Official Series Description


Lab Data Summary

Aggregate lab data for the VANSON soil series. This aggregation is based on all pedons with a current taxon name of VANSON, 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 VANSON 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
381P054281WA059004Vanson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.3263893,-122.2455521

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the VANSON 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 VANSON 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 VANSON 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 VANSON 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.

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

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with VANSON 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 VANSON 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 VANSON 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 VANSON, 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 VANSON 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
Vanson-Hatchet complex, 30 to 65 percent slopes2407550723402f8kwa01519941:24000
Vanson sandy loam, 30 to 65 percent slopes2304995723222f7zwa01519941:24000
Vanson-Rock outcrop complex, 65 to 90 percent slopes2433550723492f8vwa01519941:24000
Vanson loamy sand, overblown, 30 to 65 percent slopes2253520723152f7rwa01519941:24000
Vanson sandy loam, 5 to 30 percent slopes2293440723192f7wwa01519941:24000
Vanson-Hatchet complex, 5 to 30 percent slopes2392715723372f8gwa01519941:24000
Vanson-Hatchet loamy sands, overblown, 30 to 65 percent slopes2372460723352f8dwa01519941:24000
Vanson sandy loam, tuff substratum, 5 to 30 percent slopes2321970723282f85wa01519941:24000
Vanson-Hatchet complex, 65 to 90 percent slopes2411675723432f8nwa01519941:24000
Vanson sandy loam, tuff substratum, 30 to 65 percent slopes2331640723312f88wa01519941:24000
Vanson loamy sand, till substratum, overblown, 30 to 65 percent slopes2281570723182f7vwa01519941:24000
Vanson-Hatchet, loamy sands, overblown, 5 to 30 percent slopes2361520723342f8cwa01519941:24000
Vanson-Rock outcrop complex, 30 to 65 percent slopes2421480723462f8rwa01519941:24000
Vanson loamy sand, overblown, 5 to 30 percent slopes2241465723142f7qwa01519941:24000
Vanson loamy sand, overblown, 65 to 90 percent slopes2261020723162f7swa01519941:24000
Vanson-Hatchet loamy sands, overblown, 65 to 90 percent slopes238995723362f8fwa01519941:24000
Vanson, overblown-Rock outcrop complex, 65 to 90 percent slopes245940723612f97wa01519941:24000
Vanson loamy sand, till substratum, overblown, 5 to 30 percent slopes227805723172f7twa01519941:24000
Vanson sandy loam, 65 to 90 percent slopes231805723262f83wa01519941:24000
Vanson, overblown-Rock outcrop complex, 30 to 65 percent slopes244560723512f8xwa01519941:24000
Vanson cobbly sandy loam, till substratum, 5 to 30 percent slopes234160723322f89wa01519941:24000
Vanson cobbly sandy loam, till substratum, 30 to 65 percent slopes235130723332f8bwa01519941:24000
Vanson-Rock outcrop complex, 65 to 90 percent slopes155215513855251hhrcwa65919871:24000
Vanson loamy sand, overblown, 65 to 90 percent slopes259202313857611hhzzwa65919871:24000
Vanson sandy loam, 65 to 90 percent slopes151177113855211hhr7wa65919871:24000
Vanson loamy sand, overblown, 30 to 65 percent slopes258132913857601hhzywa65919871:24000
Vanson loamy sand, overblown, cold, 30 to 65 percent slopes261120013857631hj01wa65919871:24000
Vanson sandy loam, 30 to 65 percent slopes150113513855201hhr6wa65919871:24000
Vanson sandy loam, 5 to 30 percent slopes14997013855181hhr4wa65919871:24000
Vanson, overblown-Rock outcrop complex, 65 to 90 percent slopes26470413857661hj04wa65919871:24000
Vanson sandy loam, cold, 30 to 65 percent slopes15335113855231hhr9wa65919871:24000
Vanson loamy sand, overblown, cold, 5 to 30 percent slopes26020213857621hj00wa65919871:24000
Vanson, overblown-Rock outcrop complex, 30 to 65 percent slopes2639313857651hj03wa65919871:24000
Vanson extremely cindery loamy sand, overblown, 65 to 90 percent slopes2625513857641hj02wa65919871:24000
Vanson, cold-Rock outcrop complex, 65 to 90 percent slopes1565413855261hhrdwa65919871:24000
Vanson, overblown, cold-Rock outcrop complex, 65 to 90 percent slopes2653913857671hj05wa65919871:24000
Vanson-Rock outcrop complex, 30 to 65 percent slopes1543313855241hhrbwa65919871:24000

Map of Series Extent

Approximate geographic distribution of the VANSON 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 .