Official Series Description


Lab Data Summary

Aggregate lab data for the ARNOT soil series. This aggregation is based on all pedons with a current taxon name of ARNOT, 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 ARNOT 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
14068PA0150011968PA015001Arnot3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.6802778,-76.4841667
14068PA0150021968PA015002Arnot3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.6902778,-76.5894444
14085PA1030431985PA103043Arnot3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3086111,-75.2361111
14088PA1130031988PA113003Arnot2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3658333,-76.3958333

Water Balance

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

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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.

Soil series sharing subgroup-level classification with ARNOT, 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-2010-09-28-10 | Delaware County - 2006

    Typical pattern of soils and geologic materials in the Lackawanna-Wellsboro, Tunkhannock-Maplecrest-Barbour, and Oquaga-Lordstown-Arnot general soil map units (Soil Survey of Delaware County, New York; 2006).

  2. NY-2012-02-15-01 | Albany County - June 1992

    Typical pattern of soils and parent material in the Wellsboro-Lackawanna-Morris unit (Soil Survey of Albany County, New York; June 1992).

  3. NY-2012-02-15-02 | Albany County - June 1992

    Typical pattern of soils and parent material in the Lordstown-Kearsarge-Arnot unit (Soil Survey of Albany County, New York; June 1992).

  4. NY-2012-02-15-13 | Chenango County - December 1985

    Typical pattern of soils and underlying material in the Mardin-Lordstown-Volusia map unit (Soil Survey of Chenango County, New York; December 1985).

  5. NY-2012-02-15-23 | Greene County - February 1993

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

  6. NY-2012-02-15-43 | Seneca County - April 1972

    Cross section of Langford-Erie and Conesus-Lansing associations in southern part of Seneca County (Soil Survey of Seneca County, New York; April 1972).

  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. PA-2012-03-12-23 | Bradford and Sullivan Counties - August 1986

    Typical pattern of soils and parent material in the Morris-Oquaga-Wellsboro map unit (Soil Survey of Bradford and Sullivan Counties, PA; 1986).

  9. PA-2012-03-12-24 | Bradford and Sullivan Counties - August 1986

    Typical pattern of soils and parent material in the Wellsboro-Oquaga-Morris map unit (Soil Survey of Bradford and Sullivan Counties, PA; 1986).

  10. PA-2012-03-13-43 | Lackawanna and Wyoming Counties - March 1982

    Typical pattern of soils and underlying material in the Wellsboro-Morris-Oquaga association (Soil Survey of Lackawanna and Wyoming Counties, PA; 1982).

  11. 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).

  12. PA-2012-03-13-45 | Lackawanna and Wyoming Counties - March 1982

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

  13. 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).

  14. PA-2012-03-13-54 | Luzerne County - October 1981

    Typical pattern of soils and underlying material in association 1 (Soil Survey of Luzerne County, PA; 1981).

  15. PA-2012-03-14-32 | Wayne County - September 1985

    Typical pattern of soils and underlying material in the Oquaga-Wellsboro-Arnot association (Soil Survey of Wayne County, PA; 1985).

  16. PA-2012-03-14-34 | Wayne County - September 1985

    Typical pattern of soils and underlying material in the Lordstown-Mardin-Volusia association (Soil Survey of Wayne County, PA; 1985).

