Official Series Description


Lab Data Summary

Aggregate lab data for the BATH soil series. This aggregation is based on all pedons with a current taxon name of BATH, 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 BATH 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
14068PA0150111968PA015011Bath5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.7825,-76.305
14068PA0150121968PA015012Bath5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.9552778,-76.5358333
14071PA0890791971PA089079Bath4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.0141667,-75.2475
14088PA0790061988PA079006Bath4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3569444,-76.255
14089PA0150991989PA015099Bath4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.9469444,-76.4955556
14040A0279S1954NY107004Bath4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.1483345,-76.2627792

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BATH 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 BATH 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 BATH 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 BATH 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 flats position figure.

Competing Series

Soil series competing with BATH 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 BATH 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 BATH 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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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with BATH, 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-2010-09-28-09 | Delaware County - 2006

    Typical pattern of soils and geologic materials in the Mardin-Bath-Volusia general soil map unit (Soil Survey of Delaware County, New York; 2006).

  2. NY-2010-09-28-14 | Otsego County - 2006

    Relationships between landscape and parent material for selected soils in Otsego County (Soil Survey of Otsego County, New York; 2006).

  3. NY-2010-09-28-16 | Otsego County - 2006

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

  4. NY-2010-09-28-23 | Otsego County - 2006

    The relationship between the soils and underlying material in the Otego-Chenango-Scio general soil map unit and the Mardin-Lordstown-Bath general soil map unit (Soil Survey of Otsego County, New York; 2006).

  5. NY-2012-02-15-48 | Tompkins County - July 1965

    Typical cross section of southern Tompkins County soils, consisting mainly of low-lime and very low-lime soils with a fragipan (Soil Survey of Tompkins County, New York; July 1965).

  6. NY-2012-02-16-02 | Wyoming County - April 1974

    Typical pattern of soils in association 5 (Soil Survey of Wyoming County, New York; April 1974).

  7. NY-2012-02-16-04 | Wyoming County - April 1974

    Typical pattern of soils in association 10 (Soil Survey of Wyoming County, New York; April 1974).

  8. NY-2012-02-16-07 | Wyoming County - April 1974

    Typical pattern of soils in association 16 (Soil Survey of Wyoming County, New York; April 1974).

  9. NY-2012-02-16-08 | Wyoming County - April 1974

    Typical pattern of soils in association 18 (Soil Survey of Wyoming County, New York; April 1974).

  10. PA-2012-03-13-44 | Lackawanna and Wyoming Counties - March 1982

    Typical pattern of soils and underlying material in the Mardin-Lordstown-Volusia association (Soil Survey of Lackawanna and Wyoming Counties, PA; 1982).

  11. PA-2012-03-13-46 | Lackawanna and Wyoming Counties - March 1982

    Typical pattern of soils and underlying material in the Mardin-Bath-Volusia association (Soil Survey of Lackawanna and Wyoming Counties, PA; 1982).

  12. PA-2012-03-13-67 | Monroe County - August 1981

    Typical pattern of soils and underlying material in the Lordstown-Oquaga map unit (Soil Survey of Monroe County, PA; 1981).

  13. PA-2012-03-13-68 | Monroe County - August 1981

    Typical pattern of soils and underlying material in the Mardin-Bath-Volusia map unit (Soil Survey of Monroe County, PA; 1981).

