Official Series Description


Lab Data Summary

Aggregate lab data for the NASSAU soil series. This aggregation is based on all pedons with a current taxon name of NASSAU, 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 NASSAU 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
144A40A1173S1969NY115002Nassau5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1916656,-73.4075012

Water Balance

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

Soil series competing with NASSAU 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 NASSAU series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the NASSAU 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 terrace figure.

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

Soil series sharing subgroup-level classification with NASSAU, 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-2010-09-28-26 | Saratoga County - 2004

    Typical relationship of soils and underlying material in the Broadalbin-Mosherville-Sun general soil map unit (Soil Survey of Saratoga County, New York; 2004).

  2. NY-2012-02-15-15 | Columbia County - June 1989

    Typical pattern of Pittstown, Bernardston, Nassau, and Manlius soils on uplands and Hoosic soils on outwash plains (Soil Survey of Columbia County, New York; June 1989).

  3. NY-2012-02-15-39 | Rensselaer County - January 1988

    Typical relationship of soils and underlying material in the Bernardston-Pittstown-Nassau general soil map unit (Soil Survey of Rensselaer County, New York; January 1988).

Map Units

Map units containing NASSAU 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
Nassau-Manlius very channery silt loams, 8 to 15 percent slopes, rockyNauC2257430450872wh29nj03720021:24000
Nassau-Manlius very channery silt loams, 15 to 35 percent slopes, rockyNauD1714830450882wh2bnj03720021:24000
Nassau-Manlius very channery silt loams, 35 to 60 percent slopes, very rockyNauEg559630450892wh2dnj03720021:24000
Nassau-Manlius very channery silt loams, 0 to 8 percent slopes, rockyNauB531330450862wh28nj03720021:24000
Manlius-Nassau very channery silt loams, 35 to 60 percent slopes, very rockyMabEg72030450902wh2cnj03720021:24000
Urban land-Nassau-Manlius complex, 0 to 15 percent slopesUSNAMC523723866s97jnj03720021:24000
Urban land-Nassau-Manlius complex, 0 to 8 percent slopesUSNAMB266723865s97hnj03720021:24000
Urban land-Nassau-Manlius complex, 0 to 25 percent slopesUSNAMD218723867s97knj03720021:24000
Nassau-Manlius very channery silt loams, 15 to 35 percent slopes, rockyNauD977930450842wh2bnj04120071:12000
Nassau-Manlius very channery silt loams, 8 to 15 percent slopes, rockyNauC882130450832wh29nj04120071:12000
Nassau-Manlius very channery silt loams, 35 to 60 percent slopes, very rockyNauEg352530450852wh2dnj04120071:12000
Nassau-Manlius very channery silt loams, 0 to 8 percent slopes, rockyNauB146730450822wh28nj04120071:12000
Nassau channery silt loam, undulatingNaB14282887639pgyny00119851:15840
Nassau channery silt loam, rollingNaC14222887649pgzny00119851:15840
Nassau very channery silt loam, hilly, very rockyNrD6322887669ph1ny00119851:15840
Nassau very channery silt loam, rolling, very rockyNrC4872887659ph0ny00119851:15840
Nassau channery silt loam, hilly, very rockyNbD387752902649r1cny02119851:15840
Nassau channery silt loam, rolling, very rockyNbC369012902639r1bny02119851:15840
Nassau channery silt loam, steep, very rockyNbE135332902659r1dny02119851:15840
Nassau channery silt loam, undulating, rockyNaB54382902629r19ny02119851:15840
Nassau-Cardigan complex, hilly, very rockyNwD431672907009rhfny02719921:24000
Nassau-Cardigan complex, rolling, very rockyNwC321202906999rhdny02719921:24000
Nassau-Rock outcrop complex, steepNxE131442907019rhgny02719921:24000
Nassau-Cardigan complex, undulating, very rockyNwB77702906989rhcny02719921:24000
Nassau-Rock outcrop complex, very steepNxF15582907029rhhny02719921:24000
Valois-Nassau complex, hillyVdD45482917339skrny03919851:24000
Nassau channery silt loam, hilly, very rockyNrD30762916869sj7ny03919851:24000
Nassau channery silt loam, rollingNaC20222916849sj5ny03919851:24000
Nassau channery silt loam, rolling, very rockyNrC10842916859sj6ny03919851:24000
Nassau channery silt loam, steep, very rockyNrE9612916879sj8ny03919851:24000
Valois-Nassau complex, undulatingVdB9312917329skqny03919851:24000
