Official Series Description


Lab Data Summary

Aggregate lab data for the BEEFTRAIL soil series. This aggregation is based on all pedons with a current taxon name of BEEFTRAIL, 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 BEEFTRAIL 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 BEEFTRAIL 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 BEEFTRAIL 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 BEEFTRAIL 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 BEEFTRAIL 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 BEEFTRAIL 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 BEEFTRAIL 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 BEEFTRAIL 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 mountains figure.

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 BEEFTRAIL, 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 BEEFTRAIL 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
Beeftrail-Marcetta-Woodhurst families, complex, gentle mountain slopes521E475202404325y5qid75819981:24000
Minestope, very stony-Beeftrail, very stony-Rock outcrop complex, 8 to 30 percent slopes394E31616974891tzcqmt60420011:24000
Bearmouth-Beeftrail-Sebud families, complex, moderately steep mountain slopes538E48041486724zpwmt60520071:24000
Beeftrail-Marcetta-Woodhurst families, complex, gentle mountain slopes521E38851485974zmgmt60520071:24000
Libeg-Bearmouth-Beeftrail families, complex, glacial moraines348E36831485874zm4mt60520071:24000
Beeftrail-Bearmouth-Libeg families, complex, gentle mountain slopes528E34021486264zndmt60520071:24000
Tepecreek-Beeftrail-Bearmouth families, complex, gentle mountain slopes528X22911490525034mt60520071:24000
Bearmouth-Beeftrail-Marcetta families, complex, glacial moraines341E10371485754zlrmt60520071:24000
Shadow-Beeftrail-Sebud families, complex, gentle mountain slopes521P5991485984zmhmt60520071:24000
Beeftrail-Dinnen-Highrye complex, 8 to 45 percent slopes313E8185968820f4ymt60520071:24000
Tepecreek-Beeftrail-Bearmouth families, complex, gentle mountain slopes528X20925977525034mt61220111:24000
Shadow-Beeftrail-Sebud families, complex, gentle mountain slopes521P13725977014zmhmt61220111:24000
Beeftrail-Marcetta-Woodhurst families complex, gentle mountain slopes521E1517079871vb9cmt62319881:24000
Beeftrail-Stecum-Wissikihon complex, 8 to 25 percent slopes395E31517031631v58rmt63520061:24000
Beeftrail-Dinnen-Highrye complex, 15 to 45 percent slopes313E23917031351v57vmt63520061:24000
Highrye-Beeftrail complex, 4 to 15 percent slopes385D8517031601v58nmt63520061:24000
Beeftrail-Fleecer-Stecum complex, 8 to 45 percent slopes416E4817031671v58wmt63520061:24000
Beeftrail-Branham-Minestope complex, 2 to 15 percent slopes305D3517031321v57rmt63520061:24000
Minestope, very stony-Beeftrail, very stony-Rock outcrop complex, 8 to 30 percent slopes394E2017031621v58qmt63520061:24000
Beeftrail-Dinnen-Rock outcrop complex, 4 to 15 percent slopes380D3386362086d4s6mt67020071:24000
Beeftrail-Dinnen-Highrye complex, 8 to 45 percent slopes313E3373362388d52ymt67020071:24000
Highrye-Beeftrail-Oro Fino complex, 1 to 8 percent slopes383C2973362087d4s7mt67020071:24000
Beeftrail-Branham-Minestope complex, 2 to 15 percent slopes305D2415362085d4s5mt67020071:24000
Beeftrail, occasionally flooded-Adel-Monaberg complex, 4 to 15 percent slopes139D1350320493brhhmt67020071:24000
Minestope-Beeftrail, very bouldery-Nuley complex, 8 to 30 percent slopes405E1309362391d531mt67020071:24000
Minestope, very stony-Beeftrail, very stony-Rock outcrop complex, 8 to 30 percent slopes394E1234362094d4sgmt67020071:24000
Highrye-Beeftrail complex, 4 to 15 percent slopes385D1044362386d52wmt67020071:24000
Beeftrail-Stecum-Wissikihon complex, 8 to 25 percent slopes395E970362265d4yzmt67020071:24000
Beeftrail-Dinnen-Tuggle complex, 4 to 25 percent slopes357D671362383d52smt67020071:24000
Beeftrail, stony-Branham, stony-Fleecer complex, 8 to 20 percent slopes324E650362390d530mt67020071:24000
Typic Cryorthents, reclaimed area-Beeftrail, severely impacted complex, 4 to 30 percent slopes402E630843608x9v5mt67020071:24000
Beeftrail-Fleecer-Stecum complex, 8 to 45 percent slopes416E491909613zjjcmt67020071:24000
Beeftrail-Minestope-Dinnen complex, 4 to 25 percent slopes, moderately impacted404E287362105d4stmt67020071:24000
Philipsburg-Beeftrail, bouldery-Danielvil complex, 8 to 30 percent slopes301E266362089d4s9mt67020071:24000
Beeftrail-Bavdark-Zonite complex, 8 to 35 percent slopes321E207362389d52zmt67020071:24000
Highrye-Wissikihon-Beeftrail complex, 2 to 8 percent slopes353C160362099d4smmt67020071:24000
Rogert, extremely stony-Beeftrail, very stony complex, 5 to 30 percent slopes603691024554832nf44wy6301:24000

Map of Series Extent

Approximate geographic distribution of the BEEFTRAIL 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 .