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
Pedons used in the lab summary:
| MLRA | Lab ID | Pedon ID | Taxonname | CI | NSSL / NASIS Reports | Link To SoilWeb GMap |
|---|---|---|---|---|---|---|
| 72 | 00P0086 | 99KS069001 | Bridgeport | n/a | Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties | 37.8560829,-100.5649414 |
| 72 | 40A2233 | S1957NE057001 | Bridgeport | n/a | Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties | 40.0936127,-101.4536133 |
| 72 | 40A2234 | S1957NE057002 | Bridgeport | n/a | Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties | 40.1049995,-101.4280548 |
| 72 | 40A2235 | S1957NE057004 | Bridgeport | n/a | Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties | 40.0172234,-101.9552765 |
| 72 | 03N0654 | S2002KS055001 | Bridgeport | n/a | Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties | 38.0026398,-100.9396591 |
| n/a | 82P0752 | 82KS199002 | Bridgeport | n/a | Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties | n/a |
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.
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 .
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 .
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 .
Soil series competing with BRIDGEPORT share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .
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 .
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 .
Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.
Typical pattern of soils and parent material in the Colby-Razor association (Soil Survey of Cheyenne County, Kansas; 1989).
Typical cross section of the valley of the Arkansas River (Soil Survey of Finney County, Kansas; 1965).
Relationships of soils in association 1. Included is a small part of association 3 (Soil Survey of Grant County, Kansas; 1969).
Relationships of soils in association 2 (Soil Survey of Grant County, Kansas; 1969).
Relationships of soils in association 3 (Soil Survey of Grant County, Kansas; 1969).
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).
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).
Geologic profile extending in a north-south direction through the central part of Hamilton County (Soil Survey of Hamilton County, Kansas; 1961).
Pattern of soils in association 3 (Soil Survey of Hodgeman County, Kansas; 1973).
Pattern of soils in associations 6 and 12 (Soil Survey of Hodgeman County, Kansas; 1973).
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).
Pattern of soils in association 2 (Soil Survey of Lane County, Kansas; 1972).
Typical cross section of part of the valley of Ladder (Beaver) Creek (Soil Survey of Scott County, Kansas; 1965).
Typical pattern of soils in the Ulysses-Pendend-Colby association (Soil Survey of Sheridan County, Kansas; 1984).
Typical pattern of major soils in soil association 2 (Soil Survey of Sherman County, Kansas; 1973).
Major range sites in Sherman County (Soil Survey of Sherman County, Kansas; 1973).
A cross section of Sherman County soils extending through the center of the county (Soil Survey of Sherman County, Kansas; 1973).
Diagram of the Manter-Dalhart-Ulysses soil association in the valley of Bear Creek (Soil Survey of Stanton County, Kansas; 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).
Typical pattern of soils and underlying material in the Ulysses-Colby association (Soil Survey of Wallace County, Kansas; 1986).
Typical pattern of soils and underlying material in the Colby-Kim-Midway association (Soil Survey of Wallace County, Kansas; 1986).
Cross section of association 2 along White Woman Creek (Soil Survey of Wichita County, Kansas; 1965).
Relationship of soils to the landscape and to the common parent materials of Wichita County (Soil Survey of Wichita County, Kansas; 1965).
Colby soil association merging with the Bridgeport-Havre soil association (Soil Survey of Dundy County, Nebraska; 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).
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).
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).
Typical pattern of soils in the Hord, terrace-McCook-Bridgeport association (Soil Survey of Red Willow County, Nebraska; April 1967).
Map units containing BRIDGEPORT as a major component. Limited to 250 records.
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 .