Official Series Description


Lab Data Summary

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

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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 FOURBEAVER, 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 FOURBEAVER 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
Fourbeaver-Humarel-Canest complex, 0 to 15 percent slopes3372AO267131204401r02tor60720181:24000
Humarel-Meaufun-Fourbeaver complex, 15 to 30 percent slopes3378BO120431204451r03jor60720181:24000
Quirk-Fourbeaver complex, 0 to 15 percent slopes3437AO6431204581r059or60720181:24000
Fourbeaver-Humarel-Rock outcrop complex, 30 to 60 percent slopes3380CO6231204461r03kor60720181:24000
Humarel-Fourbeaver-Meaufun complex, 30 to 60 percent slopes3470CO5431204601r05jor60720181:24000
Sharpridge-Fourbeaver-Cougarrock complex, 0 to 15 percent slopes3474AO5231204611r05mor60720181:24000
Quirk-Fourbeaver-Humarel complex, 15 to 30 percent slopes3374BO1231204411r02wor60720181:24000
Anatone-Fourbeaver-Canest complex, 15 to 30 percent slopes1771BO279731222171qzz4or62620181:24000
Humarel-Fourbeaver-Meaufun complex, 30 to 60 percent slopes3470CO213831222631r05jor62620181:24000
Quirk-Fourbeaver-Humarel complex, 15 to 30 percent slopes3374BO194531222391r02wor62620181:24000
Humarel-Fourbeaver-Rock outcrop complex, 30 to 60 percent slopes3436CO118031222591r058or62620181:24000
Fourbeaver-Humarel-Canest complex, 0 to 15 percent slopes3372AO98431222371r02tor62620181:24000
Fourbeaver-Humarel-Rock outcrop complex, 30 to 60 percent slopes3380CO85231222421r03kor62620181:24000
Anatone-Canest-Fourbeaver complex, 0 to 15 percent slopes1812AO78831222221qzzqor62620181:24000
Meaufun-Grubcreek-Fourbeaver complex, 30 to 60 percent slopes3413CO72331221121q6zror62620181:24000
Quirk-Fourbeaver complex, 0 to 15 percent slopes3437AO62731222601r059or62620181:24000
Humarel-Meaufun-Fourbeaver complex, 15 to 30 percent slopes3378BO61831222411r03jor62620181:24000
Anatone-Fourbeaver-Canest complex, 30 to 60 percent slopes1771CO40231225141v6bwor62620181:24000
Sharpridge-Fourbeaver-Cougarrock complex, 0 to 15 percent slopes3474AO16531222641r05mor62620181:24000
Humarel-Meaufun-Fourbeaver complex, slump, 2 to 50 percent slopes4092XO9333853542sz5zor62620181:24000
Humarel-Meaufun-Fourbeaver complex, mass failure, 15 to 30 percent slopes3378BM5231222401r03hor62620181:24000
Meaufun-Grubcreek-Fourbeaver complex, mass failure, 30 to 60 percent slopes3413CM4531222481r04qor62620181:24000
Humarel-Fourbeaver-Meaufun complex, landslide, 30 to 60 percent slopes3470CL3031222621r05hor62620181:24000

Map of Series Extent

Approximate geographic distribution of the FOURBEAVER 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 .