Official Series Description


Lab Data Summary

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

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Soil series sharing subgroup-level classification with FOXOL, 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 FOXOL 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
Valmar-Warshod family, extremely stony surface-Foxol, very stony surface, complex, 30 to 60 percent slopes30021531636272x01lid70919761:24000
Valmar-Warshod family, extremely stony surface-Foxol, very stony surface, complex, 30 to 60 percent slopes30021831732342x01lid71019681:24000
Valmar-Warshod family, extremely stony surface-Foxol, very stony surface, complex, 30 to 60 percent slopes300237031732592x01lid71119831:24000
Hagenbarth-Foxol, very stony surface, complex, 2 to 25 percent slopes201012031733092x012id71220081:24000
Foxol, very stony surface-Warshod family, extremely stony surface, complex, 40 to 70 percent slopes, MLRA 43B201311431733102x015id71220081:24000
Foxol-Warshod family, complex, 45 to 80 percent slopes, extremely stony surface20143631733112x016id71220081:24000
Beehunt family-Povey-Foxol, very stony surface, complex, 30 to 55 percent slopes1019731732902w1g1id71220081:24000
Foxol, very stony surface-Povey complex, 50 to 65 percent slopes2008431733072x010id71220081:24000
Valmar-Warshod family, extremely stony surface-Foxol, very stony surface, complex, 30 to 60 percent slopes30022090929808872x01lid7131:24000
Valmar family-Warshod family, extremely stony surface-Foxol, very stony surface, complex, 30 to 60 percent slopes3003534629808882x01nid7131:24000
Beehunt family-Povey-Foxol, very stony surface, complex, 30 to 55 percent slopes1019324828994452w1g1id7131:24000
Foxol, extremely stony surface-Valmar, extremely stony surface-Lag family, complex, 10 to 35 percent slopes484186024326032mnb2id7131:24000
Foxol-Warshod family, complex, 40 to 70 percent slopes, extremely stony surface, MLRA 1320131385929808972x01tid7131:24000
Foxol, very stony surface-Povey complex, 50 to 65 percent slopes200873529808692x010id7131:24000
Hagenbarth-Foxol, very stony surface, complex, 2 to 25 percent slopes201055429808712x012id7131:24000
Northwater-Foxol, very stony surface-Vitale, extremely stony surface, complex, 50 to 80 percent slopes100-F53831634852yy4bid7131:24000
Primeaux-Foxol families, complex, 8 to 30 percent slopes82349927334332slqxid7131:24000
Foxol, very stony surface-Warshod family, extremely stony surface, complex, 40 to 70 percent slopes, MLRA 43B201345529808742x015id7131:24000
Foxol, very stony surface-Parkcity family, complex, 2 to 20 percent slopes88234727334942slsnid7131:24000
Foxol-Warshod family, complex, 45 to 80 percent slopes, extremely stony surface201430229808752x016id7131:24000
Foxol, very stony surface-Vitale, extremely stony surface complex, 20 to 55 percent slopes453909485290j8zjid71419971:24000
Northwater-Foxol, very stony surface-Vitale, extremely stony surface, complex, 50 to 80 percent slopes10087231635742yy4bid71419971:24000
Valmar-Warshod family, extremely stony surface-Foxol, very stony surface, complex, 30 to 60 percent slopes300211931733552x01lid71419971:24000
Valmar family-Warshod family, extremely stony surface-Foxol, very stony surface, complex, 30 to 60 percent slopes30034531733562x01nid71419971:24000
Valmar-Warshod family, extremely stony surface-Foxol, very stony surface, complex, 30 to 60 percent slopes30021231733832x01lid71519941:24000
Primeaux-Foxol families, complex, 8 to 30 percent slopes823141831634342slqxid7161:24000
Foxol, very stony surface-Vitale, extremely stony surface, complex, 20 to 55 percent slopes4521729841382v07vid7161:24000
Primeaux-Foxol families, complex, 8 to 30 percent slopes82333432389102slqxid77019681:24000
Foxol-Elzinga association, steepFHG11987481352j4whut60219691:20000
Foxol-Rock outcrop complex, 50 to 70 percent slopesFRG1400481353j4wjut60219691:20000
FOXOL ROCKY LOAM, 30 TO 60 PERCENT SLOPESFOG4907482717j69jut60319681:20000
Foxol extremely stony sandy loam, 30 to 60 percent slopesFFF4800503849jx96ut60419801:24000
Foxol very stony loam, 10 to 40 percent slopesFGE1340503850jx97ut60419801:24000
Foxol-Rock outcrop complex, 40 to 70 percent slopesFrG11715506547k037ut60919741:24000
Foxol-Durfee complex, 30 to 70 percent slopesFdG3360506546k036ut60919741:24000
St. Marys-Foxol association, very steepSMG2215482968j6kmut61219671:20000
Foxol-St. Marys association, very steepFOG2156482904j6hkut61219671:20000
Searla-Vickton-Foxol families, complex, 25 to 60 percent slopes, extremely stony1736922791246vkc2ut6511:24000
Foxol, very stony surface-Parkcity family, complex, 2 to 20 percent slopes882430834682slsnwy62319711:20000

Map of Series Extent

Approximate geographic distribution of the FOXOL 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 .