Official Series Description


Lab Data Summary

Aggregate lab data for the VALOIS soil series. This aggregation is based on all pedons with a current taxon name of VALOIS, 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 VALOIS 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
13965PA0390031965PA039003Valois4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.5638889,-80.1597222
13965PA0390091965PA039009Valois4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.8352778,-79.9361111

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the VALOIS 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 VALOIS 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 VALOIS 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 VALOIS 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 VALOIS 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 VALOIS 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 VALOIS 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 VALOIS, 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-2010-09-28-01 | Cattarugus County - 2007

    Representative landscape showing soils that formed in residual material, glacial till, glacial outwash, or alluvium (Soil Survey of Cattarugus County, New York; 2007).

  2. 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).

  3. 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).

  4. 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).

  5. 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).

  6. 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).

  7. 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).

  8. NY-2012-02-15-07 | Chautauqua County - August 1994

    Soils and parent material on a bedrock escarpment and on a lake plain that includes the Beach Ridge (Soil Survey of Chautauqua County, New York; August 1994).

  9. NY-2012-02-15-08 | Chautauqua County - August 1994

    A representative landscape showing the relative location of some important soils and the depth to a seasonal high water table (Soil Survey of Chautauqua County, New York; August 1994).

  10. NY-2012-02-15-10 | Chautauqua County - August 1994

    Representative landscape showing soils that formed in residual material, glacial till, glacial outwash, or alluvium (Soil Survey of Chautauqua County, New York; August 1994).

  11. NY-2012-02-15-14 | Chenango County - December 1985

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

  12. 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).

  13. 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).

