Official Series Description


Lab Data Summary

Aggregate lab data for the IUKA soil series. This aggregation is based on all pedons with a current taxon name of IUKA, 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 IUKA 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
11981HS031981AR05903Iuka3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.2967,-93.0208
129S70AL-009-370AL009003-pgmIuka3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.9533386230469,-86.570556640625
131A65GN441965AR05544Iuka3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.01556,-90.81583
131A87GN051987AR05505Iuka3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.01528,-90.73889
131A87GN081987AR05508Iuka3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.08361,-90.66222
133AS02AL-041-202AL041002-pgmIuka3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.6833333,-86.3194444
133AS84AL-109-1084AL109010-pgmIuka3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.7475051879883,-85.9200057983398
133AS85AL-011-685AL011006-pgmIuka2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.9611111,-85.775
133B61HP131961AR05713Iuka1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.7056,-93.5078
133B63CV291963AR02529Iuka3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.73944,-92.09028
133B67OT081967AR10308Iuka3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.60861,-92.81944
13459LE131959AR07713Iuka3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.7338,-90.7669
13487GN091987AR05509Iuka3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.04056,-90.67639
13440A4990S1959TN047012Iuka5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.1122208,-89.3886108
135B61HP041961AR05704Iuka3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.7192,-93.5303
135B68HW171968AR06117Iuka3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.8992,-94.02722
n/a63CS311963AR03731Iuka3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the IUKA 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 IUKA 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 IUKA 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 IUKA 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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Click the image to view it full size.

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 IUKA 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 IUKA 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 IUKA 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 IUKA, 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. AL-2010-08-27-01 | Clarke County - 2006

    Generalized patterns of soils and geomorphology and landscape relationships in general soil map units 2—Iuka-Bibb-Harleston, 6—Lucedale-Bama-Smithdale, 8—Smithdale-Wadley-Boykin, 9—Smithdale-Flomaton-Wadley, 10—Prim-Suggsville-Brantley, and 11—Okeelala-Brantley-Smithdale. The area illustrated is along Bassett Creek in the northeastern part of Clarke County, Alabama (Soil Survey of Clarke County, Alabama; 2006) .

  2. AL-2012-04-24-02 | Clarke County - August 2006

    Generalized patterns of soils and geomorphology and landscape relationships in general soil map units 2—Iuka-Bibb-Harleston, 6—Lucedale-Bama-Smithdale, 8—Smithdale-Wadley-Boykin, 9—Smithdale-Flomaton-Wadley, 10—Prim-Suggsville-Brantley, and 11—Okeelala-Brantley-Smithdale. The area illustrated is along Bassett Creek in the northeastern part of Clarke County, Alabama (Soil Survey of Clarke County, Alabama; August 2006).

  3. DC-2011-05-31-01 | District of Columbia - 1976

    Typical pattern of soils and parent material in the Urban land-Beltsville-Chillum association (Soil Survey of District of Columbia; 1976).

  4. DC-2011-05-31-02 | District of Columbia - 1976

    Typical pattern of soils and parent material in the Urban land-Christiana-Sunnyside association (Soil Survey of District of Columbia; 1976).

  5. MS-2012-02-06-07 | Prentiss County - October 1997

    Typical pattern of soils and parent material in the Mantachie-Iuka general soil map unit (Soil Survey of Prentiss County, Mississippi; October 1997).

  6. MS-2012-04-27-05 | Tippah County - February 1966

    Distribution and pattern of major soils in Mantachie-Bibb association (Soil Survey of Tippah County, Mississippi; February 1966).

  7. MS-2012-04-27-11 | Newton County - February 1960

    Soil associations of Newton County, Mississippi (Soil Survey of Newton County, Mississippi; February 1960).

  8. TX-2012-03-21-06 | Harrison County - October 1994

    Pattern of soils and parent material in the Scottsville general soil map unit (Soil Survey of Harrison County, TX; 1994).