Map Units

Map units containing BATH 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
Bath channery silt loam, 25 to 35 percent slopes134E7472997702v319ny00320131:24000
Bath channery silt loam, 15 to 25 percent slopes134D4672997692v316ny00320131:24000
Bath channery silt loam, 8 to 15 percent slopes134C1462997682v314ny00320131:24000
Bath channery silt loam, 15 to 25 percent slopesMhD275992891942v316ny00719661:15840
Bath channery silt loam, 25 to 35 percent slopesMhE95112891952v319ny00719661:15840
Bath and Lackawanna soils, 35 to 65 percent slopesMrF20352891992v31hny00719661:15840
Bath-Valois complex, hillyBvD121272899742v32bny01719821:15840
Bath channery silt loam, 15 to 25 percent slopesBaD54332899712v316ny01719821:15840
Bath channery silt loam, 8 to 15 percent slopesBaC46232899702v314ny01719821:15840
Bath-Valois complex, rollingBvC40182899732v328ny01719821:15840
Bath channery silt loam, 3 to 8 percent slopesBaB33112899692v30xny01719821:15840
Bath-Valois complex, undulatingBvB21742899722v325ny01719821:15840
Bath and Mardin soils, 25 to 40 percent slopes133E398427230422srhsny02320141:12000
Bath-Valois complex, 3 to 8 percent slopes53B266027608382v312ny02320141:12000
Bath channery silt loam, 15 to 25 percent slopes134D244527230452v316ny02320141:12000
Bath channery silt loam, 8 to 15 percent slopes134C201427230442v314ny02320141:12000
Bath channery silt loam, 3 to 8 percent slopes134B171327230432v30xny02320141:12000
Lackawanna and Bath soils, 15 to 35 percent slopes, very stonyLdE519912904922v31mny02519991:24000
Lackawanna and Bath soils, 35 to 55 percent slopes, very stonyLdF95072904932v31nny02519991:24000
Bath channery silt loam, 15 to 25 percent slopesBtD62712904622v316ny02519991:24000
Lackawanna and Bath soils, 3 to 15 percent slopes, very stonyLdC36422904912v31lny02519991:24000
Bath channery silt loam, 8 to 15 percent slopesBtC16382904612v314ny02519991:24000
Bath channery silt loam, 25 to 35 percent slopesBtE13282904632v319ny02519991:24000
Bath channery silt loam, 3 to 8 percent slopesBtB1232904602v30xny02519991:24000
Bath channery silt loam, 15 to 25 percent slopesBaD74832925262v316ny05319751:15840
Bath channery silt loam, 8 to 15 percent slopesBaC73112925252v314ny05319751:15840
Bath soils, steepBCE52002925272v31fny05319751:15840
Bath channery silt loam, 3 to 8 percent slopesBaB18812925242v30xny05319751:15840
Bath-Nassau channery silt loams, 3 to 8 percent slopesBnB158482939009vtnny07119761:15840
Bath-Nassau channery silt loams, 8 to 15 percent slopesBnC120942939019vtpny07119761:15840
Bath channery silt loam, 15 to 25 percent slopesBfD202972941792v316ny07719931:24000
Bath channery silt loam, 8 to 15 percent slopesBfC74632941782v314ny07719931:24000
Bath channery silt loam, 25 to 45 percent slopesBfE60592941802v31cny07719931:24000
Bath and Lackawanna soils, 15 to 35 percent slopes, extremely stonyBhE29692941822v31sny07719931:24000
Bath channery silt loam, 3 to 8 percent slopesBfB22942941772v30xny07719931:24000
Bath and Lackawanna soils, 8 to 15 percent slopes, extremely stonyBhC5652941812v31rny07719931:24000
Bath and Lackawanna soils, 35 to 65 percent slopesMdF22652945082v31hny09519651:15840
Bath channery silt loam, 25 to 35 percent slopesMcE20912945072v319ny09519651:15840
Bath channery silt loam, 15 to 25 percent slopesBaD27602945852v316ny09719761:15840
