Official Series Description


Lab Data Summary

Aggregate lab data for the ONTARIO soil series. This aggregation is based on all pedons with a current taxon name of ONTARIO, 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 ONTARIO were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
10106N0866S2006NY123007Ontario5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.7014389,-77.0326

Water Balance

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

There are insufficient data to create the 3D mountains figure.

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 ONTARIO, 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-2012-02-15-05 | Cayuga County - 1971

    Typical cross section of Ontario association in the north-central part of the county (Soil Survey of Cayuga County, New York; 1971).

  2. NY-2012-02-15-17 | Genesee County - March 1969

    Cross section showing typical soil patterns in the Ontario-Hilton association, the Collamer-Galen-Canandaigua-Lamson association, and the Muck association in northern Genesee County (Soil Survey of Genesee County, New York; March 1969).

  3. NY-2012-02-15-36 | Niagara County - October 1972

    Typical cross section of the Hilton-Ovid-Ontario association (Soil Survey of Niagara County, New York; October 1972).

Map Units

Map units containing ONTARIO 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
Ontario loam, 3 to 8 percent slopesOnB152702894612w3psny01119681:15840
Ontario, Honeoye, and Lansing soils, 20 to 35 percent slopesOtE81372894702w3mxny01119681:15840
Ontario loam, 8 to 15 percent slopesOnC28492894622w3pxny01119681:15840
Ontario fine sandy loam, 3 to 8 percent slopesOfB25542894582xgg3ny01119681:15840
Ontario silt loam, moderately shallow variant, 3 to 8 percent slopesOrB21502894689q6pny01119681:15840
Ontario, Honeoye, and Lansing soils, 35 to 50 percent slopesOtF19832894712w3mqny01119681:15840
Ontario fine sandy loam, 8 to 15 percent slopesOfC12542894592xgg4ny01119681:15840
Ontario loam, 14 to 20 percent slopesOnD6802894652w3q2ny01119681:15840
Ontario silt loam, moderately shallow variant, 0 to 3 percent slopesOrA6002894679q6nny01119681:15840
Ontario silt loam, moderately shallow variant, 8 to 14 percent slopesOrC3732894699q6qny01119681:15840
Ontario loam, 3 to 8 percent slopesOnB224613017632w3psny03720041:24000
Ontario loam, 0 to 3 percent slopesOnA48693017622wrdpny03720041:24000
Ontario loam, 8 to 15 percent slopesOnC43153017642w3pxny03720041:24000
Ontario loam, 3 to 8 percent slopes, stonyOsB14953017672w3pvny03720041:24000
Ontario loam, 15 to 25 percent slopesOnD6363017652w3q3ny03720041:24000
Ontario and Lansing soils, 25 to 40 percent slopesOrE4643017662w3mnny03720041:24000
Ontario loam, 8 to 15 percent slopes, stonyOsC1233017682w3pzny03720041:24000
Ontario silt loam, 15 to 25 percent slopesOnD179925183802xggcny04320181:24000
Ontario silt loam, 8 to 15 percent slopesOnC78725183792xggbny04320181:24000
Ontario silt loam, 3 to 8 percent slopesOnB61725183782xgg9ny04320181:24000
Ontario-Hilton complex, 3 to 8 percent slopes167B1671131057872ywl6ny05120191:24000
Ontario loam, 8 to 15 percent slopes52C385031002842w3pxny05120191:24000
Ontario loam, 15 to 25 percent slopes52D143031056862w3q3ny05120191:24000
Ontario loam, 3 to 8 percent slopes52B142231056842w3psny05120191:24000
Ontario-Hilton complex, 0 to 3 percent slopes167A92331057862ywl5ny05120191:24000
Ontario fine sandy loam, 8 to 15 percent slopes252C74031002892xgg4ny05120191:24000
Ontario loam, 25 to 35 percent slopes52E62331056872y9w6ny05120191:24000
Ontario fine sandy loam, 3 to 8 percent slopes252B23931057752xgg3ny05120191:24000
Ontario fine sandy loam, 15 to 25 percent slopes252D20131057772xgg5ny05120191:24000
Ontario loam, 3 to 8 percent slopesOnB16542926082w3psny05319751:15840
Ontario loam, 8 to 15 percent slopesOnC4892926092w3pxny05319751:15840
Ontario loam, 3 to 8 percent slopesOnB218742927422w3psny05519671:15840
Ontario loam, 8 to 15 percent slopesOnC76742927432w3pxny05519671:15840
Ontario fine sandy loam, 3 to 8 percent slopesOfB50172927402xgg3ny05519671:15840
Ontario loam, 15 to 25 percent slopesOnD319972927452w3q3ny05519671:15840