Map Units

Map units containing IUKA 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
Iuka silt loamIu16758328151c0gjal00319611:20000
Local alluvial landLv4285328165c0gzal00319611:20000
Iuka-Bibb complex, 0 to 1 percent slopes, frequently floodedIbA35200328266c0l7al00520011:24000
Mantachie, Kinston and Iuka soils, 0 to 1 percent slopes, frequently floodedMAA315403282602s69dal00520011:24000
Bibb-Iuka complex, 0 to 1 percent slopes, frequently floodedBdA2316022303112shs8al00720071:24000
Mantachie, Kinston and Iuka soils, 0 to 1 percent slopes, frequently floodedMIA2062522325332s69dal00720071:24000
Mantachie, Iuka, and Bibb soils, 0 to 1 percent slopes, frequently floodedMBA43870328423c0r9al01119861:20000
Mantachie, Bibb, and Iuka soils, 0 to 1 percent slopes, frequently floodedMIA56120328464c0smal01319961:20000
Bibb-Iuka complex, 0 to 1 percent slopes, frequently floodedBbA374003285932shs8al02319981:24000
Ochlockonee, Kinston, and Iuka soils, 0 to 1 percent slopes, frequently floodedOKA26540328569c0x0al02319981:24000
Iuka, Bibb, and Mantachie soils, 0 to 1 percent slopes, frequently floodedIBA57350328641c0zbal02520041:24000
Iuka-Bibb sandy loams, 0 to 2 percent slopes, frequently floodedIbA6479328766c13cal03919851:20000
Mantachie, Kinston and Iuka soils, 0 to 1 percent slopes, frequently floodedMKA293503288742s69dal04120051:24000
Bibb-Iuka complex, 0 to 1 percent slopes, frequently floodedBbA246305816112shs8al04120051:24000
Iuka-Marietta complex, 0 to 2 percent slopes, frequently floodedImA86015329981ng6kal04120051:24000
Iuka soils, local alluviumIb367328984c1bdal04519581:20000
Iuka fine sandy loamIa128328983c1bcal04519581:20000
Mantachie, Kinston and Iuka soils, 0 to 1 percent slopes, frequently floodedMKA29653222s69dal05119481:20000
Mantachie, Leaf, and Iuka soilsMk7780329470c1v2al05719631:15840
Iuka silt loamIk2686329464c1twal05719631:15840
Iuka-Ochlockonee complex, local alluviumIo1795329465c1txal05719631:15840
Iuka fine sandy loam, 0 to 2 percent slopes, occasionally floodedIs67883295702w6ffal05919621:15840
Iuka fine sandy loam, local alluviumIu806329571c1ybal05919621:15840
Mantachie, Kinston and Iuka soils, 0 to 1 percent slopes, frequently floodedMIA218253297712s69dal06520031:24000
Bibb-Iuka complex, 0 to 1 percent slopes, frequently floodedBdA156563297432shs8al06520031:24000
Mantachie, Iuka, and Kinston soils, 0 to 1 percent slopes, frequently floodedMIA4580640568phkhal06920021:24000
Iuka-Mantachie complex, 0 to 2 percent slopes, frequently floodedImA792024945432vxx1al07520101:24000
Mantachie, Kinston and Iuka soils, 0 to 1 percent slopes, frequently floodedMKI720725146132s69dal08520111:24000
Iuka-Marietta complex, 0 to 2 percent slopes, frequently floodedImA276825146502qcwkal08520111:24000
Bibb-Iuka complex, 0 to 1 percent slopes, frequently floodedBbA157903305582shs8al09119971:24000
Iuka-Mantachie complex, 0 to 2 percent slopes, frequently flooded11260003306122vxx1al09319761:20000
Mantachie-Iuka association176250330618c313al09319761:20000
Iuka and Mantachie soils, 0 to 2 percent slopes, frequently floodedImA51300330840c388al09919841:20000
Mantachie, Kinston and Iuka soils, 0 to 1 percent slopes, frequently floodedMKA215713309542s69dal10119581:20000
Iuka soils, local alluvium phasesIc1124330916c3bqal10119581:20000
Iuka soilsIb317330915c3bpal10119581:20000
Mantachie, Kinston and Iuka soils, 0 to 1 percent slopes, frequently floodedMIA297903312402s69dal10519961:24000
Ochlockonee-Kinston-Iuka complex, 0 to 2 percent slopes, frequently floodedOcA5480331269c3q3al10719971:24000
Mantachie, Kinston and Iuka soils, 0 to 1 percent slopes, frequently floodedMAA654303313182s69dal10919961:20000
Kinston, Mantachie, and Iuka soils, 0 to 1 percent slopes, frequently floodedKMA40230331344c3sjal11319971:24000
Kinston-Iuka complex, 0 to 1 percent slopes, frequently floodedKnA130014764201lkbgal12320051:24000
Iuka-Mantachie complex, 0 to 2 percent slopes, frequently flooded19368163315112vxx1al12519801:20000
Bibb-Iuka complex, 0 to 2 percent slopes, frequently floodedBiA933326420562rjqtal12920131:24000
Iuka-Mantachie silt loams (ouachita, guyton)IM5612565154lz2sar01119591:20000
Iuka fine sandy loam, occasionally flooded2942483179361lympar01919831:20000
