Official Series Description


Lab Data Summary

Aggregate lab data for the BANGOR soil series. This aggregation is based on all pedons with a current taxon name of BANGOR, 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 BANGOR 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
14384P079284VT023008Bangor6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.080555,-72.7708359
144B80P036980VT023001Bangor7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.394722,-72.3169479
144B40A0394ME-55-10-019-01BANGOR5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.8685833,-69.273
144B40A0395ME-55-10-019-02BANGOR5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.0372222,-69.3027778
144B40A0396ME-55-10-019-03BANGOR4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.0103889,-69.2803056

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BANGOR 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 BANGOR 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 BANGOR 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 BANGOR 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 BANGOR 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 BANGOR 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 BANGOR 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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Soil series sharing subgroup-level classification with BANGOR, 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

No block diagrams are available.

Map Units

Map units containing BANGOR 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
Bangor very stony silt loam, 8 to 15 percent slopesBbC20592845229k24me02719791:20000
Bangor silt loam, 8 to 15 percent slopesBaC11042845199k21me02719791:20000
Bangor very stony silt loam, 3 to 8 percent slopesBbB10842845219k23me02719791:20000
Bangor silt loam, 3 to 8 percent slopesBaB8852845189k20me02719791:20000
Bangor very stony silt loam, 15 to 25 percent slopesBbD7162845239k25me02719791:20000
Bangor silt loam, 15 to 25 percent slopesBaD1862845209k22me02719791:20000
Thorndike-Bangor silt loams, 0 to 8 percent slopesTtB195782848029kc5me60219671:20000
Bangor silt loam, 3 to 8 percent slopesBaB144762847489k9fme60219671:20000
Bangor very stony silt loam, 3 to 8 percent slopesBgB100422847509k9hme60219671:20000
Thorndike-Bangor silt loams, 8 to 15 percent slopesTtC80452848039kc6me60219671:20000
Bangor very stony silt loam, 8 to 15 percent slopesBgC65192847519k9jme60219671:20000
Bangor silt loam, 8 to 15 percent slopes, erodedBaC233672847499k9gme60219671:20000
Bangor very stony silt loam, 15 to 25 percent slopesBgD15072847529k9kme60219671:20000
Thorndike-Bangor silt loams, 15 to 30 percent slopesTtD7922848049kc7me60219671:20000
Bangor very stony silt loam, 0 to 8 percent slopesBnB249242851759kr6me61419601:20000
Bangor very stony silt loam, 8 to 15 percent slopesBnC142462851769kr7me61419601:20000
Bangor silt loam, 2 to 8 percent slopesBaB62032851699kr0me61419601:20000
Bangor very stony silt loam, 15 to 25 percent slopesBnD58402851779kr8me61419601:20000
Bangor silt loam, moderately deep, 2 to 8 percent slopesBmB42652851729kr3me61419601:20000
Bangor silt loam, 8 to 15 percent slopesBaC22432851709kr1me61419601:20000
Bangor silt loam, moderately deep, 8 to 15 percent slopesBmC14792851739kr4me61419601:20000
Bangor silt loam, 0 to 2 percent slopesBaA6042851689kqzme61419601:20000
Bangor silt loam, moderately deep, 15 to 35 percent slopesBmD1292851749kr5me61419601:20000
Bangor silt loam, 15 to 25 percent slopesBaD1202851719kr2me61419601:20000
Dixmont-Bangor association, undulating, very stony779B45232806099dzxnh60720001:24000
Bangor-Dixmont association, undulating, very stony773B24562806069dztnh60720001:24000
Bangor-Dixmont association, hilly, very stony773D13442806079dzvnh60720001:24000
Bangor silt loam, 25 to 35 percent slopes, very stony573E11932805179dwynh60720001:24000
Dixmont-Bangor association, hilly, very stony779D8542806109dzynh60720001:24000
Bangor silt loam, 15 to 25 percent slopes, very stony573D7272805169dwxnh60720001:24000
Bangor silt loam, 8 to 15 percent slopes, very stony573C5442805159dwwnh60720001:24000
Bangor silt loam, 8 to 15 percent slopes572C5092805129dwsnh60720001:24000
Bangor silt loam, 15 to 25 percent slopes572D1872805139dwtnh60720001:24000
Bangor silt loam, 3 to 8 percent slopes572B1772805119dwrnh60720001:24000
Bangor-Tunbridge association, steep, very stony873E1642806569f1fnh60720001:24000
Bangor silt loam, 3 to 8 percent slopes, very stony573B1142805149dwvnh60720001:24000

Map of Series Extent

Approximate geographic distribution of the BANGOR 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 .