Official Series Description


Lab Data Summary

Aggregate lab data for the BENNETTCREEK soil series. This aggregation is based on all pedons with a current taxon name of BENNETTCREEK, 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 BENNETTCREEK 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
43C97P0543S1997OR023004BENNETTCREEK6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.6263885,-118.586113

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BENNETTCREEK 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 BENNETTCREEK 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 BENNETTCREEK 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 BENNETTCREEK 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 BENNETTCREEK 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 BENNETTCREEK 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 BENNETTCREEK 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 BENNETTCREEK, 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 BENNETTCREEK 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
Wonder-Bennettcreek-Rock outcrop complex, 0 to 15 percent slopes4118AO31925938851r0f3or60419881:24000
Pinuscreek-Bennettcreek complex, 30 to 60 percent slopes1708CO11025938731qzfvor60419881:24000
Bennettcreek-Limberjim-Klickson complex, 0 to 15 percent slopes5941AO133231205751r2k7or60720181:24000
Olot-Bennettcreek-Crackercreek complex, 15 to 30 percent slopes5967BO109331205851r2n2or60720181:24000
Crackercreek-Bennettcreek complex, 30 to 60 percent slopes5968CO45231205861r2n4or60720181:24000
Pinuscreek-Bennettcreek complex, 30 to 60 percent slopes1708CO9031203951qzfvor60720181:24000
Unitylake-Bennettcreek complex, 0 to 15 percent slopes3312AO2331204281r016or60720181:24000
Bennettcreek-Bocker complex, 0 to 15 percent slopes4171AO931203151qy06or60720181:24000
Bennettcreek-Fivebeaver complex, 0 to 15 percent slopes4173AO755531221421qxhgor62620181:24000
Crackercreek-Bennettcreek complex, 30 to 60 percent slopes5968CO571031223721r2n4or62620181:24000
Bennettcreek-Bigcow-Linecreek complex, 30 to 60 percent slopes4178CO543931221511qxwvor62620181:24000
Pinuscreek-Bennettcreek complex, 30 to 60 percent slopes1708CO497233853091qzfvor62620181:24000
Bennettcreek-Bocker complex, 0 to 15 percent slopes4171AO453331221551qy06or62620181:24000
Pinuscreek-Bennettcreek-McWillis complex, 30 to 60 percent slopes4175CO343931221021q6slor62620181:24000
Olot-Bennettcreek-Crackercreek complex, 15 to 30 percent slopes5967BO298931223711r2n2or62620181:24000
Pinuscreek-Bennettcreek complex, 15 to 30 percent slopes1708BO295033853081qzftor62620181:24000
Bocker-Bennettcreek complex, 0 to 15 percent slopes4170AO240031222851r0yqor62620181:24000
Bennettcreek-Bocker complex, 15 to 30 percent slopes4171BO187931222861r0yror62620181:24000
Bennettcreek-Olot-Fivebeaver complex, 15 to 30 percent slopes5907BO169231223601r2g0or62620181:24000
Anatone-Bennettcreek-Rock outcrop complex, 15 to 30 percent slopes1815BO52131222241qzzsor62620181:24000
Anatone-Bennettcreek complex, 15 to 30 percent slopes4185BO23831222931r0z7or62620181:24000
Pinuscreek-Bennettcreek complex, 15 to 30 percent slopes1708BO822724864621qzftor63120181:24000
Pinuscreek-Bennettcreek complex, 30 to 60 percent slopes1708CO651824864631qzfvor63120181:24000
Bennettcreek-Fivebeaver complex, 0 to 15 percent slopes4173AO323224868221qxhgor63120181:24000
Wonder-Bennettcreek-Rock outcrop complex, 0 to 15 percent slopes4118AO320924868121r0f3or63120181:24000
Unitylake-Bennettcreek complex, 0 to 15 percent slopes3312AO161524866391r016or63120181:24000
Bennettcreek-Bocker complex, 15 to 30 percent slopes4171BO1424372161r0yror63120181:24000
Bennettcreek-Limberjim-Klickson complex, 0 to 15 percent slopes5941AO40731214771r2k7or66719841:20000

Map of Series Extent

Approximate geographic distribution of the BENNETTCREEK 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 .