Official Series Description


Lab Data Summary

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

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

Soil series sharing subgroup-level classification with COLORADO, 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 COLORADO 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
Colorado and Spur soils, 0 to 1 percent slopes, frequently floodedCo314963629472wt6xtx03319701:24000
Colorado and Spur soils, 0 to 1 percent slopes, occasionally floodedCSA97192962334f6kytx03319701:24000
Colorado loam, 0 to 1 percent slopes, frequently floodedLo22303638242vt86tx07519611:20000
Colorado loam, 0 to 1 percent slopes, frequently floodedCm123963639722vt86tx08119681:24000
Colorado and Spur soils, 0 to 1 percent slopes, frequently floodedSr41793641282wt6xtx08719651:20000
Colorado loamCo2983364098d6w3tx08719651:20000
Colorado clay loam, 0 to 1 percent slopes, rarely floodedCe8570364581307s2tx10119691:20000
Colorado very fine sandy loamCd2651364580d7cntx10119691:20000
Colorado and Yomont soils, frequently floodedCf2266364582d7cqtx10119691:20000
Colorado and Spur soils, 0 to 1 percent slopes, occasionally floodedCSA2623393605f6kytx11520041:24000
Colorado loam, 0 to 1 percent slopes, frequently floodedCd50523651152vt86tx12519651:20000
Colorado silt loam, 0 to 1 percent slopes, occasionally floodedSp171153658072vt8ctx15119641:24000
Colorado and Westola soils, 0 to 1 percent slopes, frequently floodedSo25703669632vt8htx19119651:20000
Colorado and Spur soils, 0 to 1 percent slopes, frequently floodedCd111573671262wt6xtx19719651:20000
Colorado clay loam, moist, 0 to 1 percent slopes, occasionally floodedCe4313367127307rwtx19719651:20000
Colorado silt loam, 0 to 1 percent slopes, occasionally floodedCf8483671282vt8ctx19719651:20000
Colorado loam, 0 to 1 percent slopes, occasionally floodedCa2258367426dbbgtx20519731:24000
Colorado and Westola soils, 0 to 1 percent slopes, frequently floodedCf23083684762vt8htx26319681:31680
Bippus and Colorado soils, rarely floodedBc1344370328dfc2tx31719681:24000
Colorado loam, 0 to 1 percent slopes, frequently floodedLo97353707222vt86tx33519651:20000
Colorado loam, 0 to 1 percent slopes, frequently flooded789703710322vt86tx35319791:24000
Colorado loam, occasionally flooded61939371031dg2rtx35319791:24000
Colorado and Westola soils, 0 to 1 percent slopes, frequently floodedCy235793717692vt8htx39919651:20000
Colorado and Spur soils, 0 to 1 percent slopes, frequently floodedCo138543720032wt6xtx41519661:24000
Mangum and Colorado soilsMc3980372010dh3btx41519661:24000
Colorado loam, 0 to 1 percent slopes, frequently floodedCd13803722372vt86tx43119741:31680
Colorado clay loam, 0 to 1 percent slopes, frequently floodedCd72813722652vt85tx43319701:24000
Colorado loam, moist, 0 to 1 percent slopes, frequently floodedCr20481391510307rxtx44119711:20000

Map of Series Extent

Approximate geographic distribution of the COLORADO 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 .