Official Series Description


Lab Data Summary

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

Soil series competing with VITROFF 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 VITROFF 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 VITROFF 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 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 VITROFF, 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 VITROFF 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
Foolhen, rarely flooded-Silas-Vitroff complex, 2 to 15 percent slopes522D10185969220f52mt60520071:24000
Vitroff-Elve-Karloff complex, 8 to 35 percent slopes, moderately impacted5009E97154844563zmt61620031:24000
Vitroff-Torpy loams, 35 to 60 percent slopes2705F103150989523mmt62719981:24000
Helmville-Sherlock-Vitroff families, complex, 0 to 15 percent slopes2110D50903384031316l3mt6331:24000
Vitroff-Torpy-Goosepeak families, complex, low relief mountain slopes and ridges75LB2764514956550mpmt63520061:24000
Vitroff-Torpy-Goosepeak families, complex, low relief mountain slopes and ridges, moist75LC2510814956450mnmt63520061:24000
Vitroff-Torpy-Goosepeak families, complex, low relief mountain slopes and ridges, cool75LD2482814956650mqmt63520061:24000
Torpy-Vitroff-Illiano families, complex, high relief mountain slopes and ridges, cool71LD3373314956150mkmt63520061:24000
Vitroff-Figaro-Goosepeak families, complex, moderately steep soft volcanics, moist22LD2302814957550n0mt63520061:24000
Torpy-Vitroff-Illiano families, complex, high relief mountain slopes and ridges71LB3206014955350m9mt63520061:24000
Torpy-Vitroff-Illiano families, complex, high relief mountain slopes and ridges, moist71LC3149014956250mlmt63520061:24000
Vitroff-Figaro-Goosepeak families, complex, moderately steep soft volcanics22LC2140514957350mymt63520061:24000
Evaro-Eastridge-Vitroff complex, 20 to 50 percent slopes548F41717031881v59kmt63520061:24000
Evaro-Vitroff complex, 8 to 30 percent slopes550E38417031891v59lmt63520061:24000
Evaro-Vitroff-Germangulch, very stony, complex, 20 to 50 percent slopes543F32517031861v59hmt63520061:24000
Vitroff-Torpy complex, 35 to 60 percent slopes2705F8717031181v579mt63520061:24000
Foolhen-Silas-Vitroff complex, 2 to 15 percent slopes522D3617031791v598mt63520061:24000
Silas-Vitroff complex, 2 to 15 percent slopes616D517031981v59wmt63520061:24000
Vitroff-Torpy-Goosepeak families complex, low relief mountain slopes and ridges75LB21517044931v6nnmt64419951:24000
Evaro-Eastridge-Vitroff complex, 20 to 50 percent slopes548F2761361830d4hymt67020071:24000
Evaro-Vitroff complex, 8 to 30 percent slopes550E2452361826d4htmt67020071:24000
Evaro-Vitroff-Germangulch, very stony complex, 20 to 50 percent slopes543F1192361835d4j3mt67020071:24000
Foolhen, rarely flooded-Silas-Vitroff complex, 2 to 15 percent slopes522D369320366brcdmt67020071:24000
Silas-Vitroff complex, 2 to 15 percent slopes616D21314247441jtkhmt67020071:24000

Map of Series Extent

Approximate geographic distribution of the VITROFF 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 .