Official Series Description


Lab Data Summary

Aggregate lab data for the CLIME soil series. This aggregation is based on all pedons with a current taxon name of CLIME, 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 CLIME 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
7493KS04100293KS041002Clime2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.963501,-97.1106644
7601KS16100101KS161001Clime3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2792244,-96.6436539
7679P031979KS017001Clime8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4458351,-96.5486145
7688KS06101488KS061014Clime2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8852768,-96.6730576
7688KS06130788KS061307Clime2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0019917,-96.5464694
7691KS16106991KS161069Clime2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0805168,-96.5815201
7691P102391KS161992Clime7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0822456,-96.5823135
7697KS16103697KS161036Clime3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2164459,-96.6396408

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CLIME 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 CLIME 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 CLIME 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 CLIME 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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Click the image to view it full size.

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 CLIME 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 CLIME 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 CLIME 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 CLIME, 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-2010-09-27-01 | Geary County -

    Typical pattern of soils and underlying material in the Konza-Ladysmith-Irwin association (Soil Survey of Geary County, Kansas).

  2. KS-2012-01-20-11 | Chase County - June 1974

    Pattern of soils in the Reading-Tully association (Soil Survey of Chase County, Kansas; 1974).

  3. KS-2012-01-20-12 | Chase County - June 1974

    Pattern of soils in the Chase-Osage association (Soil Survey of Chase County, Kansas; 1974).

  4. KS-2012-01-20-13 | Chase County - June 1974

    Pattern of soils in the Clime-Sogn association (Soil Survey of Chase County, Kansas; 1974).

  5. KS-2012-01-20-53 | Elk County - November 1986

    Typical pattern of soils and underlying material in the Steedman-Dennis-Eram association (Soil Survey of Elk County, Kansas; 1986).

  6. KS-2012-01-20-54 | Elk County - November 1986

    Typical pattern of soils and underlying material in the Florence-Martin association (Soil Survey of Elk County, Kansas; 1986).

  7. KS-2012-01-20-55 | Elk County - November 1986

    Typical pattern of soils and underlying material in the Clime-Sogn-Labette association (Soil Survey of Elk County, Kansas; 1986).

  8. KS-2012-01-23-29 | Harvey County - November 1974

    Typical pattern of soils in the Irwin-Rosehill-Clime association (Soil Survey of Harvey County, Kansas; 1974).

  9. KS-2012-01-24-05 | Marion County - December 1983

    Typical pattern of soils and underlying material in the Irwin-Ladysmith association (Soil Survey of Marion County, Kansas; 1983).

  10. KS-2012-01-24-06 | Marion County - December 1983

    Typical pattern of soils and underlying material in the Labette-Tully-Sogn association (Soil Survey of Marion County, Kansas; 1983).

  11. KS-2012-01-24-09 | Marion County - December 1983

    Typical pattern of soils and underlying material in the Irwin-Clime association (Soil Survey of Marion County, Kansas; 1983).

  12. KS-2012-01-24-13 | McPherson County - April 1983

    Typical pattern of soils in the Longford-Clime-Irwin association (Soil Survey of McPherson County, Kansas; 1983).

  13. KS-2012-01-24-17 | Morris County - November 1974

    Typical pattern of soils and underlying material in association 3. In many places Clime and Sogn soils, closely intermingled and mapped together, border soils of this association (Soil Survey of Morris County, Kansas; 1974).

  14. KS-2012-01-25-02 | Osage County - March 1985

    Typical pattern of soils and parent material in the Kenoma-Dennis-Summit association (Soil Survey of Osage County, Kansas; 1985).

  15. KS-2012-01-25-09 | Pottawatomie County - December 1987

    Pattern of soils and parent material in the Clime-Tully-Benfield association (Soil Survey of Pottawatomie County, Kansas; 1987).

  16. KS-2012-01-25-10 | Pottawatomie County - December 1987

    Pattern of soils and parent material in the Pawnee-Wymore association (Soil Survey of Pottawatomie County, Kansas; 1987).

  17. KS-2012-01-25-11 | Pottawatomie County - December 1987

    Pattern of soils and parent material in the Wamego-Elmont association (Soil Survey of Pottawatomie County, Kansas; 1987).

