Official Series Description


Lab Data Summary

Aggregate lab data for the BONNIE soil series. This aggregation is based on all pedons with a current taxon name of BONNIE, 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 BONNIE 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
11384IL1210541984IL121054Bonnie3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5525056,-88.7403111
11385IL1910111985IL191011Bonnie2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3253778,-88.488075
11385IL1910121985IL191012Bonnie2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3454028,-88.6200028
11385IL1910141985IL191014Bonnie2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3845528,-88.6619333
11385IL1910171985IL191017Bonnie2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3484333,-88.4848167
11385IL1910241985IL191024Bonnie2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4011278,-88.5055778
11386IL1910051986IL191005Bonnie2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5917278,-88.3921972
11388P049085IL191023Bonnie7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4844437,-88.6783371
11308N0149S07IL191001Bonnie7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4700444,-88.6508917
11340A1496S1963IL191001Bonnie5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4713898,-88.6511078
114AMR76101976IN109010Bonnie2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4775,-86.6287778
114ACL77041977IN021004Bonnie2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3444444,-87.1540444
114AGN79071979IN055007Bonnie3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0968278,-87.1123111
114B79IL1450141979IL145014Bonnie2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.9536378,-89.4203059
114BWS80192017IN175001Bonnie3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7587083,-85.9953222
114B88P042887IN143007Bonnie6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8050003,-85.7527771
115APK78021978IN125002Bonnie3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2798528,-87.2700111
115ADA67062017IN027001Bonnie2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.761481,-86.998962
120A67KY-107-00467KY-107-004Bonnie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.3018667,-87.5891444
120A68KY-107-01368KY-107-013Bonnie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.287571,-87.7250214
120A95P020393IL181075EBonnie6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.3460279,-89.064219
120A10N1294S2010KY149056Bonnie5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5941756,-87.3404884
120A10N1295S2010KY149057Bonnie5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.594274,-87.340738
120A10N1296S2010KY149058Bonnie5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5942838,-87.3404662
120A10N1297S2010KY149059Bonnie5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5942838,-87.3404889
120A10N1298S2010KY149060Bonnie5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5946443,-87.3404905
120A10N1299S2010KY149061Bonnie5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5943376,-87.3405571
120A10N1300S2010KY149062Bonnie5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5943558,-87.3405005
120A10N1302S2010KY149064Bonnie5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5944459,-87.3405236
120A10N1303S2010KY149065Bonnie5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5946443,-87.3404905
120BMT80012017IN101001Bonnie3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6473888,-86.8510667
120B93P0761S1993IN123016Bonnie6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1127777,-86.7388916
120B95P0210S1994IN123003Bonnie6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.209446,-86.7311096
120CLW80011980IN093001Bonnie3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.98825,-86.5137722
n/a85IL1910191985IL191019Bonnie2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a85IL1910211985IL191021Bonnie2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a85IL1910251985IL191025Bonnie2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a82P015381IL191002Bonnie6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a83KY-155-00883KY-155-008Bonnie3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a89KY-071-00289KY-071-002Bonnie4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a91P102191IL055027Bonnie7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BONNIE 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 BONNIE 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 BONNIE 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 BONNIE 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.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with BONNIE 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 BONNIE 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 BONNIE 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 BONNIE, 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. IL-2010-09-01-11 | Franklin and Jefferson Counties - 2003

    Typical pattern of soils and parent material in the Bluford-Wynoose association (Soil Survey of Franklin and Jefferson Counties, Illinois; 2003).

  2. IL-2010-09-01-12 | Franklin and Jefferson Counties - 2003

    Typical pattern of soils and parent material in the Colp-Hurst-Okaw association (Soil Survey of Franklin and Jefferson Counties, Illinois; 2003).

  3. IL-2010-09-01-14 | Franklin and Jefferson Counties - 2003

    Typical pattern of soils and parent material in the Grantsburg-Zanesville association (Soil Survey of Franklin and Jefferson Counties, Illinois; 2003).

