Official Series Description


Lab Data Summary

Aggregate lab data for the KORELL soil series. This aggregation is based on all pedons with a current taxon name of KORELL, 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 KORELL 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 KORELL 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 KORELL 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 KORELL 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 KORELL 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 KORELL 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 KORELL 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 KORELL 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 KORELL, 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 KORELL 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
Korell loam, 0 to 2 percent slopes, rarely floodedE4147A8482345625d1vgmt10919561:31680
Korell loam, 0 to 2 percent slopes, rarely flooded12A12091476944ypbmt63019911:24000
Korell loam, 0 to 2 percent slopes, protected112A9441476854yp1mt63019911:24000
Korell silt loam, 0 to 3 percent slopes96A3921480884z31mt63720141:24000
Korell silt loam, 0 to 3 percent slopes, foothills196A22725230262qb03mt63720141:24000
Korell silt loam, 3 to 8 percent slopes96C1401480894z32mt63720141:24000
Korell-Daglum-Fluvaquents complex, channeled, 0 to 2 percent slopes, frequently floodedE4180A40427556601vzw3nd00119831:20000
Korell-Rhoades-Daglum complex, 0 to 2 percent slopes, rarely floodedE4181A5427556611vzw4nd00119831:20000
Korell loam, 0 to 2 percent slopes, rarely floodedE4147A142755659d1vgnd00119831:20000
Korell-Daglum-Fluvaquents complex, channeled, 0 to 2 percent slopes, frequently floodedE4180A292417151921vzw3nd00719981:24000
Korell-Rhoades-Daglum complex, 0 to 2 percent slopes, rarely floodedE4181A102127071071vzw4nd00719981:24000
Korell loam, 0 to 2 percent slopes, rarely floodedE4147A3182707105d1vgnd00719981:24000
Korell loam, 0 to 2 percent slopes, rarely floodedE4147A34962563567d1vgnd01119691:20000
Korell-Daglum-Fluvaquents complex, channeled, 0 to 2 percent slopes, frequently floodedE4180A116125635681vzw3nd01119691:20000
Korell-Rhoades-Daglum complex, 0 to 2 percent slopes, rarely floodedE4181A2427584571vzw4nd01119691:20000
Korell-Rhoades-Daglum complex, 0 to 2 percent slopes, rarely floodedE4181A12126617041vzw4nd01519671:20000
Korell-Rhoades-Daglum complex, 0 to 2 percent slopes, rarely floodedE4181A373927072471vzw4nd02519811:20000
Korell-Daglum-Fluvaquents complex, channeled, 0 to 2 percent slopes, frequently floodedE4180A158027072461vzw3nd02519811:20000
Belfield-Korell loams, 0 to 2 percent slopes, rarely floodedE4101A18227584912q63lnd02519811:20000
Korell-Daglum-Fluvaquents complex, channeled, 0 to 2 percent slopes, frequently floodedE4180A33227596541vzw3nd03719851:20000
Korell-Daglum-Fluvaquents complex, channeled, 0 to 2 percent slopes, frequently floodedE4180A116725258171vzw3nd04119861:20000
Belfield-Korell loams, 0 to 2 percent slopes, rarely floodedE4101A304226992452q63lnd05719761:20000
Korell-Rhoades-Daglum complex, 0 to 2 percent slopes, rarely floodedE4181A1017151071vzw4nd05719761:20000
Korell loam, 0 to 2 percent slopes, rarely floodedE4147A21312699175d1vgnd05919981:20000
Korell-Daglum-Fluvaquents complex, channeled, 0 to 2 percent slopes, frequently floodedE4180A121617183591vzw3nd05919981:20000
Korell-Rhoades-Daglum complex, 0 to 2 percent slopes, rarely floodedE4181A4417183601vzw4nd05919981:20000
Belfield-Korell loams, 0 to 2 percent slopes, rarely floodedE4101A109425259902q63lnd06519711:20000
Korell-Rhoades-Daglum complex, 0 to 2 percent slopes, rarely floodedE4181A427557171vzw4nd06519711:20000
Korell-Rhoades-Daglum complex, 0 to 2 percent slopes, rarely floodedE4181A5227597061vzw4nd08519921:24000
Korell-Daglum-Fluvaquents complex, channeled, 0 to 2 percent slopes, frequently floodedE4180A141727158611vzw3nd08719741:20000
Korell loam, 0 to 2 percent slopes, rarely floodedE4147A42758521d1vgnd08719741:20000
Korell-Daglum-Fluvaquents complex, channeled, 0 to 2 percent slopes, frequently floodedE4180A1580127160141vzw3nd08919651:20000
Korell-Rhoades-Daglum complex, 0 to 2 percent slopes, rarely floodedE4181A502527160151vzw4nd08919651:20000

Map of Series Extent

Approximate geographic distribution of the KORELL 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 .