Official Series Description


Lab Data Summary

Aggregate lab data for the COOERS soil series. This aggregation is based on all pedons with a current taxon name of COOERS, 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 COOERS 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
58A83P071274MT087116Cooers6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.5586128,-106.2649994
67A89P081589WY021001Cooers8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.2883339,-105.1905594

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the COOERS 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 COOERS 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 COOERS 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 COOERS 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 COOERS 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 COOERS 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 COOERS 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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Soil series sharing subgroup-level classification with COOERS, 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 COOERS 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
Birney-Cooers-Kirby complex, 2 to 15 percent slopes913D24343741cjpfmt01719951:24000
Cooers-Kirby-Rock outcrop complex, 8 to 25 percent slopes8E4934342309ch67mt02519911:24000
Delpoint-Cooers-Kirby complex, 15 to 35 percent slopes371E1547342215ch36mt02519911:24000
Tanna-Greybear-Cooers complex, 4 to 8 percent slopes126C112023932042lbb4mt62420211:24000
Tanna-Greybear-Cooers complex, 8 to 15 percent slopes126D108523932052lbb5mt62420211:24000
Tanna-Greybear-Cooers complex, 15 to 35 percent slopes126E69923938742lc0rmt62420211:24000
Tanna-Greybear-Cooers complex, 2 to 4 percent slopes126B34623886322l5knmt62420211:24000
Birney-Cooers-Kirby complex, 2 to 15 percent slopes189484348008cp42mt64919851:24000
Cooers-Yamac loams, 2 to 8 percent slopes665865348099cp70mt64919851:24000
Cooers-Birney complex, 2 to 8 percent slopes655016348098cp6zmt64919851:24000
Cooers loam, 2 to 8 percent slopes643485348097cp6ymt64919851:24000
Cooers-Albicalis-like, frequently flooded-Norte-like, frequently flooded complex, 1 to 8 percent slopes120831708382wxm4wy6171:24000
Foreleft-Cooers-Hawksell complex, 2 to 20 percent slopes231033583022wxlpwy6171:24000
Foreleft-Cooers-Hawksell complex, 20 to 30 percent slopes240733582842wxmkwy6171:24000
Cooers-Albicalis-like, frequently flooded-Norte-like, frequently flooded complex, 1 to 8 percent slopes120829690812wxm4wy6291:24000
Foreleft-Cooers-Hawksell complex, 2 to 20 percent slopes231029690682wxlpwy6291:24000
Cooers-Chickenhill complex, 4 to 15 percent slopes231832090482zdqdwy6291:24000
Foreleft-Cooers-Hawksell complex, 20 to 30 percent slopes240729690922wxmkwy6291:24000
Birney-like-Colstrip-Cooers complex, 4 to 30 percent slopes535232030702zbs1wy6291:24000
Snakedraw-Cooers-Cabbart complex, 8 to 15 percent slopes412632225102ztmnwy7371:24000

Map of Series Extent

Approximate geographic distribution of the COOERS 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 .