Official Series Description


Lab Data Summary

Aggregate lab data for the CRAFT soil series. This aggregation is based on all pedons with a current taxon name of CRAFT, 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 CRAFT 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
60A88P076088NE165089Craft6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.8541679,-103.9497223
60A88P076488NE165090Craft6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.9900017,-103.757225

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CRAFT 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 CRAFT 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 CRAFT 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 CRAFT 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 CRAFT 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 CRAFT series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the CRAFT 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 CRAFT, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. SD-2012-03-15-38 | Haakon County - 1998

    Typical pattern of soils and parent material in the Bankard-Craft-Wendte, Ree, and Samsil-Pierre associations (Soil Survey of Haakon County, SD; 1998).

  2. SD-2012-03-15-53 | Jackson County, Northern Part - July 1987

    Pattern of soils and underlying material in the Samsil-Pierre and Haverson associations (Soil Survey of Jackson County, Northern Part, SD; 1987).

Map Units

Map units containing CRAFT 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
Craft very fine sandy loam, channeled11541160114955017l68ks02319871:24000
Craft very fine sandy loam, rarely flooded140612114955217l6bks02319871:24000
Craft very fine sandy loam, occasionally flooded56163838357776d095ne01319801:20000
Craft loam, channeled, frequently flooded5612111022175382dfjhne04519731:20000
Craft very fine sandy loam, channeled, frequently flooded5615226516990871v118ne05719951:24000
Craft very fine sandy loam, rarely flooded1406117016990861v117ne05719951:24000
Craft loam, channeled, frequently flooded5612330916993141v18lne08719651:20000
Craft very fine sandy loam, rarely flooded140617322288382dt90ne08719651:20000
Craft very fine sandy loam, channeled, frequently flooded561514522288492dt9cne08719651:20000
Craft very fine sandy loam, alkali, 0 to 2 percent slopes5617223416925971tt8xne12319811:20000
Craft loamy very fine sand, 0 to 2 percent slopes5613153116925951tt8vne12319811:20000
Craft very fine sandy loam, rarely flooded1406128516925961tt8wne12319811:20000
Craft loam, channeled, frequently flooded56125439357898d0f3ne16519931:20000
Craft loam, 0 to 2 percent slopes5610253833336432zj4tne16519931:20000
Craft loam, occasionally flooded5611140433336482zj4vne16519931:20000
Craft very fine sandy loam, 0 to 3 percent slopes, rarely floodedCtA21423540862zzvssd05519921:24000
Haverson-Craft complex, 0 to 3 percent slopes, rarely floodedHc15673540902zzw6sd05519921:24000
Craft very fine sandy loam, 0 to 3 percent slopes, rarely floodedCtA31103558352zzvssd13719851:24000
Haverson-Craft complex, 0 to 3 percent slopes, rarely floodedHc351225810212zzw6sd61120111:24000
Craft-Bankard variant very fine sandy loamsCv21932581011cy28sd61120111:24000

Map of Series Extent

Approximate geographic distribution of the CRAFT 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 .