Official Series Description


Lab Data Summary

Aggregate lab data for the RIVERRUN soil series. This aggregation is based on all pedons with a current taxon name of RIVERRUN, 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 RIVERRUN were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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 RIVERRUN 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 RIVERRUN series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-10-24), parsed OSD records (updated 2024-10-23) and snapshot of SC database (updated 2024-10-23).

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Select annual climate data summaries for the RIVERRUN series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

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Geomorphic description summaries for the RIVERRUN 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 (updated 2024-10-23).

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There are insufficient data to create the 3D mountains figure.

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Competing Series

Soil series competing with RIVERRUN share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2024-10-23) and snapshot of the SC database (updated 2024-10-23).

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Select annual climate data summaries for the RIVERRUN series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the RIVERRUN 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 (updated 2024-10-23).

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.

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

Soil series sharing subgroup-level classification with RIVERRUN, 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 (updated 2024-10-23).

Block Diagrams

No block diagrams are available.

Map Units

Map units containing RIVERRUN 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
Riverrun, frequently flooded-Beavrock, occasionally flooded complex, 0 to 4 percent slopes11B25781480924z35mt60420011:24000
Dillon-Riverrun-Beavrock complex, 0 to 4 percent slopes, rarely flooded183B25561482034z6rmt60420011:24000
Bronec, Amesha, and Riverrun, occasionally flooded soils, 0 to 35 percent slopes41E427609142nfvrmt60420011:24000
Dillon, saline-Dillon-Riverrun, saline complex, 0 to 4 percent slopes, rarely flooded195B4191482764z93mt60420011:24000
Riverrun, occasionally flooded-Rivra complex, 0 to 2 percent slopes60A40516974841tzckmt60420011:24000
Rivra, stony-Riverrun complex, 0 to 2 percent slopes161A11316974811tzcgmt60420011:24000
Riverrun-Cardwell complex, 0 to 2 percent slopes482A421476134ylqmt60919711:24000
Bronec, Amesha, and Riverrun, channeled soils, 0 to 35 percent slopes41151475714ykcmt60919711:24000
Dillon-Beavrock, rarely flooded-Riverrun complex, 0 to 4 percent slopes283B99423755442kqygmt61220111:24000
Riverrun, frequently flooded-Beavrock, occasionally flooded complex, 0 to 4 percent slopes11B5625976514z35mt61220111:24000
Dillon-Riverrun-Beavrock complex, 0 to 4 percent slopes, rarely flooded183B3625976664z6rmt61220111:24000
Bronec, Amesha, and Riverrun, occasionally flooded soils, 0 to 35 percent slopes41E132597683nfvrmt61220111:24000
Cardwell-Riverrun complex, 0 to 2 percent slopes521A2786151105527cmt62719981:24000
Riverrun gravelly sandy loam, 0 to 2 percent slopes481A20151510945270mt62719981:24000
Bronec, Amesha, and Riverrun, channeled, soils, 0 to 35 percent slopes4114131510665263mt62719981:24000
Pieriver-Cardwell-Riverrun loams, 0 to 2 percent slopes341A1182151045525fmt62719981:24000
Bronec, Riverrun, Channeled, and Amesha soils, 0 to 8 percent slopes9111115154252pgmt62719981:24000
Ryell-Riverrun complex, 0 to 2 percent slopes522A984151106527dmt62719981:24000
