Official Series Description


Lab Data Summary

Aggregate lab data for the BOHANNON soil series. This aggregation is based on all pedons with a current taxon name of BOHANNON, 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 BOHANNON 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
4A72C0053S1972OR011004BOHANNON7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.466053,-124.1614685
4A72C0054S1972OR011007BOHANNON7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.6020241,-124.0914688

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BOHANNON 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 BOHANNON 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 BOHANNON 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 BOHANNON 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 hills figure.

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

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with BOHANNON 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 BOHANNON 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 BOHANNON 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 hills figure.

Click the image to view it full size.

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 BOHANNON, 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 BOHANNON 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
Preacher-Bohannon-Slickrock complex, 35 to 60 percent slopes13614629854352vwzor00320041:24000
Bohannon-Preacher complex, 30 to 60 percent slopes2310946852632vqfor00320041:24000
Preacher-Bohannon complex, 5 to 35 percent slopes1357013854362vx0or00320041:24000
Digger-Bohannon complex, 5 to 30 percent slopes553281854402vx4or00320041:24000
Bohannon-Preacher complex, 60 to 90 percent slopes242432854332vwxor00320041:24000
Preacher-Blachly-Bohannon complex, 5 to 30 percent slopes1341470854392vx3or00320041:24000
Milbury-Bohannon-Umpcoos association, 50 to 80 percent slopes38F1253046119221nyor01119831:20000
Preacher-Bohannon loams, 60 to 90 percent slopes46F1058236120421pbor01119831:20000
Preacher-Bohannon loams, 30 to 60 percent slopes46E769716120321p9or01119831:20000
Preacher-Bohannon loams, 3 to 30 percent slopes46D268836120221p8or01119831:20000
Bohannon-Milbury complex, 30 to 50 percent slopes6E15676125221qwor01119831:20000
Digger-Preacher-Bohannon complex, warm, 30 to 60 percent south slopes85F784465554266nor01519951:24000
Preacher-Digger-Bohannon complex, 30 to 60 percent north slopes200F62126516425t2or01519951:24000
Digger-Preacher-Bohannon complex, 60 to 90 percent north slopes84G24065551266kor01519951:24000
Digger-Preacher-Bohannon complex, warm, 60 to 90 percent north slopes86G20065557266ror01519951:24000
Preacher-Digger-Bohannon complex, warm, 30 to 60 percent north slopes201F1236516625t4or01519951:24000
Bohannon gravelly loam, 50 to 75 percent slopes10F151726230022tpor05319771:20000
Bohannon gravelly loam, 25 to 50 percent slopes10E40096229922tnor05319771:20000
Bohannon gravelly loam, 3 to 25 percent slopes10D21526229822tmor05319771:20000
Bohannon-Preacher complex, 30 to 60 percent slopes310F90114045921j4lfor05319771:20000
Preacher-Bohannon complex, 35 to 60 percent slopes176E25836712727vdor05720061:24000
Preacher-Bohannon complex, 5 to 35 percent slopes176D676712627vcor05720061:24000
Preacher-Bohannon complex, 35 to 60 percent slopes176E1457271118027vdor07119671:24000
Bohannon gravelly loam, dissected, 50 to 90 percent slopesBmG3954814259671jvtyor60119681:20000
Bohannon-Slickrock gravelly loams, dissected, 37 to 50 percent slopesBtF1896914259771jvv8or60119681:20000
Bohannon gravelly loam, dissected, 37 to 50 percent slopesBmF1064214259661jvtxor60119681:20000
