Official Series Description


Lab Data Summary

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

Competing Series

Soil series competing with COPPERBASIN 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 COPPERBASIN series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the COPPERBASIN 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 COPPERBASIN, 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 COPPERBASIN 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
Biglost-Copperbasin complex, 0 to 4 percent slopes, occasionally flooded12-CL1031736042scgid7031:24000
Wiskisprings-Biglost-Copperbasin complex, 0 to 3 percent slopes2397159831332shqid75219991:24000
Biglost-Copperbasin complex, 0 to 4 percent slopes, occasionally flooded126221830012scgid75219991:24000
Fezip-Redfish-Copperbasin complex, 0 to 3 percent slopes714170832322slxid75219991:24000
Copperbasin, cool-Redfish complex, 1 to 4 percent slopes363156831702sjxid75219991:24000
Lemhi-Copperbasin-Lilylake complex, 0 to 2 percent slopes1182533829992scdid75219991:24000
Wiggleton-Copperbasin complex, 0 to 4 percent slopes2341880831282shkid75219991:24000
Mahaffey-Copperbasin-Wiskisprings, complex 0 to 2 percent slopes1231155830052sclid75219991:24000
Copperbasin-Redfish complex, 0 to 3 percent slopes35835831692sjwid75219991:24000
Foxgulch, rarely flooded-Mooseflat, occasionally flooded-Copperbasin, rarely flooded complex, 0 to 4 percent slopes13B2631859516w8psmt60520071:24000
Medicinelodge, occasionally flooded-Copperbasin-Mooseflat complex, 0 to 4 percent slopes240B14926334312kp41mt60520071:24000
Foxgulch, rarely flooded-Mooseflat, occasionally flooded-Copperbasin, rarely flooded complex, 0 to 4 percent slopes13B16308812720w8psmt61020051:24000
Foxgulch-Copperbasin-Wisdom complex, 0 to 2 percent slopes15A9545812391w8c5mt61020051:24000
Mooseflat-Eachuston-Copperbasin complex, 0 to 2 percent slopes54A594712923271dcrzmt61020051:24000
Foxgulch-Bearmouth-Copperbasin complex, 0 to 4 percent slopes113B130915078451mm15mt61020051:24000
Mooseflat, occasionally flooded-Regulus, occasionally flooded-Copperbasin, rarely flooded complex, 0 to 4 percent slopes13B557214722021ldydmt61220111:24000
Medicinelodge, occasionally flooded-Copperbasin-Mooseflat complex, 0 to 4 percent slopes240B313923737952kp41mt61220111:24000
Copperbasin, rarely flooded-Finn-Mooseflat, occasionally flooded complex, 1 to 4 percent slopes280B27325153922ppjlmt61220111:24000
Thaincreek-Copperbasin family, rarely flooded-Redfish family, occasionally flooded, complex, 1 to 8 percent slopes, very stony1105C4730448352v1mqmt61519921:24000
Thaincreek-Copperbasin family, rarely flooded-Redfish family, occasionally flooded, complex, 1 to 8 percent slopes, very stony1105C30628336302v1mqmt6321:24000

Map of Series Extent

Approximate geographic distribution of the COPPERBASIN 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 .