Official Series Description


Lab Data Summary

Aggregate lab data for the BEDFORD soil series. This aggregation is based on all pedons with a current taxon name of BEDFORD, 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 BEDFORD 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
114AMR76261976IN109026Bedford2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3415444,-86.5587833
120CMO79011979IN105001Bedford3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0132028,-86.3995528
120CWS80052014IN175002Bedford2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.702275,-86.2762833
122OR77101977IN117010Bedford2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6551028,-86.3633944
12207N02812006KY199010SBedford1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.0825005,-84.9023361
12207N02822006KY199011SBedford1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1102791,-84.8719406
12206N03262014IN061001Bedford7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.040995,-86.055002
12278P03812014IN117002Bedford7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.664694,-86.327397
122JN81092015IN071003Bedford2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8445222,-86.2591972
122LW78072015IN093003Bedford3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9325972,-86.5598972
12279KY-213-00579KY-213-005Bedford4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7475528,-86.6322583
12240A5233S1955IN043001BEDFORD4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3486671,-85.9349594
n/aHY-s101954-OH071-S10Bedford2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aHY-0591967-OH071-059Bedford4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a54KY-001-00154KY-001-001Bedford3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a54KY-227-00154KY-227-001Bedford4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a55KY-009-00155KY-009-001Bedford4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a55KY-009-00255KY-009-002Bedford4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a55KY-217-00255KY-217-002Bedford3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a58KY-103-00158KY-103-001Bedford4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a72KY-209-00872KY-209-008Bedford4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a40A5234S1955IN175001Bedford4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

Soil series competing with BEDFORD 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 BEDFORD 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 BEDFORD 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 BEDFORD, 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. IN-2012-01-19-38 | Orange County - May 1984

    Pattern of soils, topography, and underlying material in the Bedford-Bromer map unit (Soil Survey of Orange County, Indiana; 1984).

  2. KY-2012-01-26-07 | Allen County - September 1989

    Relationship of soils to topography and underlying material in the Christian-Mountview-Bedford general soil map unit (Soil Survey of Allen County, Kentucky; September 1989).

  3. KY-2012-01-26-08 | Allen County - September 1989

    Relationship of soils to topography and underlying material in the Trimblel-Bedford-Mountview general soil map unit (Soil Survey of Allen County, Kentucky; September 1989).

  4. KY-2012-01-26-20 | Bath County - September 1963

    Typical landscape showing the topography and the relative position of the principal soils in association 6 and the parent rocks from which the soils formed (Soil Survey of Bath County, Kentucky; September 1963).

  5. KY-2012-01-26-25 | Bath County - September 1963

    Cross section of Bath County showing the major soils and their relationship to the rock formations and to relief (Soil Survey of Bath County, Kentucky; September 1963).

  6. KY-2012-01-27-39 | Clark County - 1964

    Major soil series in soil association 6, their relationship to the landscape, and the parent rocks from which the soils formed (Soil Survey of Clark County, Kentucky; 1964).

  7. KY-2012-02-01-46 | Pulaski County - December 1974

    Pattern of soils and underlying material in association 1 (Soil Survey of Pulaski County, Kentucky; December 1974).

  8. KY-2012-02-01-47 | Pulaski County - December 1974

    Pattern of soils and underlying material in association 2 (Soil Survey of Pulaski County, Kentucky; December 1974).

  9. KY-2012-02-01-49 | Pulaski County - December 1974

    Pattern of soils and underlying material in association 4 (Soil Survey of Pulaski County, Kentucky; December 1974).

  10. KY-2012-02-01-50 | Pulaski County - December 1974

    Pattern of soils and underlying material in association 5 (Soil Survey of Pulaski County, Kentucky; December 1974).

