Official Series Description


Lab Data Summary

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

There are insufficient data to create the water balance bar figure.



There are insufficient data to create the water balance line figure.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the SCHLEYER series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the SCHLEYER series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the SCHLEYER 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 .

Click the image to view it full size.

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.

Competing Series

Soil series competing with SCHLEYER share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the SCHLEYER 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 SCHLEYER 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 .

Click the image to view it full size.

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 SCHLEYER, 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 SCHLEYER 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
Schleyer-Geist complex, 0 to 30 percent slopesGO1925514833711lskpak65620051:24000
Turbellina-Schleyer complex, 0 to 30 percent slopesGO3302014833731lskrak65620051:24000
Schleyer-Slana-Geist complex, 0 to 70 percent slopesGO2191214833721lskqak65620051:24000
Kuswash-Turbellina-Schleyer complex, 0 to 30 percent slopesGO4104814833741lsksak65620051:24000
Skarland-Schleyer complex, 8 to 20 percent slopesAFK101014833541lsk4ak65620051:24000
Schleyer-Broxson-Riverwash complexAFL52714833551lsk5ak65620051:24000
Schleyer silt loam, 0 to 5 percent slopesAFF19814833531lsk3ak65620051:24000
Schleyer-Geist complex, 0 to 30 percent slopesGO16561244533844821lskpak65920241:63360
Ahtell-Donoho-Chisana complex, 2 to 70 percent slopes8MT199086340609731d3rak65920241:63360
Schleyer-Slana-Geist complex, 0 to 70 percent slopesGO272233844831lskqak65920241:63360
Kuswash-Turbellina-Schleyer complex, 0 to 30 percent slopesGO449133844851lsksak65920241:63360
Turbellina-Schleyer complex, 0 to 30 percent slopesGO344833844841lskrak65920241:63360
Skarland-Schleyer complex, 8 to 20 percent slopesAFK34433844771lsk4ak65920241:63360
Schleyer silt loam, 0 to 5 percent slopesAFF24033844761lsk3ak65920241:63360
Schleyer-Broxson-Riverwash complexAFL23133844781lsk5ak65920241:63360
Ahtell-Donoho-Chisana complex, 2 to 70 percent slopes8MT1968659335481331d3rak7691:250000

Map of Series Extent

Approximate geographic distribution of the SCHLEYER 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 .