Official Series Description


Lab Data Summary

Aggregate lab data for the BUIST soil series. This aggregation is based on all pedons with a current taxon name of BUIST, 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 BUIST 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
1306N0926S2006ID081002Buist6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.5999451,-111.1452255

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BUIST 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 BUIST 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 BUIST 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 BUIST 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 BUIST 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 BUIST 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 BUIST 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 BUIST, 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 BUIST 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
Buist gravelly loam, 2 to 12 percent slopes12-B78632390692n4mid7031:24000
Ireland-Cedarhill-Buist complex, 10 to 45 percent slopes, MLRA 132200180832389522pdcgid71019681:24000
Buist-Ricrest-Cedarhill complex, 10 to 30 percent slopes310048632389532pt1qid71019681:24000
Buist gravelly silt loam, 1 to 4 percent slopes35437915425855j2id71220081:24000
Cedarhill-Buist complex, 10 to 30 percent slopes442093642336pkdjid71220081:24000
Buist-Arbone complex, 1 to 4 percent slopes3995615425955j3id71220081:24000
Buist gravelly silt loam, 4 to 12 percent slopes3687715426055j4id71220081:24000
Buist very gravelly silt loam, 1 to 4 percent slopes3870115426155j5id71220081:24000
Buist gravelly silt loam, dry, 4 to 12 percent slopes37213791544vknpid71220081:24000
Ricrest-Pontuge-Buist complex, 8 to 40 percent slopes70003430938862xxdhid7131:24000
Buist-Arbone complex, 0 to 4 percent slopes140A1725202385blyid7131:24000
Buist-Arbone complex, 10 to 30 percent slopes140F8296572020ffyid7131:24000
Ririe-Buist complex, 4 to 12 percent slopes1101654485578j98tid71519941:24000
Justesen-Ririe-Buist complex, 12 to 20 percent slopes58651485653j9c7id71519941:24000
Buist gravelly silt loam, 20 to 30 percent slopes16447485607j99rid71519941:24000
Ireland-Cedarhill-Buist complex, 10 to 45 percent slopes, MLRA 1322001893624845402pdcgid7161:24000
Buist-Ricrest-Cedarhill complex, 10 to 30 percent slopes3100774024954722pt1qid7161:24000
Dranyon-Ireland-Buist complex, 12 to 60 percent slopes500AA604124255162mdygid7161:24000
Buist-Arbone complex, 0 to 4 percent slopes140A26071591525blyid7161:24000
Hades-Calpac-Buist complex, 12 to 35 percent slopesBME2175599984n4bbid7161:24000
Buist gravelly silt loam, 4 to 12 percent slopes140G19101591555bm1id7161:24000
Buist-Arbone complex, 10 to 30 percent slopes140F1835185996720ffyid7161:24000
Ricrest-Pontuge-Buist complex, 8 to 40 percent slopes7000170830740342xxdhid7161:24000
Ireland-Cedarhill-Buist complex, 20 to 70 percent slopes, MLRA 43B7200110031364342ypjsid7161:24000
Buist-Arbone complex, cool, 0 to 4 percent slopes140AA53122471222ff9tid7161:24000
Buist gravelly silt loam, cool, 4 to 15 percent slopes140GG32722476492ffvtid7161:24000
Buist-Hondoho complex, 1 to 12 percent slopes, extremely stony surfaceTHX321186204820hm2id7161:24000
Buist-Arbone complex, cool, 10 to 30 percent slopes140FF10322476392ffvhid7161:24000
Buist-Lagall complex, 35 to 60 percent slopes1507408115043451jqid75819981:24000
Deecree-Buist complex, 0 to 1 percent slopesDBA9028093462mptkid75819981:24000
Simeroi-Buist complex, 5 to 30 percent slopesHBD8528093532mpx5id75819981:24000
Simeroi-Buist complex, 5 to 30 percent slopesHBD155324341252mpx5id76120181:24000
Shagel-Baldridge-Buist complex, 0 to 40 percent slopesBBE141224340242mpsxid76120181:24000
Small-Shagel-Buist complex, 4 to 35 percent slopesBSC101524340382mptcid76120181:24000
Deecree-Buist complex, 0 to 1 percent slopesDBA53524340442mptkid76120181:24000
Buist gravelly loam, 2 to 12 percent slopes12774789452n4mid76319981:24000
Ireland-Cedarhill-Buist complex, 10 to 45 percent slopes, MLRA 13220047732389902pdcgid77019681:24000
Dranyon-Ireland-Buist complex, 12 to 60 percent slopes500AA7732389792mdygid77019681:24000
McCollum-Buist family, stony-Downey, bouldery complex, 0 to 10 percent slopes1072504528482912v5vsmt63419881:24000

Map of Series Extent

Approximate geographic distribution of the BUIST 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 .