Official Series Description


Lab Data Summary

Aggregate lab data for the OCHLOCKONEE soil series. This aggregation is based on all pedons with a current taxon name of OCHLOCKONEE, 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 OCHLOCKONEE 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
133A86P018385GA261007Ochlockonee8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.0111122,-84.3972244

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the OCHLOCKONEE 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 OCHLOCKONEE 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 OCHLOCKONEE 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 OCHLOCKONEE 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 OCHLOCKONEE 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 OCHLOCKONEE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the OCHLOCKONEE 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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.

Soil series sharing subgroup-level classification with OCHLOCKONEE, 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. AR-2012-05-08-03 | Bradley County - April 1961

    General soil areas (Soil Survey of Bradley County, Arkansas; April 1961).

  2. OK-2012-02-16-49 | Hughes County - December 1968

    Typical pattern of soils in association 3 (Soil Survey of Hughes County, Oklahoma; December 1968).

  3. TN-2012-03-19-09 | Haywood County - September 1995

    Pattern of soils and parent material in the Lexington-Smithdale general soil map unit (Soil Survey of Haywood County, TN; 1995).

Map Units

Map units containing OCHLOCKONEE 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
Ochlockonee-Riverview complex, gently undulating, frequently floodedObB303022336092v5llal00720071:24000
Ochlockonee, Kinston, and Iuka soils, 0 to 1 percent slopes, frequently floodedOKA26540328569c0x0al02319981:24000
Ochlockonee sandy loam, 0 to 2 percent slopes, frequently floodedOcA4160328633c0z2al02520041:24000
Ochlockonee loamy fine sandOc117912280543sgal02919741:24000
Ochlockonee loamOc3037329479c1vcal05719631:15840
Iuka-Ochlockonee complex, local alluviumIo1795329465c1txal05719631:15840
Ochlockonee sandy loamOd297329480c1vdal05719631:15840
Ochlockonee fine sandy loamOc7274329580c1ymal05919621:15840
Ochlockonee fine sandy loamOc6571329684c21zal06320131:
Ochlockonee fine sandy loam, local alluviumOe1716329685c220al06320131:
Ochlockonee fine sandy loam, 0 to 2 percent slopes, frequently floodedOcA10524945542vxxhal07520101:24000
Ochlockonee fine sandy loam, 0 to 2 percent slopes, frequently flooded2130003306232vxxhal09319761:20000
Ochlockonee silt loamOa498330934c3c9al10119581:20000
Ochlockonee-Riverview complex, gently undulating, frequently floodedObB72803312462v5llal10519961:24000
Ochlockonee sandy loam, 0 to 1 percent slopes, occasionally floodedOaA740331245c3pbal10519961:24000
Ochlockonee-Kinston-Iuka complex, 0 to 2 percent slopes, frequently floodedOcA5480331269c3q3al10719971:24000
Ochlockonee fine sandy loam (toccoa)Oc522812286843vhal11119651:15840
Ochlockonee fine sandy loam, local alluvium (toccoa)Ok250912286943vjal11119651:15840
Ochlockonee fine sandy loam (ouachita)Oc15991565162lz31ar01119591:20000
Ochlockonee fine sandy loam, occasionally flooded4458873179378lyn7ar01919831:20000
Ochlockonee-Wehadkee association (guyton)Ow10758565307lz7qar02519651:15840
Ochlockonee very fine sandy loamOc8962565306lz7par02519651:15840
Ochlockonee loamOc1240564414ly9xar03719661:20000
Ochlockonee fine sandy loam, occasionally flooded445233179268lyn7ar05919831:20000
Ochlockonee fine sandy loam, 0 to 2 percent slopes, frequently flooded56518815429481nskjar10920051:20000
Ochlockonee fine sandy loam, 0 to 2 percent slopes, occasionally flooded55123115429521nsknar10920051:20000
Ochlockonee fine sandy loam, 0 to 2 percent slopes, rarely flooded5468815429491nskkar10920051:20000
Ouachita and Ochlockonee soils, occasionally flooded522673564928lyvhar67019811:20000
Wahee-Ochlockonee complex, commonly flooded38837614810211lq3wfl01319971:20000
Wahee and Ochlockonee soils, 0 to 3 percent slopes, occasionally flooded1197716724781t4bxfl03920061:12000
Wahee-Mantachie-Ochlockonee complex, commonly flooded50352914727701lfjqfl04519971:24000
Wahee and Ochlockonee soils, 0 to 3 percent slopes, occasionally flooded6619190322757btvjfl07720041:24000
Garcon, Ochlockonee, and Ousley soils, occasionally flooded74400322773btw1fl07720041:24000
Ochlockonee, Iuka, and Bibb soils, 0 to 5 percent slopes, frequently floodedOBB633024253972mdtmga25920091:12000
Ochlockonee, Iuka, and Bibb soils, 0 to 5 percent slopes, frequently floodedOBB103024554272nf2bga30720091:12000
