Official Series Description


Lab Data Summary

Aggregate lab data for the MANLIUS soil series. This aggregation is based on all pedons with a current taxon name of MANLIUS, 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 MANLIUS 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
14064PA1030051964PA103005Manlius3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.2080556,-74.8894444
14064PA1030061964PA103006Manlius3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.2627778,-74.8663889
14011N0151S2009NY123035Manlius6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.6148694,-77.00845

Water Balance

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

Click the image to view it full size.

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

Soil series sharing subgroup-level classification with MANLIUS, 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-2010-09-28-21 | Otsego County - 2006

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

  2. 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).

  3. 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).

  4. NY-2012-02-15-21 | Genesee County - March 1969

    Cross section showing typical soil pattern in the Fremont-Hornell-Manlius association (Soil Survey of Genesee County, New York; March 1969).

  5. 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).

  6. NY-2012-02-16-03 | Wyoming County - April 1974

    Typical pattern of soils in association 7 (Soil Survey of Wyoming County, New York; April 1974).

  7. NY-2012-02-16-06 | Wyoming County - April 1974

    Typical pattern of soils in association 13 (Soil Survey of Wyoming County, New York; April 1974).

Map Units

Map units containing MANLIUS 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
Manlius channery silt loam, 25 to 35 percent slopesMbE8182887579pgrny00119851:15840
Manlius channery silt loam, 8 to 15 percent slopesMbC5812887559pgpny00119851:15840
Manlius channery silt loam, 15 to 25 percent slopesMbD3992887569pgqny00119851:15840
Manlius channery silt loam, 3 to 8 percent slopesMbB3762887549pgnny00119851:15840
Rock outcrop-Manlius complex, 35 to 70 percent slopes82F6162897279qh1ny00920021:24000
Rock outcrop-Manlius complex, 35 to 70 percent slopesRoF7962898719qmpny01319881:15840
Manlius channery silt loam, 8 to 15 percent slopesMnC70872903649r4lny02119851:15840
Manlius channery silt loam, 3 to 8 percent slopesMnB59142903639r4kny02119851:15840
Manlius channery silt loam, 15 to 25 percent slopesMnD28442903659r4mny02119851:15840
Manlius channery silt loam, 0 to 3 percent slopesMnA2202903629r4jny02119851:15840
Manlius channery silt loam, 3 to 8 percent slopesMaB42982908479rn5ny02919791:15840
Manlius channery silt loam, 15 to 25 percent slopesMaD25272908499rn7ny02919791:15840
Manlius very channery silt loam, 35 to 50 percent slope sMbF23462908519rn9ny02919791:15840
Manlius very channery silt loam, 25 to 35 percent slope sMbE20422908509rn8ny02919791:15840
Manlius channery silt loam, 8 to 15 percent slopesMaC17292908489rn6ny02919791:15840
Manlius channery silt loam, 0 to 3 percent slopesMaA5382908469rn4ny02919791:15840
Manlius channery silt loam, 3 to 8 percent slopesMlB726301740b3zkny03720041:24000
Manlius channery silt loam, 8 to 15 percent slopesMlC676301741b3zlny03720041:24000
Manlius channery silt loam, 25 to 40 percent slopesMlE221301743b3znny03720041:24000
Manlius channery silt loam, 15 to 25 percent slopesMlD210301742b3zmny03720041:24000
Manlius shaly silt loam, 15 to 25 percent slopesMlD250025183699sy7ny04320181:24000
Manlius shaly silt loam, 8 to 15 percent slopesMlC131625183689sy6ny04320181:24000
Manlius shaly silt loam, 3 to 8 percent slopesMlB74425183679sy5ny04320181:24000
Manlius channery silt loam, 3 to 8 percent slopesMnB24092918739sq8ny04519811:15840
Nassau-Manlius channery silt loams, rocky, 25 to 50 percent slopesNbF6302918869sqpny04519811:15840
Manlius channery silt loam, 8 to 15 percent slopesMnC3812918749sq9ny04519811:15840
Manlius silt loam, 15 to 35 percent slopesMdD9372677737bmm4ny04920181:24000
Manlius silt loam, 8 to 15 percent slopesMdC5612677736bmm3ny04920181:24000
Manlius silt loam, 0 to 8 percent slopesMdB3442677735bmm2ny04920181:24000
Lordstown-Manlius-Towerville complex, 35 to 80 percent slopes, extremely stony81F245031057082wzmbny05120191:24000
Lordstown-Manlius-Towerville complex, 25 to 35 percent slopes, extremely stony81E165831057072ywlwny05120191:24000
Manlius channery silt loam, 3 to 8 percent slopes82B27731057092y9wjny05120191:24000
Manlius channery silt loam, 8 to 15 percent slopes82C24631057102y9wkny05120191:24000
Manlius channery silt loam, 15 to 25 percent slopes82D23031057112y9wlny05120191:24000
Manlius shaly silt loam, 8 to 15 percent slopesMoC9892928529tqvny05719731:24000
Manlius shaly silt loam, 15 to 25 percent slopesMoD7432928539tqwny05719731:24000
Manlius silt loam, 3 to 8 percent slopesMnB2482928519tqtny05719731:24000
Manlius-Rock outcrop association, steepMPE102928459tqmny05719731:24000
