Official Series Description


Lab Data Summary

Aggregate lab data for the SPOTTSWOOD soil series. This aggregation is based on all pedons with a current taxon name of SPOTTSWOOD, 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 SPOTTSWOOD 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
102A94P0222S93SD011-023Spottswood7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.3133316,-96.8841629
91AUMN1823S1974MN1451823Spottswood2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3711509,-94.2675705

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SPOTTSWOOD 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 SPOTTSWOOD 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 SPOTTSWOOD 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 SPOTTSWOOD 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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Click the image to view it full size.

Competing Series

Soil series competing with SPOTTSWOOD 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 SPOTTSWOOD 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 SPOTTSWOOD 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 SPOTTSWOOD, 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. SD-2010-11-01-05 | Brookings County - 2004

    Typical pattern of soils and parent material in the Fordtown-Renwash-Allivar and Divide-Lamoure-Marysland associations (Soil Survey of Brookings County, South Dakota; 2004).

Map Units

Map units containing SPOTTSWOOD 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
Spottswood loam3142109396081f94tmn01119901:20000
Spottswood loam314638430287gfr7mn07319941:20000
Spottswood loam, dry, 0 to 2 percent slopesG282A506925753012q4z5nd02119891:20000
Spottswood loam, dry, 0 to 2 percent slopesG282A298625762712q4z5nd0271:12000
Spottswood loam, dry, 0 to 2 percent slopesG282A115325764272q4z5nd03119901:20000
Lankin, terrace-Spottswood, loamy substratum loams, 0 to 2 percent slopesG501A208925770922q5p2nd04519661:20000
Spottswood loam, dry, 0 to 2 percent slopesG282A37525770632q4z5nd04519661:20000
Spottswood loam, dry, 0 to 2 percent slopesG282A32825772982q4z5nd0631:12000
Lankin, terrace-Spottswood, loamy substratum loams, 0 to 2 percent slopesG501A20625811822q5p2nd07319921:20000
Spottswood loam, dry, 0 to 2 percent slopesG282A222125794822q4z5nd08119591:12000
Spottswood loam, dry, 0 to 2 percent slopesG282A3725819832q4z5nd08319901:20000
Spottswood loamSp5057354600cwzqsd00519761:20000
Spottswood loam, 0 to 2 percent slopes, occasionally floodedZ161A272327653002qjn3sd01119951:24000
Fordtown, rarely flooded-Spottswood, ocassionally flooded, loams, 0 to 2 percent slopesZ169A228427652862rkyqsd01119951:24000
Fordtown-Spottswood loams, 0 to 2 percent slopesFc66418759g1rcsd01119951:24000
Spottswood clay loam, clayey, dry, 0 to 2 percent slopesG503A94327977822sd3vsd01319871:20000
Spottswood, dry-Divide loams, 0 to 2 percent slopesG284A62527977512sd2fsd01319871:20000
Spottswood clay loamSw538417790g0r3sd02519921:20000
Spottswood clay loam, 0 to 2 percent slopesG283A32627980142sd2dsd02519921:20000
Spottswood loam, 0 to 2 percent slopes, occasionally floodedZ161A92327130172qjn3sd02920061:12000
Spottswood loam, west, 0 to 2 percent slopesC812A140027985882shzcsd04519731:20000
Spottswood loamSp20354281cwnfsd04519731:20000
Spottswood loam, 0 to 2 percent slopes, occasionally floodedZ161A33727128732qjn3sd05119771:20000
Spottswood loam, 0 to 2 percent slopes, occasionally floodedZ161A80427653772qjn3sd05719921:20000
Spottswood loamSp18417314g07rsd05719921:20000
Spottswood loam, 0 to 2 percent slopes, occasionally floodedZ161A5527127852qjn3sd10919771:20000

Map of Series Extent

Approximate geographic distribution of the SPOTTSWOOD 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 .