Official Series Description


Lab Data Summary

Aggregate lab data for the BRAYTON soil series. This aggregation is based on all pedons with a current taxon name of BRAYTON, 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 BRAYTON 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
14309N0164S08ME021012.BraytonBRAYTON6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.9179722,-69.1575
14393P0069S1992VT019001Brayton6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.814167,-72.3766632
14393P0070S1992VT019002Brayton6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.8255539,-72.3438873
144B12N7813S11ME019001Brayton6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.9234167,-68.6833611
144B93P0835S1993VT005005Brayton7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.4536095,-72.0913925
144B93P0836S1993VT005006Brayton7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.4536095,-72.0922241

Water Balance

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

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

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Soil series sharing subgroup-level classification with BRAYTON, 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-2012-02-01-06 | Berkshire County - February 1988

    Typical pattern of soils and parent material in the Taconic-Macomber-Lanesboro general soil map unit (Soil Survey of Berkshire County, Massachusetts; February 1988).

  2. ME-2010-09-03-01 | Franklin County Area and Part of Somerset County - 2003

    Typical pattern of the soils and underlying material in the Dixfield-Colonel-Marlow general soil map unit (Soil Survey of Franklin County Area and Part of Somerset County, Maine; 2003).

  3. ME-2010-09-03-03 | Franklin County Area and Part of Somerset County - 2003

    Typical pattern of the soils and underlying material in the Tunbridge-Lyman-Abram general soil map unit (Soil Survey of Franklin County Area and Part of Somerset County, Maine; 2003).

  4. ME-2012-02-03-01 | Knox and Lincoln Counties - January 1987

    The typical pattern of the soils on the landscape and the underlying material and bedrock in the Peru-Tunbridge-Marlow map unit (Soil Survey of Knox and Lincoln Counties, Maine; January 1987).

  5. ME-2012-02-03-03 | Knox and Lincoln Counties - January 1987

    The typical pattern of the soils on the landscape and the underlying material and bedrock in the Boothbay-Swanville-Lyman map unit (Soil Survey of Knox and Lincoln Counties, Maine; January 1987).

  6. ME-2012-02-03-04 | Knox and Lincoln Counties - January 1987

    The typical pattern of the soils on the landscape and the underlying material and bedrock in the Peru-Swanville-Lyman map unit (Soil Survey of Knox and Lincoln Counties, Maine; January 1987).

  7. ME-2012-02-03-09 | Oxford County Area - March 1995

    Typical pattern of the soils and underlying material in the Colonel-Brayton-Skerry general soil map unit (Soil Survey of Oxford County Area, Maine; March 1995).

  8. ME-2012-02-03-14 | York County - June 1982

    Typical pattern of soils and underlying material in the Hermon-Lyman association (Soil Survey of York County, Maine; June 1982).

  9. ME-2012-02-03-21 | York County - June 1982

    Typical pattern of soils and underlying material in the Marlow-Brayton-Peru association (Soil Survey of York County, Maine; June 1982).

  10. VT-2012-03-22-15 | Windham County - February 1987

    Typical landscape pattern of soils and underlying material in the Dummerston-Macomber-Taconic general soil map unit (Soil Survey of Windham County, VT; 1987).

