Official Series Description


Lab Data Summary

Aggregate lab data for the BETHANY soil series. This aggregation is based on all pedons with a current taxon name of BETHANY, 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 BETHANY were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
7940A1775S1958KS155003BETHANY7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8722229,-97.8402786
7940A1776S1958KS155004BETHANY7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.9088898,-97.8838882
80A68-OK-60-368-OK119-60-3Bethany4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.1208139,-97.0939528
80A81P017780OK017001Bethany7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.5552788,-98.0500031
80A90P095090OK103005Bethany8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.5558319,-97.2136078
80A40A4693S1956OK109002Bethany7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.3944435,-97.6355591
80A91P0907S1995OK109005Bethany7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.6941681,-97.6208344

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the BETHANY series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the BETHANY series and siblings. 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 BETHANY 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 .

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.

Competing Series

Soil series competing with BETHANY share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the BETHANY 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 BETHANY 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.

Click the image to view it full size.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with BETHANY, 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-2012-01-25-14 | Pratt County - September 1968

    Major soils of association 7 and the positions they normally occupy on the landscape (Soil Survey of Pratt County, Kansas; 1968).

  2. KS-2012-01-25-16 | Reno County - March 1966

    Cross section of the Renfrow-Vernon association downslope from the Clark-Ost association (Soil Survey of Reno County, Kansas; 1966).

  3. KS-2012-01-25-18 | Reno County - March 1966

    Cross section of the Clark-Ost association showing the topographic relationship of the Clark and Ost soils to the soils of the Renfrow-Vernon association (Soil Survey of Reno County, Kansas; 1966).

  4. OK-2010-09-29-12 | Noble County - 2005

    Typical pattern of soils and underlying material in the Norge-Bethany-Kirkland general soil map unit (Soil Survey of Noble County, Oklahoma; 2005).

  5. OK-2010-09-29-13 | Noble County - 2005

    Typical pattern of soils and underlying material in the Milan-Norge-Bethany general soil map unit (Soil Survey of Noble County, Oklahoma; 2005).

  6. OK-2012-02-16-34 | Garfield County - October 1967

    Typical pattern of soils in the Kirkland-Bethany-Tabler association (Soil Survey of Garfield County, Oklahoma; October 1967).

  7. OK-2012-02-16-53 | Kay County - December 1967

    Relationship of the soils in the level to very gently sloping areas of soil association 3 (Soil Survey of Kay County, Oklahoma; December 1967).

  8. OK-2012-02-17-05 | Logan County - June 1960

    Soils of central and western Logan County on recent alluvium and on loams and sands of Quaternary age. Red beds are exposed in the upper right corner (Soil Survey of Logan County, Oklahoma; June 1960).

  9. OK-2012-02-17-15 | Oklahoma County - February 1969

    Typical pattern of soils in soil association 2 (Soil Survey of Oklahoma County, Oklahoma; February 1969).

  10. OK-2012-02-17-30 | Payne County - April 1987

    Typical pattern of soils and underlying material in the Norge-Teller-Konawa map unit (Soil Survey of Payne County, Oklahoma; April 1987).

  11. OK-2012-02-17-50 | Stephens County - 1964

    Typical pattern of soils in association 4 (Soil Survey of Stephens County, Oklahoma; 1964).

Map Units

Map units containing BETHANY 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
Bethany silt loam, 1 to 3 percent slopes63211175913829231hf1fks03519771:24000
Bethany silt loam, 0 to 1 percent slopes6320792413829221hf1dks03519771:24000
Bethany silt loam, 0 to 1 percent slopes6320919313826692tp52ks07719651:24000
Bethany silt loam, 1 to 3 percent slopes6321171213826702tp48ks07719651:24000
Bethany silt loam, 0 to 1 percent slopes6320193614440091kglyks17319761:24000
Bethany silt loam, 1 to 3 percent slopes6321167414440101kglzks17319761:24000
Bethany silt loam, 0 to 1 percent slopes632011007114446462tp52ks19119741:24000
Bethany silt loam, 1 to 3 percent slopes63218186314446472tp48ks19119741:24000
Bethany silt loam, 0 to 1 percent slopesBeA194133817122tp52ok01119651:24000
Bethany silt loam, 0 to 1 percent slopesBeA407873819312tp52ok01719721:24000
Bethany silt loam, 0 to 1 percent slopes6029873821232tp52ok02719841:24000
Bethany silt loam, 1 to 3 percent slopes6116153821242tp48ok02719841:24000
Bethany-Pawhuska complex, 0 to 3 percent slopes529213821152tp53ok02719841:24000
Bethany-Urban land complex, 0 to 3 percent slopes597543821212tp54ok02719841:24000
Bethany silt loam, 0 to 1 percent slopesBeA208023824832tp52ok04719651:24000
Bethany silt loam, 1 to 3 percent slopes780433826052tp48ok04919821:24000
Bethany silt loam, 0 to 1 percent slopes622553825942tp52ok04919821:24000
Bethany silt loam, 0 to 1 percent slopes293873826382tp52ok05119751:24000
Bethany silt loam, 0 to 1 percent slopes4291813827292tp52ok05319831:24000
Bethany silt loam, 0 to 1 percent slopesBeA240613833182tp52ok07119651:24000
Bethany silt loam, 1 to 3 percent slopesBetB5426234732tp48ok07119651:24000
Bethany silt loam, 0 to 1 percent slopesBeA261143833852tp52ok07319601:24000
Bethany silt loam, 0 to 1 percent slopesBetA2493835932tp52ok08319941:12000
Bethany silt loam, 1 to 3 percent slopesBetB1353835942tp48ok08319941:12000
Bethany silt loam, 0 to 1 percent slopes335643837862tp52ok08719761:24000
Bethany silt loam, 1 to 3 percent slopes428513837972tp48ok08719761:24000
Bethany-Pawhuska complex, 0 to 3 percent slopes514253838062tp53ok08719761:24000
Bethany silt loam, 1 to 3 percent slopesBetB211463840372tp48ok10319941:24000
Bethany silt loam, 0 to 1 percent slopesBetA83493840362tp52ok10319941:24000
Bethany-Urban land complex, 0 to 3 percent slopesBeUB48513842722tp54ok10919961:12000
Bethany silt loam, 0 to 1 percent slopesBetA15733842732tp52ok10919961:12000
Bethany silt loam, 1 to 3 percent slopesBetB12643842742tp48ok10919961:12000
Bethany-Pawhuska complex, 1 to 5 percent slopes12248546234072yhdjok11319751:24000
Bethany silt loam, 3 to 5 percent slopes1144216234062yhdhok11319751:24000
Bethany silt loam, 1 to 3 percent slopes1017886234052tp48ok11319751:24000
Bethany silt loam, 1 to 3 percent slopesBetB117214231482tp48ok11720071:24000
Bethany silt loam, 0 to 1 percent slopesBetA46314231472tp52ok11720071:24000
Bethany silt loam, 1 to 3 percent slopes514223845482tp48ok11919831:24000
Bethany silt loam, 0 to 1 percent slopesBetA89653851582tp52ok15119951:24000
Bethany silty clay loam, 1 to 3 percent slopes, erodedBthB2725385159dxshok15119951:24000

Map of Series Extent

Approximate geographic distribution of the BETHANY 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 .