Official Series Description


Lab Data Summary

Aggregate lab data for the BARNSTABLE soil series. This aggregation is based on all pedons with a current taxon name of BARNSTABLE, 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 BARNSTABLE were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BARNSTABLE 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 BARNSTABLE 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 BARNSTABLE 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 BARNSTABLE 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 mountains figure.

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Competing Series

Soil series competing with BARNSTABLE 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 BARNSTABLE 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 BARNSTABLE 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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Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with BARNSTABLE, 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-2012-02-01-02 | Barnstable County - March 1993

    Relationship of soils, landscapes, and parent material between Sandy Neck to the north and Hyannis Harbor to the south. The diagram represents an area approximately 4 by 8 miles (Soil Survey of Barnstable County, Massachusetts; March 1993).

Map Units

Map units containing BARNSTABLE 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
Plymouth-Barnstable complex, hilly, extremely bouldery484D838827655398s2ma00119841:25000
Barnstable-Plymouth complex, rolling485C391027648798pyma00119841:25000
Barnstable-Plymouth-Nantucket complex, rolling, very bouldery494C336627649198q2ma00119841:25000
Plymouth-Barnstable complex, rolling, extremely bouldery484C311327655298s1ma00119841:25000
Plymouth-Barnstable complex, rolling, very bouldery483C295527655098rzma00119841:25000
Plymouth-Barnstable complex, hilly, very bouldery483D267027655198s0ma00119841:25000
Barnstable-Plymouth complex, rolling, very bouldery489C261927648998q0ma00119841:25000
Plymouth-Barnstable-Nantucket complex, hilly, very bouldery493D196027655498s3ma00119841:25000
Barnstable-Plymouth complex, rolling, bouldery488C158527648898pzma00119841:25000
Barnstable sandy loam, 3 to 8 percent slopes, very stony431B137327648498pvma00119841:25000
Barnstable-Plymouth-Nantucket complex, rolling490C84527649098q1ma00119841:25000
Barnstable sandy loam, 3 to 8 percent slopes430B54627648298psma00119841:25000
Barnstable sandy loam, 8 to 15 percent slopes, very stony431C31827648598pwma00119841:25000
Barnstable sandy loam, 15 to 25 percent slopes, very stony431D17427648698pxma00119841:25000
Barnstable sandy loam, 8 to 15 percent slopes430C16427648398ptma00119841:25000
Barnstable loamy sand, 3 to 8 percent slopes430B6892961099y3xma02320101:12000
Barnstable - Plymouth complex, 8 to 15 percent slopes486C649309508bd24ma02320101:12000
Barnstable loamy sand, 3 to 8 percent slopes, very stony431B5882961079y3vma02320101:12000
Barnstable - Plymouth complex, 3 to 8 percent slopes486B560309505bd21ma02320101:12000
Barnstable - Plymouth complex, 8 to 15 percent slopes, very bouldery483C529309509bd25ma02320101:12000
Barnstable - Plymouth complex, 15 to 35 percent slopes, very bouldery483E506319840bqtfma02320101:12000
Barnstable loamy sand, 8 to 15 percent slopes430C3502961049y3rma02320101:12000
Barnstable - Plymouth complex, 15 to 35 percent slopes486E247309507bd23ma02320101:12000
Barnstable loamy sand, 8 to 15 percent slopes, extremely bouldery433C2442961109y3yma02320101:12000
Barnstable loamy sand, 8 to 15 percent slopes, very stony431C1662961119y3zma02320101:12000
Barnstable loamy sand, 0 to 3 percent slopes430A1432961059y3sma02320101:12000
Barnstable loamy sand, 3 to 8 percent slopes, extremely bouldery433B1192961089y3wma02320101:12000

Map of Series Extent

Approximate geographic distribution of the BARNSTABLE 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 .