Official Series Description


Lab Data Summary

Aggregate lab data for the LEWBEACH soil series. This aggregation is based on all pedons with a current taxon name of LEWBEACH, 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 LEWBEACH 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
14087P021986NY025010Lewbeach4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.292778,-74.6500015
14087P020086NY025011Lewbeach4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.4124985,-74.6100006
14093P0630S1993NY025005Lewbeach7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.2335014,-74.7647247
14011N0146S2010NY003002Lewbeach6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0144,-77.7855

Water Balance

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

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 LEWBEACH, 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-2010-09-28-08 | Delaware County - 2006

    The landscape pattern of upland soils developed in coarse loamy glacial till and ground water flow patterns (arrow shows general flow direction) (Soil Survey of Delaware County, New York; 2006).

  2. NY-2010-09-28-11 | Delaware County - 2006

    Typical pattern of soils and geologic materials in the Willowemoc-Lewbeach-Onteora and the Vly-Halcott-Mongaup general soil map units (Soil Survey of Delaware County, New York; 2006).

  3. NY-2010-09-28-18 | Otsego County - 2006

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

  4. NY-2012-02-15-25 | Greene County - February 1993

    Typical pattern of soils and underlying material in the Lewbeach-Willowemoc-Onteora association (Soil Survey of Greene County, New York; February 1993).

  5. NY-2012-02-15-45 | Sullivan County - July 1989

    Typical landscape pattern of the soils and the underlying material in the Willowemoc-Mongaup-Lewbeach general soil map unit (Soil Survey of Sullivan County, New York; July 1989).

Map Units

Map units containing LEWBEACH 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
Lewbeach channery silt loam, 25 to 35 percent slopes114E16542997192w0c9ny00320131:24000
Lewbeach channery silt loam, 15 to 25 percent slopes114D13572997182w0c8ny00320131:24000
Lewbeach channery silt loam, 8 to 15 percent slopes114C2982997172w0c7ny00320131:24000
Lewbeach channery silt loam, 3 to 8 percent slopes114B12997162w0c6ny00320131:24000
Lewbeach and Lewbath soils, 15 to 35 percent slopes, very stonyLkE424982905042w0cfny02519991:24000
Lewbeach channery loam, 15 to 25 percent slopesLhD213422905012w0c4ny02519991:24000
Lewbeach channery loam, 8 to 15 percent slopesLhC153342905002w0c3ny02519991:24000
Lewbeach and Lewbath soils, 3 to 15 percent slopes, very stonyLkC63722905032w0cdny02519991:24000
Lewbeach channery loam, 3 to 8 percent slopesLhB33872904992w0c2ny02519991:24000
Lewbeach channery loam, 25 to 40 percent slopesLhE32672905022w0c5ny02519991:24000
Lewbeach and Lewbath soils, 35 to 55 percent slopes, very stonyLkF20302905052w0cgny02519991:24000
Lewbeach and Willowemoc channery silt loams, moderately steep, very boulderyLmD236902916622w0ckny03919851:24000
Lewbeach and Willowemoc channery silt loams, strongly sloping, very boulderyLmC134402916612w0clny03919851:24000
Lewbeach and Willowemoc channery silt loams, 3 to 15 percent slopes, very stonyLlC79272916592w0chny03919851:24000
Lewbeach and Willowemoc channery silt loams, 15 to 35 percent slopes, very stonyLlD61572916602w0cjny03919851:24000
Lewbeach channery silt loam, 8 to 15 percent slopesLeC32032916542w0c7ny03919851:24000
Lewbeach channery silt loam, 15 to 25 percent slopesLeD18692916552w0c8ny03919851:24000
Lewbeach channery silt loam, very steep, very boulderyLgF14432916582w0ccny03919851:24000
Lewbeach channery silt loam, 3 to 8 percent slopesLeB10472916532w0c6ny03919851:24000
Lewbeach channery silt loam, 35 to 55 percent slopes, very stonyLfF3492916572w0cbny03919851:24000
Lewbeach channery silt loam, 25 to 35 percent slopesLeE2052916562w0c9ny03919851:24000
Lewbeach channery silt loam, 8 to 15 percent slopesLhC4792942362w0c7ny07719931:24000
Lewbeach silt loam, steep, very stonyLfE62882950809x1qny10519841:15840
Lewbeach silt loam, 8 to 15 percent slopesLeC33622950789x1nny10519841:15840
Lewbeach silt loam, 15 to 25 percent slopesLeD20232950799x1pny10519841:15840
Lewbeach silt loam, 3 to 8 percent slopesLeB18172950779x1mny10519841:15840
Lewbeach silt loam, very steep, very stonyLfF5132950819x1rny10519841:15840
Lewbeach channery silt loam, 15 to 25 percent slopesLhD354724330342w0c8pa10519531:24000
Lewbeach channery silt loam, 3 to 8 percent slopesLhB223624330352w0c6pa10519531:24000
Lewbeach channery silt loam, 8 to 15 percent slopesLhC130024330192w0c7pa10519531:24000
Lewbeach channery silt loam, 25 to 35 percent slopesLhE85929940442w0c9pa10519531:24000
Lewbeach channery silt loam, 8 to 25 percent slopes, extremely stonyLhsD38024401772wbpdpa10519531:24000

Map of Series Extent

Approximate geographic distribution of the LEWBEACH 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 .