Official Series Description


Lab Data Summary

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

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

Competing Series

Soil series competing with STOTT KNOB 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 STOTT KNOB 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 STOTT KNOB 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.

Click the image to view it full size.

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 STOTT KNOB, 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-2010-09-28-10 | Surry County - 2007

    Relationship of soils, landscape, and geology in the Fairview general soil map unit and the Colvard and Suches general soil map unit (Soil Survey of Surry County, North Carolina; 2007).

  2. NC-2010-09-28-11 | Surry County - 2007

    Relationship of soils, landscape, and geology in the Fairview-Clifford general soil map unit (Soil Survey of Surry County, North Carolina; 2007).

Map Units

Map units containing STOTT KNOB 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
Stott Knob fine sandy loam, 15 to 45 percent slopesStF409324338152mpl5nc06719701:15840
Stott Knob fine sandy loam, 6 to 15 percent slopesStD70524338142mpl4nc06719701:15840
Rhodhiss-Stott Knob complex, 25 to 60 percent slopes, stonyRhF232024244982mcwmnc09720111:12000
Fairview-Stott Knob complex, 25 to 45 percent slopesFyF157424247172md3pnc09720111:12000
Stott Knob-Westfield complex, 25 to 60 percent slopes, stonySwF24424247102md3gnc09720111:12000
Rhodhiss, Fairview, and Stott Knob soils, 25 to 60 percent slopesRpE5140223890422l5zwnc16919921:24000
Stott Knob gravelly loam, 25 to 60 percent slopes, stonyStE18023890172l5z2nc16919921:24000
Stott Knob gravelly loam, 8 to 25 percent slopes, stonyStD17123890132l5yync16919921:24000
Fairview-Stott Knob complex, 25 to 45 percent slopesFsE1281414276241jxkdnc17120051:24000
Stott Knob gravelly loam, 25 to 45 percent slopes, stonyStE304014277011jxmwnc17120051:24000
Rhodhiss-Stott Knob complex, 25 to 45 percent slopes, stonyRsE290614276761jxm2nc17120051:24000
Fairview-Stott Knob complex, 25 to 45 percent slopes, stonyFtE280214276251jxkfnc17120051:24000
Rhodhiss-Stott Knob complex, 8 to 15 percent slopes, stonyRsC164914276771jxm3nc17120051:24000
Rhodhiss-Stott Knob complex, 15 to 25 percent slopes, stonyRsD160214276721jxlync17120051:24000
Meadowfield-Stott Knob complex, 25 to 45 percent slopes, very stonyMsE111314276481jxl5nc17120051:24000
Stott Knob gravelly loam, 15 to 25 percent slopes, stonyStD108014277001jxmvnc17120051:24000
Meadowfield-Stott Knob complex, 15 to 25 percent slopes, very stonyMsD67214276471jxl4nc17120051:24000
Stott Knob gravelly loam, 8 to 15 percent slopes, stonyStC55714277021jxmxnc17120051:24000
Meadowfield-Stott Knob complex, 8 to 15 percent slopes, very stonyMsC29414276501jxl7nc17120051:24000
Rhodhiss-Stott Knob complex, 2 to 8 percent slopes, stonyRsB17514276741jxm0nc17120051:24000
Fairview-Stott Knob complex, 25 to 45 percent slopesFsF412123979852lh9cnc19719601:15840
Fairview-Stott Knob complex, 25 to 45 percent slopes, moderately erodedFsF276223979872lh9fnc19719601:15840
Rhodhiss-Stott Knob complex, 15 to 25 percent slopes, stonyRdE27223985192lhvlnc19719601:15840
Rhodhiss-Stott Knob complex, 8 to 15 percent slopes, stonyRdD18923985182lhvknc19719601:15840
Rhodhiss-Stott Knob complex, 25 to 45 percent slopes, stonyRdF17223985202lhvmnc19719601:15840
Fairview-Stott Knob complex, 25 to 45 percent slopes, stonyFtF6423967412lg07nc19719601:15840
Stott Knob-Rhodhiss complex, 25 to 50 percent slopes36E209541367004l7pva00920041:24000
Stott Knob-Rhodhiss complex, 25 to 50 percent slopes, very stony37E110671367024l7rva00920041:24000
Stott Knob-Rhodhiss complex, 15 to 25 percent slopes36D21061366994l7nva00920041:24000
Stott Knob-Rhodhiss complex, 15 to 25 percent slopes, very stony37D7021367014l7qva00920041:24000
Hickoryknob-Rhodhiss-Stott Knob complex, 25 to 60 percent slopes22E11828581991mjlxva06720041:24000
Hickoryknob-Rhodhiss-Stott Knob complex, 15 to 25 percent slopes22D1835581989mjlvva06720041:24000
Hickoryknob-Rhodhiss-Stott Knob complex, 8 to 15 percent slopes22C778581988mjltva06720041:24000
Rhodhiss-Stott Knob complex, 25 to 45 percent slopes40E16013210867328s7qva14120081:24000
Fairview-Stott Knob complex, 25 to 45 percent slopes21E1075814741831lh09va14120081:24000
Meadowfield-Stott Knob complex, 25 to 45 percent slopes, very rocky32E635514738301lgmxva14120081:24000
Meadowfield-Stott Knob complex, 15 to 25 percent slopes, very stony31D172614738291lgmwva14120081:24000
Meadowfield-Stott Knob complex, 45 to 90 percent slopes, very rocky32F99214738311lgmyva14120081:24000
Meadowfield-Stott Knob complex, 8 to 15 percent slopes, very stony31C96914738281lgmvva14120081:24000
Fairview-Stott Knob complex, 25 to 45 percent slopes, very stony22E69314742071lh12va14120081:24000

Map of Series Extent

Approximate geographic distribution of the STOTT KNOB 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 .