Official Series Description


Lab Data Summary

Aggregate lab data for the SHAVENAUGH soil series. This aggregation is based on all pedons with a current taxon name of SHAVENAUGH, 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 SHAVENAUGH 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
9697P0135S1996MI019004Shavenaugh6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.6952782,-85.8927765
9740A1916S1975MI021012Shavenaugh7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0233611,-86.3944444
9811N0158S2010MI117006Shavenaugh6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1374167,-85.25925

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SHAVENAUGH 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 SHAVENAUGH 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 SHAVENAUGH 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 SHAVENAUGH 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 SHAVENAUGH 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 SHAVENAUGH 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 SHAVENAUGH 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 SHAVENAUGH, 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 SHAVENAUGH 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
Shavenaugh sand, 0 to 6 percent slopes109B90431933606h6fmi61420051:12000
Boyer-Shavenaugh complex, 0 to 6 percent slopes120B28181935096hc7mi61420051:12000
Spinks-Shavenaugh sands, 0 to 6 percent slopes118B22211935036hc1mi61420051:12000
Shavenaugh sand, 6 to 12 percent slopes109C19201933596h6dmi61420051:12000
Shavenaugh sand, 18 to 35 percent slopes109E14721933576h6bmi61420051:12000
Shavenaugh sand, 12 to 18 percent slopes109D10441933586h6cmi61420051:12000
Spinks-Shavenaugh sands, 6 to 12 percent slopes118C10161935046hc2mi61420051:12000
Spinks-Shavenaugh sands, 12 to 18 percent slopes118D7661935056hc3mi61420051:12000
Boyer-Shavenaugh complex, 6 to 12 percent slopes120C6941935106hc8mi61420051:12000
Spinks-Shavenaugh sands, 18 to 35 percent slopes118E6881935066hc4mi61420051:12000
Spinks-Shavenaugh sands, 35 to 50 percent slopes118F3351935076hc5mi61420051:12000
Boyer-Shavenaugh complex, 12 to 18 percent slopes120D279893251yzhkmi61420051:12000
Boyer-Shavenaugh complex, 35 to 50 percent slopes120F274894102z0d0mi61420051:12000
Boyer-Shavenaugh complex, 18 to 35 percent slopes120E2581935116hc9mi61420051:12000
Shavenaugh sand, 35 to 50 percent slopes109F1421933566h69mi61420051:12000

Map of Series Extent

Approximate geographic distribution of the SHAVENAUGH 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 .