Official Series Description


Lab Data Summary

Aggregate lab data for the HESCH soil series. This aggregation is based on all pedons with a current taxon name of HESCH, 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 HESCH 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
105UMN2744S1978MN1692744Hesch3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.9641304,-92.0198822

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HESCH 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 HESCH 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 HESCH 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 HESCH 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 HESCH 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 HESCH 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 HESCH 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 mountains figure.

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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with HESCH, 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 HESCH 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
Shelby, sandy substratum-Hesch, deep-Hesch complex, 9 to 14 percent slopes, moderately eroded247D29224849082pdrbia02920101:12000
Shelby, sandy substratum-Hesch, deep-Hesch complex, 9 to 14 percent slopes, moderately eroded247D240425412302qhz3ia13719871:15840
Marshall, sandstone substratum-Hesch complex, 14 to 25 percent slopes517F21625412312qhz4ia13719871:15840
Channahon-Hesch fine sandy loams, 0 to 2 percent slopes817A11415474801ny8qil06320051:12000
Channahon-Hesch fine sandy loams, 2 to 6 percent slopes817B4415474811ny8ril06320051:12000
Channahon-Hesch fine sandy loams, 2 to 6 percent slopes817B162514160581jjj9il09920061:12000
Channahon-Hesch fine sandy loams, 0 to 2 percent slopes817A133914160571jjj8il09920061:12000
Hesch-Rasset complex, 1 to 6 percent slopesN535B164916700031t1s2mn04920071:12000
Hesch sandy loam, deep, 20 to 30 percent slopes, moderately eroded245E223825617482qr2hwi01119601:12000
Hesch loam, deep, 20 to 30 percent slopes, moderately eroded240E220625617442kpz7wi01119601:12000
Hesch loam, deep, 12 to 20 percent slopes, moderately eroded240D219425617432kpz6wi01119601:12000
Hesch sandy loam, deep, 12 to 20 percent slopes, moderately eroded245D216625617452kpz8wi01119601:12000
Hesch loam, deep, 6 to 12 percent slopes, moderately eroded240C214725617472qr2gwi01119601:12000
Hesch sandy loam, deep, 6 to 12 percent slopes, moderately eroded245C29425617502qr2jwi01119601:12000
Hesch sandy loam, deep, 12 to 20 percent slopes, moderately eroded245D29425039912kpz8wi02319601:12000
Hesch loam, deep, 20 to 30 percent slopes, moderately eroded240E28725039902kpz7wi02319601:12000
Hesch loam, deep, 12 to 20 percent slopes, moderately eroded240D27225039892kpz6wi02319601:12000
Hesch fine sandy loam, 20 to 45 percent slopes, moderately erodedHcF2447424253g7glwi04319591:20000
Hesch fine sandy loam, 15 to 20 percent slopes, moderately erodedHcE2387424250g7ghwi04319591:20000
Hesch fine sandy loam, 10 to 15 percent slopes, moderately erodedHcD2346424247g7gdwi04319591:20000
Hesch loam, 15 to 20 percent slopes, moderately erodedHeE2150424256g7gpwi04319591:20000
Hesch loam, 10 to 15 percent slopes, moderately erodedHeD2105424255g7gnwi04319591:20000
Hesch fine sandy loam, 2 to 10 percent slopes, moderately erodedHcC246424246g7gcwi04319591:20000
Hesch loam, 2 to 10 percent slopes, moderately erodedHeC221424254g7gmwi04319591:20000
Hesch loam, deep, 12 to 20 percent slopes, moderately eroded240D217527748052kpz6wi04919601:20000
Hesch sandy loam, deep, 20 to 30 percent slopes, moderately eroded245E22327748082qr2hwi04919601:20000
Hesch fine sandy loam, 2 to 6 percent slopesHeB582422147g58nwi10919751:15840
Hesch fine sandy loam, 12 to 20 percent slopes, erodedHeD2316422149g58qwi10919751:15840
Hesch fine sandy loam, 6 to 12 percent slopes, erodedHeC2260422148g58pwi10919751:15840

Map of Series Extent

Approximate geographic distribution of the HESCH 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 .