Official Series Description


Lab Data Summary

Aggregate lab data for the DUBBS soil series. This aggregation is based on all pedons with a current taxon name of DUBBS, 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 DUBBS 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
115BM91143041991MO143004Dubbs4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
131AM99017491999MO017062Dubbs4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1286545,-89.9568176
131AM99017711999MO017085Dubbs4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1052704,-90.009079
131AM99017691999MO017102Dubbs4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1058807,-90.0027924
131AM03023182003MO023018Dubbs4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.6509171,-90.312561
131AM03031032003MO031003Dubbs4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1477661,-89.8544464
131A80P033980MS119001Dubbs6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.1913872,-90.2188873
131A80P034080MS143002Dubbs6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.5999985,-90.4066696
131A40A4385S1960AR093001Dubbs6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.5,-90.2788925
131A40A4386S1960AR093003Dubbs6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.4697227,-90.2675018
131A40A4866S1960KY075005Dubbs6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.5131416,-89.2936783
131A10N0425S2009MS135020Dubbs7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.016,-90.3568056
n/a40A4779S1944MS119006DUBBS4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a40A4780S1944MS119008DUBBS4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a40A4781S1944MS143001DUBBS4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a40A4782S1944MS143003DUBBS4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a40A4783S1944MS143004DUBBS4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a40A4784S1944MS143005DUBBS4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

Click the image to view it full size.

Soil series sharing subgroup-level classification with DUBBS, 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. MO-2012-02-06-21 | Butler County and Part of Ripley County - November 1983

    Typical pattern of soils and parent material in the Calhoun-Amagon association (Soil Survey of Butler County and Part of Ripley County, Missouri; November 1983).

  2. MS-2010-09-08-01 | Holmes County -

    Typical pattern of soils and underlying material in the Dundee-Dubbs-Tensas general soil map unit.

  3. MS-2012-02-06-01 | Carroll County - May 1990

    Pattern of soils and underlying material in the Dundee-Dubbs-Sharkey general soil map unit (Soil Survey of Carroll County, Mississippi; May 1990).

  4. MS-2012-04-26-09 | De Soto County - September 1959

    Soil associations in De Soto County (Soil Survey of De Soto County, Mississippi; September 1959).

  5. MS-2012-04-27-01 | Quitman County - December 1958

    Soil associations, Quitman County, Miss. (Soil Survey of Quitman County, Mississippi; December 1958).

  6. MS-2012-04-27-03 | Sunflower County - February 1959

    East-west cross section, 2 miles south of Doddsville, showing relation of soils to topography (Soil Survey of Sunflower County, Mississippi; February 1959).

  7. MS-2012-04-27-09 | Tunica County - May 1956

    Soil association map of Tunica County, Miss (Soil Survey of Tunica County, Mississippi; May 1956).

  8. TN-2012-03-19-07 | Haywood County - September 1995

    Pattern of soils and parent material in the Routon-Dubbs and Oaklimeter-Tichnor general soil map units (Soil Survey of Haywood County, TN; 1995).

