Official Series Description


Lab Data Summary

Aggregate lab data for the OCILLA soil series. This aggregation is based on all pedons with a current taxon name of OCILLA, 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 OCILLA 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
133AS37_0261978-FL073-S37_026Ocilla3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.5010281,-84.3680573
133AS40_0201985-FL079-S40_020Ocilla3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.3972416,-83.3983078
133AS89AL-105-289AL105002-pgmOcilla3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.5936111,-87.2619444
138S12_0101979-FL023-S12_010Ocilla3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.0825386,-82.5925827
138S12_0121979-FL023-S12_012Ocilla3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.2852383,-82.7350693
138S63_0081986-FL125-S63_008Ocilla3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.9777241,-82.5494385
152AS23_0241990-FL045-S23_024Ocilla3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.9725037,-85.0789413
152AS62_0151990-FL123-S62_015Ocilla3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.1383305,-83.5083313
153AS04_0021985-FL007-S04_002Ocilla3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.0466442,-82.1882782
153AS45_0231985-FL089-S45_023Ocilla3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.6172142,-81.7674408
153AS02_0061988-FL003-S02_006Ocilla3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.2430859,-82.1469193
153AS02_0101988-FL003-S02_010Ocilla3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.3405781,-82.1222992
153AS24_0131989-FL047-S24_013Ocillan/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.6041698,-83.0286102
153AS10_0151994-FL019-S10_015Ocilla3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.1100941,-81.9735947
153A00P042499GA103053Ocilla6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.4268608,-81.2839737
153A00P044599GA299009Ocilla6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.3933334,-82.5597229

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the OCILLA 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 OCILLA 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 OCILLA 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 OCILLA 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 OCILLA 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 OCILLA 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 OCILLA 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 OCILLA, 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. FL-2010-03-08-05 | Baker County - April 1996

    Pattern of soils and parent material in the Pelham-Pantego-Ocilla and Osier-Surrency-Mulat general soil map units (Soil Survey of Baker County, Florida; 1996).

  2. FL-2011-05-31-01 | Bradford County - 1991

    Pattern of soils on a gently rolling landscape near major drainageways (Soil Survey of Bradford County, Florida; 1991).

  3. FL-2011-05-31-02 | Bradford County - 1991

    Pattern of soils in a flatwoods landscape that includes slightly elevated areas, depressions, and flood plains (Soil Survey of Bradford County, Florida; 1991).

  4. FL-2012-04-26-16 | Union County - October 1991

    Pattern of soils on a gently rolling landscape near major drainageways (Soil Survey of Union County, Florida; October 1991).

  5. FL-2012-04-26-17 | Union County - October 1991

    Pattern of soils on a flatwoods landscape that includes slightly elevated areas, depressions, and flood plains (Soil Survey of Union County, Florida; October 1991).

