Official Series Description


Lab Data Summary

Aggregate lab data for the KEWAKE soil series. This aggregation is based on all pedons with a current taxon name of KEWAKE, 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 KEWAKE 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 KEWAKE 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 KEWAKE 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 KEWAKE 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 KEWAKE 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 KEWAKE 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 KEWAKE 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 KEWAKE 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 KEWAKE, 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 KEWAKE 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
Kewake-Helphenstein, dry, complex, 0 to 25 percent slopes383960916898901tqglor63520061:24000
Kewake-Turpin complex, sodic, 0 to 45 percent slopes387632416898941tqgqor63520061:24000
Southcat-Kewake complex, 1 to 15 percent slopes603507316901031tqpgor63520061:24000
Kewake-Turpin complex, 0 to 45 percent slopes386414916898931tqgpor63520061:24000
Turpin-Kewake-Playas complex, 0 to 15 percent slopes643390916901431tqqror63520061:24000
Kewake ashy loamy sand, 2 to 45 percent slopes380312016898881tqgjor63520061:24000
Kewake-Helphenstein complex, 0 to 25 percent slopes382293916898891tqgkor63520061:24000
Mesman-McConnel-Kewake complex, 2 to 8 percent slopes447226016899511tqjkor63520061:24000
Helphenstein-Kewake complex, 0 to 45 percent slopes361207616898691tqfxor63520061:24000
Thornlake-Kewake complex, 2 to 15 percent slopes630199116901301tqqbor63520061:24000
Helphenstein-Turpin-Kewake complex, 0 to 15 percent slopes364137616898721tqg0or63520061:24000
Thornlake-Catlow-Kewake complex, 1 to 45 percent slopes629135116901291tqq9or63520061:24000
Kewake-Ozamis-Reese complex, 0 to 15 percent slopes38543616898921tqgnor63520061:24000
Kewake-Icene complex, 0 to 15 percent slopes38418416898911tqgmor63520061:24000
Kewake-Helphenstein complex, 0 to 15 percent slopes119C21055488909jdr8or63619911:24000
Kewake-Helphenstein complex, 0 to 25 percent slopes474C552917209841vrtmor63619911:24000
Kewake-Icene complex, 0 to 15 percent slopes120C3598488912jdrcor63619911:24000
Helphenstein-Turpin-Kewake complex, 0 to 15 percent slopes112C2019488900jdqzor63619911:24000
Kewake-Ozamis-Reese complex, 0 to 15 percent slopes121C1887488914jdrfor63619911:24000
Southcat-Kewake complex, 1 to 15 percent slopes484B56817209861vrtpor63619911:24000
Kewake ashy loamy sand, 2 to 45 percent slopes409C8517209761vrtcor63619911:24000

Map of Series Extent

Approximate geographic distribution of the KEWAKE 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 .