Official Series Description


Lab Data Summary

Aggregate lab data for the SWYGERT soil series. This aggregation is based on all pedons with a current taxon name of SWYGERT, 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 SWYGERT 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
11053IL0530011953IL053001Swygert5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7164358,-88.2267222
110BE80451980IN007045Swygert3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6712722,-87.5277167
110BE80461980IN007046Swygert3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6785722,-87.5097583
11081IL0530041981IL053004Swygert1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4130002,-87.9630633
11081IL0530071981IL053007Swygert1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6393394,-88.1923376
11086IL1050471986IL105047Swygert2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.0888889,-88.6805556
11040A278777IL105001aSWYGERT7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.84669,-88.4097644
11080IL10500280IL-105-002Swygert1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7510993,-88.2581204
11081IL05300281IL-053-002Swygert1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.412953,-87.9686496
11089IL10500589IL-105-005Swygert2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7836806,-88.4491722
11089IL10500689IL-105-006Swygert2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7887389,-88.3956889
11089IL10500789IL-105-007Swygert2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8172861,-88.3948889
11089IL10500889IL-105-008Swygert2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7943417,-88.4108111
11040A2786S1977IL075005Swygert7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6433601,-87.8830795
9878IL0750051978IL075005Swygert1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.935117,-87.6228439
9878IL0750061978IL075006Swygert1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.9359837,-87.6172798
n/a40A2776S1948IL197003Swygert4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SWYGERT 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 SWYGERT 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 SWYGERT 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 SWYGERT 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.

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Competing Series

Soil series competing with SWYGERT 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 SWYGERT 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 SWYGERT 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 SWYGERT, 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-2010-09-01-37 | Livingston County - 1996

    Typical pattern of soils and parent material in the Bryce-Swygert association (Soil Survey of Livingston County, Illinois; 1996).

  2. IL-2011-08-04-10 | Ford County - 1990

    Typical pattern of soils and parent material in the Bryce-Swygert association (Soil Survey of Ford County, Illinois; 1990).

  3. IL-2011-08-04-50 | Livingston County - 1996

    Typical pattern of soils and parent material in the Bryce-Swygert association (Soil Survey of Livingston County, Illinois; 1996).

  4. IN-2012-01-19-03 | Benton County - 1989

    Pattern of soils and parent material in the Bryce-Swygert association (Soil Survey of Benton County, Indiana; 1989).

Map Units

Map units containing SWYGERT 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
Swygert silty clay loam, 2 to 4 percent slopes, eroded91B227902430092st2lil01919991:12000
Swygert silty clay loam, 4 to 6 percent slopes, eroded91C24112429542t6zqil01919991:12000
Swygert silty clay loam, 0 to 2 percent slopes91A732430282t6znil01919991:12000
Swygert silty clay loam, 0 to 2 percent slopes91A84521087042t6znil03120081:12000
Swygert silty clay loam, 2 to 4 percent slopes91B48223884452x88bil03120081:12000
Swygert silty clay loam, 0 to 2 percent slopes91A661834632t6znil04319981:12000
Swygert silty clay loam, 0 to 2 percent slopes91A156391982852t6znil05320011:12000
Swygert silty clay loam, 2 to 4 percent slopes, eroded91B290601982872st2lil05320011:12000
Swygert silty clay loam, 0 to 2 percent slopes91A40368687602t6znil06320051:12000
Swygert silty clay loam, 2 to 4 percent slopes91B161414158882x88bil06320051:12000
Swygert silty clay loam, 4 to 6 percent slopes, eroded91C220715409082t6zqil06320051:12000
Swygert silty clay loam, 2 to 4 percent slopes, eroded91B220115409072st2lil06320051:12000
Swygert silty clay loam, 0 to 2 percent slopes91A188941756042t6znil07519801:15840
Swygert silty clay loam, 2 to 4 percent slopes91B51611756052x88bil07519801:15840
Swygert silty clay loam, 2 to 4 percent slopes, eroded91B24926488762st2lil07519801:15840
Swygert silty clay loam, 0 to 2 percent slopes91A7059684422t6znil09120031:12000
Swygert silty clay loam, 2 to 4 percent slopes, eroded91B23569684442st2lil09120031:12000
Swygert silty clay loam, 0 to 2 percent slopes91A72266387262t6znil09320071:12000
Swygert silty clay loam, 2 to 4 percent slopes91B12776387272x88bil09320071:12000
Swygert silty clay loam, 4 to 6 percent slopes, eroded91C236517106382t6zqil09320071:12000
Swygert silty clay loam, 2 to 4 percent slopes, eroded91B24717156222st2lil09320071:12000
Swygert silty clay loam, 2 to 4 percent slopes91B1368014156412x88bil09920061:12000
Swygert silty clay loam, 4 to 6 percent slopes, eroded91C2581010301122t6zqil09920061:12000
Swygert silty clay loam, 2 to 4 percent slopes, eroded91B2305210301112st2lil09920061:12000
Swygert silty clay loam, 0 to 2 percent slopes91A177510301102t6znil09920061:12000
Swygert silty clay loam, 4 to 6 percent slopes, severely eroded91C3158314156422xclhil09920061:12000
Swygert silty clay loam, 2 to 4 percent slopes, eroded91B2282931770082st2lil10519911:15840
Swygert silty clay loam, 0 to 2 percent slopes91A265731770062t6znil10519911:15840
Swygert silty clay loam, 2 to 4 percent slopes91B10761770072x88bil10519911:15840
Swygert silty clay loam, 4 to 6 percent slopes, eroded91C23826488852t6zqil10519911:15840
Swygert silty clay loam, 2 to 4 percent slopes, eroded91B21481990682st2lil11320001:12000
Swygert silty clay loam, 2 to 4 percent slopes, eroded91B24741822582st2lil12319971:15840
Swygert silty clay loam, 0 to 2 percent slopes91A664116010142t6znil18320061:12000
Swygert silty clay loam, 2 to 4 percent slopes, eroded91B2334816011122st2lil18320061:12000
Swygert silty clay loam, 4 to 6 percent slopes, eroded91C217516011132t6zqil18320061:12000
Swygert silty clay loam, 2 to 4 percent slopes, eroded91B26196342792st2lil19720021:12000
Swygert silty clay loam, 4 to 6 percent slopes, eroded91C24126176092t6zqil19720021:12000
Swygert silty clay loam, 0 to 2 percent slopes91A86176072t6znil19720021:12000
Swygert silty clay loam, 2 to 4 percent slopes, eroded91B2213222179632st2lil20320081:12000
Swygert silty clay loam, 0 to 2 percent slopes91A16878692572t6znil20320081:12000
Swygert silty clay loam, 0 to 2 percent slopesSxA10891646382t6znin00719851:15840
Swygert silty clay loam, 2 to 6 percent slopes, erodedSxB26321646395j9yin00719851:15840
Swygert silty clay loam, 0 to 2 percent slopesSyA11931637772t6znin11119901:15840
Swygert variant-Simonin complex, 2 to 6 percent slopes, erodedSzB28011637825hf9in11119901:15840
Swygert variant-Simonin complex, 6 to 15 percent slopes, erodedSzC21061637835hfbin11119901:15840

Map of Series Extent

Approximate geographic distribution of the SWYGERT 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 .