Official Series Description


Lab Data Summary

Aggregate lab data for the DORMONT soil series. This aggregation is based on all pedons with a current taxon name of DORMONT, 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 DORMONT 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
12662PA1290111962PA129011Dormont4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3427778,-79.5069444
12665PA0030071965PA003007Dormont3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3022222,-80.0691667
12681PA0590021981PA059002Dormont5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7791667,-80.1194444
12681PA0590061981PA059006Dormont4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7669444,-80.1055556
126WVU0041S02WV051004Dormont5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9097222,-80.6522222

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DORMONT 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 DORMONT 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 DORMONT 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 DORMONT 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 flats position figure.

Competing Series

Soil series competing with DORMONT 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 DORMONT series and competing. 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 DORMONT 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 .

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There are insufficient data to create the 3D mountains figure.

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

Soil series sharing subgroup-level classification with DORMONT, 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. PA-2012-03-13-34 | Greene and Washington Counties - September 1983

    Typical pattern of soils and underlying material in the Dormont-Culleoka association (Soil Survey of Greene and Washington Counties, PA; 1983).

Map Units

Map units containing DORMONT 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
Dormont silt loam, 15 to 25 percent slopesDoD13724011262llkpmd00120091:12000
Dormont silt loam, 8 to 15 percent slopesDoC7324011252llknmd00120091:12000
Dormont silt loam, 25 to 45 percent slopesDoE4524011272llkqmd00120091:12000
Dormont silt loam, 8 to 15 percent slopesDoC168735416742s5ghpa00319731:15840
Dormont silt loam, 15 to 25 percent slopesDoD132225416752s5gkpa00319731:15840
Dormont silt loam, 3 to 8 percent slopesDoB71695416732s5gjpa00319731:15840
Dormont silt loam, 25 to 35 percent slopesDoE18415416762s5glpa00319731:15840
Dormont-Culleoka complex, 25 to 50 percent slopesDrE13924217312s5gzpa00520121:24000
Dormont-Culleoka complex, 15 to 25 percent slopesDrD11624217302s5gypa00520121:24000
Dormont silt loam, 3 to 8 percent slopesDoB4524216522s5gjpa00520121:24000
Dormont silt loam, 8 to 15 percent slopesDoC3324216532s5ghpa00520121:24000
Dormont silt loam, 15 to 25 percent slopesDoD2729003352s5gkpa00719781:15840
Dormont silt loam, 8 to 15 percent slopesDoC829003342s5ghpa00719781:15840
Dormont silt loam, 25 to 35 percent slopesDoE329003362s5glpa00719781:15840
Dormont-Culleoka complex, 15 to 25 percent slopesDrD1467115910422s5gypa05120051:24000
Dormont silt loam, 8 to 15 percent slopesDoC1317615910632s5ghpa05120051:24000
Dormont-Culleoka complex, 25 to 50 percent slopesDrE1261815910432s5gzpa05120051:24000
Dormont silt loam, 3 to 8 percent slopesDoB462215910622s5gjpa05120051:24000
Dormont silt loam, 15 to 25 percent slopesDoD417815910642s5gkpa05120051:24000
Dormont-Culleoka complex, 15 to 25 percent slopesDrD93623938352s5gypa06320121:24000
Dormont-Culleoka complex, 25 to 50 percent slopesDrE30723938362s5gzpa06320121:24000
Dormont silt loam, 3 to 8 percent slopesDoB7023938372s5gjpa06320121:24000
Dormont silt loam, 8 to 15 percent slopesDoC3023938382s5ghpa06320121:24000
Dormont silt loam, 8 to 15 percent slopesDoC142415445762s5ghpa12920031:24000
Dormont silt loam, 15 to 25 percent slopesDoD104485445772s5gkpa12920031:24000
Dormont-Culleoka complex, 15 to 25 percent slopesDrD100415445662s5gypa12920031:24000
Dormont-Culleoka complex, 25 to 50 percent slopesDrE74345445672s5gzpa12920031:24000
Dormont silt loam, 3 to 8 percent slopesDoB67155445752s5gjpa12920031:24000
Dormont silt loam, 25 to 35 percent slopesDoE4915445742s5glpa12920031:24000
Dormont-Culleoka complex, 25 to 50 percent slopesDtF2876765421532s5gzpa61119791:15840
Dormont-Culleoka complex, 15 to 25 percent slopesDtD1456765421522s5gypa61119791:15840
Dormont silt loam, 8 to 15 percent slopesDoC880715421502s5ghpa61119791:15840
Dormont silt loam, 15 to 25 percent slopesDoD477905421512s5gkpa61119791:15840
Dormont silt loam, 3 to 8 percent slopesDoB176055421492s5gjpa61119791:15840
Dormont silt loam, loamy substratum, 15 to 25 percent slopesDoD5810513645k7h6wv01119841:20000
Dormont-Latham complex, 15 to 25 percent slopesDlD167553340lkspwv04320051:24000
Dormont-Latham complex, 25 to 35 percent slopesDlE152553343lksswv04320051:24000
Dormont-Culleoka complex, 35 to 70 percent slopes, very stonyDsF55677749372t4s9wv05120071:12000
Dormont-Culleoka complex, 25 to 35 percent slopesDrE31094749371t4s8wv05120071:12000
Culleoka-Dormont complex, 15 to 25 percent slopesCmD288207493692s5hdwv05120071:12000
Gilpin-Dormont silt loams, 35 to 70 percent slopes, very stonyGdF1889516036501qtqnwv05120071:12000
Culleoka-Dormont-Peabody complex, 35 to 65 percent slopes, very stonyCrF1726617206371vrgfwv05120071:12000
Culleoka-Dormont-Peabody complex, 15 to 25 percent slopesCpD44531884886218cswv05120071:12000
Culleoka-Dormont-Peabody complex, 25 to 35 percent slopesCpE430916035931qtntwv05120071:12000
Culleoka-Dormont complex, 8 to 15 percent slopesCmC214716023172s5hfwv05120071:12000
Dormont silt loam, 15 to 25 percent slopesDoD175417206471vrgrwv05120071:12000
Dormont silt loam, 25 to 35 percent slopesDoE92617206481vrgswv05120071:12000
Culleoka-Dormont-Urban land complex, 15 to 25 percent slopesCuD921749374t4scwv05120071:12000
Culleoka-Dormont-Peabody complex, 8 to 15 percent slopesCpC8801884892218czwv05120071:12000
Culleoka-Dormont-Urban land complex, 8 to 15 percent slopesCuC57616026761qsq7wv05120071:12000
Dormont silt loam, 8 to 15 percent slopesDoC24417206461vrgqwv05120071:12000
Dormont-Latham complex, 25 to 35 percent slopesDrE30195515011k8x8wv09919931:24000
Dormont-Latham complex, 15 to 25 percent slopesDrD8095515010k8x7wv09919931:24000
Dormont and Guernsey silt loams, 15 to 25 percent slopesDgD11890514371k87mwv61119771:20000
Dormont and Guernsey silt loams, 8 to 15 percent slopesDgC8195514370k87lwv61119771:20000
Dormont and Guernsey silt loams, 3 to 8 percent slopesDgB1023514369k87kwv61119771:20000

Map of Series Extent

Approximate geographic distribution of the DORMONT 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 .