Official Series Description


Lab Data Summary

Aggregate lab data for the ASSUMPTION soil series. This aggregation is based on all pedons with a current taxon name of ASSUMPTION, 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 ASSUMPTION 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
108B88P00811987IL109065Assumption7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5091628,-90.8477974
108B12N7648S2011IL021281Assumption4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.6609601,-89.2850644

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ASSUMPTION 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 ASSUMPTION 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 ASSUMPTION 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 ASSUMPTION 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 ASSUMPTION 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 ASSUMPTION 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 ASSUMPTION 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 mountains figure.

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Click the image to view it full size.

Soil series sharing subgroup-level classification with ASSUMPTION, 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-2010-09-01-53 | McDonough County - 1997

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

  2. IL-2011-08-03-09 | Christian County - 1994

    Typical pattern of soils and parent material in the Ipava-Sable-Tama association (Soil Survey of Christian County, Illinois; 1994).

  3. IL-2011-08-04-26 | Henry County - 1984

    Pattern of soils in the Sawmill-Radford association (Soil Survey of Henry County, Illinois; 1984).

  4. IL-2011-08-04-41 | Knox County - 1986

    Typical pattern of soils and parent material in the Tama-Ipava association (Soil Survey of Knox County, Illinois; 1986).

  5. IL-2011-08-04-70 | Mercer County - 1991

    Typical pattern of soils and parent material in the Marseilles-Assumption-Tama association (Soil Survey of Mercer County, Illinois; 1991).

Map Units

Map units containing ASSUMPTION 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
Assumption silty clay loam, 10 to 18 percent slopes, severely eroded259D387618627282rmnhil01120071:12000
Assumption silt loam, 5 to 10 percent slopes, eroded259C235012616972rmndil02119991:12000
Assumption silt loam, 5 to 10 percent slopes, eroded259C25126156482rmndil05719971:12000
Assumption silt loam, 5 to 10 percent slopes, eroded259C2252117632rmndil06119681:15840
Assumption silt loam, 5 to 10 percent slopes, eroded259C251051751662rmndil06719931:15840
Assumption silt loam, 5 to 10 percent slopes, eroded259C239514810662rmndil07120051:12000
Assumption silt loam, 2 to 5 percent slopes259B27642446762rmnbil07320011:12000
Assumption silt loam, 5 to 10 percent slopes, eroded259C222912446772rmndil07320011:12000
Assumption silt loam, 10 to 18 percent slopes, eroded259D213212446782rmngil07320011:12000
Assumption silt loam, 5 to 10 percent slopes, eroded259C26157284902rmndil08320021:12000
Assumption silt loam, 5 to 10 percent slopes, eroded259C240696808772rmndil09520021:12000
Assumption silt loam, 10 to 18 percent slopes, eroded259D229406808782rmngil09520021:12000
Assumption silty clay loam, 10 to 18 percent slopes, severely eroded259D39806808792rmnhil09520021:12000
Assumption silt loam, 5 to 10 percent slopes, eroded259C23899268812rmndil10320041:12000
Assumption silt loam, 5 to 10 percent slopes, eroded259C217646341962rmndil10920021:12000
Assumption silt loam, 10 to 18 percent slopes, eroded259D22896341972rmngil10920021:12000
Assumption silt loam, 5 to 10 percent slopes, eroded259C225721991862rmndil11719991:12000
Assumption silt loam, 2 to 5 percent slopes259B20481991842rmnbil11719991:12000
Assumption silt loam, 2 to 5 percent slopes, eroded259B214961991852rmncil11719991:12000
Assumption silt loam, 5 to 10 percent slopes, eroded259C215632449712rmndil13120001:12000
Assumption silt loam, 10 to 18 percent slopes, eroded259D27022449722rmngil13120001:12000
Assumption silt loam, 5 to 10 percent slopes, eroded259C2161017213972rmndil13520071:12000
Assumption silt loam, 5 to 10 percent slopes, eroded259C2312916721332rmndil13719841:15840
Assumption silt loam, 10 to 18 percent slopes, eroded259D2117316721342rmngil13719841:15840
Assumption silt loam, 2 to 5 percent slopes259B106242085782rmnbil14120051:12000
Assumption silt loam, 5 to 10 percent slopes, eroded259C241032085792rmndil14120051:12000
Assumption silt loam, 0 to 2 percent slopes259A13702085512ww9ril14120051:12000
Assumption silt loam, 5 to 10 percent slopes, eroded259C26272089752rmndil14319861:15840
Assumption silt loam, 10 to 18 percent slopes, eroded259D23252089762rmngil14319861:15840
Assumption silt loam, 5 to 10 percent slopes, eroded259C261941993142rmndil16719991:12000
Assumption silt loam, 10 to 18 percent slopes, eroded259D257971993152rmngil16719991:12000
Assumption silt loam, 10 to 18 percent slopes, eroded259D28325420732rmngil17119841:12000
Assumption silt loam, 10 to 18 percent slopes, eroded259D29341790812rmngil17519921:15840
Assumption silt loam, 5 to 10 percent slopes, eroded259C25771790802rmndil17519921:15840
Assumption silty clay loam, 10 to 18 percent slopes, severely eroded259D34201790822rmnhil17519921:15840
Assumption silt loam, 5 to 10 percent slopes, eroded259C2110015920732rmndil17720061:12000
Assumption silt loam, 10 to 18 percent slopes, eroded259D248092448802rmngil18720021:12000
Assumption silt loam, 5 to 10 percent slopes, eroded259C227952448792rmndil18720021:12000
Assumption silt loam, 2 to 5 percent slopes, eroded259B210341739982rmncil20119971:12000
Assumption silt loam, 5 to 10 percent slopes, eroded259C21231739992rmndil20119971:12000

Map of Series Extent

Approximate geographic distribution of the ASSUMPTION 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 .