Official Series Description


Lab Data Summary

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

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

Competing Series

Soil series competing with BORDENGULCH 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 BORDENGULCH 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 BORDENGULCH 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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Click the image to view it full size.

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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 BORDENGULCH, 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 BORDENGULCH 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
Bordengulch family-Coerock family, bouldery-Rock outcrop complex, 8 to 35 percent slopes2820E73602485043316lrmt6331:24000
Coerock, bouldery-Bordengulch families-Rock outcrop complex, 8 to 35 percent slopes820D2500428482742v5v6mt66320171:24000
Angelpeak-Bordengulch complex, 15 to 30 percent slopes7794BO697431206631sghgor60720181:24000
Towermountain-Angelpeak-Bordengulch complex, 0 to 15 percent slopes1328AO440231202711q718or60720181:24000
Bordengulch-Angelpeak complex, 0 to 15 percent slopes7558AO367131206212pgszor60720181:24000
Towermountain-Bordengulch complex, 0 to 30 percent slopes1321NO151331203832pg2gor60720181:24000
Angelpeak-Bordengulch complex, 30 to 60 percent slopes1322CO130431203841qyz5or60720181:24000
Vandamine-Bordengulch complex, 30 to 60 percent slopes7728CO130131206361sgdqor60720181:24000
Bordengulch-Angelpeak-Vandamine complex, 15 to 30 percent slopes7727BO9513120230qsqhor60720181:24000
Bordengulch-Angelpeak complex, 15 to 30 percent slopes7341BO77331206082pgssor60720181:24000
Angelpeak-Bordengulch complex, 0 to 15 percent slopes7794AO66331207861v6m6or60720181:24000
Bordengulch-Angelpeak-Blackgulch complex, 30 to 60 percent slopes7363CO54831206152pgswor60720181:24000
Angelpeak-Bordengulch-Rock outcrop complex, 30 to 60 percent slopes7361CO33831206131sgbjor60720181:24000
Angelpeak-Bordengulch-Rock outcrop complex, 15 to 30 percent slopes7361BO32231206121sgbhor60720181:24000
Angelpeak-Bordengulch-Blackgulch complex, 0 to 15 percent slopes7362AO31831206141sgbkor60720181:24000
Fruitcreek-Bordengulch-Rock outcrop complex, without serpentine, 30 to 60 percent slopes7568CO29431206251sgc9or60720181:24000
Bordengulch, shallow, gravelly silt loam, without serpentine, 0 to 15 percent slopes7563AO26131206231sgc4or60720181:24000
Bordengulch-Fruitcreek complex, without serpentine, 15 to 30 percent slopes7562BO22731206221sgc3or60720181:24000
Bordengulch-Vandamine-Rock outcrop complex, 60 to 90 percent slopes7808DO20231206721sghsor60720181:24000
Angelpeak-Bordengulch complex, sandstone substratum, frost, 0 to 15 percent slopes2012AF19731204241r00qor60720181:24000
Eastlakesbasin-Bordengulch complex, without serpentine, 0 to 15 percent slopes7566AO15131206241sgc7or60720181:24000
Angelpeak-Bordengulch complex, sandstone substratum, 30 to 60 percent slopes2012CO4931204251r00ror60720181:24000
Bordengulch-Angelpeak-Vandamine complex, 60 to 90 percent north slopes7727DN2731206351sgdpor60720181:24000
Vandamine-Bordengulch complex, 30 to 60 percent slopes7728CO145131224191sgdqor62620181:24000
Bordengulch-Angelpeak complex, 15 to 30 percent slopes7341BO44231223982pgssor62620181:24000
Bordengulch-Angelpeak-Vandamine complex, 15 to 30 percent slopes7727BO2623122089qsqhor62620181:24000
Bordengulch-Angelpeak complex, mass failure, 15 to 30 percent slopes7341BM14531223971sg9wor62620181:24000
Bordengulch-Angelpeak complex, 0 to 15 percent slopes7558AO10431224062pgszor62620181:24000
Bordengulch-Fruitcreek complex, without serpentine, 15 to 30 percent slopes7562BO1331224071sgc3or62620181:24000
Fruitcreek-Bordengulch-Rock outcrop complex, without serpentine, 30 to 60 percent slopes7568CO531224081sgc9or62620181:24000
Bordengulch-Angelpeak-Vandamine complex, 60 to 90 percent north slopes7727DN547624868911sgdpor63120181:24000
Bordengulch-Angelpeak-Vandamine complex, 15 to 30 percent slopes7727BO49942437485qsqhor63120181:24000
Vandamine-Bordengulch complex, 30 to 60 percent slopes7728CO139924374861sgdqor63120181:24000
Bordengulch-Rock outcrop-Eastlakesbasin complex, 30 to 60 percent slopes9366CR119724375261sgkgor63120181:24000
Angelpeak-Bordengulch complex, 15 to 30 percent slopes7794BO102424375051sghgor63120181:24000
Bordengulch-Rock outcrop-Eastlakesbasin complex, 60 to 90 percent slopes9366DR78124375271sgkhor63120181:24000
Bordengulch-Rock outcrop-Eastlakesbasin complex, 15 to 30 percent slopes9366BR59324375251sgkfor63120181:24000
Bordengulch-Angelpeak complex, 0 to 15 percent slopes7558AO47224868812pgszor63120181:24000
Angelpeak-Bordengulch-Blackgulch complex, 0 to 15 percent slopes7362AO21124868771sgbkor63120181:24000
Bordengulch-Fruitcreek complex, 0 to 15 percent slopes7737AO17424374931sgf0or63120181:24000
Angelpeak-Bordengulch complex, 30 to 60 percent slopes1322CO9224861841qyz5or63120181:24000
Towermountain-Angelpeak-Bordengulch complex, 0 to 15 percent slopes1328AO8824861861q718or63120181:24000
Towermountain-Bordengulch complex, 0 to 30 percent slopes1321NO2824861832pg2gor63120181:24000
Bordengulch-Angelpeak complex, 15 to 30 percent slopes7341BO724868752pgssor63120181:24000
Bordengulch-Angelpeak-Blackgulch complex, 30 to 60 percent slopes7363CO324868782pgswor63120181:24000
Vandamine-Bordengulch-Rock outcrop complex, 60 to 90 percent north slopes344114847412v5lor67019991:24000
Vandamine-Bordengulch complex, 30 to 60 percent north slopes34337847402v5kor67019991:24000

Map of Series Extent

Approximate geographic distribution of the BORDENGULCH 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 .