Official Series Description


Lab Data Summary

Aggregate lab data for the BOXSPRING soil series. This aggregation is based on all pedons with a current taxon name of BOXSPRING, 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 BOXSPRING 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 BOXSPRING 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 BOXSPRING 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 BOXSPRING 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 BOXSPRING 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 BOXSPRING 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 BOXSPRING 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 BOXSPRING 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 BOXSPRING, 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 BOXSPRING 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
Boxspring-Umberci-Rock outcrop complex, 30 to 100 percent slopes313163543394079319rgca79520231:24000
Boxspring-Rock outcrop complex, 30 to 100 percent slopes3111374329210352wbt3ca79520231:24000
Boxspring-Umberci-Rock outcrop complex, 30 to 100 percent slopes31341153394084319rgca8051:24000
Boxspring-Rock outcrop complex, 30 to 100 percent slopes311281233940582wbt3ca8051:24000
Boxspring-Zeheme-Rock outcrop complex, 15 to 50 to percent slopes MLRA 30BZF191617124432vjqhnv60819671:24000
Boxspring-Seralin-Rock outcrop associationBSG109717124441vgy4nv60819671:24000
Boxspring-Rock outcrop associationBXR1222653883pyf0nv61119671:24000
Boxspring-Theriot-Rock outcrop association MLRA 29BTR5736538842whmcnv61119671:24000
Boxspring-Rock outcrop association1810967714781492v42rnv75419921:24000
Boxspring-Theriot-Rock outcrop association MLRA 291811269574781502whmcnv75419921:24000
Zeheme-Boxspring-Rock outcrop association106612546478028j1f8nv75419921:24000
Zaqua-Boxspring association183110476478154j1kbnv75419921:24000
Boxspring-Potosi-Rock outcrop association32253742468866hqwqnv75520061:24000
Boxspring-Scrapy-Rock outcrop association3233429715995461qpg8nv75520061:24000
Boxspring-Zeheme-Rock outcrop complex, 15 to 50 to percent slopes MLRA 30320292654688642vjqhnv75520061:24000
Zeheme-Rock outcrop-Boxspring association343777215987241qnlrnv75520061:24000
Boxspring-Seralin-Rock outcrop association3213703468865hqwpnv75520061:24000
Boxspring-Sheeppass association1515153124804472p83fnv75720111:24000
Mormonwell-Boxspring association2301235324804522p83lnv75720111:24000
Boxsprings-Scrapy-Rock outcrop association150957224804462p83dnv75720111:24000
Boxspring-Cruzspring-Lostleader association152486625171512qh57nv75720111:24000
Wamp-Boxspring-Nilesval association272398824804622p83xnv75720111:24000
Boxspring-Rock outcrop association1810494811762v42rnv78420061:24000
Boxspring-Zeheme-Rock outcrop complex, 15 to 50 to percent slopes MLRA 30132040746066502vjqhnv78519951:24000
Boxspring-Seralin-Rock outcrop association1321501469059hr2ynv78519951:24000
Boxspring-Zeheme-Rock outcrop complex, 15 to 50 to percent slopes MLRA 303201275116809972vjqhnv78819821:24000
Boxspring-Scrapy-Rock outcrop association323202516809981tf6rnv78819821:24000

Map of Series Extent

Approximate geographic distribution of the BOXSPRING 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 .