Official Series Description


Lab Data Summary

Aggregate lab data for the EEL soil series. This aggregation is based on all pedons with a current taxon name of EEL, 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 EEL 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
111AWY78061978IN177006Eel3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.8380278,-84.8345806
111AHY80041980IN065004Eel3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.8440361,-85.4851
111A81P0724S1981IN011001Eel7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9876175,-86.2744141
111BAL-1121959-OH003-112Eel3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.742775,-84.3128891
111BDK77011977IN033001Eel3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3985861,-85.0213083
111BRA78141978IN135014Eel3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.2788417,-85.0722194
111BAD79031979IN001003Eel3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6004361,-84.9390028
111BJY80151980IN075015Eel3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3596389,-84.9529889
111D40A5243S1959IN045004Eel6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1803093,-87.4077835
99WD-1021957-OH173-102Eel3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.402916,-83.4943924
99DF-0381977-OH039-038Eel4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3663902,-84.4354401
n/aUN-0011953-OH159-001Eel4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aAL-0301954-OH003-030Eel3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aPB-0521960-OH135-052Eel2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWA-0511961-OH165-051Eel3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aDL-0431962-OH041-043Eel3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aSH-0191975-OH149-019Eel3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

Click the image to view it full size.

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Competing Series

Soil series competing with EEL 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 EEL 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 EEL 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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 EEL, 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. IN-2010-09-09-03 | Boone County - 2004

    General pattern of soils, topography, and parent material in the Miami-Rainsville-Crosby association (Soil Survey of Boone County, Indiana; 2004).

  2. IN-2012-01-19-17 | Fountain County - 1966

    Major soil series in the county in relation to their topography and underlying material (Soil Survey of Fountain County, Indiana; 1966).

  3. IN-2012-01-19-26 | Huntington County - December 1982

    Relationship of soils to topography and underlying materials in the Genesee-Ockley-Fox map unit (Soil Survey of Huntington County, Indiana; 1982).

  4. IN-2012-01-19-41 | Pulaski County - January 1968

    Topographical relationships between a few of the major soils in the county (Soil Survey of Pulaski County, Indiana; 1968).

  5. NY-2012-02-15-04 | Cayuga County - 1971

    Typical cross section of Honeoye-Lima association (Soil Survey of Cayuga County, New York; 1971).

  6. NY-2012-02-15-22 | Genesee County - March 1969

    Cross section showing typical soil pattern in the Palmyra association (Soil Survey of Genesee County, New York; March 1969).

  7. NY-2012-02-15-47 | Tompkins County - July 1965

    Typical cross section of Lima-Honeoye association and Palmyra association in northwestern Tompkins County (Soil Survey of Tompkins County, New York; July 1965).

  8. OH-2012-02-16-05 | Allen County - August 1965

    A schematic drawing that shows the relationship of the soils formed in alluvium to drainage and to the soils of the uplands (Soil Survey of Allen County, Ohio; August 1965).

  9. OH-2012-02-16-23 | Darke County - August 1987

    Typical pattern of soils and parent material in the Eldean-Eel-Medway association (Soil Survey of Darke County, Ohio; August 1987).

  10. OH-2012-02-16-28 | Delaware County - July 1969

    Major soils in the Bennington-Pewamo-Cardington soil association and their underlying material (Soil Survey of Delaware County, Ohio; July 1969).

  11. OH-2012-02-16-44 | Wood County - December 1966

    Relationship of some local soils to underlying material and relief (Soil Survey of Wood County, Ohio; December 1966).

