Official Series Description


Lab Data Summary

Aggregate lab data for the PITTSTOWN soil series. This aggregation is based on all pedons with a current taxon name of PITTSTOWN, 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 PITTSTOWN 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
144A40A049356NH017001Pittstown4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.3194427,-70.9458313
144A1982MA027001S1982MA027001Pittstown3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.4982167,-71.5638806
144B78P056778NH005025Pittstown7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.9488907,-72.4499969
144B78P057278NH019010Pittstown7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.3133316,-72.3483353
144B40A0604S1959NH019001Pittstown5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1834101,-72.3645322
14540A0483S1958NH019001Pittstown6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.3764623,-72.3889786

Water Balance

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

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Competing Series

Soil series competing with PITTSTOWN 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 PITTSTOWN 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 PITTSTOWN 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.

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Soil series sharing subgroup-level classification with PITTSTOWN, 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-2010-09-10-01 | Middlesex County - 2009

    A typical pattern of soils and underlying material in the Bernardston-Pittstown general soil map unit (Soil Survey of Middlesex County, Massachusetts; 2009).

  2. NH-2012-02-14-04 | Cheshire County - June 1989

    Typical landscape pattern of soils and underlying material in the Bernardston-Cardigan-Kearsarge-Dutchess general soil map unit (Soil Survey of Cheshire County, New Hampshire; June 1989).

  3. NH-2012-02-14-09 | Grafton County Area - 1999

    Typical pattern of soils and underlying material in the Bernardston-Cardigan-Pittstown unit (Soil Survey of Grafton County Area, New Hampshire; 1999).

  4. NY-2012-02-15-15 | Columbia County - June 1989

    Typical pattern of Pittstown, Bernardston, Nassau, and Manlius soils on uplands and Hoosic soils on outwash plains (Soil Survey of Columbia County, New York; June 1989).

  5. NY-2012-02-15-39 | Rensselaer County - January 1988

    Typical relationship of soils and underlying material in the Bernardston-Pittstown-Nassau general soil map unit (Soil Survey of Rensselaer County, New York; January 1988).

  6. VT-2012-03-22-07 | Rutland County - 1998

    Typical pattern of soils and underlying material in the Dutchess-Bomoseen-Pittstown unit (Soil Survey of Rutland County, VT; 1998).

