Official Series Description


Lab Data Summary

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

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LEWBATH 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 LEWBATH 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 LEWBATH 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 LEWBATH 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 terrace figure.

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

Competing Series

Soil series competing with LEWBATH 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 LEWBATH 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 LEWBATH 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 the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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 LEWBATH, 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. NY-2010-09-28-15 | Otsego County - 2006

    Ground water flow pattern and typical landscape pattern of upland soils that formed in glacial till. The arrow shows the general direction of flow (Soil Survey of Otsego County, New York; 2006).

  2. NY-2010-09-28-17 | Otsego County - 2006

    Typical pattern of soils and underlying material in the Mongaup-Willdin-Lewbath general soil map unit (Soil Survey of Otsego County, New York; 2006).

Map Units

Map units containing LEWBATH 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
Lewbath channery silt loam, 25 to 35 percent slopes124E21892997482wbm0ny00320131:24000
Lewbath channery silt loam, 3 to 8 percent slopes124B8212997452wblxny00320131:24000
Lewbath channery silt loam, 8 to 15 percent slopes124C7312997462wblyny00320131:24000
Lewbath channery silt loam, 15 to 25 percent slopes124D6782997472wblzny00320131:24000
Lewbath channery silt loam, 15 to 25 percent slopes124D123327608392wblzny02320141:12000
Lewbath channery silt loam, 3 to 8 percent slopes124B116527230742wblxny02320141:12000
Lewbath channery silt loam, 8 to 15 percent slopes124C93927230752wblyny02320141:12000
Lewbeach and Lewbath soils, 15 to 35 percent slopes, very stonyLkE424982905042w0cfny02519991:24000
Lewbeach and Lewbath soils, 3 to 15 percent slopes, very stonyLkC63722905032w0cdny02519991:24000
Lewbath flaggy loam, 15 to 25 percent slopesLeD26222904972wbm3ny02519991:24000
Lewbath flaggy loam, 8 to 15 percent slopesLeC25202904962wbm2ny02519991:24000
Lewbeach and Lewbath soils, 35 to 55 percent slopes, very stonyLkF20302905052w0cgny02519991:24000
Lewbath flaggy loam, 3 to 8 percent slopesLeB2622904952wbm1ny02519991:24000
Lewbath flaggy loam, 25 to 35 percent slopesLeE2092904982wbm4ny02519991:24000
Lewbath channery silt loam, 3 to 8 percent slopes51B363231056812wblxny05120191:24000
Lewbath channery silt loam, 8 to 15 percent slopes51C323331056822wblyny05120191:24000
Lewbath channery silt loam, 15 to 25 percent slopes51D195831056832wblzny05120191:24000
Lewbath-Ontusia complex, 3 to 15 percent slopes151C164731057432y9xjny05120191:24000
Lewbath-Willdin channery silt loams, 8 to 15 percent slopes152C118831057452y9xlny05120191:24000
Lewbath-Willdin channery silt loams, 3 to 8 percent slopes152B85631057442y9xkny05120191:24000
Lewbath channery silt loam, 15 to 25 percent slopesLfD54392942342wblzny07719931:24000
Lewbath channery silt loam, 8 to 15 percent slopesLfC44612942332wblyny07719931:24000
Lewbath channery silt loam, 3 to 8 percent slopesLfB13732942322wblxny07719931:24000
Lewbath channery silt loam, 25 to 35 percent slopesLfE8572942352wbm0ny07719931:24000
Lewbath channery silt loam, 3 to 8 percent slopesLfB234524329552wblxpa10519531:24000
Lewbath channery silt loam, 15 to 25 percent slopesLfD173724330262wblzpa10519531:24000
Lewbath channery silt loam, 8 to 15 percent slopesLfC86624329562wblypa10519531:24000

Map of Series Extent

Approximate geographic distribution of the LEWBATH 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 .