Official Series Description


Lab Data Summary

Aggregate lab data for the DRUMMOND soil series. This aggregation is based on all pedons with a current taxon name of DRUMMOND, 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 DRUMMOND were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
80A79-OK-27-1079-OK053-27-10Drummond4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8082611,-98.0205417
80A80P0068S1979OK053030DRUMMOND6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7544441,-97.6388855

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the DRUMMOND series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the DRUMMOND series and siblings. 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 DRUMMOND 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 .

Click the image to view it full size.

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.

Click the image to view it full size.

Competing Series

Soil series competing with DRUMMOND share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the DRUMMOND 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 DRUMMOND 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.

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 DRUMMOND, 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. KS-2012-01-23-03 | Finney County - November 1965

    Typical cross section of the Scott-Finney depression (Soil Survey of Finney County, Kansas; 1965).

  2. KS-2012-01-24-14 | McPherson County - April 1983

    Typical pattern of soils in the Carwile-Attica association (Soil Survey of McPherson County, Kansas; 1983).

Map Units

Map units containing DRUMMOND 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
Mangum-Drummond complex, rarely flooded5360208413824991hdlrks00719731:24000
Osage-Drummond complex, occasionally flooded8204489414533901ksckks01919721:24000
Mason-Drummond silt loams, rarely flooded850271314533941kscpks01919721:24000
Tabler-Drummond complex, 0 to 1 percent slopes5969279113803952ww13ks04719671:24000
Zenda-Drummond complex, occasionally flooded5693113213804032zt7hks04719671:24000
Drummond loam, 0 to 1 percent slopes, rarely ponded6335237613826811hdsmks07719651:24000
Zenda-Drummond complex, occasionally flooded56932414447632zt7hks09519771:24000
Zenda-Drummond complex, occasionally flooded569369014451212zt7hks15119651:24000
Zenda-Drummond complex, occasionally flooded56935214436352zt7hks18519751:24000
Brewer-Drummond silty clay loams, rarely flooded6222357014446341kh83ks19119741:24000
Brewer-Drummond complex, 0 to 1 percent slopes, rarely floodedBu8307381414dswpok00319711:24000
Drummond silt loam, 0 to 3 percent slopes, rarely floodedDrB180638142230g6zok00319711:24000
Waldeck-Drummond complex, 0 to 1 percent slopes, occasionally floodedLh2208381739dt75ok01119651:24000
Lela-Drummond complex, 0 to 1 percent slopes, occasionally floodedLe1241381738dt74ok01119651:24000
Brewer-Drummond complex, 0 to 1 percent slopes, rarely floodedBu3417381934dtfgok01719721:24000
Drummond loam, 0 to 1 percent slopes, rarely floodedDr518638248730g70ok04719651:24000
Miller-Drummond complex, 0 to 1 percent slopes, occasionally floodedMs1610382506dv0xok04719651:24000
McLain-Drummond complex, 0 to 1 percent slopes, rarely flooded3524069382724dv7yok05319831:24000
Drummond loam, 0 to 1 percent slopes, saline, rarely flooded8192638274930g6xok05319831:24000
Lela-Drummond complex, 0 to 1 percent slopes, occasionally floodedLe2547383338dvwrok07119651:24000
Drummond silt loam, 0 to 1 percent slopes, rarely floodedDr386383391dvygok07319601:24000
Braman-Drummond complex, 0 to 1 percent slopes, rarely flooded3346156234282yhddok11319751:24000
Brewer-Drummond complex, 0 to 1 percent slopes, rarely floodedBrDA32216773561t9f8ok11720071:24000

Map of Series Extent

Approximate geographic distribution of the DRUMMOND 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 .