Map Units

Map units containing PITTSTOWN 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
Pittstown silt loam, 3 to 8 percent slopes345B3552789389c80ma01120121:12000
Pittstown silt loam, 3 to 8 percent slopes, very stony346B1482790919cdyma01120121:12000
Pittstown silt loam, 8 to 15 percent slopes345C382789379c7zma01120121:12000
Pittstown silt loam, 8 to 15 percent slopes, very stony346C142790909cdxma01120121:12000
Pittstown silt loam, 3 to 8 percent slopes345B1521276871993bma01719911:24000
Pittstown silt loam, 0 to 3 percent slopes345A792768709939ma01719911:24000
Pittstown loam, 3 to 8 percent slopes, very stony346B290309397bcykma02320101:12000
Pittstown loam, 3 to 8 percent slopes345B223309395bcyhma02320101:12000
Pittstown loam, 0 to 3 percent slopes345A217309396bcyjma02320101:12000
Pittstown loam, 0 to 3 percent slopes, very stony346A187309394bcygma02320101:12000
Pittstown loam, 0 to 8 percent slopes, very stony346B202780075v5qqma60319791:20000
Pittstown loam, 0 to 8 percent slopes345B134780069v5qjma60319791:20000
Pittstown silt loam, 2 to 8 percent slopes345B325791784vkxfma61619851:25000
Pittstown silt loam, 8 to 15 percent slopes, very stony336C24902796469czvnh00519851:20000
Pittstown silt loam, 3 to 8 percent slopes334B20002796439czrnh00519851:20000
Pittstown silt loam, 3 to 8 percent slopes, very stony336B18562796459cztnh00519851:20000
Pittstown silt loam, 8 to 15 percent slopes334C8382796449czsnh00519851:20000
Pittstown loam, 8 to 15 percent slopes, very stony336C42502811009fhrnh00919861:24000
Pittstown loam, 3 to 8 percent slopes334B22912810979fhnnh00919861:24000
Pittstown loam, 3 to 8 percent slopes, very stony336B22272810999fhqnh00919861:24000
Pittstown loam, 8 to 15 percent slopes334C13672810989fhpnh00919861:24000
Pittstown loam, 15 to 25 percent slopes, very stony336D5712811019fhsnh00919861:24000
Pittstown stony silt loam, 8 to 15 percent slopesPvC21922798219d5hnh01919811:20000
Pittstown silt loam, 3 to 8 percent slopesPtB21732798189d5dnh01919811:20000
Pittstown stony silt loam, 3 to 8 percent slopesPvB20812798209d5gnh01919811:20000
Pittstown silt loam, 8 to 15 percent slopesPtC6172798199d5fnh01919811:20000
Pittstown silt loam, 0 to 3 percent slopesPtA2142798179d5cnh01919811:20000
Pittstown silt loam, 8 to 15 percent slopesPtC56332902759r1qny02119851:15840
Pittstown silt loam, 3 to 8 percent slopesPtB31892902749r1pny02119851:15840
Pittstown silt loam, 15 to 25 percent slopesPtD13562902769r1rny02119851:15840
Pittstown silt loam, 3 to 8 percent slopesPwB44362907079rhnny02719921:24000
Pittstown silt loam, 8 to 15 percent slopesPwC18872907089rhpny02719921:24000
Pittstown gravelly silt loam, 8 to 15 percent slopesPtC226832931929v2tny08319801:15840
Pittstown gravelly silt loam, 3 to 8 percent slopesPtB117232931919v2sny08319801:15840
Bernardston-Pittstown association, moderately steepBoD24802931499v1fny08319801:15840
Pittstown-Bernardston association, slopingPuC17282931939v2vny08319801:15840
Scriba-Pittstown association, gently slopingSvB2382932069v38ny08319801:15840
Pittstown silt loam, 3 to 8 percent slopesPwB6202944189wccny09119931:24000
Pittstown silt loam, 0 to 3 percent slopesPwA3142944179wcbny09119931:24000
Pittstown silt loam, 0 to 3 percent slopesPmA58232862719lwkri60019771:12000
Pittstown silt loam, 3 to 8 percent slopesPmB54892862729lwlri60019771:12000
Pittstown very stony silt loam, 0 to 8 percent slopesPnB12442862739lwmri60019771:12000
Pittstown loam, 8 to 15 percent slopes48C37882815129fy1vt00319921:20000
Pittstown loam, 15 to 25 percent slopes, very stony49D26742815189fy7vt00319921:20000
Pittstown loam, 8 to 15 percent slopes, very stony49C26462815179fy6vt00319921:20000
Pittstown loam, 15 to 25 percent slopes48D8262815139fy2vt00319921:20000
Pittstown loam, 3 to 8 percent slopes48B5792815119fy0vt00319921:20000
Bomoseen and Pittstown soils, 8 to 15 percent slopes148C64942821909gmxvt02119851:20000
Bomoseen and Pittstown soils, 15 to 25 percent slopes, very stony149D49572821949gn1vt02119851:20000
Bomoseen and Pittstown soils, 8 to 15 percent slopes, very stony149C49452821939gn0vt02119851:20000
Bomoseen and Pittstown soils, 2 to 8 percent slopes148B39242821899gmwvt02119851:20000
Bomoseen and Pittstown soils, 15 to 25 percent slopes148D37862821919gmyvt02119851:20000
Bomoseen and Pittstown soils, 25 to 40 percent slopes, very stony149E21062821959gn2vt02119851:20000
Bomoseen and Pittstown soils, 3 to 8 percent slopes, very stony149B16202821929gmzvt02119851:20000

Map of Series Extent

Approximate geographic distribution of the PITTSTOWN 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 .