Map Units

Map units containing DUBBS 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
Dubbs silt loam, 0 to 3 percent slopes4B620579299mft2ar00119951:24000
Dubbs very fine sandy loam241189564056lxycar02119751:20000
Dubbs fine sandy loam, 0 to 1 percent slopes159400564121ly0gar03119761:20000
Dubbs fine sandy loam, 0 to 3 percent slopes1659005641222wn5jar03119761:20000
Dubbs silt loam, 0 to 1 percent slopes1732305641232wn6xar03119761:20000
Dubbs silt loam, 0 to 3 percent slopesDsU170105641682wn5lar03519701:20000
Dubbs silt loam, 0 to 1 percent slopesDsA57005641672wn6xar03519701:20000
Dubbs fine sandy loam, 0 to 3 percent slopesDbB29705643832wn5jar03719661:20000
Dubbs fine sandy loam, undulatingDbC1720564384ly8yar03719661:20000
Dubbs fine sandy loam, 1 to 3 percent slopesDbB2692565539lzh6ar04719671:20000
Dubbs and Cleora soilsDC1640565537lzh4ar04719671:20000
Dubbs fine sandy loam, 0 to 1 percent slopesDbA382565538lzh5ar04719671:20000
Dubbs very fine sandy loam, 0 to 3 percent slopes8B3294577964mdf0ar05519951:24000
Dubbs silt loam, 0 to 3 percent slopes1616925657352wn5lar06319801:20000
Dubbs silt loam, 1 to 3 percent slopesDeB111005645312wn5kar07519731:20000
Dubbs silt loam, 0 to 1 percent slopesDeA18805645302wn6xar07519731:20000
Dubbs loam, gently undulatingDsB4070564082lxz6ar07719741:20000
Tiptonville and Dubbs silt loamsTd7580564363ly88ar09319671:20000
Dundee-Dubbs-Crevasse complexDv3980564343ly7mar09319671:20000
Dubbs silt loam, 0 to 1 percent slopesDbA235045659642wn6xar09519741:20000
Dubbs silt loam, 0 to 3 percent slopesDbB69015659652wn5lar09519741:20000
Dubbs silt loam, 0 to 3 percent slopesDsU83305642282wn5lar10719711:20000
Dubbs silt loam, undulatingDbU6558564269ly57ar11119731:20000
Dubbs fine sandy loam, undulatingDbC2360564442lybtar12319641:20000
Dubbs fine sandy loam, 0 to 3 percent slopesDbB20705644412wn5jar12319641:20000
Bosket-Dubbs fine sandy loam, gently undulatingBdB2000564429lybdar12319641:20000
Bosket-Dubbs fine sandy loam, undulatingBdC1800564430lybfar12319641:20000
Bosket-Dubbs fine sandy loams, 0 to 1 percent slopesBdA280564428lybcar12319641:20000
Dubbs silt loam, 0 to 1 percent slopesDbA57347493962wn6xar14719951:24000
Dubbs silt loam, 1 to 3 percent slopesDbB48517493972wn5kar14719951:24000
Dubbs silt loam, 3 to 8 percent slopesDbC851749398t4t4ar14719951:24000
Dubbs silt loam, 1 to 3 percent slopes966155643292wn5kar68019801:20000
Dubbs silt loam, 0 to 1 percent slopes815525643282wn6xar68019801:20000
Dundee-Dubbs complex2121955570377m4j8la12319751:24000
Dubbs silt loam, 0 to 3 percent slopes, occasionally flooded860001433712024rwxjmo01720041:24000
Dubbs silt loam, 0 to 1 percent slopes8200085324977342wn6xmo01720041:24000
Dubbs silt loam, 1 to 5 percent slopes, rarely flooded820711925715002r01mmo01720041:24000
Dubbs silt loam, 1 to 5 percent slopes, rarely flooded82071536625715012r01mmo02319821:24000
Dubbs silt loam, 1 to 5 percent slopes82033452624978532pqr3mo02319821:24000
Dubbs silt loam, 0 to 3 percent slopes, occasionally flooded8600015452571672rwxjmo02319821:24000
Dubbs silt loam, 0 to 1 percent slopes, frequently flooded86095103525716772q0jbmo02319821:24000
Dubbs silt loam, 0 to 1 percent slopes82000131624977332wn6xmo03119781:24000
Dubbs silt loam, 0 to 1 percent slopes, rarely flooded8208161425715202r01wmo03119781:24000
Dubbs silt loam, 0 to 3 percent slopes, occasionally flooded86000782571697rwxjmo03119781:24000
Dubbs silt loam, 0 to 1 percent slopes820002209824977322wn6xmo06919771:24000
Dubbs-Silverdale, rarely flooded, complex, 0 to 1 percent slopes8203414973894194z0gzmo06919771:24000
Dubbs silt loam, 0 to 1 percent slopes, rarely flooded82081187926076512r01wmo06919771:24000
Dubbs silt loam, 0 to 1 percent slopes, frequently flooded8609519225010892q0jbmo06919771:24000
Dubbs silt loam, 0 to 3 percent slopes, occasionally flooded86000462689840rwxjmo06919771:24000
Dubbs silt loam, 0 to 1 percent slopes, rarely flooded82081146025715392r01wmo13319781:24000
Dubbs silt loam, 0 to 1 percent slopes820007824977302wn6xmo13319781:24000
Dubbs silt loam, 0 to 1 percent slopes, rarely flooded82081430925715442r01wmo14319741:24000
Dubbs silt loam, 0 to 1 percent slopes82000322124977352wn6xmo14319741:24000
Dubbs silt loam, 0 to 3 percent slopes, occasionally flooded860001882689885rwxjmo14319741:24000
Dubbs silt loam, 0 to 1 percent slopes, frequently flooded8609514725010902q0jbmo14319741:24000
Dubbs silt loam, 0 to 1 percent slopes, rarely flooded82081201425715492r01wmo15519661:24000
Dubbs silt loam, 0 to 3 percent slopes, occasionally flooded86000152689894rwxjmo15519661:24000
