Official Series Description


Lab Data Summary

Aggregate lab data for the BOONE soil series. This aggregation is based on all pedons with a current taxon name of BOONE, 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 BOONE were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
104UMN1059S1970MN1311059Boone3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.4064407,-93.1965714
105X3-210-1S1986IA005003Boone3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.4642237,-91.5465228
105X3-210-2S1986IA005005Boone3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.3038566,-91.4259891
105X3-210F-6S1986IA005006Boone3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.2410591,-91.382744
105X3-841G-1S1988IA005014Boone3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.2788434,-91.3920688
105X3-841G-2S1988IA005015Boone3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.2757977,-91.3805778
8991P0483S1990WI019036Boone5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.5038872,-90.7808304

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the BOONE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the BOONE series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the BOONE 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 .

Click the image to view it full size.

Click the image to view it full size.

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

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with BOONE share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the BOONE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the BOONE 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 .

Click the image to view it full size.

Click the image to view it full size.

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

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with BOONE, 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. IA-2010-09-02-02 | Allalmakee County - 1998

    Typical pattern of soils and parent material in the Fayette-Nordness-Dubuque association (Soil Survey of Allamakee County, Iowa; 1998).

  2. IA-2010-09-09-26 | Winneshiek County - 2007

    Typical pattern of soils and parent material in the Fayette-Lacrescent-Village association (Soil Survey of Winneshiek County, Iowa; 2007).

  3. IA-2011-05-31-02 | Allamakee County - 1958

    Typical pattern of soils and parent material in the Fayette-Nordness-Dubuque association (Soil Survey of Allamakee County, Iowa; 1958).

  4. WI-2010-11-08-08 | Pepin County - 2002

    Typical pattern of soils and parent material in the Urne-Drammen and Markey-Farrington-Aldo associations (Soil Survey of Pepin County, Wisconsin; 2002).

  5. WI-2012-03-22-02 | Buffalo County - March 1962

    Soil associations and relief in Buffalo County. 1. Silty soils of the rolling limestone uplands and Steep stony and rocky land: Dubuque, Fayette, Steep stony and rocky land. 2. Loamy soils of the rolling to hilly sandstone uplands: Gale, Hixton. 3. Sandy soils of the rolling to hilly sandstone uplands: Boone, Hixton. 4. Sandy soils of stream terraces: Sparta, Plainfield. 5. Silty soils of stream terraces: Bertrand, Richwood. 6. Loamy terrace soils underlain by sand on stream terraces: Meridian, Tell. 7. Wet organic and mineral soils of bottom lands: Peat and Muck, Ettrick, Wallkill. 8. Soils of overflow bottom lands: Loamy alluvial lands, Marsh (Soil Survey of Bayfield County, WI; 1961).

  6. WI-2012-03-23-05 | Jackson County - 2001

    Relationship of soils, topography, and parent material in the Urne-Council-La Farge association (Soil Survey of Jackson County, WI; 2001).

  7. WI-2012-03-23-06 | Jackson County - 2001

    Relationship of soils, topography, and parent material in the Tarr-Boone-Rockdam association (Soil Survey of Jackson County, WI; 2001).

  8. WI-2012-03-23-12 | Juneau County - January 1991

    Typical pattern of soils and parent material in the Urne-La Farge-Rozetta association (Soil Survey of Juneau County, WI; 1991).

  9. WI-2012-03-23-23 | Monroe County - June 1984

    Relationship of soils and parent material in the Tarr-Boone-Impact map unit (Soil Survey of Monroe County, WI; 1984).

  10. WI-2012-03-23-26 | Monroe County - June 1984

    Relationship of soils and parent material in the Wyeville-Wautoma-Newson map unit (Soil Survey of Monroe County, WI; 1984).

  11. WI-2012-03-23-30 | Pepin County - March 1964

    Cross section showing the geology and the associated soils in Pepin County (Soil Survey of Pepin County, WI; 1964).

