Official Series Description


Lab Data Summary

Aggregate lab data for the TUMBLING soil series. This aggregation is based on all pedons with a current taxon name of TUMBLING, 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 TUMBLING 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 TUMBLING 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 TUMBLING 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 TUMBLING 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 TUMBLING 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 terrace figure.

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

Competing Series

Soil series competing with TUMBLING 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 TUMBLING 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 TUMBLING 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 TUMBLING, 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. VA-2010-11-05-27 | Lee County - 2006

    Typical pattern of soils in areas of Powell Mountain, Wallen Ridge, and Poor Valley Ridge. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to parent material and landform position (Soil Survey of Lee County, Virginia; 2006).

  2. VA-2012-05-11-08 | Lee County - 2006

    Typical pattern of soils in areas of Powell Mountain, Wallen Ridge, and Poor Valley Ridge. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to parent material and landform position (Soil Survey of Lee County, Virginia; 2006).

Map Units

Map units containing TUMBLING 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
Tumbling loam, 15 to 35 percent slopes, very stony36D562314027131j2mtva02120051:24000
Tumbling loam, 8 to 15 percent slopes, very stony36C185814027121j2msva02120051:24000
Tumbling loam, 7 to 15 percent slopes34C136814027102t3gjva02120051:24000
Tumbling loam, karst, 8 to 15 percent slopes35C39514026981j2mbva02120051:24000
Tumbling loam, karst, 15 to 25 percent slopes35D28014026991j2mcva02120051:24000
Tumbling loam, 15 to 25 percent slopes34D26614027112t3g3va02120051:24000
Tumbling loam, 2 to 7 percent slopes34B25914027092t3ghva02120051:24000
Tumbling cobbly loam, 15 to 30 percent slopes, very stony57D4000519132kf66va02319901:20000
Tumbling cobbly loam, 15 to 30 percent slopes56D3172519130kf64va02319901:20000
Tumbling cobbly loam, 7 to 15 percent slopes56C2658519129kf63va02319901:20000
Tumbling loam, 7 to 15 percent slopes55C22575191272t3gjva02319901:20000
Tumbling cobbly loam, 2 to 15 percent slopes, very stony57C1498519131kf65va02319901:20000
Tumbling loam, 15 to 30 percent slopes55D889519128kf62va02319901:20000
Tumbling-Urban land complex, 2 to 15 percent slopes58C776519133kf67va02319901:20000
Tumbling loam, 2 to 7 percent slopes55B4745191262t3ghva02319901:20000
Tumbling loam, 7 to 15 percent slopes36C154224810402t3gjva04520101:24000
Tumbling loam, 15 to 35 percent slopes, very stony37E54924810732p8rmva04520101:24000
Tumbling loam, 15 to 25 percent slopes36D49024810412t3g3va04520101:24000
Tumbling loam, 8 to 15 percent slopes, very stony37C22724810722p8rlva04520101:24000
Tumbling loam, 2 to 7 percent slopes36B10324810392t3ghva04520101:24000
Tumbling loam, 25 to 35 percent slopes, very stony31E7300521748khxlva10519971:24000
Tumbling loam, 7 to 15 percent slopes30C41945217442t3gjva10519971:24000
Tumbling loam, 15 to 25 percent slopes30D35005217452t3g3va10519971:24000
Tumbling loam, 15 to 25 percent slopes, very stony31D1218521747khxkva10519971:24000
Tumbling loam, 7 to 15 percent slopes, very stony31C2155217462wpkwva10519971:24000
Tumbling loam, 7 to 15 percent slopes49C32945203312t3gjva16119901:24000
