Official Series Description


Lab Data Summary

Aggregate lab data for the BRIDGEPORT soil series. This aggregation is based on all pedons with a current taxon name of BRIDGEPORT, 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 BRIDGEPORT 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
7200P008699KS069001Bridgeport8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8560829,-100.5649414
7240A2233S1957NE057001Bridgeport7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0936127,-101.4536133
7240A2234S1957NE057002Bridgeport7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1049995,-101.4280548
7240A2235S1957NE057004Bridgeport7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0172234,-101.9552765
7203N0654S2002KS055001Bridgeport8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0026398,-100.9396591
7340A183153KS141007Bridgeport5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4230537,-98.6394424
n/a82P075282KS199002Bridgeport3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

There are insufficient data to create the 2D hillslope position figure.

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

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 BRIDGEPORT, 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. KS-2012-01-20-19 | Cheyenne County - June 1989

    Typical pattern of soils and parent material in the Colby-Razor association (Soil Survey of Cheyenne County, Kansas; 1989).

  2. KS-2012-01-23-02 | Finney County - November 1965

    Typical cross section of the valley of the Arkansas River (Soil Survey of Finney County, Kansas; 1965).

  3. KS-2012-01-23-12 | Grant County - December 1969

    Relationships of soils in association 1. Included is a small part of association 3 (Soil Survey of Grant County, Kansas; 1969).

  4. KS-2012-01-23-13 | Grant County - December 1969

    Relationships of soils in association 2 (Soil Survey of Grant County, Kansas; 1969).

  5. KS-2012-01-23-14 | Grant County - December 1969

    Relationships of soils in association 3 (Soil Survey of Grant County, Kansas; 1969).

  6. KS-2012-01-23-18 | Gray County - January 1968

    Soils of the Mansic-Ulysses soil association are on the right; on the left are soils of the Pratt-Tivoli soil association (Soil Survey of Gray County, Kansas; 1968).

  7. KS-2012-01-23-20 | Gray County - January 1968

    Approximate geologic cross section through the central part of Gray County and the general location of soils on the landscape (Soil Survey of Gray County, Kansas; 1968).

  8. KS-2012-01-23-25 | Hamilton County - November 1961

    Geologic profile extending in a north-south direction through the central part of Hamilton County (Soil Survey of Hamilton County, Kansas; 1961).

  9. KS-2012-01-23-35 | Hodgeman County - June 1973

    Pattern of soils in association 3 (Soil Survey of Hodgeman County, Kansas; 1973).

  10. KS-2012-01-23-36 | Hodgeman County - June 1973

    Pattern of soils in associations 6 and 12 (Soil Survey of Hodgeman County, Kansas; 1973).

  11. KS-2012-01-23-44 | Kearny County - November 1963

    An approximate geologic profile of Kearny County, extending in a north-south direction across the county near Hartland (Soil Survey of Kearny County, Kansas; 1963).

  12. KS-2012-01-23-52 | Lane County - November 1972

    Pattern of soils in association 2 (Soil Survey of Lane County, Kansas; 1972).

  13. KS-2012-01-25-33 | Scott County - December 1965

    Typical cross section of part of the valley of Ladder (Beaver) Creek (Soil Survey of Scott County, Kansas; 1965).

  14. KS-2012-01-26-03 | Sheridan County - March 1984

    Typical pattern of soils in the Ulysses-Pendend-Colby association (Soil Survey of Sheridan County, Kansas; 1984).

  15. KS-2012-01-26-06 | Sherman County - March 1973

    Typical pattern of major soils in soil association 2 (Soil Survey of Sherman County, Kansas; 1973).

  16. KS-2012-01-26-08 | Sherman County - March 1973

    Major range sites in Sherman County (Soil Survey of Sherman County, Kansas; 1973).

  17. KS-2012-01-26-09 | Sherman County - March 1973

    A cross section of Sherman County soils extending through the center of the county (Soil Survey of Sherman County, Kansas; 1973).

  18. KS-2012-01-26-11 | Stanton County - December 1961

    Diagram of the Manter-Dalhart-Ulysses soil association in the valley of Bear Creek (Soil Survey of Stanton County, Kansas; 1961).

  19. KS-2012-01-26-12 | Stanton County - December 1961

    Pattern of soils of the upland in northeastern Stanton County and cross section of part of the valley of Bear Creek (Soil Survey of Stanton County, Kansas; 1961).

  20. KS-2012-01-26-24 | Wallace County - March 1986

    Typical pattern of soils and underlying material in the Ulysses-Colby association (Soil Survey of Wallace County, Kansas; 1986).

  21. KS-2012-01-26-25 | Wallace County - March 1986

    Typical pattern of soils and underlying material in the Colby-Kim-Midway association (Soil Survey of Wallace County, Kansas; 1986).

  22. KS-2012-01-26-30 | Wichita County - November 1965

    Cross section of association 2 along White Woman Creek (Soil Survey of Wichita County, Kansas; 1965).