Map Units

Map units containing ARNOT 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
Arnot-Lordstown-Rock outcrop complex, 15 to 35 percent slopesArvD7440620180ntbtnj03720021:24000
Arnot-Lordstown-Rock outcrop complex, 35 to 60 percent slopesArvE4557620181ntbvnj03720021:24000
Arnot-Lordstown complex, 0 to 15 percent slopes, very rockyAruCh3490620179ntbsnj03720021:24000
Rock outcrop-Arnot-Rubble land complex, 60 to 80 percent slopesRnaF329624846nz6bnj03720021:24000
Arnot-Lordstown-Rock outcrop complex, 15 to 35 percent slopesArvD2341114746817j13nj04120071:12000
Arnot-Lordstown-Rock outcrop complex, 35 to 60 percent slopesArvE1765114746917j14nj04120071:12000
Arnot-Lordstown complex, 0 to 15 percent slopes, very rockyAruCh1180114746717j12nj04120071:12000
Rock outcrop-Arnot-Rubble land complex, 60 to 80 percent slopesRnaF1013740975sw1fnj04120071:12000
Arnot-Rock outcrop complex, 25 to 70 percent slopesAsF95702886942wbn3ny00119851:15840
Lordstown-Arnot complex, 25 to 45 percent slopes, very rockyLrE66022887529pglny00119851:15840
Arnot very channery silt loam, 8 to 15 percent slopesArC50672886922wbmlny00119851:15840
Arnot-Rock outcrop complex, 0 to 8 percent slopesAsB38472886932wbnfny00119851:15840
Rock outcrop-Arnot complex, 25 to 70 percent slopes18F3322998142wbnbny00320131:24000
Arnot channery silt loam, 0 to 25 percent slopesArD12272891652wbm5ny00719661:15840
Arnot channery silt loam, 25 to 45 percent slopesAvE5952893572wbmjny01119681:15840
Arnot channery silt loam, 3 to 15 percent slopesAuC4592893552wbmfny01119681:15840
Arnot channery silt loam, 15 to 25 percent slopesAuD3362893562wbmhny01119681:15840
Lordstown and Arnot soils, 25 to 35 percent slopes, very rockyLoE314342899332zxq1ny01519691:20000
Arnot channery silt loam, 2 to 8 percent slopesArB108522899082wbm9ny01519691:20000
Lordstown and Arnot very rocky soils, 35 to 70 percent slopesLoF80902899349qpqny01519691:20000
Arnot channery silt loam, 3 to 8 percent slopesAsB28952899662wbmcny01719821:15840
Arnot channery silt loam, 8 to 15 percent slopesAsC4152899672wbmgny01719821:15840
Lordstown-Arnot complex, 3 to 8 percent slopes179B526927230982ywl9ny02320141:12000
Oquaga, Lordstown, and Arnot soils, 35 to 70 percent slopes, very rockyOrF215462905422zxqvny02519991:24000
Oquaga, Lordstown, and Arnot soils, 15 to 35 percent slopes, very rockyOrE151122905412zxqtny02519991:24000
Oquaga, Lordstown, and Arnot soils, 2 to 15 percent slopes, very rockyOrC55712905409rb8ny02519991:24000
Arnot-Lordstown channery silt loams, 3 to 15 percent slopes, rockyAuC115622915989sfdny03919851:24000
Arnot-Lordstown channery silt loams, rolling, rockyAsC932929159530jxtny03919851:24000
Arnot channery silt loam, 3 to 8 percent slopesArB65892915932wbmcny03919851:24000
Arnot-Lordstown channery silt loams, 15 to 35 percent slopes, very rockyAvD54882915999sffny03919851:24000
Oquaga-Arnot complex, 3 to 15 percent slopes, very rockyOsC47072917022xp9jny03919851:24000
Arnot-Oquaga complex, rollingAwC44652916012xp95ny03919851:24000
Oquaga-Arnot complex, 15 to 35 percent slopes, very rockyOsD22952917032xp9kny03919851:24000
Arnot-Lordstown channery silt loams, 15 to 25 percent slopes, rockyAsD10622915962zxplny03919851:24000
Arnot-Lordstown channery silt loams, 35 to 55 percent slopes, very rockyAvF10242916009sfgny03919851:24000
Oquaga-Arnot complex, 35 to 55 percent slopes, very rockyOsF7002917042xp9lny03919851:24000
Arnot channery silt loam, 8 to 15 percent slopesArC6102915942wbmgny03919851:24000
Arnot-Oquaga complex, 15 to 25 percent slopesAwD5322916022xp96ny03919851:24000
Arnot-Lordstown channery silt loams, 25 to 45 percent slopes, rockyAsE201159034230jxrny03919851:24000
Arnot channery silt loam, 0 to 3 percent slopesArA1962915922wbm6ny03919851:24000
Arnot-Oquaga complex, 25 to 45 percent slopesAwE14815903432xp97ny03919851:24000
Rock outcrop-Arnot complex, 25 to 70 percent slopes83F501331002602wbnbny05120191:24000
Lordstown-Arnot complex, steep, rockyLXE617629259430jy0ny05319751:15840
