Official Series Description


Lab Data Summary

Aggregate lab data for the DUNMORE soil series. This aggregation is based on all pedons with a current taxon name of DUNMORE, 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 DUNMORE 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
12840A4961S1953TN009001Dunmore4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.8574982,-83.7727814
12840A4962S1953TN009002Dunmore4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.8195419,-83.7873993

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DUNMORE 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 DUNMORE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

There are insufficient data to create the sibling sketch figure.

Select annual climate data summaries for the DUNMORE 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 DUNMORE 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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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.

Competing Series

Soil series competing with DUNMORE 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 DUNMORE 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 DUNMORE 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 DUNMORE, 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

No block diagrams are available.

Map Units

Map units containing DUNMORE 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
Dunmore gravelly silty clay loam, 5 to 12 percent slopes, erodedDnh149935250962t3hhtn05919541:15840
Dunmore gravelly silty clay loam, 12 to 25 percent slopes, erodedDng97995250952t3hjtn05919541:15840
Dunmore cherty silt loam, rolling phaseDnb3076525090kmddtn05919541:15840
Dunmore cherty silt loam, hilly phaseDna2383525089kmdctn05919541:15840
Dunmore cherty silty clay, severely eroded hilly phaseDnd1787525092kmdgtn05919541:15840
Dunmore cherty silty clay loam, eroded steep phaseDnk1450525097kmdmtn05919541:15840
Dunmore cherty silt loam, steep phaseDnc1326525091kmdftn05919541:15840
Dunmore cherty silty clay, severely eroded rolling phaseDne606525093kmdhtn05919541:15840
Dunmore cherty silty clay, severely eroded steep phaseDnf449525094kmdjtn05919541:15840
Dunmore and Fullerton soils, karst, 10 to 30 percent slopes, erodedDxE27202525470kmsntn08919911:24000
Dunmore and Fullerton soils, 10 to 30 percent slopes, gulliedDwE31724525469kmsmtn08919911:24000
Fullerton silt loam, very steep phase (Dunmore)FsF455525953kn97tn10519581:15840
Dunmore-Rock outcrop complex, 20 to 35 percent slopesDrE1011528410kqvhtn17119801:24000
Dunmore-Rock outcrop complex, 10 to 20 percent slopesDrD432528409kqvgtn17119801:24000
Gullied land-Dunmore complex, 12 to 50 percent slopesGuE29116896601tq75tn17919551:15840
Dunmore gravelly silt loam, 5 to 12 percent slopesDv193318994852t3hdtn60919551:20000
Dunmore gravelly silt loam, 12 to 25 percent slopesDw164018994862t3hftn60919551:20000
Dunmore gravelly silt loam, 25 to 50 percent slopesDx15318994872t3hgtn60919551:20000
Frederick and Dunmore soils, 25 to 45 percent slopes, very rockyFFE10183514488k8cdwv06319621:24000
Frederick and Dunmore soils, 15 to 25 percent slopes, very rockyFFD7380514487k8ccwv06319621:24000
Frederick and Dunmore soils, 3 to 15 percent slopes, very rockyFFC1618514486k8cbwv06319621:24000
Dunmore channery silt loam, 8 to 15 percent slopesDtC118617162871vly3wv06319621:24000
Dunmore channery silt loam, 15 to 25 percent slopesDtD46217162881vly4wv06319621:24000
Dunmore silt loam, 8 to 15 percent slopesDvC412514471k8bvwv06319621:24000
Dunmore channery silt loam, 3 to 8 percent slopesDtB41217162861vly2wv06319621:24000
Dunmore silt loam, 15 to 25 percent slopesDvD403514472k8bwwv06319621:24000
Dunmore silt loam, 3 to 8 percent slopesDvB265514470k8btwv06319621:24000
Dunmore channery silty clay loam, 15 to 25 percent slopesDuD9817161341vls5wv06319621:24000

Map of Series Extent

Approximate geographic distribution of the DUNMORE 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 .