Map Units

Map units containing OCILLA 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
Ocilla loamy fine sand, 0 to 2 percent slopesOcA6980328246c0klal00520011:24000
Lynchburg-Ocilla complex, 0 to 2 percent slopes, rarely floodedLyA9857328422c0r8al01119861:20000
Ocilla loamy fine sand, 0 to 2 percent slopes, rarely floodedOcA49273284292v5ljal01119861:20000
Ocilla-Pelham complex, gently undulatingOdB4180114756017j42al02520041:24000
Pelham-Ocilla complex, 0 to 2 percent slopes, rarely floodedPoA795014138442tl1mal04120051:24000
Ocilla-Albany complex, 0 to 2 percent slopesOiA4137330416c2tlal06920021:24000
Ocilla loamy fine sand, 0 to 2 percent slopesOcA84025149272qdhhal08520111:24000
Ocilla loamy fine sand, 0 to 2 percent slopes, rarely floodedOcA36143304792v5ljal08719971:24000
Pelham-Ocilla complex, 0 to 2 percent slopes, rarely floodedPoA20603304842tl1mal08719971:24000
Ocilla-Jedburg complex, 1 to 3 percent slopesOcB1430331247c3pdal10519961:24000
Ocilla loamy fine sand, 0 to 2 percent slopes, rarely floodedOcA42403313332v5ljal11319971:24000
Ocilla, Alapaha, and Mandarin soils, occasionally flooded84166320790brt2fl00119821:15840
Ocilla fine sand, 0 to 3 percent slopes321273514448901khjcfl00319911:20000
Ocilla fine sand, 0 to 5 percent slopes32903631615p67pfl00719881:15840
Ocilla loamy fine sand, 0 to 5 percent slopes435551328294g6tfl01919861:24000
Ocilla fine sand, 0 to 5 percent slopes4012520797462vrtlfl02319811:24000
Albany-Ocilla-Chipley complex, 0 to 5 percent slopes101422514218171jqj2fl03920061:12000
Ocilla sand, 0 to 5 percent slopes4389113815832wyxwfl03920061:12000
Goldsboro-Ocilla complex, 5 to 8 percent slopes7257713816111hcp3fl03920061:12000
Ocilla loamy fine sand, overwash, occasionally flooded26287614727471lfhzfl04519971:24000
Ocilla loamy fine sand, 0 to 5 percent slopes243550114882017kfqfl04719951:24000
Ocilla fine sand32437514544411ktggfl07319891:20000
Ocilla sand, 0 to 5 percent slopes301498013803142wyxwfl07919881:15840
Ocilla fine sand, 0 to 5 percent slopes2319151329104g9ffl08919891:15840
Ocilla-Albany-Blanton complex, 0 to 5 percent slopes25583102332113bvcfl12120031:24000
Ocilla sand22113014252161jv1qfl12319981:24000
Ocilla fine sand, 0 to 5 percent slopes3467014145951jh03fl12519891:15840
Ocilla sand, 0 to 5 percent slopes3048013990571hytwfl12919881:24000
Albany-Ocilla complex, 0 to 5 percent slopes, occasionally flooded54734023984732lht3fl13320091:12000
Ocilla-Leefield complex, 0 to 5 percent slopes57556023984762lht6fl13320091:12000
Albany-Ocilla complex, 5 to 8 percent slopes56146023984752lht5fl13320091:12000
Ocilla loamy sand, 0 to 2 percent slopesOcA37013246002wywtga03319821:20000
Ocilla loamy fine sand, 0 to 2 percent slopesOcA81257542712wyxxga08720011:24000
Ocilla loamy sand, 0 to 2 percent slopesOhA14353246542wywtga09519651:20000
Ocilla loamy sand, 0 to 2 percent slopesOdA86503247762wywtga10719931:20000
Ocilla loamy fine sand, 0 to 2 percent slopes, frequently floodedOcA75053365852wyxyga13120001:12000
Ocilla loamy sand, 0 to 2 percent slopesOhA61453248212wywtga16519661:20000
Ocilla loamy sand, 0 to 2 percent slopesOcA608025803852wywtga25120111:24000
Ocilla loamy sand, 0 to 2 percent slopesOcA53024253992mdtpga25920091:12000
Ocilla loamy sand, 0 to 2 percent slopesOc65603249432wywtga27719791:20000
Ocilla loamy sand, occasionally floodedOf720324944bx42ga27719791:20000
Ocilla-Urban land complexOnA509324945bx43ga27719791:20000
Ocilla loamy sand, 0 to 2 percent slopesOcA92024554282wywtga30720091:12000
Ocilla loamy sand, 0 to 2 percent slopesOcA56503251242wywtga32119851:20000
