Official Series Description


Lab Data Summary

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

There are insufficient data to create the 2D hillslope position figure.

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 BEELEM, 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 BEELEM 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
Gabbvally-Beelem-Rock outcrop association656ec129723906342v434ca76319841:24000
Beelem-Rock outcrop complex, 15 to 50 percent slopesBR776433812whpdnv61119671:24000
Vinini-Beelem-Gabbvally associationVBG44534956482v41gnv62219721:24000
Petspring-Uripnes-Beelem association12919940476747j02ynv77419851:24000
Stewval-Beelem association415688404769452s21gnv77419851:24000
Lomoine-Beelem-Rock outcrop association18256778476814j053nv77419851:24000
Beelem-Bellehelen-Stewval association60944769477012j0chnv77419851:24000
Gabbvally-Beelem-Rock outcrop association136632124767702v434nv77419851:24000
Chill-Beelem-Rock outcrop association12812950476743j02tnv77419851:24000
Brier-Beelem-Wassit association41902296476970j0b4nv77419851:24000
Armoine-Beelem association701020424770162v42dnv77419851:24000
Beelem-Wassit association609218724770102w4cmnv77419851:24000
Stewval-Beelem association1220165274807052s21gnv78119941:24000
Armoine-Beelem association218074634808552v42dnv78119941:24000
Vinini-Beelem-Gabbvally association162142494807922v41gnv78119941:24000
Stewval-Beelem association3220752684809302s21gnv78319911:24000
Stewval-Gabbvally-Beelem association322840090480935j4g1nv78319911:24000
Gabbvally-Stewval-Beelem association310227426480904j4f1nv78319911:24000
Stewval-Beelem-Bellehelen association322420694480933j4fznv78319911:24000
Beelem-Rock outcrop complex, 15 to 50 percent slopes3710205504810312whpdnv78319911:24000
Gabbvally-Beelem-Rock outcrop association65638094851122v434nv79619841:63360
Beelem-Rock outcrop-Bellehelen association10501824484895j8ksnv79619841:63360
Beelem-Wassit association21014314776162w4cmnv79919911:24000
Beelem-Bluegulch, rubbly families, complex, 3 to 25 percent slopes6B4458791072vk5gut6511:24000

Map of Series Extent

Approximate geographic distribution of the BEELEM 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 .