Official Series Description


Lab Data Summary

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

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BICKMORE 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 BICKMORE 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 BICKMORE 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 BICKMORE 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 BICKMORE 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 BICKMORE 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 BICKMORE 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 BICKMORE, 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 BICKMORE 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
Bickmore family, stony surface-Broad Canyon, very stony surface-Stringam complex, 30 to 75 percent slopes9644531732842wxblid71220081:24000
Bickmore, low effective precipitation-McCadden, very stony surface-Bickmore families, complex, 40 to 75 percent slopes920487627335052slt1id7131:24000
Bickmore family, stony surface-Broad Canyon, very stony surface-Stringam complex, 30 to 75 percent slopes964331329682372wxblid7131:24000
Bickmore-Parkcity-Starley families, complex, 15 to 60 percent slopes984197729638832wv3bid7131:24000
Bickmore, very bouldery surface-Goodski, rubbly surface, families, complex, 40 to 70 percent slopes841186427334512slrnid7131:24000
Namela, extremely stony surface-Bickmore families, complex, 40 to 75 percent slopes842158627334522slrpid7131:24000
Bickmore-Nieman, extremely stony surface, families, complex, 35 to 70 percent slopes884104227334962slsqid7131:24000
Nieman family-Rock outcrop-Bickmore family, low effective precipitation, complex, 45 to 80 percent slopes854103727334642sls4id7131:24000
Bickmore family, 40 to 85 percent slopes83661427334462slrhid7131:24000
Bickmore-Lionhead-Sponsor families, complex, 5 to 20 percent slopes99259329638742wv30id7131:24000
Nieman family-Rock outcrop-Bickmore family, low effective precipitation, complex, 45 to 80 percent slopes85424131634412sls4id7161:24000
Bickmore family, 40 to 85 percent slopes83615931634362slrhid7161:24000
Bickmore family, stony surface-Broad Canyon, very stony surface-Stringam complex, 30 to 75 percent slopes9642231634802wxblid7161:24000
Nieman family-Rock outcrop-Bickmore family, low effective precipitation, complex, 45 to 80 percent slopes85463028586532sls4id75819981:24000
Namela, extremely stony surface-Bickmore families, complex, 40 to 75 percent slopes84231228586482slrpid75819981:24000
Bickmore, very bouldery surface-Goodski, rubbly surface, families, complex, 40 to 70 percent slopes841128586472slrnid75819981:24000
Farlow, extremely stony-McCadden, rubbly-Bickmore, stony families, complex, 20 to 70 percent slopes6361G9231692642v11bmt60019691:24000
Helmville, stony-Bickmore, stony, Geemore-very stony families, complex, 35 to 70 percent slopes6362G729428324572v11cmt6321:24000
Farlow, extremely stony-McCadden, rubbly-Bickmore, stony families, complex, 20 to 70 percent slopes6361G577628324562v11bmt6321:24000
Dranburn-Bickmore-Elkwalow families, complex, 4 to 30 percent slopes6345E189129110382w757mt6321:24000
Lostminer-McCadden-Bickmore complex, 4 to 40 percent slopesDOC1351014230791jrtsut0131:24000
Ridgecrest-Bickmore families association, 30 to 60 percent slopes7028335481282j4t7ut60119851:24000
Nielsen-Bickmore families-Rock outcrop association, 20 to 60 percent slopes5419021481264j4snut60119851:24000
Bickmore-Eyre families-Rock outcrop association, 30 to 60 percent slopes612495481270j4svut60119851:24000
Bickmore-Nielsen families association, 5 to 45 percent slopes711850481281j4t6ut60119851:24000
Datemark-Bickmore, cool-Nielsen families complex, 20 to 60 percent slopes2411224481231j4rlut60119851:24000
Bickmore loam, 50 to 70 percent slopesBCG566481323j4vkut60219691:20000
BICKMORE-SHEEP CREEK ASSOCIATION, ERODEDBLG28423482675j685ut60319681:20000
DESPAIN-BICKMORE ASSOCIATIONDPG1772482707j696ut60319681:20000
BICKMORE-AGASSIZ ASSOCIATION, ERODEDBKG21338482674j684ut60319681:20000
BICKMORE GRAVELLY SILT LOAM, 30 TO 70 PERCENT SLOPESBGG747482673j683ut60319681:20000
Bickmore family-Senchert family complex, 2 to 20 percent slopes242A1575512454k67sut6461:24000
Behanin-Adel-Bickmore families association, 15 to 60 percent slopes107581631mj79ut6491:24000
Behanin-Bickmore-Condie families complex, 15 to 70 percent slopes108581632mj7but6491:24000
Behanin family-Rock outcrop-Bickmore family complex, 15 to 60 percent slopes109581633mj7cut6491:24000
Bickmore-Condie families association, 15 to 60 percent slopes112581636mj7gut6491:24000
Bickmore-Elwood-Behanin families complex, 5 to 20 percent slopes113581638mj7jut6491:24000
Castino-Sessions-Bickmore families association, 15 to 70 percent slopes124581640mj7lut6491:24000
Wildcow family-Bickmore family, extremely stony complex, 10 to 40 percent slopes961181815247wcb9ut6511:24000
Bickmore-Parkcity-Starley families, complex, 15 to 60 percent slopes9844330834922wv3bwy62319711:20000
Bickmore-Nieman, extremely stony surface, families, complex, 35 to 70 percent slopes884030834692slsqwy62319711:20000

Map of Series Extent

Approximate geographic distribution of the BICKMORE 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 .