Official Series Description


Lab Data Summary

Aggregate lab data for the WATTERSON soil series. This aggregation is based on all pedons with a current taxon name of WATTERSON, 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 WATTERSON 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 WATTERSON 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 WATTERSON 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 WATTERSON 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 WATTERSON 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 WATTERSON 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 WATTERSON 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 WATTERSON 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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Click the image to view it full size.

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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with WATTERSON, 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 WATTERSON 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
Kilburn family-Watterson-Watterson wet association, 4 to 30 percent slopes227bo190022291532dtm5ca73219981:24000
Pass Canyon family-Watterson-Rock outcrop association, 0 to 30 percent slopes279bo171922291632dtmhca73219981:24000
Watterson family-Torriorthentic Haploxerolls complex, 5 to 15 percent slopes.4101689471511htn1ca73219981:24000
Watterson gravelly loamy sand, 0 to 4 percent slopes350bo87022291932dtngca73219981:24000
Watterson sandy loam, 0 to 4 percent slopes349bo48922291922dtnfca73219981:24000
Kilburn family-Watterson association, 4 to 15 percent slopes226bo39122291522dtm4ca73219981:24000
Watterson gravelly sandy loam, 4 to 15 percent slopes353bo36422291962dtnkca73219981:24000
Kilburn family-Watterson-Xerofluvents association, 0 to 8 percent slopes228bo29922291542dtm6ca73219981:24000
Watterson-Conway-Ulymeyer complex, 0 to 15 slopes slopes354bo6422291972dtnlca73219981:24000
Conway-Watterson complex, 0 to 2 percent slopes172bo4622291392dtlqca73219981:24000
Conway-Aquents-Watterson complex, 0 to 2 percent slopes169bo2022291372dtlnca73219981:24000
Watterson gravelly loamy sand, wet, 0 to 4 percent slopes351bo222291942dtnhca73219981:24000
Kilburn family-Watterson-Watterson wet association, 4 to 30 percent slopes227bo19922300532dvk6ca74019961:24000
Watterson gravelly loamy sand, 0 to 4 percent slopes3507525488312jd40ca80219961:24000
Conway-Aquents-Watterson complex, 0 to 2 percent slopes1692729488062jcvyca80219961:24000
Watterson sandy loam, 0 to 4 percent slopes3491788488311jd3zca80219961:24000
Watterson gravelly loamy sand, wet, 0 to 4 percent slopes3511117488313jd41ca80219961:24000
Watterson-Conway-Ulymeyer complex, 0 to 15 slopes slopes354655488316jd44ca80219961:24000
Watterson gravelly sandy loam, 0 to 2 percent slopes352653488314jd42ca80219961:24000
Kilburn family-Watterson association, 4 to 15 percent slopes226562488149jcyrca80219961:24000
Pass Canyon family-Watterson-Rock outcrop association, 0 to 30 percent slopes279539488227jd18ca80219961:24000
Conway-Watterson complex, 0 to 2 percent slopes172484488065jcw1ca80219961:24000
Kilburn family-Watterson-Watterson wet association, 4 to 30 percent slopes227459488151jcytca80219961:24000
Watterson gravelly sandy loam, 4 to 15 percent slopes353450488315jd43ca80219961:24000
Kilburn family-Watterson-Xerofluvents association, 0 to 8 percent slopes228371488153jcywca80219961:24000

Map of Series Extent

Approximate geographic distribution of the WATTERSON 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 .