Tumbling loam, 25 to 45 percent slopes, very stony50E1642520340kgg5va16119901:24000
Tumbling loam, 15 to 25 percent slopes49D15465203322t3g3va16119901:24000
Tumbling loam, 2 to 7 percent slopes49B9705203302t3ghva16119901:24000
Tumbling loam, 15 to 25 percent slopes, very stony50D741520338kgg3va16119901:24000
Tumbling-Urban land complex, 2 to 15 percent slopes51C539520343kgg8va16119901:24000
Tumbling loam, 7 to 15 percent slopes, very stony50C2275203362wpkwva16119901:24000
Vanella-Tumbling complex, 15 to 35 percent slopes, very stony73E965125148822qddnva16320101:24000
Tumbling-Vanella complex, 8 to 15 percent slopes67C313725148642qdd8va16320101:24000
Vanella-Tumbling complex, 3 to 15 percent slopes, very stony73C220725148812qddmva16320101:24000
Tumbling-Vanella complex, 15 to 25 percent slopes67D173125148652qdd9va16320101:24000
Tumbling-Vanella complex, 25 to 35 percent slopes67E125825148742qddbva16320101:24000
Tumbling-Vanella-Urban land complex, 8 to 25 percent slopes68D36625148752qddgva16320101:24000
Tumbling loam, 15 to 25 percent slopes52D668016712062t3g3va16720061:24000
Tumbling loam, 7 to 15 percent slopes52C439816718752t3gjva16720061:24000
Tumbling loam, 25 to 45 percent slopes, very stony53E179316718771t3qjva16720061:24000
Tumbling loam, 35 to 45 percent slopes, very stony40E1841778101v3p1va16920031:24000
Tumbling loam, 15 to 35 percent slopes40D1131778099v3nzva16920031:24000
Tumbling loam, 7 to 15 percent slopes40C10587780972t3gjva16920031:24000
Tumbling loam, 7 to 15 percent slopes39C49425187322t3gjva17319951:24000
Tumbling loam, 15 to 25 percent slopes, very stony40D4008518738kdshva17319951:24000
Tumbling loam, 7 to 15 percent slopes, very stony40C25575187372wpkwva17319951:24000
Tumbling loam, 15 to 25 percent slopes39D17745187332t3g3va17319951:24000
Tumbling loam, 25 to 65 percent slopes, very stony40E1633518739kdsjva17319951:24000
Tumbling loam, 2 to 7 percent slopes39B11785187312t3ghva17319951:24000
Tumbling loam, 25 to 35 percent slopes39E552518735kdsdva17319951:24000
Tumbling loam, 2 to 7 percent slopes, very stony49B9522189kjctva18519961:24000
Tumbling loam, 7 to 15 percent slopes, very stony49C45221902wpkwva18519961:24000
Tumbling loam, 7 to 15 percent slopes44C34175194132t3glva19119981:15840
Tumbling loam, 15 to 25 percent slopes44D20665194142t3g3va19119981:15840
Tumbling loam, 25 to 45 percent slopes44E1623519415kfhbva19119981:15840
Tumbling loam, 7 to 15 percent slopes, very bouldery43C718519378kfg4va19119981:15840
Tumbling loam, 2 to 7 percent slopes44B4095194122t3gkva19119981:15840
Tumbling loam, 2 to 7 percent slopes, very bouldery43B310519377kfg3va19119981:15840
Tumbling loam, 15 to 25 percent slopes, very bouldery43D172519379kfg5va19119981:15840
Tumbling loam, 15 to 35 percent slopes, very stony74E70325086132q7rvva19520101:24000
Tumbling loam, 8 to 15 percent slopes73C22825086122q7rtva19520101:24000
Tumbling fine sandy loam, 15 to 35 percent slopes25D68225252392qm15va6061:24000
Tumbling fine sandy loam, 3 to 15 percent slopes25C50425252382qm14va6061:24000
Tumbling fine sandy loam, 35 to 60 percent slopes25E27125568412r7cbva6061:24000
Tumbling loam, 15 to 30 percent slopes36E3131740882z3ftva8501:24000
Tumbling cobbly loam, 15 to 30 percent slopes35E2731740852z3frva8501:24000
Tumbling loam, 7 to 15 percent slopes36C2131740902z3fwva8501:24000
Tumbling-Urban land complex, 2 to 15 percent slopes37C1231740912z3fxva8501:24000
Tumbling cobbly loam, 7 to 15 percent slopes35C931740862z3fsva8501:24000
Tumbling loam, 2 to 7 percent slopes36B731740892z3fvva8501:24000

Map of Series Extent

Approximate geographic distribution of the TUMBLING 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 .