Official Series Description


Lab Data Summary

Aggregate lab data for the CLARK soil series. This aggregation is based on all pedons with a current taxon name of CLARK, 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 CLARK 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
7940A182076KS155002Clark8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8061104,-98.1372223

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CLARK 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 CLARK 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 CLARK 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 CLARK 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with CLARK 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 CLARK series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the CLARK 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.

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

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

Soil series sharing subgroup-level classification with CLARK, 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. KS-2010-09-03-03 | Reno County - 2002

    Typical pattern of soils and parent material in the Shellabarger-Albion-Nalim association (Soil Survey of Reno County, Kansas; 2002).

  2. KS-2012-01-20-36 | Comanche County - June 1989

    Typical pattern of soils and parent material in the Albion-Shellabarger association (Soil Survey of Comanche County, Kansas; 1989).

  3. KS-2012-01-25-14 | Pratt County - September 1968

    Major soils of association 7 and the positions they normally occupy on the landscape (Soil Survey of Pratt County, Kansas; 1968).

  4. KS-2012-01-25-15 | Pratt County - September 1968

    Major soils of associations 8 and 9 and the positions they normally occupy on the landscape (Soil Survey of Pratt County, Kansas; 1968).

  5. KS-2012-01-25-16 | Reno County - March 1966

    Cross section of the Renfrow-Vernon association downslope from the Clark-Ost association (Soil Survey of Reno County, Kansas; 1966).

  6. KS-2012-01-25-17 | Reno County - March 1966

    Cross section of the Nash-Lucien association in the south-central part of the county (Soil Survey of Reno County, Kansas; 1966).

  7. KS-2012-01-25-18 | Reno County - March 1966

    Cross section of the Clark-Ost association showing the topographic relationship of the Clark and Ost soils to the soils of the Renfrow-Vernon association (Soil Survey of Reno County, Kansas; 1966).

Map Units

Map units containing CLARK 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
Clark clay loam, 0 to 1 percent slopes5872380913824702ww2cks00719731:24000
Case-Clark clay loams, 3 to 7 percent slopes5419290113824642wtwsks00719731:24000
Clark clay loam, 1 to 3 percent slopes587338613824712ww16ks00719731:24000
Case-Clark clay loams, 7 to 15 percent slopes54204213824652wtwtks00719731:24000
Clark fine sandy loam, 1 to 3 percent slopes58751713824722ww2dks00719731:24000
Clark-Ost clay loams, 0 to 1 percent slopes5878913824732ww2hks00719731:24000
Clark clay loam, 3 to 6 percent slopes587417513817091hcs8ks02519801:24000
Clark clay loam, 1 to 3 percent slopes58738713817081hcs7ks02519801:24000
Clark loam, 1 to 3 percent slopes5876313817102ww2fks02519801:24000
Clark clay loam, 1 to 3 percent slopes58732603513812521hc9jks03319871:24000
Clark-Kingsdown complex, 5 to 12 percent slopes54211312013812541hc9lks03319871:24000
Clark clay loam, 3 to 6 percent slopes5874862813812531hc9kks03319871:24000
Clark clay loam, 0 to 1 percent slopes5872424713812511hc9hks03319871:24000
Case-Clark clay loams, 3 to 7 percent slopes541926713826742wtwsks07719651:24000
Clark clay loam, 1 to 3 percent slopes587341111554452ww16ks07919701:24000
Clark clay loam, 1 to 3 percent slopes58731436014447752ww16ks09519771:24000
Case-Clark clay loams, 3 to 7 percent slopes5419792114447492wtwsks09519771:24000
Case-Clark clay loams, 7 to 15 percent slopes5420338414447502wtwtks09519771:24000
Clark clay loam, 0 to 1 percent slopes5872137614447742ww2cks09519771:24000
Clark fine sandy loam, 1 to 3 percent slopes587547214447762ww2dks09519771:24000
Ost-Clark loams, 1 to 3 percent slopes592438814447952w9klks09519771:24000
Clark-Ost loams, 3 to 7 percent slopes58808914447782ww2kks09519771:24000
Clark-Ost clay loams, 0 to 1 percent slopes58782514447772ww2hks09519771:24000
Clark loam, 3 to 7 percent slopes5877624913805012ww2gks09719831:24000
Clark loam, 1 to 3 percent slopes5876570713805002ww2fks09719831:24000
Clark clay loam, 1 to 3 percent slopes587328313804981hbj6ks09719831:24000
Clark clay loam, 3 to 6 percent slopes587419313804991hbj7ks09719831:24000
Geary-Clark complex, 3 to 7 percent slopes, eroded3849527333392r9d3ks11319801:24000
Clark clay loam, 1 to 3 percent slopes58732182014451282ww16ks15119651:24000
Case-Clark clay loams, 3 to 7 percent slopes54191522614451142wtwsks15119651:24000
Clark fine sandy loam, 1 to 3 percent slopes5875537514451292ww2dks15119651:24000
Case-Clark clay loams, 7 to 15 percent slopes5420329314451152wtwtks15119651:24000
Clark-Ost clay loams, 0 to 1 percent slopes5878274414451322ww2hks15119651:24000
Clark loam, 1 to 3 percent slopes587615514451302ww2fks15119651:24000
Clark loam, 3 to 7 percent slopes58771214451312ww2gks15119651:24000
Ost-Clark loams, 1 to 3 percent slopes59242347914438402w9klks15519991:24000
Clark-Ost loams, 3 to 7 percent slopes5880317414438262ww2kks15519991:24000
Geary-Clark complex, 3 to 7 percent slopes, eroded38491391227333552r9d3ks15919711:24000
Clark clay loam, 1 to 3 percent slopes5873336614332782ww16ks15919711:24000
Clark loam, 1 to 3 percent slopes587656214332792ww2fks15919711:24000
Clark-Ost clay loams, 1 to 3 percent slopes5879261114439732ww2jks17319761:24000
Ost-Clark loams, 1 to 3 percent slopes592426414439812w9klks17319761:24000
Clark loam, 1 to 3 percent slopes587661314436482ww2fks18519751:24000
Clark-Ost loams, 3 to 7 percent slopes588015914436492ww2kks18519751:24000

Map of Series Extent

Approximate geographic distribution of the CLARK 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 .