Official Series Description


Lab Data Summary

Aggregate lab data for the KIM soil series. This aggregation is based on all pedons with a current taxon name of KIM, 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 KIM 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
58B40A3119S1969WY019001Kim6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.709446,-106.226387
58B40A3120S1969WY019008Kim2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.8388901,-106.6549988
67A40A3453S1950WY015005Kim6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.9994431,-104.3122253
67A40A3454S1952WY015003Kim6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.9238892,-104.2649994
67B07N012507CO087004Kim8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4361115,-103.8077469
67B88P053488CO063163Kim6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1286125,-102.4633331
67B01P0165S2001CO069001Kim8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6578064,-104.9996109

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KIM 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 KIM 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 KIM 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 KIM 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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Competing Series

Soil series competing with KIM 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 KIM 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 KIM 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 KIM, 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. CO-2011-05-27-03 | Bent County - 1971

    Representation pattern of soil and underlying materials in association 5 (Soil Survey of Bent County, Colorado; 1971).

  2. CO-2011-05-27-09 | Otero County - 1972

    Travessilla-Kim-Wiley soil association (Soil Survey of Otero County, Colorado; 1972).

  3. CO-2011-05-27-11 | Otero County - 1972

    Cross section of Otero County showing relief, drainage, and relation of soils to underlying geologic formations (Soil Survey of Otero County, Colorado; 1972).

  4. KS-2012-01-20-20 | Cheyenne County - June 1989

    Typical pattern of soils and parent material in the Colby-Ulysses-Keith association (Soil Survey of Cheyenne County, Kansas; 1989).

  5. KS-2012-01-20-21 | Cheyenne County - June 1989

    Typical pattern of soils and parent material in the Manter-Satanta-Kim association (Soil Survey of Cheyenne County, Kansas; 1989).

  6. KS-2012-01-26-25 | Wallace County - March 1986

    Typical pattern of soils and underlying material in the Colby-Kim-Midway association (Soil Survey of Wallace County, Kansas; 1986).

  7. WY-2012-03-23-08 | Goshen County, Southern Part - November 1971

    Typical pattern of soils, topography, and parent material in association 7 (Soil Survey of Goshen County, Wyoming, Southern Part; 1971).

