Official Series Description


Lab Data Summary

Aggregate lab data for the BELHAVEN soil series. This aggregation is based on all pedons with a current taxon name of BELHAVEN, 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 BELHAVEN 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 BELHAVEN 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 BELHAVEN 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 BELHAVEN 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 BELHAVEN 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 BELHAVEN 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 BELHAVEN series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the BELHAVEN 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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 BELHAVEN, 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. NC-2012-02-07-03 | Carteret County - September 1987

    In east-central Carteret County, the drainage and organic matter content of soils on the Pamlico Surface are influenced by position on the landscape (Soil Survey of Carteret County, North Carolina; September 1987).

  2. NC-2012-02-07-11 | Dare County - March 1992

    Landscape relationship among some mineral and organic soils on the mainland of Dare County (Soil Survey of Dare County, North Carolina; March 1992).

  3. NC-2012-02-07-35 | Pamlico County - August 1987

    The natural drainage and organic matter content of soils on the Pamlico Surface are influenced by position on the landscape (Soil Survey of Pamlico County, North Carolina; August 1987).

  4. VA-2012-05-10-07 | City of Chesapeake - 2007

    The dry edge effect on the water table of soils located in Northwest Park (Soil Survey of the City of Chesapeake, Virginia; 2007).

Map Units

Map units containing BELHAVEN 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
Belhaven muck, 0 to 2 percent slopes, rarely floodedBb31951115472v9n8nc01319861:24000
Belhaven muck, 0 to 2 percent slopesBaA120571117783r9rnc02919881:24000
Belhaven muck, 0 to 2 percent slopes, rarely floodedBH86841155702v9n8nc03119841:24000
Belhaven muck, 0 to 2 percent slopes, rarely floodedBvA386161109692v9n8nc05519871:24000
Belhaven muck, 0 to 2 percent slopesBeA64951159253wmjnc07319901:24000
Belhaven muck, 0 to 2 percent slopes, rarely floodedBmA197471132722v9n8nc09519961:24000
Belhaven muck, 0 to 2 percent slopes, frequently floodedBnA79011132733svznc09519961:24000
Belhaven muckBH118691161143wtmnc13719841:24000
Belhaven muck, 0 to 2 percent slopesBcA1051217222271vt3qnc13920061:24000
Belhaven muck, 0 to 2 percent slopes, rarely floodedBa236391152482v9n8nc17719851:24000
Belhaven muck, 0 to 2 percent slopes, rarely floodedBa257151162002v9n8nc18719791:24000
Pungo-Belhaven soils, 0 to 1 percent slopes, frequently ponded364358914450551khppva55020041:12000
Dorovan-Belhaven complex, 0 to 1 percent slopes, frequently flooded181464314450051khn2va55020041:12000
Belhaven muck21340012085541rkva80019791:15840

Map of Series Extent

Approximate geographic distribution of the BELHAVEN 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 .