Official Series Description


Lab Data Summary

Aggregate lab data for the THORNDIKE soil series. This aggregation is based on all pedons with a current taxon name of THORNDIKE, 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 THORNDIKE 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
14309N0149S08ME003007.ThorndikeThorndike6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.8929667,-68.8075028

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the THORNDIKE 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 THORNDIKE 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 THORNDIKE 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 THORNDIKE 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 terrace figure.

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Competing Series

Soil series competing with THORNDIKE 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 THORNDIKE 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 THORNDIKE 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 terrace figure.

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

Soil series sharing subgroup-level classification with THORNDIKE, 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-2010-09-03-02 | Franklin County Area and Part of Somerset County - 2003

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

Map Units

Map units containing THORNDIKE 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
Thorndike-Winnecook complex, 8 to 15 percent slopes, rockyThC113932845882wqn5me02719791:20000
Thorndike-Winnecook complex, 3 to 8 percent slopes, rockyThB70342845872wqn4me02719791:20000
Thorndike-Rock outcrop complex, 8 to 15 percent slopes, very stonyTkC30262845912wqn0me02719791:20000
Thorndike-Winnecook complex, 15 to 35 percent slopes, very rockyThD26832845892wqn6me02719791:20000
Thorndike-Rock outcrop complex, 15 to 45 percent slopes, very stonyTkE20942845922w3zsme02719791:20000
Thorndike-Rock outcrop complex, 3 to 8 percent slopes, very stonyTkB8792845902wqmyme02719791:20000
Thorndike silt loam, 3 to 15 percent slopes, very rockyTkC202332847972wqmkme60219671:20000
Thorndike-Bangor silt loams, 0 to 8 percent slopesTtB195782848029kc5me60219671:20000
Thorndike-Bangor silt loams, 8 to 15 percent slopesTtC80452848039kc6me60219671:20000
Thorndike silt loam 15 to 30 percent slopes, very rockyTkD74632847982wqm9me60219671:20000
Thorndike-Plaisted association, 8 to 15 percent slopes, rockyTpC70092848002wqmwme60219671:20000
Thorndike-Plaisted association, 0 to 8 percent slopes, rockyTpB63002847992wqmvme60219671:20000
Rock outcrop-Thorndike-Lyman association, 15 to 45 percent slopes, very stonyRtE15202847912w3zvme60219671:20000
Rock outcrop-Thorndike-Lyman association, 0 to 15 percent slopes, very stonyRtC10042847902w3ztme60219671:20000
Thorndike-Plaisted association, 15 to 30 percent slopes, rockyTpD8632848012wqn7me60219671:20000
Thorndike-Bangor silt loams, 15 to 30 percent slopesTtD7922848049kc7me60219671:20000
Thorndike channery silt loam, 8 to 15 percent slopes, rockyThC772973018852t0k6me60719601:20000
Thorndike channery silt loam, 15 to 25 percent slopes, very rockyThD501443018862wqm4me60719601:20000
Thorndike channery silt loam, 0 to 8 percent slopes, rockyThB193443018842t0k5me60719601:20000
Thorndike channery silt loam, 25 to 45 percent slopes, very rockyThE150743018872wqm7me60719601:20000
Thorndike-Howland association, 8 to 15 percent slopes, very rockyTsC144613018942wqmhme60719601:20000
Thorndike-Howland association, 0 to 8 percent slopes, very rockyTsB62173018932wqmcme60719601:20000
Thorndike silt loam 15 to 30 percent slopes, very rockyTkD56373018902wqm9me60719601:20000
Rock outcrop-Thorndike association, 25 to 45 percent slopes, very stonySb50713018782w3zrme60719601:20000
Thorndike silt loam, 25 to 45 percent slopes, very rockyTkE46473018912wqmbme60719601:20000
Thorndike silt loam, 8 to 15 percent slopes, very rockyTkC40953018892wqm8me60719601:20000
Thorndike-Rock outcrop complex, 15 to 45 percent slopes, very stonyTrE12393018922w3zsme60719601:20000
