Official Series Description


Lab Data Summary

Aggregate lab data for the BUSHVALLEY soil series. This aggregation is based on all pedons with a current taxon name of BUSHVALLEY, 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 BUSHVALLEY 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
3940A3588S1965AZ001022Bushvalley3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.853611,-109.1422195
48A84P073084CO109002Bushvalley7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8291664,-106.3791656

Water Balance

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

Soil series sharing subgroup-level classification with BUSHVALLEY, 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 BUSHVALLEY 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
Bushvalley cobbly sandy loam, 5 to 40 percent slopesBsE821017184651vp6caz63519681:31680
Bushvalley loam, 1 to 5 percent slopesBuC100017184661vp6daz63519681:31680
Cambern-Bushvalley complex, 1 to 15 percent slopes1818961856573209xgaz67520091:24000
Bushvalley-Youga complex, 3 to 25 percent slopes814800498631jqvwco63019751:24000
Bushvalley very stony loam, 10 to 40 percent slopes72450498630jqvvco63019751:24000
Bushvalley-Gelkie-Rock outcrop complex, 3 to 65 percent slopes1027921498440jqnqco63319811:24000
Bushvalley-Tellura complex, 9 to 65 percent slopes1116985498441jqnrco63319811:24000
Bushvalley cobbly loam, 3 to 45 percent slopes98820498519jqr8co63319811:24000
Bushvalley cobbly loam, 5 to 40 percent slopes1414367498277jqhgco63719861:24000
Ess-Bushvalley complex, 10 to 45 percent slopes3313351498298jqj4co63719861:24000
Bushvalley-Whiteman cobbly loams, 15 to 50 percent slopes1511582498278jqhhco63719861:24000
Seitz-Bushvalley complex, 15 to 50 percent slopes1036902498246jqggco63719861:24000
Woodhall-Bushvalley complex, 15 to 65 percent slopes20122501509573k37vco66019941:24000
Woodhall, dry-Bushvalley complex, 5 to 40 percent slopes202500509575k37xco66019941:24000
Quander-Bushvalley association, 15 to 60 percent slopes1603043524536972nc8jco66419871:24000
Bushvalley-Bowen association, 20 to 60 percent slopes1122513324536652nc7hco66419871:24000
Bushvalley-Rock outcrop complex, 10 to 90 percent slopes1132346624538062ncd1co66419871:24000
Bushvalley-Rogert complex, 12 to 50 percent slopes1141438224538072ncd2co66419871:24000
Bowen, cool-Bushvalley association, 35 to 60 percent slopes109580124536622nc7dco66419871:24000
Skisams-Bushvalley-Cryoborolls, moderately deep complex, 2 to 15 percent slopes9612373502160jvjqco67519861:24000
Bushvalley-Nordicol Variant complex, 2 to 10 percent slopes293763502031jvdkco67519861:24000
Ewetopia-Bushvalley, rubbly-Tricorner, extremely stony complex, 2 to 15 percent slopesMt54504026084671ift5ut6291:24000
Bushvalley very stony loam, 15 to 40 percent slopes3401263483864j7hjut63419971:24000
Bushvalley very stony loam, 15 to 40 percent slopes273213504419jxwlut63619841:24000
Sheckle-Perma family-Bushvalley-Rubble land complex, 2 to 15 percent slopes88136824552052ndv5ut6421:63360
Bushvalley family-Rock outcrop complex, 10 to 75 percent slopes122625177nzk0ut6491:24000
Elwood-Bushvalley families, complex, 15 to 75 percent slopes146625199nzkqut6491:24000
Elwood, moderately deep-Bushvalley-Elwood families, association, 0 to 60 percent slopes147625237nzlyut6491:24000

Map of Series Extent

Approximate geographic distribution of the BUSHVALLEY 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 .