Official Series Description


Lab Data Summary

Aggregate lab data for the CHESHIRE soil series. This aggregation is based on all pedons with a current taxon name of CHESHIRE, 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 CHESHIRE 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
14540A123769CT009001Cheshire7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.4297218,-72.7986145
14540A123869CT009002Cheshire7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.5327797,-72.9133301
14540A123969CT009003Cheshire5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.4891663,-72.930275
14585P005783CT009001Cheshire6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.4041672,-72.9258347
14585P005583CT009002Cheshire6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.4166679,-72.7783356
14597P010296CT007001Cheshire7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.503334,-72.7399979
149B96P0179S1995NY085044Cheshire6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5720528,-74.1581778

Water Balance

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

Soil series competing with CHESHIRE 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 CHESHIRE 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 CHESHIRE 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 terrace figure.

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

Soil series sharing subgroup-level classification with CHESHIRE, 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-2012-02-15-40 | Rockland County - October 1990

    Relationship between soils, landscape position, and parent materials in Rockland County (Soil Survey of Rockland County, New York; October 1990).

  2. NY-2012-02-15-46 | Sullivan County - July 1989

    Typical landscape pattern of the soils and the underlying material in the Wellsboro-Oquaga-Lackawanna general soil map unit (Soil Survey of Sullivan County, New York; July 1989).

Map Units

Map units containing CHESHIRE 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
Cheshire-Holyoke complex, 3 to 15 percent slopes, very rocky77C921633958189lqsct60120031:12000
Cheshire fine sandy loam, 3 to 8 percent slopes63B918233957949lpwct60120031:12000
Cheshire-Holyoke complex, 15 to 35 percent slopes, very rocky77D677733958199lqtct60120031:12000
Cheshire fine sandy loam, 8 to 15 percent slopes63C329333957959lpxct60120031:12000
Cheshire-Urban land complex, 3 to 8 percent slopes263B308233956899lldct60120031:12000
Cheshire fine sandy loam, 3 to 8 percent slopes, very stony64B246833957979lpzct60120031:12000
Cheshire fine sandy loam, 3 to 15 percent slopes, extremely stony65C240333957999lq1ct60120031:12000
Cheshire-Urban land complex, 8 to 15 percent slopes263C211833956909llfct60120031:12000
Cheshire fine sandy loam, 15 to 25 percent slopes63D134633957969lpyct60120031:12000
Cheshire fine sandy loam, 8 to 15 percent slopes, very stony64C114233957989lq0ct60120031:12000
Cheshire fine sandy loam, 15 to 35 percent slopes, extremely stony65D42433958009lq2ct60120031:12000
Cheshire-Holyoke complex, 3 to 15 percent slopes, very rocky77C287934001919lqsct60220031:12000
Cheshire-Holyoke complex, 15 to 35 percent slopes, very rocky77D232134001929lqtct60220031:12000
Cheshire fine sandy loam, 3 to 8 percent slopes63B173734001679lpwct60220031:12000
Cheshire fine sandy loam, 3 to 8 percent slopes, very stony64B113534001709lpzct60220031:12000
Cheshire fine sandy loam, 8 to 15 percent slopes63C53834001689lpxct60220031:12000
Cheshire fine sandy loam, 8 to 15 percent slopes, very stony64C43334001719lq0ct60220031:12000
Cheshire-Urban land complex, 8 to 15 percent slopes263C9334000639llfct60220031:12000
Cheshire fine sandy loam, 15 to 25 percent slopes63D5934001699lpyct60220031:12000
Cheshire fine sandy loam, 15 to 35 percent slopes, extremely stony65D3034001739lq2ct60220031:12000
Cheshire-Urban land complex, 3 to 8 percent slopes263B1334000629lldct60220031:12000
Cheshire fine sandy loam, 8 to 15 percent slopes462C395621164nvckma01120121:12000
Cheshire fine sandy loam, 15 to 25 percent slopes462D92621165nvclma01120121:12000
Cheshire fine sandy loam, 3 to 8 percent slopes462B1190307621w9kma60719751:15840
Cheshire loam, 8 to 15 percent slopesCeC10924845832pddvny08520141:12000
Cheshire loam, 15 to 25 percent slopesCeD9925890812r301ny08520141:12000
Cheshire loam, 3 to 8 percent slopesCeB5524845822pddtny08520141:12000
Cheshire loam, 0 to 3 percent slopesCeA1024845812pddsny08520141:12000
Cheshire-Urban land complex, 2 to 8 percent slopesCuB33342932379v48ny08719861:24000
Cheshire gravelly fine sandy loam, 2 to 8 percent slopesCrB23862932359v46ny08719861:24000
Cheshire gravelly fine sandy loam, 8 to 15 percent slopesCrC7312932369v47ny08719861:24000
Cheshire-Urban land complex, 8 to 15 percent slopesCuC5922932389v49ny08719861:24000
Cheshire channery loam, 8 to 15 percent slopes, stonyCsC34432950609x12ny10519841:15840
Cheshire channery loam, 15 to 25 percent slopes, stonyCsD33392950619x13ny10519841:15840
Cheshire channery loam, 35 to 60 percent slopes, stonyCsF27482950639x15ny10519841:15840
Cheshire channery loam, 3 to 8 percent slopes, stonyCsB25962950599x11ny10519841:15840
Cheshire channery loam, 25 to 35 percent slopes, stonyCsE21532950629x14ny10519841:15840

Map of Series Extent

Approximate geographic distribution of the CHESHIRE 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 .