Official Series Description


Lab Data Summary

Aggregate lab data for the OCANA soil series. This aggregation is based on all pedons with a current taxon name of OCANA, 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 OCANA 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 OCANA 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 OCANA 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 OCANA 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 OCANA 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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Click the image to view it full size.

Competing Series

Soil series competing with OCANA 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 OCANA 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 OCANA 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.

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

Soil series sharing subgroup-level classification with OCANA, 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. TN-2010-11-02-03 | Clay County - 2004

    The relatiohship between soils and landscape in the Dellrose-Renox-Barfield and Garmon-Newbern general soil map units (Soil Survey of Clay County, Tennessee; 2004)

Map Units

Map units containing OCANA 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
Ocana gravelly silt loam, 0 to 3 percent slopes, occasionally floodedOc16685244532td2stn01519991:24000
Ocana gravelly silt loam, occasionally floodedOn686524454klqwtn01519991:24000
Ocana gravelly silt loam, 0 to 3 percent slopes, occasionally floodedOc23966367872td2stn02720021:24000
Ocana gravelly silt loam, 0 to 3 percent slopes, occasionally floodedOc46375234352td2stn03719771:15840
Ocana gravelly silt loam, 0 to 3 percent slopes, occasionally floodedOc37765302032td2stn08719991:24000
Ocana gravelly silt loam, 0 to 3 percent slopes, occasionally floodedOc19465277162td2stn11119921:24000
Ocana gravelly silt loam, 0 to 3 percent slopes, occasionally floodedHm92385277952td2stn11919551:20000
Huntington cherty silt loam, phosphatic phaseHl1473527794kq6mtn11919551:20000
Ocana gravelly silt loam, 0 to 3 percent slopes, occasionally floodedOc13328432342td2stn13320031:24000
Ocana gravelly silt loam, 0 to 3 percent slopes, occasionally floodedOc19685298342td2stn15919921:24000
Ocana gravelly silt loam, 0 to 3 percent slopes, occasionally floodedEc173123969022td2stn16119531:20000
Ocana gravelly silt loam, bedrock substratum, occasionally floodedOc4926528379kqthtn16519931:20000
Ocana gravelly silt loam, 0 to 3 percent slopes, occasionally floodedOb3465283782td2stn16519931:20000
Ocana gravelly silt loam, 0 to 3 percent slopes, occasionally floodedOc4015300372td2stn16919931:24000
Ocana gravelly silt loam, 0 to 3 percent slopes, occasionally floodedHr9635298922td2stn17719651:15840
Ocana gravelly silt loam, 0 to 3 percent slopes, occasionally floodedHs86924274512td2stn61019601:15840

Map of Series Extent

Approximate geographic distribution of the OCANA 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 .