Map Units

Map units containing VALOIS 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
Valois gravelly loam, 3 to 8 percent slopesVaB11292888079pjcny00119851:15840
Valois gravelly loam, 8 to 15 percent slopesVaC6942888089pjdny00119851:15840
Valois gravelly loam, 15 to 25 percent slopesVaD4592888099pjfny00119851:15840
Valois-Volusia-Mardin complex, 3 to 15 percent slopes53C84692999152srg6ny00320131:24000
Valois gravelly silt loam, 3 to 8 percent slopes52B2451299910b22jny00320131:24000
Valois gravelly silt loam, 8 to 15 percent slopes52C2078299911b22kny00320131:24000
Valois gravelly silt loam, 15 to 25 percent slopes52D2015299912b22lny00320131:24000
Valois gravelly silt loam, 25 to 35 percent slopes52E1836299913b22mny00320131:24000
Valois gravelly silt loam, 35 to 50 percent slopes52F879299914b22nny00320131:24000
Valois gravelly silt loam, 0 to 3 percent slopes52A231318646bpkxny00320131:24000
Valois-Volusia-Mardin complex, 3 to 15 percent slopes53C171622896372srg6ny00920021:24000
Valois gravelly silt loam, 3 to 8 percent slopes52B107752896329qczny00920021:24000
Valois gravelly silt loam, 8 to 15 percent slopes52C86932896339qd0ny00920021:24000
Valois gravelly silt loam, 15 to 25 percent slopes52D32472896349qd1ny00920021:24000
Valois gravelly silt loam, 25 to 35 percent slopes52E17662896359qd2ny00920021:24000
Valois gravelly silt loam, 35 to 50 percent slopes52F8412896369qd3ny00920021:24000
Valois gravelly silt loam, 3 to 8 percent slopesVaB109102898949qnfny01319881:15840
Valois gravelly silt loam, 8 to 15 percent slopesVaC78162898959qngny01319881:15840
Valois gravelly silt loam, rollingVcC64512898999qnlny01319881:15840
Valois gravelly silt loam, 15 to 25 percent slopesVaD26832898969qnhny01319881:15840
Valois gravelly silt loam, 25 to 35 percent slopesVaE10092898979qnjny01319881:15840
Valois gravelly silt loam, 35 to 50 percent slopesVaF8702898989qnkny01319881:15840
Valois gravelly loam, 25 to 40 percent slopesVaE17732899549qqcny01519691:20000
Valois gravelly loam, 8 to 15 percent slopesVaC15062899529qq9ny01519691:20000
Valois gravelly loam, 2 to 8 percent slopesVaB8272899519qq8ny01519691:20000
Valois gravelly loam, 15 to 25 percent slopesVaD7132899539qqbny01519691:20000
Bath-Valois complex, hillyBvD121272899742v32bny01719821:15840
Valois gravelly silt loam, 8 to 15 percent slopesVaC54142900479qtcny01719821:15840
Valois gravelly silt loam, 3 to 8 percent slopesVaB51542900469qtbny01719821:15840
Bath-Valois complex, rollingBvC40182899732v328ny01719821:15840
Valois gravelly silt loam, 15 to 25 percent slopesVaD29382900489qtdny01719821:15840
Bath-Valois complex, undulatingBvB21742899722v325ny01719821:15840
Valois gravelly silt loam, 35 to 50 percent slopesVaF17842900509qtgny01719821:15840
Valois gravelly silt loam, 25 to 35 percent slopesVaE11962900499qtfny01719821:15840
Valois-Howard complex, 15 to 25 percent slopes53D298627231072rwcwny02320141:12000
Valois-Howard complex, 8 to 15 percent slopes53C290527231062rwcxny02320141:12000
Bath-Valois complex, 3 to 8 percent slopes53B266027608382v312ny02320141:12000
Valois and Howard gravelly loams, 25 to 40 percent slopes53E261327231052rwcvny02320141:12000
Valois channery silt loam, 15 to 25 percent slopes52D197927231112rwd1ny02320141:12000
Valois channery silt loam, 8 to 15 percent slopes52C194127231122rwd2ny02320141:12000
Valois channery silt loam, 25 to 40 percent slopes52E106627231132rwd3ny02320141:12000
Valois very fine sandy loam, 8 to 15 percent slopesVaC23942905689rc5ny02519991:24000
Valois very fine sandy loam, 25 to 60 percent slopesVaE23112905709rc7ny02519991:24000
Valois very fine sandy loam, 15 to 25 percent slopesVaD17992905699rc6ny02519991:24000
Valois very fine sandy loam, 3 to 8 percent slopesVaB12432905679rc4ny02519991:24000
Mardin-Valois complex, 25 to 50 percent slopesMeF37342908572srhqny02919791:15840
Valois gravelly silt loam, 15 to 25 percent slopesVaD25462909279rqrny02919791:15840
Valois gravelly silt loam, 8 to 15 percent slopesVaC20302909269rqqny02919791:15840
Valois gravelly silt loam, 3 to 8 percent slopesVaB16742909259rqpny02919791:15840
Valois-Nassau complex, hillyVdD45482917339skrny03919851:24000
Valois gravelly loam, 15 to 35 percent slopes, very stonyVbE43062917309sknny03919851:24000
Valois gravelly loam, rollingVaC27892917279skkny03919851:24000
Valois gravelly loam, 15 to 25 percent slopesVaD20282917289sklny03919851:24000
Valois gravelly loam, 25 to 60 percent slopesVaF10332917299skmny03919851:24000
Valois-Nassau complex, undulatingVdB9312917329skqny03919851:24000
Valois gravelly loam, 3 to 8 percent slopesVaB8592917269skjny03919851:24000
Valois gravelly loam, 35 to 50 percent slopes, very stonyVbF3302917319skpny03919851:24000
Valois gravelly loam, 3 to 8 percent slopes50B439231057352y9x8ny05120191:24000
Valois gravelly loam, 8 to 15 percent slopes50C377931057362y9x9ny05120191:24000
Valois gravelly loam, cool, 8 to 15 percent slopes150C349531057402y9xfny05120191:24000
Valois gravelly loam, cool, 15 to 25 percent slopes150D207531057412y9xgny05120191:24000
Valois gravelly loam, 15 to 25 percent slopes50D179431057372y9xbny05120191:24000
Valois gravelly loam, cool, 3 to 8 percent slopes150B174231057392y9xdny05120191:24000
Valois gravelly loam, 25 to 35 percent slopes50E144131057382y9xcny05120191:24000
Valois gravelly loam, cool, 25 to 35 percent slopes150E84531057422y9xhny05120191:24000
Valois gravelly loam, 15 to 25 percent slopes152D302025049162q6b4ny06920121:12000
Valois gravelly loam, 25 to 35 percent slopes152E204225049172q6b5ny06920121:12000
