Official Series Description


Lab Data Summary

Aggregate lab data for the CANDOR soil series. This aggregation is based on all pedons with a current taxon name of CANDOR, 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 CANDOR 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
13704N0749S2003NC123003Candor6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.2036095,-79.6766663

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CANDOR 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 CANDOR 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 CANDOR 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 CANDOR 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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Competing Series

Soil series competing with CANDOR 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 CANDOR 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 CANDOR 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 CANDOR, 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

No block diagrams are available.

Map Units

Map units containing CANDOR 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
Candor sand, 1 to 8 percent slopesCaB38231145023v4mnc00719991:24000
Candor sand, 8 to 15 percent slopesCaC3441145033v4nnc00719991:24000
Candor sand, 1 to 8 percent slopesCaB31898811069w6zjnc05119811:24000
Candor sand, 8 to 15 percent slopesCaD1640811070w6zknc05119811:24000
Candor sand, 0 to 8 percent slopesCaB106731130873snznc08519841:24000
Candor sand, 8 to 15 percent slopesCaD15881130883sp0nc08519841:24000
Candor sand, 1 to 8 percent slopesCaB32082811261w75qnc09319811:24000
Candor sand, 8 to 15 percent slopesCaD1520811262w75rnc09319811:24000
Candor sand, 0 to 8 percent slopesCaB34121135753t5qnc10519821:24000
Candor sand, 0 to 8 percent slopesCdB807522335612dz6cnc12320071:24000
Candor sand, 8 to 15 percent slopesCdC79722335622dz6dnc12320071:24000
Candor sand, 0 to 4 percent slopesCaB502661138923thync12519871:24000
Candor sand, 4 to 12 percent slopesCaC204931138933thznc12519871:24000
Candor-Urban land complex, 2 to 12 percent slopesCbC54431138943tj0nc12519871:24000
Wakulla and Candor soils, 0 to 8 percent slopesWcB7298114022451j24qnc15319961:24000
Candor and Wakulla soils, 8 to 15 percent slopesCaC2245314022351j24dnc15319961:24000
Wakulla-Candor-Urban land complex, 0 to 10 percent slopesWuB249314022461j24rnc15319961:24000
Wakulla and Candor soils, 0 to 8 percent slopesWcB3193014086171j8s8nc16520061:12000
Wakulla and Candor soils, moderately wet, 0 to 8 percent slopesWkB327214144961jgwxnc16520061:12000
Candor and Wakulla soils, 8 to 15 percent slopesCaC124814141741jgkjnc16520061:12000
Candor sand, 0 to 6 percent slopesCaB333891319954fbxsc02519891:20000
Candor sand, 6 to 10 percent slopesCaC161381319964fbysc02519891:20000
Candor sand, 10 to 15 percent slopesCaD25751319974fbzsc02519891:20000
Candor sand, 0 to 6 percent slopesCaB6924618789nrwysc03119981:24000
Candor sand, 6 to 10 percent slopesCaC224622232nwh0sc03119981:24000
Candor sand, 10 to 15 percent slopesCaD48618791nrx0sc03119981:24000
Candor sand, 0 to 6 percent slopesCaB205416065191qxq6sc06120051:24000
Candor sand, 0 to 6 percent slopesCaB45301306104cx7sc06919951:24000
Candor sand, moderately wet, 0 to 6 percent slopesCdB28391306134cxbsc06919951:24000
Candor sand, 6 to 10 percent slopesCaC8521306114cx8sc06919951:24000
Candor sand, 10 to 15 percent slopesCaD4081306124cx9sc06919951:24000
Alpin-Candor-Troup complex, 0 to 6 percent slopesApB62024858772pfrlsc08519691:20000
Candor sand, 2 to 6 percent slopesCaB21861315074dv5sc08919851:20000
Candor sand, 0 to 2 percent slopesCaA15261315064dv4sc08919851:20000

Map of Series Extent

Approximate geographic distribution of the CANDOR 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 .