Official Series Description


Lab Data Summary

Aggregate lab data for the SPEARVILLE soil series. This aggregation is based on all pedons with a current taxon name of SPEARVILLE, 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 SPEARVILLE 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
7208N034708KS067003Spearville8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.7141528,-101.416975
7340A186263KS057001Spearville6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8675003,-100.1366653
7391P080591KS069004Spearville6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6063881,-100.4775009
7340A5193S1963KS057002Spearville7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8825378,-100.1173553

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SPEARVILLE 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 SPEARVILLE 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 SPEARVILLE 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 SPEARVILLE 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 SPEARVILLE 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 SPEARVILLE 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 SPEARVILLE 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 SPEARVILLE, 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. KS-2012-01-23-05 | Ford County - August 1965

    A geologic cross section west of Dodge City showing the major soil associations in Ford County (Soil Survey of Ford County, Kansas; 1965).

  2. KS-2012-01-23-17 | Gray County - January 1968

    Soils of the Spearville-Richfield soil association (Soil Survey of Gray County, Kansas; 1968).

  3. KS-2012-01-23-20 | Gray County - January 1968

    Approximate geologic cross section through the central part of Gray County and the general location of soils on the landscape (Soil Survey of Gray County, Kansas; 1968).

  4. KS-2012-01-23-32 | Haskell County - October 1968

    Landscape showing soils of the Richfield-Spearville-Ulysses association in the southeastern part of the county (Soil Survey of Haskell County, Kansas; 1968).

Map Units

Map units containing SPEARVILLE 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
Richfield-Spearville complex, 0 to 1 percent slopes17683105511523422tv5vks05519621:24000
Spearville silty clay loam, 0 to 1 percent slopes28012467211523482twl8ks05519621:24000
Spearville complex, 1 to 3 percent slopes, eroded2800237211523472yl40ks05519621:24000
Spearville silty clay loam, 0 to 1 percent slopes28011453413804702twl8ks05719621:24000
Spearville complex, 1 to 3 percent slopes, eroded28001256313804692yl40ks05719621:24000
Spearville silty clay loam, 0 to 1 percent slopes280112090213806032twl8ks06919651:24000
Richfield-Spearville complex, 0 to 1 percent slopes17682493713805952tv5vks06919651:24000
Spearville complex, 1 to 3 percent slopes, eroded2800246613806022yl40ks06919651:24000
Spearville silty clay loam, 0 to 1 percent slopes2801915413806352twl8ks08119651:24000
Spearville silty clay loam, 0 to 1 percent slopes28013123211524282twl8ks08319661:24000
Spearville complex, 1 to 3 percent slopes, eroded280053311524272yl40ks08319661:24000
Spearville silty clay loam, 0 to 1 percent slopes28013650413818172twl8ks11919731:24000
Spearville silty clay loam, 0 to 1 percent slopes28012544913826502twl8ks17519631:24000

Map of Series Extent

Approximate geographic distribution of the SPEARVILLE 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 .