Official Series Description


Lab Data Summary

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

Soil series competing with DERBY 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 DERBY 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 DERBY 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.

Click the image to view it full size.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with DERBY, 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-2010-09-29-04 | Logan County - 2006

    Typical pattern of soils and underlying material in the Dougherty-Konawa-Derby general soil map unit (Soil Survey of Logan County, Oklahoma; 2006).

  2. OK-2012-02-16-13 | Cleveland County - April 1987

    Typical pattern of soils and underlying material in the Norge-Teller-Vanoss map unit and Asher-Keokuk-Canadian map unit (Soil Survey of Cleveland County, Oklahoma; April 1987).

  3. OK-2012-02-17-05 | Logan County - June 1960

    Soils of central and western Logan County on recent alluvium and on loams and sands of Quaternary age. Red beds are exposed in the upper right corner (Soil Survey of Logan County, Oklahoma; June 1960).

  4. OK-2012-02-17-31 | Payne County - April 1987

    Typical pattern of soils and underlying material in the Konawa-Dougherty-Derby map unit (Soil Survey of Payne Oklahoma; April 1987).

Map Units

Map units containing DERBY 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
Aline-Derby fine sands, 5 to 12 percent slopes6200335932211322xqqlks00719731:24000
Aline-Derby fine sands, 5 to 12 percent slopes6200720332211352xqqlks07719651:24000
Aline-Derby fine sands, 5 to 12 percent slopes62001414446192xqqlks19119741:24000
Aline-Derby fine sands, 5 to 12 percent slopesAlDE525930411122xqqlok00319711:24000
Derby loamy fine sand, 3 to 15 percent slopesDerE51886225342tq7qok00319711:24000
Gracemore, rarely flooded-Derby fine sands, 0 to 3 percent slopes, salineGcDB12283814232y2sjok00319711:24000
Derby loamy fine sand, 15 to 30 percent slopesDerG618622533nwsqok00319711:24000
Derby-Goodnight fine sands, 5 to 12 percent slopesDeGE593814472y2shok00319711:24000
Derby loamy fine sand, 0 to 3 percent slopesDerB20131092392tq7pok01119651:24000
Derby loamy fine sand, 3 to 15 percent slopes1315243820862tq7qok02719841:24000
Derby loamy fine sand, 0 to 3 percent slopes127813820852tq7pok02719841:24000
Derby-Urban land complex, 3 to 15 percent slopes14134382087dtldok02719841:24000
Derby loamy fine sand, 3 to 15 percent slopesDerE4425163632tq7qok03719521:24000
Derby loamy fine sand, 3 to 15 percent slopes5343803827442tq7qok05319831:24000
Derby loamy fine sand, 15 to 30 percent slopes542955382745dv8mok05319831:24000
Derby loamy fine sand, 3 to 8 percent slopesToC538383256dvt3ok06719671:24000
Derby loamy fine sand, 3 to 8 percent slopesDerD3103383607dw5fok08319941:12000
Derby loamy fine sand, 8 to 15 percent slopesDerE2137383608dw5gok08319941:12000
Derby loamy fine sand, 0 to 3 percent slopesDerB19523836062tq7pok08319941:12000
Derby loamy fine sand, 0 to 3 percent slopesDerB2300031092382tq7pok09319651:24000
Derby-Goodnight fine sands, 5 to 12 percent slopesDeGE460632211562y2shok09319651:24000
Derby-Urban land-Dougherty complex, 0 to 15 percent slopesDUDE2222384282dww6ok10919961:12000
Derby-Dougherty complex, 0 to 15 percent slopesDeDE1703384285dww9ok10919961:12000
Derby loamy fine sand, 8 to 15 percent slopesDerE1299384287dwwcok10919961:12000
Derby loamy fine sand, 0 to 3 percent slopesDerB6593842862tq7pok10919961:12000
Derby loamy fine sand, 3 to 15 percent slopesDerE24616758932tq7qok11720071:24000
Derby loamy fine sand, 3 to 15 percent slopesDerE343619082452tq7qok11919831:24000
Derby-Slaughterville complex, 1 to 5 percent slopes821780384584dx5yok11919831:24000
Derby loamy fine sand, 15 to 35 percent slopes901219384590dx64ok11919831:24000

Map of Series Extent

Approximate geographic distribution of the DERBY 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 .