Official Series Description


Lab Data Summary

Aggregate lab data for the CHESTER soil series. This aggregation is based on all pedons with a current taxon name of CHESTER, 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 CHESTER 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
14804N025403PA071002Chester7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.8597221,-76.3002777
14890PA0710471990PA071047Chester4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9105556,-76.2905556
14890PA0710481990PA071048Chester4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9097222,-76.29
14890PA0710501990PA071050Chester5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9111111,-76.2888889
14890PA0710521990PA071052Chester4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9083333,-76.2902778
14890PA0710551990PA071055Chester3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9122222,-76.2908333
14840A1202S1954MD031001Chester3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0782667,-76.9878139
14840A0386S1955PA071015Chester2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9000015,-76.058609
14899P0570S1999DE003003CHESTER6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.722589,-75.760103
14899P0571S1999DE003004CHESTER6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.719125,-75.759561
n/a40A4189S1952VA107001CHESTER3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CHESTER 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 CHESTER 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 CHESTER 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 CHESTER 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 CHESTER 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 CHESTER series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the CHESTER 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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

Soil series sharing subgroup-level classification with CHESTER, 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. MD-2012-02-03-06 | Baltimore County - March 1976

    Cross section showing typical soil pattern in the Chester-Glenelg association (Soil Survey of Baltimore County, Maryland; March 1976).

  2. MD-2012-02-03-08 | Baltimore County - March 1978

    Cross section showing relationships of parent material and topography to certain soil series of Baltimore County. Fall line shown in drawing separates soil of Piedmont Province (left) from soils of Atlantic Coastal Plain (right) (Soil Survey of Baltimore County, Maryland; March 1976).

  3. PA-2010-09-30-16 | York County - 2002

    Typical pattern of soils and parent material in the Chester-Glenelg general soil map unit (Soil Survey of York County, Pennsylvania; 2002).

  4. PA-2010-09-30-17 | York County - 2002

    Typical pattern of soils and parent material in the Mt. Airy-Manor general soil map unit (Soil Survey of York County, Pennsylvania; 2002).

  5. PA-2012-03-13-48 | Lancaster County - May 1985

    Typical pattern of soils and underlying material in the Manor-Chester-Glenelg unit (Soil Survey of Lancaster County, PA; 1985).

  6. PA-2012-03-13-49 | Lancaster County - May 1985

    Typical pattern of soils and underlying material in the Letort-Pequea-Conestoga unit (Soil Survey of Lancaster County, PA; 1985).

  7. PA-2012-03-13-51 | Lancaster County - May 1985

    Typical pattern of soils and underlying material in the Clymer-Chester unit (Soil Survey of Lancaster County, PA; 1985).

  8. PA-2012-03-13-71 | Montgomery County - April 1967

    Typical landscape in the southern part of Montgomery County, showing the pattern of soils formed on schist and the relationship of the soils in the pattern (Soil Survey of Montgomery County, PA; 1967).

