Official Series Description


Lab Data Summary

Aggregate lab data for the EASTWOOD soil series. This aggregation is based on all pedons with a current taxon name of EASTWOOD, 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 EASTWOOD 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
133B87P039986LA085016Eastwood6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.5966663,-93.3777771
133B89P077889LA115023Eastwood7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.1519451,-93.1536102
133B40A3995S1945LA013001Eastwood4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.5449982,-93.0175018
133B40A1342S1974LA017007EASTWOOD1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.4702797,-93.9477768
133B40A3992S1974LA017008EASTWOOD2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.4302788,-93.953331
133B40A1339S1974LA017009Eastwood1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.3525009,-93.7458344
133BS85TX203002S85TX203002Eastwood4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.459837,-94.138417
133BS87TX419002S87TX419002Eastwood5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.7091942,-93.9089203

Water Balance

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

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 EASTWOOD, 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-2010-11-04-16 | San Augustine and Sabine Counties -

    Eastwood-Latex-Sawlit association (Soil Survey of San Augustine and Sabine Counties, Texas).

  2. TX-2010-11-04-17 | San Augustine and Sabine Counties -

    (Soil Survey of San Augustine and Sabine Counties, Texas).

  3. TX-2012-03-21-06 | Harrison County - October 1994

    Pattern of soils and parent material in the Scottsville general soil map unit (Soil Survey of Harrison County, TX; 1994).

Map Units

Map units containing EASTWOOD 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
Eastwood fine sandy loam, 5 to 12 percent slopesECE619317245812tcnvla01319921:24000
Eastwood fine sandy loam, 1 to 5 percent slopesEcC5242172458330d19la01319921:24000
Eastwood fine sandy loam, 12 to 20 percent slopesECF495617245821vwkpla01319921:24000
Eastwood fine sandy loam, 5 to 15 percent slopesEaG4646328057102ssx3la01720131:24000
Eastwood fine sandy loam, 1 to 5 percent slopesEaC26140280570930d19la01720131:24000
Urban land-Eastwood complex, 5 to 15 percent slopesUED787728057482ssy6la01720131:24000
Urban land-Eastwood complex, 1 to 5 percent slopesUEC502828057472ssy5la01720131:24000
Eastwood very fine sandy loam, 5 to 12 percent slopesEd4879556931830g40la02719861:20000
Eastwood very fine sandy loam, 1 to 5 percent slopesEa1833656931730d1bla02719861:20000
Eastwood very fine sandy loam, 5 to 20 percent slopesEe11869327958052qtfbla03119861:24000
Eastwood very fine sandy loam, 1 to 5 percent slopesEb91920279580430d1bla03119861:24000
Eastwood fine sandy loam, 1 to 5 percent slopesEa516172452930d19la03119861:24000
Eastwood fine sandy loam, 5 to 12 percent slopesEc48717245302tcnvla03119861:24000
Eastwood fine sandy loam, 1 to 5 percent slopesEa4971190316730d19la06919831:24000
Eastwood fine sandy loam, 5 to 12 percent slopesEd356619031692tcnvla06919831:24000
Eastwood very fine sandy loam, 5 to 20 percent slopesEe85630410582qtfbla06919831:24000
Eastwood very fine sandy loam, 1 to 5 percent slopesEb300304105730d1bla06919831:24000
Eastwood fine sandy loam, 1 to 5 percent slopesEcC38240136630d19la08119731:24000
Eastwood fine sandy loam, 5 to 12 percent slopesECE3424013672tcnvla08119731:24000
Eastwood fine sandy loam, 12 to 20 percent slopesECF2524013682llthla08119731:24000
Eastwood fine sandy loam, 5 to 12 percent slopesEDE5887719030292tcnvla08519911:24000
Eastwood fine sandy loam, 1 to 5 percent slopesEdC51341190303030d19la08519911:24000
Eastwood very fine sandy loam, 5 to 20 percent slopesEe256130410622qtfbla08519911:24000
Eastwood very fine sandy loam, 1 to 5 percent slopesEb2235304106330d1bla08519911:24000
Eastwood very fine sandy loam, 5 to 12 percent slopesED346172533230g40la11119921:24000
Eastwood silt loam, 5 to 12 percent slopesEAE6924417255451vxkrla11519921:24000
Eastwood silt loam, 1 to 5 percent slopesEaC2726017255461vxksla11519921:24000
Eastwood very fine sandy loam, 5 to 12 percent slopesEO108257034230g40la11919891:24000
Eastwood very fine sandy loam, 1 to 5 percent slopesEa103657034330d1bla11919891:24000
Eastwood very fine sandy loam, 5 to 20 percent slopesEasE3333226072342qtfbtx20319891:24000
Eastwood very fine sandy loam, 1 to 5 percent slopesEasCn30933260723330d1btx20319891:24000
Eastwood very fine sandy loam, 5 to 20 percent slopesEasE1752130094312qtfbtx34719761:24000
Eastwood very fine sandy loam, 1 to 5 percent slopesEasC4276300943030d1btx34719761:24000
Eastwood very fine sandy loam, 5 to 20 percent slopesEasE8636726072432qtfbtx36519711:20000
Eastwood very fine sandy loam, 1 to 5 percent slopesEasC44753260724230d1btx36519711:20000
Eastwood very fine sandy loam, 5 to 20 percent slopesEasE5045230094382qtfbtx40119931:24000
Eastwood very fine sandy loam, 1 to 5 percent slopesEasC9241300943930d1btx40119931:24000
Eastwood very fine sandy loam, 5 to 20 percent slopesEasE12686130094472qtfbtx41920021:24000
Eastwood very fine sandy loam, 1 to 5 percent slopesEasC6146057576130d1btx41920021:24000
Eastwood-Latex complex, 1 to 3 percent slopes, moundedElA3939612321nk59tx41920021:24000
Eastwood very fine sandy loam, 5 to 15 percent slopesEeD81735765322tcnxtx61620041:24000
Eastwood very fine sandy loam, 1 to 5 percent slopesEasCn7833265603030d1btx61620041:24000
Eastwood very fine sandy loam, 5 to 20 percent slopesEasEn206626560312qtfbtx61620041:24000
Eastwood very fine sandy loam, 1 to 5 percent slopesEeB23118189478630d1btx61920071:24000
Eastwood very fine sandy loam, 5 to 15 percent slopesEeD1326918947872tcnxtx61920071:24000
Eastwood very fine sandy loam, 5 to 20 percent slopesEasE713531007532qtfbtx61920071:24000
Eastwood-Latex complex, 1 to 3 percent slopes, moundedElA1776189478821lp6tx61920071:24000

Map of Series Extent

Approximate geographic distribution of the EASTWOOD 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 .