Arnot channery silt loam, 3 to 8 percent slopesAsB24122925182wbmcny05319751:15840
Arnot-Lordstown complex, very steep, very rockyATF69029252030jy2ny05319751:15840
Arnot channery silt loam, 8 to 15 percent slopesAsC4102925192wbmgny05319751:15840
Arnot-Angola channery silt loams, 3 to 8 percent slopesAvB46322927889tnsny05719731:24000
Arnot channery silt loam, 8 to 15 percent slopes, rockyAtC27302927869tnqny05719731:24000
Arnot-Rock outcrop association, very steepAZF18182927899tntny05719731:24000
Arnot channery silt loam, 15 to 25 percent slopes, rockyAtD14932927879tnrny05719731:24000
Arnot channery silt loam, 0 to 8 percent slopesArB82927859tnpny05719731:24000
Arnot channery silt loam, 3 to 8 percent slopes355B4482934062wbmcny06519931:24000
Arnot-Lordstown association, very steep, very rockyAVF307829351330jy1ny06719731:20000
Lordstown-Arnot channery silt loams, moderately steep, rockyLXD173629358930jxyny06719731:20000
Arnot channery silt loam, gently slopingATB9992935122wbmdny06719731:20000
Rock outcrop-Arnot complex, 25 to 70 percent slopes13F434825049182wbnbny06920121:12000
Arnot-Lordstown complex, sloping, rockyANC900029389530jxvny07119761:15840
Arnot-Lordstown complex, steep, rockyAND541229389630jxwny07119761:15840
Rock outcrop-Arnot complex, 3 to 15 percent slopesRKC47622939612wbn6ny07119761:15840
Rock outcrop-Arnot complex, 15 to 25 percent slopesRKD38232939622wbn7ny07119761:15840
Rock outcrop-Arnot complex, 25 to 70 percent slopesRKF17842939632wbnbny07119761:15840
Arnot-Lordstown complex, very steep, very rockyANF131629389730jy2ny07119761:15840
Lordstown-Arnot complex, 1 to 8 percent slopes, rockyLoB134432942399w5lny07719931:24000
Oquaga-Arnot complex, 25 to 45 percent slopes, rockyOgE61902942682xp9hny07719931:24000
Oquaga-Arnot complex, 15 to 25 percent slopes, rockyOgD45922942672xp9gny07719931:24000
Oquaga-Arnot complex, 1 to 8 percent slopes, rockyOgB36422942652xp9dny07719931:24000
Oquaga-Arnot complex, 8 to 15 percent slopes, rockyOgC34402942662xp9fny07719931:24000
Arnot channery silt loam, 0 to 8 percent slopesArB4360309538bd33ny09319731:15840
Arnot-Rock outcrop association, very steepAZF2138309542bd37ny09319731:15840
Arnot flaggy silt loam, 0 to 15 percent slopesArC54812944502wbmkny09519651:15840
Lordstown-Arnot complex, steep, rockyLTE57142946312ywlbny09719761:15840
Lordstown-Arnot complex, very steep, very rockyLTF49512946322ywlcny09719761:15840
Rock outcrop-Arnot complex, 25 to 70 percent slopesROF10292946462wbnbny09719761:15840
Arnot channery silt loam, 3 to 8 percent slopesArB6782945772wbmcny09719761:15840
Arnot channery silt loam, 8 to 15 percent slopesArC5022945782wbmgny09719761:15840
Arnot channery silt loam, 15 to 25 percent slopesAuD1132946842wbmhny09919661:15840
Lordstown-Arnot complex, very steep, very rockyLRF664882948292ywlcny10119721:15840
Lordstown-Arnot complex, steep, rockyLRE384462948282ywlbny10119721:15840
Arnot channery silt loam, 2 to 20 percent slopesARC310572947842wbmbny10119721:15840
Arnot-Lordstown complex, 0 to 15 percent slopes, very rockyAlC213902950442zxpwny10519841:15840
Arnot-Oquaga complex, 0 to 15 percent slopes, very rockyAoC198132950462xp98ny10519841:15840
Arnot-Lordstown complex, 15 to 35 percent slopes, very rockyAlE170612950452zxpxny10519841:15840
Arnot-Oquaga complex, 15 to 35 percent slopes, very rockyAoE169552950472xp99ny10519841:15840
Arnot-Rock outcrop complex, 35 to 70 percent slopesArF125182950502wbn2ny10519841:15840
Oquaga-Arnot complex, 8 to 15 percent slopesOgC111452951022xp9bny10519841:15840
Oquaga-Arnot complex, 15 to 25 percent slopesOgD50562951032xp9cny10519841:15840
Arnot-Rock outcrop complex, 15 to 35 percent slopesArE50382950492wbn1ny10519841:15840
Arnot-Rock outcrop complex, 0 to 15 percent slopesArC40272950482wbmxny10519841:15840
Lordstown-Arnot complex, 8 to 15 percent slopes, very stonyLrC30792950839x1tny10519841:15840
Arnot-Rock outcrop complex, 25 to 70 percent slopesSsL8922958412wbn3ny10719471:31680
Arnot-Oquaga-Rock outcrop complex, very steepARF937702954472xp9pny11119741:15840
