Official Series Description


Lab Data Summary

Aggregate lab data for the EDNA soil series. This aggregation is based on all pedons with a current taxon name of EDNA, 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 EDNA 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
150A40A442655TX157092Edna4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.5316658,-95.8000031
150A10N0612S09TX1574051Edna7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.4828892,-95.6953583
150A10N0607S2009TX0395300Edna8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.1475277,-95.7066422
150A10N0976S2010TX1575064Edna8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.4488888,-95.9492188

Water Balance

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

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.

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Competing Series

Soil series competing with EDNA 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 EDNA 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 EDNA 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 EDNA, 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. TX-2010-11-03-13 | Goliad County - 2010

    Pattern of soils and underlying material in the Telferner-Laewest-Edna general soil map unit (Soil Survey of Goliad County, Texas; 2010).

  2. TX-2010-11-04-02 | Matagorda County - 2001

    Typical pattern of soils and underlying material in the Brazoria-Norwood-Clemville general soil map unit (Soil Survey of Matagorda County, Texas; 2001).

  3. TX-2012-03-22-01 | Wharton County - March 1974

    Typical landscape of the soils in association 1 (Soil Survey of Wharton County, TX; 1974).

Map Units

Map units containing EDNA 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
Bernard-Edna complex, 0 to 1 percent slopes8490503630822v3cgtx03919791:20000
Edna loam, 0 to 1 percent slopes13379283630442v3cctx03919791:20000
Edna-Aris complex, 0 to 1 percent slopes15259823630462vv5qtx03919791:20000
Edna fine sandy loam, 1 to 3 percent slopes1454713630452v3cdtx03919791:20000
Edna loam, 0 to 1 percent slopesEd56793635502v3cctx05719721:20000
Edna very fine sandy loam, lowEn1104363551d69gtx05719721:20000
Edna loam, 0 to 1 percent slopesEdA24223642712v3cctx08919971:24000
Edna loam, 0 to 1 percent slopesEdA25553650562v3cctx12319731:20000
Edna loam, 0 to 1 percent slopesEa752333659332v3cctx15719561:20000
Bernard-Edna complex, 0 to 1 percent slopesBe594083659302v3cgtx15719561:20000
Edna-Cieno frequently ponded complex, 0 to 1 percent slopesEc167513659352vv5ptx15719561:20000
Edna fine sandy loam, 1 to 3 percent slopesEb74563659342v3cdtx15719561:20000
Bernard-Edna clay loam, 1 to 4 percent slopesBc2716365928d8s4tx15719561:20000
Bernard-Edna clay loams, 4 to 8 percent slopesBd1301365929d8s5tx15719561:20000
Edna loam, 0 to 1 percent slopesEd66183660652v3cctx16719851:24000
Bernard-Edna complex, 0 to 1 percent slopesBn58733660612v3cgtx16719851:24000
Edna-Aris complex, 0 to 1 percent slopesEs9253660662vv5qtx16719851:24000
Edna loam, 0 to 1 percent slopesEbA197024368052v3cctx17520101:24000
Bernard-Edna complex, 0 to 1 percent slopesBe345153673742v3cgtx20119731:20000
Edna loam, 0 to 1 percent slopesEd38963673802v3cctx20119731:20000
Edna loam, 0 to 1 percent slopesEdA183343754362v3cctx23919861:24000
Edna loam, 0 to 1 percent slopesEdA9493690232v3cctx28519861:24000
Edna loam, 0 to 1 percent slopesEdA718393704972v3cctx32119911:24000
Edna silty clay, 0 to 1 percent slopes, overwashEoA62353704982v3cftx32119911:24000
Edna-Cieno frequently ponded complex, 0 to 1 percent slopesExA50503704992vv5ptx32119911:24000
Edna loam, 0 to 1 percent slopesEdA327423730912v3cctx46919801:24000
Edna fine sandy loam, 1 to 3 percent slopesEdB4893730922v3cdtx46919801:24000
Edna loam, 0 to 1 percent slopesEdA963073732522v3cctx48119681:20000
Bernard-Edna complex, 0 to 1 percent slopesBeA472143732472v3cgtx48119681:20000
Edna-Cieno frequently ponded complex, 0 to 1 percent slopesEtA139093732552vv5ptx48119681:20000
Edna silty clay, 0 to 1 percent slopes, overwashEh32113732542v3cftx48119681:20000
Edna fine sandy loam, 1 to 3 percent slopesEdB15973732532v3cdtx48119681:20000
Edna loam, 0 to 1 percent slopesEdA48963738372v3cctx60019811:24000
Edna fine sandy loam, 1 to 3 percent slopesEdB19613738382v3cdtx60019811:24000
Katy-Edna complex, 0 to 3 percent slopesKcB810373850dk0ptx60019811:24000

Map of Series Extent

Approximate geographic distribution of the EDNA 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 .