Official Series Description


Lab Data Summary

Aggregate lab data for the THURMONT soil series. This aggregation is based on all pedons with a current taxon name of THURMONT, 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 THURMONT 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
130B00P1345S2000NC021001Thurmont7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.7561111,-82.3925018

Water Balance

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

Soil series sharing subgroup-level classification with THURMONT, 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. MD-2010-09-07-01 | Frederick County - 2002

    Relationship of soils, topography, and underlying material in the Bagtown-Stumptown-Edgemont general soil map unit (Soil Survey of Frederick County, Maryland; 2002).

  2. MD-2012-02-03-16 | Frederick County - 2002

    Relationship of soils, topography, and underlying material in the Bagtown-Stumptown-Edgemont general soil map unit (Soil Survey of Frederick County, Maryland; 2002).

Map Units

Map units containing THURMONT 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
Thurmont and Braddock fine sandy loams, severely eroded sloping phasesTaD328012438045f8ga11719571:20000
Thurmont and Braddock fine sandy loams, very gently sloping phasesTaB24512437845f6ga11719571:20000
Thurmont and Braddock fine sandy loams, eroded very gently sloping phasesTaB217012437945f7ga11719571:20000
Thurmont loamy sand, 2 to 6 percent slopesTkB186012474145sxga19919601:15840
Thurmont loamy sand, 6 to 10 percent slopesTkC176012474245syga19919601:15840
Thurmont loamy sand, 10 to 15 percent slopesTkD69012474345szga19919601:15840
Thurmont fine sandy loam, 6 to 12 percent slopesThC10030531789kvchga63719901:20000
Thurmont fine sandy loam, 12 to 25 percent slopesThE3660531790kvcjga63719901:20000
Thurmont fine sandy loam, 2 to 6 percent slopesThB1810531788kvcgga63719901:20000
Thurmont gravelly loam, 3 to 8 percent slopes, very stonyThB601535077kyskmd02120011:12000
Thurmont gravelly loam, 3 to 8 percent slopesTaB531534876kyl2md02120011:12000
Thurmont gravelly loam, 8 to 15 percent slopesTaC342534878kyl4md02120011:12000
Thurmont gravelly loam, 8 to 15 percent slopesThC1524534696kyd8md04319981:12000
Braddock-Thurmont gravelly loams, 3 to 8 percent slopesBrB1350534171kxvbmd04319981:12000
Braddock-Thurmont gravelly loams, 8 to 15 percent slopesBrC1308534173kxvdmd04319981:12000
Thurmont gravelly loam, 3 to 8 percent slopesThB1205534694kyd6md04319981:12000
Thurmont gravelly loam, 15 to 25 percent slopesThD354534698kydbmd04319981:12000
Braddock-Thurmont gravelly loams, 15 to 25 percent slopesBrD154534175kxvgmd04319981:12000
Thurmont-Dillard complex, 8 to 15 percent slopesThC868224231702mbhsnc03920091:12000
Thurmont-Dillard complex, 2 to 8 percent slopesThB524424231692mbhrnc03920091:12000
Thurmont-Dillard complex, 2 to 8 percent slopesThB18431912787226dtnc07520071:12000
Thurmont loam, 8 to 15 percent slopesThC1138756641tdbsnc60520071:12000
Thurmont loam, 15 to 30 percent slopesThD4131910256223s5nc60520071:12000
Thurmont-Dillard complex, 2 to 8 percent slopesTdB22319126252267lnc60520071:12000
Thurmont gravelly loam, 8 to 25 percent slopes, very stonyToD1351545203l9b6pa05519991:24000
Thurmont gravelly loam, 3 to 8 percent slopes, stonyThB354545201l9b4pa05519991:24000
Thurmont gravelly loam, 8 to 15 percent slopes, stonyThC182545202l9b5pa05519991:24000
Thurmont loam, 8 to 15 percent slopes, stonyThC13214145741jgzftn64020071:24000
Thurmont-Dillard complex, 2 to 8 percent slopes, stonyThB1014145751jgzgtn64020071:24000
Thurmont loam, 7 to 15 percent slopes81C2560516476kbfjva00319811:15840
