Official Series Description


Lab Data Summary

Aggregate lab data for the ELEVASIL soil series. This aggregation is based on all pedons with a current taxon name of ELEVASIL, 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 ELEVASIL 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
10588P0181S1987WI053003Elevasil5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.4130554,-90.9316635
10501P0208S2000WI063022Elevasil5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.9892159,-90.9516449
10501P0209S2000WI063023Elevasil5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.9925652,-90.9574966

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ELEVASIL 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 ELEVASIL 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 ELEVASIL 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 ELEVASIL 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 ELEVASIL 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 ELEVASIL series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the ELEVASIL 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.

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 ELEVASIL, 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. WI-2012-03-23-04 | Jackson County - 2001

    Relationship of soils, topography, and parent material in the Seaton-Council association (Soil Survey of Jackson County, WI; 2001).

  2. WI-2012-03-23-07 | Jackson County - 2001

    Relationship of soils, topography, and parent material in the Bilson-Elevasil-Merit association (Soil Survey of Jackson County, WI; 2001).

Map Units

Map units containing ELEVASIL 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
Elevasil sandy loam, 6 to 12 percent slopes, moderately eroded224C2426625617532yt3cwi01119601:20000
Elevasil sandy loam, 20 to 30 percent slopes, moderately eroded224E2302925617552yt3fwi01119601:20000
Elevasil sandy loam, 12 to 20 percent slopes, moderately eroded224D2298325617542yt3dwi01119601:20000
Boone-Elevasil complex, 15 to 45 percent slopes, rocky1224F199125617562yt3hwi01119601:20000
Elevasil sandy loam, 2 to 6 percent slopes224B158025617522yt3bwi01119601:20000
Elevasil sandy loam, 6 to 12 percent slopes, moderately erodedElC250654215152yt3cwi01719851:15840
Elevasil sandy loam, 2 to 6 percent slopesElB37594215142yt3bwi01719851:15840
Elevasil sandy loam, 12 to 20 percent slopes, moderately erodedElD29784215162yt3dwi01719851:15840
Boone-Elevasil complex, 15 to 45 percent slopes, rockyBpF11794318452yt3hwi01919941:20000
Elevasil sandy loam, 6 to 12 percent slopes, moderately erodedElC26574318572yt3cwi01919941:20000
Elevasil sandy loam, 2 to 6 percent slopesElB3654318562yt3bwi01919941:20000
Elevasil sandy loam, 12 to 20 percent slopes, moderately erodedElD22484318582yt3dwi01919941:20000
Elevasil sandy loam, 20 to 30 percent slopes, moderately eroded224E2217625039422yt3fwi02319601:12000
Elevasil sandy loam, 12 to 20 percent slopes, moderately eroded224D2130224981942yt3dwi02319601:12000
Boone-Elevasil complex, 15 to 45 percent slopes, rocky1224F47024991672yt3hwi02319601:12000
Elevasil sandy loam, 20 to 30 percent slopes, very stony231E24325039482lb3pwi02319601:12000
Elevasil sandy loam, 6 to 12 percent slopes, moderately eroded224C211424981462yt3cwi02319601:12000
Elevasil sandy loam, 12 to 20 percent slopes, very stony231D7225039452lb3nwi02319601:12000
Elevasil sandy loam, 2 to 6 percent slopes224B1324981392yt3bwi02319601:12000
Hayriver and Elevasil fine sandy loams, 6 to 12 percent slopes, moderately eroded275C289012518509n56pwi03320031:15840
Hayriver and Elevasil fine sandy loams, 12 to 20 percent slopes, moderately eroded275D288962518510n56rwi03320031:15840
Elevasil sandy loam, 6 to 12 percent slopes, moderately eroded224C2624524981472yt3cwi03320031:15840
Elevasil sandy loam, 2 to 6 percent slopes224B491124981402yt3bwi03320031:15840
Hayriver and Elevasil fine sandy loams, 2 to 6 percent slopes, moderately eroded275B237472518508n56mwi03320031:15840
Elevasil sandy loam, 12 to 20 percent slopes, moderately eroded224D2106224981952yt3dwi03320031:15840
Boone-Elevasil complex, 15 to 45 percent slopes, rocky1224F60824991682yt3hwi03320031:15840
Elevasil sandy loam, 20 to 30 percent slopes, moderately eroded224E222125039432yt3fwi03320031:15840
Elevasil sandy loam, 6 to 12 percent slopes, moderately eroded224C2601230997322yt3cwi03519741:15840
Elevasil sandy loam, 2 to 6 percent slopes224B475430997312yt3bwi03519741:15840
Elevasil sandy loam, 12 to 20 percent slopes, moderately eroded224D2320630997332yt3dwi03519741:15840
Boone-Elevasil complex, 15 to 45 percent slopes, rocky1224F40330996652yt3hwi03519741:15840
Elevasil sandy loam, 20 to 30 percent slopes, moderately eroded224E21930997362yt3fwi03519741:15840
Elevasil sandy loam, 20 to 30 percent slopes, very stony231E43327748072lb3pwi04919601:20000
