Official Series Description


Lab Data Summary

Aggregate lab data for the BERNARDSTON soil series. This aggregation is based on all pedons with a current taxon name of BERNARDSTON, 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 BERNARDSTON 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
144A40A05211968VT003002Bernardston6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.2397232,-73.2513885
144A40A05171968VT021005Bernardston6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.4905548,-73.2413864
144A80P04141980VT021007Bernardston7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.5530548,-73.1011124
144A81P0746S1981VT021002Bernardston6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.5866661,-73.003891
144B78P05691978NH005024Bernardston6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.893055,-72.4888916
14540A1246S1977NH019001Bernardston6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.3686104,-72.2866669
14593P0700S1993MA011002Bernardston7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.5877762,-72.5363922
n/a40A1177S1969NY115006Bernardston7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BERNARDSTON 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 BERNARDSTON 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 BERNARDSTON 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 BERNARDSTON 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 BERNARDSTON 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 BERNARDSTON 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 BERNARDSTON 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 BERNARDSTON, 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. MA-2012-02-02-25 | Plymouth County - 1969

    Relationship of soils to topography and underlying material in association 2 (Soil Survey of Plymouth County, Massachusetts; 1969).

  3. 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).

  4. 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).

  5. 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).

  6. 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).

Map Units

Map units containing BERNARDSTON 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
Bernardston silt loam, 8 to 15 percent slopes80C54533958259lr0ct60120031:12000
Bernardston silt loam, 15 to 25 percent slopes, extremely stony81D50133958279lr2ct60120031:12000
Bernardston silt loam, 3 to 15 percent slopes, extremely stony81C44433958269lr1ct60120031:12000
Bernardston silt loam, 3 to 8 percent slopes80B43833958249lqzct60120031:12000
Bernardston silt loam, 25 to 45 percent slopes, very stony331F7492788499c54ma01120121:12000
Bernardston silt loam, 8 to 15 percent slopes330C6452788449c4zma01120121:12000
Bernardston silt loam, 15 to 25 percent slopes330D4502788459c50ma01120121:12000
Bernardston silt loam, 15 to 25 percent slopes, very stony331D3362788489c53ma01120121:12000
Bernardston silt loam, 3 to 8 percent slopes330B2492788439c4yma01120121:12000
Bernardston silt loam, 3 to 8 percent slopes, very stony331B2362788469c51ma01120121:12000
Bernardston silt loam, 8 to 15 percent slopes, very stony331C1732788479c52ma01120121:12000
Bernardston very fine sandy loam, 15 to 25 percent slopes330D1395796426vqr5ma01719911:24000
Bernardston very fine sandy loam, 3 to 8 percent slopes330B1141796424vqr3ma01719911:24000
Bernardston very fine sandy loam, 8 to 15 percent slopes330C819276859992yma01719911:24000
Bernardston very fine sandy loam, 25 to 35 percent slopes330E636796427vqr6ma01719911:24000
Bernardston silt loam, 15 to 25 percent slopes, very stony331D47482796419czpnh00519851:20000
Bernardston silt loam, 8 to 15 percent slopes330C37592796389czlnh00519851:20000
Bernardston silt loam, 25 to 50 percent slopes, very stony331E36922796429czqnh00519851:20000
Bernardston silt loam, 15 to 25 percent slopes330D36702796399czmnh00519851:20000
Bernardston silt loam, 3 to 8 percent slopes330B12862796379czknh00519851:20000
Bernardston silt loam, 8 to 15 percent slopes, very stony331C12722796409cznnh00519851:20000