  4. IL-2010-09-01-15 | Franklin and Jefferson Counties - 2003

    Typical pattern of soils and parent material in the Wynoose, bench-Rend-Bluford, bench, association (Soil Survey of Franklin and Jefferson Counties, Illinois; 2003).

  5. IL-2010-09-09-05 | Wayne County -

    Typical pattern of soils and parent material in the Bonnie-Belknap association (Soil Survey of Wayne County, Illinois).

  6. IL-2011-08-04-17 | Hamilton County - 1986

    Pattern of soils and parent material in the Belknap-Bonnie association (Soil Survey of Hamilton County, Illinois; 1986).

  7. IL-2011-08-04-84 | Perry County - 1988

    Typical pattern of soils and parent material in the Hurst-Okaw-Colp association (Soil Survey of Perry County, Illinois; 1988).

  8. IL-2011-08-04-85 | Perry County - 1988

    Typical pattern of soils and parent material in the Stoy-Hosmer association (Soil Survey of Perry County, Illinois; 1988).

  9. IL-2011-08-04-86 | Perry County - 1988

    Typical pattern of soils and parent material in the Bluford-Wynoose-Ava association (Soil Survey of Perry County, Illinois; 1988).

  10. KY-2012-01-31-29 | Knox County and Eastern Part of Whitley County - May 1988

    Pattern of soils, topography, and underlying material in the Stendal-Shelocta map unit (Soil Survey of Knox County and Eastern Part of Whitley County, Kentucky; May 1988).

  11. KY-2012-01-31-30 | Knox County and Eastern Part of Whitley County - May 1988

    Pattern of soils, topography, and underlying material in the Allegheny-Huntington-Newark map unit (Soil Survey of Knox County and Eastern Part of Whitley County, Kentucky; May 1988).

  12. KY-2012-01-31-31 | Knox County and Eastern Part of Whitley County - May 1988

    Pattern of soils, topography, and underlying material in the Allegheny-Cotaco-Huntington map unit (Soil Survey of Knox County and Eastern Part of Whitley County, Kentucky; May 1988).