  18. KS-2012-01-25-30 | Saline County - May 1992

    Pattern of soils and parent material in the Crete-Longford association (Soil Survey of Saline County, Kansas; 1992).

  19. KS-2012-01-25-31 | Saline County - May 1992

    Pattern of soils and parent material in the Irwin-Clime association (Soil Survey of Saline County, Kansas; 1992).

  20. KS-2012-01-26-18 | Wabaunsee County - May 1991

    Typical pattern of soils and parent material in the Clime-Sogn-Martin association (Soil Survey of Wabaunsee County, Kansas; 1991).

  21. KS-2012-01-26-19 | Wabaunsee County - May 1991

    Typical pattern of soils and parent material in the Florence-Irwin-Labette association (Soil Survey of Wabaunsee County, Kansas; 1991).

  22. KS-2012-01-26-20 | Wabaunsee County - May 1991

    Typical pattern of soils and parent material in the Irwin-Martin-Ladysmith association (Soil Survey of Wabaunsee County, Kansas; 1991).

  23. KS-2012-01-26-21 | Wabaunsee County - May 1991

    Typical pattern of soils and parent material in the Martin-Wamego-Elmont association (Soil Survey of Wabaunsee County, Kansas; 1991).

  24. KS-2012-01-26-22 | Wabaunsee County - May 1991

    Typical pattern of soils and parent material in the Pawnee-Martin-Wymore association (Soil Survey of Wabaunsee County, Kansas; 1991).

