Official Series Description


Lab Data Summary

Aggregate lab data for the SWANWICK soil series. This aggregation is based on all pedons with a current taxon name of SWANWICK, 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 SWANWICK 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
114B80IL1450251980IL145025Swanwick1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.9748568,-89.5495267
114B11N0116S2010IL157001Swanwick5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.149975,-89.7329861
114B11N0119S2010IL157004Swanwick7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1569778,-89.7368222
115C78IL0950361978IL095036Swanwick4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.0392787,-90.0398548
115C78IL0950371978IL095037Swanwick4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.0258039,-90.0367936
115C78IL0950401978IL095040Swanwick4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.9973735,-90.1586087
120A11N036709KY183021Swanwick6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4211139,-86.9126722

Water Balance

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

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 SWANWICK 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 SWANWICK 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 SWANWICK 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 SWANWICK, 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. IL-2010-09-01-55 | McDonough County - 1997

    Typical pattern of soils and parent material in the Rapatee-Swanwick association (Soil Survey of McDonough County, Illinois; 1997).

Map Units

Map units containing SWANWICK 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
Swanwick silt loam, 2 to 5 percent slopes824B53326041972rbdyil00919841:12000
Swanwick silt loam, 1 to 5 percent slopes824B127326750372rtn3il05919661:20000
Swanwick silt loam, 5 to 10 percent slopes824C98026750382rtn4il05919661:20000
Swanwick silt loam, 1 to 5 percent slopes824B225015408751nqdnil07720061:12000
Swanwick silt loam, 5 to 10 percent slopes824C97415408761nqdpil07720061:12000
Swanwick silt loam, 2 to 5 percent slopes824B1575634237p8z8il10920021:12000
Swanwick silt loam, 1 to 5 percent slopes824B891614059531j60bil14520051:12000
Swanwick silt loam, 5 to 10 percent slopes824C22562005156qn7il15720011:12000
Swanwick silt loam, 1 to 5 percent slopes824B8772005146qn6il15720011:12000
Swanwick silty clay loam, 1 to 5 percent slopes824B46218314064kril16319971:12000
Swanwick silt loam, 5 to 10 percent slopes824C125927961451t20gil16519741:15840
Swanwick silt loam, 1 to 5 percent slopes824B84526750492rtnhil16519741:15840
Swanwick silt loam, 2 to 5 percent slopes824B15112021136s9sil16920001:12000
Swanwick silt loam, 1 to 5 percent slopes824B119828576941t20dil18519621:20000
Swanwick silt loam, 1 to 5 percent slopes824B139916702301t20dil19920071:12000
Swanwick silt loam, 5 to 10 percent slopes824C51016702321t20gil19920071:12000
Swanwick variant silt loam, 1 to 15 percent slopesSvC140631601595cnfin05119861:15840
Swanwick silt loam, 0 to 6 percent slopesuSwaB285632525052nb75ky10119641:15840
Swanwick silt loam, 6 to 12 percent slopesuSwaC14332525062zs4tky10119641:15840
Swanwick silt loam, 0 to 6 percent slopesuSwaB26031753762nb75ky10719741:12000
Swanwick silt loam, 0 to 6 percent slopesuSwaB46929730292nb75ky18319831:20000
Swanwick silt loam, 0 to 6 percent slopesuSwaB60429730222nb75ky61519711:20000
Swanwick silt loam, 0 to 6 percent slopesuSwaB9030372742nb75ky63119761:20000
Swanwick silt loam, 0 to 6 percent slopesuSwaB23134286512nb75ky63519781:20000

Map of Series Extent

Approximate geographic distribution of the SWANWICK 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 .