Official Series Description


Lab Data Summary

Aggregate lab data for the BOWERY soil series. This aggregation is based on all pedons with a current taxon name of BOWERY, 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 BOWERY were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
4692P072592MT041001BOWERY4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.3191681,-109.6886139

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BOWERY 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.

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the BOWERY series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

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

Click the image to view it full size.

Geomorphic description summaries for the BOWERY 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with BOWERY share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

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

Click the image to view it full size.

Geomorphic description summaries for the BOWERY 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with BOWERY, 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 BOWERY 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
Bowery loam, 4 to 8 percent slopes76C1479344060ck0qmt04119941:24000
Bowery loam, 8 to 15 percent slopes76D1282344061ck0rmt04119941:24000
Bowery loam, 0 to 4 percent slopes76B609344059ck0pmt04119941:24000
Bowery-Lolo complex, 2 to 12 percent slopes12D1083039569pcw3mt60219631:20000
Enbar-Bowery-Nythar complex, 4 to 15 percent slopes512D51476704ynkmt60919711:24000
Enbar-Bowery-Nythar complex, 4 to 15 percent slopes512D270915555556vxmt62219971:24000
Meagher-Shawmut-Bowery complex, 15 to 45 percent slopes752E2031155709570wmt62219971:24000
Bowery loam, 2 to 8 percent slopes14C198915529956lnmt62219971:24000
Reedwest-Cabba-Bowery complex, 15 to 45 percent slopes947E1056155770572vmt62219971:24000
Bowery, rarely flooded-Meadowcreek, rarely flooded-Whitlash complex, 2 to 8 percent slopes270C50923927982l9x1mt6321:24000
Bowery-Lolo complex, 2 to 12 percent slopes12D16324862432pg4dmt6321:24000
Bowery-Meadowcreek-Whitlash complex, 2 to 8 percent slopes270C357113833721hfhxmt63720141:24000
Bowery-Lolo complex, 2 to 12 percent slopes12D1490637022pcw3mt63720141:24000
Enbar-Bowery-Nythar complex, 4 to 15 percent slopes512D11123775652kt1nmt63720141:24000
Winspect-Work-Bowery, 8 to 35 percent slopes, extremely bouldery419E13521499835125mt63920001:24000
Pianohill-Whitlash-Adel complex, 15 to 45 percent slopes411E1279149973511vmt63920001:24000
Castner-Laceycreek-Bowery complex 25 to 60 percent slopes397F870149958511cmt63920001:24000
Castner-Laceycreek-Bowery complex, 8 to 25 percent slopes397E807149957511bmt63920001:24000
Bowery-Nesda-Bonebasin complex, 2 to 15 percent slopes400D690149961511gmt63920001:24000
Work, very stony-Bowery complex, 8 to 35 percent slopes422E6611499875129mt63920001:24000
Work, stony-Bowery complex, 2 to 8 percent slopes422C6151499865128mt63920001:24000
Bowery clay loam, 0 to 4 percent slopes282B52214985250xymt63920001:24000
Cabba-Bowery complex, 2 to 60 percent slopes413E416149976511ymt63920001:24000
Sawicki, extremely bouldery-Bowery complex, 4 to 25 percent slopes421E2021499855127mt63920001:24000
Bowery loam, 2 to 15 percent slopes436D149150001512rmt63920001:24000
Absarokee-Bowery loams, 15 to 45 percent slopes364E1451499225106mt63920001:24000
Whitlash, very stony-Bowery-Shawmut, very stony complex, 2 to 70 percent slopes3608F3432697414rdq7mt6691:24000
Tolbert, very cobbly-Vershal, very cobbly-Bowery complex, 4 to 35 percent slopes5542E2108699261rgmtmt6691:24000
Shawmut, stony-Bowery-Gnojek, very stony complex, cool, 15 to 60 percent slopes801F16801017170134fymt6691:24000
Shawmut, very stony-Bowery-Bigbear, very stony complex, 4 to 45 percent slopes3541E1539655067pzn6mt6691:24000
Sawicki, very bouldery-Bowery-Whitlash, very cobbly complex, 15 to 60 percsent slopes7602F1305699357rgqxmt6691:24000
Work, very stony-Bowery complex, 8 to 35 percent slopes422E27424813592p91vmt6691:24000
Tolbert, stony-Blaincreek, stony-Bowery complex, cool, 35 to 60 percent slopes802F2211017171134fzmt6691:24000
Work, stony-Bowery complex, 2 to 8 percent slopes422C19924813582p91tmt6691:24000
Pianohill-Whitlash-Adel complex, 15 to 45 percent slopes411E88620232ntdhmt6691:24000
Enbar-Bowery-Nythar complex, 4 to 15 percent slopes512D85741462swk4mt6691:24000
Sawicki, extremely bouldery-Bowery complex, 4 to 25 percent slopes421E18620233ntdjmt6691:24000

Map of Series Extent

Approximate geographic distribution of the BOWERY 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 .