Map Units

Map units containing CHESTER 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
Chester-Urban land complex, 0 to 8 percent slopes6UB674533972kxmxmd51019931:12000
Chester loam, 0 to 8 percent slopes6B119533971kxmwmd51019931:12000
Chester silt loam, 3 to 8 percent slopesCcB2207265333632tt7ymd60019721:15840
Chester silt loam, 8 to 15 percent slopesCcC248115333642tt7zmd60019721:15840
Chester gravelly silt loam, 3 to 8 percent slopes, moderately erodedCgB22781533365kx0bmd60019721:15840
Chester gravelly silt loam, 8 to 15 percent slopes, moderately erodedCgC22045533366kx0cmd60019721:15840
Chester gravelly silt loam, 15 to 25 percent slopes, moderately erodedCgD2401533367kx0dmd60019721:15840
Chester silt loam, 0 to 3 percent slopesCcA1915333622tt7xmd60019721:15840
Chester loam, 10 to 25 percent slopesCeE22136545900lb1pnc00519671:15840
Chester loam, 6 to 10 percent slopesCeC9752545899lb1nnc00519671:15840
Chester loam, 25 to 45 percent slopesCeF3362545901lb1qnc00519671:15840
Chester loam, 2 to 6 percent slopesCeB1324545898lb1mnc00519671:15840
Urban land-Chester complex, 0 to 8 percent slopesUkB8275543735l7svpa01719971:24000
Urban land-Chester complex, 8 to 25 percent slopesUkD2405543736l7swpa01719971:24000
Chester silt loam, 3 to 8 percent slopesCdB12645436152tt7ypa01719971:24000
Chester silt loam, 8 to 15 percent slopesCdC6395436162tt7zpa01719971:24000
Chester silt loam, 0 to 3 percent slopesCdA1925436142tt7xpa01719971:24000
Chester silt loam, 3 to 8 percent slopesCdB41646414662tt7ypa02920081:24000
Chester silt loam, 0 to 3 percent slopesCdA10296414642tt7xpa02920081:24000
Urban land-Chester complex, 0 to 8 percent slopesUrdB62716122441r3nwpa02920081:24000
Chester silt loam, 8 to 15 percent slopesCdC606414692tt7zpa02920081:24000
Urban land-Chester complex, 8 to 25 percent slopesUrdD3116122451r3nxpa02920081:24000
Chester silt loam, 3 to 8 percent slopesCdB96098446130ynlpa04519601:20000
Chester silt loam, 0 to 3 percent slopesCdA27098445830ynkpa04519601:20000
Chester silt loam, 8 to 15 percent slopesCdC7498446330ynnpa04519601:20000
Chester silt loam, 3 to 8 percent slopesCbB420735427342tt7ypa07119821:15840
Chester silt loam, 8 to 15 percent slopesCbC118645427352tt7zpa07119821:15840
Chester silt loam, 0 to 3 percent slopesCbA45625427332tt7xpa07119821:15840
Chester extremely stony loam, 8 to 25 percent slopesChC883541282l57qpa07519761:20000
Chester channery loam, 3 to 8 percent slopesCeB573541280l57npa07519761:20000
Chester channery loam, 8 to 15 percent slopesCeC546541281l57ppa07519761:20000
Chester silt loam, 3 to 8 percent slopesCgB6923840742tt7ypa09120081:12000
Chester silt loam, 0 to 3 percent slopesCgA2623840732tt7xpa09120081:12000
Urban land-Chester complex, 0 to 8 percent slopesUdB2113714795701lnm2pa10119711:15840
Urban land-Chester complex, 8 to 15 percent slopesUdC209514795711lnm3pa10119711:15840
Manor and Chester extremely stony loams, 25 to 50 percent slopesMcE138214795621lnltpa10119711:15840
Chester silt loam, 3 to 8 percent slopesCeB83714795122tt7ypa10119711:15840
Chester silt loam, 8 to 15 percent slopesCeC14814795132tt7zpa10119711:15840
Chester silt loam, 0 to 3 percent slopesCeA4214795112tt7xpa10119711:15840
Chester silt loam, 15 to 25 percent slopesCeD1614795141lnk8pa10119711:15840
Chester silt loam, 3 to 8 percent slopesCeB729815428262tt7ypa13319901:24000
Chester silt loam, 8 to 15 percent slopesCeC295545428272tt7zpa13319901:24000
Urban land-Chester complex, 0 to 8 percent slopesUdB4014542956l6zqpa13319901:24000
Chester very stony loam, 25 to 45 percent slopes15E10860516311kb86va00319811:15840
Chester loam, 15 to 25 percent slopes14D6440516307kb82va00319811:15840
Chester loam, 7 to 15 percent slopes14C5380516306kb81va00319811:15840
Chester very stony loam, 15 to 25 percent slopes15D4550516310kb85va00319811:15840
Chester loam, 25 to 45 percent slopes14E2950516308kb83va00319811:15840
Chester very stony loam, 7 to 15 percent slopes15C1630516309kb84va00319811:15840
Chester loam, 2 to 7 percent slopes14B1220516305kb80va00319811:15840
Chester-Glenelg loams, slopingChC19657519194kf86va03519651:15840
Chester-Glenelg loams, steepChE18470519196kf88va03519651:15840
Chester-Glenelg loams, sloping, erodedChC26200519195kf87va03519651:15840
Chester-Glenelg loams, steep, erodedChE25721519197kf89va03519651:15840
Chester-Glenelg cobbly loams, steepCgE4062519190kf82va03519651:15840
Chester-Glenelg cobbly loams, steep, erodedCgE24013519191kf83va03519651:15840
Chester-Glenelg cobbly loams, slopingCgC3046519188kf80va03519651:15840
Chester-Glenelg cobbly loams, sloping, erodedCgC21850519189kf81va03519651:15840
Chester-Glenelg loams, gently slopingChB1394519192kf84va03519651:15840
Chester-Glenelg loams, gently sloping, erodedChB2254519193kf85va03519651:15840
Chester-Glenelg cobbly loams, gently slopingCgB134519187kf7zva03519651:15840
Chester and Parker soils, very stony, 15 to 25 percent slopesCmD2877516882kbvmva07919831:15840
Chester loam, 15 to 25 percent slopesChD694516880kbvkva07919831:15840
Chester and Parker soils, very stony, 7 to 15 percent slopesCmC620516881kbvlva07919831:15840
Chester loam, 7 to 15 percent slopesChC511516879kbvjva07919831:15840
Chester-Brandywine loams, very deep, 7 to 15 percent slopesCkC853516953kbxxva11319671:15840
Chester-Brandywine loams, very deep, 2 to 7 percent slopesCkB642516952kbxwva11319671:15840
Chester-Brandywine loams, very deep, 7 to 15 percent slopes, erodedCkC2533516954kbxyva11319671:15840
Chester-Brandywine loams, very deep, 15 to 25 percent slopesCkD373516955kbxzva11319671:15840
Chester-Brandywine loams, eroded sloping phasesCeC23577517415kcdtva15719581:20000
Chester loam, gently sloping phaseCdB861517412kcdqva15719581:20000
Eubanks-Chester complex, sloping phasesEcC762517427kcf6va15719581:20000
Chester loam, eroded sloping phaseCdC2686517413kcdrva15719581:20000
Eubanks-Chester complex, gently sloping phasesEcB487517426kcf5va15719581:20000
Chester-Brandywine loams, eroded gently sloping phasesCeB2452517414kcdsva15719581:20000
Chester-Manor complex, 25 to 60 percent slopes, very stony11E9361518805kdvnva18719801:15840
Chester loam, 7 to 15 percent slopes10C1915518801kdvjva18719801:15840
Chester loam, 15 to 25 percent slopes10D1745518802kdvkva18719801:15840
Chester-Manor complex, 15 to 25 percent slopes, very stony11D1399518804kdvmva18719801:15840
Chester loam, 25 to 65 percent slopes10E649518803kdvlva18719801:15840

Map of Series Extent

Approximate geographic distribution of the CHESTER 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 .