Official Series Description


Lab Data Summary

Aggregate lab data for the VICKING soil series. This aggregation is based on all pedons with a current taxon name of VICKING, 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 VICKING 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
1191P003790ID023005Vicking4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.5263901,-113.3105545

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the VICKING 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 VICKING 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 VICKING 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 VICKING 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 VICKING 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 VICKING 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 VICKING 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 terrace figure.

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

Soil series sharing subgroup-level classification with VICKING, 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. UT-2012-03-22-02 | Box Elder County, Western Part - September 1997

    Relationship of soils and parent material in the Dahar-Bullump-Raftriver general soil map unit (Soil Survey of Box Elder County Utah, Western Part; 1997).

Map Units

Map units containing VICKING 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
Vicking-Cokeville complex, 15 to 35 percent slopes219441415276811n8p1id71220081:24000
Vicking silt loam, dry, 2 to 12 percent slopes2171518791741vkw1id71220081:24000
Ireland-Falula-Vicking complex, 15 to 40 percent slopes112713778206v3sfid71220081:24000
Vicking silt loam, dry, 12 to 20 percent slopes218610791744vkw4id71220081:24000
Vicking silt loam, 12 to 20 percent slopes21659515437455mtid71220081:24000
Vicking silt loam, 4 to 12 percent slopes21545715437555mvid71220081:24000
Vicking silt loam, 1 to 4 percent slopes21422815437355msid71220081:24000
Vicking-Clegg-Horrocks complex, 5 to 30 percent slopes2010218129897332x3mwid7161:24000
Vicking-Cedarhill complex, 10 to 35 percent slopesKCG570600002n4bxid7161:24000
Vicking silt loam, 1 to 4 percent slopes885A4581592625bqhid7161:24000
Vicking silt loam, 4 to 12 percent slopes885C1261592645bqkid7161:24000
Vicking silt loam, cool, 1 to 4 percent slopes885AA5023707152kkxpid7161:24000
Vicking silt loam, 12 to 20 percent slopes885B381592635bqjid7161:24000
Vicking-Clegg-Horrocks complex, 5 to 30 percent slopes201015332389872x3mwid77019681:24000
Vicking-Ramshorn family association, 3 to 25 percent slopes9810552481312j4v6ut60119851:24000
Vicking-Raftriver-Codquin complex, 2 to 60 percent slopes973469481311j4v5ut60119851:24000
Vicking silt loam, 3 to 8 percent slopes961038481310j4v4ut60119851:24000
Vicking silt loam, dry, 4 to 15 percent slopesVCD1030503921jxcjut60419801:24000
Vicking-Krueger association, 2 to 15 percent slopes2134380483623j77rut6281:24000
Demner, dry-Vicking complex, 2 to 25 percent slopes1213646483465j72nut6281:24000
Vicking-Carshal family complex, 4 to 65 percent slopesNWM143225199412qjtvut6291:24000
Vicking-Krueger association, 2 to 15 percent slopes21361925105892syg3ut6291:24000
Vicking loam, 4 to 15 percent slopesVMD141522307022dw74ut6511:24000
Vicking very stony loam, 15 ro 40 percent slopes, stonyVOF77422307042dw76ut6511:24000
Vicking cobbly clay loam, 8 to 25 percent slopesVNE213422307032dw75ut6511:24000
Vicking family-Hondoho-Araveton complex, 4 to 15 percent slopes3709340649831fxnwy7231:24000
Cokeville-Vicking-Leefel complex, 4 to 15 percent slopes355530833722y0y0wy7231:24000
Drage-Vicking complex, 2 to 15 percent slopes375029253142xyfvwy7231:24000
Vicking-Bancroft complex, 2 to 15 percent slopes355429253052xyfswy7231:24000

Map of Series Extent

Approximate geographic distribution of the VICKING 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 .