Official Series Description


Lab Data Summary

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

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
130B02N102602NC173009Fannin7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.3845497,-83.4359973
130B04N049403NC021006Fannin6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.5206375,-82.4367828
130B87P082687NC199003Fannin6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.9133339,-82.2669449
130B91P021590NC121002Fannin7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.8841667,-82.003891
130B00P0683S2000NC021004Fannin6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.5233345,-82.4241638
130B00P0684S2000NC021005Fannin6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.5122223,-82.4483337
130B00P0685S2000NC021006Fannin6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.4650002,-82.4794464
130B00P0686S2000NC021007Fannin6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.4700012,-82.4855576
n/a90P039190NC099001Fannin6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FANNIN 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 FANNIN 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 FANNIN 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 FANNIN 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.

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.

Competing Series

Soil series competing with FANNIN 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 FANNIN 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 FANNIN 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 FANNIN, 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-2012-02-07-21 | 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 FANNIN 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
Fannin fine sandy loam, 10 to 25 percent slopesFaE2817012565746rgga63219671:15840
Fannin sandy clay loam, 10 to 25 percent slopes, erodedFbE2833012565946rjga63219671:15840
Fannin fine sandy loam, 6 to 10 percent slopesFaC496012565646rfga63219671:15840
Fannin sandy clay loam, 6 to 10 percent slopes, erodedFbC2305012565846rhga63219671:15840
Fannin soils, 25 to 60 percent slopesFcF75512566046rkga63219671:15840
Fannin fine sandy loam, 2 to 6 percent slopesFaB54012565546rdga63219671:15840
Fannin fine sandy loam, 10 to 25 percent slopesFaE1830531395ktysga65119761:20000
Fannin fine sandy loam, 2 to 10 percent slopesFaC380531394ktyrga65119761:20000
Fannin silt loam, 10 to 25 percent slopes, erodedFnE25019545912lb22nc00519671:15840
Fannin silt loam, 6 to 10 percent slopes, erodedFnC21661545911lb21nc00519671:15840
Fannin silt loam, 25 to 45 percent slopesFnF865545913lb23nc00519671:15840
Fannin silty clay loam, 15 to 45 percent slopes, erodedFoF2500545914lb24nc00519671:15840
Fannin loam, 15 to 25 percent slopesFnE4200545953lb3dnc00919821:24000
Fannin loam, 8 to 15 percent slopesFnD2500545952lb3cnc00919821:24000
Fannin fine sandy loam, 15 to 30 percent slopesFaD1110548070ld9pnc01119971:12000
Fannin fine sandy loam, 8 to 15 percent slopesFaC125548069ld9nnc01119971:12000
Fannin sandy clay loam, 15 to 30 percent slopes, erodedFeD2110548072ld9rnc01119971:12000
Fannin sandy clay loam, 30 to 50 percent slopes, erodedFeE2102548073ld9snc01119971:12000
Fannin sandy clay loam, 8 to 15 percent slopes, erodedFeC233548071ld9qnc01119971:12000
Fannin-Lauada complex, 15 to 30 percent slopes, moderately erodedFaD2132416720221t3w6nc02120061:12000
Fannin-Lauada complex, 30 to 50 percent slopes, moderately erodedFaE291016720231t3w7nc02120061:12000
Fannin-Lauada complex, 8 to 15 percent slopes, moderately erodedFaC256016720211t3w5nc02120061:12000
Fannin-Lauada-Urban land complex, 15 to 30 percent slopesFnD24916720241t3w8nc02120061:12000