Oquaga-Arnot-Rock outcrop complex, moderately steepORD505452955162xp9nny11119741:15840
Lordstown-Arnot-Rock outcrop complex, slopingLOC451622954972zxq3ny11119741:15840
Rock outcrop-Arnot complex, 25 to 70 percent slopesRXF287242955352wbnbny11119741:15840
Arnot-Lordstown-Rock outcrop complex, moderately steepARD238542954462zxq4ny11119741:15840
Oquaga-Arnot-Rock outcrop complex, slopingORC236812955152xp9mny11119741:15840
Rock outcrop-Arnot complex, 15 to 25 percent slopesRXE102642955342wbn7ny11119741:15840
Rock outcrop-Arnot complex, 3 to 15 percent slopesRXC83572955332wbn6ny11119741:15840
Arnot channery silt loam, 0 to 8 percent slopesAcB43292954452wbm7ny11119741:15840
Arnot channery silt loam, 2 to 8 percent slopesAtB9122952982wbm9ny12119691:20000
Arnot channery silt loam, 8 to 15 percent slopesAtC3292952992wbmgny12119691:20000
Rock outcrop-Arnot complex, 25 to 70 percent slopes13F341314078912wbnbny12319481:12000
Arnot-Rock outcrop complex, 3 to 25 percent slopesASD3813836002wbmzpa03719651:20000
Arnot-Rock outcrop complex, 8 to 25 percent slopesAsD128832992762wbn0pa06919761:20000
Arnot-Rock outcrop complex, steepASE88482992772wbn4pa06919761:20000
Arnot very channery silt loam, 3 to 15 percent slopes, very rockyArC37092992742wbmmpa06919761:20000
Arnot-Rock outcrop complex, 0 to 8 percent slopesAsB35592992752wbmwpa06919761:20000
Rock outcrop-Arnot complex, 3 to 25 percent slopesRoD843199632wbn5pa06919761:20000
Arnot-Rock outcrop complex, steepASF165202964032wbn4pa07919741:20000
Arnot-Rock outcrop complex, 8 to 25 percent slopesArD115122964082wbn0pa07919741:20000
Arnot-Rock outcrop complex, 0 to 8 percent slopesArB57622964072wbmwpa07919741:20000
Arnot-Rock outcrop complex, 3 to 25 percent slopesASD514230862wbmzpa07919741:20000
Arnot-Rock outcrop complex, 3 to 25 percent slopesAsD4110194132wbmzpa08119811:20000
Oquaga-Arnot-Rock outcrop complex, 20 to 60 percent slopes240F1682963992xp9qpa08919751:20000
Arnot channery silt loam, 15 to 25 percent slopesAtD658194875123dtypa09520071:12000
Arnot channery silt loam, 8 to 15 percent slopesAtC628194875023dtxpa09520071:12000
Arnot channery silt loam, 3 to 8 percent slopesAtB332194874923dtwpa09520071:12000
Oquaga-Arnot-Rock outcrop complex, 20 to 60 percent slopes240F225722972022xp9qpa10319951:24000
Manlius-Arnot-Rock outcrop complex, 30 to 80 percent slopes121F76352971892xp94pa10319951:24000
Arnot very channery loam, 3 to 15 percent slopes, very rocky402C51212972272wbmspa10319951:24000
Manlius-Arnot-Rock outcrop complex, 15 to 30 percent slopes121D38792971882xp93pa10319951:24000
Arnot very channery loam, 15 to 35 percent slopes, very rocky402E32782972282wbmtpa10319951:24000
Arnot-Rock outcrop complex, steepASE393093512wbn4pa11519681:20000
Arnot-Rock outcrop complex, 8 to 25 percent slopesAsD272961292wbn0pa11519681:20000
Arnot channery loam, 3 to 12 percent slopesAoB20782970982wbmnpa11719731:20000
Arnot-Rock outcrop complex, 3 to 12 percent slopesArB8912970992wbmypa11719731:20000
Arnot channery loam, 15 to 25 percent slopes, very rockyArD125592965902wbmrpa12719771:20000
Arnot channery loam, 3 to 8 percent slopes, very rockyArB93732965882wbmppa12719771:20000
Arnot channery loam, 8 to 15 percent slopes, very rockyArC70102965892wbmqpa12719771:20000
Rock outcrop-Arnot complex, 3 to 25 percent slopesRoD10742966232wbn5pa12719771:20000
Oquaga-Arnot-Rock outcrop complex, 20 to 60 percent slopes240F1263198632xp9qpa12719771:20000
Arnot very channery silt loam, 3 to 15 percent slopes, very rockyArC93613019022wbmmpa13119761:20000
Arnot-Rock outcrop complex, 8 to 25 percent slopesAsD51713019042wbn0pa13119761:20000
Arnot-Rock outcrop complex, steepASE47823019052wbn4pa13119761:20000
Arnot-Rock outcrop complex, 0 to 8 percent slopesAsB5283019032wbmwpa13119761:20000
Arnot-Rock outcrop complex, 3 to 25 percent slopesAsD155472967472wbmzpa61019781:20000
Arnot very channery loam, 3 to 15 percent slopes, rockyArC57082967462wbmvpa61019781:20000

Map of Series Extent

Approximate geographic distribution of the ARNOT 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 .