Official Series Description


Lab Data Summary

Aggregate lab data for the TAUMSAUK soil series. This aggregation is based on all pedons with a current taxon name of TAUMSAUK, 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 TAUMSAUK 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
116AM97613301997MO203030MTaumsauk4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1253611,-91.2344861
116AM98613611998MO203061MTaumsauk4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.0755694,-91.2190944
116AM98613691998MO203069MTaumsauk4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1196611,-91.1735361
116AM98613711998MO203071MTaumsauk4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1191444,-91.1752389
116AM99221201999MO221217Taumsauk4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0013974,-91.0199301
116CM88123041988MO123004MTaumsauk3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4858322,-90.3563919
116CM88123071988MO123007MTaumsauk3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4899712,-90.4294968
116CM98223111998MO223025Taumsauk4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1862335,-90.6593475
116CM98223131998MO223028Taumsauk4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.192749,-90.6635132
116CM00221172000MO221280Taumsauk4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2062889,-90.5253806
116CM00221182000MO221281Taumsauk4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2028389,-90.5199806

Water Balance

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

Click the image to view it full size.

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 TAUMSAUK 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 TAUMSAUK 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 TAUMSAUK 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 TAUMSAUK, 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. MO-2010-09-08-08 | Madison County - 2005

    Typical pattern of soils and parent material in the Irondale-Killarney-Trackler association (Soil Survey of Madison County, Missouri; 2005).

Map Units

Map units containing TAUMSAUK 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
Taumsauk-Irondale-Rock outcrop complex, 15 to 45 percent slopes, extremely stony7700736225012072vxpkmo03519881:24000
Taumsauk-Irondale-Rock outcrop complex, 3 to 15 percent slopes, very stony7701112025012222vxppmo03519881:24000
Taumsauk-Irondale-Rock outcrop complex, 15 to 45 percent slopes, extremely stony77007426225012002vxpkmo09319881:24000
Taumsauk-Irondale-Rock outcrop complex, 3 to 15 percent slopes, very stony7701122025012182vxppmo09319881:24000
Taumsauk-Irondale-Rock outcrop complex, 15 to 45 percent slopes, extremely stony77007349225012012vxpkmo12319991:24000
Taumsauk-Irondale-Rock outcrop complex, 15 to 45 percent slopes, extremely stony77007500125012022vxpkmo17920041:24000
Taumsauk-Irondale-Rock outcrop complex, 3 to 15 percent slopes, very stony77011207425012192vxppmo17920041:24000
Taumsauk-Irondale-Rock outcrop complex, 15 to 45 percent slopes, extremely stony77007108925012032vxpkmo18719791:24000
Taumsauk-Irondale-Rock outcrop complex, 3 to 15 percent slopes, very stony770117925012202vxppmo18719791:24000
Taumsauk-Irondale-Rock outcrop complex, 3 to 15 percent slopes, very stony77011163425012232vxppmo20320041:24000
Taumsauk-Irondale-Rock outcrop complex, 15 to 45 percent slopes, extremely stony77007112725012062vxpkmo20320041:24000
Taumsauk-Irondale-Rock outcrop complex, 15 to 45 percent slopes, extremely stony7700740388862942vxpkmo22120031:24000
Taumsauk-Irondale-Rock outcrop complex, 3 to 15 percent slopes, very stony7701112118862952vxppmo22120031:24000
Rock outcrop-Taumsauk complex, 3 to 35 percent slopes, extremely stony77014150886296yr86mo22120031:24000
Taumsauk-Irondale-Rock outcrop complex, 15 to 45 percent slopes, extremely stony77007116325012042vxpkmo22320041:24000

Map of Series Extent

Approximate geographic distribution of the TAUMSAUK 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 .