Official Series Description


Lab Data Summary

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

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

Competing Series

Soil series competing with SAW 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 SAW 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 SAW 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.

Click the image to view it full size.

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

Soil series sharing subgroup-level classification with SAW, 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 SAW 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
Wedowee-Saw complex, 2 to 10 percent slopes, very boulderyWgC57514764551lkclal12320051:24000
Pacolet-Saw complex, 6 to 15 percent slopes, stonyPsD70201018602135y4ga03520031:24000
Pacolet-Saw complex, 15 to 25 percent slopes, stonyPsE15801018603135y5ga03520031:24000
Pacolet-Saw complex, 6 to 10 percent slopes, moderately eroded, boulderyPgC2568516723741t47kga12120071:12000
Urban land-Pacolet-Saw complex, 2 to 10 percent slopes, moderately eroded, boulderyUpC270016540381sj52ga12120071:12000
Pacolet-Saw complex, 15 to 45 percent slopes, stonyPsF1910640010pgzhga13519661:15840
Pacolet-Saw complex, 6 to 15 percent slopes, stonyPdD942522005562cvvpga20720071:24000
Pacolet-Saw complex, 15 to 25 percent slopes, stonyPdE481522005572cvvqga20720071:24000
Pacolet-Saw complex, 10 to 15 percent slopes, moderately eroded, boulderyLlD216351249792y778ga25519621:15840
Pacolet-Saw complex, 25 to 45 percent slopes, stonyPsF180924314122mm2nnc03519691:15840
Pacolet-Saw complex, 15 to 25 percent slopes, stonyPtD171801170893xv2nc04520001:24000
Pacolet-Saw complex, 8 to 15 percent slopes, moderately erodedPsC2142911170883xv1nc04520001:24000
Pacolet-Saw complex, 2 to 8 percent slopes, moderately erodedPsB258741170873xv0nc04520001:24000
Hulett-Saw complex, 4 to 15 percent slopes, very rockyHuC7861170713xthnc04520001:24000
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
Saw-Pacolet complex, 2 to 8 percent slopesSaB8441150153vp5nc15919961:24000
Saw-Pacolet complex, 8 to 15 percent slopesSaC6511150163vp6nc15919961:24000
Saw-Pacolet complex, 2 to 8 percent slopes, moderately erodedScB262024225802m9wrnc15919961:24000
Pacolet-Saw complex, 15 to 25 percent slopes, moderately erodedPsD273281176423ydxnc16119971:24000
Pacolet-Saw complex, 8 to 15 percent slopes, moderately erodedPsC260671176413ydwnc16119971:24000
Pacolet-Saw complex, 2 to 8 percent slopes, moderately erodedPsB227491176403ydvnc16119971:24000
Wedowee-Saw complex, 2 to 6 percent slopesWfB1428130502792xn42nc18319661:24000
Wake-Louisburg-Saw complex, 2 to 6 percent slopes, rockyWeB165024550052ndmqnc18520091:24000
Wake-Louisburg-Saw complex, 2 to 8 percent slopes, rockyWkB58024550062ndmrnc18520091:24000
Bethlehem-Saw complex, 6 to 10 percent slopesBaC45426787442r2t8sc08319651:20000
Pacolet-Saw complex, 10 to 15 percent slopesPsD44626788182r2tnsc08319651:20000
Urban Land-Hard Labor-Saw complex, 2 to 10 percent slopesUsC137725138732lq4fsc09120131:15840
Saw sandy loam, 2 to 6 percent slopesSaB112725138662lq3bsc09120131:15840

Map of Series Extent

Approximate geographic distribution of the SAW 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 .