Map Units

Map units containing BEDFORD 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
Bedford silt loam, 10 to 18 percent slopes, severely eroded598D32241713938ryx8il06920031:12000
Bedford silt loam, 10 to 18 percent slopes598D450713936ryx6il06920031:12000
Bedford silt loam, 10 to 18 percent slopes, eroded598D2255713937ryx7il06920031:12000
Bedford silt loam, 5 to 10 percent slopes, severely eroded598C3206713935ryx5il06920031:12000
Bedford silt loam, 5 to 10 percent slopes, eroded598C248713934ryx4il06920031:12000
Bedford silt loam, 10 to 18 percent slopes598D27414525771krjbil15120031:12000
Bedford silt loam, 5 to 10 percent slopes, eroded598C2263637241pd35il15120031:12000
Bedford silt loam, 10 to 18 percent slopes, eroded598D2258608138ndtcil15120031:12000
Bedford silt loam, 5 to 10 percent slopes, severely eroded598C3194608137ndtbil15120031:12000
Bedford silt loam, 10 to 18 percent slopes, severely eroded598D3156608139ndtdil15120031:12000
Bedford silt loam, 5 to 10 percent slopes598C13608136ndt9il15120031:12000
Bedford silt loam, 2 to 5 percent slopes598B9694815rb0dil15120031:12000
Crider-Bedford-Navilleton silt loams, 2 to 6 percent slopesCtwB37552010716r75in01920011:12000
Bedford silt loam, 0 to 2 percent slopesBdoA1152009292wh4fin01920011:12000
Bedford silt loam, 2 to 6 percent slopesBdoB962009306r2min01920011:12000
Crider-Bedford-Navilleton silt loams, 2 to 6 percent slopesCtwB941218523466r9in04320001:12000
Bedford silt loam, 2 to 6 percent slopesBdoB1565611519242s2cyin06120071:12000
Bedford silt loam, 0 to 2 percent slopesBdoA186811519232wh4fin06120071:12000
Crider-Bedford-Navilleton silt loams, 2 to 6 percent slopesCtwB172615858361q760in06120071:12000
Bedford silt loam, 2 to 6 percent slopesBdoB3001190675022042in07119851:15840
Bedford silt loam, 2 to 6 percent slopesBdoB1593416515162s2cyin09319821:15840
Bedford-Stoy silt loams, 1 to 4 percent slopes complexBdyB145816515291sfk4in09319821:15840
Bedford silt loam, 2 to 6 percent slopesBdB78615355172s2cyin10519791:15840
Bedford silt loam, 6 to 12 percent slopes, erodedBeC22131631955gtcin10919791:15840
Bedford silt loam, 2 to 6 percent slopesBeB1781631942s2cyin10919791:15840
Bedford silt loam, 2 to 6 percent slopesBdoB673614429682s2cyin11719801:15840
Bedford silt loam, 0 to 2 percent slopesBdoA384814429672wh4fin11719801:15840
Bedford silt loam, 2 to 6 percent slopesBdoB291655915k9nin14319951:12000
Bedford silt loam, 2 to 6 percent slopesBdB371525354562s2cyin17519841:15840
Bedford silt loam, 0 to 2 percent slopesBdA43165354552wh4fin17519841:15840
Bedford silt loam, 6 to 12 percent slopes, erodedBdC23311535457kz5tin17519841:15840
Bedford silt loam, 2 to 6 percent slopesBeB21870548751lf0nky00319861:20000
Bedford silt loam, 2 to 6 percent slopesBrB321315330792s2cyky11120051:12000
Bedford silt loam, 6 to 12 percent slopesBrC56230370772wh4hky11120051:12000
Bedford silt loam, 0 to 2 percent slopesBrA25615330782wh4fky11120051:12000
Bedford silt loam, 2 to 6 percent slopesBrB5595523582s2cyky15519861:20000
Bedford silt loam, 2 to 6 percent slopesBeB5980549889lg6cky17119771:20000
Bedford silt loam, 6 to 12 percent slopesBeC2460549890lg6dky17119771:20000
Bedford silt loam, 2 to 6 percent slopesBrB59855499352s2cyky17919671:15840
Bedford silt loam, 6 to 12 percent slopes, erodedBrC211645499362wh5dky17919671:15840
Bedford silt loam, 0 to 2 percent slopesBrA4325499342wh4fky17919671:15840
Bedford silt loam, 2 to 6 percent slopesBrB480330371272s2cyky18519751:20000
Bedford silt loam, 6 to 12 percent slopesBrC77530370782wh4hky18519751:20000
Bedford silt loam, 2 to 6 percent slopesBeB18795552382ljssky19919691:12000
Bedford silt loam, 0 to 2 percent slopesBeA412552381ljsrky19919691:12000
Bedford silt loam, 2 to 6 percent slopes, erodedBrB226525496042wh5cky60719921:20000
Bedford silt loam, 6 to 12 percent slopes, erodedBrC211475496052wh5dky60719921:20000
Bedford soils, 4 to 12 percent slopes, very severely erodedBrC43725496062wh5fky60719921:20000
Bedford silt loam, 2 to 6 percent slopesBrB26935510062s2cyky60819831:20000
Bedford silt loam, 6 to 12 percent slopesBrC79230370792wh4hky60819831:20000
Bedford silt loam, 0 to 2 percent slopesBrA1905510052wh4fky60819831:20000
Bedford silt loam, 2 to 6 percent slopesBrB248105510552s2cyky62119751:20000
Bedford silt loam, 0 to 2 percent slopesBrA41005510542wh4fky62119751:20000
Bedford silt loam, 2 to 6 percent slopesBdB1487552246ljndky62819731:20000
Bedford silt loam, 2 to 5 percent slopesBnB1406527971kqdbtn12519721:15840

Map of Series Extent

Approximate geographic distribution of the BEDFORD 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 .