Bath soils, steepBHE20722945862v31fny09719761:15840
Bath channery silt loam, 8 to 15 percent slopesBaC9762945842v314ny09719761:15840
Bath channery silt loam, 3 to 8 percent slopesBaB3912945832v30xny09719761:15840
Bath soils, steepBBE119752947892v31gny10119721:15840
Bath channery silt loam, 3 to 12 percent slopesBaB99372947862v311ny10119721:15840
Bath channery silt loam, 12 to 20 percent slopesBaC78432947872v315ny10119721:15840
Bath channery silt loam, 20 to 30 percent slopesBaD60022947882v318ny10119721:15840
Bath channery silt loam, 15 to 25 percent slopesBcm7782958002v316ny10719471:31680
Bath channery silt loam, 5 to 15 percent slopesBcs6642958012v313ny10719471:31680
Bath and Valois soils, 5 to 15 percent slopesBgC250012955822v32cny10919631:20000
Bath and Valois soils, 15 to 25 percent slopes, erodedBgD60632955842v32dny10919631:20000
Bath and Valois soils, 25 to 35 percent slopesBoE54902955852v32hny10919631:20000
Bath channery silt loam, 5 to 15 percent slopesBaC48842955792v313ny10919631:20000
Bath channery silt loam, 15 to 25 percent slopesBaD44682955812v316ny10919631:20000
Bath, Valois, and Lansing soils, 35 to 60 percent slopesBtF23092955862v32jny10919631:20000
Bath and Valois soils, 5 to 15 percent slopes, erodedBgC34372955832v32fny10919631:20000
Bath channery silt loam, 2 to 5 percent slopesBaB1132955782v30zny10919631:20000
Bath channery silt loam, 5 to 15 percent slopes, erodedBaC3952955802v32gny10919631:20000
Bath-Nassau-Rock outcrop complex, hillyBOD288882954569xfvny11119741:15840
Bath-Nassau complex, 8 to 25 percent slopesBnC231332954559xftny11119741:15840
Nassau-Bath-Rock outcrop complex, very steepNBF165322955079xhhny11119741:15840
Bath and Mardin soils, sloping, very stonyBRC66982954572v30nny11119741:15840
Bath gravelly silt loam, 8 to 15 percent slopesBgC43432954529xfqny11119741:15840
Bath very stony soils, steepBHE11812954549xfsny11119741:15840
Bath gravelly silt loam, 15 to 25 percent slopesBgD10962954539xfrny11119741:15840
Bath-Valois complex, 3 to 8 percent slopesBlB122112953072v322ny12119691:20000
Bath-Valois complex, 8 to 15 percent slopesBlC111222953082v323ny12119691:20000
Bath channery silt loam, 3 to 8 percent slopesBaB91672953022v30xny12119691:20000
Bath channery silt loam, 8 to 15 percent slopesBaC36062953032v314ny12119691:20000
Bath-Valois complex, 15 to 25 percent slopesBlD27842953092v324ny12119691:20000
Bath channery silt loam, 25 to 40 percent slopesBaE19582953052v31bny12119691:20000
Bath channery silt loam, 15 to 25 percent slopesBaD17912953042v316ny12119691:20000
Bath-Valois complex, 0 to 3 percent slopesBlA13562953062v321ny12119691:20000
Bath channery silt loam, 0 to 3 percent slopesBaA7442953012v30vny12119691:20000
Wooster very stony silt loam, 12 to 35 percent slopesWpD558539584l3gypa03719651:20000
Bath channery silt loam, 3 to 8 percent slopesBaB13413836042v30xpa03719651:20000
Bath channery silt loam, 8 to 15 percent slopesBaC1113836062v314pa03719651:20000
Bath channery silt loam, 8 to 25 percent slopes, extremely stonyBbD513836082v31vpa03719651:20000
Bath channery silt loam, 15 to 25 percent slopesBaD413836072v316pa03719651:20000
Bath channery silt loam, 8 to 25 percent slopes, rubblyBbD42242992832v31zpa06919761:20000
Bath channery silt loam, 3 to 8 percent slopes, rubblyBbB30072992822v31ypa06919761:20000
