Official Series Description


Lab Data Summary

Aggregate lab data for the DEERFIELD soil series. This aggregation is based on all pedons with a current taxon name of DEERFIELD, 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 DEERFIELD 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
144A40A0428S1959MA005001Deerfield5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.9638634,-71.127243
14505N08782005CT003002Deerfield7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.7512207,-72.6092224
14540A1230S1970MA011004Deerfield5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.4958115,-72.6128464
14505N0879S2005CT003003Deerfield6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.7516937,-72.6093369
149B91P0792S1991MA023005Deerfield6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.7488899,-70.7741699
149B14N0346S2013NY085002Deerfield6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6087,-74.1797917
n/a97P0236S1996NH013005Deerfield6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DEERFIELD 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 DEERFIELD 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 DEERFIELD 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 DEERFIELD 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 DEERFIELD 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 DEERFIELD 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 DEERFIELD 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.

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Soil series sharing subgroup-level classification with DEERFIELD, 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. MA-2010-09-10-03 | Middlesex County - 2009

    A typical pattern of soils and underlying material in the Hinckley-Freetown-Windsor association (Soil Survey of Middlesex County, Massachusetts; 2009).

  2. MA-2012-02-01-03 | Barnstable County - March 1993

    Relationship of soils, landscapes, and parent material in the Enfield-Merrimac-Carver general soil map unit (Soil Survey of Barnstable County, Massachusetts; March 1993).

  3. MA-2012-02-01-11 | Bristol County, Southern Part - October 1981

    Typical pattern of soils and underlying material in the Hinckley-Freetown-Scarboro association (Soil Survey of Bristol County, Massachusetts, Southern Part; October 1981).

  4. MA-2012-02-02-02 | Essex County, Northern Part - February 1981

    Typical pattern of soils and parent material in the Hinckley-Windsor-Merrimac association (Soil Survey of Essex County, Massachusetts, Northern Part; February 1981).

  5. MA-2012-02-02-07 | Essex County, Southern Part - May 1984

    Typical pattern of soils and parent material in the Merrimac-Hinckley-Urban land association (Soil Survey of Essex County, Massachusetts, Southern Part; May 1984).

  6. MA-2012-02-03-02 | Worcester County, Northeastern Part - December 1985

    Typical pattern of soils and parent material in the Hinckley-Merrimac-Windsor map unit (Soil Survey of Worcester County, Massachusetts, Northeastern Part; December 1985).

  7. NH-2012-02-14-19 | Rockingham County - October 1994

    Typical pattern of soils and parent material in the Windsor-Hinckley-Canton general soil map unit (Soil Survey of Rockingham County, New Hampshire; October 1994).

  8. NH-2012-02-14-24 | Strafford County - March 1973

    Typical pattern of soils and underlying material in the Hinckley-Windsor-Saugatuck association (Soil Survey of Strafford County, New Hampshire; March 1973).

  9. NY-2010-09-28-25 | Saratoga County - 2004

    Typical relationship of soils and underlying material in the Windsor-Deerfield-Scio general soil map unit. Many areas of this unit are farmed and are easily eroded after cultivation (Soil Survey of Saratoga County, New York; 2004).

  10. VT-2012-03-22-02 | Chittenden County - January 1974

    Relationship of soils in associations 6 and 8 (Soil Survey of Chittenden County, VT; 1974).