Ontario loam, 25 to 60 percent slopesOnF17352927462w3q7ny05519671:15840
Ontario fine sandy loam, 8 to 15 percent slopesOfC14862927412xgg4ny05519671:15840
Ontario-Palmyra-Arkport complex, 25 to 60 percent slopesOpF11022927492w3q8ny05519671:15840
Ontario-Palmyra-Arkport complex, 8 to 15 percent slopesOpC8632927472w3pyny05519671:15840
Ontario-Palmyra-Arkport complex, 15 to 25 percent slopesOpD8362927482w3q4ny05519671:15840
Ontario loam, 3 to 8 percent slopesOgB108842936312w3psny06719731:20000
Honeoye, Lansing, and Ontario soils, 25 to 35 percent slopesHTE90792935662w3mtny06719731:20000
Ontario gravelly loam, 8 to 15 percent slopesOnC58102936322w3qcny06719731:20000
Honeoye, Lansing, and Ontario soils, 35 to 50 percent slopesHTF53952935672w3mrny06719731:20000
Ontario and Madrid soils, 15 to 25 percent slopesOpD40492936352w3qgny06719731:20000
Ontario loam, 3 to 8 percent slopes116B571617276152w3psny06920121:12000
Ontario fine sandy loam, 3 to 8 percent slopes112B552917276072xgg3ny06920121:12000
Ontario loam, 8 to 15 percent slopes116C217917276142w3pxny06920121:12000
Ontario fine sandy loam, 25 to 35 percent slopes112E208117276092xgg8ny06920121:12000
Ontario fine sandy loam, 8 to 15 percent slopes112C190617276082xgg4ny06920121:12000
Ontario, Honeoye, and Lansing soils, 35 to 55 percent slopes118F186617276162w3mpny06920121:12000
Ontario fine sandy loam, 15 to 25 percent slopes112D131017276102xgg5ny06920121:12000
Ontario loam, 15 to 25 percent slopes116D127317276132w3q3ny06920121:12000
Ontario gravelly loam, 3 to 8 percent slopes114B110117276122w3q9ny06920121:12000
Ontario gravelly loam, 8 to 15 percent slopes114C42817276112w3qcny06920121:12000
Ontario gravelly loam, 15 to 25 percent slopes114D14825127472w3qfny06920121:12000
Ontario loam, 3 to 8 percent slopesOnB26682940632w3psny07319731:15840
Ontario loam, 3 to 8 percent slopes, stonyOoB11762940652w3pvny07319731:15840
Ontario loam, 8 to 15 percent slopesOnC7042940642w3pxny07319731:15840
Ontario loam, 0 to 8 percent slopes, bedrock substratumOtB4402940672w3prny07319731:15840
Ontario loam, 3 to 15 percent slopes, very stonyOsC3212940662w3q0ny07319731:15840
Ontario loam, 3 to 8 percent slopesOnB53042947572w3psny09919661:15840
Ontario loam, 15 to 25 percent slopesOnD311792947602w3q3ny09919661:15840
Honeoye, Ontario, and Lansing soils, 25 to 40 percent slopesHoE9752947282w3mvny09919661:15840
Ontario fine sandy loam, 3 to 8 percent slopesOfB9622947552xgg3ny09919661:15840
Ontario loam, 8 to 15 percent slopesOnC4792947582w3pxny09919661:15840
Ontario fine sandy loam, 8 to 15 percent slopesOfC32512947562xgg4ny09919661:15840
Ontario silt loam, Moderately shallow variant, and Farmington soils, 2 to 8 percent slopesOpB1532947619wqfny09919661:15840
Ontario gravelly loam, 3 to 8 percent slopesOnB278072957642w3q9ny11719721:15840
Ontario gravelly loam, 8 to 15 percent slopesOnC158332957652w3qcny11719721:15840
Ontario gravelly loam, 25 to 35 percent slopesOSE143142957622w3qhny11719721:15840
Ontario gravelly loam, 15 to 25 percent slopesOnD72132957662w3qfny11719721:15840
Ontario, Honeoye, and Lansing soils, 35 to 55 percent slopes118F210532503722w3mpny12319481:12000
Ontario loam, 3 to 8 percent slopes116B160332503822w3psny12319481:12000
Ontario gravelly loam, 8 to 15 percent slopes114C74132503852w3qcny12319481:12000
Ontario gravelly loam, 3 to 8 percent slopes114B58032503842w3q9ny12319481:12000
Ontario loam, 8 to 15 percent slopes116C57432503832w3pxny12319481:12000
Ontario gravelly loam, 15 to 25 percent slopes114D19832503862w3qfny12319481:12000
Ontario fine sandy loam, 25 to 35 percent slopes112E8232504002xgg8ny12319481:12000
Ontario loam, 3 to 8 percent slopesOnB31352930292w3psny66419681:15840
Ontario loam, 0 to 3 percent slopes, bedrock substratumOoA7742930332w3ppny66419681:15840
Ontario loam, 3 to 8 percent slopes, bedrock substratumOoB7232930342w3ptny66419681:15840
Ontario loam, 8 to 15 percent slopesOnC4762930302w3pxny66419681:15840
Ontario loam, 15 to 30 percent slopesOnD31832930322w3q5ny66419681:15840

Map of Series Extent

Approximate geographic distribution of the ONTARIO 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 .