Official Series Description


Lab Data Summary

Aggregate lab data for the BETHERA soil series. This aggregation is based on all pedons with a current taxon name of BETHERA, 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 BETHERA 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
133AS32_0341975-FL063-S32_034Bethera3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.9105587,-85.0035629

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BETHERA 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 BETHERA 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 BETHERA 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 BETHERA 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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Click the image to view it full size.

Competing Series

Soil series competing with BETHERA 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 BETHERA series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the BETHERA 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.

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

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

Soil series sharing subgroup-level classification with BETHERA, 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. NC-2012-02-07-32 | Northampton County - August 1994

    Typical relationship of soils and landscape in the Craven-Bethera-Lenoir, Wickham-Altavista, and Wehadkee-Congaree general soil map units (Soil Survey of Northampton County, North Carolina; August 1994).

Map Units

Map units containing BETHERA 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
Rains-Bethera complex, 0 to 1 percent slopes, occasionally floodedRbA326203284742tl18al01319961:20000
Izagora, rarely flooded-Bethera, occasionally flooded association, 0 to 3 percent slopesIbA21320328731c127al03519851:20000
Rains-Bethera complex, 0 to 2 percent slopes, frequently floodedRbA8293328779c13sal03919851:20000
Rains-Bethera complex, 0 to 1 percent slopes, occasionally floodedRbA25803305192tl18al04120051:24000
Bethera clay loam, 0 to 1 percent slopes, frequently floodedBeA2196330447c2vlal08719971:24000
Smithton, Daleville and Bethera soils, occasionally ponded, 0 to 2 percent slopesSDA232529950762x5rfal09720181:24000
Smithton, Daleville and Bethera soils, occasionally ponded, 0 to 2 percent slopesSNA2453726421322x5rfal12920131:24000
Bethera silt loam4417014249441jtryfl06319771:20000
Coxville (Bethera) loamCv1525125128466dga60119691:20000
Wahee-Bethera association, 0 to 2 percent slopes, occasionally floodedWB11028325411bxm4ga61019921:20000
Bethera loamBe16911156313wb1nc04719861:24000
Bethera loam, 0 to 1 percent slopesBaA42051130223slwnc08319951:24000
Bethera loamBa256101111183qmgnc11719851:24000
Bethera silt loam, 0 to 1 percent slopesBe308001140263tn8nc13119881:24000
Bethera clay loamBb23901317354f2jsc61519811:20000
Bethera silt loam, 0 to 2 percent slopes3A8611178933yp0va03619931:24000
Bethera and Daleville soils3123811964740hlva11919821:15840
Bethera silt loam5336212083441qwva69519811:15840
Bethera-Urban land complex, 0 to 2 percent slopes5199912245843f8va71519951:12000

Map of Series Extent

Approximate geographic distribution of the BETHERA 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 .