Map Units

Map units containing KIM 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
Kim loam, 0 to 9 percent slopesKmD1084094199350pco00919661:20000
Kim-Midway complex, 6 to 15 percent slopes25907594313354cco01719851:24000
Stoneham-Kim loams, 6 to 12 percent slopes438879943333550co01719851:24000
Kim loam, 3 to 12 percent slopes227634943103548co01719851:24000
Kim loam, 1 to 3 percent slopes, eroded216725943093547co01719851:24000
Kim-Canyon loams, 5 to 35 percent slopes24249494312354bco01719851:24000
Kim-Pultney complex, 1 to 9 percent slopes26220594314354dco01719851:24000
Kim-Canyon loams, 2 to 5 percent slopes231365943113549co01719851:24000
Kim-Harvey-Stoneham loams, 1 to 3 percent slopes2110336944303584co06119771:24000
Kim-Stoneham-Larimer loams, 3 to 12 percent slopes227686944313585co06119771:24000
Thedalund-Kim-Shingle complex, 9 to 20 percent slopes109906794470359fco07519741:24000
Kim loam, 3 to 9 percent slopes5146859453435chco07519741:24000
Kim loam, 3 to 6 percent slopes2424499506735xpco12519761:24000
Kim-Mitchell complex, 0 to 6 percent slopes31640839512335zhco61719801:24000
Kim-Mitchell complex, 6 to 9 percent slopes32224829512435zjco61719801:24000
Kim-Shingle complex, 6 to 30 percent slopes33124269512535zkco61719801:24000
Kim loam, 1 to 3 percent slopes324226795211362bco61819761:24000
Kim loam, 3 to 5 percent slopes33712295212362cco61819761:24000
Kim loam, 5 to 9 percent slopes34625695213362dco61819761:24000
Kim loam, 0 to 1 percent slopes314182952103629co61819761:24000
Kim-Cascajo complex, 1 to 12 percent slopes273427496462jnlxco62719801:24000
Kim fine sandy loam, 3 to 9 percent slopes262514496461jnlwco62719801:24000
Kim loam, cool, 3 to 8 percent slopes509739498317jqjrco63719861:24000
Kim-Shingle complex, 3 to 20 percent slopes536212498320jqjvco63719861:24000
Kim loam, moderately wet, 0 to 3 percent slopes51707498318jqjsco63719861:24000
Nunn-Kim complexNv2664497596jpshco64319751:20000
Kim loam, 1 to 3 percent slopes538257497702jpwxco64419801:24000
Kim loam, 3 to 5 percent slopes547915497703jpwyco64419801:24000
Kim-Thedalund loams, 3 to 15 percent slopes564659497705jpx0co64419801:24000
Kim loam, 5 to 9 percent slopes554018497704jpwzco64419801:24000
Kim loam, 3 to 6 percent slopes402100496782jny7co68319771:24000
Kim loam, 6 to 12 percent slopes411200496783jny8co68319771:24000
Canyon-Kim loams, 5 to 30 percent slopes156815263114955917l6kks02319871:24000
Kim loam, 3 to 6 percent slopes16294778114956817l6vks02319871:24000
Kim loam, 1 to 3 percent slopes16281926114956717l6tks02319871:24000
Kim-Razor complex, 3 to 6 percent slopes16461510114956917l6wks02319871:24000
Kim-Penden silty clay loams, 3 to 6 percent slopes, eroded16436713804332yl3rks05719621:24000
Kim-Penden clay loams, 6 to 15 percent slopes16375765611506802yl3pks06319741:24000
Kim-Penden silty clay loams, 3 to 6 percent slopes, eroded16431944011523892yl3rks08319661:24000
Kim-Penden clay loams, 6 to 15 percent slopes1637452111520242yl3pks10119661:24000
Penden-Kim clay loams, 3 to 6 percent slopes, eroded2763348211520362twf2ks10119661:24000
Kim-Penden clay loams, 6 to 15 percent slopes, eroded1638252511520252yl3qks10119661:24000
Kim-Otero complex, 6 to 25 percent slopes1634458115052317m6nks10919621:24000
Kim-Penden clay loams, 6 to 15 percent slopes16375511520802yl3pks13519711:24000
Kim-Penden silty clay loams, 3 to 6 percent slopes, eroded16431011520812yl3rks13519711:24000
Kim-Otero complex, 6 to 25 percent slopes16343244114962117l8kks18119671:24000
Canyon-Kim loams, 5 to 30 percent slopes156866114960917l85ks18119671:24000
Kim-Penden clay loams, 6 to 15 percent slopes163735511508612yl3pks19519861:24000
Kim-Otero complex, 6 to 25 percent slopes163425662115019817lw5ks19919841:24000
Kim loam, 4 to 15 percent slopesKg7496346023cm21mt60719701:24000
Kim-Manzano associationKm775943031454dmv7nm05919721:24000
Kim-Manzano association, moist, 0 to 9 percent slopesKmmD1454230315472xxtjnm05919721:24000
Kim sandy loam, 1 to 9 percent slopesKaD71873031453dmv6nm05919721:24000
Kim sandy loam, moist, 1 to 9 percent slopesKamD195330315462xxthnm05919721:24000
Shingle, eroded-Kim associationSL9439556911vyhnm60019731:24000
Kim-Badland associationKD2966556521vx7nm60019731:24000
Kim fine sandy loam 1 to 8 percent slopesKaB1760556591vxgnm60019731:24000
Kim silty clay loam, 3 to 5 percent slopesKbB1380556601vxhnm60019731:24000
Hernandez-Kim association, 1 to 5 percent slopesHKC2438507820k1f9nm67019761:24000
Kim-Pastura-Tapia loamsKp4905814739281lgr2nm67419651:24000
Kim-Otero-Pastura complexKo710314739271lgr1nm67419651:24000
Kim-Pinon-Witt loamsKw679214739291lgr3nm67419651:24000
Kim loam, 3 to 5 percent slopesBc49332382053dtk9ok02519581:20000
Kim loam, 1 to 3 percent slopesBb6986382052dtk8ok02519581:20000
Kim fine sandy loam, 3 to 5 percent slopesBa6892382051dtk7ok02519581:20000
Kim-Zigweid loams, 3 to 10 percent slopes902435349370cqk0wy01119781:24000
Kim loam, 1 to 6 percent slopes872209349367cqjxwy01119781:24000
Kim loam, 6 to 10 percent slopes881684349368cqjywy01119781:24000
Kim clay loam, 0 to 3 percent slopes89731349369cqjzwy01119781:24000
Kim clay loam, alkali, 0 to 1 percent slopesKyA139831047103hyrwy61519651:20000
Kim clay loam, alkali, 3 to 10 percent slopesKyC69751047123hytwy61519651:20000
Kim clay loam, alkali, 1 to 3 percent slopesKyB51551047113hyswy61519651:20000
Kim-Haverson associationKH10251350867cs39wy61919711:24000
Kim-Travessilla associationKT8046350868cs3bwy61919711:24000
Kim-Zigweid association, gently slopingKZB5399350869cs3cwy61919711:24000
Stoneham-Kim associationSTf3986350942cs5qwy61919711:24000
Otero-Kim associationOK3375350899cs4bwy61919711:24000
Potts-Kim associationPS2884350905cs4jwy61919711:24000
Kim-Zigweid association, moderately steepKZD2045350870cs3dwy61919711:24000
Kim loam, 3 to 6 percent slopesKdB1246350872cs3gwy61919711:24000
Kim loam, 0 to 3 percent slopesKdA951350871cs3fwy61919711:24000
Kim loam, 6 to 10 percent slopesKdC709350873cs3hwy61919711:24000
Kim loam, wetKe490350874cs3jwy61919711:24000
Kim-Mitchell complex, 0 to 6 percent slopes788181047943j1gwy62119801:24000
Kim-Mitchell complex, 6 to 9 percent slopes73351047913j1cwy62119801:24000

Map of Series Extent

Approximate geographic distribution of the KIM 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 .