Official Series Description


Lab Data Summary

Aggregate lab data for the YADKIN soil series. This aggregation is based on all pedons with a current taxon name of YADKIN, 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 YADKIN 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
13604N108704NC097021Yadkin7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.8897781,-80.7907257

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the YADKIN 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 YADKIN 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 YADKIN 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 YADKIN 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 flats position figure.

Competing Series

Soil series competing with YADKIN 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 YADKIN 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 YADKIN 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 YADKIN, 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 YADKIN 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
Yadkin clay loam, 2 to 8 percent slopes, moderately erodedYaB247523903452l7bxnc00319881:24000
Yadkin clay loam, 8 to 15 percent slopes, moderately erodedYaC237523903472l7bznc00319881:24000
Yadkin clay loam, 2 to 8 percent slopes, moderately erodedYaB211026792772r949nc02720121:12000
Yadkin clay loam, 8 to 15 percent slopes, moderately erodedYaC24126792782r94bnc02720121:12000
Yadkin clay loam, 2 to 8 percent slopes, moderately erodedYaB236429739472wx35nc03320161:24000
Yadkin clay loam, 8 to 15 percent slopes, moderately erodedYaC218029739482wx36nc03320161:24000
Yadkin sandy clay loam, 2 to 6 percent slopes, moderately erodedYaB235624244942mcwhnc09720111:12000
Yadkin sandy clay loam, 6 to 10 percent slopes, moderately erodedYaC227324244952mcwjnc09720111:12000
Yadkin sandy clay loam, 10 to 15 percent slopes, moderately erodedYaD21324244962mcwknc09720111:12000
Yadkin loam, 2 to 8 percent slopesYaB79823889972l5yfnc15719831:24000
Yadkin loam, 8 to 15 percent slopesYaD13223889982l5ygnc15719831:24000
Yadkin loam, 2 to 8 percent slopes, moderately erodedYaB217623980092lhb4nc19719601:15840
Yadkin clay loam, 2 to 7 percent slopes23B234051632630yn3va00319811:15840
Yadkin loam, 2 to 7 percent slopes41B14805163772v7j3va00319811:15840
Yadkin clay loam, 7 to 15 percent slopes23C120051632730yn4va00319811:15840
Yadkin clay loam, 7 to 15 percent slopes, severely eroded42C36305163802v7j6va00319811:15840
Yadkin loam, 7 to 15 percent slopes41C3805163782v7j4va00319811:15840
Yadkin clay loam, 2 to 7 percent slopes, severely eroded42B32805163792v7j5va00319811:15840
Yadkin clay loam, 15 to 25 percent slopes, severely eroded42D32205163812v7j7va00319811:15840
Yadkin and Wintergreen loams, 2 to 15 percent slopesHtC7985192312yztsva03519651:15840
Yadkin and Wintergreen fine sandy loams, 2 to 15 percent slopesHvC4275192352yztxva03519651:15840
Yadkin and Wintergreen loams, 15 to 25 percent slopesHtD3685192322yzttva03519651:15840
Yadkin and Wintergreen cobbly fine sandy loams, 7 to 15 percent slopesHuC2675192332yztvva03519651:15840
Yadkin and Wintergreen loams, 2 to 7 percent slopesHtB2065192302yztrva03519651:15840
Yadkin and Wintergreen cobbly fine sandy loams, 15 to 25 percent slopesHuD2065192342yztwva03519651:15840
Yadkin fine sandy loam, 2 to 8 percent slopes57B222714728691lfmxva08320041:24000
Yadkin fine sandy loam, 8 to 15 percent slopes57C73114728701lfmyva08320041:24000
Yadkin clay loam, 2 to 8 percent slopes, severely eroded58B359814728711lfmzva08320041:24000
Yadkin clay loam, 8 to 15 percent slopes, severely eroded58C310614728721lfn0va08320041:24000
Yadkin loam, 2 to 7 percent slopes, moderately erodedHsB27311198492z1xsva13719661:15840
Yadkin clay loam, 4 to 15 percent slopes, severely erodedHwC32741198512z1xvva13719661:15840
Yadkin loam, 2 to 7 percent slopesHsB2701198482z1xrva13719661:15840
Yadkin loam, 7 to 15 percent slopes, moderately erodedHsC22691198502z1xtva13719661:15840
Yadkin clay loam, 7 to 15 percent slopes, severely eroded18C326861199622yzs6va14319891:24000
Yadkin clay loam, 2 to 7 percent slopes, severely eroded18B321581199612yzs5va14319891:24000
Yadkin loam, 2 to 7 percent slopes17B16531199602yzs4va14319891:24000
Yadkin cobbly sandy loam, 2 to 7 percent slopes19B3561199632yzs7va14319891:24000
Yadkin cobbly sandy loam, 7 to 15 percent slopes19C2801199642yzs3va14319891:24000

Map of Series Extent

Approximate geographic distribution of the YADKIN 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 .