Map Units

Map units containing EEL 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
Eel silt loam, 0 to 2 percent slopes, frequently floodedEs89511646852z6cwin00319651:15840
Eel loamEe4991646845jcdin00319651:15840
Eel loam, 0 to 2 percent slopes, frequently flooded, brief durationEcyAH17532008836r13in00520021:12000
Eel loam, 0 to 2 percent slopes, occasionally flooded, very brief durationEcyAW94320909270kxin00520021:12000
Eel silt loam, 0 to 2 percent slopes, occasionally flooded, very brief durationEdeAW1120906770k3in00520021:12000
Eel clay loam, frequently floodedEe919623790ny38in00919831:15840
Eel Variant silty clay, occasionally floodedEf274623791ny39in00919831:15840
Eel and Beckville soils, 0 to 2 percent slopes, occasionally flooded, very brief durationEdeAW3538697268rdkjin01120031:12000
Eel-Urban land-Beckville complex, 0 to 2 percent slopes, occasionally flooded, very brief durationYebA4331050572w57qin01120031:12000
Eel loam, frequently floodedEm19121603235ctqin03319801:15840
Gessie-Eel silt loams, 0 to 1 percent slopes, frequently flooded, brief durationGlnAH12511648505jjrin03519971:12000
Eel silt loam, 0 to 2 percent slopes, frequently floodedEs656616128292w0vgin04119581:15840
Eel loamEe88416128281r48qin04119581:15840
Eel and Beckville soils, 0 to 2 percent slopes, occasionally flooded, brief durationEdeAK5270242388846zin04519991:12000
Eel and Beckville soils, 0 to 2 percent slopes, occasionally flooded, very brief durationEdeAW283291291rdkjin05719761:15840
Eel silt loam, 0 to 2 percent slopes, frequently floodedEs232912982w0vgin05719761:15840
Eel silt loam, 0 to 2 percent slopes, frequently floodedEe20921608232w0vgin05919741:15840
Eel silt loam, 0 to 2 percent slopes, occasionally floodedEe28141614042ygzpin06919801:15840
Eel-Urban land complex, 0 to 2 percent slopes, occasionally floodedYeoAK3332168382zkflin06919801:15840
Eel clay loam, frequently floodedEe4616210637725rin07519831:15840
Eel variant silty clay, occasionally floodedEf786210638725sin07519831:15840
Eel silt loam, 0 to 2 percent slopes, frequently floodedEe36611616602w0vgin08119751:15840
Eel silt loam-Urban land complex, 0 to 2 percent slopes, frequently flooded, brief durationYelAH37531052292xf6hin08119751:15840
Eel silt loam, 0 to 2 percent slopes, occasionally flooded, very brief durationEdeAW11416527611sgtwin08119751:15840
Urban land-Eel silt loam complex, 0 to 2 percent slopes, frequently flooded, brief durationUelAH1531052282y479in08119751:15840
Eel loam, 0 to 2 percent slopes, frequently flooded, brief durationEcyAH1516527591sgttin08119751:15840
Eel silt loam, 0 to 2 percent slopes, frequently floodedEs39141620722w0vgin09519651:15840
Eel silt loam, 0 to 2 percent slopes, frequently floodedEe8841644202w0vgin09719751:15840
Eel silt loam-Urban land complex, 0 to 2 percent slopes, frequently flooded, brief durationYelAH69031046802xf6hin09719751:15840
Urban land-Eel silt loam complex, 0 to 2 percent slopes, frequently flooded, brief durationUelAH10831046792y479in09719751:15840
Eel silt loam, 0 to 2 percent slopes, frequently floodedEl72171597362w0vgin12119651:20000
Eel silty clay loamEn23001597385c6vin12119651:20000
Eel loamEa5661597345c6qin12119651:20000
Eel silt loam, high bottomEm4791597375c6tin12119651:20000
Eel loam, high bottomEb1001597355c6rin12119651:20000
Eel silt loam, frequently floodedEe62211612915dtyin13519841:15840
Eel silt loam, 0 to 2 percent slopes, frequently floodedEe20341607112w0vgin14519681:15840
Eel silt loamEs46571626675g8bin15319661:15840
Eel silt loam, 0 to 2 percent slopes, frequently floodedEs455416129782w0vgin16119581:15840
Eel loamEe23016129771r4fjin16119581:15840
