Official Series Description


Lab Data Summary

Aggregate lab data for the WAKE soil series. This aggregation is based on all pedons with a current taxon name of WAKE, 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 WAKE 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 WAKE 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 WAKE 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 WAKE 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 WAKE 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 WAKE 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 WAKE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the WAKE 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.

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 WAKE, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. NC-2010-09-28-03 | Cleveland County - 2006

    The relationship between soils and parent material in the Pacolet-Saw general soil map unit. The very deep Pacolet soils occur in areas away from stones, boulders, and rock outcrops. They formed in residuum from biotite gneiss and metamorphosed granite bedrock. The moderately deep Saw soils occur in stony or bouldery areas or near rock outcrops. They formed from residuum from metamorphosed granite bedrock (Soil Survey of Cleveland County, North Carolina; 2006).

Map Units

Map units containing WAKE 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
Ashlar-Rock outcrop-Wake complex, 2 to 10 percent slopesArC1901018571135x4ga03520031:24000
Ashlar-Wake complex, 15 to 25 percent slopesAwE1601018572135x5ga03520031:24000
Rock outcrop-Wake complex, 2 to 15 percent slopesRwD670640011pgzjga13519661:15840
Ashlar-Wake complex, 15 to 25 percent slopesAwE36522005222cvtlga20720071:24000
Wake-Ashlar-Rock outcrop complex, 2 to 15 percent slopesWaD9022005692cvw3ga20720071:24000
Wateree-Wake complex, 15 to 25 percent slopesWrE142525112252lnh6ga22320101:12000
Wateree-Wake complex, 6 to 10 percent slopesWrC78025112272lnh8ga22320101:12000
Wateree-Wake complex, 25 to 45 percent slopes, boulderyWrF51525112842p7dbga22320101:12000
Wateree-Wake complex, 10 to 15 percent slopesWrD32025112262lnh7ga22320101:12000
Rock outcrop-Wake-Wateree complex, 6 to 60 percent slopesRwF12025112312lnjbga22320101:12000
Rion-Ashlar-Wake complex, 10 to 25 percent slopesRaE5780127117488kga64519951:12000
Rion-Wateree-Wake complex, 2 to 10 percent slopesReC2350127118488lga64519951:12000
Wateree-Rock outcrop-Wake complex, 6 to 25 percent slopesWaE751747872t36xga65520121:24000
Rock outcrop-Wake complex, 2 to 8 percent slopesRwB651145573v6dnc00719991:24000
Saw-Wake complex, 15 to 30 percent slopes, very rockySaD6451170953xv8nc04520001:24000
Saw-Wake complex, 4 to 15 percent slopes, very rockySaC1391170943xv7nc04520001:24000
Wake-Saw-Wedowee complex, 2 to 8 percent slopes, rockyWaB266291126223s5znc06919971:24000
Wake-Wateree-Wedowee complex, 8 to 15 percent slopes, rockyWbD263011126233s60nc06919971:24000
Wake-Wateree complex, 15 to 30 percent slopes, very rockyWcE60761126243s61nc06919971:24000
Rock outcrop-Wake complex, 2 to 10 percent slopesRwC451126083s5jnc06919971:24000
Wake-Rolesville complex, 10 to 15 percent slopes, very rockyWaD836830502712xhbfnc18319661:24000
Wake-Rolesville complex, 15 to 25 percent slopes, very rockyWaE403130502722xhbgnc18319661:24000
Wake-Rolesville complex, 6 to 10 percent slopes, very rockyWaC178230502742xn3xnc18319661:24000
Wake-Rolesville complex, 2 to 6 percent slopes, very rockyWaB60730502732xn3wnc18319661:24000
Wake-Louisburg-Saw complex, 2 to 6 percent slopes, rockyWeB165024550052ndmqnc18520091:24000
Louisburg-Ashlar-Wake complex, 6 to 10 percent slopes, rockyLoC97724550032ndmnnc18520091:24000
Louisburg-Ashlar-Wake complex, 8 to 15 percent slopes, rockyLwC84724550042ndmpnc18520091:24000
Wake-Ashlar-Wedowee complex, 10 to 15 percent slopes, rockyWaD82824550372ndnrnc18520091:24000
Wake-Louisburg-Saw complex, 2 to 8 percent slopes, rockyWkB58024550062ndmrnc18520091:24000
Wake-Ashlar-Wedowee complex, 15 to 50 percent slopes, rockyWaF16524550382ndnsnc18520091:24000
Rock Outcrop-Wake complex, 2 to 8 percent slopesRwC11125138652lq39sc09120131:15840

Map of Series Extent

Approximate geographic distribution of the WAKE 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 .