  23. KS-2012-01-26-31 | Wichita County - November 1965

    Relationship of soils to the landscape and to the common parent materials of Wichita County (Soil Survey of Wichita County, Kansas; 1965).

  24. NE-2012-02-10-27 | Dundy County - February 1963

    Colby soil association merging with the Bridgeport-Havre soil association (Soil Survey of Dundy County, Nebraska; February 1963).

  25. NE-2012-02-10-29 | Dundy County - February 1963

    The Bridgeport-Havre soil association, on the right, merges with the Sandy alluvial land-Las association (Soil Survey of Dundy County, Nebraska; February 1963).

  26. NE-2012-02-13-46 | Kimball County - March 1962

    Typical soil pattern in the Altvan-Rosebud-Dix association: (1) deep Altvan loams; (2) Goshen loams; (3) moderately deep Altvan loams; (4) Gravelly land; (5) Bridgeport loams; and (6) Tripp loams (Soil Survey of Kimball County, Nebraska; March 1962).

  27. NE-2012-02-13-47 | Kimball County - March 1962

    Pattern of soils in valley of Lodgepole Creek: (1) Rosebud loams; (2) Bridgeport loams; (3) Tripp loams; (4) Parshall sandy loams; (5) Havre silt loam; (6) Vebar sandy loams; (7) Altvan loams; (8) Canyon complexes; (9) Gravelly land; and (10) Canyon-Rosebud loams (Soil Survey of Kimball County, Nebraska; March 1962).

  28. NE-2012-02-13-75 | Red Willow County - April 1967

    Typical pattern of soils in the Hord, terrace-McCook-Bridgeport association (Soil Survey of Red Willow County, Nebraska; April 1967).

