Official Series Description


Lab Data Summary

Aggregate lab data for the CROSGRAIN soil series. This aggregation is based on all pedons with a current taxon name of CROSGRAIN, 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 CROSGRAIN 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 CROSGRAIN 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 CROSGRAIN 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 CROSGRAIN 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 CROSGRAIN 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 CROSGRAIN 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 CROSGRAIN 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 CROSGRAIN 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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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with CROSGRAIN, 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 CROSGRAIN 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
Crosgrain extremely gravelly loam, 8 to 30 percent slopes11012070466593hnjdca69720001:24000
Crosgrain-Twobitter association, 4 to 30 percent slopes1116006466610hnjyca69720001:24000
Juratrias-crosgrain association, 15 to 50 percent slopes1094145466725hnnnca69720001:24000
Crosgrain-Cronese-Arizo association, 2 to 8 percent slopes1122508466685hnmcca69720001:24000
Crosgrain complex, 2 to 8 percent slopes1142100466687hnmfca69720001:24000
Crosgrain-Popups complex, 4 t0 15 percent slopes1131380466686hnmdca69720001:24000
Crosgrain-Fortirwin complex, 2 to 8 percent slopes2611314466697hnmrca69720001:24000
Fortirwin-Crosgrain association, 2 to 15 percent slopes310969466651hnl8ca69720001:24000
Arizo-Crosgrain-Twobitter association, 2 to 15 percent slopes351393114034611j3dyca6981:24000
Crosgrain-Crackerjack-Pinkcan complex, 4 to 30 percent slopes403144625052032pz5bca79420121:24000
Crosgrain-Irongold associationCID28906189751221pj2nv60819671:24000
Haleburu-Crosgrain-Rock outcrop association75024328468950hqzfnv75520061:24000
Crosgrain-Irongold-Nickel association24021447468844hqw0nv75520061:24000
Arizo-Peskah-Crosgrain association4519992468884hqx9nv75520061:24000
Tenwell-Crosgrain association1107726468808hqtvnv75520061:24000
Crosgrain-Typic Torriorthents-Nickel association2414853468845hqw1nv75520061:24000
Crosgrain very stony loam, 8 to 30 percent slopes6613924468928hqyqnv75520061:24000
Crosgrain-Tenwell association1203645468810hqtxnv75520061:24000
Crosgrain-Vace association6653498468931hqytnv75520061:24000
Crosgrain-Arizo association6623288468929hqyrnv75520061:24000
Crosgrain-Kidwell-Arizo association6633017468930hqysnv75520061:24000
Nickel-Crosgrain association2112961468840hqvwnv75520061:24000
Peskah-Crosgrain association6502726468925hqymnv75520061:24000
Crosgrain extremely gravelly loam, 4 to 15 percent slopes6602560468927hqypnv75520061:24000
Haleburu-Crosgrain-Rock outcrop association4501030469317hrc8nv78819821:24000
Nickel-Crosgrain association21143216809921tf6knv78819821:24000
Crosgrain very stony loam, 8 to 30 percent slopes66116416810061tf70nv78819821:24000

Map of Series Extent

Approximate geographic distribution of the CROSGRAIN 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 .