Map Units

Map units containing BRAYTON 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
Brayton-Loonmeadow complex, extremely stony44337703395930qwzkct60120031:12000
Brayton mucky silt loam, 0 to 8 percent slopes, very stony409B36133958749lslct60120031:12000
Brayton loam4421443395931qwzlct60120031:12000
Brayton silt loam, 0 to 8 percent slopes, very stony89B186527657298spma00319841:25000
Colonel-Brayton assocation, 0 to 8 percent slopes, very stonyCFB9685315664blgqme00519691:24000
Brayton-Peacham complex, gently sloping, very stonyBRB2426315770bll4me00519691:24000
Brayton-Peacham complex, very stonyBp1754315769bll3me00519691:24000
Brayton fine sandy loam, 0 to 8 percent slopes, very stonyBvB324962845332t0jkme02719791:20000
Brayton fine sandy loam, 0 to 8 percent slopesBtB24082845322t0jlme02719791:20000
Brayton extremely stony fine sandy loam, 0 to 8 percent slopesBxB14392845349k2jme02719791:20000
Brayton and Westbury very stony fine sandy loams, 0 to 8 percent slopesBsB448222846149k53me03119781:20000
Brayton and Westbury fine sandy loams, 0 to 8 percent slopesBrB30722846139k52me03119781:20000
Lyman-Brayton variant-Rock outcrop complex, 0 to 8 percent slopesLmB165682847052tsvnme60119831:20000
Brayton fine sandy loam, 0 to 8 percent slopes, very stonyBtB116382846902t0jkme60119831:20000
Brayton fine sandy loam, 0 to 8 percent slopesBsB12122846892t0jlme60119831:20000
Brayton fine sandy loam, 0 to 8 percent slopes, very stonyBvB811532532t0jkme60219671:20000
Brayton-Colonel association, 0 to 8 percent slopes, very stonyBSB364032849652ty7sme61019921:20000
Brayton-Peacham-Pondicherry association, 0 to 2 percent slopes, very stonyBTB338182849662w9r4me61019921:20000
Brayton fine sandy loam, 0 to 8 percent slopes, very stonyBrB59332849752t0jkme61019921:20000
Brayton fine sandy loam, 0 to 8 percent slopesBpB7632849742t0jlme61019921:20000
Brayton fine sandy loam, 8 to 15 percent slopes, very stonyBrC3332849762x1c2me61019921:20000
Peacham-Brayton complex, 0 to 8 percent slopes, very stonyPeB2862850469km1me61019921:20000
Brayton-Colonel association, 0 to 8 percent slopes, very stonyBSB340932850772ty7rme61119881:20000
Brayton fine sandy loam, 0 to 8 percent slopes, very stonyBgB122212850812t0jkme61119881:20000
Brayton-Colonel association, gently sloping, rubblyBTB58542850789kn2me61119881:20000
Lyman-Brayton-Schoodic complex, 3 to 15 percent slopes , rockyLHC43652851102tsw3me61119881:20000
Brayton fine sandy loam, 0 to 8 percent slopes, rubblyBhB15262850822x1c1me61119881:20000
Lyman-Brayton complex, 3 to 15 percent slopes, very stonyLgB11962851152tsw2me61119881:20000
Brayton fine sandy loam, 0 to 8 percent slopesBfB6762850802t0jlme61119881:20000
Brayton-Colonel complex, 0 to 8 percent slopes, very stonyBRB21956746267t1k4me61220161:24000
Colonel-Peru-Brayton complex, 0 to 8 percent slopes, very stonyCDB19535744551szrsme61220161:24000
Brayton-Peacham complex, 0 to 3 percent slopes, extremely stonyBPA11238744547szrnme61220161:24000
Brayton-Colonel-Lyman complex, 0 to 8 percent slopes, rockyBYB8357744552szrtme61220161:24000
Brayton-Colonel complex, 0 to 8 percent slopes, very stonyBcB157224819842p9q0me61220161:24000
Brayton-Peacham complex, gently sloping, very stonyBRB289642857369lb9me61319871:20000
Brayton-Peacham complex, very stonyBp13472857439lbjme61319871:20000
Colonel-Brayton-Peru association, 0 to 8 percent slopes, very stonyCPB650892853112ty7qme61519941:24000
Brayton-Peacham association, 0 to 8 percent slopes, extremely stonyBP132512853052ty7vme61519941:24000
Colonel-Brayton-Lyman complex, undulating, very stonyCQB87712853129kwmme61519941:24000
Brayton-Colonel association, 0 to 8 percent slopes, very stonyBRB503672855322ty7rme61720041:24000
Brayton-Colonel association, 0 to 8 percent slopes, extremely stonyBTB64642855339l3rme61720041:24000
Brayton fine sandy loam, 0 to 8 percent slopes, very stonyBnB14442855372t0jkme61720041:24000
Brayton-Colonel-Peru association, 0 to 8 percent slopes, extremely stonyBCB4440325499142trrlme62020111:24000
Brayton-Peacham association, 0 to 8 percent slopes, extremely stonyBPA3988225499162ty7vme62020111:24000
Colonel-Peru-Brayton association, 3 to 15 percent slopes, very boulderyCDB2971325499152trrrme62020111:24000
Brayton-Colonel-Skerry association, 0 to 8 percent slopes, extremely boulderyBSB1587925499002x9q9me62020111:24000
Brayton-Colonel-Ragmuff association, 0 to 8 percent slopes, extremely stonyBRB1152825499092qtlyme62020111:24000
Colonel-Peru-Brayton association, 3 to 15 percent slopes, very boulderyCDB1132625498562trrrme62120111:24000
Brayton-Colonel-Peru association, 0 to 8 percent slopes, extremely stonyBCB958425498552trrlme62120111:24000
Brayton-Peacham association, 0 to 8 percent slopes, extremely stonyBPA696325498572ty7vme62120111:24000
Colonel-Brayton-Peru association, 0 to 8 percent slopes, very stonyCLB8978819092882ty7qme62220071:24000
Colonel-Peru-Brayton association, 0 to 15 percent slopes, very stonyCNC5449519092892trrkme62220071:24000
Brayton-Peacham association, 0 to 8 percent slopes, extremely stonyBPA5408319092902ty7vme62220071:24000
Colonel-Skerry-Brayton association, 0 to 15 percent slopes, very stonyCOC2901619091792x9qdme62220071:24000
Brayton-Colonel association, 0 to 8 percent slopes, very stonyBLB1265019090922ty7rme62220071:24000
Brayton-Colonel association, 0 to 8 percent slopes, extremely stonyBNB63781909093222knme62220071:24000
Brayton-Colonel association, 0 to 8 percent slopes, rubblyBOB45861909275222rjme62220071:24000
Brayton stony loam, 0 to 3 percent slopesBea116802677525bmbzny03320181:24000
Brayton very stony loam, 0 to 8 percent slopesBfb54362677478bmc1ny03320181:24000
Brayton stony loam, 3 to 8 percent slopesBeb50412677434bmc0ny03320181:24000
Westbury and Brayton very stony very fine sandy loams, 8 to 15 percent slopesWoc4052677460bmgmny03320181:24000
Brayton very stony silt loam, nearly levelBrA103992931509v1gny08319801:15840
Brayton loam, 0 to 5 percent slopes, very stony51B3052815249fyfvt00319921:20000
Brayton loam, 0 to 5 percent slopes50B2682815229fycvt00319921:20000
Brayton-Cabot-Pinnebog association, rolling, very stony403C37212823149grxvt02119851:20000
Brayton loam, 8 to 15 percent slopes, very stony7C7862824609gxmvt02119851:20000
Brayton silt loam, 2 to 8 percent slopes, very stony75B18242820879gjlvt02519841:20000

Map of Series Extent

Approximate geographic distribution of the BRAYTON 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 .