Official Series Description


Lab Data Summary

Aggregate lab data for the OKOLONA soil series. This aggregation is based on all pedons with a current taxon name of OKOLONA, 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 OKOLONA 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
135AS86AL-105-686AL105006-pgmOkolona3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.4963889,-87.3591667

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the OKOLONA 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 OKOLONA 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 OKOLONA 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 OKOLONA 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 OKOLONA 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 OKOLONA 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 OKOLONA 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 OKOLONA, 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 OKOLONA 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
Okolona silty clay loam, 0 to 3 percent slopesOkB33843297562svnsal06520031:24000
Okolona silty clay loam, 1 to 3 percent slopesOkB14825146582qdgkal08520111:24000
Okolona silty clay loam, 0 to 3 percent slopesOkB180303312482svnsal10519961:24000
Okolona silty clay, 1 to 3 percent slopesOkB3300331279c3qfal10719971:24000
Okolona silty clay, 0 to 1 percent slopesOkA2220331278c3qdal10719971:24000
Okolona silty clay, 0 to 3 percent slopesOkB4420331485c3y2al11919861:24000
Okolona silty clay, 2 to 5 percent slopesOkB366633189630wbvms01719691:20000
Okolona silty clay, 0 to 2 percent slopesOkA83333189530wbsms01719691:20000
Houston clay, 0 to 2 percent slopes (okolona)HuA2667331997c4glms02319631:15840
Houston clay, 2 to 5 percent slopes (okolona)HuB1938331998c4gmms02319631:15840
Okolona silty clay, 1 to 3 percent slopesOkB66833320952w9w2ms02519741:20000
Okolona silty clay, 0 to 1 percent slopesOkA10843320942w9vzms02519741:20000
Okolona clay, 1 to 3 percent slopes, erodedOkB2907332638c548ms06119741:20000
Okolona silty clay, 1 to 3 percent slopesOaA5363327712w9w2ms06919911:20000
Okolona silty clay, 1 to 3 percent slopesOkB124323330822w9w2ms08719771:20000
Okolona silty clay, 0 to 1 percent slopesOkA48193330812w9vzms08719771:20000
Okolona silty clay, 2 to 5 percent slopesHoB1842533317530wbvms09519631:15840
Okolona silty clay, 0 to 2 percent slopesHoA754533317430wbsms09519631:15840
Okolona silty clay, 1 to 3 percent slopesOkB102453334332w9w2ms10319831:20000
Okolona silty clay, 0 to 1 percent slopesOkA66623334322w9vzms10319831:20000

Map of Series Extent

Approximate geographic distribution of the OKOLONA 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 .