Official Series Description


Lab Data Summary

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the WATEREE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the WATEREE series and siblings. 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 WATEREE 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 .

Click the image to view it full size.

Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

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 WATEREE share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the WATEREE 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 WATEREE 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 .

Click the image to view it full size.

Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

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 WATEREE, 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 WATEREE 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
Louisburg-Wateree complex, 10 to 25 percent slopes2240303302042xpwtal08119791:20000
Wateree-Rion complex, 10 to 25 percent slopesLnE35301242062xpwsga06719691:15840
Wateree-Rock outcrop-Louisburg complex, 15 to 45 percent slopes, boulderyLDF13601242032xpwqga06719691:15840
Ashlar, Rion, and Wateree soils, 10 to 25 percent slopesARE10960640009pgzgga13519661:15840
Ashlar-Wateree complex, 15 to 45 percent slopes, stonyAsF3090639997pgz2ga13519661:15840
Wateree-Rion complex, 15 to 25 percent slopesWnE42052511224218cyga22320101:12000
Wateree-Rion complex, 10 to 15 percent slopesWnD20052511223218cxga22320101:12000
Wateree-Rion complex, 6 to 10 percent slopesWnC15552511222218ctga22320101:12000
Wateree-Wake complex, 15 to 25 percent slopesWrE142525112252lnh6ga22320101:12000
Wateree-Rion complex, 15 to 25 percent slopes, boulderyWeE80025112131tjqzga22320101:12000
Wateree-Wake complex, 6 to 10 percent slopesWrC78025112272lnh8ga22320101:12000
Crawfordville-Wateree complex, 6 to 15 percent slopesCrD67525112412m7ydga22320101:12000
Wateree-Wake complex, 25 to 45 percent slopes, boulderyWrF51525112842p7dbga22320101:12000
Wateree-Rion complex, 6 to 15 percent slopes, boulderyWeD49025112141tjr0ga22320101:12000
Sedgefield-Wateree complex, 2 to 10 percent slopesSeC47025112292lnhbga22320101:12000
Wateree-Wake complex, 10 to 15 percent slopesWrD32025112262lnh7ga22320101:12000
Wateree-Helena complex, 10 to 15 percent slopesWaD12525112352m7y5ga22320101:12000
Rock outcrop-Wake-Wateree complex, 6 to 60 percent slopesRwF12025112312lnjbga22320101:12000
Wateree-Helena complex, 6 to 10 percent slopesWaC10525112342m7y4ga22320101:12000
Rion-Wateree complex, 10 to 25 percent slopesLuE118451253192xn6jga60619731:20000
Wateree-Rion-Rock outcrop complex, 2 to 15 percent slopesWaD343526390932rj4nga63920121:24000
Rion-Wateree-Wake complex, 2 to 10 percent slopesReC2350127118488lga64519951:12000
Wateree-Rock outcrop-Wake complex, 6 to 25 percent slopesWaE751747872t36xga65520121:24000
Wateree-Rion-Wedowee complex, 15 to 25 percent slopesWcE27324335692mpb7nc06719701:15840
Wedowee-Wateree complex, 10 to 15 percent slopesWeD24924336482mpdsnc06719701:15840
Wedowee-Wateree complex, 6 to 10 percent slopesWeC18924336462mpdqnc06719701:15840
Wateree-Rion complex, 15 to 45 percent slopesWaF9924335622mpb0nc06719701:15840
Wedowee-Wateree complex, 2 to 6 percent slopesWeB9324336432mpdmnc06719701:15840
Wateree-Rion complex, 6 to 15 percent slopesWaD2924335652mpb3nc06719701:15840
Wake-Wateree-Wedowee complex, 8 to 15 percent slopes, rockyWbD263011126233s60nc06919971:24000
Wake-Wateree complex, 15 to 30 percent slopes, very rockyWcE60761126243s61nc06919971:24000
Wateree-Rion-Wedowee complex, 15 to 30 percent slopesWdE1341126253s62nc06919971:24000
Rion-Wateree-Wedowee complex, 8 to 15 percent slopesReD801126053s5fnc06919971:24000
Wateree-Rion-Wedowee complex, 15 to 30 percent slopesWaE8211127893sccnc07719931:24000
Rion-Wateree-Wedowee complex, 8 to 15 percent slopesRwD7671127823sc4nc07719931:24000
Louisburg (Wateree) sandy loam, 15 to 45 percent slopesLoF22391141153tr4nc13519751:20000
Louisburg (Wateree) sandy loam, 6 to 15 percent slopesLoC17071141143tr3nc13519751:20000
Louisburg (Wateree) loamy coarse sand, 15 to 40 percent slopesLoE40521176823yg6nc18119771:20000
Louisburg (Wateree) loamy coarse sand, 8 to 15 percent slopesLoD38011176813yg5nc18119771:20000
Louisburg (Wateree) loamy coarse sand, 2 to 8 percent slopesLoB20671176803yg4nc18119771:20000
Wateree-Rion complex, 15 to 40 percent slopesWaF45751322094fktsc02319771:20000
Wateree-Rion complex, 6 to 15 percent slopesWaD12951322084fkssc02319771:20000
Wateree sandy loam, 10 to 25 percent slopesWeE7021298904c50sc03719781:20000
Wateree-Rion complex, 15 to 40 percent slopesWaF208151299354c6gsc03919771:20000
Wateree-Rion complex, 6 to 15 percent slopesWaD90951299344c6fsc03919771:20000
Louisburg sandy loam, 10 to 25 percent slopesLoE2031310474dcbsc07719671:20000
Wateree sandy loam, 25 to 60 percent slopesWaF1731317854f44sc61519811:20000
Wateree-Rock outcrop complex, 25 to 70 percent slopes30E33612105441yzva03319961:24000
Pacolet-Wateree complex, 15 to 25 percent slopes30D694615874321q8vhva04920051:24000
Wateree sandy loam, 15 to 25 percent slopes42D258815874551q8w7va04920051:24000
Wateree sandy loam, 7 to 15 percent slopes42C98915874541q8w6va04920051:24000
Pacolet-Wateree complex, 25 to 45 percent slopes30E26915874331q8vjva04920051:24000
Wateree-Wedowee complex, 20 to 45 percent slopes44E13371401004pscva76020041:24000
Wateree sandy loam, 12 to 20 percent slopes43D10231400994psbva76020041:24000
Wateree-Wedowee-Rock outcrop complex, 45 to 60 percent slopes45F6211401014psdva76020041:24000
Wateree-Urban land complex, 4 to 12 percent slopes43C2471400984ps9va76020041:24000
Grover-Wateree-Urban land complex, 6 to 12 percent slopes20C21399944pnyva76020041:24000

Map of Series Extent

Approximate geographic distribution of the WATEREE 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 .