Official Series Description


Lab Data Summary

Aggregate lab data for the HOMME soil series. This aggregation is based on all pedons with a current taxon name of HOMME, 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 HOMME were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

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

Click the image to view it full size.

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 HOMME, 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. SD-2012-03-14-05 | Bon Homme County - January 1983

    Pattern of soils and underlying material in the Homme-Ethan-Onita association (Soil Survey of Bon Homme County, SD; 1983).

  2. SD-2012-03-15-57 | Jerauld County - September 1994

    Pattern of soils and parent material in the Homme-Peno association (Soil Survey of Jerauld County, SD; 1994).

Map Units

Map units containing HOMME 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
Homme-Ethan-Onita complex, 1 to 6 percent slopesHnB368114182762yyfxsd00919811:20000
Homme-Ethan-Tetonka complex, 0 to 6 percent slopesHpB23677418277g17tsd00919811:20000
Homme-Onita silty clay loams, 1 to 6 percent slopesHrB148854182802xhdpsd00919811:20000
Ethan-Homme complex, 6 to 9 percent slopesEpC141264182712yyfysd00919811:20000
Homme-Onita silty clay loams, 0 to 2 percent slopesHrA121694182792yyfwsd00919811:20000
Homme-Davison-Tetonka complex, 0 to 3 percent slopesHmA10648418275g17rsd00919811:20000
Homme-Onita-Tetonka complex, 0 to 3 percent slopesHtA5392418281g17ysd00919811:20000
Homme-Ethan-Tetonka complex, 0 to 9 percent slopesHpC3419418278g17vsd00919811:20000
Homme-Ethan-Onita complex, 1 to 6 percent slopesHmB166793550362wkqdsd02319801:20000
Homme-Onita silty clay loams, 1 to 6 percent slopesHoB63863550382xhdpsd02319801:20000
Homme-Onita silty clay loams, 0 to 2 percent slopesHoA54053550372wkqgsd02319801:20000
Ethan-Homme complex, 6 to 9 percent slopesEuC42763550252wkprsd02319801:20000
Homme-Onita silty clay loams, 0 to 2 percent slopesHnA55393549052yyfwsd04319791:20000
Homme-Ethan-Onita complex, 1 to 6 percent slopesHmB11393549042yyfxsd04319791:20000
Homme-Onita silty clay loams, 1 to 6 percent slopesHhB7503549032xhdpsd04319791:20000
Ethan-Homme complex, 6 to 9 percent slopesEwC18531192112yyfysd04319791:20000
Homme-Peno complex, 2 to 6 percent slopesHpB13237356442cyx4sd07319871:20000
Homme-Onita-Raber complex, 0 to 2 percent slopesHlA48083564412yyk2sd07319871:20000
Homme-Peno complex, 6 to 9 percent slopesHpC2551356443cyx5sd07319871:20000
Homme-Ethan-Onita complex, 1 to 6 percent slopesHnB86224180732yyfxsd13519771:20000
Homme-Onita silty clay loams, 1 to 6 percent slopesEchB522130825742xhdpsd13519771:20000
Homme-Onita silty clay loams, 0 to 2 percent slopesHrA454531192072yyfwsd13519771:20000
Homme-Onita silty clay loams, 1 to 6 percent slopesHtB58544179842xhdpsd60219751:20000
Ethan-Homme complex, 6 to 9 percent slopesHoC32324179822yyfysd60219751:20000
Homme-Onita silty clay loams, 0 to 2 percent slopesHtA31554179832yyfwsd60219751:20000
Homme-Ethan-Onita complex, 1 to 6 percent slopesHoB10514179532yyfxsd60219751:20000

Map of Series Extent

Approximate geographic distribution of the HOMME 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 .