Map Units

Map units containing BRIDGEPORT 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
Bridgeport loam1610969449535b7co07519741:24000
Bridgeport loam, 1 to 3 percent slopesBrB26419492335s1co11519691:15840
Bridgeport loam, 0 to 1 percent slopesBrA16369492135rzco11519691:15840
Bridgeport loam, 0 to 3 percent slopesBraB10399492235s0co11519691:15840
Bridgeport silt loam1167399497035tkco12119821:24000
Bridgeport silt loam, rarely flooded2310789114404572twlcks00919791:24000
Bridgeport silt loam, rarely flooded2310980111495912twljks02319871:24000
Bridgeport silt loam, channeled1124509311495462w5dxks02319871:24000
Bridgeport silt loam, 2 to 5 percent slopes1560353911495582w5dwks02319871:24000
Bridgeport silt loam, occasionally flooded1125251911495472x2x0ks02319871:24000
Bridgeport silt loam, occasionally flooded112560613820052zt6zks02919721:24000
Bridgeport silt loam, rarely flooded23101957111505662twljks03919851:24000
Bridgeport silt loam, 2 to 5 percent slopes1560501011505642w5dwks03919851:24000
Bridgeport silt loam, occasionally flooded1125379111505652x2x0ks03919851:24000
Bridgeport silt loam, occasionally flooded1125629211523032x2x0ks05519621:24000
Bridgeport clay loam, rarely flooded13426212115230117p20ks05519621:24000
Bridgeport loam, channeled1122373111523022zwjlks05519621:24000
Bridgeport silt loam, rarely flooded231039814543622twlcks05519621:24000
Bridgeport clay loam, saline, rarely flooded134311714537771kss1ks05519621:24000
Bridgeport silty clay loam, 2 to 5 percent slopes15628313804122yl49ks05719621:24000
Bridgeport silt loam, channeled11244713804112w5dxks05719621:24000
Bridgeport silt loam, occasionally flooded1125911611506582x2x0ks06319741:24000
Munjor-Bridgeport complex, occasionally flooded2203273711506872yl3sks06319741:24000
Penden-Bridgeport complex, 0 to 15 percent slopes275823111506922twdpks06319741:24000
Bridgeport loam, rarely flooded1345311506572zwjqks06319741:24000
Bridgeport silt loam, rarely flooded2310611411507882twljks06519851:24000
Bridgeport silty clay loam, rarely flooded1349903013806512zwjjks06719651:24000
Bridgeport fine sandy loam, rarely flooded1344207013806501hbp3ks06719651:24000
Bridgeport silt loam, channeled1124363713805592w5dxks06919651:24000
Bridgeport silty clay loam, 1 to 3 percent slopes1350238813805602yl48ks06919651:24000
Bridgeport silty clay loam, rarely flooded1349143613805612yl4bks06919651:24000
Bridgeport clay loam, rarely flooded13424013805581hbl4ks06919651:24000
Bridgeport silt loam, rarely flooded23105060115182517nknks07119591:24000
Bridgeport clay loam, saline, rarely flooded134311245115220917nz1ks07519591:24000
Bridgeport silt loam, channeled1124396911522102w5dxks07519591:24000
Bridgeport clay loam, rarely flooded1342193314522881kr70ks07519591:24000
Roxbury-Bridgeport complex, channeled, frequently flooded2232119581152394307nxks08319661:24000
Bridgeport silt loam, rarely flooded2310586611523982twlcks08319661:24000
Bridgeport silty clay loam, 2 to 5 percent slopes1562423911523882yl49ks08319661:24000
Bridgeport loam, channeled11225911523872zwjlks08319661:24000
Bridgeport clay loam, saline, rarely flooded13437633115225317p0gks09319611:24000
Bridgeport loam, channeled1122125411522542yl47ks09319611:24000
Bridgeport silty clay loam, rarely flooded1349119211522552zwjjks09319611:24000
Bridgeport loam, channeled1122403911520082zwjlks10119661:24000
Bridgeport silt loam, rarely flooded2310207111520102twlcks10119661:24000
Bridgeport loam, rarely flooded13451111520092zwjqks10119661:24000
Bridgeport loam, rarely flooded1345905011505042zwjqks10919621:24000
Bridgeport silt loam, channeled1124645411505052w5dxks10919621:24000
Bridgeport silt loam, rarely flooded2310267711505062twljks10919621:24000
Bridgeport loam, channeled112277511505022zwjlks10919621:24000
Bridgeport loam, occasionally flooded1123361115050317m60ks10919621:24000
Bridgeport silt loam, rarely flooded2310852214291952twlcks11319801:24000
Bridgeport silt loam, channeled1124613817722w5dxks11919731:24000
Penden-Bridgeport complex, 0 to 15 percent slopes27581531211520892twdpks13519711:24000
Bridgeport silt loam, rarely flooded23101286411520612twlcks13519711:24000
Bridgeport loam, channeled11228911520602zwjlks13519711:24000
Bridgeport silt loam, rarely flooded23103011507492twlcks13719731:24000
Bridgeport silt loam, rarely flooded23101362613801132twlcks14519761:24000
Bridgeport silt loam, rarely flooded2310409111508972twlcks14719851:24000
Bridgeport silt loam, occasionally flooded11251477630306832x2x0ks15319791:24000
Bridgeport silt loam, rarely flooded2310120657729692twljks15319791:24000
Bridgeport silt loam, 2 to 5 percent slopes156072677729702w5dwks15319791:24000
Bridgeport silt loam, rarely flooded2310869711521162twlcks16519781:24000
Bridgeport silt loam, rarely flooded231024113821552twlcks16919891:24000
Bridgeport loam, rarely flooded1345333411519692zwjqks17119631:24000
Bridgeport fine sandy loam, rarely flooded13441395115196717nq7ks17119631:24000
Bridgeport loam, channeled1122125011519682zwjlks17119631:24000
Bridgeport silt loam, occasionally flooded11254311519702x2x0ks17119631:24000
Bridgeport loam, channeled, frequently flooded112228713826191hdqmks17519631:24000
Bridgeport silt loam, rarely flooded23101034511499872twljks17919821:24000
Bridgeport silt loam, 2 to 5 percent slopes156096511499862w5dwks17919821:24000
Bridgeport silt loam, channeled1124480811496062w5dxks18119671:24000
Bridgeport silt loam, rarely flooded2310348711496072twljks18119671:24000
Bridgeport silt loam, 2 to 5 percent slopes1560285411496052w5dwks18119671:24000
Bridgeport loam, occasionally flooded1123442114960417l80ks18119671:24000
Bridgeport-Arvada complex, rarely flooded1351348114960817l84ks18119671:24000
Bridgeport clay loam, rarely flooded1342644013825501hdndks18719591:24000
Bridgeport silty clay loam, rarely flooded1349363813825512zwjjks18719591:24000
Bridgeport silt loam, rarely flooded2310107011504552twljks19319781:24000
Bridgeport silt loam, occasionally flooded112526711504542x2x0ks19319781:24000
Munjor-Bridgeport complex, occasionally flooded22031911508682yl3sks19519861:24000
Bridgeport silt loam, occasionally flooded1125711508342x2x0ks19519861:24000
Bridgeport silt loam, rarely flooded23101280711501862twljks19919841:24000
Bridgeport loam, occasionally flooded11238150115018417lvqks19919841:24000
Bridgeport silt loam, 2 to 5 percent slopes1560299711501852w5dwks19919841:24000
Bridgeport-Arvada complex, rarely flooded13512873115018717lvtks19919841:24000
Bridgeport loam, rarely flooded1345432911519322zwjqks20319631:24000
Bridgeport silt loam, channeled112489211519332w5dxks20319631:24000
Bridgeport silt loam, rarely flooded2310215115193417np5ks20319631:24000
Bridgeport complexBp4157354375cwrgsd12319751:20000
Bridgeport complex, channeledBt1150354376cwrhsd12319751:20000
Bridgeport silt loamBp27932580879cygfsd60620111:24000
Bridgeport loam, cool, 0 to 3 percent slopes, rarely floodedU240A29824852622pf3rsd61220111:20000
Bridgeport loam, cool, 0 to 3 percent slopes, rarely floodedU240A10125828272pf3rsd61320111:24000

Map of Series Extent

Approximate geographic distribution of the BRIDGEPORT 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 .