Official Series Description


Lab Data Summary

Aggregate lab data for the FORT MOTT soil series. This aggregation is based on all pedons with a current taxon name of FORT MOTT, 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 FORT MOTT 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
149A86P027685NJ033009Fort Mott6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5713882,-75.2986145
149A86P027885NJ033011Fort Mott7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.6366653,-75.3188858
149A95P0266S1994MD003016Fort Mott6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9447972,-76.6775528
153D86P010885MD019003Fort Mott7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5416679,-75.7777786
153D85P0013S1984MD019003Fort Mott7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.503334,-75.8083344

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FORT MOTT 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 FORT MOTT 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 FORT MOTT 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 FORT MOTT 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 FORT MOTT 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 FORT MOTT 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 FORT MOTT 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.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with FORT MOTT, 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-2010-09-10-13 | Wicomico County -

    Typical pattern of soils and examples of profiles and underlying material in general soil map unit 3 (Soil Survey of Wicomico County, Maryland).

  2. MD-2012-02-03-07 | Baltimore County - March 1977

    Cross section showing typical pattern in the Sassafras-Woodstown-Fallsington association (Soil Survey of Baltimore County, Maryland; March 1976).

  3. MD-2012-02-03-34 | Worcester County - May 1973

    Cross section showing typical soil pattern in the Fallingston-Woodstown-Sassafras association (Soil Survey of Worcester County, Maryland; May 1973).

  4. NJ-2010-09-13-01 | Cumberland County -

    Typical relationship of the soils, landform position, and parent material of soils that formed in loamy materials and sandy eolian deposits. The well drained Aura, Sassafras, Fort Mott, and Downer soils are in the higher landform positions. The moderately well drained Hammonton soils are in the lower landform positions in depressions or on flats (Soil Survey of Cumberland County, New Jersey).

  5. NJ-2012-02-14-01 | Cape May County - 2002

    The relationship of soils, landform position, and underlying material in the Downer-Ingleside-Swainton general soil map unit. Evesboro, Fort Mott, and Aura soils are minor components in the map unit (Soil Survey of Cape May County, New Jerser; 2002).

Map Units

Map units containing FORT MOTT 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
Fort Mott loamy sand, 2 to 5 percent slopesFmB192616060381qx6pde00120061:24000
Fort Mott loamy sand, 0 to 2 percent slopesFmA66916060371qx6nde00120061:24000
Fort Mott-Henlopen complex, 2 to 5 percent slopesFhB24416060391qx6qde00120061:24000
Fort Mott-Henlopen complex, 0 to 2 percent slopesFhA1047016033971qtghde00520061:24000
Fort Mott loamy sand, 0 to 2 percent slopesFmA1030616033991qtgkde00520061:24000
Fort Mott loamy sand, 2 to 5 percent slopesFmB686516034001qtglde00520061:24000
Fort Mott-Henlopen complex, 2 to 5 percent slopesFhB515616033981qtgjde00520061:24000
Patapsco-Fort Mott-Urban land complex, 0 to 5 percent slopesPgB171791378094mdgmd00320031:12000
Patapsco-Evesboro-Fort Mott complex, 0 to 5 percent slopesPeB99431378074mddmd00320031:12000
Patapsco-Fort Mott complex, 0 to 5 percent slopesPfB40451377114m99md00320031:12000
Patapsco-Fort Mott-Urban land complex, 5 to 15 percent slopesPgD14161378104mdhmd00320031:12000
Patapsco-Fort Mott complex, 5 to 10 percent slopesPfC12481378084mdfmd00320031:12000
Patapsco-Fort Mott complex, 10 to 15 percent slopesPfD3541378044md9md00320031:12000
Fort Mott loamy sand, 0 to 5 percent slopesFcB22924042682lpv1md00520101:12000
Fort Mott-Urban land complex, 0 to 5 percent slopesFdB19724042692lpv2md00520101:12000
Fort Mott-Cedartown complex, 15 to 25 percent slopesFcE27825168702pz87md00919671:20000
Fort Mott loamy sand, 2 to 5 percent slopesFmB85861289374b58md01919921:15840
Fort Mott loamy sand, 0 to 2 percent slopesFmA72871289364b57md01919921:15840
Fort Mott, Evesboro, and Downer soils, 15 to 30 percent slopesFNE1661289384b59md01919921:15840
Patapsco-Fort Mott complex, 5 to 10 percent slopesPfC2811454w7cymd02720041:12000
Fort Mott loamy sand, 0 to 5 percent slopesFmB6571279774959md02919781:15840
Fort Mott loamy sand, 5 to 10 percent slopes, moderately erodedFmC2288127978495bmd02919781:15840
Galestown-Fort Mott loamy sands, 0 to 5 percent slopesGfB27131396954pc9md03519951:12000
Fort Mott loamy sand, 2 to 5 percent slopesFmB9391396914pc5md03519951:12000
Fort Mott loamy sand, 0 to 2 percent slopesFmA4231396904pc4md03519951:12000
Galestown-Fort Mott loamy sands, 5 to 10 percent slopesGfC3131396964pcbmd03519951:12000
Fort Mott loamy sand, 0 to 2 percent slopesFmA641597555611r4kmd04520051:12000
Fort Mott loamy sand, 2 to 5 percent slopesFmB212697555711r4lmd04520051:12000
Fort Mott-Urban land complex, 0 to 2 percent slopesFuA683115326517q23md04520051:12000
Urban land-Fort Mott complex, 0 to 5 percent slopesUsB668115327217q2bmd04520051:12000
Fort Mott-Urban land complex, 2 to 5 percent slopesFuB219115326617q24md04520051:12000
Fort Mott loamy sand, 2 to 5 percent slopesFmB25121293034bk2md04719951:12000
Fort Mott loamy sand, 0 to 2 percent slopesFmA7291293014bk0md04719951:12000
Fort Mott sand, 0 to 5 percent slopesFobB2977745838t139nj00119751:24000
Fort Mott sand, 0 to 5 percent slopesFobB3473745566t0tjnj00919971:24000
Fort Mott loamy sand, 0 to 5 percent slopesFodB31151358344kbrnj01120031:24000
Fort Mott loamy sand, 0 to 5 percent slopesFodB9271351504jmpnj02119691:24000
Fort Mott loamy sand, 5 to 10 percent slopesFodC2121351514jmqnj02119691:24000
Fort Mott loamy sand, 0 to 5 percent slopesFodB10381353764jvznj02319851:24000
Fort Mott loamy sand, 0 to 5 percent slopesFodB11347264j60nj02519851:24000
Fort Mott loamy sand, 0 to 5 percent slopesFodB19991356004k36nj03320041:24000

Map of Series Extent

Approximate geographic distribution of the FORT MOTT 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 .