Official Series Description


Lab Data Summary

Aggregate lab data for the SCHOHARIE soil series. This aggregation is based on all pedons with a current taxon name of SCHOHARIE, 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 SCHOHARIE 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
14094P0368S1993NY095002Schoharie6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.3836098,-74.4586105

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SCHOHARIE 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 SCHOHARIE 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 SCHOHARIE 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 SCHOHARIE 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 SCHOHARIE 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 SCHOHARIE 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 SCHOHARIE 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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Click the image to view it full size.

Soil series sharing subgroup-level classification with SCHOHARIE, 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

No block diagrams are available.

Map Units

Map units containing SCHOHARIE 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
Schoharie silt loam, 2 to 6 percent slopesSeB31492894872xgh4ny01119681:15840
Cazenovia and Schoharie soils, 20 to 40 percent slopesChE8422893802xghgny01119681:15840
Schoharie silty clay loam, 6 to 12 percent slopesShC7992894882xgglny01119681:15840
Schoharie silty clay loam, 12 to 20 percent slopesShD6792894892xggqny01119681:15840
Urban land-Schoharie complex, 0 to 3 percent slopesUu56572909212xggfny02919791:15840
Schoharie silt loam, 3 to 8 percent slopesSaB32112908992xgh8ny02919791:15840
Schoharie silt loam, 0 to 3 percent slopesSaA26672908982xgh1ny02919791:15840
Schoharie silty clay loam, 8 to 15 percent slopesSbC35782909002xggnny02919791:15840
Schoharie silt loam, 1 to 6 percent slopesSeB11733017942xgh3ny03720041:24000
Schoharie silty clay loam, 6 to 12 percent slopesShC33433017952xgglny03720041:24000
Schoharie silty clay loam, 12 to 20 percent slopesShD31623017962xggqny03720041:24000
Schoharie silty clay loam, 20 to 60 percent slopesSlE3423017972xggwny03720041:24000
Odessa-Schoharie complex, 3 to 8 percent slopes336B1201431002942wrdjny05120191:24000
Odessa-Schoharie complex, 0 to 3 percent slopes135A1028931002922wrddny05120191:24000
Schoharie silt loam, 8 to 15 percent slopes236C307231002482xghcny05120191:24000
Schoharie silty clay loam, 3 to 8 percent slopes36B219631002532xggkny05120191:24000
Schoharie silty clay loam, 25 to 35 percent slopes36E151531056762xggxny05120191:24000
Schoharie silty clay loam, 15 to 25 percent slopes36D125231056752xggsny05120191:24000
Schoharie silty clay loam, 8 to 15 percent slopes36C69331002522xggnny05120191:24000
Schoharie silt loam, 3 to 8 percent slopes236B60131057732xgh8ny05120191:24000
Elmridge-Schoharie complex, 3 to 8 percent slopes136B30831002952xgh2ny05120191:24000
Schoharie silt loam, 0 to 3 percent slopes236A30031057722xgh1ny05120191:24000
Schoharie and Cayuga soils, 3 to 8 percent slopes436B8231002932xghdny05120191:24000
Schoharie-Cazenovia complex, 25 to 50 percent slopesSEE22492926302xggzny05319751:15840
Schoharie silt loam, 3 to 8 percent slopesScB14052926272xgh8ny05319751:15840
Schoharie silty clay loam, 8 to 15 percent slopesSdC9262926282xggnny05319751:15840
Schoharie silty clay loam, 15 to 25 percent slopesSdD37262926292xggsny05319751:15840
Schoharie silt loam, 2 to 6 percent slopesSeB59702927652xgh4ny05519671:15840
Schoharie silt loam, 0 to 3 percent slopesSeA35222927642xgh1ny05519671:15840
Schoharie silty clay loam, 6 to 12 percent slopesShC35172927662xgglny05519671:15840
