Official Series Description


Lab Data Summary

Aggregate lab data for the TYGART soil series. This aggregation is based on all pedons with a current taxon name of TYGART, 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 TYGART 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
14788PA0550681988PA055068Tygart5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.2236111,-77.6966667
n/aSK-0281965-OH151-028Tygart4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a40A4908S1954KY101016Tygart4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a40A4909S1954KY101017Tygart4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TYGART 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 TYGART 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 TYGART 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 TYGART 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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Competing Series

Soil series competing with TYGART 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 TYGART 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 TYGART 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.

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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with TYGART, 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. PA-2012-03-13-38 | Indiana County - January 1968

    Parent material, position, and pattern of soils in the Monongahela-Allegheny-Pope-Philo association (Soil Survey of Indiana County, PA; 1968).

  2. VA-2010-11-05-29 | Rockbridge County -

    Generalized diagram of a sequence of landforms along a river system underlain by shale bedrock in the western part of Rockbridge County. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to parent material and landform position (Soil Survey of Rockbridge County, Virginia).

Map Units

Map units containing TYGART 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
Tygart silt loam, 0 to 3 percent slopesTrA305536049kzsxoh07919811:15840
Tygart silt loam, 2 to 7 percent slopes59B761519134kf68va02319901:20000
Tygart silt loam, 0 to 3 percent slopes48A934517284kc8lva13919951:20000
Tygart-Purdy complex, 0 to 3 percent slopes69A50725148762qdd7va16320101:24000
Tygart silt loam, 0 to 5 percent slopes188225252342qm10va6061:24000
Tygart silt loam, 3 to 8 percent slopesTyB967516285kb7cwv00319971:24000
Tygart silt loam, 0 to 3 percent slopesTyA624516284kb7bwv00319971:24000
Tygart silt loam, 0 to 3 percent slopesTyA394555687ln7dwv06520031:24000
Tygart silt loam, 3 to 8 percent slopesTyB342514219k82qwv07119881:20000
Tygart silt loamTg611515497k9dywv09719811:20000
Tygart silt loamTy899514639k8j8wv60119661:15840
Tygart silt loamTg1748515605k9jfwv60319781:20000
Tygart variant silt loamTv1532515606k9jgwv60319781:20000
Tygart silt loamTg4099555983lnjywv60819731:20000
Tygart silt loamTg456515828k9rmwv61019731:20000
Tygart variant cobbly silt loam, 3 to 8 percent slopesTvB1248515968k9x4wv62819801:20000
Tygart silt loam, 0 to 3 percent slopesTgA713515966k9x2wv62819801:20000
Tygart silt loam, 3 to 8 percent slopesTgB507515967k9x3wv62819801:20000
Tygart silt loam, 0 to 3 percent slopesTvA6452516665261qjwv7131:24000

Map of Series Extent

Approximate geographic distribution of the TYGART 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 .