Official Series Description


Lab Data Summary

Aggregate lab data for the FOSTER soil series. This aggregation is based on all pedons with a current taxon name of FOSTER, 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 FOSTER 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 FOSTER 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 FOSTER 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 FOSTER 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 FOSTER 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 FOSTER 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 FOSTER 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 FOSTER 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 FOSTER, 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 FOSTER 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
Foster very fine sandy loam, very porly drained, slightly saline-alkali, 0 to 1 percent slopesFoA128462581hjbzca64419591:24000
Foster fine sandy loam, slightly saline-alkali, 0 to 1 percent slopesFdA856463021hjt5ca64819591:20000
Foster fine sandy loam, very poorly drained, 0 to 1 percent slopesFbA628463019hjt3ca64819591:20000
Foster fine sandy loam, 0 to 1 percent slopesFaA322463018hjt2ca64819591:20000
Foster fine sandy loam, very poorly drained, slightly saline- alkali, 0 to 1 percent slopesFcA211463020hjt4ca64819591:20000
Foster gravelly fine sandy loam, 0 to 1 percent slopesFeA202463022hjt6ca64819591:20000
Foster loams, 0 to 1 percent slopesFbA1747463399hk6cca65119591:20000
Foster clay loam, slightly saline-alkali, 0 to 1 percent slopesFaaA924463396hk68ca65119591:20000
Foster-Chino loams, strongly saline alkali, 0 to 1 percent slopesFdcA642463406hk6lca65119591:20000
Foster loams, moderately saline-Alkali, 0 to 1 percent slopesFbbA470463401hk6fca65119591:20000
Foster loams, strongly saline-Alkali, 0 to 1 percent slopesFbcA336463402hk6gca65119591:20000
Foster clay loam, 0 to 1 percent slopesFaA333463395hk67ca65119591:20000
Foster loams, slightly saline-Alkali, 0 to 1 percent slopesFbaA329463400hk6dca65119591:20000
Foster clay loam, moderately saline-alkali, 0 to 1 percent slopesFabA319463397hk69ca65119591:20000
Foster loams, moderately deep and deep over temple soils, 0 to percent slopesFbeA299463404hk6jca65119591:20000
Foster clay loam, strongly saline-alkali, 0 to 1 percent slopesFacA150463398hk6bca65119591:20000
Foster loams, moderately deep and deep over temple soils, moderately saline-Alkali, 0 to 1 percent slopesFcbA38463405hk6kca65119591:20000
Foster loams, sandy substratum, 0 to 1 percent slopesFbdA20463403hk6hca65119591:20000
Foster sandy loamFm2657464299hl4dca65419661:24000
Foster loamFn1234464300hl4fca65419661:24000
Foster loam, moderately deep, saline-alkaliFr1233464303hl4jca65419661:24000
Foster loam, saline-alkaliFo388464301hl4gca65419661:24000
Foster loam, moderately deepFp347464302hl4hca65419661:24000

Map of Series Extent

Approximate geographic distribution of the FOSTER 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 .