Dubbs silt loam, 1 to 5 percent slopes, rarely flooded820713925715032r01mmo18119821:24000
Dubbs silt loam, 1 to 5 percent slopes82033724978522pqr3mo18119821:24000
Dubbs silt loam, 0 to 1 percent slopes82000328124977292wn6xmo20119781:24000
Dubbs silt loam, 1 to 5 percent slopes82033354724978542pqr3mo20719831:24000
Dubbs silt loam, 0 to 3 percent slopes, occasionally flooded8600018842689936rwxjmo20719831:24000
Dubbs silt loam, 1 to 5 percent slopes, rarely flooded82071172125715042r01mmo20719831:24000
Dubbs silt loam, 0 to 1 percent slopes8200051124977382wn6xmo20719831:24000
Dubbs silt loam, 0 to 1 percent slopes, rarely flooded8208115426899302r01wmo20719831:24000
Dubbs silt loam, 0 to 3 percent slopes, occasionally flooded860001782571661rwxjmo22320041:24000
Dubbs silt loam, 1 to 5 percent slopes, rarely flooded820713325715052r01mmo22320041:24000
Dubbs very fine sandy loam, 0 to 3 percent slopes, rarely floodedDe53955674862wf68ms01119561:20000
Dubbs very fine sandy loam, 3 to 7 percent slopes, moderately eroded, rarely floodedDg5265674872wf69ms01119561:20000
Dubbs silt loam, 0 to 2 percent slopes, rarely flooded2A23185675402wf67ms01519851:20000
Dubbs very fine sandy loam, 0 to 3 percent slopes, rarely floodedDd201995676342wf68ms02719561:24000
Dubbs very fine sandy loam, 3 to 7 percent slopes, moderately eroded, rarely floodedDe14025676352wf69ms02719561:24000
Dubbs silt loam, 0 to 3 percent slopesDc778567633m1nrms02719561:24000
Dubbs very fine sandy loam, very gently sloping phaseDd1929567735m1s1ms03319551:24000
Dubbs silt loam, very gently sloping phaseDc323567734m1s0ms03319551:24000
Dubbs very fine sandy loam, gently sloping phaseDe264567736m1s2ms03319551:24000
Dubbs silty clay loamDb146567843m1wjms04319651:15840
Dubbs silt loam, 0 to 2 percent slopes, rarely floodedDbA179865679552wf67ms05119971:20000
Dubbs silt loam, 2 to 5 percent slopesDbB3836567956m205ms05119971:20000
Dubbs very fine sandy loam, 0 to 2 percent slopesDg1414568010m21xms05319561:20000
Dubbs very fine sandy loam, 2 to 5 percent slopesDh543568011m21yms05319561:20000
Dubbs silt loam, 0 to 2 percent slopes, rarely floodedDe3895680092wf67ms05319561:20000
Dubbs loam, 1 to 3 percent slopes1717461568111m255ms08319971:24000
Dubbs loam, 0 to 1 percent slopes1617311568110m254ms08319971:24000
Dubbs-Dundee complex, 0 to 3 percent slopes1917289568113m257ms08319971:24000
Dubbs very fine sandy loam, 3 to 7 percent slopes, moderately eroded, rarely flooded1817605681122wf69ms08319971:24000
Dubbs-Dundee-Urban land complex, 0 to 3 percent slopes201207568114m258ms08319971:24000
Dubbs fine sandy loam, nearly level phaseDb4382568376m2fqms11919561:24000
Dubbs fine sandy loam, gently sloping phaseDc491568377m2frms11919561:24000
Dubbs silt loam, nearly level phaseDd207568378m2fsms11919561:24000
Dubbs silt loam, gently sloping phaseDe77568379m2ftms11919561:24000
Dubbs very fine sandy loam, 0 to 3 percent slopes, rarely floodedDg101535684612wf68ms13319561:20000
Dubbs silt loam, 0 to 3 percent slopesDd3008568459m2jdms13319561:20000
Dubbs very fine sandy loam, 3 to 7 percent slopes, moderately eroded, rarely floodedDh6975684622wf69ms13319561:20000
Dubbs silt loam, 3 to 7 percent slopesDe195568460m2jfms13319561:20000
Dubbs very fine sandy loam, 0 to 2 percent slopesDbA17190568513m2l4ms13519661:24000
Dubbs very fine sandy loam, 2 to 5 percent slopesDbB3101568514m2l5ms13519661:24000
Dubbs silt loam, 0 to 2 percent slopes110340917159601vllkms14320061:24000
Dubbs very fine sandy loam, 0 to 2 percent slopesDd881568745m2tmms15119591:20000
Dubbs silt loam, 0 to 2 percent slopes, rarely floodedDc5545687442wf67ms15119591:20000
Dubbs silt loam, 0 to 2 percent slopes, rarely floodedDbA123045687832wf67ms16319691:20000
Dubbs silt loam, 2 to 5 percent slopesDbB1345568784m2vwms16319691:20000
Dubbs silt loamDs405566780m0s7tn04519631:15840
Dubbs silt loam, 1 to 5 percent slopes, erodedDuB21980567074m12qtn07519901:24000
Routon-Dubbs complexRu1060567112m13ytn07519901:24000
Dubbs silt loam, 1 to 3 percent slopes, occasionally floodedDb280567073m12ptn07519901:24000
Dubbs silt loam, occasionally floodedDu479567157m15dtn09719851:24000
Dubbs-Routon complex, 0 to 4 percent slopesDx7131567339m1c8tn16719891:24000
Dubbs silt loam, 1 to 5 percent slopes, erodedDuB24386567336m1c5tn16719891:24000
Dubbs-Dekoven complex, 0 to 4 percent slopesDv1496567338m1c7tn16719891:24000
Dubbs silt loam, 5 to 8 percent slopes, severely erodedDuC3865567337m1c6tn16719891:24000

Map of Series Extent

Approximate geographic distribution of the DUBBS 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 .