Official Series Description


Lab Data Summary

Aggregate lab data for the KAPOWSIN soil series. This aggregation is based on all pedons with a current taxon name of KAPOWSIN, 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 KAPOWSIN were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

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

Soil series competing with KAPOWSIN 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 KAPOWSIN 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 KAPOWSIN 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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Click the image to view it full size.

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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 KAPOWSIN, 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

No block diagrams are available.

Map Units

Map units containing KAPOWSIN 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
Kapowsin gravelly ashy loam, 15 to 30 percent slopes1011315738962t61ywa63419861:24000
Kapowsin gravelly ashy loam, 30 to 65 percent slopes102602738972t620wa63419861:24000
Kapowsin gravelly ashy loam, 6 to 15 percent slopes100493738952t61xwa63419861:24000
Kapowsin gravelly ashy loam, 0 to 6 percent slopes2211408741922t61wwa63519771:24000
Kapowsin gravelly ashy loam, 6 to 15 percent slopes235700741932t61xwa63519771:24000
Kapowsin variant gravelly clay loam, 0 to 5 percent slopes241090741942y5vkwa63519771:24000
Kapowsin gravelly ashy loam, 0 to 6 percent slopes19B51836746652t61wwa65319741:24000
Kapowsin gravelly ashy loam, 6 to 15 percent slopes19C18218746662t61xwa65319741:24000
Kapowsin gravelly ashy loam, 15 to 30 percent slopes19D3657746672t61ywa65319741:24000
Kapowsin gravelly loam, 50 to 70 percent slopes19F2555746692hppwa65319741:24000
Kapowsin gravelly ashy loam, 30 to 65 percent slopes19E1535746682t620wa65319741:24000
Urban land-Kapowsin complex, 0 to 5 percent slopes306833432420562zl8hwa65319741:24000
Urban land-Kapowsin complex, 12 to 35 percent slopes3070632420582zl8kwa65319741:24000
Urban land-Kapowsin complex, 5 to 12 percent slopes3069332420572zl8jwa65319741:24000
Kapowsin silt loam, 3 to 15 percent slopes51862324547322ndbxwa66719831:24000
Kapowsin silt loam, 0 to 3 percent slopes50805924546792nd96wa66719831:24000
Kapowsin stony loam, 3 to 15 percent slopes55154224547362ndc1wa66719831:24000
Kapowsin silt loam, 15 to 30 percent slopes52113724547332ndbywa66719831:24000
Kapowsin silt loam, 30 to 50 percent slopes5387224547342ndbzwa66719831:24000
Kapowsin stony loam, 0 to 3 percent slopes5453924547352ndc0wa66719831:24000
Urban land-Kapowsin complex, 0 to 5 percent slopes306873632270612zl8hwa77620211:24000
Urban land-Kapowsin complex, 5 to 12 percent slopes30691232270622zl8jwa77620211:24000
Urban land-Kapowsin complex, 12 to 35 percent slopes3070932270632zl8kwa77620211:24000

Map of Series Extent

Approximate geographic distribution of the KAPOWSIN 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 .