Bernardston silt loam, 15 to 25 percent slopes, very stony331D45082810959fhlnh00919861:24000
Bernardston silt loam, 8 to 15 percent slopes, very stony331C37142810949fhknh00919861:24000
Bernardston silt loam, 8 to 15 percent slopes330C20102810919fhgnh00919861:24000
Bernardston silt loam, 25 to 35 percent slopes, very stony331E17242810969fhmnh00919861:24000
Bernardston silt loam, 15 to 25 percent slopes330D10592810929fhhnh00919861:24000
Bernardston silt loam, 3 to 8 percent slopes330B8262810909fhfnh00919861:24000
Bernardston silt loam, 3 to 8 percent slopes, very stony331B3492810939fhjnh00919861:24000
Bernardston silt loam, 8 to 15 percent slopesBdC27942797389d2tnh01919811:20000
Bernardston stony silt loam, 15 to 25 percent slopesBeD26452797429d2ynh01919811:20000
Bernardston stony silt loam, 8 to 15 percent slopesBeC20322797419d2xnh01919811:20000
Bernardston silt loam, 3 to 8 percent slopesBdB19062797379d2snh01919811:20000
Bernardston silt loam, 15 to 25 percent slopesBdD14682797399d2vnh01919811:20000
Bernardston stony silt loam, 25 to 50 percent slopesBeE12142797439d2znh01919811:20000
Bernardston stony silt loam, 3 to 8 percent slopesBeB3662797409d2wnh01919811:20000
Bernardston silt loam, 8 to 15 percent slopesBeC49932903069r2qny02119851:15840
Bernardston silt loam, 15 to 25 percent slopesBeD24792903079r2rny02119851:15840
Bernardston silt loam, 25 to 35 percent slopesBeE12712903089r2sny02119851:15840
Bernardston silt loam, 3 to 8 percent slopesBeB9282903059r2pny02119851:15840
Bernardston silt loam, 8 to 15 percent slopesBeC81722906149rdnny02719921:24000
Bernardston silt loam, 15 to 25 percent slopesBeD48192906159rdpny02719921:24000
Bernardston silt loam, 3 to 8 percent slopesBeB23282906139rdmny02719921:24000
Bernardston-Urban land complex, 3 to 8 percent slopesBgB6282906179rdrny02719921:24000
Bernardston silt loam, 25 to 45 percent slopesBeE2482906169rdqny02719921:24000
Bernardston gravelly silt loam, 15 to 25 percent slopesBeD245882931429v16ny08319801:15840
Bernardston-Nassau complex, rollingBnC140682931479v1cny08319801:15840
Bernardston gravelly silt loam, 8 to 15 percent slopesBeC95962931419v15ny08319801:15840
Bernardston-Nassau complex, hillyBnD82592931489v1dny08319801:15840
Bernardston-Nassau complex, undulatingBnB75552931469v1bny08319801:15840
Bernardston very stony silt loam, 15 to 40 percent slopesBfD58462931459v19ny08319801:15840
Bernardston very stony silt loam, 3 to 15 percent slopesBfC55742931449v18ny08319801:15840
Bernardston gravelly silt loam, 25 to 35 percent slopesBeE44982931439v17ny08319801:15840
Bernardston-Pittstown association, moderately steepBoD24802931499v1fny08319801:15840
Bernardston gravelly silt loam, 3 to 8 percent slopesBeB23462931409v14ny08319801:15840
Pittstown-Bernardston association, slopingPuC17282931939v2vny08319801:15840
Bernardston-Manlius-Nassau complex, undulatingBnB32662943469w91ny09119931:24000
Bernardston-Manlius-Nassau complex, rollingBnC29462943479w92ny09119931:24000
Bernardston silt loam, 3 to 8 percent slopesBmB15782943439w8yny09119931:24000
Bernardston silt loam, 8 to 15 percent slopesBmC14552943449w8zny09119931:24000
Bernardston silt loam, 15 to 25 percent slopesBmD8902943459w90ny09119931:24000
Bernardston-Manlius-Nassau complex, hillyBnD6932943489w93ny09119931:24000
Bernardston gravelly silt loam, 8 to 15 percent slopesBnC176562959489xyqny11519721:20000
Bernardston gravelly silt loam, 15 to 25 percent slopesBnD131212959499xyrny11519721:20000
Bernardston gravelly silt loam, 3 to 8 percent slopesBnB114422959479xypny11519721:20000
Bernardston soils, steep and very steepBUF110482959449xylny11519721:20000
Bernardston-Nassau shaly silt loams, 8 to 15 percent slopesBrC109752959519xytny11519721:20000
Bernardston-Nassau shaly silt loams, rolling and hillyBSCK92772959429xyjny11519721:20000
Bernardston-Nassau shaly silt loams, 3 to 8 percent slopesBrB52902959509xysny11519721:20000
Bernardston very stony soils, gently sloping through moderately steepBTC41682959439xykny11519721:20000

Map of Series Extent

Approximate geographic distribution of the BERNARDSTON 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 .