Official Series Description


Lab Data Summary

Aggregate lab data for the CROW soil series. This aggregation is based on all pedons with a current taxon name of CROW, 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 CROW 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
43B84P055783MT077002CROW6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7666664,-112.8166656
43B89P034888MT077943UCrow6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.8094444,-112.7305527
43B92P031690MT039898Crow7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.75,-113.1833344

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CROW 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 CROW 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 CROW 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 CROW 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 CROW 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 CROW 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 CROW 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 terrace figure.

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Soil series sharing subgroup-level classification with CROW, 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 CROW 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
Crow-Lubrecht loams, 8 to 35 percent slopes630E1265346865cmy6mt61519921:24000
Crow-Bignell complex, 15 to 35 percent slopes983E24821446654vjmmt62119971:24000
Crow-Bignell complex, 8 to 15 percent slopes983D12211446644vjlmt62119971:24000
Bignell-Yreka-Crow complex, 15 to 35 percent slopes799E7131445854vg1mt62119971:24000
Bignell-Yreka-Crow complex, 8 to 15 percent slopes799D1891445844vg0mt62119971:24000
Crow clay loam, 4 to 15 percent slopes83D1141446084vgsmt62119971:24000
Crow silt loam, 15 to 35 percent slopes83E141446094vgtmt62119971:24000
Crow clay loam, moist, 4 to 15 percent slopes283D41443124v57mt62119971:24000
Crow loam, 4 to 25 percent slopes415D29531478124yt4mt63019911:24000
Crow-Bignell complex, 15 to 35 percent slopes983E37017030151v53zmt63520061:24000
Crow-Bignell complex, 8 to 15 percent slopes983D27717030141v53ymt63520061:24000
Crow clay loam, 4 to 15 percent slopes83D16717032271v5btmt63520061:24000
Bignell-Yreka-Crow complex, 15 to 35 percent slopes799E10917030111v53vmt63520061:24000
Crow clay loam, 15 to 35 percent slopes83E8017032281v5bvmt63520061:24000
Crow silt loam, 4 to 15 percent slopes3374871454504wbymt63819851:24000
Crow-Bignell complex, 15 to 35 percent slopes983E74451459764wwxmt64419951:24000
Crow-Bignell complex, 8 to 15 percent slopes983D31691459754wwwmt64419951:24000
Bignell-Yreka-Crow complex, 15 to 35 percent slopes799E25041458944wt8mt64419951:24000
Crow clay loam, moist, 4 to 15 percent slopes283D23701456444wk6mt64419951:24000
Crow clay loam, moist, 15 to 35 percent slopes283E23671456454wk7mt64419951:24000
Crow clay loam, 15 to 35 percent slopes83E20071459174wv0mt64419951:24000
Crow-Bignell complex, moist, 8 to 25 percent slopes883E6371459454wvxmt64419951:24000
Crow clay loam, 4 to 15 percent slopes83D5821459164wtzmt64419951:24000
Bignell-Yreka-Crow complex, 8 to 15 percent slopes799D4941458934wt7mt64419951:24000
Crow-Bignell complex, moist, 25 to 50 percent slopes883F2311459464wvymt64419951:24000
Crow-Haugan-Curlew families, complex, fan remnants17B33916633754p8gpmt64520131:12000
Crow-Haugan-Curlew families, complex, fan remnants17B336398150221519vmt64720071:24000

Map of Series Extent

Approximate geographic distribution of the CROW 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 .