Official Series Description


Lab Data Summary

Aggregate lab data for the RAPIDCREEK soil series. This aggregation is based on all pedons with a current taxon name of RAPIDCREEK, 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 RAPIDCREEK 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 RAPIDCREEK 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 RAPIDCREEK 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 RAPIDCREEK 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 RAPIDCREEK 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 RAPIDCREEK 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 RAPIDCREEK 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 RAPIDCREEK 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 RAPIDCREEK, 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 RAPIDCREEK 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
Rapidcreek silt loam, poorly drained, 0 to 2 percent slopes, occasionally floodedP348A2526688782rvgnsd01919701:24000
Rapidcreek loam, warm, 3 to 9 percent slopes, rarely floodedP346C32427331322rvgmsd04719801:24000
Rapidcreek loam, dry, 3 to 9 percent slopes, rarely floodedQ0646C26724346372mqfpsd04719801:24000
Barnum, cool-Rapidcreek complex, 0 to 6 percent slopes, rarely floodedQ0603B14725169932mhlfsd04719801:24000
Cordeston-Rapidcreek, rarely flooded complex, dry, 2 to 9 percent slopesQ0620C1825169972krlhsd04719801:24000
Barnum-Rapidcreek, warm complex, 0 to 6 percent slopes, floodedP034B927681002qt22sd04719801:24000
Rapidcreek very gravelly loam, noncalcareous, 1 to 9 percent slopes, rarely floodedQ0229C96924258832mfb9sd08120071:24000
Rapidreek gravelly loam, 2 to 10 percent slopes, rarely floodedQ0560C95623758362kr7wsd08120071:24000
Rapidcreek gravelly loam, warm, 1 to 3 percent slopes, occasionally floodedP342A84527332822rvgksd08120071:24000
Rapidcreek, warm-Nihill, moderately deep-Barnum complex, 1 to 20 percent slopes, floodedP350D76527332832rvgpsd08120071:24000
Sodawells, somewhat poorly drained-Rapidcreek, poorly drained complex, 0 to 2 percent slopes, occasionally floodedP468A73127332492rxshsd08120071:24000
Cordeston-Rapidcreek, rarely flooded complex, 2 to 9 percent slopesQ0520C27723757522kr55sd08120071:24000
Rapidcreek silt loam, poorly drained, 0 to 2 percent slopes, occasionally floodedP348A19827332912rvgnsd08120071:24000
Rapidcreek gravelly loam, poorly drained, 0 to 2 percent slopes, occasionally floodedP340A3127332462rvgjsd08120071:24000
Rapidcreek very cobbly sandy loam, warm, 1 to 6 percent slopes, nonfloodedP344B229327456402rvglsd60019741:24000
Rapidcreek gravelly loam, warm, 1 to 3 percent slopes, occasionally floodedP342A31127681202rvgksd60019741:24000
Rapidreek gravelly loam, 2 to 10 percent slopes, rarely floodedQ0560C22225142772kr7wsd60019741:24000
Rapidcreek cobbly loam, dry, 2 to 10 percent slopes, rarely floodedQ0645C21925171212mj7fsd60019741:24000
Cordeston-Rapidcreek, rarely flooded complex, 2 to 9 percent slopesQ0520C8725139652kr55sd60019741:24000
Cordeston-Rapidcreek, rarely flooded complex, dry, 2 to 9 percent slopesQ0620C5425169962krlhsd60019741:24000
Rapidcreek very gravelly loam, noncalcareous, 1 to 9 percent slopes, rarely floodedQ0229C3425139482mfb9sd60019741:24000
Cordeston-Rapidcreek, rarely flooded complex, dry, 2 to 9 percent slopesQ0620C465625864422krlhsd60720111:24000
Barnum-Rapidcreek, warm complex, 0 to 6 percent slopes, floodedP034B318027456432qt22sd60720111:24000
Barnum, cool-Rapidcreek complex, 0 to 6 percent slopes, rarely floodedQ0603B240925865502mhlfsd60720111:24000
Rapidcreek cobbly loam, dry, 2 to 10 percent slopes, rarely floodedQ0645C181825864742mj7fsd60720111:24000
Rapidcreek cobbly loam, warm, 2 to 10 percent slopes, rarely floodedP338C97927457012rvghsd60720111:24000
Cordeston-Rapidcreek, rarely flooded complex, 2 to 9 percent slopesQ0520C75325864122kr55sd60720111:24000
Rapidcreek very gravelly loam, noncalcareous, 1 to 9 percent slopes, rarely floodedQ0229C49125864902mfb9sd60720111:24000
Barnum, moist-Rapidcreek, warm complex, 0 to 6 percent slopes, floodedP035B33827456442s039sd60720111:24000
Rapidreek gravelly loam, 2 to 10 percent slopes, rarely floodedQ0560C21125864302kr7wsd60720111:24000
Rapidcreek gravelly loam, warm, 1 to 3 percent slopes, occasionally floodedP342A18427681462rvgksd60720111:24000
Rapidcreek loam, dry, 3 to 9 percent slopes, rarely floodedQ0646C2025865562mqfpsd60720111:24000
Rapidcreek gravelly loam, warm, 1 to 3 percent slopes, occasionally floodedP342A527459532rvgkwy01119781:24000
Barnum-Rapidcreek, warm complex, 0 to 6 percent slopes, floodedP034B6327682102qt22wy04519841:24000

Map of Series Extent

Approximate geographic distribution of the RAPIDCREEK 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 .