Official Series Description


Lab Data Summary

Aggregate lab data for the HURST soil series. This aggregation is based on all pedons with a current taxon name of HURST, 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 HURST 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
114B79IL1450101979IL145010Hurst1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.9603294,-89.4099306
114B80IL1450061980IL145006Hurst1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.9780208,-89.387716
n/a77IL0650081977IL065008Hurst1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HURST 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 HURST 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 HURST 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 HURST 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 HURST 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 HURST 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 HURST 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 HURST, 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. IL-2010-09-01-12 | Franklin and Jefferson Counties - 2003

    Typical pattern of soils and parent material in the Colp-Hurst-Okaw association (Soil Survey of Franklin and Jefferson Counties, Illinois; 2003).

  2. IL-2010-09-01-81 | Washington County - 1998

    Typical pattern of soils and parent material in the Hurst-Okaw association (Soil Survey of Washington County, Illinois; 1998).

  3. IL-2011-08-04-78 | Monroe County - 1987

    Typical pattern of soils and parent material in the Colp-Hurst-Okaw association (Soil Survey of Monroe County, Illinois; 1987).

  4. IL-2011-08-04-84 | Perry County - 1988

    Typical pattern of soils and parent material in the Hurst-Okaw-Colp association (Soil Survey of Perry County, Illinois; 1988).

  5. IL-2011-08-04-97 | Randolph County - 1988

    Pattern of soils and parent material in the St. Charles-Hurst-Martinsville association (Soil Survey of Randolph County, Illinois; 1988).

  6. IL-2011-08-05-06 | Washington County - 1998

    Typical pattern of soils and parent material in the Hurst-Okaw association (Soil Survey of Washington County, Illinois; 1998).

Map Units

Map units containing HURST 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
Hurst silt loam, 0 to 2 percent slopes, rarely flooded7338A516602283n6qhil00320021:12000
Hurst silt loam, 2 to 5 percent slopes, rarely flooded7338B230602284n6qjil00320021:12000
Hurst silt loam, 0 to 2 percent slopes, rarely flooded7338A3181755195wmxil01319861:15840
Hurst silt loam, 0 to 2 percent slopes, rarely flooded7338A11701746702tbsdil02719921:15840
Hurst silt loam, 2 to 5 percent slopes, eroded, rarely flooded7338B25351746712tbsril02719921:15840
Hurst silt loam, 0 to 2 percent slopes338A35278069372tbsbil05520051:12000
Hurst silt loam, 0 to 2 percent slopes, rarely flooded7338A182211726739wil06119681:15840
Hurst silt loam, 0 to 2 percent slopes, rarely flooded7338A261714015ryzril06920031:12000
Hurst silty clay loam, 0 to 2 percent slopes, occasionally flooded8693A89714059rz15il06920031:12000
Hurst silt loam, 0 to 2 percent slopes338A837115378352tbsbil07720061:12000
Hurst silt loam, 2 to 5 percent slopes, eroded, rarely flooded7338B2294515408092tbsril07720061:12000
Hurst silt loam, 2 to 5 percent slopes, eroded338B2225415390922tbspil07720061:12000
Hurst silt loam, 0 to 2 percent slopes, rarely flooded7338A140315407912tbsdil07720061:12000
Hurst silty clay loam, 2 to 5 percent slopes, eroded, rarely flooded7338B298728389sfyfil08320021:12000
Hurst silt loam, 0 to 2 percent slopes, rarely flooded7338A1761989092tbsdil11920011:12000
Hurst silty clay loam, 0 to 2 percent slopes, occasionally flooded8693A1878808157w3ylil12720041:12000
Hurst silt loam, 2 to 5 percent slopes, occasionally flooded8338B31718413965lzil13319981:12000
Hurst silt loam, 0 to 2 percent slopes, rarely flooded7338A162714059132tbsdil14520051:12000
Hurst silty clay loam, 0 to 2 percent slopes, occasionally flooded8693A1198608158ndv0il15120031:12000
Hurst silt loam, 0 to 2 percent slopes, rarely flooded7338A120607170nct4il15120031:12000
Hurst silt loam, 0 to 2 percent slopes, rarely flooded7338A164748990t4czil15320041:12000
Hurst silt loam, 2 to 5 percent slopes, rarely flooded7338B62748991t4d0il15320041:12000
Hurst silt loam, 2 to 5 percent slopes338B19142004752wcypil15720011:12000
Hurst silt loam, 0 to 2 percent slopes338A11222004742tbsbil15720011:12000
Hurst silty clay loam, 5 to 10 percent slopes, eroded, occasionally flooded8338C216261831482tp2hil16319971:12000
Hurst silt loam, 2 to 5 percent slopes, eroded, occasionally flooded8338B211081831472tbsqil16319971:12000
Redbud-Hurst silty clay loams, 5 to 10 percent slopes, severely eroded906C394518318664m7il16319971:12000
Hurst silt loam, 0 to 2 percent slopes, occasionally flooded8338A8001831462tbscil16319971:12000
Hurst silt loam, sandy substratum, 0 to 2 percent slopes, occasionally flooded8489A5591831552tbsnil16319971:12000
Hurst silt loam, 0 to 2 percent slopes338A53351788752tbsbil16519741:15840
Hurst silt loam, 0 to 2 percent slopes, rarely flooded7338A186615289962tbsdil18920061:12000
Hurst silt loam, 0 to 2 percent slopes338A142515289442tbsbil18920061:12000
Hurst silt loam, 0 to 2 percent slopes338A344614781202tbsbil19920071:12000
Hurst silt loam, 0 to 2 percent slopes, rarely flooded7338A5517107172tbsdil19920071:12000
Hurst silt loam, 2 to 5 percent slopes, eroded, rarely flooded7338B2219028642tbsril19920071:12000
Hurst silt loam, 0 to 2 percent slopes, rarely floodedHuA47215961871qkyxky60219721:12000
Hurst silt loam, 0 to 2 percent slopes, protectedHrA39615961891qkyzky60219721:12000
Hurst silt loam, 0 to 2 percent slopes, rarely flooded6603942751845486615mo18319791:24000

Map of Series Extent

Approximate geographic distribution of the HURST 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 .