Official Series Description


Lab Data Summary

Aggregate lab data for the ALLAGASH soil series. This aggregation is based on all pedons with a current taxon name of ALLAGASH, 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 ALLAGASH 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 ALLAGASH 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 ALLAGASH 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 ALLAGASH 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 ALLAGASH 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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Click the image to view it full size.

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Click the image to view it full size.

Competing Series

Soil series competing with ALLAGASH 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 ALLAGASH series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the ALLAGASH 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 .

Click the image to view it full size.

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.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with ALLAGASH, 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. ME-2010-09-03-05 | Franklin County Area and Part of Somerset County - 2003

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

  2. ME-2010-09-03-07 | Franklin County Area and Part of Somerset County - 2003

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

  3. ME-2010-09-03-08 | Franklin County Area and Part of Somerset County - 2003

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

  4. ME-2012-02-03-18 | York County - June 1982

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

Map Units

Map units containing ALLAGASH 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
Allagash fine sandy loam, 3 to 8 percent slopes281B20352786149bxkma61419931:25000
Allagash fine sandy loam, 8 to 15 percent slopes281C3592786159bxlma61419931:25000
Allagash very fine sandy loam, 3 to 8 percent slopesAlB23032846039k4rme03119781:20000
Allagash very fine sandy loam, 8 to 15 percent slopesAlC7712846049k4sme03119781:20000
Allagash fine sandy loam, 0 to 3 percent slopesAgA1782846809k77me60119831:20000
Allagash fine sandy loam, 8 to 15 percent slopesAgC782846829k79me60119831:20000
Allagash fine sandy loam, 3 to 8 percent slopesAgB322846819k78me60119831:20000
Allagash fine sandy loam, 3 to 8 percent slopesAgB1115325617q1tme60219671:20000
Allagash fine sandy loam, 2 to 8 percent slopesAgB4170301805b41nme60719601:20000
Allagash fine sandy loam, 0 to 2 percent slopesAgA1460301804b41mme60719601:20000
Allagash fine sandy loam, 8 to 15 percent slopesAgC1239301806b41pme60719601:20000
Allagash fine sandy loam, 15 to 35 percent slopesAgD678301807b41qme60719601:20000
Madawaska-Allagash association, gently slopingMDB26462850209kl6me61019921:20000
Allagash fine sandy loam, 3 to 8 percent slopesAgB12742849639kjcme61019921:20000
Allagash fine sandy loam, 0 to 3 percent slopesAgA3202849629kjbme61019921:20000
Allagash fine sandy loam, 8 to 15 percent slopesAgC3052849649kjdme61019921:20000
Allagash fine sandy loam, 8 to 15 percent slopesAgC23122851669kqxme61419601:20000
Allagash fine sandy loam, 2 to 8 percent slopesAgB16422851659kqwme61419601:20000
Allagash fine sandy loam, 15 to 25 percent slopesAgD5052851679kqyme61419601:20000
Allagash fine sandy loam, 0 to 2 percent slopesAgA592851649kqvme61419601:20000
Allagash-Adams complex, 3 to 15 percent slopesAHC11152852982x1cmme61519941:24000
Allagash very fine sandy loam, 0 to 8 percent slopesAgB8512853009kw7me61519941:24000
Allagash very fine sandy loam, 8 to 15 percent slopesAgC6102853019kw8me61519941:24000
Adams-Allagash complex, 15 to 25 percent slopesAFD5172852972x1crme61519941:24000
Allagash-Madawaska association, 0 to 8 percent slopesAMB140525498942qtlhme62020111:24000
Allagash-Madawaska association, 0 to 8 percent slopesAMB574325498422qtjxme62120111:24000
Allagash fine sandy loam, 3 to 8 percent slopes1027B837319673bqn1ny03520071:24000
Allagash fine sandy loam, 8 to 15 percent slopes1027C665319670bqmyny03520071:24000
Allagash fine sandy loam, 15 to 35 percent slopes1027E406319674bqn2ny03520071:24000
Allagash fine sandy loam, 8 to 15 percent slopes1027C12677583bqmyny04320181:24000
Allagash fine sandy loam, strongly slopingALC37912943289w8gny09119931:24000
Allagash fine sandy loam, nearly levelALA7522943279w8fny09119931:24000
Allagash fine sandy loam, steepALE3142943299w8hny09119931:24000
Allagash very fine sandy loam, 2 to 8 percent slopesAgB3582818839gb0vt01519791:20000

Map of Series Extent

Approximate geographic distribution of the ALLAGASH 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 .