Official Series Description


Lab Data Summary

Aggregate lab data for the HILIGHT soil series. This aggregation is based on all pedons with a current taxon name of HILIGHT, 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 HILIGHT 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
58B91P019991WY005001Hilight5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.7416649,-105.1197205

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HILIGHT 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 HILIGHT 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 HILIGHT 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 HILIGHT 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 HILIGHT 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 HILIGHT series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the HILIGHT 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.

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 HILIGHT, 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

No block diagrams are available.

Map Units

Map units containing HILIGHT 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
Hilight-Savageton clays, 6 to 15 percent slopes143405863496002tvvfwy02719931:24000
Hilight-Rock outcrop complex, 6 to 40 percent slopes14230193349598cqscwy02719931:24000
Grummit-Hilight-Rock outcrop complex, 15 to 45 percent slopes1327676349578cqrqwy02719931:24000
Grummit-Hilight clays, 6 to 15 percent slopes1312520349576cqrnwy02719931:24000
Renohill-like-Spyglass-like-Hilight complex, 2 to 30 percent slopes533333566702ynm3wy04319761:24000
Chipendale-like-Hilight-Cielito-like complex, 5 to 50 percent slopes5D34335670430zsswy04319761:24000
Hilight-Wags-Badland complex, 3 to 45 percent slopes13962383616962v08wwy04519841:24000
Hilight clay loam, 3 to 30 percent slopes512787349456cqmswy04519841:24000
Hilight-Savageton clays, 6 to 15 percent slopes15724916148422tvvfwy04519841:24000
Hilight-Wags-Badland complex, 3 to 45 percent slopes163808643498542v08wwy60519951:24000
Hilight-Taluce, cool-Wags complex, 6 to 40 percent slopes1615187349852cr1kwy60519951:24000
Chipendale-like-Hilight-Cielito-like complex, 5 to 50 percent slopes5D34335826030zsswy6171:24000
Badland-Shingle-Hilight complex, 15 to 35 percent slopes546233028862ypp0wy6171:24000
Renohill-like-Spyglass-like-Hilight complex, 2 to 30 percent slopes533333582852ynm3wy6171:24000
Hilight-Lonebear-like-Renohill complex, 4 to 20 percent slopes532831332372ynlwwy6291:24000
Badland-Shingle-Hilight complex, 15 to 35 percent slopes546231368632ypp0wy6291:24000
Renohill-Hilight-Pultney complex, 15 to 55 percent slopes542931332462ynm5wy6291:24000
Renohill-like-Spyglass-like-Hilight complex, 2 to 30 percent slopes533331332442ynm3wy6291:24000
Razsun-like-Hilight complex, 20 to 55 percent slopes546631332382ynlxwy6291:24000
Samday-Gayhart-Hilight clay loams, moist, 2 to 60 percent slopes2449763360586d36twy63319871:24000
Hilight-Rock outcrop complex, 10 to 30 percent slopes1684766361151d3t1wy63319871:24000
Samday-Hilight clay loams, 2 to 45 percent slopes2451119360585d36swy63319871:24000
Hilight-Wags-Badland complex, 3 to 45 percent slopes20627043612792v08wwy70919831:24000

Map of Series Extent

Approximate geographic distribution of the HILIGHT 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 .