Official Series Description


Lab Data Summary

Aggregate lab data for the OBERT soil series. This aggregation is based on all pedons with a current taxon name of OBERT, 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 OBERT 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 OBERT 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 OBERT 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 OBERT 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 OBERT 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 OBERT 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 OBERT 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 OBERT 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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Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with OBERT, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. SD-2010-11-01-11 | Minnehaha County - 2004

    Typical pattern of soils and parent material in the Moody-Nora association (Soil Survey of Minnehaha County, South Dakota; 2004).

Map Units

Map units containing OBERT 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
Obert silt loam, 0 to 2 percent slopes, frequently ponded63635622159552y231ne00319751:20000
Obert silty clay loam, occasionally flooded63671559427111gbfsne02719821:20000
Obert silt loam, 0 to 2 percent slopes, frequently ponded63635422168102y231ne02719821:20000
Obert silt loam, 0 to 2 percent slopes, frequently ponded636314544277892y230ne03919731:20000
Obert silty clay loam, frequently ponded6364955427773gc44ne03919731:20000
Obert silt loam, occasionally flooded636628716997981v1s6ne07119841:20000
Obert soils, occasionally flooded63655216918321tsh7ne09519701:20000
Obert silt loam, 0 to 2 percent slopes, frequently ponded6363285725704772y231ne10719891:20000
Obert silty clay loam, frequently ponded63642147427410gbrfne11919811:20000
Obert silt loam, occasionally flooded6366510117096551vd15ne12119781:20000
Obert silt loam, occasionally flooded636695622290012dtg8ne12519581:20000
Obert soils, occasionally flooded6365441427513gbvrne12519581:20000
Obert silt loam, 0 to 2 percent slopes, frequently ponded636324054276142y231ne13919701:20000
Obert silty clay loam, frequently ponded63642587427651gc06ne14119841:20000
Obert silty clay loam, occasionally flooded6367180816914371ts2hne15519951:12000
Obert silty clay loam, frequently flooded6368129716914361ts2gne15519951:12000
Obert silty clay loam, frequently ponded636435916912561trwnne15919671:20000
Obert silty clay loam, frequently ponded6364432426836gb4xne16719801:20000
Obert silty clay loam, frequently ponded6364216426809gb41ne17919701:20000
Obert silt loam, 0 to 2 percent slopes, frequently ponded63631622173472y230ne17919701:20000
Obert silty clay loam, 0 to 1 percent slopesOb10884446068gz59sd09919951:24000

Map of Series Extent

Approximate geographic distribution of the OBERT 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 .