Ocilla loamy sand, 0 to 2 percent slopesOcA1021531162162ybc4ga60119691:20000
Ocilla loamy sand, 0 to 2 percent slopesOhA186973252122wywtga60819651:20000
Ocilla loamy sand, 0 to 2 percent slopesBa274231162722ybcgga60919671:20000
Eulonia and Ocilla soils, 0 to 3 percent slopesEOA25026867902rz9cga61120121:24000
Ocilla loamy sand, 0 to 2 percent slopesOd79903254432wywtga61219751:20000
Ocilla complexOj2920512538946gtga61319691:20000
Ocilla-Urban land complexOjc614012539046gvga61319691:20000
Ocilla loamy sand, 0 to 2 percent slopesOc67203254922wywtga61519811:20000
Ocilla loamy fine sand, 0 to 2 percent slopes, frequently floodedOn50003255652wyxyga62719701:20000
Ocilla loamy sand, 0 to 2 percent slopesOh27803255642wywtga62719701:20000
Ocilla loamy sand, 0 to 2 percent slopes, rarely floodedOc193012655547pfga63019951:20000
Ocilla loamy sand, 0 to 2 percent slopesOc3873256032wywtga63119781:20000
Ocilla loamy sand, 0 to 2 percent slopesOd6003257892wywtga63419801:20000
Ocilla loamy sand, 0 to 2 percent slopesOcA36033258602wywtga63819871:20000
Ocilla loamy sand, 0 to 2 percent slopes, occasionally floodedOoA130325861by2nga63819871:20000
Ocilla loamy sand, 0 to 3 percent slopesOcA62526390772rj40ga63920121:24000
Ocilla loamy sand, 0 to 2 percent slopesOd69603259672wywtga64119861:20000
Ocilla loamy sand, 0 to 2 percent slopesOc29653260072wywtga64319741:20000
Ocilla loamy fine sandOc2811412581746xmga64419801:20000
Ocilla loamy sand, 0 to 2 percent slopesOh125853260372wywtga64619711:20000
Ocilla loamy sand, 0 to 2 percent slopesOh122203260622wywtga64719701:20000
Ocilla loamy sand, 0 to 2 percent slopesOd61453263622wywtga65419791:20000
Ocilla loamy sand, 0 to 2 percent slopesOcA128516051021qw7hga65820051:24000
Ocilla loamy sand, 0 to 2 percent slopesOc20833324012x54gms04519791:20000
Ocilla loamy sand, 0 to 2 percent slopesOc47333324392x54gms04719711:20000
Ocilla loamy sand, 0 to 2 percent slopes, occasionally flooded5557963325902x54fms05919971:24000
Ocilla loamy sandOc51261155053w5znc01719831:24000
Ocilla loamy fine sand, 0 to 3 percent slopesOcA4171140543tp5nc13119881:24000
Ocilla loamy fine sand, 0 to 4 percent slopesOcB180151143373tz9nc14719691:15840
Ocilla loamy sand, 0 to 2 percent slopesOcA115614804971lpkznc16520061:12000
Ocilla fine sand, 0 to 2 percent slopesOcA77411323864frjsc00519891:20000
Ocilla sand, 0 to 3 percent slopesOcA60151380894mphsc00919971:24000
Ocilla loamy fine sandOc160001319654f9ysc01519741:20000
Ocilla loamy sandOc31341322334fllsc02719721:20000
Ocilla loamy sand45299681322824fn5sc02919801:20000
Ocilla sand, 0 to 2 percent slopesOcA64001298184c2psc03519851:20000
Ocilla fine sand, 0 to 2 percent slopesOcA238801301184cdcsc04919901:20000
Albany-Pelham-Ocilla associationAC127691325204fwvsc05319751:20000
Ocilla loamy fine sandOc126361325654fy9sc05319751:20000
Ocilla sand, 0 to 4 percent slopesOcB9991306554cypsc06919951:24000
Ocilla loamy sand, 0 to 2 percent slopesOcA98191309024d6nsc07519851:20000
Durham loamy sand, thick surface, 2 to 6 percent slopesDyB3031311724dhcsc08119601:20000
Ocilla variant loamy sandOd16131317654f3hsc61519811:20000
Ocilla loamy sand, 0 to 2 percent slopesOcA14881313574dpbsc69619881:15840
Ocilla loamy sand, 0 to 6 percent slopes20B1802705283rnx2va17519961:24000
Ocilla loamy sand, 6 to 10 percent slopes20C230705284rnx3va17519961:24000
Ocilla loamy sand, 0 to 6 percent slopes21B1323917231001vv0wva18320061:24000

Map of Series Extent

Approximate geographic distribution of the OCILLA 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 .