Official Series Description


Lab Data Summary

Aggregate lab data for the BELTSVILLE soil series. This aggregation is based on all pedons with a current taxon name of BELTSVILLE, 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 BELTSVILLE 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
14888P038988MD510008Beltsville5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3419456,-76.6011124
149A01N096601MD017002Beltsville7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.557251,-77.0073853
149A40A128670MD031001BELTSVILLE4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0584222,-76.9578472
149A86P0168S1985MD031002Beltsville7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0587083,-76.9583111
149A95P0269S1994MD033001Beltsville6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6280556,-76.7585389
n/a40A424276MD029002Beltsville7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BELTSVILLE 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 BELTSVILLE 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 BELTSVILLE 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 BELTSVILLE 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 BELTSVILLE 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 BELTSVILLE 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 BELTSVILLE 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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Click the image to view it full size.

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 BELTSVILLE, 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. DC-2011-05-31-01 | District of Columbia - 1976

    Typical pattern of soils and parent material in the Urban land-Beltsville-Chillum association (Soil Survey of District of Columbia; 1976).

  2. DC-2011-05-31-04 | District of Columbia - 1976

    Diagram of fall line between the Piedmont Plateau and the Coastal Plain. Diagram also shows the relationship of parent material and topography (Soil Survey of District of Columbia; 1976).

  3. MD-2010-09-03-03 | City of Baltimore - 1998

    Pattern of soils in the Urban land-Joppa-Sassafras association (Soil Survey of City of Baltimore, Maryland; 1998).

  4. MD-2012-02-03-04 | City of Baltimore - 1998

    Pattern of soils in the Urban land-Joppa-Sassafras association (Soil Survey of City of Baltimore, Maryland; 1998).

  5. MD-2012-02-03-08 | Baltimore County - March 1978

    Cross section showing relationships of parent material and topography to certain soil series of Baltimore County. Fall line shown in drawing separates soil of Piedmont Province (left) from soils of Atlantic Coastal Plain (right) (Soil Survey of Baltimore County, Maryland; March 1976).

  6. MD-2012-02-03-09 | Charles County - July 1974

    Cross section of association 1 showing topography, important soils, and underlying material (Soil Survey of Charles County, Maryland; July 1974).

  7. MD-2012-02-03-10 | Charles County - July 1974

    Cross section of association 2 showing topography, important soils, and underlying material (Soil Survey of Charles County, Maryland; July 1974).

