Official Series Description


Lab Data Summary

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

Soil series competing with WATKINS RIDGE 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 WATKINS RIDGE 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 WATKINS RIDGE 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 WATKINS RIDGE, 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 WATKINS RIDGE 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
Watkins Ridge-Bancroft-Ririe, very deep, complex, 5 to 15 percent slopes22003732389692pdd2id71119831:24000
Lilcan-Watkins Ridge, dry-Jacanyon complex, 8 to 50 percent slopes13895815451455sbid71220081:24000
Watkins Ridge gravelly silt loam, dry, 4 to 12 percent slopes227523791747vkw7id71220081:24000
Watkins Ridge family-Pyrenees family-Preussrange complex, 20 to 55 percent slopes200225231733052x00vid71220081:24000
Bancroft-Watkins Ridge-Cloudless complex, 4 to 15 percent slopes35445729844082xyfpid71220081:24000
Cavemountain-Watkins Ridge family, complex, 25 to 55 percent slopes2000831733032x00sid71220081:24000
Watkins Ridge family-Pyrenees family-Preussrange complex, 20 to 55 percent slopes2002347629808642x00vid7131:24000
Cavemountain-Watkins Ridge family, complex, 25 to 55 percent slopes2000123829808622x00sid7131:24000
Bezzant-Watkins Ridge-Drage complex, 12 to 50 percent slopes5520162131365442ypjvid7161:24000
Watkins Ridge-Bancroft-Ririe, very deep, complex, 5 to 15 percent slopes222093824845592pdd2id7161:24000
Watkins Ridge-Echocreek-Canburn, occasionally flooded complex, 1 to 8 percent slopesRPB219414803051lpcsut0131:24000
Despain-Bezzant, extremely stony-Watkins Ridge complex, 4 to 50 percent slopesEPD110314605481l0tgut0131:24000
Watkins Ridge gravelly loam, 4 to 25 percent slopes, very stonyWVD544749046t4fsut0131:24000
Heiseton, occasionally flooded-Watkins Ridge-Labenzo, occasionally flooded complex, 0 to 4 percent slopesYVB17914857791lw2cut0131:24000
Soberville-Watkins Ridge-Phage association, 4 to 25 percent slopesULD14414804861lpkmut0131:24000
Watkins Ridge-Clegg complex, 6 to 15 percent slopesWLC4480504309jxs1ut62219671:24000
Deer Creek-Watkins Ridge complex, 15 to 25 percent slopesDWD3286504231jxpjut62219671:24000
Watkins Ridge-Deer Creek complex, 15 to 25 percent slopesWND2392504312jxs4ut62219671:24000
Watkins Ridge silt loam, 6 to 15 percent slopesWcC1208504317jxs9ut62219671:24000
Deer Creek-Watkins Ridge complex, 6 to 15 percent slopesDWC846504230jxphut62219671:24000
Watkins Ridge-Clegg complex, 15 to 25 percent slopesWLD768504310jxs2ut62219671:24000
Watkins Ridge silt loam, 15 to 25 percent slopesWcD455504318jxsbut62219671:24000
Watkins Ridge-Deer Creek complex, 6 to 15 percent slopesWNC392504311jxs3ut62219671:24000
Watkins Ridge silt loam, 1 to 6 percent slopesWhB1430482362j5y2ut62719711:24000
Watkins Ridge stony loam, high rainfall, 4 to 25 percent slopesWGD805482361j5y1ut62719711:24000
Wye-Atepic-Watkins Ridge families complex, 20 to 60 percent slopes223A8316331284030gvhut6451:24000
Bradshaw-Watkins Ridge families complex, 30 to 60 percent slopes2236201331283930gvgut6451:24000
McCarey-Everry-Watkins Ridge families complex, 8 to 25 percent slopes30C2474791111vk6qut6511:24000
Watkins Ridge cobbly loam, 2 to 15 percent slopesCND60122306932dw6vut6511:24000
Bancroft-Watkins Ridge-Cloudless complex, 4 to 15 percent slopes354429253022xyfpwy7231:24000

Map of Series Extent

Approximate geographic distribution of the WATKINS RIDGE 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 .