Map Units

Map units containing BONNIE 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
Bonnie silt loam, 0 to 2 percent slopes, occasionally flooded8108A57386018452tbrwil00320021:12000
Bonnie and Petrolia soils, undrained, 0 to 2 percent slopes, frequently flooded1843A786603218n7pnil00320021:12000
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded3108A140601844n68bil00320021:12000
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded3108A847621092042tbrril02519931:12000
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded3108A47551754102tbrril04719671:15840
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded3108A144538092522tbrril05520051:12000
Bonnie silt loam, undrained, 0 to 2 percent slopes, frequently flooded1108A31818092432ytszil05520051:12000
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded3108A9542115822tbrril05919661:20000
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded3108A222901751142tbrril06519821:15840
Bonnie silt loam, 0 to 2 percent slopes, occasionally flooded8108A3547140352vp3jil06920031:12000
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded3108A116713980ryymil06920031:12000
Bonnie and Petrolia soils, undrained, 0 to 2 percent slopes, frequently flooded1843A112713972ryycil06920031:12000
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded3108A521415378752tbrril07720061:12000
Bonnie silt loam, 0 to 2 percent slopes, occasionally flooded8108A300515380962tbrwil07720061:12000
Bonnie and Petrolia soils, undrained, 0 to 2 percent slopes, frequently flooded1843A137715408661nqdcil07720061:12000
Bonnie silt loam, undrained, 0 to 2 percent slopes, frequently flooded1108A2416119282ytszil07720061:12000
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded3108A1183915405022tbrril08120051:12000
Bonnie silt loam, undrained, 0 to 2 percent slopes, frequently flooded1108A220315404992ytszil08120051:12000
Bonnie and Petrolia soils, undrained, 0 to 2 percent slopes, frequently flooded1843A5097817765wfyjil08720051:12000
Bonnie silt loam, 0 to 2 percent slopes, occasionally flooded8108A411611461902vp3jil08720051:12000
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded3108A1951114618817gptil08720051:12000
Bonnie silt loam, 0 to 2 percent slopes, occasionally flooded8108A12031767642tbrwil10119521:42240
Bonnie silt loam, sodic, 0 to 2 percent slopes, frequently flooded3108T308120274282tbs4il12120081:12000
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded3108A3120275822tbrril12120081:12000
Bonnie silt loam, 0 to 2 percent slopes, occasionally flooded8108A60348081332vp3jil12720041:12000
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded3108A1146808076w3vzil12720041:12000
Bonnie and Petrolia soils, undrained, 0 to 2 percent slopes, frequently flooded1843A611808068w3vqil12720041:12000
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded, long duration3108L92808077w3w0il12720041:12000
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded3108A2134014054312tbrril14520051:12000
Bonnie silt loam, undrained, 0 to 2 percent slopes, frequently flooded1108A144514061562ytszil14520051:12000
Bonnie silt loam, 0 to 2 percent slopes, occasionally flooded8108A27976068142vp3jil15120031:12000
Bonnie and Petrolia soils, undrained, 0 to 2 percent slopes, frequently flooded1843A167608293ndzcil15120031:12000
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded3108A152606813ncfmil15120031:12000
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded, long duration3108L40789692vhqyil15120031:12000
Bonnie silt loam, 0 to 2 percent slopes, occasionally flooded8108A52727490112vp3jil15320041:12000
Bonnie and Petrolia soils, undrained, 0 to 2 percent slopes, frequently flooded1843A4147748936t4b7il15320041:12000
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded3108A1025748947t4blil15320041:12000
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded3108A891020268232tbrril15919671:12000
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded3108A129631788512tbrril16519741:15840
Bonnie silt loam, undrained, 0 to 2 percent slopes, frequently flooded1108A7221789102ytszil16519741:15840
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded3108A70311796722tbrril18519621:20000
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded3108A11315289852tbrril18920061:12000
Bonnie silt loam, sodic, 0 to 2 percent slopes, frequently flooded3108T6967622313942tbs4il19120081:12000
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded3108A196420250952tbrril19120081:12000
Bonnie silt loam, sodic, undrained, 0 to 2 percent slopes, frequently flooded1108T1056202509325z8lil19120081:12000
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded3108A1786415439352tbrril19320061:12000
