Official Series Description


Lab Data Summary

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

There are insufficient data to create the lab data summary figure.


Water Balance

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

Competing Series

Soil series competing with CAROLINE 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 CAROLINE 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 CAROLINE 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 CAROLINE, 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-2012-02-07-31 | Northampton County - August 1994

    Typical relationship of soils and landscape in the Gritney-Caroline and Norfolk-Bonneau-Goldsboro general soil map units (Soil Survey of Northampton County, North Carolina; August 1994).

  2. SC-2012-03-14-01 | Bamberg County - January 1966

    Soil series in soil association 1 and their relation to the landscape and the underlying material (Soil Survey of Bamberg County, SC; 1966).

  3. SC-2012-03-14-11 | Calhoun County - 1963

    Major soils in the Norfolk-Ruston-Lakeland soil association and their relationship to the landscape (Soil Survey of Calhoun County, SC; 1963).

  4. SC-2012-03-14-12 | Calhoun County - 1963

    Major soils of the Magnolia-Faceville-Ruston soil association and their relationship to the landscape (Soil Survey of Calhoun County, SC; 1963).

Map Units

Map units containing CAROLINE 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
Caroline silt loam, 5 to 10 percent slopes, severely erodedCaC3336412829549hkmd03719751:20000
Caroline silt loam, 5 to 10 percent slopes moderately erodedCaC2258012829449hjmd03719751:20000
Caroline silt loam, 2 to 5 percent slopes, moderately erodedCaB2140312829349hhmd03719751:20000
Caroline silt loam, 10 to 15 percent slopes, severely erodedCaD395412829749hmmd03719751:20000
Caroline silt loam, 10 to 15 percent slopes, moderately erodedCaD287812829649hlmd03719751:20000
Caroline fine sandy loam, 0 to 2 percent slopesCaA43591131533sr3nc09119811:24000
Caroline fine sandy loam, 2 to 6 percent slopesCaB17281131543sr4nc09119811:24000
Caroline sandy loam, 2 to 6 percent slopesCaB95471140303tndnc13119881:24000
Caroline sandy loam, 0 to 2 percent slopesCaA45871140293tncnc13119881:24000
Caroline fine sandy loam, 2 to 6 percent slopesCoB89001319494f9fsc01519741:20000
Caroline fine sandy loam, 0 to 2 percent slopesCoA12051319484f9dsc01519741:20000
Caroline-Emporia complex, 2 to 6 percent slopes7B64651179763yrpva03619931:24000
Craven-Caroline complex, 2 to 6 percent slopes14B15571177793ykbva03619931:24000
Craven-Caroline complex, 6 to 10 percent slopes, severely eroded15C33581177903ykpva03619931:24000
Caroline silt loam, 2 to 6 percent slopes6B3021179533yqyva03619931:24000
Caroline-Emporia complex, 6 to 10 percent slopes7C1631179783yrrva03619931:24000
Caroline loam, 0 to 4 percent slopes2B3651189683zspva07319781:15840
Caroline-Dogue complex, 7 to 15 percent slopes, eroded13C238301190763zx5va08519761:15840
Caroline-Dogue complex, 2 to 7 percent slopes, eroded13B28901190753zx4va08519761:15840
Caroline fine sandy loam, 15 to 25 percent slopes, eroded12D26701190743zx3va08519761:15840
Caroline fine sandy loam, 2 to 7 percent slopes12B6401190733zx2va08519761:15840
Caroline very fine sandy loam, 2 to 6 percent slopes, erodedCaB24110119210401hva08719731:15840
Caroline very fine sandy loam, 6 to 10 percent slopes, erodedCaC22485119211401jva08719731:15840
Caroline clay loam, 2 to 10 percent slopes, severely erodedCbC3732119213401lva08719731:15840
Caroline very fine sandy loam, 10 to 15 percent slopes, erodedCaD2297119212401kva08719731:15840
Caroline sandy loam, 1 to 7 percent slopes4B2844119471409xva11119791:20000
Caroline-Emporia complex, 2 to 6 percent slopes7B946411970340kdva12719851:15840
Craven-Caroline complex, 2 to 6 percent slopes11B194211966140j1va12719851:15840
Caroline-Emporia complex, 6 to 10 percent slopes7C172311970440kfva12719851:15840
Caroline loam, 2 to 6 percent slopes6B48211970240kcva12719851:15840
Caroline very fine sandy loam, gently sloping, erodedCfB234911973540lfva13319601:20000
Caroline very fine sandy loam, sloping, erodedCfC229811973640lgva13319601:20000
Caroline clay loam, strongly sloping, severely erodedCaD316111973440ldva13319601:20000
Caroline clay loam, sloping, severely erodedCaC311811973340lcva13319601:20000
Caroline fine sandy loam, 6 to 10 percent slopes, erodedCaC271424535542nc3xva15319851:15840
Caroline fine sandy loam, 2 to 6 percent slopes, erodedCaB256424535532nc3wva15319851:15840
Caroline-Sassafras complex, 15 to 30 percent slopesCdE54324535552nc3yva15319851:15840
Caroline-Sassafras complex, 15 to 30 percent slopesCdE1186312050141d4va17919701:15840
Caroline fine sandy loam, 2 to 6 percent slopes, erodedCaB2607612049541cyva17919701:15840
Caroline fine sandy loam, 6 to 10 percent slopes, erodedCaC2422012049641czva17919701:15840
Caroline fine sandy loam, 10 to 18 percent slopes, erodedCaD2235512049741d0va17919701:15840
Caroline clay loam, 6 to 10 percent slopes, severely erodedCcC3176912049841d1va17919701:15840
Caroline-Sassafras complex, 10 to 15 percent slopesCdD134012050041d3va17919701:15840
Caroline clay loam, 10 to 18 percent slopes, severely erodedCcD371512049941d2va17919701:15840
Caroline silt loam, 2 to 6 percent slopes6B200712247543ftva18119971:24000
Caroline fine sandy loam, 2 to 6 percent slopes8B59312083741qzva69519811:15840

Map of Series Extent

Approximate geographic distribution of the CAROLINE 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 .