Shaly rock land, very steepShF796825183979sz4ny04320181:24000
Nassau silt loam, 15 to 25 percent slopesNaD179125183779syhny04320181:24000
Nassau silt loam, 8 to 15 percent slopesNaC118625183769sygny04320181:24000
Nassau silt loam, 3 to 8 percent slopesNaB67925183759syfny04320181:24000
Nassau channery silt loam, 8 to 15 percent slopesNaC13182918859sqnny04519811:15840
Nassau-Manlius channery silt loams, rocky, 25 to 50 percent slopesNbF6302918869sqpny04519811:15840
Nassau channery silt loam, 8 to 25 percent slopesNaD32928629tr5ny05719731:24000
Bath-Nassau channery silt loams, 3 to 8 percent slopesBnB158482939009vtnny07119761:15840
Bath-Nassau channery silt loams, 8 to 15 percent slopesBnC120942939019vtpny07119761:15840
Rock outcrop-Nassau complex, hillyRSD97942939709vwxny07119761:15840
Rock outcrop-Nassau complex, undulatingRSB78652939699vwwny07119761:15840
Nassau channery silt loam, 15 to 25 percent slopesNaD36952939409vvyny07119761:15840
Rock outcrop-Nassau complex, very steepRSF11442939719vwyny07119761:15840
Nassau-Rock outcrop complex, hillyNrD196602931879v2nny08319801:15840
Nassau-Manlius complex, rollingNaC144882931859v2lny08319801:15840
Bernardston-Nassau complex, rollingBnC140682931479v1cny08319801:15840
Bernardston-Nassau complex, hillyBnD82592931489v1dny08319801:15840
Bernardston-Nassau complex, undulatingBnB75552931469v1bny08319801:15840
Nassau-Rock outcrop, complex, rollingNrC60712931869v2mny08319801:15840
Nassau-Manlius complex, undulatingNaB56542931849v2kny08319801:15840
Broadalbin-Manlius-Nassau, complex, undulatingBvB73682943529w97ny09119931:24000
Bernardston-Manlius-Nassau complex, undulatingBnB32662943469w91ny09119931:24000
Bernardston-Manlius-Nassau complex, rollingBnC29462943479w92ny09119931:24000
Manlius-Nassau complex, undulating, rockyMnB27532943949wblny09119931:24000
Manlius-Nassau complex, rolling, rockyMnC18672943959wbmny09119931:24000
Broadalbin-Manlius-Nassau, complex, rollingBvC16232943539w98ny09119931:24000
Nassau-Rock outcrop complex, hillyNaD14552944029wbvny09119931:24000
Nassau-Rock outcrop complex, rollingNaC9422944019wbtny09119931:24000
Bernardston-Manlius-Nassau complex, hillyBnD6932943489w93ny09119931:24000
Manlius-Nassau complex, hilly, rockyMnD5362943969wbnny09119931:24000
Broadalbin-Manlius-Nassau, complex, hillyBvD3152943549w99ny09119931:24000
Nassau channery silt loam, 0 to 8 percent slopesNaB950309624bd5wny09319731:15840
Nassau channery silt loam, 8 to 25 percent slopesNaD406309625bd5xny09319731:15840
Lordstown, Oquaga, and Nassau soils, 35 to 70 percent slopes, very rockyLrF312642944992zxqwny09519651:15840
Nassau shaly silt loam, 15 to 35 percent slopesNaE15812945239wgrny09519651:15840
Nassau shaly silt loam, 2 to 15 percent slopesNaC5782945229wgqny09519651:15840
Bath-Nassau-Rock outcrop complex, hillyBOD288882954569xfvny11119741:15840
Bath-Nassau complex, 8 to 25 percent slopesBnC231332954559xftny11119741:15840
Nassau-Bath-Rock outcrop complex, very steepNBF165322955079xhhny11119741:15840
Mardin-Nassau complex, 3 to 8 percent slopesMgB149712955012v30kny11119741:15840
Nassau-Manlius complex, very steepNNF45482955099xhkny11119741:15840
Nassau-Manlius shaly silt loams, rollingNMC32142955089xhjny11119741:15840
Nassau-Rock outcrop complex, hillyNOD8202955109xhlny11119741:15840
Nassau-Rock outcrop association, undulating through hillyNBC541632959889y00ny11519721:20000
Nassau-Rock outcrop association, steep and very steepNBF440982959899y01ny11519721:20000
Nassau shaly silt loam, undulating through hillyNAC412382959879xzzny11519721:20000
Bernardston-Nassau shaly silt loams, 8 to 15 percent slopesBrC109752959519xytny11519721:20000
Bernardston-Nassau shaly silt loams, rolling and hillyBSCK92772959429xyjny11519721:20000
Bernardston-Nassau shaly silt loams, 3 to 8 percent slopesBrB52902959509xysny11519721:20000
Nassau extremely rocky silt loam, 3 to 25 percent slopesNdC34532812919fpxvt00119671:15840
Nassau-Dutchess rocky complex, 3 to 8 percent slopesNaB4972812889fptvt00119671:15840
Nassau-Dutchess rocky complex, 8 to 15 percent slopesNaC3652812899fpvvt00119671:15840
Nassau-Dutchess rocky complex, 15 to 25 percent slopesNaD2162812909fpwvt00119671:15840

Map of Series Extent

Approximate geographic distribution of the NASSAU 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 .