Valois gravelly loam, 8 to 15 percent slopes152C176725049152q6b3ny06920121:12000
Valois gravelly loam, cool, 15 to 25 percent slopes153D96225049212q6b9ny06920121:12000
Valois gravelly loam, cool, 8 to 15 percent slopes153C78025049202q6b8ny06920121:12000
Valois gravelly loam, 3 to 8 percent slopes152B45125049142q6b2ny06920121:12000
Valois gravelly loam, cool, 25 to 35 percent slopes153E33625049222q6bbny06920121:12000
Valois gravelly loam, cool, 3 to 8 percent slopes153B18625049192q6b7ny06920121:12000
Valois gravelly loam, 8 to 15 percent slopesVaC111152942999w7jny07719931:24000
Valois gravelly loam, 15 to 25 percent slopesVaD101372943009w7kny07719931:24000
Valois gravelly loam, 25 to 35 percent slopesVaE47682943019w7lny07719931:24000
Valois gravelly loam, 3 to 8 percent slopesVaB39082942989w7hny07719931:24000
Valois gravelly loam, 35 to 55 percent slopesVaF15152943029w7mny07719931:24000
Valois fine gravelly silt loam, 2 to 6 percent slopesVcB3152943039w7nny07719931:24000
Valois gravelly silt loam, 8 to 15 percent slopesVaC74182946609wm5ny09719761:15840
Valois gravelly silt loam, 3 to 8 percent slopesVaB48702946599wm4ny09719761:15840
Valois gravelly silt loam, 15 to 25 percent slopesVaD31242946619wm6ny09719761:15840
Valois and Howard soils, very steepVHF18292946639wm8ny09719761:15840
Valois soils, steepVEE14252946629wm7ny09719761:15840
Valois gravelly sandy loam, 3 to 8 percent slopesVaB36132951469x3vny10519841:15840
Valois gravelly sandy loam, 8 to 15 percent slopesVaC29782951479x3wny10519841:15840
Valois gravelly sandy loam, 15 to 25 percent slopesVaD17002951489x3xny10519841:15840
Valois gravelly sandy loam, 35 to 50 percent slopesVaF15532951509x3zny10519841:15840
Valois gravelly sandy loam, 25 to 35 percent slopesVaE12982951499x3yny10519841:15840
Woostern gravelly silt loam, 6 to 15 percent slopesWr40862958569xvrny10719471:31680
Woostern gravelly silt loam, 16 to 25 percent slopesWh39282958559xvqny10719471:31680
Woostern gravelly silt loam, 26 to 45 percent slopeWt25982958579xvsny10719471:31680
Woostern gravelly silt loam, 0 to 5 percent slopesWu7002958589xvtny10719471:31680
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, Valois, and Lansing soils, 35 to 60 percent slopesBtF23092955862v32jny10919631:20000
Howard-Valois gravelly loams, 5 to 15 percent slopesHrC17822956209xm4ny10919631:20000
Howard-Valois gravelly loams, 15 to 25 percent slopesHrD6992956219xm5ny10919631:20000
Bath and Valois soils, 5 to 15 percent slopes, erodedBgC34372955832v32fny10919631:20000
Valois very bouldery soils, gently slopingVAB86432955579xk3ny11119741:15840
Valois very bouldery soils, moderately steepVAD44862955589xk4ny11119741:15840
Bath-Valois complex, 3 to 8 percent slopesBlB122112953072v322ny12119691:20000
Bath-Valois complex, 8 to 15 percent slopesBlC111222953082v323ny12119691:20000
Bath-Valois complex, 15 to 25 percent slopesBlD27842953092v324ny12119691:20000
Bath-Valois complex, 0 to 3 percent slopesBlA13562953062v321ny12119691:20000
Valois gravelly loam, 8 to 15 percent slopes152C344932503392q6b3ny12319481:12000
Valois gravelly loam, 15 to 25 percent slopes152D340532503402q6b4ny12319481:12000
Valois gravelly loam, 25 to 35 percent slopes152E340332503412q6b5ny12319481:12000
Valois gravelly loam, 3 to 8 percent slopes152B146932503382q6b2ny12319481:12000
Valois gravelly loam, cool, 8 to 15 percent slopes153C82332503432q6b8ny12319481:12000
Valois gravelly loam, cool, 15 to 25 percent slopes153D56832503442q6b9ny12319481:12000
Valois gravelly loam, cool, 3 to 8 percent slopes153B33032503422q6b7ny12319481:12000
Valois gravelly loam, cool, 25 to 35 percent slopes153E6032503452q6bbny12319481:12000
Valois gravelly silt loam, 3 to 8 percent slopesVaB182893319q28ny60519811:24000
Valois soils, very steepVLF122042961959y6ppa03919731:20000
Valois-Cambridge complex, 3 to 8 percent slopesVmB83112961992vzq2pa03919731:20000
Valois gravelly silt loam, 15 to 25 percent slopesVaD75232961989y6spa03919731:20000
Valois gravelly silt loam, 8 to 15 percent slopesVaC74962961979y6rpa03919731:20000
Valois gravelly silt loam, 3 to 8 percent slopesVaB51622961969y6qpa03919731:20000
Valois-Cambridge complex, 8 to 15 percent slopesVmC11742962002vzq5pa03919731:20000
Towerville and Valois soils, 40 to 70 percent slopesTvF522626330812rg7tpa04920121:12000
Valois silt loam, 15 to 25 percent slopesVaD256126330752rg7mpa04920121:12000
Valois silt loam, 25 to 40 percent slopesVaE238726330762rg7npa04920121:12000
Valois silt loam, 8 to 15 percent slopesVaC217926330742rg7lpa04920121:12000
Valois silt loam, 3 to 8 percent slopesVaB142926330732rg7kpa04920121:12000
Valois gravelly silt loam, 15 to 25 percent slopes, coolVcD66329442362wbp7pa10519531:24000
Valois gravelly silt loam, 25 to 50 percent slopesVaF61829442372wbp4pa10519531:24000
Valois gravelly silt loam, 25 to 50 percent slopes, coolVcF43929442352wbp8pa10519531:24000
Valois gravelly silt loam, 8 to 15 percent slopes, coolVcC27629442342wbp6pa10519531:24000
Valois gravelly silt loam, 15 to 25 percent slopesVaD24629442322wbp3pa10519531:24000
Valois gravelly silt loam, 8 to 15 percent slopesVaC16829442312wbp2pa10519531:24000
Valois gravelly silt loam, 3 to 8 percent slopes, coolVcB15229442332wbp5pa10519531:24000
Valois gravelly silt loam, 3 to 8 percent slopesVaB10929442302wbp1pa10519531:24000
Valois gravelly loam, 25 to 40 percent slopesVaE414525441krh8pa61019781:20000
Valois gravelly loam, 8 to 15 percent slopesVaC214525431krh7pa61019781:20000

Map of Series Extent

Approximate geographic distribution of the VALOIS 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 .