Official Series Description


Lab Data Summary

Aggregate lab data for the HARGREAVE soil series. This aggregation is based on all pedons with a current taxon name of HARGREAVE, 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 HARGREAVE 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 HARGREAVE 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 HARGREAVE 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 HARGREAVE 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 HARGREAVE 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 HARGREAVE 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 HARGREAVE 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 HARGREAVE 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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Soil series sharing subgroup-level classification with HARGREAVE, 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. WY-2012-03-23-04 | Goshen County, Northern Part - October 1981

    Typical landscape and parent material of Satanta-Noden soils, Rosebud-Hargreave soils, and Satanta-Willowman-Lambman soils (Soil Survey of Goshen County, Wyoming, Northern Part; 1981).

Map Units

Map units containing HARGREAVE 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
Cushman-Hargreave complex, 8 to 15 percent slopes152280496404jnk1co62319771:24000
Hargreave-Bernal sandy loams, 9 to 15 percent slopes59736497504jppjco64119801:24000
Hargreave sandy loam, 3 to 9 percent slopes58338497503jpphco64119801:24000
Hargreave fine sandy loam, 3 to 9 percent slopesHaD1351497574jprsco64319751:20000
Hargreave fine sandy loam, 1 to 3 percent slopesHaB624497573jprrco64319751:20000
Hargreave-Noden fine sandy loams, 0 to 6 percent slopes13522541349584cqrxwy02719931:24000
Hargreave-Lambman association, 1 to 8 percent slopes1347319349582cqrvwy02719931:24000
Hargreave-Cedak fine sandy loams, 2 to 10 percent slopes1337177349580cqrswy02719931:24000
Hargreave-Cedak fine sandy loams, 2 to 10 percent slopes16139516696901t1fzwy60920061:24000
Rosebud and Hargreave fine sandy loams, 0 to 6 percent sl opesRhB79731047373hzmwy61519651:20000
Rosebud and Hargreave fine sandy loams, 6 to 10 percent sl opesRhC23541047463hzxwy61519651:20000
Hargreave-Moskee fine sandy loams, 9 to 15 percent slopes14910860361136d3skwy63319871:24000
Hargreave-Moskee sandy loams, 3 to 9 percent slopes14810417361137d3slwy63319871:24000
Hargreave-Moskee association, dry, 3 to 15 percent slopes1504752361135d3sjwy63319871:24000
Lambman-Hargreave association, 3 to 15 percent slopes1733947361167d3tkwy63319871:24000
Rosebud-Hargreave fine sandy loams, 0 to 6 percent slopes23B61021048683j3vwy71519741:20000
Hargreave-Noden fine sandy loams, 0 to 6 percent slopes13B40341048522wcbfwy71519741:20000
Rosebud-Hargreave fine sandy loams, 6 to 10 percent slopes23C30301048693j3wwy71519741:20000
Hargreave-Noden fine sandy loams, 6 to 10 percent slopes13C10461048532wcbgwy71519741:20000
Hargreave-Lambman association, 1 to 8 percent slopes6024414151611jhlcwy71519741:20000
Hargreave-Cedak fine sandy loams, 2 to 10 percent slopes598414151601jhlbwy71519741:20000
Hargreave-Moskee-Mittenbutte sandy loams, 3 to 25 percent slopes7581628186815420pz1wy71920131:24000
Hargreave-Moskee sandy loams, 3 to 9 percent slopes75980713862401hjhfwy71920131:24000
Hargreave-Moskee fine sandy loams, 9 to 15 percent slopes76042186824620q20wy71920131:24000

Map of Series Extent

Approximate geographic distribution of the HARGREAVE 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 .