Official Series Description


Lab Data Summary

Aggregate lab data for the KEELER soil series. This aggregation is based on all pedons with a current taxon name of KEELER, 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 KEELER 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 KEELER 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 KEELER 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 KEELER 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 KEELER 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 terrace figure.

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with KEELER 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 KEELER 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 KEELER 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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 KEELER, 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 KEELER 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
Keeler-Jacot complex, 30 to 55 percent slopesJg4j1687250197254ppid05720131:24000
Carrico-Keeler complex, 25 to 65 percent slopesCr3900644805pmz5id05720131:24000
Aldermand-Keeler, dry complex, 25 to 70 percent slopesAk2868644639pmstid05720131:24000
Keeler, dry-Keeler complex, 20 to 50 percent slopesKe3697644679pmv3id05720131:24000
Aldermand-Keeler complex, 10 to 35 percent slopesKe562916892801tptxid05720131:24000
Carrico-Cobbler-Keeler complex, 10 to 35 percent slopesKk155016892701tptlid05720131:24000
Keeler, warm-Keeler complex, 30 to 55 percent slopesKe6j20250206554pnid05720131:24000
Keeler-Kruse complex, 15 to 30 percent slopes541331830990112wcrid60619761:24000
Keeler-Kruse complex, 30 to 60 percent slopes5414443099059nvf7id60619761:24000
Keeler-Jacot complex, 30 to 55 percent slopes56351915347154ppid60819941:24000
Floodwood-Keeler, warm complex, 15 to 35 percent slopes25351315343754nlid60819941:24000
Keeler, warm-Keeler complex, 30 to 55 percent slopes55146715347054pnid60819941:24000
Floodwood-Keeler, warm complex, 35 to 65 percent slopes26128715343854nmid60819941:24000
Keeler, moist-Keeler complex, 35 to 75 percent slopes1354205777308v2vgid61220031:24000
Noil-Keeler complex, 40 to 75 percent slopes1773755768937tt4fid61220031:24000
Floodwood-Keeler complex, 15 to 35 percent slopes803696776647v254id61220031:24000
Keeler-Lado complex, 10 to 35 percent slopes1383068777368v2xdid61220031:24000
Keeler, dry-Keeler complex, 35 to 70 percent slopes1341799777309v2vhid61220031:24000
Keeler-Aldermand complex, 35 to 70 percent slopes1361572768938tt4gid61220031:24000
Floodwood, warm-Keeler complex, 35 to 65 percent slopes79817776648v255id61220031:24000
Floodwood-Keeler complex, 35 to 65 percent slopes81567776649v256id61220031:24000
Keeler-Jacot complex, 30 to 55 percent slopes137217776695v26pid61220031:24000
Bigtalk-Keeler complex, 15 to 35 percent slopes19159777361v2x5id61220031:24000
Floodwood-Keeler, warm complex, 15 to 35 percent slopes54nl24285096754nlid6701:24000
Keeler-Kruse complex, 15 to 30 percent slopes54133313858932wcrwa06320121:24000
Keeler-Kruse complex, 30 to 60 percent slopes54142058621216nvf7wa06320121:24000
Keeler fine gravelly ashy loam, 8 to 15 percent slopes5412718858922wcqwa06320121:24000
Keeler fine gravelly ashy loam, 8 to 15 percent slopes541218326513362wcqwa06519781:24000
Keeler-Kruse complex, 15 to 30 percent slopes541317426513372wcrwa06519781:24000

Map of Series Extent

Approximate geographic distribution of the KEELER 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 .