Official Series Description


Lab Data Summary

Aggregate lab data for the BREGAR soil series. This aggregation is based on all pedons with a current taxon name of BREGAR, 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 BREGAR 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
2582P075582ID073002BREGAR4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1202774,-116.723053

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BREGAR 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 BREGAR 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 BREGAR 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 BREGAR 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 BREGAR 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 BREGAR 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 BREGAR 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 terrace figure.

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

Soil series sharing subgroup-level classification with BREGAR, 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 BREGAR 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
Bregar-Cavin-Brownsbowl association321701513871421hkfjca68520061:24000
Bregar extremely cobbly loam, 2 to 8 percent slopes320333213871401hkfgca68520061:24000
Bregar-Slinger families-Rock outcrop, metasedimentary complex, 30 to 60 percent slopes.11719670471533htnrca76319841:24000
Basket-Bregar families complex, 15 to 30 percent slopes.1085767471524htngca76319841:24000
Simpson-Hartig-Bregar families association, 30 to 60 percent slopes.161255471577htq5ca76319841:24000
Sharesnout-Bregar-Coser complex, 5 to 35 percent slopes15131241485997j9qbid67519921:24000
Wickahoney-Parkay-Bregar complex, 3 to 50 percent2056732486118j9v7id67519921:24000
Sharesnout-Bregar complex, 5 to 35 percent slopes1504253485995j9q8id67519921:24000
Doodlelink-Bregar-Sharesnout complex, 5 to 40 percent slopes483805486204j9y0id67519921:24000
Parkay-Bregar complex, 5 to 25 percent slopes1203655485930j9n5id67519921:24000
Lerrow-Cotant-Bregar association72323726339892rhhfnv62119711:24000
Bregar-Sumine-Rock outcrop association18037325477123j0h2nv76319861:24000
Bregar-Deseed-Linkup association18056660477124j0h3nv76319861:24000
Bregar, moderately steep-Bregar-Carstump association18004865477121j0h0nv76319861:24000
Alyan, steep-Bregar-Alyan association20013770477161j0j9nv76319861:24000
Bregar-Ninemile-Pequop association18023675477122j0h1nv76319861:24000
Chen-Bregar-Ramires association18752750477141j0hnnv76319861:24000
Chen-Bregar-Loncan association18772000477143j0hqnv76319861:24000
Bregar-McIvey-Cotant association18084639478779j26hnv76719861:24000
Bregar-Bregar, eroded-McIvey association18072446478778j26gnv76719861:24000
Yuko-Tuffo-Bregar association7611910478995j2fgnv76719861:24000
Bregar-Sumine-Hapgood association18051622478776j26dnv76719861:24000
Bregar-Graley-Chen association18061508478777j26fnv76719861:24000
Lerrow-Cotant-Bregar association7231502478992j2fcnv76719861:24000
Cotant-Bregar-Donna association18221061478783j26mnv76719861:24000
Chen-Bregar-Loncan association1877672478797j272nv76719861:24000
Bregar family, 2 to 15 percent slopes2082629476858j06jnv77419851:24000
Roca-Glean-Bregar association8757220479739j36gnv77519851:24000
Bregar-Roca-Quarz association34325065479630j32ynv77519851:24000
Graley-Loncan-Bregar association12634720479443j2wxnv77519851:24000
Cleavage-Rubble land-Bregar association15323830479478j2y1nv77519851:24000
Bregar-Punchbowl association34333625479631j32znv77519851:24000
Locane-Robson-Bregar association35603025479636j334nv77519851:24000
Wiskan-Roca-Bregar association12123000479437j2wqnv77519851:24000
Roca-Bregar-Linrose association900160026339562rhgdnv77519851:24000
Bregar-Jivas-Duff association97241001479914j3d3nv77619831:63360
Quarz-Bregar-Duff association8127045479890j3cbnv77619831:63360
Bregar-Fortank-Jivas association9715040479913j3d2nv77619831:63360
Cherry Spring variant-Tomera-Bregar association5654220479857j3b8nv77619831:63360
Bregar variant-Hymas-Quarz association9751115479915j3d4nv77619831:63360
Roca-Bregar-Linrose association90014189475973hz8znv77719931:24000
Dutchjohn-Cleavage bregar association12559290475462hyrhnv77719931:24000
Cleavage-Burrita-Bregar association8817650475964hz8pnv77719931:24000
Bregar-Tusel-Cleavage association1226474475455hyr8nv77719931:24000
Udelope-Bregar-Rock outcrop association8003495475929hz7knv77719931:24000
Bregar-Tusk association1201259475447hyr0nv77719931:24000
Bregar-Erakatak-Mahogee complex, 0 to 15 percent slopes461907429868542wz5hor64420211:24000
Ninemile-Bregar-Reluctan associationfnv553775229868722wz5vor64420211:24000
Erakatak-Chen-Bregar complex, 2 to 15 percent slopes445593729868522wz5for64420211:24000
Oreneva-Bregar-Rock outcrop complex, 2 to 10 percent slopes423300029868312wbjfor64420211:24000
Bregar-Rubble land complex, 0 to 35 percent slopes439165729868382wbjqor64420211:24000
Boost-Bregar complex, 0 to 15 percent slopes459118429868622x2m0or64420211:24000
Sharesnout-Bregar complex, 5 to 35 percent slopesID015037624872272ph54or64420211:24000
Ninemile-Anawalt-Bregar associationfnv5503629868712wz5ror64420211:24000
Bregar family-Duco family, stony-Rock outcrop complex, 15 to 75 percent slopes117581643mj7put6491:24000
Dacore-Breger-Bluecrest families complex, 10 to 60 percent slopes136581652mj7zut6491:24000

Map of Series Extent

Approximate geographic distribution of the BREGAR 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 .