Official Series Description


Lab Data Summary

Aggregate lab data for the CARROLLTON soil series. This aggregation is based on all pedons with a current taxon name of CARROLLTON, 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 CARROLLTON 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
14092P000190NY009001Carrollton4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.1766663,-78.8791656
n/a91P091690NY009004Carrollton4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CARROLLTON 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 CARROLLTON 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 CARROLLTON 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 CARROLLTON 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 terrace figure.

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with CARROLLTON 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 CARROLLTON series and competing. 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 CARROLLTON 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 .

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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 CARROLLTON, 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. NY-2010-09-28-01 | Cattarugus County - 2007

    Representative landscape showing soils that formed in residual material, glacial till, glacial outwash, or alluvium (Soil Survey of Cattarugus County, New York; 2007).

  2. NY-2012-02-15-10 | Chautauqua County - August 1994

    Representative landscape showing soils that formed in residual material, glacial till, glacial outwash, or alluvium (Soil Survey of Chautauqua County, New York; August 1994).

Map Units

Map units containing CARROLLTON 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
Carrollton channery silt loam, 25 to 35 percent slopes96E420300037b26mny00320131:24000
Carrollton channery silt loam, 8 to 15 percent slopes96C169300035b26kny00320131:24000
Carrollton channery silt loam, 15 to 25 percent slopes96D129300036b26lny00320131:24000
Carrollton channery silt loam, 3 to 8 percent slopes96B123300034b26jny00320131:24000
Carrollton channery silt loam, 35 to 50 percent slopes96F30300038b26nny00320131:24000
Carrollton channery silt loam, 25 to 35 percent slopes96E105622897559qhyny00920021:24000
Carrollton channery silt loam, 15 to 25 percent slopes96D56262897549qhxny00920021:24000
Carrollton channery silt loam, 8 to 15 percent slopes96C52312897539qhwny00920021:24000
Carrollton channery silt loam, 3 to 8 percent slopes96B44472897529qhvny00920021:24000
Carrollton channery silt loam, 35 to 50 percent slopes96F43372897569qhzny00920021:24000
Carrollton channery silt loam, 15 to 25 percent slopesCfD1222897909qk2ny01319881:15840
Carrollton channery silt loam, 8 to 15 percent slopesCfC1192897899qk1ny01319881:15840
Carrollton channery silt loam, 15 to 25 percent slopesCaD89818346wgk8pa60919791:20000
Carrollton channery silt loam, 8 to 15 percent slopesCaC7818345wgk7pa60919791:20000

Map of Series Extent

Approximate geographic distribution of the CARROLLTON 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 .