Official Series Description


Lab Data Summary

Aggregate lab data for the OCHEYEDAN soil series. This aggregation is based on all pedons with a current taxon name of OCHEYEDAN, 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 OCHEYEDAN 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.


Water Balance

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

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

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Soil series sharing subgroup-level classification with OCHEYEDAN, 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 OCHEYEDAN 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
Ocheyedan loam, 2 to 5 percent slopes878B290403966fkc5ia03519871:15840
Ocheyedan loam, 5 to 9 percent slopes, moderately eroded878C2206403967fkc6ia03519871:15840
Ocheyedan clay loam, lacustrine substratum, 2 to 5 percent slopes379B994399348fdk6ia04120021:12000
Ocheyedan loam, 2 to 5 percent slopes878B584399441fdn6ia04120021:12000
Ocheyedan loam, 0 to 2 percent slopes878386399440fdn5ia04120021:12000
Ocheyedan clay loam, lacustrine substratum, 0 to 2 percent slopes379246399347fdk5ia04120021:12000
Ocheyedan loam, 2 to 5 percent slopes878B1683186907520qxria05920111:12000
Ocheyedan loam, 0 to 2 percent slopes878628186907420qxqia05920111:12000
Ocheyedan loam, 2 to 5 percent slopes878B1581406262fmr7ia07319831:15840
Ocheyedan loam, 5 to 9 percent slopes, moderately eroded878C2587406264fmr9ia07319831:15840
Ocheyedan loam, 2 to 5 percent slopes, moderately eroded878B2446406263fmr8ia07319831:15840
Ocheyedan loam, 0 to 2 percent slopes878383406261fmr6ia07319831:15840
Ocheyedan loam, 2 to 5 percent slopes878B3508409148fqrbia11919731:15840
Ocheyedan loam, 5 to 9 percent slopes, moderately eroded878C21401409150fqrdia11919731:15840
Ocheyedan loam, 2 to 5 percent slopes, moderately eroded878B21053409149fqrcia11919731:15840
Ocheyedan loam, 0 to 2 percent slopes878357409147fqr9ia11919731:15840
Ocheyedan loam, 9 to 14 percent slopes, moderately eroded878D2285409151fqrfia11919731:15840
Ocheyedan loam, 2 to 5 percent slopes878B456410099frr0ia14119771:15840
Ocheyedan loam, 2 to 5 percent slopes878B102624992382q4m2ia14319851:15840
Ocheyedan loam, 5 to 9 percent slopes, moderately eroded878C2904411268fsyqia16719871:15840
Ocheyedan loam, 2 to 5 percent slopes, moderately eroded878B2280411267fsypia16719871:15840
Ocheyedan loam, 2 to 5 percent slopes878B264411266fsynia16719871:15840
Ocheyedan loam, 2 to 8 percent slopes275B597396165f97jmn01319751:12000
Clarion-Ocheyedan complex, 2 to 5 percent slopesL228B112217160421vlp6mn03320081:12000
Ocheyedan loam, 2 to 6 percent slopes275B10830397101fb6qmn04319891:20000
Ocheyedan loam, 6 to 12 percent slopes, eroded275C22054397102fb6rmn04319891:20000
Ocheyedan loam, 1 to 5 percent slopes275B1821400042ff8lmn09119851:20000

Map of Series Extent

Approximate geographic distribution of the OCHEYEDAN 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 .