Map Units

Map units containing CLIME 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
Clime-Sogn complex, 3 to 20 percent slopes45903142126686581igwoks01519701:24000
Clime stony silty clay loam, 15 to 30 percent slopes4580613828592tt71ks01519701:24000
Clime-Sogn complex, 3 to 20 percent slopes45909588626686601igwoks01719671:24000
Clime silty clay loam, 20 to 40 percent slopes, stony4545475813828142tt6hks01719671:24000
Clime stony silty clay loam, 15 to 30 percent slopes458011913828152tt71ks01719671:24000
Clime-Sogn complex, 3 to 20 percent slopes45906493926686611igwoks01919721:24000
Clime stony silty clay loam, 15 to 30 percent slopes45804314533672tt71ks01919721:24000
Clime-Sogn complex, 3 to 20 percent slopes45901826687651igwoks02719831:24000
Clime-Sogn complex, 3 to 20 percent slopes45906481526687701igwoks03519771:24000
Clime stony silty clay loam, 15 to 30 percent slopes45801684913829262tt71ks03519771:24000
Clime-Sogn complex, 3 to 20 percent slopes45902545126687741igwoks04119771:24000
Clime silty clay loam, 3 to 7 percent slopes45551423614545512tt6kks04119771:24000
Clime silty clay loam, 7 to 15 percent slopes45601072414545522tt6lks04119771:24000
Clime silty clay loam, 1 to 3 percent slopes454013614545502tt6gks04119771:24000
Kipson-Clime complex, 6 to 20 percent slopes47204914545562ww03ks04119771:24000
Clime-Sogn complex, 3 to 20 percent slopes45906418226687761igwoks04919841:24000
Clime stony silty clay loam, 15 to 30 percent slopes4580942614532982tt71ks04919841:24000
Clime silty clay, 3 to 7 percent slopes457097014532972tt73ks04919841:24000
Clime-Sogn complex, 3 to 20 percent slopes45904935526687781igwoks06119911:24000
Clime silty clay loam, 20 to 40 percent slopes, very stony4550838613871822tt6jks06119911:24000
Clime-Sogn complex, 3 to 20 percent slopes459019243026687801igwoks07319811:24000
Clime silty clay, 3 to 7 percent slopes45701280414536422tt73ks07319811:24000
Clime stony silty clay loam, 15 to 30 percent slopes45801033914536432tt71ks07319811:24000
Clime-Hobbs complex, 0 to 20 percent slopes4585535611554252tt72ks07919701:24000
Clime silty clay, 1 to 3 percent slopes4565532311554222tt6wks07919701:24000
Clime silty clay, 3 to 7 percent slopes4570487311554232tt6xks07919701:24000
Clime silty clay loam, 7 to 15 percent slopes4560275411554212tt6lks07919701:24000
Clime silty clay, 3 to 7 percent slopes, eroded4575210611554242tt74ks07919701:24000
Clime silty clay loam, 1 to 3 percent slopes454028211554192tt6gks07919701:24000
Clime silty clay loam, 3 to 7 percent slopes455514911554202tt6kks07919701:24000
Clime-Sogn complex, 3 to 20 percent slopes45901810626687811igwoks08519761:24000
Clime-Sogn complex, 3 to 20 percent slopes45905754226687861igwoks11119771:24000
Clime silty clay, 3 to 7 percent slopes4570841214537032tt73ks11119771:24000
Clime silty clay, 3 to 7 percent slopes, eroded4575409614537042tt70ks11119771:24000
Tully-Clime complex, 7 to 15 percent slopes4788374014537172tt5lks11119771:24000
Clime silty clay loam, 3 to 7 percent slopes455514514537022tt6kks11119771:24000
Clime silty clay, 3 to 7 percent slopes4570752914292302tt6xks11319801:24000
Clime silty clay, 1 to 3 percent slopes4565429914292292tt6wks11319801:24000
Clime silty clay loam, 3 to 7 percent slopes455583614292282tt6kks11319801:24000
Clime silty clay loam, 1 to 3 percent slopes45406290113827642tt6gks11519811:24000
Clime silty clay loam, 3 to 7 percent slopes45552819813827652tt6kks11519811:24000
Clime-Sogn complex, 3 to 20 percent slopes45901807526687891igwoks11519811:24000
Clime stony silty clay loam, 15 to 30 percent slopes458076913827672tt71ks11519811:24000
Clime silty clay loam, 7 to 15 percent slopes4560313827662tt6lks11519811:24000
Clime-Sogn complex, 3 to 20 percent slopes4590385026687921igwoks11719771:24000
Clime-Sogn complex, 3 to 20 percent slopes45901599226687981igwoks12719701:24000
Clime-Sogn complex, 3 to 20 percent slopes459016526688001igwoks13119801:24000
Clime-Sogn complex, 3 to 20 percent slopes4590315026688021igwoks13919831:24000
Clime-Sogn complex, 3 to 20 percent slopes459010691126687431igwoks14919841:24000
Clime silty clay loam, 20 to 40 percent slopes, stony45451765514806922tt6hks14919841:24000
Clime silty clay, 1 to 3 percent slopes4565614332492tt6wks15919711:24000
Clime-Sogn complex, 3 to 20 percent slopes45907748626688101igwoks16119701:24000
Clime silty clay loam, 20 to 40 percent slopes, very stony45501777914723062tt6jks16119701:24000
Elmont-Clime complex, 5 to 15 percent slopes724552014723322xlgcks16119701:24000
Clime silty clay loam, 3 to 7 percent slopes45555014723072tt6kks16119701:24000
Clime silty clay loam, 3 to 7 percent slopes4555844113821572tt6kks16919891:24000
Kipson-Clime complex, 6 to 20 percent slopes4720525213821742ww03ks16919891:24000
Clime silty clay, 3 to 7 percent slopes45704813821582tt6xks16919891:24000
Clime silty clay, 3 to 7 percent slopes4570981214439502tt6xks17319761:24000
Clime-Sogn complex, 3 to 20 percent slopes459013997226688211igwoks19719881:24000
Clime silty clay loam, 20 to 40 percent slopes, stony4545963014721392tt6hks19719881:24000
Clime silty clay loam, 3 to 7 percent slopes4555345014721402tt6kks19719881:24000
Clime silty clay loam, 20 to 40 percent slopes, very stony455023414730192tt6jks19719881:24000
Clime-Sogn complex, 3 to 20 percent slopes4590102026688251igwoks20519851:20000
Clime-Sogn complex, 3 to 20 percent slopes4590112326688271igwoks20719731:20000
Clime silty clay, 3 to 7 percent slopes457041114271542tt73ks20719731:20000

Map of Series Extent

Approximate geographic distribution of the CLIME 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 .