Ochlockonee loamy sandOc2795325442bxn4ga61219751:20000
Ochlockonee sandy loam, rarely floodedOc207612620147b0ga62019921:20000
Bigbee-Ochlockonee complex, 0 to 5 percent slopes, occasionally floodedBoC793126168478yga62019921:20000
Ochlockonee sandy loamOc4925325788by09ga63419801:20000
Ochlockonee sandy loam, occasionally floodedOc2135325966by61ga64119861:20000
Ochlockonee soils, local alluviumOi4545326272byhxga65219691:20000
Ochlockonee sandy loamOc5635326361bylsga65419791:20000
Vicksburg-Ochlockonee complex, 0 to 3 percent slopes, rarely floodedVo508822322242dxt7ky61019681:12000
Iuka and Ochlockonee soils, frequently floodedIU1478417245411vwjcla03119861:24000
Ouachita, Ochlockonee, and Guyton soils, nearly level to undulating, frequently floodedOUA19674577016mcffla03320071:24000
Ouachita, Ochlockonee and Guyton soils, 0 to 3 percent slopes, frequently floodedOG5247816052752w8y5la03719921:24000
Guyton-Ouachita-Ochlockonee association, frequently floodedGYA7309317252571vx8gla04919911:24000
Ouachita, Ochlockonee and Guyton soils, 0 to 3 percent slopes, frequently floodedOU367755697492w8y5la06319871:24000
Ouachita, Ochlockonee and Guyton soils, 0 to 3 percent slopes, frequently floodedOG5791217216432w8y5la09119911:24000
Ouachita, Ochlockonee and Guyton soils, 0 to 3 percent slopes, frequently floodedOG6235315365182w8y5la10519851:24000
Ouachita, Ochlockonee and Guyton soils, 0 to 3 percent slopes, frequently floodedOG530017256092w8y5la12520021:24000
Jena and Ochlockonee soilsJe5104331807c48gms00919721:20000
Iuka fine sandy loam (ochlockonee)Ik3708331999c4gnms02319631:15840
Iuka soils, local alluvium (ochlockonee)Iu1587332000c4gpms02319631:15840
Ochlockonee fine sandy loam, occasionally flooded131317567800m1v4ms03719921:20000
Ochlockonee silt loam, 0 to 3 percent slopes, frequently floodedOcB22626422222rs2yms04120121:24000
Ochlockonee sandy loam, occasionally flooded911461332843c5bwms07119791:20000
Ochlockonee-Bruno association, frequently flooded405792332826c5bbms07119791:20000
Ochlockonee-Bruno complex, frequently flooded41335332827c5bcms07119791:20000
Vicksburg and Ochlockonee soilsVo10791568301m2c9ms09319681:20000
Ochlockonee sandy loamOc4987568290m2byms09319681:20000
Iuka fine sandy loam (ochlockonee) (0 to 2 percent slopes)Ic5387333320c5v8ms10119571:20000
Iuka very fine sandy loam, local alluvium phase (ochlockonee) (0 to 2 percent slopes)Ib690333319c5v7ms10119571:20000
Ochlockonee fine sandy loam, local alluvium phase (0 to 2 percent slopes)Oa232333342c5vzms10119571:20000
Ochlockonee fine sandy loam, occasionally floodedOc402333431c5yvms10319831:20000
Ochlockonee loam (jena)Oc6194333500c612ms10519681:20000
Iuka and Ochlockonee soilsIo4820333644c65qms11319651:15840
Ochlockonee and Bruno soilsOb588333646c65sms11319651:15840
Iuka and Ochlockonee soilsIo2563333699c67hms11519691:20000
Ochlockonee-iuka soils, (jena-kirkville)Oc9103334287c6vgms14719651:20000
Local alluvial landLo14041309804d95sc60219601:20000
Ochlockonee sandy loamOc62981317644f3gsc61519811:20000
Ochlockonee loamy sand, occasionally floodedOa3951313564dp9sc69619881:15840
Ochlockonee fine sandy loam, 0 to 3 percent slopes, rarely floodedOk144225453622qsgrtn00520111:12000
Ochlockonee loam, occasionally floodedOc5633327229bzhstn02319891:24000
OCHLOCKONEE FINE SANDY LOAMSk1265327363bzn3tn03920081:24000
OCHLOCKONEE SILT LOAMSl800327364bzn4tn03920081:24000
OCHLOCKONEE FINE SANDY LOAM, 0 TO 2 PERCENT SLOPESAb405327258bzjqtn03920081:24000
Ochlockonee silt loam, rarely floodedOc11357327485bzs1tn06919961:24000
Vicksburg loam, local alluvium (Ochlockonee)Vc3637327663bzystn07119611:15840
Vicksburg loam (Ochlockonee)Vb483327662bzyrtn07119611:15840
Ochlockonee fine sandy loam, occasionally floodedOc4070567100m13ktn07519901:24000
Ochlockonee fine sandy loam, 0 to 3 percent slopes, rarely floodedOk444225452822qs8vtn07920121:12000
Ochlockonee fine sandy loam, occasionally floodedOc1900327966c08ktn10919941:20000
Ochlockonee fine sandy loamOc3642567222m17htn11319741:20000
Ochlocknee fine sandy loam, occasionally floodedEd323969032lg5gtn16119531:20000
Ochlockonee loam, occasionally floodedOh4369567384m1dqtn18319861:24000
Ochlockonee loam, rarely floodedOc531567383m1dptn18319861:24000
Ochlockonee loamy fine sandOa2166575359m9pztx07319491:20000
Ochlockonee soils, occasionally floodedOc2258374440dkmqtx61119801:20000
Ochlockonee-Ochlockonee variant complex1914691189513zs4va07319781:15840
Ochlockonee silt loam1555611963440h5va11919821:15840

Map of Series Extent

Approximate geographic distribution of the OCHLOCKONEE 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 .