Official Series Description


Lab Data Summary

Aggregate lab data for the WHITESIDE soil series. This aggregation is based on all pedons with a current taxon name of WHITESIDE, 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 WHITESIDE were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
130B86P074586NC113025Whiteside6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.0991669,-83.2788925

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the WHITESIDE 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 WHITESIDE 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 WHITESIDE 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 WHITESIDE 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 WHITESIDE 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 WHITESIDE series and competing. 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 WHITESIDE 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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Soil series sharing subgroup-level classification with WHITESIDE, 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-2012-02-07-20 | Jackson County - June 1997

    Relationship of soils and landscape position in the Whiteside-Tuckasegee-Nikwasi general soil map unit (Soil Survey of Jackson County, North Carolina; June 1997).

  2. NC-2012-02-07-21 | Jackson County - June 1997

    Relationship of soils, aspect, and parent material in the Chandler-Fannin-Cashiers general soil map unit (Soil Survey of Jackson County, North Carolina; June 1997).

Map Units

Map units containing WHITESIDE 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
Tusquitee-Whiteside complex, 2 to 8 percent slopesTwB42116720991t3ypnc02120061:12000
Whiteside loam, 8 to 15 percent slopesWtC27016722151t42fnc02120061:12000
Whiteside loam, 2 to 8 percent slopesWtB22716722141t42dnc02120061:12000
Sylva-Whiteside complex, 2 to 8 percent slopes, rarely flooded800B3925092802p7yfnc08919741:20000
Tusquitee-Whiteside complex, 8 to 15 percent slopes100C3325091332p7nznc08919741:20000
Whiteside-Tusquitee complex, 2 to 8 percent slopes100B2125092742p7xznc08919741:20000
Wesser-Whiteside complex, 2 to 8 percent slopes, rarely flooded862B2025092812p7yjnc08919741:20000
Tuckasegee-Whiteside complex, 8 to 15 percent slopesTwC5942547115lc9wnc09919911:12000
Whiteside-Tuckasegee complex, 2 to 8 percent slopesWtB2581547127lcb8nc09919911:12000
Sylva-Whiteside complex, 0 to 2 percent slopesSyA792547109lc9pnc09919911:12000
Tuckasegee-Whiteside complex, 8 to 15 percent slopesTwC2133545878lb0znc11319901:12000
Tuckasegee-Whiteside complex, 2 to 8 percent slopesTwB548545877lb0ync11319901:12000
Sylva-Whiteside complex, 0 to 3 percent slopesSyA235545872lb0snc11319901:12000
Tusquitee-Whiteside complex, 2 to 8 percent slopesTwB12916714581t390nc11520061:12000
Whiteside loam, 2 to 8 percent slopesWtB12816715081t3bmnc11520061:12000
Wesser-Whiteside complex, 2 to 8 percent slopes, rarely flooded862B54225018582q8nhnc17519681:12000
Sylva-Whiteside complex, 2 to 8 percent slopes, rarely flooded800B25425018572q8ngnc17519681:12000
Whiteside-Tusquitee complex, 2 to 8 percent slopes100B18825018512q8nbnc17519681:12000
Tusquitee-Whiteside complex, 8 to 15 percent slopes100C9625017982q8n5nc17519681:12000
Alarka-Whiteside complex, 8 to 15 percent slopesAwC121532517kw3znc60520071:12000
Whiteside-Sylva complex, windswept, frigid, 2 to 8 percent slopes802B525091212pf5xnc60619911:12000
Alarka-Whiteside complex, 8 to 15 percent slopes, stonyAwC20557243lpvltn64020071:24000

Map of Series Extent

Approximate geographic distribution of the WHITESIDE 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 .