Cardwell-Riverrun-Pieriver complex, 0 to 2 percent slopes523A952151107527fmt62719981:24000
Riverrun sandy loam, 0 to 2 percent slopes48A7861510975273mt62719981:24000
Riverrun, Handke, and Ryell soils, 0 to 2 percent slopes, channeled483A7641510965272mt62719981:24000
Cardwell-Riverrun complex, 0 to 2 percent slopes, saline525A517151109527hmt62719981:24000
Nestley-Riverrun-Pieriver complex, 0 to 2 percent slopes413A4311510695266mt62719981:24000
Riverrun-Cardwell complex, 0 to 2 percent slopes482A4211510955271mt62719981:24000
Meadowcreek-Nestley-Riverrun complex, 0 to 2 percent slopes692A38115125652d7mt62719981:24000
Riverrun, frequently ponded family-Riverwash-Water, complex, 0 to 2 percent slopes328266831692352z1dzmt63619831:24000
Riverrun-Rivra complex, 0 to 2 percent slopes2472016975011tzd3mt63619831:24000
Riverrun-Gash complex, 0 to 2 percent slopes151A157124226152m9xwmt63819851:24000
Curlew-Riverrun complex, 0 to 2 percent slopes146A99924226122m9xsmt63819851:24000
Riverrun complex, 0 to 2 percent slopes150A90324226142m9xvmt63819851:24000
Riverrun-Canarway-Fredburr complex, 0 to 2 percent slopes11A62424225952m9x7mt63819851:24000
Riverwash-Water-Riverrun complex, 0 to 2 percent slopes10A42324225942m9x6mt63819851:24000
Riverrun-Gash-Curlew complex, 0 to 2 percent slopes160A42324226212m9y2mt63819851:24000
Losthorse, rubbly-Poverty-Riverrun, stony, complex, 1 to 35 percent slopes20E15924225982m9xbmt63819851:24000
Gash-Riverrun complex, 0 to 2 percent slopes153A14624226162m9xxmt63819851:24000
Chereete-Riverrun-Curlew complex, 0 to 8 percent slopes17C6824227572mb2gmt63819851:24000
Riverrun-Canarway-Fredburr complex, 0 to 2 percent slopes, occassionally flooded11A6405757589tfbcmt64520131:12000
Gash, occasionally flooded-Riverrun, rarely flooded complex, 0 to 2 percent slopes153A543015855659zqmt64520131:12000
Riverwash-Water-Riverrun, frequently flooded complex, 0 to 2 percent slopes10A5070757588tfbbmt64520131:12000
Riverrun complex, 0 to 2 percent slopes, rarely flooded150A390915855959ztmt64520131:12000
Curlew-Riverrun complex, 0 to 2 percent slopes, rarely flooded146A343815856059zvmt64520131:12000
Riverrun, rarely flooded-Gash, occasionally flooded-Curlew, rarely flooded complex, 0 to 2 percent slopes160A32551585745b09mt64520131:12000
Chereete-Riverrun, rarely flooded-Curlew, rarely flooded complex, 0 to 8 percent slopes17C3243633397p835mt64520131:12000
Riverrun-Gash complex, 0 to 2 percent slopes, rarely flooded151A251115855859zsmt64520131:12000
Riverrun-Curlew complex, 0 to 2 percent slopes, rarely flooded12A2283757590tfbdmt64520131:12000
Losthorse, rubbly-Poverty-Riverrun, rarely flooded complex, 0 to 35 percent slopes20E2161757593tfbhmt64520131:12000
Losthorse, rubbly-Poverty-Riverrun, stony, complex, 1 to 35 percent slopes20E19119078232217pmt64720071:24000
Riverwash-Water-Riverrun complex, 0 to 2 percent slopes10A5524871542ph2smt64720071:24000
Chereete-Riverrun-Curlew complex, 0 to 8 percent slopes17C3319078222217nmt64720071:24000
Riverrun-Curlew complex, 0 to 2 percent slopes12A324871552ph2tmt64720071:24000
Curlew-Riverrun complex, 0 to 2 percent slopes146A124871572ph2wmt64720071:24000
Riverrun-Rivra complex, 0 to 2 percent slopes60A59014246391jtg3mt67020071:24000
Riverrun, occasionally flooded-Mannixlee, frequently flooded complex, 0 to 4 percent slopes12A349320239br79mt67020071:24000
Rivra, stony-Riverrun complex, 0 to 2 percent slopes61A33014246381jtg2mt67020071:24000
Perma, very stony-Riverrun, extremely stony complex, 1 to 6 percent slopes, frequently flooded121131368552ypnrwy6291:24000
Perma, very stony-Riverrun, extremely stony complex, 1 to 6 percent slopes, frequently flooded121132533472ypnrwy65620081:24000

Map of Series Extent

Approximate geographic distribution of the RIVERRUN 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 (updated 2024-10-30).