Map Units

Map units containing DEERFIELD 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
Deerfield loamy fine sand, 0 to 3 percent slopes24A98933956792xfg8ct60120031:12000
Deerfield-Urban land complex, 0 to 3 percent slopes224A29333956552xfgbct60120031:12000
Deerfield loamy fine sand, 0 to 3 percent slopes24A1034000522xfg8ct60220031:12000
Deerfield loamy fine sand, 0 to 3 percent slopes256A10482765072xfg8ma00119841:25000
Deerfield loamy fine sand, 0 to 3 percent slopes256A8442765792xfg8ma00319841:25000
Deerfield loamy fine sand, 0 to 3 percent slopes256A15072789032xfg8ma01120121:12000
Deerfield loamy fine sand, 3 to 8 percent slopes256B4972790632xfg9ma01120121:12000
Deerfield loamy fine sand, 0 to 3 percent slopes256A65492767972xfg8ma01719911:24000
Deerfield loamy fine sand, 3 to 8 percent slopes256B50542767982xfg9ma01719911:24000
Deerfield loamy fine sand, 3 to 8 percent slopes256B82013093462xfg9ma02320101:12000
Deerfield loamy fine sand, 0 to 3 percent slopes256A74243093452xfg8ma02320101:12000
Deerfield-Urban land complex, 0 to 3 percent slopes619A5455998522xfgbma02320101:12000
Deerfield loamy fine sand, 0 to 3 percent slopes256A69022770182xfg8ma60219761:20000
Deerfield loamy fine sand, 0 to 3 percent slopes256A14757799512xfg8ma60319791:20000
Deerfield loamy fine sand, 0 to 3 percent slopes256A38097901732xfg8ma60519771:15840
Deerfield loamy fine sand, 0 to 3 percent slopes256A9427910512xfg8ma60619811:15840
Deerfield loamy fine sand, 0 to 3 percent slopes256A12162774132xfg8ma60719751:15840
Deerfield loamy fine sand, 0 to 3 percent slopes256A13432777192xfg8ma60919801:15840
Deerfield loamy fine sand, 0 to 3 percent slopes256A3537897382xfg8ma61019851:25000
Deerfield loamy fine sand, 0 to 3 percent slopes249A7878074232xfg8ma61319821:20000
Deerfield loamy fine sand, 3 to 8 percent slopes256B4707917012xfg9ma61619851:25000
Deerfield loamy fine sand, 0 to 3 percent slopes256A2457916992xfg8ma61619851:25000
Deerfield loamy fine sand, 3 to 8 percent slopesDeB139663156792xfg9me00519691:24000
Deerfield loamy fine sand, 0 to 3 percent slopesDeA33233156782xfg8me00519691:24000
Deerfield loamy fine sand, 0 to 8 percent slopesDeB20492844579k01me01119741:20000
Deerfield loamy fine sand, 0 to 3 percent slopes3136322810882xfg8nh00919861:24000
Deerfield loamy fine sand, 0 to 3 percent slopes313A67112793102xfg8nh01519861:24000
Deerfield loamy fine sand, 3 to 8 percent slopes313B35292793112xfg9nh01519861:24000
Deerfield loamy fine sand, 0 to 3 percent slopesDeA14412798662xfg8nh01719681:20000
Deerfield loamy fine sand, 3 to 8 percent slopesDeB7392798672xfg9nh01719681:20000
Deerfield loamy fine sand, 0 to 3 percent slopesDeA39082809682xfg8nh60119801:20000
Deerfield loamy fine sand, 3 to 8 percent slopesDeB9122809692xfg9nh60119801:20000
Deerfield loamy fine sand, 0 to 3 percent slopes313A22062801782xfg8nh60920071:24000
Deerfield fine sand, 0 to 3 percent slopesDeA9332901479qxlny01919951:24000
Deerfield fine sand, 3 to 8 percent slopesDeB5462901489qxmny01919951:24000
Deerfield loamy sand, 0 to 3 percent slopesDeA1131316475bm9wny03120071:24000
Deerfield loamy sand, 3 to 8 percent slopesDeB441316476bm9xny03120071:24000
Deerfield loamy fine sand, 3 to 8 percent slopesDeB215926682xfg9ny03520071:24000
Deerfield loamy fine sand, 0 to 8 percent slopesDeB97032918119sn8ny04519811:15840
Deerfield loamy fine sand, 0 to 6 percent slopesDeB33502941079w1bny07519731:15840
Deerfield loamy fine sand, 0 to 3 percent slopesDfA18525205312xfg8ny08520141:12000
Deerfield loamy fine sand, 0 to 3 percent slopesDeA50482943702xfg8ny09119931:24000
Deerfield loamy fine sand, 3 to 8 percent slopesDeB49232943712xfg9ny09119931:24000
Deerfield loamy fine sand, 0 to 3 percent slopesDe25082952332xfg8ny10319701:20000
Deerfield loamy fine sand, 0 to 3 percent slopesDc13402862312xfg8ri60019771:12000
Duane and Deerfield soils, 0 to 5 percent slopesDdA22932816839g3kvt00719691:15840
Duane and Deerfield soils, 5 to 12 percent slopesDdB11172816849g3lvt00719691:15840
Duane and Deerfield soils, 12 to 20 percent slopesDdC2882816859g3mvt00719691:15840
Deerfield loamy fine sand, 0 to 8 percent slopesDeB26802817879g6xvt01119761:20000
Deerfield loamy fine sand, 8 to 15 percent slopesDeC3462817889g6yvt01119761:20000
Deerfield loamy fine sand, 0 to 3 percent slopes59A30892823882xfg8vt02119851:20000
Deerfield loamy fine sand, 3 to 8 percent slopes9B9412820902xfg9vt02519841:20000

Map of Series Extent

Approximate geographic distribution of the DEERFIELD 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 .