Official Series Description


Lab Data Summary

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

Soil series sharing subgroup-level classification with OWENSPRING, 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 OWENSPRING 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
Owenspring-Shineberger-Stubbs complex, 8 to 35 percent slopes15E15524962982p9ssid75819981:24000
Owenspring-Knep-Shineberger complex, 4 to 15 percent slopes15D2825118122p9wmid75819981:24000
Owenspring-Knep-Shineberger complex, 4 to 15 percent slopes15D275326114572mf55id76120181:24000
Owenspring-Shineberger-Stubbs complex, 8 to 35 percent slopes15E215826114722p9ssid76120181:24000
Ratiopeak, extremely bouldery-Crownmountain, stony-Owenspring, very stony families, complex, 4 to 15 percent slopes6212D241031692672tympmt60019691:24000
Lymanson-Knep-Shineberger complex, 4 to 15 percent slopes15D66124509162n8ctmt60520071:24000
Owenspring-Knep-Shineberger complex, 4 to 15 percent slopes15D698124257242mf55mt61220111:24000
Ratiopeak, extremely bouldery-Crownmountain, stony-Owenspring, very stony families, complex, 4 to 15 percent slopes6212D2430941022tympmt63019911:24000
Owenspring-Cheadle, extremely stony-Rockisland, stony families, complex, 4 to 25 percent slopes1175E589824376192mtjwmt6321:24000
Ratiopeak, extremely bouldery-Crownmountain, stony-Owenspring, very stony families, complex, 4 to 15 percent slopes6212D178728268462tympmt6321:24000
Kimpton-Owenspring complex, 35 to 60 percent slopes271F31124862512pg4nmt6321:24000
Kimpton-Owenspring complex, 35 to 60 percent slopes271F375413861441hjdbmt63720141:24000
Owenspring-Hardhart-Philipsburg complex, 2 to 8 percent slopes358C854780864v6k5mt63720141:24000
Owenspring-Cheadle, extremely stony-Rockisland, stony families, complex, 4 to 25 percent slopes1175E229796762mtjwmt63720141:24000
Ratiopeak, extremely bouldery-Crownmountain, stony-Owenspring, very stony families, complex, 4 to 15 percent slopes6212D34930941312tympmt65719901:24000

Map of Series Extent

Approximate geographic distribution of the OWENSPRING 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 .