Official Series Description


Lab Data Summary

Aggregate lab data for the UNADILLA soil series. This aggregation is based on all pedons with a current taxon name of UNADILLA, 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 UNADILLA 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
14578P056878NH005023Unadilla7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.961113,-72.5111084
n/a40A0291S1961NY073009Unadilla5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the UNADILLA 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 UNADILLA 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 UNADILLA 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 UNADILLA 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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Competing Series

Soil series competing with UNADILLA 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 UNADILLA 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 UNADILLA 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 mountains figure.

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

Soil series sharing subgroup-level classification with UNADILLA, 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. NH-2012-02-14-26 | Sullivan County - December 1983

    Typical pattern of soils and underlying material in the Windsor-Unadilla Variant-Agawam unit (Soil Survey of Sullivan County, New Hampshire; December 1983).

  2. NY-2010-09-28-22 | Otsego County - 2006

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

  3. NY-2012-02-15-44 | Seneca Nation of Indians - August 1984

    Typical relationship of soils to parent material in the Allegheny River Valley (Soil Survey of Seneca Nation of Indians, New York; August 1984).

  4. PA-2012-03-12-25 | Bradford and Sullivan Counties - August 1986

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

  5. PA-2012-03-13-76 | Montour County - April 1985

    Typical pattern of soils and underlying material in the Holly-Monongahela-Basher association (Soil Survey of Montour County, PA; 1985).

  6. VT-2012-03-22-11 | Windham County - February 1987

    Typical landscape pattern of several soils and underlying material in Windham County (Soil Survey of Windham County, VT; 1987).