Map Units

Map units containing BOONE 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
Boone loamy sand, 25 to 40 percent slopes210G3393402408fhqxia00519921:15840
Rock outcrop-Boone complex, 20 to 70 percent slopes841G3025402569fhx3ia00519921:15840
Boone loamy sand, 18 to 25 percent slopes210F645402407fhqwia00519921:15840
Boone loamy sand, 9 to 18 percent slopes210E370402406fhqvia00519921:15840
Boone fine sandy loam, 18 to 40 percent slopes210G1699409289fqwwia12319711:15840
Boone-rock outcrop complex, 20 to 70 percent slopes841G379514003101j049ia19120051:12000
Boone loamy fine sand, 15 to 35 percent slopes397F51913868101hk2til09920061:12000
Boone loamy fine sand, 15 to 35 percent slopes397F45394216710mdhil10320041:12000
Boone loamy fine sand, 7 to 15 percent slopes397D19094216610mdgil10320041:12000
Boone loamy fine sand, 15 to 35 percent slopes397F272514790111ln11il14120051:12000
Boone loamy fine sand, 7 to 15 percent slopes397D81114790101ln10il14120051:12000
Boone loamy fine sand, 2 to 7 percent slopes397B23514790121ln12il14120051:12000
Boone loamy fine sand, 6 to 12 percent slopes81C1361396886f9zsmn03719801:15840
Boone loamy fine sand, 2 to 6 percent slopes81B999396885f9zrmn03719801:15840
Boone loamy fine sand, 12 to 40 percent slopes81E545396887f9ztmn03719801:15840
Chelsea and Boone loamy fine sands, 18 to 35 percent slopesCf95622167072ddnpmn04520081:12000
Chelsea and Boone loamy fine sands, 7 to 11 percent slopesCd55022167092ddnrmn04520081:12000
Chelsea and Boone loamy fine sands, 2 to 6 percent slopesCc47322167082ddnqmn04520081:12000
Chelsea and Boone loamy fine sands, 12 to 17 percent slopesCe34822167062ddnnmn04520081:12000
Boone sand, rocky, 20 to 70 percent slopes81F669398322fch3mn05519811:15840
Boone loamy fine sand, 6 to 18 percent slopes81D486429724gf52mn13119961:12000
Boone loamy fine sand, 18 to 25 percent slopes81E418429725gf53mn13119961:12000
Boone loamy fine sand, 1 to 6 percent slopes81B279429722gf50mn13119961:12000
Boone and Chelsea loamy fine sands, 6 to 12 percent slopesBhC24522162952dd7dmn15720081:12000
Boone loamy fine sand, 18 to 35 percent slopesBfE19322162962dd7fmn15720081:12000
Boone and Chelsea loamy fine sands, 12 to 18 percent slopesBhD13422162932dd7bmn15720081:12000
Boone and Chelsea loamy fine sands, 2 to 6 percent slopesBhB9122162942dd7cmn15720081:12000
Spinks-Boone-Sogn complex, rocky, 15 to 60 percent slopes831F978429096gdhtmn16919871:20000
Boone loamy fine sand, 2 to 6 percent slopes81B409429090gdhmmn16919871:20000
Boone loamy fine sand, 6 to 15 percent slopes81C297429091gdhnmn16919871:20000
Boone-Rock outcrop complex, 20 to 60 percent slopes8000367427808gc58ne02119781:20000
Boone-Rock outcrop complex, 25 to 45 percent slopesBpF2974422925g62rwi00119781:20000
Boone sand, 2 to 6 percent slopesBnB2112422922g62nwi00119781:20000
Boone sand, 6 to 12 percent slopesBnC1605422923g62pwi00119781:20000
Boone sand, 12 to 25 percent slopesBnD835422924g62qwi00119781:20000
Boone sand, 15 to 30 percent slopes233E2665256168320rb2wi01119601:20000
Boone sand, 6 to 15 percent slopes233C238825616821lmwxwi01119601:20000
Boone-Elevasil complex, 15 to 45 percent slopes, rocky1224F199125617562yt3hwi01119601:20000
Boone sand, 1 to 6 percent slopes233B94825616842fj7swi01119601:20000
Boone-Tarr sands, 15 to 50 percent slopes1233F1326394361lmytwi01119601:20000
Boone fine sand, 20 to 45 percent slopesBoE4728421499g4lrwi01719851:15840
Boone sand, 15 to 50 percent slopesBoF1306431844ghcgwi01919941:20000
Boone-Elevasil complex, 15 to 45 percent slopes, rockyBpF11794318452yt3hwi01919941:20000
Boone sand, 6 to 15 percent slopesBoC704431843ghcfwi01919941:20000
Boone loamy fine sand, 12 to 45 percent slopesBnE1265423254g6fcwi02119721:15840
Boone loamy fine sand, 6 to 12 percent slopesBnC392423253g6fbwi02119721:15840
Boone-Elevasil complex, 15 to 45 percent slopes, rocky1224F47024991672yt3hwi02319601:12000
Boone fine sand, 12 to 30 percent slopes201E347250393120rb1wi02319601:12000