Eel silt loamEe19701604285cy3in16519771:20000
Eel silt loam, 0 to 2 percent slopes, frequently floodedEe27071596622w0vgin16719711:20000
Eel silt loam, 0 to 2 percent slopes, frequently floodedEe6211612482z6cwin17919881:15840
Landes-Eel loamsLa139518801169mwmi06719651:15840
Landes-Eel sandy loamsLe38818801269mxmi06719651:15840
Genesee and Eel loams, 0 to 3 percent slopesGcA15041884836b43mi09119571:20000
Eel, Landes, and Abscota soils10922024224932m9symi14519911:15840
Eel, Landes, and Abscota soilsEn31818779369dvmi15519671:12000
Podunk and Eel fine sandy loams, 0 to 2 percent slopesPda6202677458bmf4ny03320181:24000
Podunk and Eel fine sandy loams, high bottoms, 0 to 2 percent slopesPea5712677481bmf5ny03320181:24000
Teel silt loam, 0 to 2 percent slopesEaA7252677661bmjpny04920181:24000
Eel silt loamEe7212947159wnyny09919661:15840
Eel silt loam, 0 to 2 percent slopes, occasionally floodedEe10601697532w0vcoh01719771:15840
Urban land-Eel complex, 0 to 2 percent slopes, occasionally floodedUEe119338107730tpgoh01719771:15840
Eel-Urban land complex, 0 to 2 percent slopes, occasionally floodedEeU113338107630tpfoh01719771:15840
Eel silt loam, 0 to 2 percent slopes, occasionally floodedEe6611714352w0vcoh02119661:15840
Eel silt loam, 0 to 2 percent slopes, occasionally floodedEe19571687842w0vcoh02519721:20000
Eel silt loam, occasionally floodedEe27291684985nbfoh03719841:15840
Eel silt loam, gravelly substratum, 0 to 1 percent slopes, occasionally floodedEfA6213921221hqm5oh03719841:15840
Eel loamEe22715397561np7koh03919811:15840
Eel silt loam, gravelly substratum, occasionally floodedEe35981722445s78oh04519981:12000
Eel silt loam, 0 to 2 percent slopes, occasionally floodedEe32331678942ygzpoh04919771:15840
Eel silt loam, 0 to 2 percent slopes, frequently floodedEe4291690792z6cwoh05119811:15840
Eel loamEe12311692935p52oh05719741:15840
Eel silt loam, 0 to 2 percent slopes, occasionally floodedEe14951689292ygzpoh06519871:15840
Eel loam, 0 to 2 percent slopes, frequently floodedEe215366351nkzwoh06919681:15840
Eel silt loam, 0 to 2 percent slopes, occasionally floodedEe406814204092w0vcoh07119731:15840
Eel silt loam, 0 to 2 percent slopes, occasionally floodedEe11281711092ygzpoh09119771:15840
Eel loam, occasionally floodedEe11471698405pqqoh09519781:15840
Eel silt loam, 0 to 2 percent slopes, occasionally floodedEe17681699282ygzpoh10719751:15840
Eel silt loam, 0 to 2 percent slopes, occasionally floodedEe11631694792w0vcoh10919731:15840
Eel silt loam, gravelly substratum, 0 to 1 percent slopes, occasionally floodedEeA615901091qcmvoh11319691:15840
Eel silt loam, occasionally floodedEe11961712545r6boh12919771:15840
Eel silt loam, gravelly substratum, 0 to 1 percent slopes, occasionally floodedEeA1763622559nwtkoh13520051:12000
Eel silt loam, 0 to 2 percent slopes, occasionally floodedEe25551700312ygzpoh14919771:15840
Eel-Urban land complex, 0 to 2 percent slopes, occasionally floodedEgA1032169332zkfloh14919771:15840
Eel silt loam, 0 to 2 percent slopes, occasionally floodedEe158714060662ygzpoh15919701:15840
Eel silt loam, 0 to 2 percent slopes, frequently floodedEm711680802z6cwoh16119671:15840
Eel loamEe6351713375r90oh16519671:20000
Eel loamEe18261681475mz3oh17119751:15840
Eel silt loam, 0 to 2 percent slopes, frequently floodedEmA24091682255n1moh17320001:12000
Eel loam, 0 to 2 percent slopes, frequently floodedEaA2511682245n1loh17320001:12000
Eel silt loam, moderately deep to limestone, 0 to 2 percent slopes, frequently floodedEnA1001682265n1noh17320001:12000

Map of Series Extent

Approximate geographic distribution of the EEL 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 .