Official Series Description


Lab Data Summary

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

Click the image to view it full size.

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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with SHANLEY, 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 SHANLEY 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
Braziel-Shanley gravelly loams, 15 to 35 percent slopes542E16261444854vbtmt62119971:24000
Shanley-Braziel-Water complex, 8 to 25 percent slopes142E10861442114v1zmt62119971:24000
Braziel-Shanley gravelly loams, 35 to 60 percent slopes542F10401444864vbvmt62119971:24000
Shanley-Tolbert complex, 15 to 35 percent slopes846E7961446134vgymt62119971:24000
Shanley gravelly loam, 15 to 35 percent slopes19E4791442724v3ymt62119971:24000
Shanley gravelly loam, 8 to 15 percent slopes19D4551442714v3xmt62119971:24000
Braziel-Shanley gravelly loams, 8 to 15 percent slopes542D3931444844vbsmt62119971:24000
Shanley stony loam, 15 to 35 percent slopes119E3521441854v14mt62119971:24000
Shanley-Tolbert complex, 8 to 15 percent slopes846D3111446124vgxmt62119971:24000
Shanley gravelly loam, 4 to 8 percent slopes19C1621442704v3wmt62119971:24000
Shanley-Tolbert complex, 35 to 60 percent slopes846F1481446144vgzmt62119971:24000
Shanley-Tolbert complex, 4 to 8 percent slopes846C501446114vgwmt62119971:24000
Braziel-Shanley gravelly loams, 4 to 8 percent slopes542C381444834vbrmt62119971:24000
Braziel-Shanley complex, 35 to 60 percent slopes542F16017029681v52gmt63520061:24000
Braziel-Shanley complex, 15 to 35 percent slopes542E15017029671v52fmt63520061:24000
Shanley, bouldery-Chivington-Meagher complex, 15 to 45 percent slopes999F204616132241r4phmt63720141:24000
Shanley-Wickes, bouldery-Sinnigam, very bouldery complex, 15 to 35 percent slopes680E160124797202p7bzmt63720141:24000
Shanley-Blaincreek, stony complex, 4 to 15 percent slopes140D969637148pd05mt63720141:24000
Blaincreek, stony-Braziel-Shanley complex, 15 to 35 percent slopes388E26724947432prr4mt63720141:24000
Shanley-Sawicki complex, 8 to 15 percent slopes358D1324380402mtzgmt63819851:24000

Map of Series Extent

Approximate geographic distribution of the SHANLEY 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 .