Official Series Description


Lab Data Summary

Aggregate lab data for the HERTY soil series. This aggregation is based on all pedons with a current taxon name of HERTY, 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 HERTY 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
133B80P022380TX005009Herty8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.1708336,-94.5791702
133BS81TX005001S81TX005001Herty4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.166378,-94.6690445

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HERTY 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 HERTY 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 HERTY 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 HERTY 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with HERTY 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 HERTY 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 HERTY 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 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 HERTY, 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. TX-2010-11-03-40 | Houston County - 2002

    Typical pattern of soils and parent material on terraces, uplands, and flood plains of the Neches River (Soil Survey of Houston County, Texas; 2002).

  2. TX-2010-11-04-21 | Trinity County - 2003

    Typical pattern of soils and parent material in the Herty-Moswell general soil map unit (Soil Survey of Trinity County, Texas; 2003).

  3. TX-2012-03-19-01 | Angelina County - February 1988

    Typical pattern of soils and underlying material in the Fuller-Keltys map unit (Soil Survey of Angelina County, TX; 1988).

  4. TX-2012-03-19-02 | Angelina County - February 1988

    Typical pattern of soils and underlying material in the Diboll-Keltys map unit (Soil Survey of Angelina County, TX; 1988).

  5. TX-2012-03-19-03 | Angelina County - February 1988

    Typical pattern of soils and underlying material in the Rosenwall map unit (Soil Survey of Angelina County, TX; 1988).

Map Units

Map units containing HERTY 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
Herty very fine sandy loam, 1 to 5 percent slopesHtC172319030322tf4qla08519911:24000
Herty very fine sandy loam, 1 to 5 percent slopesHeB123805752022tf4qtx00519841:24000
Herty very fine sandy loam, 0 to 1 percent slopesHeA1072575201m9jwtx00519841:24000
Herty-Urban land complex, 1 to 5 percent slopesHuB52575203m9jytx00519841:24000
Herty loam, 1 to 3 percent slopesHeB293565755142tf40tx22519941:24000
Herty loam, 0 to 1 percent slopesHeA16135755132s32ctx22519941:24000
Herty loam, 1 to 3 percent slopesHeB117385770842tf40tx45519991:24000
Herty loam, 0 to 1 percent slopesHeA14885770832s32ctx45519991:24000
Herty silt loam, 1 to 3 percent slopesHrB3194576194mbkxtx61719831:24000
Herty loam, 1 to 3 percent slopesHeB377718947852tf40tx61920071:24000

Map of Series Extent

Approximate geographic distribution of the HERTY 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 .