Lackawanna and Bath soils, steep, rubblyLCE29042992972v320pa06919761:20000
Bath channery silt loam, 8 to 15 percent slopesBaC5442992802v314pa06919761:20000
Bath channery silt loam, 3 to 8 percent slopesBaB5382992792v30xpa06919761:20000
Bath channery silt loam, 15 to 25 percent slopesBaD4702992812v316pa06919761:20000
Lackawanna and Bath soils, steep, extremely stonyLEF35422964392v31tpa07919741:20000
Bath channery silt loam, 3 to 8 percent slopesBkB10712964112v30xpa07919741:20000
Bath channery silt loam, 8 to 15 percent slopesBkC10232964122v314pa07919741:20000
Bath channery silt loam, 8 to 25 percent slopes, extremely stonyBnD9742964152v31vpa07919741:20000
Bath channery silt loam, 15 to 25 percent slopesBkD7322964132v316pa07919741:20000
Bath channery silt loam, 3 to 8 percent slopes, extremely stonyBnB4282964142v31ppa07919741:20000
Lackawanna and Bath soils, steep, rubblyLBE26562963112v320pa08919751:20000
Bath channery silt loam, 8 to 15 percent slopesBaC17502962732v314pa08919751:20000
Bath channery silt loam, 3 to 8 percent slopesBaB15642962722v30xpa08919751:20000
Bath channery silt loam, 8 to 25 percent slopes, extremely stonyBbC9192962762v31vpa08919751:20000
Bath channery silt loam, 0 to 8 percent slopes, extremely stonyBbB5132962752v31kpa08919751:20000
Bath channery silt loam, 15 to 25 percent slopesBaD2842962742v316pa08919751:20000
Bath channery silt loam, 15 to 25 percent slopesBhD13618827112v316pa10519531:24000
Bath channery silt loam, 8 to 15 percent slopesBhC3324324912v314pa10519531:24000
Bath channery silt loam, 3 to 8 percent slopesBhB1824338982v30xpa10519531:24000
Lordstown, Oquaga, and Bath soils, 3 to 12 percent slopesLoC1875031057902ywljpa11519681:20000
Lordstown, Oquaga, and Bath soils, 12 to 25 percent slopesLoD1445931057912ywlkpa11519681:20000
Bath very stony loam, 12 to 30 percent slopesBsD64162970289z2kpa11519681:20000
Bath very stony loam, 30 to 60 percent slopesBsF46962970299z2lpa11519681:20000
Bath flaggy loam, 20 to 30 percent slopes, moderately erodedBfD221972970269z2hpa11519681:20000
Bath channery loam, 12 to 20 percent slopes, moderately erodedBeC216122970239z2dpa11519681:20000
Bath flaggy loam, 12 to 20 percent slopes, moderately erodedBfC214762970259z2gpa11519681:20000
Bath channery loam, 3 to 12 percent slopes, moderately erodedBeB211392970229z2cpa11519681:20000
Bath very stony loam, 0 to 12 percent slopesBsB10902970279z2jpa11519681:20000
Bath flaggy loam, 3 to 12 percent slopes, moderately erodedBfB24772970249z2fpa11519681:20000
Bath channery silt loam, 3 to 12 percent slopes, extremely stonyBsB146702971012v31qpa11719731:20000
Bath channery silt loam, 3 to 12 percent slopesBaB14642971002v311pa11719731:20000
Lackawanna and Bath soils, steep, rubblyLCE155383019262v320pa13119761:20000
Bath channery silt loam, 8 to 25 percent slopes, rubblyBbD38403019112v31zpa13119761:20000
Bath channery silt loam, 15 to 25 percent slopesBaD23683019092v316pa13119761:20000
Bath channery silt loam, 8 to 15 percent slopesBaC20033019082v314pa13119761:20000
Bath channery silt loam, 3 to 8 percent slopesBaB9553019072v30xpa13119761:20000
Bath channery silt loam, 3 to 8 percent slopes, rubblyBbB5293019102v31ypa13119761:20000

Map of Series Extent

Approximate geographic distribution of the BATH 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 .