Manlius channery silt loam, 25 to 45 percent slopes168E33042933579v84ny06519931:24000
Manlius channery silt loam, 15 to 25 percent slopes168D16312933569v83ny06519931:24000
Manlius channery silt loam, 8 to 15 percent slopes168C15952933559v82ny06519931:24000
Manlius channery silt loam, 3 to 8 percent slopes168B13272933549v81ny06519931:24000
Manlius channery silt loam, 6 to 12 percent slopesMnC6702936139vjdny06719731:20000
Manlius channery silt loam, 12 to 18 percent slopesMnD4872936149vjfny06719731:20000
Manlius channery silt loam, 2 to 6 percent slopesMnB1982936129vjcny06719731:20000
Lordstown-Manlius-Towerville complex, 35 to 80 percent slopes, extremely stony171F912525042542wzmbny06920121:12000
Lordstown-Manlius-Towerville complex, 25 to 35 percent slopes, extremely stony171E397525042532ywlwny06920121:12000
Lordstown-Manlius-Towerville complex, 15 to 25 percent slopes, very stony171D184625042522ywlxny06920121:12000
Lordstown-Manlius-Towerville complex, 8 to 15 percent slopes, very stony171C26325124242zfflny06920121:12000
Manlius channery silt loam, 15 to 25 percent slopes82D19525042632pq3mny06920121:12000
Manlius channery silt loam, 8 to 15 percent slopes82C4125042642pq3pny06920121:12000
Manlius channery silt loam, 3 to 8 percent slopes82B2425042622pq3nny06920121:12000
Lordstown, Chadakoin, and Manlius soils, 25 to 50 percent slopes, very rockyLrE316712942429w5pny07719931:24000
Manlius channery silt loam, 8 to 15 percent slopesMcC8502942489w5wny07719931:24000
Manlius channery silt loam, 3 to 8 percent slopesMcB8402942479w5vny07719931:24000
Manlius channery silt loam, 15 to 25 percent slopesMcD7642942499w5xny07719931:24000
Nassau-Manlius complex, rollingNaC144882931859v2lny08319801:15840
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
Bernardston-Manlius-Nassau complex, hillyBnD6932943489w93ny09119931:24000
Manlius-Nassau complex, hilly, rockyMnD5362943969wbnny09119931:24000
Broadalbin-Manlius-Nassau, complex, hillyBvD3152943549w99ny09119931:24000
Manlius-Rock outcrop association, steepMPE2144309605bd58ny09319731:15840
Manlius silt loam, 3 to 8 percent slopesMnB635309611bd5gny09319731:15840
Manlius shaly silt loam, 8 to 15 percent slopesMoC536309612bd5hny09319731:15840
Manlius shaly silt loam, 15 to 25 percent slopesMoD405309613bd5jny09319731:15840
Manlius channery silt loam, 3 to 8 percent slopesMaB4062950849x1vny10519841:15840
Manlius channery silt loam, 8 to 15 percent slopesMaC3522950859x1wny10519841:15840
Manlius channery silt loam, 15 to 25 percent slopesMaD2872950869x1xny10519841:15840
Nassau-Manlius complex, very steepNNF45482955099xhkny11119741:15840
Nassau-Manlius shaly silt loams, rollingNMC32142955089xhjny11119741:15840
Manlius and Lordstown soils, 25 to 60 percent slopesMnF16602954022ywlhny12119691:20000
Manlius channery silt loam, 25 to 40 percent slopesMlE13382954019xd2ny12119691:20000
Manlius channery silt loam, 15 to 25 percent slopesMlD8062954009xd1ny12119691:20000
Manlius channery silt loam, 2 to 8 percent slopesMlB7072953989xczny12119691:20000
Manlius channery silt loam, 8 to 15 percent slopesMlC5882953999xd0ny12119691:20000
Lordstown-Manlius-Towerville complex, 35 to 80 percent slopes, extremely stony171F358214078302wzmbny12319481:12000
Lordstown-Manlius-Towerville complex, 25 to 35 percent slopes, extremely stony171E242414078262ywlwny12319481:12000
Manlius channery silt loam, 8 to 15 percent slopes82C103132648772pq3pny12319481:12000
Lordstown-Manlius-Towerville complex, 15 to 25 percent slopes, very stony171D102832504022ywlxny12319481:12000
Manlius channery silt loam, 3 to 8 percent slopes82B61432503372pq3nny12319481:12000
Lordstown-Manlius-Towerville complex, 8 to 15 percent slopes, very stony171C44532504042zfflny12319481:12000
Manlius channery silt loam, 15 to 25 percent slopes82D32232503362pq3mny12319481:12000
Manlius very shaly silt loam, 35 to 50 percent slopesMbF1602892939q11ny60519811:24000
Manlius shaly silt loam, 15 to 25 percent slopesMaD822892919q0zny60519811:24000
Manlius very shaly silt loam, 25 to 35 percent slopesMbE632892929q10ny60519811:24000
Manlius shaly silt loam, 3 to 8 percent slopesMaB442892909q0yny60519811:24000
Manlius shaly silt loam, 0 to 3 percent slopesMaA252892899q0xny60519811:24000
Manlius channery silt loam, 8 to 15 percent slopesMaC2641194880223dwlpa09520071:12000
Manlius channery silt loam, 3 to 8 percent slopesMaB2270194879723dwfpa09520071:12000
Manlius channery silt loam, 15 to 25 percent slopesMaD1427194881823dx3pa09520071:12000
Manlius-Arnot-Rock outcrop complex, 30 to 80 percent slopes121F76352971892xp94pa10319951:24000
Manlius-Arnot-Rock outcrop complex, 15 to 30 percent slopes121D38792971882xp93pa10319951:24000
Manlius very channery silt loam, 3 to 8 percent slopes, very bouldery21B17142971979z80pa10319951:24000
Manlius very channery silt loam, 8 to 15 percent slopes, very bouldery21C15202971989z81pa10319951:24000

Map of Series Extent

Approximate geographic distribution of the MANLIUS 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 .