Map Units

Map units containing BELTSVILLE 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
Beltsville-Urban land complex, 0 to 8 percent slopesBeB65112856649s9dc00119751:12000
Urban land-Beltsville complex, 0 to 8 percent slopesUcB29412867349wrdc00119751:12000
Beltsville silt loam, 0 to 8 percent slopesBdB5212856549s8dc00119751:12000
Beltsville-Urban land complex, 0 to 5 percent slopesBfB171224041502lpq7md00520101:12000
Beltsville silt loam, 2 to 5 percent slopesBeB86924041412lppymd00520101:12000
Beltsville-Urban land complex, 5 to 15 percent slopesBfD84324041512lpq8md00520101:12000
Beltsville silt loam, 5 to 10 percent slopesBeC69024041482lpq5md00520101:12000
Beltsville silt loam, 0 to 2 percent slopesBeA16124041382lppvmd00520101:12000
Matapeake-Beltsville complex, 2 to 5 percent slopesMeB216825168952pz8pmd00919671:20000
Beltsville-Aquasco complex, 2 to 5 percent slopesBeB95425168582pz7smd00919671:20000
Matapeake-Beltsville complex, 0 to 2 percent slopesMeA22925168942pz8nmd00919671:20000
Beltsville silt loam, 2 to 5 percent slopesBeB388324406132mxngmd01520091:12000
Beltsville silt loam, 5 to 10 percent slopesBeC273024406142mxnhmd01520091:12000
Beltsville silt loam, 0 to 2 percent slopesBeA51724406122mxnfmd01520091:12000
Beltsville silt loam, 2 to 5 percent slopesBaB5783416086231qzx2md01720071:12000
Grosstown-Woodstown-Beltsville complex, 5 to 15 percent slopesGwD1527516086291qzx8md01720071:12000
Beltsville silt loam, 5 to 10 percent slopesBaC1167016086241qzx3md01720071:12000
Beltsville-Grosstown-Woodstown complex, 0 to 5 percent slopesBgB680616086281qzx7md01720071:12000
Beltsville-Aquasco complex, 0 to 2 percent slopesBcA662516086171qzwwmd01720071:12000
Marr-Beltsville complex, 5 to 15 percent slopesMkD515716086451qzxsmd01720071:12000
Beltsville-Urban land complex, 0 to 5 percent slopesBuB507216086251qzx4md01720071:12000
Urban land-Beltsville complex, 0 to 5 percent slopesUmB167316086141qzwsmd01720071:12000
Marr-Beltsville complex, 15 to 25 percent slopesMkE98216086461qzxtmd01720071:12000
Marr-Beltsville complex, 2 to 5 percent slopesMkB85716086441qzxrmd01720071:12000
Marr-Beltsville complex, 25 to 40 percent slopesMkF31216086471qzxvmd01720071:12000
Urban land-Chillum-Beltsville complex, 0 to 5 percent slopesUcB2463793649vmvlmd02720041:12000
Russett and Beltsville soils, 2 to 5 percent slopesRuB1200793638vmv7md02720041:12000
Urban land-Chillum-Beltsville complex, 5 to 15 percent slopesUcD887793650vmvmmd02720041:12000
Urban land-Sassafras-Beltsville complex, 0 to 5 percent slopesUsB844793653vmvqmd02720041:12000
Russett and Beltsville soils, 5 to 10 percent slopesRuC593793639vmv8md02720041:12000
Urban land-Sassafras-Beltsville complex, 5 to 15 percent slopesUsD316793655vmvsmd02720041:12000
Beltsville silt loam, 3 to 8 percent slopes59B3793098159kx9rmd03119891:15840
Beltsville silt loam, 0 to 3 percent slopes59A1473098158kx9qmd03119891:15840
Beltsville silt loam, 2 to 5 percent slopesBaB1088724552332ndw2md03320091:12000
Beltsville-Urban land complex, 0 to 5 percent slopesBuB738924552382ndw7md03320091:12000
Urban land-Beltsville complex, 0 to 5 percent slopesUrbB423024552402ndw9md03320091:12000
Beltsville silt loam, 0 to 2 percent slopesBaA332824552322ndw1md03320091:12000
Beltsville silt loam, 5 to 10 percent slopesBaC330224552372ndw6md03320091:12000
Beltsville-Urban land complex, 5 to 15 percent slopesBuD133824552392ndw8md03320091:12000
Grosstown-Woodstown-Beltsville complex, 5 to 15 percent slopesGwD31124552422ndwcmd03320091:12000
Beltsville-Grosstown-Woodstown complex, 0 to 5 percent slopesBgB24124552412ndwbmd03320091:12000
Beltsville silt loam, 2 to 5 percent slopes, moderately erodedBlB23319212828649h8md03719751:20000
Beltsville silt loam, 5 to 10 percent slopes, severely erodedBlC3452412828949hcmd03719751:20000
Beltsville silt loam, 5 to 10 percent slopes moderately erodedBlC2336912828849hbmd03719751:20000
Beltsville silt loam, 0 to 2 percent slopesBlA331612828549h7md03719751:20000
Beltsville silt loam, 2 to 5 percent slopes, severely erodedBlB355212828749h9md03719751:20000
Beltsville-Urban land complex, 0 to 8 percent slopes2UB984533939kxlvmd51019931:12000
Urban land-Beltsville complex, 0 to 8 percent slopes4UB291533969kxmtmd51019931:12000
Urban land-Beltsville-Keyport complex, 0 to 8 percent slopes3UB193533958kxmgmd51019931:12000
Beltsville-Keyport complex, 0 to 8 percent slopes2B168533938kxltmd51019931:12000
Beltsville-Urban land complex, 8 to 15 percent slopes2UC74533940kxlwmd51019931:12000
Beltsville silt loam, 2 to 5 percent slopesBeB2776533357kx02md60019721:15840
Beltsville silt loam, 0 to 2 percent slopesBeA849533356kx01md60019721:15840
Beltsville silt loam, 5 to 10 percent slopesBeC830533358kx03md60019721:15840
Beltsville silt loam, 2 to 5 percent slopesBeB12221295944bvgmd60119981:12000
Beltsville-Udorthents-Urban land complex, 0 to 5 percent slopesBU1861295924bvdmd60119981:12000
Beltsville silt loam, 0 to 2 percent slopesBeA1521295934bvfmd60119981:12000
Beltsville silt loam, 5 to 10 percent slopesBeC751295954bvhmd60119981:12000
Beltsville-Urban land complex, 3 to 8 percent slopesBeB8139844402yh35pa04519601:20000
Beltsville-Urban land complex, 0 to 3 percent slopesBeA2169844392yh34pa04519601:20000
Beltsville silt loam, 2 to 7 percent slopes7B253822502572fjkyva05920071:12000
Kingstowne-Beltsville complex, 2 to 7 percent slopes67B174822504502fjs5va05920071:12000
Beltsville very fine sandy loam, nearly levelBeA130111972840l6va13319601:20000
Beltsville very fine sandy loam, gently sloping, erodedBeB285411973040l8va13319601:20000
Beltsville very fine sandy loam, gently slopingBeB6711972940l7va13319601:20000

Map of Series Extent

Approximate geographic distribution of the BELTSVILLE 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 .