Official Series Description


Lab Data Summary

Aggregate lab data for the REEDWEST soil series. This aggregation is based on all pedons with a current taxon name of REEDWEST, 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 REEDWEST 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
43B04N0988S2004MT059014Reedwest7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.6450005,-111.2091675

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the REEDWEST 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 REEDWEST 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 REEDWEST 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 REEDWEST 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 flats position figure.

Competing Series

Soil series competing with REEDWEST 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 REEDWEST 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 REEDWEST 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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Soil series sharing subgroup-level classification with REEDWEST, 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 REEDWEST 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
Cabba-Reedwest-Anceney complex, 15 to 45 percent slopes747E3894155707570tmt62219971:24000
Reedwest-Adel-Castner complex, 15 to 45 percent slopes447E287815548656spmt62219971:24000
Castner-Reedwest-Rock outcrop complex, 25 to 60 percent slopes770F26541557205717mt62219971:24000
Reedwest-Cabba complex, 35 to 60 percent slopes689F192215565956z8mt62219971:24000
Reedwest-Cabba-Bowery complex, 15 to 45 percent slopes947E1056155770572vmt62219971:24000
Cabba-Reedwest complex, 4 to 15 percent slopes415D66715546656s1mt62219971:24000
Reedwest-Cabba-Castner complex, 25 to 60 percent slopes347F60415540856q5mt62219971:24000
Reedwest-Castner complex, 2 to 8 percent slopes753C165024875002phfymt62420211:24000
Reedwest-Roundor-Cabba complex, 2 to 8 percent slopes, foothills945C156425232354z2wmt62420211:24000
Reedwest-Roundor-Cabba complex, 8 to 35 percent slopes, foothills945E5631768364z2xmt62420211:24000
Whitecow, stony-Reedwest complex, 8 to 35 percent slopes180E59324862472pg4jmt6321:24000
Reedwest-Cabba-Watne complex, 4 to 15 percent slopes80D54924863082pg6hmt6321:24000
Ipano-Reedwest complex, 2 to 8 percent slopes70C23124863062pg6fmt6321:24000
Bacbuster-Reedwest-Castner complex, 4 to 15 percent slopes158D20224862442pg4fmt6321:24000
Reedwest-Cabba complex, 35 to 60 percent slopes19781465624xhtmt63619831:24000
Reedwest-Bacbuster-Cabba complex, 8 to 35 percent slopes658E123881480644z28mt63720141:24000
Reedwest-Bacbuster complex, 2 to 8 percent slopes458C98201480364z1cmt63720141:24000
Bacbuster-Reedwest-Castner complex, 4 to 15 percent slopes158D83531479894yzvmt63720141:24000
Bacbuster-Reedwest-Castner complex, 4 to 15 percent slopes, mountains58D738024963702pqk4mt63720141:24000
Ipano-Reedwest complex, 2 to 8 percent slopes70C6059603546n817mt63720141:24000
Bacbuster-Reedwest-Castner complex, 4 to 15 percent slopes, foothills258D561024963692pqk3mt63720141:24000
Reedwest-Roundor-Cabba complex, 2 to 8 percent slopes445C517824963772pqkbmt63720141:24000
Bacbuster-Auchard-Reedwest complex, 2 to 8 percent slopes258C51751480094z0hmt63720141:24000
Reedwest gravelly loam, 2 to 8 percent slopes245C50361480034z09mt63720141:24000
Reedwest loam, 2 to 8 percent slopes145C49241479854yzqmt63720141:24000
Whitecow, stony-Reedwest complex, 8 to 35 percent slopes180E492114876391ly0cmt63720141:24000
Reedwest-Bacbuster-Martinsdale, stony complex, 8 to 35 percent slopes958E33601480864z2zmt63720141:24000
Reedwest-Roundor-Cabba complex, 8 to 35 percent slopes445E282825173572q9zvmt63720141:24000
Bacbuster-Reedwest-Tolbert complex, 2 to 8 percent slopes158C26551479884yztmt63720141:24000
Reedwest-Roundor-Cabba complex, 2 to 8 percent slopes, foothills945C25291480834z2wmt63720141:24000
Reedwest, very stony-Martinsdale complex, 2 to 8 percent slopes466C231213833741hfhzmt63720141:24000
Bacbuster-Reedwest-Tolbert complex, 2 to 8 percent slopes, foothills558C180625173512q9zpmt63720141:24000
Reedwest-Bacbuster-Martinsdale, stony complex, 8 to 35 percent slopes, foothills758E132224963822pqkgmt63720141:24000
Reedwest-Cabba-Watne complex, 4 to 15 percent slopes80D113513833821hfj7mt63720141:24000
Bacbuster-Reedwest complex, 2 to 8 percent slopes958C8781480244z0zmt63720141:24000
Bacbuster-Reedwest complex, 8 to 25 percent slopes968E710640012pgzkmt63720141:24000
Wilsall-Reedwest-Cabba complex, 15 to 45 percent slopes106F649603549n81bmt63720141:24000
Absarokee-Reedwest complex, 2 to 8 percent slopes872C573813819w9v7mt63720141:24000
Reedwest-Roundor-Cabba complex, 8 to 35 percent slopes, foothills945E3211480844z2xmt63720141:24000
Reedwest-Castner complex, 2 to 8 percent slopes253C258214981350wpmt63920001:24000
Reedwest-Castner complex, 8 to 15 percent slopes253D213414981450wqmt63920001:24000
Reedwest-Castner complex, 15 to 35 percent slopes253E168814981550wrmt63920001:24000
Reedwest-Cabba loams, 2 to 8 percent slopes176C160214970950sbmt63920001:24000
Reedwest-Cabba-Castner complex, 15 to 60 percent slopes399F1538149960511fmt63920001:24000
Vershal-Reedwest complex, 8 to 35 percent slopes393E8251499535116mt63920001:24000
Farnuf-Reedwest-Shawmut complex, 15 to 35 percent slopes346E46714990150zjmt63920001:24000
Reedwest-Rock outcrop complex, 15 to 60 percent slopes, very stony402F247149963511jmt63920001:24000
Reedwest, extremely stony-Shawmut, stony-Cabba, stony complex, 15 to 60 percent slopes5617F466615648257ttmt6691:24000
Work-Bacbuster_Reedwest complex, 4 to 15 percent slopes747D126715695658b3mt6691:24000
Reedwest-Cabba-Castner complex, 25 to 60 percent slopes347F132741431swj4mt6691:24000
Vershal-Reedwest complex, 8 to 35 percent slopes393E8324813352p912mt6691:24000
Reedwest-Castner complex, 8 to 15 percent slopes253D72620207ntcpmt6691:24000

Map of Series Extent

Approximate geographic distribution of the REEDWEST 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 .