Official Series Description


Lab Data Summary

Aggregate lab data for the DEEPWOOD soil series. This aggregation is based on all pedons with a current taxon name of DEEPWOOD, 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 DEEPWOOD 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 DEEPWOOD 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 DEEPWOOD 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 DEEPWOOD 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 DEEPWOOD 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with DEEPWOOD 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 DEEPWOOD 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 DEEPWOOD 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 DEEPWOOD, 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. OK-2010-09-29-20 | Woods County - 2003

    Typical pattern of soils and underlying material in the Quinlan-Woodward-Deepwood general soil map unit (Soil Survey of Woods County, Oklahoma; 2003).

Map Units

Map units containing DEEPWOOD 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
Woodward-Deepwood complex, 1 to 3 percent slopesWoDB566225452w5q3ok00319711:24000
Quinlan-Woodward-Deepwood complex, 5 to 12 percent slopesQWDE42731012762t6qrok00720211:24000
Quinlan-Woodward-Deepwood complex, 5 to 12 percent slopesQWDE479233831072t6qrok05919981:24000
Deepwood loam, 1 to 3 percent slopesDpwB314338298230fq1ok05919981:24000
Deepwood loam, 3 to 5 percent slopesDpwC187638298330fq2ok05919981:24000
Deepwood loam, 5 to 8 percent slopesDpwD736325447630fq3ok05919981:24000
Deepwood loam, 8 to 12 percent slopesDpwE55538309030fq4ok05919981:24000
Quinlan-Woodward-Deepwood complex, 5 to 12 percent slopesQWDE267433852262t6qrok15119951:24000
Woodward-Deepwood complex, 3 to 5 percent slopesWoDC8042385256dxwmok15119951:24000
Woodward-Deepwood complex, 1 to 3 percent slopesWoDB47763852552w5q3ok15119951:24000
Deepwood-Quinlan-Cottonwood complex, 5 to 50 percent slopesDCG505583651432wt7htx12519651:20000
Woodward-Deepwood-Quinlan complex, warm, 2 to 12 percent slopesWQE411853651612wt7jtx12519651:20000
Deepwood-Woodward-Quinlan complex, warm, 2 to 45 percent slopesDQG191093651122y7bdtx12519651:20000
Deepwood-Woodward-Rock outcrop complex, warm, 12 to 50 percent slopesDRG1893631007422y7bftx12519651:20000
Woodward-Deepwood complex, warm, 3 to 5 percent slopesWoC86783651602wt7ftx12519651:20000
Woodward-Deepwood complex, warm, 3 to 5 percent slopesWoC381263686152wt7ftx26919991:31680
Woodward-Deepwood-Quinlan complex, warm, 2 to 12 percent slopesWQE350333686172wt7jtx26919991:31680
Deepwood-Woodward-Quinlan complex, warm, 2 to 45 percent slopesDQG287703686072y7bdtx26919991:31680
Deepwood-Quinlan-Cottonwood complex, 5 to 50 percent slopesDCG117253686062wt7htx26919991:31680
Woodward-Deepwood complex, warm, 5 to 8 percent slopesWoD112583686162wt7gtx26919991:31680

Map of Series Extent

Approximate geographic distribution of the DEEPWOOD 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 .