Iuka soils, local alluvium, 3 to 8 percent slopes (beulah)IvC1190564402ly9jar03719661:20000
Iuka loam, 0 to 1 percent slopesIuA1020564399ly9far03719661:20000
Iuka soils, local alluvium, 1 to 3 percent slopesIvB450564401ly9har03719661:20000
Iuka loam, gently undulatingIuB290564400ly9gar03719661:20000
Bruno and Iuka soilsBu9433565532lzgzar04719671:20000
Iuka fine sandy loam, occasionally flooded294023179251lympar05919831:20000
Iuka soilsIk600564457lyc9ar12319641:20000
Iuka sandy loamIk27312861349ttdc00119751:12000
Iuka-Urban land complexIp25312861449tvdc00119751:12000
Iuka fine sandy loam, frequently flooded7190014253761jv6wfl03319981:24000
Iuka loam3797014249411jtrvfl06319771:20000
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
Iuka sandy loam, occasionally floodedIu9476126186479jga62019921:20000
Collins-Iuka complex, occasionally floodedCu7111570625m4s8ky08319951:12000
Collins-Iuka complex, 0 to 4 percent slopes, rarely floodedCo87015973321qm4vky60219721:12000
Collins-Iuka complex, 0 to 2 percent slopes, occasionally floodedCu1489022322322dxthky61019681:12000
Collins-Iuka complex, 0 to 2 percent slopes, frequently floodedCi807422323332dxxrky61019681:12000
Iuka sandy loam, occasionally floodedIu662570526m4p2ky61119911:20000
Iuka-Mantachie complex, frequently floodedIUA606217257111vxr3la01119931:24000
Iuka fine sandy loam, 0 to 1 percent slopes, frequently floodedIB141117256532ynxsla02119851:24000
Iuka-Dela complex, 0 to 1 percent slopes, frequently floodedIo274355693242ynxtla02719861:20000
Iuka and Ochlockonee soils, frequently floodedIU1478417245411vwjcla03119861:24000
Iuka-Dela complex, 0 to 1 percent slopes, frequently floodedIUA440525711232ynxtla06119911:24000
Guyton-Iuka association, frequently floodedGYA76803190303121w83la08519911:24000
Iuka-Dela complex, 0 to 1 percent slopes, frequently floodedID3953217253442ynxtla11119921:24000
Iuka-Dela complex, 0 to 1 percent slopes, frequently floodedIU47985703522ynxtla11919891:24000
Mantachie, Bibb, and Iuka soils (kirkville, kinston, iuka)Mn31002332011c4h1ms02319631:15840
Bibb-Iuka complex, 0 to 2 percent slopes, frequently floodedBiA1811026421632rrxqms04120121:24000
Collins and Iuka soilsCs4139568147m26bms08519611:20000
Iuka soilsIu780333178c5ppms09519631:15840
Iuka fine sandy loamIu1804333246c5rwms09719711:20000
Iuka and Ochlockonee soilsIo4820333644c65qms11319651:15840
Iuka and Ochlockonee soilsIo2563333699c67hms11519691:20000
Iuka fine sandy loam, 0 to 2 percent slopes, occasionally floodedIu91473338042w6ffms11719951:24000
Bibb and Iuka sandy loams, frequently floodedBI2601333796c6bmms11719951:24000
Iuka soilsIk1608334198c6rlms13919631:15840
Iuka soils, local alluviumIu541334199c6rmms13919631:15840
Ochlockonee-iuka soils, (jena-kirkville)Oc9103334287c6vgms14719651:20000
Bibb-Iuka complex, 0 to 1 percent slopes, frequently floodedBkA3909624034302shs8ms15320081:24000
Iuka loam, 0 to 2 percent slopes, occasionally floodedIk1008125453492qsg9tn00520111:12000
Iuka silt loam, occasionally floodedIu7282327218bzhftn02319891:24000
Iuka fine sandy loam, 0 to 2 percent slopes, occasionally floodedEk34713273052w6fftn03920081:24000
Iuka silt loam, occasionally floodedIu13505327468bzrhtn06919961:24000
Collins loam, local alluvium (Iuka)Cg5378327535bztntn07119611:15840
Collins fine sandy loam (Iuka)Cf1496327534bztmtn07119611:15840
Collins silt loam (Iuka)Ch1487327536bztptn07119611:15840
Hymon fine sandy loam, local alluvium phase (Iuka)Hc5435327748c01jtn07719551:20000
Hymon fine sandy loam (Iuka)Hb593327747c01htn07719551:20000
Iuka loam, 0 to 2 percent slopes, occasionally floodedIk1032225452642qs88tn07920121:12000
Iuka fine sandy loam, 0 to 2 percent slopes, occasionally floodedIu239023279612w6fftn10919941:20000
Iuka fine sandy loamIu6356567204m16xtn11319741:20000
Iuka soils, frequently floodedIu26096374425dkm7tx61119801:20000
Iuka fine sandy loam, local alluvium, 0 to 4 percent slopesIu28024535692nc4dva15319851:15840
Iuka fine sandy loam, local alluvium, 0 to 4 percent slopesIu307212052841f0va17919701:15840

Map of Series Extent

Approximate geographic distribution of the IUKA 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 .