Official Series Description


Lab Data Summary

Aggregate lab data for the KIDMAN soil series. This aggregation is based on all pedons with a current taxon name of KIDMAN, 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 KIDMAN 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
28A81P048581UT011001Kidman8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41,-112

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KIDMAN 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 KIDMAN 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 KIDMAN 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 KIDMAN 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 KIDMAN 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 KIDMAN 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 KIDMAN 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 .

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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.

Soil series sharing subgroup-level classification with KIDMAN, 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. ID-2010-08-30-04 | Franklin County Area - 2008

    Typical pattern of soils and underlying material in general soil map unit 4 (Welby-Kidman-Preston) (Soil Survey of Franklin County Area, Idaho; 2008).

Map Units

Map units containing KIDMAN 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
Kidman fine sandy loam, 0 to 2 percent slopes685182485315j90bid71419971:24000
Kidman fine sandy loam, 2 to 4 percent slopes692044485316j90cid71419971:24000
Kidman fine sandy loam, 20 to 40 percent slopes701706485318j90fid71419971:24000
Kidman fine sandy loam, wet, 0 to 2 percent slopes711277485319j90gid71419971:24000
Kidman-Sterling complex, 0 to 2 percent slopes72594485320j90hid71419971:24000
Kidman fine sandy loam, 1 to 4 percent slopes615554485657j9ccid71519941:24000
Kidman-Preston association, 2 to 12 percent slopes621638485658j9cdid71519941:24000
Kidman fine sandy loam, 0 to 2 percent slopesKlA5915481394j4xvut60219691:20000
Kidman loam, 1 to 6 percent slopesKmB2383481397j4xyut60219691:20000
Kidman loam, 10 to 20 percent slopesKmE655481399j4y0ut60219691:20000
Kidman loam, 6 to 10 percent slopesKmD588481398j4xzut60219691:20000
Kidman fine sandy loam, 2 to 4 percent slopesKlB432481395j4xwut60219691:20000
Kidman loam, 0 to 1 percent slopesKmA300481396j4xxut60219691:20000
KIDMAN FINE SANDY LOAM, DEEP WATER TABLE, 0 TO 2 PERCENT SLOPESKfA7937482752j6bnut60319681:20000
KIDMAN FINE SANDY LOAM, 0 TO 2 PERCENT SLOPESKdA2858482750j6blut60319681:20000
KIDMAN FINE SANDY LOAM, DEEP WATER TABLE, 4 TO 8 PERCENT SLOPESKfC581482754j6bqut60319681:20000
KIDMAN FINE SANDY LOAM, DEEP WATER TABLE, 2 TO 4 PERCENT SLOPESKfB362482753j6bput60319681:20000
KIDMAN FINE SANDY LOAM, 8 TO 15 PERCENT SLOPESKdD143482751j6bmut60319681:20000
Kidman fine sandy loam, 0 to 1 percent slopesKaA12194481583j53yut60719651:15840
Kidman fine sandy loam, 1 to 3 percent slopesKaB6428481584j53zut60719651:15840
Kidman fine sandy loam, 3 to 6 percent slopesKaC851481585j540ut60719651:15840
Francis-Kidman complex, 20 to 50 percent slopes, erodedFKG2633481555j531ut60719651:15840
Kidman fine sandy loam, 6 to 10 percent slopesKaD483481586j541ut60719651:15840
Kidman fine sandy loam, 10 to 20 percent slopes, erodedKaE2349481587j542ut60719651:15840
Rawnjay-Kidman-Sterling complex, 5 to 20 percent slopes801426829813772tjszut60819811:24000
Kidman-Sterling complex, 3 to 15 percent slopes802412729813712tjt9ut60819811:24000
Kidman very fine sandy loam, 1 to 3 percent slopesKdB3926482933j6jhut61219671:20000
Kidman very fine sandy loam, 0 to 1 percent slopesKdA3785482932j6jgut61219671:20000
Kidman very fine sandy loam, 3 to 6 percent slopesKdC554482934j6jjut61219671:20000
Kidman very fine sandy loam, silty clay loam substratum, 0 to 1 percent slopesKfA426482935j6jkut61219671:20000
Rawnjay-Kidman-Sterling complex, 5 to 20 percent slopes801437129813912tjszut61219671:20000
Kidman very fine sandy loam, silty clay loam substratum, 1 to 3 percent slopesKfB344482936j6jlut61219671:20000
Kidman-Sterling complex, 3 to 15 percent slopes802421329813872tjt9ut61219671:20000
Lodar-Kidman complex, 15 to 50 percent slopes861457481885j5fput61819951:24000
Kidman-Preston complex, 2 to 30 percent slopes76633481872j5f8ut61819951:24000
Kidman very fine sandy loam, 1 to 3 percent slopesKmB1738483319j6xyut62119661:20000
Kidman very fine sandy loam, 3 to 6 percent slopesKmC813483320j6xzut62119661:20000
Kidman very fine sandy loam, 0 to 1 percent slopesKmA800483318j6xxut62119661:20000
Kidman-Sterling complex, 3 to 15 percent slopes802441429813982tjt9ut62119661:20000
Rawnjay-Kidman-Sterling complex, 5 to 20 percent slopes80145629814012tjszut62119661:20000

Map of Series Extent

Approximate geographic distribution of the KIDMAN 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 .