Boone sand, 15 to 30 percent slopes233E79250394920rb2wi02319601:12000
Boone sand, 6 to 15 percent slopes233C130324983071lmwxwi03320031:15840
Boone-Elevasil complex, 15 to 45 percent slopes, rocky1224F60824991682yt3hwi03320031:15840
Boone-Tarr sands, 15 to 50 percent slopes1233F16524991711lmytwi03320031:15840
Boone-Plainbo complex, 12 to 45 percent slopesBoE7031421751g4vwwi03519741:15840
Boone-Plainbo complex, 6 to 12 percent slopesBoC3116421750g4vvwi03519741:15840
Boone-Plainbo complex, 2 to 6 percent slopesBoB1215421749g4vtwi03519741:15840
Boone-Tarr sands, 15 to 50 percent slopes1233F101030996901lmytwi03519741:15840
Boone sand, 6 to 15 percent slopes233C69030996771lmwxwi03519741:15840
Boone sand, 15 to 30 percent slopes233E569309972420rb2wi03519741:15840
Boone-Elevasil complex, 15 to 45 percent slopes, rocky1224F40330996652yt3hwi03519741:15840
Boone sand, 1 to 6 percent slopes233B2530997252fj7swi03519741:15840
Boone fine sand, 2 to 20 percent slopesBoD338425206g8gbwi04519691:12000
Boone fine sand, 12 to 30 percent slopes,moderately erodedBoD22317424514g7r0wi04919601:20000
Boone fine sand, 6 to 12 percent slopes, moderately erodedBoC277424513g7qzwi04919601:20000
Boone-Elevasil complex, 15 to 45 percent slopes, rocky1224F3086924991702yt3hwi05319941:20000
Boone sand, 6 to 15 percent slopes233C1579124983081lmwxwi05319941:20000
Boone-Tarr sands, 15 to 50 percent slopes1233F563724991721lmytwi05319941:20000
Boone sand, 1 to 6 percent slopes233B1333925615012fj7swi05719871:15840
Boone sand, 6 to 15 percent slopes233C541325614591lmwxwi05719871:15840
Boone-Tarr sands, 15 to 50 percent slopes1233F471325614851lmytwi05719871:15840
Boone-Elevasil complex, 15 to 45 percent slopes, rocky1224F70125614552yt3hwi05719871:15840
Boone-Tarr sands, 15 to 50 percent slopes1233F164924991731lmytwi06320011:12000
Boone sand, 6 to 15 percent slopes233C73624983091lmwxwi06320011:12000
Boone fine sand, 6 to 20 percent slopes, moderately erodedBoD2104424746g7zhwi06519641:15840
Boone-Elevasil complex, 15 to 45 percent slopes, rocky1224F1117926850512yt3hwi08119811:15840
Boone sand, 6 to 15 percent slopes233C631326851641lmwxwi08119811:15840
Boone-Tarr sands, 15 to 50 percent slopes1233F630826850501lmytwi08119811:15840
Boone-Rock outcrop complex, 30 to 70 percent slopes1203F27626850522kqyhwi08119811:15840
Boone sand, 6 to 15 percent slopes233C72024983111lmwxwi09119981:12000
Boone-Elevasil complex, 15 to 45 percent slopes, rocky1224F35124991692yt3hwi09119981:12000
Dorerton, very stony-Boone-Whalan complex, 20 to 60 percent slopes1105F581816986131v0jzwi09320061:12000
Boone loamy fine sand, till plain, 15 to 50 percent slopes230F67916927581ttg3wi09320061:12000
Lilah-Wykoff-Boone complex, 20 to 35 percent slopes1816F62017008001v2tjwi09320061:12000
Boone loamy fine sand, till plain, 6 to 15 percent slopes230C44216927591ttg4wi09320061:12000
Boone loamy fine sand, 12 to 20 percent slopesBnD1012422115g57mwi10919751:15840
Boone loamy fine sand, 6 to 12 percent slopesBnC829422114g57lwi10919751:15840
Boone loamy fine sand, 2 to 6 percent slopesBnB541422113g57kwi10919751:15840
Boone sand, 12 to 30 percent slopesBoD3386423131g69dwi11119771:15840
Boone sand, 2 to 6 percent slopesBoB3293423129g69bwi11119771:15840
Boone sand, 6 to 12 percent slopesBoC3220423130g69cwi11119771:15840
Boone-Elevasil complex, 15 to 45 percent slopes, rocky1224F122132578232yt3hwi11119771:15840
Boone-Tarr sands, 15 to 50 percent slopes1233F3032578241lmytwi11119771:15840
Boone-Elevasil complex, 15 to 45 percent slopes, rocky1224F6184426394912yt3hwi12119691:15840
Boone sand, 6 to 15 percent slopes233C211326834561lmwxwi12119691:15840
Boone sand, 15 to 30 percent slopes233E2111268346020rb2wi12119691:15840
Boone sand, 1 to 6 percent slopes233B57326834612fj7swi12119691:15840
Boone fine sand, 12 to 30 percent slopes201E124250393220rb1wi12319651:12000

Map of Series Extent

Approximate geographic distribution of the BOONE 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 .