Official Series Description


Lab Data Summary

Aggregate lab data for the DUTCHESS soil series. This aggregation is based on all pedons with a current taxon name of DUTCHESS, 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 DUTCHESS 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
144A40A052268VT003003Dutchess4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.273056,-73.1666641
144A40A051468VT021002Dutchess4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.416111,-73.2327805
144A40A051568VT021003Dutchess5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.4988899,-73.2319412
144A83P0117S1982VT003033Dutchess6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.7640266,-73.2063904
144B78P057178NH019009Dutchess7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.3138885,-72.3399963

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DUTCHESS 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 DUTCHESS 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 DUTCHESS 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 DUTCHESS 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 DUTCHESS 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 DUTCHESS 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 DUTCHESS 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 DUTCHESS, 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. 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).

  2. 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 DUTCHESS 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
Dutchess-Cardigan complex, 15 to 25 percent slopes141D2652790039cb3ma01120121:12000
Dutchess-Cardigan complex, 8 to 15 percent slopes141C1602790049cb4ma01120121:12000
Dutchess channery silt loam, 25 to 60 percent slopes, very stony471F1452790659cd3ma01120121:12000
Dutchess channery silt loam, 8 to 15 percent slopes470C1132789059c6yma01120121:12000
Dutchess channery silt loam, 15 to 25 percent slopes470D1112789069c6zma01120121:12000
Dutchess-Cardigan complex, 3 to 8 percent slopes141B862790059cb5ma01120121:12000
Dutchess channery silt loam, 3 to 8 percent slopes470B622789049c6xma01120121:12000
Dutchess channery silt loam, 3 to 15 percent slopes, very stony471C432789079c70ma01120121:12000
Dutchess channery silt loam, 15 to 25 percent slopes, very stony471D372790649cd2ma01120121:12000
Dutchess silt loam, 15 to 25 percent slopes, very stony367D31502796639d0dnh00519851:20000
Dutchess silt loam, 25 to 50 percent slopes, very stony367E25432796649d0fnh00519851:20000
Dutchess silt loam, 8 to 15 percent slopes, very stony367C22102796629d0cnh00519851:20000
Dutchess silt loam, 8 to 15 percent slopes366C13642796609d09nh00519851:20000
Dutchess silt loam, 15 to 25 percent slopes366D9232796619d0bnh00519851:20000
Dutchess silt loam, 3 to 8 percent slopes366B5682796599d08nh00519851:20000
Dutchess stony silt loam, 15 to 25 percent slopesDuD27442797609d3jnh01919811:20000
Dutchess stony silt loam, 8 to 15 percent slopesDuC22192797599d3hnh01919811:20000
Dutchess stony silt loam, 25 to 50 percent slopesDuE13062797619d3knh01919811:20000
Dutchess silt loam, 8 to 15 percent slopesDtC9982797579d3fnh01919811:20000
Dutchess silt loam, 15 to 25 percent slopesDtD6872797589d3gnh01919811:20000
Dutchess silt loam, 3 to 8 percent slopesDtB6482797569d3dnh01919811:20000
Dutchess-Cardigan complex, rolling, rockyDwC317732906469rfpny02719921:24000
Dutchess-Cardigan complex, undulating, rockyDwB262742906459rfnny02719921:24000
Dutchess-Cardigan complex, hilly, rockyDwD89642906479rfqny02719921:24000
Dutchess silt loam, 8 to 15 percent slopesDuC30412906439rflny02719921:24000
Dutchess-Cardigan-Urban land complex, undulating, rockyDxB29922906489rfrny02719921:24000
Dutchess silt loam, 3 to 8 percent slopesDuB18552906429rfkny02719921:24000
Dutchess-Cardigan-Urban land complex, rolling, rockyDxC10592906499rfsny02719921:24000
Dutchess silt loam, 15 to 25 percent slopesDuD7492906449rfmny02719921:24000
Dutchess extremely stony loam, 3 to 15 percent slopesDsC8892812549fnqvt00119671:15840
Dutchess stony loam, 3 to 8 percent slopesDcB6312812519fnmvt00119671:15840
Dutchess extremely stony loam, 15 to 50 percent slopesDsE5282812559fnrvt00119671:15840
Nassau-Dutchess rocky complex, 3 to 8 percent slopesNaB4972812889fptvt00119671:15840
Nassau-Dutchess rocky complex, 8 to 15 percent slopesNaC3652812899fpvvt00119671:15840
Dutchess stony loam, 8 to 15 percent slopesDcC2862812529fnnvt00119671:15840
Nassau-Dutchess rocky complex, 15 to 25 percent slopesNaD2162812909fpwvt00119671:15840
Dutchess stony loam, 15 to 25 percent slopesDcD902812539fnpvt00119671:15840
Dutchess channery loam, 25 to 60 percent slopes, very stony47E221882815109fxzvt00319921:20000
Dutchess channery loam, 15 to 25 percent slopes, very stony47D71132815099fxyvt00319921:20000
Dutchess channery loam, 8 to 15 percent slopes, very stony47C24802815089fxxvt00319921:20000
Dutchess channery loam, 15 to 25 percent slopes44D19662814999fxmvt00319921:20000
Dutchess channery loam, 8 to 15 percent slopes44C16892814989fxlvt00319921:20000
Dutchess channery loam, 3 to 8 percent slopes44B3382814979fxkvt00319921:20000
St. Albans-Dutchess rocky loams, 3 to 8 percent slopesSbB3502792749clvvt01319561:20000
St. Albans-Dutchess rocky loams, 8 to 15 percent slopesSbC352792759clwvt01319561:20000
St. Albans-Dutchess very rocky loams, 15 to 25 percent slopesScD102792779clyvt01319561:20000
St. Albans-Dutchess very rocky loams, 3 to 8 percent slopesScB82792769clxvt01319561:20000
St. Albans-Dutchess loams, 3 to 8 percent slopesSaB72792739cltvt01319561:20000
Dutchess silt loam, 25 to 60 percent slopes, very stony47E57912823529gt4vt02119851:20000
Dutchess silt loam, 15 to 25 percent slopes, very stony47D40472823519gt3vt02119851:20000
Macomber-Dutchess complex, 3 to 8 percent slopes52B33332823729gtsvt02119851:20000
Dutchess silt loam, 8 to 15 percent slopes44C25602823409gsrvt02119851:20000
Dutchess silt loam, 8 to 15 percent slopes, very stony47C21942823509gt2vt02119851:20000
Dutchess silt loam, 15 to 25 percent slopes44D11132823419gssvt02119851:20000
Dutchess silt loam, 3 to 8 percent slopes44B11012823399gsqvt02119851:20000
Dutchess silt loam, 3 to 8 percent slopes, very stony47B4142823499gt1vt02119851:20000

Map of Series Extent

Approximate geographic distribution of the DUTCHESS 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 .