Elevasil sandy loam, 12 to 20 percent slopes, very stony231D19027748062lb3nwi04919601:20000
Boone-Elevasil complex, 15 to 45 percent slopes, rocky1224F3086924991702yt3hwi05319941:20000
Council-Elevasil-Norden complex, 20 to 45 percent slopes, rocky1743F2428325013752yt3gwi05319941:20000
Bilson-Elevasil sandy loams, 6 to 12 percent slopes, eroded1234C2774324991762fj6nwi05319941:20000
Elevasil sandy loam, 6 to 12 percent slopes, moderately eroded224C2426124981482yt3cwi05319941:20000
Elevasil sandy loam, 2 to 6 percent slopes224B416224981412yt3bwi05319941:20000
Elevasil sandy loam, 12 to 20 percent slopes, moderately eroded224D2344524981962yt3dwi05319941:20000
Bilson-Elevasil sandy loams, 12 to 20 percent slopes, eroded1234D2131024991772fj6pwi05319941:20000
Council-Elevasil-Norden complex, 20 to 45 percent slopes, rocky1743F2126525614862yt3gwi05719871:15840
Elevasil sandy loam, 2 to 6 percent slopes224B157125615212yt3bwi05719871:15840
Elevasil sandy loam, 6 to 12 percent slopes, moderately eroded224C296825615222yt3cwi05719871:15840
Elevasil sandy loam, 12 to 20 percent slopes, moderately eroded224D281925615232yt3dwi05719871:15840
Boone-Elevasil complex, 15 to 45 percent slopes, rocky1224F70125614552yt3hwi05719871:15840
Council-Elevasil-Norden complex, 20 to 45 percent slopes, rocky1743F1991325013762yt3gwi06320011:12000
Elevasil sandy loam, 12 to 20 percent slopes, moderately eroded224D213524981972yt3dwi06320011:12000
Elevasil sandy loam, 6 to 12 percent slopes, moderately eroded224C211224981492yt3cwi06320011:12000
Elevasil sandy loam, 2 to 6 percent slopes224B8924981422yt3bwi06320011:12000
Council-Elevasil-Norden complex, 20 to 45 percent slopes, rocky1743F2932226850322yt3gwi08119811:15840
Boone-Elevasil complex, 15 to 45 percent slopes, rocky1224F1117926850512yt3hwi08119811:15840
Elevasil sandy loam, 20 to 30 percent slopes, moderately eroded224E2777226850772yt3fwi08119811:15840
Elevasil sandy loam, 12 to 20 percent slopes, moderately eroded224D2204826850762yt3dwi08119811:15840
Elevasil sandy loam, 6 to 12 percent slopes, moderately eroded224C2134626850752yt3cwi08119811:15840
Bilson-Elevasil sandy loams, 6 to 12 percent slopes, eroded1234C2426851432fj6nwi08119811:15840
Boone-Elevasil complex, 15 to 45 percent slopes, rocky1224F35124991692yt3hwi09119981:12000
Elevasil sandy loam, 6 to 12 percent slopes, moderately eroded224C26824981512yt3cwi09119981:12000
Elevasil sandy loam, 2 to 6 percent slopes224B6824981442yt3bwi09119981:12000
Elevasil sandy loam, 12 to 20 percent slopes, moderately eroded224D26224981992yt3dwi09119981:12000
Elevasil fine sandy loam, till plain, 6 to 12 percent slopes, moderately eroded220C2330216974041tz8zwi09320061:12000
Elevasil fine sandy loam, till plain, 12 to 20 percent slopes, moderately eroded220D2131516974031tz8ywi09320061:12000
Council-Elevasil-Norden complex, 20 to 45 percent slopes, rocky1743F186625013772yt3gwi10320021:12000
Elevasil sandy loam, 12 to 20 percent slopes, very stony231D55925039462lb3nwi10320021:12000
Council-Elevasil-Norden complex, 20 to 45 percent slopes, rocky1743F697932578252yt3gwi11119771:15840
Elevasil sandy loam, 20 to 30 percent slopes, moderately erodedElE48104231452yt3fwi11119771:15840
Elevasil sandy loam, 2 to 6 percent slopesElB43194231422yt3bwi11119771:15840
Elevasil sandy loam, 12 to 20 percent slopes, moderately erodedElD236334231442yt3dwi11119771:15840
Elevasil sandy loam, 6 to 12 percent slopes, moderately erodedElC233014231432yt3cwi11119771:15840
Boone-Elevasil complex, 15 to 45 percent slopes, rocky1224F122132578232yt3hwi11119771:15840
Boone-Elevasil complex, 15 to 45 percent slopes, rocky1224F6184426394912yt3hwi12119691:15840
Elevasil sandy loam, 12 to 20 percent slopes, moderately eroded224D2788926834642yt3dwi12119691:15840
Elevasil sandy loam, 6 to 12 percent slopes, moderately eroded224C2538326834632yt3cwi12119691:15840
Elevasil sandy loam, 20 to 30 percent slopes, moderately eroded224E2432226834652yt3fwi12119691:15840
Elevasil sandy loam, 2 to 6 percent slopes224B161026834622yt3bwi12119691:15840
Council-Elevasil-Norden complex, 20 to 45 percent slopes, rocky1743F64126394952yt3gwi12119691:15840
Bilson-Elevasil sandy loams, 6 to 12 percent slopes, eroded1234C22326835032fj6nwi12119691:15840
Council-Elevasil-Norden complex, 20 to 45 percent slopes, rocky1743F299925013782yt3gwi12319651:12000
Elevasil sandy loam, 12 to 20 percent slopes, very stony231D80625039472lb3nwi12319651:12000
Elevasil sandy loam, 20 to 30 percent slopes, moderately eroded224E262025039442yt3fwi12319651:12000
Elevasil sandy loam, 12 to 20 percent slopes, moderately eroded224D230424982002yt3dwi12319651:12000
Elevasil sandy loam, 6 to 12 percent slopes, moderately eroded224C27124981522yt3cwi12319651:12000

Map of Series Extent

Approximate geographic distribution of the ELEVASIL 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 .