Official Series Description


Lab Data Summary

Aggregate lab data for the ENBAR soil series. This aggregation is based on all pedons with a current taxon name of ENBAR, 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 ENBAR 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 ENBAR 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 ENBAR 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 ENBAR 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 ENBAR 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 ENBAR 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 ENBAR 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 ENBAR 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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Soil series sharing subgroup-level classification with ENBAR, 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 ENBAR 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
Enbar-Nesda loams, 0 to 2 percent slopes832535342587chh6mt02719791:24000
Enbar loam, 0 to 2 percent slopes822172342586chh5mt02719791:24000
Enbar-Straw-Eagleton loams, 0 to 2 percent slopes833A4812344084ck1hmt04119941:24000
Enbar-Bigsandy-Korchea loams, 0 to 4 percent slopes493B5185344215ck5qmt05119921:24000
Enbar-Nesda loams, 0 to 4 percent slopes491B1326344214ck5pmt05119921:24000
Enbar-Bigsandy-Korchea loams, 0 to 4 percent slopes831B172345291cl9fmt10119921:24000
Enbar-Bowery-Nythar complex, 4 to 15 percent slopes512D51476704ynkmt60919711:24000
Enbar-Straw-Eagleton loams, 0 to 2 percent slopes493A4002346799cmw2mt61519921:24000
Enbar loam, 0 to 4 percent slopes509B441415554856vpmt62219971:24000
Enbar-Nythar loams, 0 to 4 percent slopes512B362315555456vwmt62219971:24000
Enbar-Nythar loams, cool, 0 to 4 percent slopes523A343015556956wcmt62219971:24000
Enbar-Bowery-Nythar complex, 4 to 15 percent slopes512D270915555556vxmt62219971:24000
Enbar clay loam, 0 to 2 percent slopes522A214515556756w9mt62219971:24000
Enbar-Nesda complex, 0 to 2 percent slopes, rarely flooded183A29325232371ndsxmt62420211:24000
Enbar-Nythar loams, cool, 0 to 4 percent slopes185211465504xhfmt63619831:24000
Enbar-Bowery-Nythar complex, 4 to 15 percent slopes512D11123775652kt1nmt63720141:24000
Enbar-Nythar complex, cool, 0 to 4 percent slopes523A21185853920cywmt63720141:24000
Enbar-Nesda complex, 0 to 2 percent slopes, rarely flooded183A33615316451ndsxmt66620081:24000
Enbar-Bowery-Nythar complex, 4 to 15 percent slopes512D85741462swk4mt6691:24000
Enbar-Straw-Dalecreek complex, 2 to10 percent slopesLVD229586712nczrut0131:24000

Map of Series Extent

Approximate geographic distribution of the ENBAR 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 .