Official Series Description


Lab Data Summary

Aggregate lab data for the HETLAND soil series. This aggregation is based on all pedons with a current taxon name of HETLAND, 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 HETLAND 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
102A90P024089SD037015Hetland8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.1527786,-97.4980545
102A90P024889SD077030Hetland7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.3747215,-97.1669464
102A90P0250S89SD077-043Hetland7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.4638901,-97.3722229

Water Balance

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

There are insufficient data to create the 3D terrace figure.

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Competing Series

Soil series competing with HETLAND 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 HETLAND 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 HETLAND 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.

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Soil series sharing subgroup-level classification with HETLAND, 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-2012-03-15-63 | Kingsbury County - November 1997

    Typical pattern of soils and underlying material in the Poinsett-Hetland association (Soil Survey of Kingsbury County, SD; 1997).

Map Units

Map units containing HETLAND 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
Hetland silty clay loam, 2 to 6 percent slopesHeB22494187662t5qxsd01119951:24000
Hetland silty clay loam, 0 to 2 percent slopesHeA15634187652t5qwsd01119951:24000
Hetland silty clay loam, 0 to 2 percent slopesHmA25204177382t5qwsd02519921:20000
Hetland silty clay loam, 2 to 6 percent slopesHmB9044177392t5qxsd02519921:20000
Hetland silty clay loam, 0 to 2 percent slopesJ141A378416843092t5qwsd02920061:12000
Hetland silty clay loam, 2 to 6 percent slopesZ128B58227652622t5qxsd02920061:12000
Hetland-Rusklyn silty clay loams, 2 to 6 percent slopesHuB17954170902t5qysd03719921:20000
Hetland silty clay loam, 0 to 2 percent slopesHtA11964170892t5qwsd03719921:20000
Hetland silty clay loam, 2 to 6 percent slopesZ128B6427129182t5qxsd05119771:20000
Hetland silty clay loam, 0 to 2 percent slopesHeA19394172802t5qwsd05719921:20000
Hetland silty clay loam, 2 to 6 percent slopesHeB16644172812t5qxsd05719921:20000
Hetland silty clay loam, 0 to 2 percent slopesHeA167534174852t5qwsd07719921:20000
Hetland silty clay loam, 2 to 6 percent slopesHeB46214174862t5qxsd07719921:20000

Map of Series Extent

Approximate geographic distribution of the HETLAND 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 .