Bonnie silt loam, 0 to 2 percent slopes, frequently flooded3108A681214780802tbrril19920071:12000
Bonnie silt loam, undrained, 0 to 2 percent slopes, frequently flooded1108A62614782282ytszil19920071:12000
Bonnie and Petrolia soils, undrained, 0 to 2 percent slopes, frequently flooded1843A4817095771vcynil19920071:12000
Bonnie silt loam, 0 to 1 percent slopes, frequently flooded, very brief durationBodAV30212023066sj0in00520021:12000
Bonnie silt loam, 0 to 1 percent slopes, occasionally flooded, very brief durationBodAW383210761729rin01920011:12000
Bonnie silt loam, frequently floodedBo43411595945c26in02119801:15840
Bonnie silt loam, 0 to 2 percent slopes, frequently floodedBo20421629332tbrrin02719691:20000
Bonnie silt loam, frequently floodedBo6026535618kzc0in03719781:15840
Bonnie silt loam, 0 to 2 percent slopes, frequently floodedBo56231601112tbrrin05119861:15840
Bonnie silt loam, pondedBp10631601125clxin05119861:15840
Bonnie silt loam, frequently floodedBo75531615255f2hin05519841:15840
Bonnie silt loam, 0 to 1 percent slopes, frequently flooded, very brief durationBodAV14620316nth6in07119851:15840
Bonnie silt loam, 0 to 1 percent slopes, rarely floodedBodAQ10524279282mhg8in07920101:12000
Bonnie silt loam, 0 to 1 percent slopes, frequently flooded, brief durationBodAH9582027132261dcin09319821:15840
Bonnie silt loam, 0 to 1 percent slopes, occasionally flooded, very brief durationBodAW81417081171vbfkin10119841:15840
Bonnie silt loam, 0 to 1 percent slopes, frequently flooded, brief durationBodAH29517081161vbfjin10119841:15840
Bonnie silt loam, frequently floodedBo1314535519kz7tin10519791:15840
Bonnie silt loamBo3741631985gtgin10919791:15840
Bonnie silt loam, 0 to 1 percent slopes, frequently flooded, very brief durationBodAV3501659055kmsin11919971:12000
Bonnie silt loam, 0 to 1 percent slopes, frequently flooded, brief durationBodAH373535706kzfvin12319971:12000
Bonnie silt loam, ponded, 0 to 1 percent slopes, frequently flooded, brief durationBodAM29535707kzfwin12319971:12000
Bonnie silt loam, 0 to 2 percent slopes, frequently floodedBo45931618962tbrrin12519831:15840
Bonnie silt loam, pondedBp14791618975fghin12519831:15840
Bonnie silt loam, 0 to 1 percent slopes, frequently flooded, brief durationBodAH31621656045kb2in14319951:12000
Bonnie silt loam, 0 to 1 percent slopes, occasionally flooded, very brief durationBodAW8551656055kb3in14319951:12000
Bonnie silt loam, frequently flooded, brief durationBo85817177391vnfyin14719661:15840
Bonnie silt loamBo8861627355gbjin16319721:15840
Bonnie silt loam, 0 to 2 percent slopes, frequently floodedBn94141599452tbrrin17319761:15840
Bonnie silt loam, frequently floodedBo1078535461kz5yin17519841:15840
Bonnie silt loam, 0 to 2 percent slopes, occasionally floodeduBonA154125838952vp3jky03320051:12000
Bonnie silt loam, 0 to 2 percent slopes, occasionally floodeduBonA378425268252vp3jky04719771:20000
Bonnie silt loam, occasionally floodedBo447552514ljy1ky05119941:24000
Bonnie silt loam, 0 to 2 percent slopes, occasionally floodeduBonA92325839032vp3jky05519851:20000
Bonnie silt loam, 0 to 2 percent slopes, occasionally floodeduBonA12305496442vp3jky08519671:20000
Bonnie silt loam, 0 to 2 percent slopes, occasionally floodeduBonA48615492492vp3jky10119641:15840
Bonnie silt loam, 0 to 2 percent slopes, occasionally floodeduBonA1383325268282vp3jky10719741:12000
Bonnie and Karnak soils, 0 to 1 percent slopes, pondeduBKp67425492642yq54ky10719741:12000
Bonnie silt loam, 0 to 2 percent slopes, occasionally floodeduBonA9355486922vp3jky14119721:20000
Bonnie silt loam, 0 to 2 percent slopes, occasionally floodeduBonA78085512392vp3jky18319831:20000
Bonnie silt loam, 0 to 1 percent slopes, pondeduBop7635512402zs4rky18319831:20000
Bonnie silt loamBo1685550387lgqfky60519751:20000
Bonnie silt loam, 0 to 2 percent slopes, occasionally floodeduBonA162695494312vp3jky61519711:20000
Bonnie silt loam, terraceBo428552544ljz0ky62019791:20000
Bonnie silt loam, frequently floodedBo2833552212ljm9ky62719841:20000
Bonnie silt loamBn3045552249ljnhky62819731:20000
Bonnie silt loam, terraceBo745552250ljnjky62819731:20000
Bonnie silt loam, 0 to 2 percent slopes, occasionally floodeduBonA98165511292vp3jky63119761:20000
Bonnie silt loam, 0 to 1 percent slopes, pondeduBop36185511302zs4rky63119761:20000
Bonnie silt loam, 0 to 2 percent slopes, occasionally floodeduBonA387625268382vp3jky63519781:20000
Bonnie silt loam, occasionally floodedBo893552109ljhzky63819891:24000
Bonnie silt loamBo101014787531lmrqky64519711:20000
Bonnie silt loam, 0 to 2 percent slopes, frequently floodedBne1AF96024533572nbxkoh16319981:15840
Bonnie silt loam, ponded, 0 to 2 percent slopesBne1AP33724533582nbxloh16319981:15840

Map of Series Extent

Approximate geographic distribution of the BONNIE 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 .