Thurmont loam, 2 to 7 percent slopes81B1960516475kbfhva00319811:15840
Thurmont very stony loam, 7 to 15 percent slopes82C1060516478kbflva00319811:15840
Thurmont very stony loam, 15 to 25 percent slopes82D790516479kbfmva00319811:15840
Thurmont loam, 15 to 25 percent slopes81D460516477kbfkva00319811:15840
Thurmont fine sandy loam, 7 to 15 percent slopes31C23951359734kh7va01919851:24000
Thurmont fine sandy loam, 2 to 7 percent slopes31B7111359724kh6va01919851:24000
Thurmont fine sandy loam, 15 to 25 percent slopes31D3271359744kh8va01919851:24000
Thurmont loam, 15 to 30 percent slopes, very stony52D557519123kf5xva02319901:20000
Thurmont loam, 2 to 15 percent slopes, very stony52C433519122kf5wva02319901:20000
Thurmont gravelly loam, 3 to 8 percent slopes50B297516569kbjjva04319801:15840
Thurmont loam, 3 to 8 percent slopes49B193516568kbjhva04319801:15840
Thurmont-Wintergreen complex, 8 to 15 percent slopes36C2278582042mjnkva06720041:24000
Thurmont-Wintergreen complex, 2 to 8 percent slopes36B248582041mjnjva06720041:24000
Thurmont-Urban land-Wintergreen complex, 8 to 15 percent slopes35C218582040mjnhva06720041:24000
Thurmont-Wintergreen complex, 15 to 25 percent slopes36D172582043mjnlva06720041:24000
Thurmont very stony loam, 15 to 25 percent slopesTvD1284516909kbwhva07919831:15840
Thurmont loam, 7 to 15 percent slopesThC653516907kbwfva07919831:15840
Thurmont loam, 15 to 25 percent slopesThD238516908kbwgva07919831:15840
Braddock-Thurmont loams, 2 to 7 percent slopesBcB522516925kbx0va11319671:15840
Braddock-Thurmont loams, 7 to 15 percent slopesBcC379516926kbx1va11319671:15840
Braddock-Thurmont loams, 15 to 25 percent slopes, erodedBcD2179516927kbx2va11319671:15840
Thurmont loam, 7 to 15 percent slopes46C8751371084lnvva12519921:24000
Thurmont loam, 2 to 7 percent slopes46B6251371064lnsva12519921:24000
Thurmont loam, 2 to 7 percent slopes, very stony47B5851371124lnzva12519921:24000
Thurmont loam, 15 to 25 percent slopes, very stony47D5021371144lp1va12519921:24000
Thurmont loam, 7 to 15 percent slopes, very stony47C3901371134lp0va12519921:24000
Thurmont loam, 15 to 25 percent slopes46D2591371104lnxva12519921:24000
Thurmont fine sandy loam, 7 to 15 percent slopes46C4831517281kc8hva13919951:20000
Thurmont fine sandy loam, 15 to 25 percent slopes46D3972517282kc8jva13919951:20000
Thurmont fine sandy loam, 2 to 7 percent slopes46B2456517280kc8gva13919951:20000
Thurmont fine sandy loam, 8 to 15 percent slopes43C325914740141lgtvva14120081:24000
Thurmont fine sandy loam, 2 to 8 percent slopes43B216314740131lgttva14120081:24000
Thurmont fine sandy loam, 15 to 25 percent slopes43D78814740151lgtwva14120081:24000
Thurmont cobbly fine sandy loam, 8 to 15 percent slopes, very stony44C34314740821lgx1va14120081:24000
Thurmont cobbly fine sandy loam, 15 to 25 percent slopes, very stony44D17314740831lgx2va14120081:24000
Unison-Thurmont complex, 7 to 15 percent slopes, very stonyStC30195174692tmclva15719581:20000
Unison-Thurmont complex, 15 to 25 percent slopes, very stonyStD12965174702tmcmva15719581:20000
Thurmont sandy loam, 7 to 15 percent slopes47C1028520324kgfnva16119901:24000
Thurmont sandy loam, 2 to 7 percent slopes47B262520322kgflva16119901:24000
Thurmont loam, 2 to 15 percent slopes, very stony33C631740832z3fpva8501:24000
Thurmont loam, 15 to 30 percent slopes, very stony33E131740822z3fnva8501:24000
Thurmont gravelly loam, 15 to 25 percent slopesThD27117102521vdnfwv0371:24000
Thurmont gravelly loam, 8 to 15 percent slopesThC21417102511vdndwv0371:24000

Map of Series Extent

Approximate geographic distribution of the THURMONT 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 .