Aggregate lab data for the SCARBORO soil series. This aggregation is based on all pedons with a current taxon name of SCARBORO, 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 SCARBORO were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE
Monthly water balance estimated using a leaky-bucket style model for the SCARBORO 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 SCARBORO series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-10-24), parsed OSD records (updated 2024-10-23) and snapshot of SC database (updated 2024-10-23).
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Select annual climate data summaries for the SCARBORO series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).
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Geomorphic description summaries for the SCARBORO 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 (updated 2024-10-23).
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Competing Series
Soil series competing with SCARBORO share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2024-10-23) and snapshot of the SC database (updated 2024-10-23).
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Select annual climate data summaries for the SCARBORO series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).
Click the image to view it full size.
Geomorphic description summaries for the SCARBORO 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 (updated 2024-10-23).
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Click the image to view it full size.
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 SCARBORO, 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 (updated 2024-10-23).
Block Diagrams
Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.
A typical pattern of soils and underlying material in the Hinckley-Freetown-Windsor association (Soil Survey of Middlesex County, Massachusetts; 2009).
A typical pattern of soils and underlying material in the Urban land-Merriac-Udorthents association (Soil Survey of Middlesex County, Massachusetts; 2009).
Typical pattern of soils and underlying material in the Hinckley-Freetown-Scarboro association (Soil Survey of Bristol County, Massachusetts, Southern Part; October 1981).
Typical pattern of soils and parent material in the Ipswich-Westbrook-Udipsamments association (Soil Survey of Essex County, Massachusetts, 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).
Typical pattern of soils and parent material in the Merrimac-Hinckley-Urban land association (Soil Survey of Essex County, Massachusetts, Southern Part; May 1984).
MA-2012-02-02-21 | Norfolk and Suffolk Counties - September 1989
Typical pattern of soils and underlying material in the Freetown-Swansea-Saco general soil map unit (Soil Survey of Norfolk and Suffolk Counties, Massachusetts; September 1989).
MA-2012-02-02-22 | Norfolk and Suffolk Counties - September 1989
Typical pattern of soils and underlying material in the Hinckley-Merrimac-Urban land general soil map unit (Soil Survey of Norfolk and Suffolk Counties, Massachusetts; September 1989).
Relationship of soils to topography and underlying material in associations 4 and 5 (Soil Survey of Plymouth County, Massachusetts; 1969).
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).
Typical pattern of soils and underlying material in the Merrimac-Hinckley-Windsor association (Soil Survey of Worcester County, Massachusetts, Southern Part; 1998).
Typical pattern of soils and underlying material in the Freetown-Swansea-Saco association (Soil Survey of Worcester County, Massachusetts, Southern Part; 1998).
Diagram of two typical landscapes, showing the varying influence of the five soil-forming factors on the major soils of the county (Soil Survey of Belknap County, New Hampshire; November 1968).
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).
Map Units
Map units containing SCARBORO as a major component. Limited to 250 records.
Approximate geographic distribution of the SCARBORO 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 (updated 2024-10-30).
