Official Series Description


Lab Data Summary

Aggregate lab data for the OAK LEVEL soil series. This aggregation is based on all pedons with a current taxon name of OAK LEVEL, 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 OAK LEVEL 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
13604N0044S2002NC097023Oak Level6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.8919182,-80.7665863
13604N0045S2002NC097024Oak Level6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.8919182,-80.7665863
13604N0046S2002NC097028Oak Level6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.8919182,-80.7665863

Water Balance

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

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 OAK LEVEL 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 OAK LEVEL 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 OAK LEVEL 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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 OAK LEVEL, 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 OAK LEVEL 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
Oak Level clay loam, 2 to 8 percent slopes, moderately erodedOkB2442724245602mcymnc05919881:24000
Oak Level clay loam, 8 to 15 percent slopes, moderately erodedOkC2187424245612mcynnc05919881:24000
Oak Level loam, dark surface, 6 to 10 percent slopesOkC98524337452mphxnc06719701:15840
Oak Level loam, dark surface, 2 to 6 percent slopesOkB68024337442mphwnc06719701:15840
Oak Level loam, dark surface, 10 to 15 percent slopesOkD42924337472mphznc06719701:15840
Oak Level sandy clay loam, 2 to 6 percent slopes, moderately erodedOkB238824334282mp5pnc08119751:20000
Oak Level sandy clay loam, 6 to 10 percent slopes, moderately erodedOkC237024334292mp5qnc08119751:20000
Oak Level loam, 2 to 6 percent slopesOaB65224393072mw9bnc14519871:24000
Oak Level loam, 6 to 10 percent slopesOaC25924393102mw9fnc14519871:24000
Oak Level sandy clay loam, 2 to 8 percent slopes, moderately erodedOkB269823899632l6ylnc15719831:24000
Oak Level loam, 8 to 15 percent slopes, moderately erodedOkC225023983542lhp8nc19719601:15840
Oak Level loam, 2 to 8 percent slopes, moderately erodedOkB224823983532lhp7nc19719601:15840
Oak Level loam, 15 to 25 percent slopes, moderately erodedOkE26823983552lhp9nc19719601:15840
Oak Level loam, 7 to 15 percent slopes24C48801359542xx6kva01919851:24000
Oak Level loam, 15 to 25 percent slopes24D33361359552xx6lva01919851:24000
Oak Level loam, 2 to 7 percent slopes24B15171359532xx6jva01919851:24000
Oak Level-Siloam complex, 7 to 15 percent slopes30C3928024794272p71jva02920101:24000
Oak Level-Diana Mills complex, 2 to 7 percent slopes29B1108524794262p71hva02920101:24000
Oak Level-Siloam complex, 15 to 25 percent slopes30D708424794282p71kva02920101:24000
Oak Level loam, 7 to 15 percent slopes, extremely bouldery28C159924794242p71fva02920101:24000
Oak Level loam, 15 to 50 percent slopes, extremely bouldery28E18424794252p71gva02920101:24000
Oak Level-Diana Mills complex, 2 to 7 percent slopes28B72915874291q8vdva04920051:24000
Oak Level-Siloam complex, 7 to 15 percent slopes29C66515874301q8vfva04920051:24000
Oak Level-Siloam complex, 15 to 25 percent slopes29D22215874311q8vgva04920051:24000
Oak Level loam, 2 to 8 percent slopes37B196914728391lflyva08320041:24000
Oak Level loam, 8 to 15 percent slopes37C155514728401lflzva08320041:24000
Oak Level silt loam, 2 to 7 percent slopes, moderately erodedMvB22341198802zhfhva13719661:15840
Oak Level silt loam, 7 to 15 percent slopes, moderately erodedMvC21591198812zhfjva13719661:15840

Map of Series Extent

Approximate geographic distribution of the OAK LEVEL 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 .