Official Series Description


Lab Data Summary

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the VIDRINE 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 VIDRINE 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 VIDRINE 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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.

Competing Series

Soil series competing with VIDRINE 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 VIDRINE 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 VIDRINE 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 .

There are insufficient data to create the 2D hillslope position figure.

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 VIDRINE, 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 VIDRINE 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
Kinder-Vidrine complex, 0 to 1 percent slopesKvA551253769202syc7la00120001:24000
Crowley-Vidrine complex, 0 to 1 percent slopesCr2782215861012thq2la00319781:24000
Kinder-Vidrine complex, 0 to 1 percent slopesWr168215861142syc7la00319781:24000
Crowley-Vidrine complex, 1 to 3 percent slopesCo215864362thq3la00319781:24000
Mowata-Vidrine complex, 0 to 1 percent slopes, rarely floodedMt12446714136962thq6la01919831:24000
Crowley-Vidrine complex, 0 to 1 percent slopesCr4446214136782thq2la01919831:24000
Vidrine silt loam, 1 to 3 percent slopesVn280914137022vv46la01919831:24000
Mowata-Vidrine complex, 0 to 1 percent slopes, rarely floodedMt2761817235282thq6la02319861:24000
Crowley-Vidrine complex, 0 to 1 percent slopesCw1439717235162thq2la02319861:24000
Crowley-Vidrine complex, 0 to 1 percent slopesCv6001510171222thq2la03919701:24000
Kinder-Vidrine complex, 0 to 1 percent slopesWv5891410171532syc7la03919701:24000
Crowley-Vidrine complex, 0 to 1 percent slopesCrA14828014146692thq2la05319891:24000
Mowata-Vidrine complex, 0 to 1 percent slopes, rarely floodedMwA1554614146852thq6la05319891:24000
Crowley-Vidrine complex, 1 to 3 percent slopesCrB1165614146702thq3la05319891:24000
Vidrine silt loam, 1 to 3 percent slopesVnB122414146882vv46la05319891:24000
Kinder-Vidrine complex, 0 to 1 percent slopesWv73528235602syc7la09719831:24000
Kinder-Vidrine silt loams, 0 to 1 percent slopesKvA470823569wmzrla09719831:24000

Map of Series Extent

Approximate geographic distribution of the VIDRINE 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 .