Schoharie silty clay loam, 20 to 60 percent slopesShF4262927682xggwny05519671:15840
Schoharie silty clay loam, 12 to 20 percent slopes, erodedShD33362927679tn3ny05519671:15840
Schoharie silt loam, 3 to 8 percent slopes61B3922934642xgh8ny06519931:24000
Schoharie silt loam, 20 to 40 percent slopes61E2812934662xghfny06519931:24000
Schoharie silt loam, 8 to 15 percent slopes61C2672934652xghcny06519931:24000
Schoharie silt loam, 0 to 3 percent slopes61A1642934632xgh1ny06519931:24000
Schoharie silt loam, 8 to 15 percent slopesScC15172936562xghcny06719731:20000
Schoharie silt loam, 2 to 6 percent slopesScB8602936552xgh4ny06719731:20000
Schoharie silty clay loam, 15 to 25 percent slopesSdD8592936572xggsny06719731:20000
Schoharie silty clay loam, 25 to 35 percent slopesSEE7352936542xggxny06719731:20000
Schoharie silty clay loam, 3 to 8 percent slopes36B1176823784232xggkny06920121:12000
Schoharie silty clay loam, 0 to 3 percent slopes36A578323784252wrdrny06920121:12000
Schoharie silty clay loam, 8 to 15 percent slopes36C485223784162xggnny06920121:12000
Schoharie silty clay loam, 15 to 25 percent slopes36D247623784242xggsny06920121:12000
Schoharie silty clay loam, 25 to 45 percent slopes36E213123784222xggyny06920121:12000
Schoharie silt loam, 0 to 3 percent slopes37A140423784322xgh1ny06920121:12000
Schoharie silt loam, 3 to 8 percent slopes37B125423784282xgh8ny06920121:12000
Schoharie silt loam, 2 to 6 percent slopesScB6092940762xgh4ny07319731:15840
Schoharie silt loam, 20 to 40 percent slopesSoE41732945502xghfny09519651:15840
Schoharie and Hudson silt loams, 2 to 6 percent slopesShB35702945452xgh6ny09519651:15840
Schoharie and Hudson silty clay loams, 6 to 12 percent slopesSnC335112945482xggmny09519651:15840
Schoharie and Hudson silt loams, 6 to 12 percent slopesShC27842945462xghbny09519651:15840
Schoharie and Hudson soils, 12 to 20 percent slopesSnD321482945492xggrny09519651:15840
Schoharie and Hudson silty clay loams, 2 to 6 percent slopesSnB33542945472xgghny09519651:15840
Schoharie silty clay loam, 8 to 15 percent slopesScC322912946482xggnny09719761:15840
Schoharie silty clay loam, 3 to 8 percent slopesScB311992946472xggkny09719761:15840
Schoharie variant silty clay loam, 15 to 25 percent slopes, severely erodedShD35512946519wlwny09719761:15840
Schoharie variant silty clay loam, 8 to 15 percent slopes, severely erodedShC33562946509wlvny09719761:15840
Schoharie silty clay loam, 15 to 25 percent slopesScD32322946492xggsny09719761:15840
Schoharie silty clay loam, 2 to 6 percent slopesShB56302947732xgggny09919661:15840
Schoharie silt loam, 2 to 6 percent slopesSeB51932947712xgh4ny09919661:15840
Schoharie silty clay loam, 0 to 3 percent slopesShA23422947722wrdrny09919661:15840
Schoharie silty clay loam, 6 to 12 percent slopesShC38082947742xgglny09919661:15840
Schoharie silty clay loam, 12 to 20 percent slopesShD32762947752xggqny09919661:15840
Hudson and Schoharie soils, 15 to 25 percent slopesHwD24182954882xggtny11119741:15840
Schoharie silt loam, 8 to 15 percent slopesSaC22322955372xghcny11119741:15840
Schoharie silt loam, 3 to 8 percent slopesSaB21372955362xgh8ny11119741:15840
Hudson and Schoharie soils, 25 to 55 percent slopesHXE14392954892xgh0ny11119741:15840
Hudson and Schoharie soils, 8 to 15 percent slopesHvC31842954872xggpny11119741:15840
Schoharie silty clay loam, 8 to 15 percent slopes36C30714078832xggnny12319481:12000
Schoharie silty clay loam, 3 to 8 percent slopes36B14314078842xggkny12319481:12000
Schoharie silty clay loam, 15 to 25 percent slopes36D11414078892xggsny12319481:12000
Schoharie silty clay loam, 2 to 6 percent slopesShB8132930522xgggny66419681:15840

Map of Series Extent

Approximate geographic distribution of the SCHOHARIE 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 .