Official Series Description


Lab Data Summary

Aggregate lab data for the ELNORA soil series. This aggregation is based on all pedons with a current taxon name of ELNORA, 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 ELNORA 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.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
13903N0672S2003OH085001Elnora7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.8000068664551,-81.0666732788086
n/aAB-0661955-OH007-066Elnora2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

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Click the image to view it full size.

Competing Series

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

Click the image to view it full size.

Geomorphic description summaries for the ELNORA 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.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with ELNORA, 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. NY-2012-02-15-37 | Niagara County - October 1972

    Typical cross section of the Otisville-Altmar-Fredon-Stafford association (Soil Survey of Niagara County, New York; October 1972).

  2. OH-2010-09-29-02 | Ashtabula County - 2007

    Representative pattern of soils and parent materials in the Conneaut-Painesville-Elnora association (Soil Survey of Ashtabula County, Ohio; 2007).

  3. OH-2012-02-16-11 | Ashtabula County - May 1973

    Soil pattern in the Elnora-Colonie-Kingsville soil association (Soil Survey of Ashtabula County, Ohio; May 1973).

  4. OH-2012-02-16-12 | Ashtabula County - May 1973

    Soil pattern in the Conneaut-Swanton-Claverack soil association (Soil Survey of Ashtabula County, Ohio; May 1973).

Map Units

Map units containing ELNORA 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
Elnora loamy fine sand, 0 to 3 percent slopesEnA45882887239pfnny00119851:15840
Elnora loamy fine sand, 3 to 8 percent slopesEnB22432887249pfpny00119851:15840
Elnora fine sandy loam, 0 to 3 percent slopes42A3392896039qc1ny00920021:24000
Elnora fine sandy loam, 3 to 8 percent slopes42B2792896049qc2ny00920021:24000
Elnora fine sandy loam, 3 to 8 percent slopesElB15842898239ql4ny01319881:15840
Elnora fine sandy loam, 0 to 3 percent slopesElA10042898229ql3ny01319881:15840
Elnora fine sandy loamEn5042903279r3dny02119851:15840
Elnora loamy fine sand, 0 to 3 percent slopesElA18062908019rlpny02919791:15840
Elnora loamy fine sand, 3 to 8 percent slopesElB17442908029rlqny02919791:15840
Elnora loamy fine sand, 2 to 6 percent slopesElB1513301702b3ybny03720041:24000
Elnora loamy fine sandEn8752925519tf4ny05319751:15840
Elnora loamy fine sand, 0 to 2 percent slopesElA41952926969tktny05519671:15840
Elnora loamy fine sand, 2 to 6 percent slopesElB25992926979tkvny05519671:15840
Elnora loamy fine sand, 0 to 3 percent slopes56A29751914311227zzny06920121:12000
Elnora loamy fine sand, 0 to 6 percent slopesElB67422940259vypny07319731:15840
Elnora loamy fine sandEn1602309568bd42ny09319731:15840
Elnora loamy fine sand, 0 to 2 percent slopesElA2752947169wnzny09919661:15840
Elnora loamy fine sand, 2 to 6 percent slopesElB2642947179wp0ny09919661:15840
Elnora loamy fine sandEn10492958789xwgny11319821:15840
Elnora loamy fine sand, 0 to 2 percent slopesElA37122957249xqhny11719721:15840
Elnora loamy fine sand, 2 to 6 percent slopesElB29082957259xqjny11719721:15840
Elnora loamy fine sand, 0 to 3 percent slopes56A1913250285227zzny12319481:12000
Elnora loamy fine sand, 3 to 8 percent slopesElB1482892669q05ny60519811:24000
Elnora loamy fine sand, 0 to 3 percent slopesElA392892659q04ny60519811:24000
Elnora loamy fine sand, 0 to 2 percent slopesElA26672929929twcny66419681:15840
Elnora loamy fine sand, 2 to 6 percent slopesElB12682929939twdny66419681:15840
Elnora loamy fine sand, 1 to 5 percent slopesEnB4414298888b10koh00720011:12000
Urban land-Elnora complex, 1 to 5 percent slopesUrB658298925b11roh00720011:12000
Urban land-Elnora complex, nearly levelUeA171052872729mxvoh03519781:15840
Elnora loamy fine sand, 0 to 4 percent slopesEnA63831721365s3soh04319981:12000
Elnora loamy fine sand, bedrock substratum, 0 to 4 percent slopesEoA7251721375s3toh04319981:12000
Elnora loamy fine sand, 1 to 3 percent slopesEnA5731679725msgoh07719881:15840
Elnora loamy fine sand, 0 to 4 percent slopesEmA7316059711qx4joh07719881:15840
Elnora loamy fine sand, 1 to 5 percent slopesEnB56152868119mfzoh08519761:15840
Elnora loamy fine sand, 1 to 3 percent slopesEnA2752877589nfjoh09319721:15840
Elnora loamy fine sand, 2 to 6 percent slopesEyB2602870359mp6oh15519861:15840
Elnora fine sandy loam, 3 to 8 percent slopesEnB168426330532rg6xpa04920121:12000
Elnora fine sandy loam, 0 to 3 percent slopesEnA164526330522rg6wpa04920121:12000
Urban land-Elnora complex, 0 to 8 percent slopesUlB86026330862rg7zpa04920121:12000

Map of Series Extent

Approximate geographic distribution of the ELNORA 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 .