Bohannon-Slickrock gravelly loams, 35 to 50 percent slopesBsF658714259741jvv5or60119681:20000
Bohannon gravelly loam, 50 to 75 percent slopesBlG574614259641jvtvor60119681:20000
Bohannon gravelly loam, 35 to 50 percent slopesBlF569814259631jvttor60119681:20000
Bohannon-Slickrock gravelly loams, dissected, 25 to 37 percent slopesBtE273014259761jvv7or60119681:20000
Bohannon gravelly loam, ridge, 25 to 37 percent slopesBnE264514259681jvtzor60119681:20000
Bohannon loam, ridge, 5 to 25 percent slopesBkD251414259611jvtror60119681:20000
Bohannon-Slickrock gravelly loams, 25 to 35 percent slopesBsE249214259731jvv4or60119681:20000
Bohannon-Slickrock gravelly loams, dissected, 50 to 75 percent slopesBtG229214259781jvv9or60119681:20000
Bohannon gravelly loam, ridge, 37 to 50 percent slopesBnF109614259691jvv0or60119681:20000
Bohannon rocky loam, 75 to 100 percent slopesBoG90014259701jvv1or60119681:20000
Bohannon gravelly loam, 5 to 35 percent slopesBlE78314259621jvtsor60119681:20000
Bohannon-Slickrock gravelly loams, 50 to 75 percent slopesBsG67814259751jvv6or60119681:20000
Bohannon gravelly loam, syenite substratum, dissected, 50 to 75 percent slopesBrG35314259721jvv3or60119681:20000
Bohannon gravelly loam, syenite substratum, 5 to 50 percent slopesBpF34414259711jvv2or60119681:20000
Bohannon gravelly loam, dissected, 25 to 37 percent slopesBmE27514259651jvtwor60119681:20000
Preacher-Bohannon-Slickrock complex, 50 to 75 percent slopes112G11111862581233ror63719811:20000
Bohannon gravelly loam, 50 to 90 percent slopes16H8927762637235kor63719811:20000
Bohannon gravelly loam, 25 to 50 percent slopes16F2637662636235jor63719811:20000
Bohannon gravelly loam, 3 to 25 percent slopes16D1680462635235hor63719811:20000
Bohannon-Preacher complex, 30 to 60 percent slopes310F145214215001jq5vor63719811:20000
Preacher-Bohannon-Slickrock complex, 35 to 60 percent slopes307F55314214991jq5tor63719811:20000
Bohannon-Preacher complex, 60 to 90 percent slopes315G49214215011jq5wor63719811:20000
Preacher-Bohannon complex, 5 to 35 percent slopes305E38714214971jq5ror63719811:20000
Digger-Bohannon complex, 5 to 30 percent slopes318E23514215031jq5yor63719811:20000
Preacher-Blachly-Bohannon complex, 5 to 30 percent slopes306E13814214981jq5sor63719811:20000
Preacher-Bohannon-Slickrock complex, 35 to 60 percent slopes50G881646471825bpor63819901:20000
Bohannon-Preacher complex, 60 to 90 percent slopes7H356006479125f1or63819901:20000
Preacher-Bohannon complex, 5 to 35 percent slopes49E228106471325bjor63819901:20000
Bohannon cobbly loam, 3 to 25 percent slopes15D2206426824w5or63919831:20000
Damewood-Bohannon-Umpcoos complex, 60 to 90 percent slopes49G970756689627lyor64919941:24000
Digger-Bohannon-Umpcoos complex, 60 to 90 percent slopes58G773766698427psor64919941:24000
Preacher-Bohannon-Xanadu complex, 30 to 60 percent slopes200F2804366550277sor64919941:24000
Bohannon-Preacher-Damewood complex, 60 to 90 percent slopes27G233636675427gcor64919941:24000
Preacher-Bohannon-Blachly complex, 30 to 70 percent slopes198F1888366537277cor64919941:24000
Preacher-Bohannon-Digger complex, 60 to 90 percent slopes199G1382466538277dor64919941:24000
Damewood-Bohannon-Umpcoos complex, 30 to 60 percent slopes49F129496689527lxor64919941:24000
Preacher-Bohannon complex, 3 to 30 percent slopes197E9588665322776or64919941:24000
Preacher-Bohannon complex, 30 to 60 percent slopes197F9139665332777or64919941:24000
Digger-Bohannon complex, 30 to 60 percent slopes57F75036697727pkor64919941:24000
Digger-Bohannon complex, 3 to 30 percent slopes57E42676697627pjor64919941:24000

Map of Series Extent

Approximate geographic distribution of the BOHANNON 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 .