Map Units

Map units containing UNADILLA 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
Unadilla silt loam, 0 to 3 percent slopes230A17302788769c60ma01120121:12000
Unadilla silt loam, 3 to 8 percent slopes230B6822788819c65ma01120121:12000
Unadilla very fine sandy loam, 3 to 8 percent slopes230B2522770559998ma60219761:20000
Unadilla very fine sandy loam, 0 to 3 percent slopes230A1752770549997ma60219761:20000
Unadilla very fine sandy loam, 3 to 8 percent slopes230B413790802vjwrma60519771:15840
Unadilla very fine sandy loam, 0 to 3 percent slopes230A225790799vjwnma60519771:15840
Unadilla very fine sandy loam, 8 to 15 percent slopes230C219790811vjx1ma60519771:15840
Unadilla very fine sandy loam, 3 to 8 percent slopes230B30127750199rnma60719751:15840
Unadilla very fine sandy loam, 8 to 15 percent slopes230C19027750299rpma60719751:15840
Unadilla very fine sandy loam, 3 to 8 percent slopes30B7452796359czhnh00519851:20000
Unadilla very fine sandy loam, 0 to 3 percent slopes30A7122796349czgnh00519851:20000
Unadilla very fine sandy loam, 8 to 15 percent slopes30C2742796369czjnh00519851:20000
Unadilla very fine sandy loam, 3 to 8 percent slopes30B3602793099cmznh01519861:24000
Unadilla very fine sandy loam, 0 to 3 percent slopes30A2052793089cmynh01519861:24000
Unadilla variant silt loam, 15 to 50 percent slopesUnE10792798439d66nh01919811:20000
Unadilla variant silt loam, 3 to 8 percent slopesUnB6622798419d64nh01919811:20000
Unadilla variant silt loam, 8 to 15 percent slopesUnC2452798429d65nh01919811:20000
Unadilla silt loam, 3 to 8 percent slopesUnfB370613448nlbnnj03720021:24000
Unadilla silt loam, 0 to 3 percent slopesUnfA78613447nlbmnj03720021:24000
Unadilla silt loam, 0 to 3 percent slopesUnfA57740991sw1ynj04120071:12000
Unadilla silt loam, 3 to 8 percent slopesUnfB25740992sw1znj04120071:12000
Unadilla silt loam, 3 to 8 percent slopesUnB12172888019pj5ny00119851:15840
Unadilla silt loam, 8 to 15 percent slopesUnC7612888029pj6ny00119851:15840
Unadilla silt loam, 15 to 25 percent slopesUnD7092888039pj7ny00119851:15840
Unadilla silt loam, 0 to 3 percent slopesUnA812888009pj4ny00119851:15840
Unadilla silt loam, 0 to 3 percent slopes20A252299826b1ztny00320131:24000
Unadilla silt loam, 3 to 8 percent slopes20B57299827b1zvny00320131:24000
Unadilla silt loam, 15 to 25 percent slopes20D53299829b1zxny00320131:24000
Unadilla silt loam, 25 to 35 percent slopes20E46318639bpkpny00320131:24000
Unadilla silt loam, 8 to 15 percent slopes20C34299828b1zwny00320131:24000
Unadilla silt loam, 0 to 5 percent slopesUnB35412892119pydny00719661:15840
Unadilla silt loam, 5 to 15 percent slopesUnC15572892129pyfny00719661:15840
Unadilla silt loam, 0 to 3 percent slopes20A8132895589q9lny00920021:24000
Unadilla silt loam, 3 to 8 percent slopes20B2572895599q9mny00920021:24000
Unadilla silt loam, 15 to 25 percent slopes20D2332895619q9pny00920021:24000
Unadilla silt loam, 8 to 15 percent slopes20C2212895609q9nny00920021:24000
Unadilla silt loam, 0 to 3 percent slopesUnA6512898909qn9ny01319881:15840
Unadilla silt loam, 3 to 8 percent slopesUnB5982898919qnbny01319881:15840
Unadilla silt loam, 8 to 15 percent slopesUnC2192898929qncny01319881:15840
Unadilla silt loam, 0 to 3 percent slopesUnA40822899509qq7ny01519691:20000
Unadilla silt loam, 3 to 8 percent slopesUnB8332900459qt9ny01719821:15840
Unadilla silt loam, 0 to 3 percent slopesUnA5702900449qt8ny01719821:15840
Unadilla silt loam, 15 to 25 percent slopesUnD8602902999r2hny02119851:15840
Unadilla silt loam, 3 to 8 percent slopesUnB8422902979r2fny02119851:15840
Unadilla silt loam, 8 to 15 percent slopesUnC4722902989r2gny02119851:15840
Unadilla silt loam, 0 to 3 percent slopesUnA2652902969r2dny02119851:15840
Unadilla silt loamUn15552905659rc2ny02519991:24000
Unadilla silt loam, 3 to 8 percent slopesUnB6642907279rj9ny02719921:24000
Unadilla silt loam, 3 to 8 percent slopes151B47635456pb7lny03520071:24000
Unadilla silt loam, 15 to 25 percent slopesUnD3522928969ts8ny05719731:24000
Unadilla silt loam, 8 to 15 percent slopesUnC1082928959ts7ny05719731:24000
Unadilla silt loam, 0 to 8 percent slopesUnB32928949ts6ny05719731:24000
Unadilla silt loam, 3 to 8 percent slopes35B10042934089v9sny06519931:24000
Unadilla silt loam, 0 to 3 percent slopes35A3562934079v9rny06519931:24000
Unadilla silt loam, 8 to 15 percent slopes35C2292934099v9tny06519931:24000
Unadilla silt loam, 0 to 8 percent slopesUnB5892939859vxdny07119761:15840
Unadilla silt loam, 8 to 15 percent slopesUnC2332939869vxfny07119761:15840
Unadilla silt loam, 2 to 6 percent slopesUnB9552942979w7gny07719931:24000
Unadilla silt loam, 0 to 2 percent slopesUnA9162942969w7fny07719931:24000
Unadilla silt loam, 2 to 6 percent slopesUdB642931159v0bny07919871:12000
Unadilla silt loam, 3 to 8 percent slopesUnB5782932129v3gny08319801:15840
Unadilla silt loam, 8 to 15 percent slopesUnC2552932139v3hny08319801:15840
Unadilla silt loam, 0 to 3 percent slopesUnA2152932119v3fny08319801:15840
Unadilla very fine sandy loam, 3 to 8 percent slopesUnB17222944389wd0ny09119931:24000
Unadilla very fine sandy loam, 8 to 15 percent slopesUnC3922944399wd1ny09119931:24000
Unadilla silt loam, 0 to 8 percent slopesUnB552309660bd71ny09319731:15840
Unadilla silt loam, 8 to 15 percent slopesUnC51309661bd72ny09319731:15840
Unadilla silt loamUn28932948569wthny10119721:15840
Unadilla silt loam, 0 to 2 percent slopesUnA2232951449x3sny10519841:15840
Unadilla silt loam, 2 to 6 percent slopesUnB1412951459x3tny10519841:15840
Unadilla silt loam, 0 to 3 percent slopesUnn30762958489xvhny10719471:31680
Unadilla silt loam, 6 to 15 percent slopesUns7802958499xvjny10719471:31680
Unadilla silt loamUn50512955569xk2ny11119741:15840
Unadilla silt loam, 2 to 6 percent slopesUdB109309674bd7hny11919871:12000
Unadilla silt loamUa10822893309q27ny60519811:24000
Unadilla silt loam, 0 to 3 percent slopesUdA72926331252rg97pa04920121:12000
Unadilla silt loam, 3 to 8 percent slopesUnB30299343b1h7pa06919761:20000
Unadilla silt loamUn1782962619y8tpa08519671:20000
Unadilla silt loam, 3 to 8 percent slopesUnB252539024l2wwpa09319801:20000
Unadilla silt loam, 15 to 25 percent slopesUnD158539026l2wypa09319801:20000
Unadilla silt loam, 8 to 15 percent slopesUnC144539025l2wxpa09319801:20000
Unadilla silt loam, 8 to 15 percent slopesUnC479539673l3ktpa09719801:20000
Unadilla silt loam, 3 to 8 percent slopesUnB429539672l3kspa09719801:20000
Unadilla silt loam, 15 to 25 percent slopesUnD161539674l3kvpa09719801:20000
Unadilla silt loam752792972419z9fpa10319951:24000
Unadilla silt loam, 0 to 3 percent slopesUnA52118837302175hpa10519531:24000
Unadilla silt loamUs15632970779z44pa11519681:20000
Unadilla silt loam, 3 to 8 percent slopesUnB808301972b471pa13119761:20000
Unadilla silt loam, 8 to 15 percent slopesUnC730301973b472pa13119761:20000
Unadilla silt loam, 0 to 3 percent slopesUnA2432539265l34npa60919791:20000
Unadilla silt loam, 3 to 8 percent slopesUnB16362967859ytqpa61019781:20000
Unadilla silt loam, 8 to 15 percent slopesUnC9692967869ytrpa61019781:20000
Unadilla silt loam, 0 to 3 percent slopes1A6852819749gdyvt02519841:20000
Unadilla silt loam, 3 to 8 percent slopes1B4862819759gdzvt02519841:20000
Unadilla silt loam, 8 to 15 percent slopes1C1492819769gf0vt02519841:20000
Unadilla silt loam, 15 to 25 percent slopes1D1002819779gf1vt02519841:20000

Map of Series Extent

Approximate geographic distribution of the UNADILLA 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 .