Official Series Description


Lab Data Summary

Aggregate lab data for the DELLWOOD soil series. This aggregation is based on all pedons with a current taxon name of DELLWOOD, 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 DELLWOOD 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
130B86P075286NC087007Dellwood6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.4422226,-83.0058365
130B88P087888NC121004Dellwood6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.0519447,-82.1208344
130B88P086988NC199002Dellwood6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.7583351,-82.2086105
130B00P1347S2000NC021003Dellwood6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.7591667,-82.3708344

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DELLWOOD 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 DELLWOOD 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 DELLWOOD 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 DELLWOOD 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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Click the image to view it full size.

Click the image to view it full size.

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Competing Series

Soil series competing with DELLWOOD 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 DELLWOOD 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 DELLWOOD 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 DELLWOOD, 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-2012-02-07-07 | Clay County - 1998

    Typical relationship of soils, aspect, landscape position, and parent material in the Edneyville-Plott-Chestnut-Cullasaja general soil map unit in the intermediate mountains (Soil Survey of Clay County, North Carolina; 1998).

  2. NC-2012-02-07-17 | Haywood County Area - October 1997

    Typical relationship between soils, aspect, landscape position, and parent material of intermediate mountains in an area of the Plott-Edneyville-Chestnut general soil map unit (Soil Survey of Haywood County Area, North Carolina; October 1997).

  3. NC-2012-02-07-19 | Jackson County - June 1997

    Relationship of soils, aspect, parent material, and landscape position in the Plott-Edneyville-Chestnut-Cullasaja soil map unit (Soil Survey of Jackson County, North Carolina; June 1997).

  4. NC-2012-02-07-22 | Jackson County - June 1997

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

Map Units

Map units containing DELLWOOD 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
Dellwood cobbly sandy loam, 1 to 5 percent slopes, occasionally floodedDeB926548063ld9gnc01119971:12000
Dellwood-Reddies complex, 0 to 3 percent slopes, occasionally floodedDeA161316720021t3vknc02120061:12000
Dellwood gravelly fine sandy loam, 0 to 5 percent slopes, occasionally floodedDeB15072423110lbkwnc03920091:12000
Reddies-Dellwood complex, 0 to 3 percent slopes, occasionally floodedRdA115324231462mbh0nc03920091:12000
Reddies-Dellwood-Urban land complex, 0 to 3 percent slopes, occasionally floodedRnA15524231472mbh1nc03920091:12000
Dellwood gravelly fine sandy loam, 0 to 5 percent slopes, occasionally floodedDgB1072546402lbkwnc04319911:12000
Dellwood-Reddies complex, 0 to 5 percent slopes, occasionally floodedDeB14171912745226cgnc07520071:12000
Dellwood-Reddies complex, 0 to 3 percent slopes, occasionally flooded1432425091272p7n3nc08919741:20000
Dellwood gravelly fine sandy loam, 0 to 3 percent slopes, occasionally floodedDfA1128547059lc82nc09919911:12000
Dellwood gravelly fine sandy loam, 0 to 5 percent slopes, frequently floodedDgB518545821l9z4nc11319901:12000
Dellwood-Reddies complex, 0 to 3 percent slopes, occasionally floodedDeA134316713421t358nc11520061:12000
Dellwood-Reddies complex, 0 to 3 percent slopes, occasionally floodedDeA999547559lcs6nc12119971:12000
Dellwood-Reddies complex, 0 to 3 percent slopes, occasionally flooded14135525017922q8n4nc17519681:12000
Dellwood-Reddies complex, 0 to 5 percent slopes, occasionally floodedRs112323903932l7dgnc17519681:12000
Dellwood cobbly sandy loam, 1 to 5 percent slopes, occasionally floodedDeB2391529732ks74nc18920011:12000
Dellwood-Reddies complex, 0 to 3 percent slopes, occasionally floodedDeA2984547834ld22nc19919971:12000
Reddies-Dellwood complex, 0 to 3 percent slopes, occasionally floodedRdA330556310lnwhnc60520071:12000
Dellwood-Smokemont complex, 0 to 5 percent slopes, occasionally floodedDfB319556268lnv4nc60520071:12000
Dellwood-Wesser complex, 0 to 5 percent slopes, occasionally floodedDgB145755850tcj8nc60520071:12000
Dellwood cobbly sandy loam, 0 to 3 percent slopes, occasionally floodedDeA2913546758lbycnc60619911:12000
Dellwood-Urban land complex, 0 to 3 percent slopes, occasionally floodedDhA1039546759lbydnc60619911:12000
Dellwood-Reddies complex, windswept, frigid, 0 to 3 percent slopes, rarely flooded24225091202pf5nnc60619911:12000
Dellwood-Smokemont complex, 0 to 5 percent slopes, frequently floodedDg2116553581ll1gtn64020071:24000
Dellwood-Wesser complex, 0 to 5 percent slopes, frequently floodedDhB691188375521769tn64020071:24000
Reddies-Dellwood complex, 0 to 5 percent slopes, frequently floodedRd550553587ll1ntn64020071:24000
Dellwood-Smokemont-Urban land complex, 0 to 5 percent slopes, occasionally floodedDd53557322lpy4tn64020071:24000
Cullasaja-Tuckasegee-Dellwood complex, 0 to 15 percent slopes, very stony14C362581971mjl8va06720041:24000
French-Dellwood complex, 0 to 4 percent slopes, frequently flooded27A102814740291lgvbva14120081:24000
Nikwasi-Dellwood complex, 0 to 4 percent slopes, frequently flooded35A62014738061lgm4va14120081:24000

Map of Series Extent

Approximate geographic distribution of the DELLWOOD 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 .