Official Series Description


Lab Data Summary

Aggregate lab data for the DANFORTH soil series. This aggregation is based on all pedons with a current taxon name of DANFORTH, 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 DANFORTH 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
1432013NH6050642013NH605064Danforth1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0590389,-71.8375583
1432014NH6050322014NH605032Danforth1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0489889,-71.7917917
1432014NH6050472014NH605047Danforth1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0530222,-71.7895833
1432014NH6050832014NH605083Danforth1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0547278,-71.8274417
n/a04N0386ME-03-11-019-16Danforth5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a04N0385ME-03-11-019-17Danforth5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DANFORTH 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 DANFORTH 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 DANFORTH 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 DANFORTH 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 DANFORTH 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 DANFORTH 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 DANFORTH 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.

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

Soil series sharing subgroup-level classification with DANFORTH, 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 DANFORTH 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
Danforth channery silt loam, 3 to 8 percent slopesDaB2711532582x1djme60219671:20000
Danforth-Winnecook association, 3 to 15 percent slopes, rockyDWC473314830631ls7rme61220161:24000
Danforth very fine sandy loam, 3 to 15 percent slopes, extremely stonyDFC1896744554szrwme61220161:24000
Danforth channery silt loam, 8 to 15 percent slopes, extremely stonyDaC121214829811ls53me61220161:24000
Danforth-Monadnock complex , 3 to 15 percent slopes, extremely stonyDMC619744556szryme61220161:24000
Danforth channery silt loam, 3 to 8 percent slopesDaB571741218sw98me61220161:24000
Danforth-Masardis-Peacham association, 0 to 15 percent slopes, extremely stonyDEC259062853212x1dpme61519941:24000
Danforth channery silt loam, 3 to 15 percent slopes, extremely stonyDBC143532853192x1dkme61519941:24000
Danforth channery silt loam, 15 to 25 percent slopes, extremely stonyDBD20632853202x1dlme61519941:24000
Danforth channery silt loam, 3 to 8 percent slopesDaB9732853242x1djme61519941:24000
Danforth-Elliottsville association, 3 to 15 percent slopes, extremely stonyDAC13442855582x1dmme61720041:24000
Danforth-Elliottsville association, 3 to 15 percent slopes, extremely stonyDEC454552856632x1dmme61920051:24000
Masardis-Danforth-Peacham association, 0 to 15 percent slopes, extremely stonyMMC319652856622x1dhme61920051:24000
Danforth-Elliottsville association, 15 to 30 percent slopes, extremely stonyDED100982856642x1dnme61920051:24000
Danforth-Masardis-Peacham association, 0 to 15 percent slopes, extremely stonyDMB2534325498962x1dpme62020111:24000
Danforth-Ragmuff association, 3 to 15 percent slopes, extremely stonyDAC816925498982x1dqme62020111:24000
Danforth and Masardis soils, 3 to 15 percent slopes, extremely stonyDMC319025498972qtllme62020111:24000
Danforth-Monson association, 15 to 35 percent slopes, extremely stonyDME130525498992x1drme62020111:24000
Danforth-Masardis-Peacham association, 0 to 15 percent slopes, extremely stonyDMB2198625498452x1dpme62120111:24000
Danforth-Ragmuff association, 3 to 15 percent slopes, extremely stonyDAC1226425498492x1dqme62120111:24000
Danforth and Masardis soils, 3 to 15 percent slopes, extremely stonyDMC540225498812qtk1me62120111:24000
Danforth-Monson association, 15 to 35 percent slopes, extremely stonyDME211625498502x1drme62120111:24000
Danforth-Elliottsville association, 3 to 15 percent slopes, extremely stonyDEC2574519090862x1dmme62220071:24000
Danforth-Masardis-Peacham association, 0 to 15 percent slopes, extremely stonyDMC354919089782x1dpme62220071:24000

Map of Series Extent

Approximate geographic distribution of the DANFORTH 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 .