty clay loamWb3101700685pz2oh14919771:15840
Wallkill silt loam, clayey subsoil variantWc4772880979nsgoh15119671:15840
Wallkill silt loamWg415955481qk99oh15119671:15840
Wallkill silt loamWc241825412wpx6oh15319691:20000
Wallkill silt loamWc5032872399mwsoh16919811:15840
Wallkill silt loam, 0 to 2 percent slopesWc56116821130kc5oh17119751:15840
Wallkill silt loamWa9862818629g9bvt01119761:20000
Wallkill silt loam, 0 to 2 percent slopes, frequently flooded649A121925123212psw4wi01119601:12000
Wallkill silt loamWb540423379g6kdwi02119721:15840
Wallkill silt loamWa113425585g8vkwi03919671:15840
Wallkill silt loam, frequently floodedWa372425386g8n4wi04519691:12000
Wallkill silt loamWa79424734g7z3wi04919601:20000
Wallkill silt loamWa833268724g7b7wi05920231:15840
Wallkill silt loamWa833403374g96twi07920231:15840
Wallkill silt loamWa2583268801g7b7wi10120231:15840
Wallkill silt loam, 0 to 2 percent slopes, frequently flooded649A224426395022psw4wi12119691:12000
Wallkill silt loamWa302425684g8yrwi12719671:15840
Wallkill silt loamWa782425791g926wi13119671:15840
Wallkill silt loamWa6513403485g96twi13320231:15840

Map of Series Extent

Approximate geographic distribution of the WALLKILL soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry .