Official Series Description


Lab Data Summary

Aggregate lab data for the KEYPORT soil series. This aggregation is based on all pedons with a current taxon name of KEYPORT, 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 KEYPORT 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
149A92P048092NJ005007Keyport6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1316681,-74.6200027
149A93P025692NJ033012Keyport7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5783348,-75.375
149A93P025792NJ033014Keyport5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5783348,-75.3850021
153D85P001184MD019001Keyport7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5922203,-76.2108307

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KEYPORT 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 KEYPORT 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 KEYPORT 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 KEYPORT 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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Competing Series

Soil series competing with KEYPORT 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 KEYPORT 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 KEYPORT 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 KEYPORT, 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-2011-05-31-02 | District of Columbia - 1976

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

  2. MD-2010-09-03-01 | City of Baltimore - 1998

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

  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-2012-02-03-01 | Anne Arundel County - February 1973

    Representative pattern of soils and parent material in soil association 2 (Soil Survey of Anne Arundel County, Maryland; February 1973).

  5. MD-2012-02-03-02 | Anne Arundel County - February 1973

    Representative pattern of soils and parent material in soil association 5 (Soil Survey of Anne Arundel County, Maryland; February 1973).

  6. 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).

  7. MD-2012-02-03-05 | City of Baltimore - 1998

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

  8. MD-2012-02-03-11 | Charles County - July 1974

    Cross section of association 7 showing topography, important soils, and underlying material (Soil Survey of Charles County, Maryland; July 1974).

Map Units

Map units containing KEYPORT 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
Keyport-Urban land complex, 0 to 8 percent slopesKmB35412862349v4dc00119751:12000
Urban land-Keyport complex, 0 to 8 percent slopesUpB18812868249x1dc00119751:12000
Keyport-Urban land complex, 8 to 15 percent slopesKmC11412862449v5dc00119751:12000
Keyport fine sandy loam, 0 to 8 percent slopesKeB11212862149v2dc00119751:12000
Keyport fine sandy loam, 8 to 15 percent slopesKeC4612862249v3dc00119751:12000
Keyport silt loam, 0 to 2 percent slopesKpA18216060811qx82de00120061:24000
Keyport fine sandy loam, 0 to 2 percent slopesKfA6616060801qx81de00120061:24000
Keyport silt loam, 2 to 5 percent slopesKpB222524798142p7g0de00320091:24000
Keyport sandy loam, 5 to 10 percent slopesKhC121324798152p7g1de00320091:24000
Keyport silt loam, 0 to 2 percent slopesKpA31724798132p7fzde00320091:24000
Keyport loam, 10 to 25 percent slopesKmE8624798122p7fyde00320091:24000
Keyport fine sandy loam, 0 to 2 percent slopesKfA115116034331qthnde00520061:24000
Keyport silt loam, 0 to 2 percent slopesKpA48316034381qthtde00520061:24000
Keyport silt loam, 2 to 5 percent slopesKpB2516034391qthvde00520061:24000
Keyport-Urban land complex, 0 to 5 percent slopesKuB109924049072lqhnmd00520101:12000
Keyport silt loam, 2 to 5 percent slopesKeB75224049052lqhlmd00520101:12000
Keyport silt loam, 5 to 10 percent slopesKeC35424049062lqhmmd00520101:12000
Keyport silt loam, 0 to 2 percent slopesKeA20524048722lqgjmd00520101:12000
Keyport-Urban land complex, 5 to 15 percent slopesKuD14124813692p925md00520101:12000
Keyport silt loam, wet subsoil, 0 to 2 percent slopesKwA32225168812pz8lmd00919671:20000
Keyport silt loam, wet subsoil, 2 to 5 percent slopesKwB24225168822pz8mmd00919671:20000
Keyport silt loam, 2 to 5 percent slopesKpB224824406442mxpgmd01520091:12000
Keyport loam, 5 to 10 percent slopesKmC87724406422mxpdmd01520091:12000
Keyport silt loam, 5 to 10 percent slopesKpC39924406452mxphmd01520091:12000
Keyport silt loam, 0 to 2 percent slopesKpA20924406432mxpfmd01520091:12000
Keyport silt loam, 0 to 2 percent slopesKpA51041289494b5nmd01919921:15840
Keyport silt loam, 2 to 5 percent slopesKpB21285127987495mmd02919781:15840
Keyport silt loam, 0 to 2 percent slopesKpA1255127986495lmd02919781:15840
Keyport fine sandy loam, 2 to 5 percent slopesKmB2579127985495kmd02919781:15840
Keyport silt loam, 5 to 15 percent slopes, moderately erodedKpC2531127988495nmd02919781:15840
Keyport fine sandy loam, 0 to 2 percent slopesKmA263127984495jmd02919781:15840
Keyport silt loam, 0 to 2 percent slopesKrA153112832249jfmd03719751:20000
Keyport silt loam, 2 to 5 percent slopes moderately erodedKrB2102412832349jgmd03719751:20000
Keyport silt loam, 5 to 10 percent slopes, moderately erodedKrC251612832449jhmd03719751:20000
Keyport fine sandy loam, 2 to 5 percent slopes, moderately erodedKpB243012832149jdmd03719751:20000
Keyport fine sandy loam, 0 to 2 percent slopesKpA42012832049jcmd03719751:20000
Keyport silt loam, 0 to 2 percent slopesKpA17116002321qq5dmd03920061:12000
Keyport fine sandy loam, 0 to 2 percent slopesKfA226997557111r51md04520051:12000
Keyport fine sandy loam, 2 to 5 percent slopesKfB47497557211r52md04520051:12000
Keyport-Urban land complex, 0 to 8 percent slopes15UB854533899kxkkmd51019931:12000
Urban land-Beltsville-Keyport complex, 0 to 8 percent slopes3UB193533958kxmgmd51019931:12000
Keyport loam, 0 to 8 percent slopes15B183533898kxkjmd51019931:12000
Beltsville-Keyport complex, 0 to 8 percent slopes2B168533938kxltmd51019931:12000
Urban land-Keyport complex, 0 to 8 percent slopes16UB164533900kxklmd51019931:12000
Keyport silt loam, 2 to 5 percent slopesKpB1551533403kx1kmd60019721:15840
Keyport silt loam, 0 to 2 percent slopesKpA318533402kx1jmd60019721:15840
Keyport loam, 2 to 5 percent slopesKeoB1337697771rf2rnj00519671:24000
Keyport loam, 0 to 2 percent slopesKeoA865697770rf2qnj00519671:24000
Keyport loam, 5 to 10 percent slopesKeoC849697772rf2snj00519671:24000
Keyport loam, 10 to 15 percent slopesKeoD769697773rf2tnj00519671:24000
Keyport fine sandy loam, 2 to 5 percent slopesKenB662697769rf2pnj00519671:24000
Keyport loam, 15 to 25 percent slopesKeoE526697774rf2vnj00519671:24000
Keyport loamy sand, 0 to 5 percent slopesKefB221697768rf2nnj00519671:24000
Keyport-Urban land complex, 0 to 10 percent slopesKeuC36697775rf2wnj00519671:24000
Keyport sandy loam, 2 to 5 percent slopesKemB1642108948415kpnnj01520041:24000
Keyport loam, 0 to 2 percent slopesKeoA374108948815kpsnj01520041:24000
Keyport sandy loam, 5 to 10 percent slopes, erodedKemC2168108948615kpqnj01520041:24000
Keyport-Urban land complex, 0 to 5 percent slopesKeuB121108948915kptnj01520041:24000
Lenoir-Keyport silt loams, 0 to 5 percent slopesLenB7281351714jncnj02119691:24000
Keyport loam, 2 to 5 percent slopesKeoB20411353934jwjnj02319851:24000
Keyport sandy loam, 2 to 5 percent slopesKemB17981353904jwfnj02319851:24000
Keyport loam, 0 to 2 percent slopesKeoA12421353924jwhnj02319851:24000
Keyport sandy loam, 0 to 2 percent slopesKemA12161353894jwdnj02319851:24000
Keyport-Urban land complex, 0 to 10 percent slopesKeuC10541353964jwmnj02319851:24000
Keyport loam, 5 to 10 percent slopesKeoC6401353944jwknj02319851:24000
Keyport loam, 10 to 15 percent slopesKeoD6121353954jwlnj02319851:24000
Keyport sandy loam, 10 to 15 percent slopesKemD3751353914jwgnj02319851:24000
Keyport silt loam, 0 to 2 percent slopesKepA211606486nc32nj02319851:24000
Keyport silt loam, 2 to 5 percent slopesKepB36606487nc33nj02319851:24000
Keyport sandy loam, 5 to 10 oercent slopesKemC1606669nc8znj02319851:24000
Keyport sandy loam, 2 to 5 percent slopesKemB22501347914j83nj02519851:24000
Keyport-Urban land complex, 0 to 10 percent slopesKeuC14781347944j86nj02519851:24000
Keyport sandy loam, 0 to 2 percent slopesKemA12671347904j82nj02519851:24000
Keyport sandy loam, 5 to 10 percent slopesKemC3711347924j84nj02519851:24000
Keyport sandy loam, 10 to 15 percent slopesKemD2801347934j85nj02519851:24000
Keyport loam, 2 to 5 percent slopesKeoB491347324j66nj02519851:24000
Keyport loam, 10 to 15 percent slopesKeoD171347334j67nj02519851:24000
Keyport loam, 0 to 2 percent slopesKeoA51347314j65nj02519851:24000
Keyport sandy loam, 0 to 2 percent slopesKemA690697527rdtwnj02919781:24000
Keyport loam, 5 to 10 percent slopesKeoC221356394k4gnj03320041:24000
Keyport silt loam, 2 to 5 percent slopesKepB469548477ldqtnj03519721:24000
Keyport silt loam, 0 to 2 percent slopesKepA349548476ldqsnj03519721:24000
Keyport silt loam, 8 to 12 percent slopes, erodedKyD29511948940bhva11519601:20000
Keyport silt loam, 0 to 2 percent slopesKyA7911948840bgva11519601:20000

Map of Series Extent

Approximate geographic distribution of the KEYPORT 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 .