Thorndike silt loam, 0 to 8 percent slopes, very rockyTkB3693018882wqm0me60719601:20000
Thorndike channery silt loam, 8 to 15 percent slopes, rockyThC636076142102t0k6me60819621:20000
Thorndike channery silt loam, 0 to 8 percent slopes, rockyThB484026142092t0k5me60819621:20000
Thorndike-Howland association, 0 to 8 percent slopes, very rockyTsB243586142172wqmcme60819621:20000
Thorndike-Howland association, 8 to 15 percent slopes, very rockyTsC233296142182wqmhme60819621:20000
Thorndike channery silt loam, 15 to 25 percent slopes, very rockyThD204796142112wqm4me60819621:20000
Thorndike silt loam, 8 to 15 percent slopes, very rockyTkC65746142142wqm8me60819621:20000
Thorndike silt loam 15 to 30 percent slopes, very rockyTkD54796142152wqm9me60819621:20000
Thorndike silt loam, 0 to 8 percent slopes, very rockyTkB46666142132wqm0me60819621:20000
Thorndike channery silt loam, 25 to 45 percent slopes, very rockyThE19156142122wqm7me60819621:20000
Thorndike silt loam, 25 to 45 percent slopes, very rockyTkE14366142162wqmbme60819621:20000
Thorndike-Elliottsvillle complex, 3 to 15 percent slopes, very rockyTOC28342850632wqmgme61019921:20000
Elliottsville-Thorndike complex, 8 to 15 percent slopesEtC17172850072wqn2me61019921:20000
Elliottsville-Thorndike complex, 3 to 8 percent slopesEtB7632850062wqn1me61019921:20000
Thorndike-Elliottsville complex, 15 to 45 percent slopes, very rockyTOE5892850642wqmrme61019921:20000
Elliottsville-Thorndike complex, 15 to 25 percent slopes, very rockyEtD3242850082wqn3me61019921:20000
Winnecook-Thorndike complex, 3 to 15 percent slopes, rockyWkC1652851582w404me61119881:20000
Thorndike-Winnecook complex, 0 to 15 percent slopes, very rockyThC1512851502w409me61119881:20000
Winnecook-Thorndike complex,3 to 15 percent slopes, rockyWTC2760746079t1c2me61220161:24000
Thorndike-Winnecook complex, 3 to 15 percent slopes, rockyTwC785740933sw02me61220161:24000
Thorndike-Winnecook complex, 8 to 15 percent slopes, rockyTvC362352852912wqn5me61419601:20000
Thorndike-Winnecook complex, 3 to 8 percent slopes, rockyTvB341472852902wqn4me61419601:20000
Rock outcrop-Thorndike association, 15 to 25 percent slopes, very stonyRmD322732852612w3zqme61419601:20000
Thorndike channery silt loam, 0 to 8 percent slopes, rockyThB178752852842t0k5me61419601:20000
Thorndike-Winnecook complex, 15 to 35 percent slopes, very rockyTvD172422852922wqn6me61419601:20000
Thorndike silt loam, 0 to 8 percent slopes, very rockyTkB125112852882wqm0me61419601:20000
Thorndike silt loam, 8 to 15 percent slopes, very rockyTkC119672852892wqm8me61419601:20000
Thorndike channery silt loam, 8 to 15 percent slopes, rockyThC95122852852t0k6me61419601:20000
Rock outcrop-Thorndike association, 3 to 15 percent slopes, very stonyRmC82432852602w3zpme61419601:20000
Thorndike channery silt loam, 15 to 25 percent slopes, very rockyThD21392852862wqm4me61419601:20000
Thorndike channery silt loam, 25 to 45 percent slopes, very rockyThE1892852872wqm7me61419601:20000
Monarda-Howland-Thorndike complex, 3 to 15 percent slopes, very stonyMXB206392853442w3znme61519941:24000
Thorndike-Penquis complex, 3 to 25 percent slopes, very stonyTSC141902853712w408me61519941:24000
Thorndike-Abram complex, 3 to 20 percent slopes, very rockyTRC69562853702w3zxme61519941:24000
Thorndike-Penquis-Abram complex, 3 to 8 percent slopes, very rockyTtB40992853742w3zyme61519941:24000
Penquis-Thorndike complex, 3 to 8 percent slopes, rockyPhB34352853552t0k8me61519941:24000
Thorndike-Abram complex, 8 to 15 percent slopes, very rockyToC24092853732w3zwme61519941:24000
Penquis-Thorndike complex, 8 to 15 percent slopes, rockyPhC12242853562w401me61519941:24000
Winnecook-Thorndike complex, 15 to 45 percent slopes, very rockyWTE32725499542x1c4me62020111:24000
Winnecook-Thorndike complex, 15 to 45 percent slopes, very rockyWTE3031425498792x1c4me62120111:24000

Map of Series Extent

Approximate geographic distribution of the THORNDIKE 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 .