Fannin-Lauada-Urban land complex, 8 to 15 percent slopesFnC20316720261t3wbnc02120061:12000
Fannin-Lauada-Urban land complex, 2 to 8 percent slopesFnB15216720251t3w9nc02120061:12000
Fannin fine sandy loam, 15 to 30 percent slopesFaD883546416lblbnc04319911:12000
Fannin fine sandy loam, 8 to 15 percent slopesFaC618546415lbl9nc04319911:12000
Fannin-Urban land complex, 2 to 15 percent slopesFmC191546417lblcnc04319911:12000
Fannin silt loam, 15 to 25 percent slopesFaE2786546861lc1pnc08919741:20000
Fannin silt loam, 7 to 15 percent slopesFaC2228546860lc1nnc08919741:20000
Fannin silt loam, 25 to 45 percent slopesFaF722546862lc1qnc08919741:20000
Fannin fine sandy loam, 30 to 50 percent slopesFaE5060547076lc8mnc09919911:12000
Fannin fine sandy loam, 15 to 30 percent slopesFaD3169547075lc8lnc09919911:12000
Fannin fine sandy loam, 50 to 95 percent slopesFaF1508547077lc8nnc09919911:12000
Fannin fine sandy loam, 8 to 15 percent slopesFaC208547074lc8knc09919911:12000
Fannin fine sandy loam, 30 to 50 percent slopesFaE4024545843l9zvnc11319901:12000
Fannin fine sandy loam, 15 to 30 percent slopesFaD2854545842l9ztnc11319901:12000
Fannin fine sandy loam, 50 to 95 percent slopesFaF562545844l9zwnc11319901:12000
Fannin fine sandy loam, 8 to 15 percent slopesFaC215545841l9zsnc11319901:12000
Fannin sandy clay loam, 15 to 30 percent slopes, moderately erodedFnD21916713871t36qnc11520061:12000
Fannin sandy clay loam, 30 to 50 percent slopes, erodedFeE26001547570lcsknc12119971:12000
Fannin sandy clay loam, 15 to 30 percent slopes, erodedFeD24286547569lcsjnc12119971:12000
Fannin sandy clay loam, 8 to 15 percent slopes, erodedFeC21860547568lcshnc12119971:12000
Fannin-Cowee complex, 30 to 50 percent slopes, stonyFcE78191110863qlfnc14919921:24000
Fannin-Cowee complex, 15 to 30 percent slopes, stonyFcD26981110853qldnc14919921:24000
Fannin-Cowee complex, 50 to 85 percent slopes, stonyFcF15621110873qlgnc14919921:24000
Fannin fine sandy loam, 30 to 50 percent slopes, stonyFaE39361176213yd7nc16119971:24000
Fannin fine sandy loam, 15 to 30 percent slopes, stonyFaD11151176203yd6nc16119971:24000
Fannin-Chestnut complex, 50 to 85 percent slopes, rockyFbF3871176223yd8nc16119971:24000
Fannin fine sandy loam, 30 to 50 percent slopesFaF516723903772l7cync17519681:12000
Fannin fine sandy loam, 15 to 30 percent slopesFaE148923903762l7cxnc17519681:12000
Fannin fine sandy loam, 50 to 95 percent slopesFaG46623903782l7cznc17519681:12000
Fannin fine sandy loam, 15 to 30 percent slopes352D5625018102q8njnc17519681:12000
Fannin loam, 30 to 50 percent slopes, stonyFaE558529768ks89nc18920011:12000
Fannin loam, 15 to 30 percent slopes, stonyFaD376529767ks88nc18920011:12000
Fannin sandy clay loam, 30 to 50 percent slopes, erodedFeE25915547844ld2dnc19919971:12000
Fannin sandy clay loam, 15 to 30 percent slopes, erodedFeD24835547843ld2cnc19919971:12000
Fannin sandy clay loam, 8 to 15 percent slopes, erodedFeC2980547842ld2bnc19919971:12000
Lauada-Fannin complex, 30 to 50 percent slopesLdE1054191261122674nc60520071:12000
Lauada-Fannin complex, 50 to 95 percent slopesLdF663191261222675nc60520071:12000
Lauada-Fannin complex, 15 to 30 percent slopesLdD542191261022673nc60520071:12000
Lauada-Fannin complex, 8 to 15 percent slopesLdC4724848932pdqvnc60520071:12000
Fannin loam, 30 to 50 percent slopes, erodedFnE23753546773lbyvnc60619911:12000
Fannin fine sandy loam, 15 to 40 percent slopesFaF12161324854fvqsc04519721:20000
Lauada-Fannin complex, 50 to 95 percent slopesLeF156637230pd2ttn64020071:24000
Lauada-Fannin complex, 30 to 50 percent slopesLeE154637231pd2vtn64020071:24000
Lauada-Fannin complex, 15 to 30 percent slopesLeD35637232pd2wtn64020071:24000

Map of Series Extent

Approximate geographic distribution of the FANNIN 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 .