Official Series Description


Lab Data Summary

Aggregate lab data for the BARNES soil series. This aggregation is based on all pedons with a current taxon name of BARNES, 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 BARNES were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). 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
102A87P057187MN149001Barnes7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.5,-96.0666656
102A87P057287MN149001ABarnes8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.6811104,-95.7986145
102A87P057387MN149001BBarnes8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.6836128,-95.797226
102A92P011991MN149001Barnes6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.6800003,-95.809166
102A92P012291MN149001BBarnes2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.6805573,-95.809166
102A92P012391MN149001CBarnes2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.6811104,-95.809166
102A08N0180S07SD039001Barnes7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.7902222,-96.5940018
102A08N0181S07SD039002Barnes7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.7903595,-96.5942535
102A40A2362S1957SD029003Barnes5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.0052795,-96.9030533
102A40A2469S1957SD029008Barnes5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.9911118,-97.0136108
102A40A2470S1957SD029009Barnes6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.0261116,-97.0244446
102A40A2471S1958SD029002Barnes6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.8375015,-97.0283356
102AUMN1155S1970MN0511155Barnes3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.9076767,-95.7781677
102AUMN1132S1970MN0831132Barnes3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.3701363,-96.0430908
102AUMN1092S1970MN1171092Barnes3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.141571,-96.082695
102AUMN1109S1970MN1171109Barnes2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.1596947,-96.1654968
102AUMN1299S1971MN0831299Barnes3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.3838768,-95.9791107
102AUMN1316S1971MN1171316Barnes4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.143383,-96.1229935
102AUMN2806S1978MN153060 (2806)Barnes4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.796177,-95.077086
53B87P056987ND083522Barnes7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.5672226,-100.1074982
53B87P056887ND083525Barnes7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.5672226,-100.1072235
53B87P056787ND083532Barnes7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.5672226,-100.1074982
53B87P057087ND083534Barnes7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.5672226,-100.1072235
53B94P068394ND093006Barnes8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.905101776123,-98.9285888671875
53B40A2392S1951SD115003Barnes7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.105278,-98.6969452
53B97P0520S1997ND093001Barnes8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9355545,-99.2786102
53B97P0521S1997ND093002Barnes8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9541664,-99.2791672
53B97P0522S1997ND093003Barnes8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9583321,-99.2799988
55A89P027988ND013066Barnes4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.9385795593262,-102.02278137207
55A89P028088ND013067Barnes4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.9777488708496,-102.04500579834
55A89P028188ND013068Barnes4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.9799690246582,-102.071678161621
55B77ND0350131977ND035013Barnes2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.9186111,-97.8808333
55B40A000853ND003001Barnes5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.094425201416,-97.7906646728516
55B40A001453ND091001Barnes5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.255256652832,-97.770393371582
55B87P017786SD025025Barnes5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.7608337,-97.7641678
55B87P017486SD025030Barnes6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.0222206,-97.9175034
55B89P025588ND039100Barnes4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.2716445922852,-98.4370803833008
55B89P025688ND039101Barnes4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.3180351257324,-98.1923522949219
55B89P025788ND039102Barnes4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.2733116149902,-98.2945785522461
55B88ND09151088ND091510Barnes3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.329003,-97.7611824
55B88ND09152288ND091522Barnes3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.3289475,-97.7617102
55B40A0011S1953ND021002Barnes6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.9949989,-98.230835

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BARNES 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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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 BARNES series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-02-21), parsed OSD records (updated 2023-10-02) and snapshot of SC database (updated 2023-10-02).

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Select annual climate data summaries for the BARNES series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2023-10-09).

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Geomorphic description summaries for the BARNES 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 (updated 2023-10-04).

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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 BARNES share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2023-10-02) and snapshot of the SC database (updated 2023-10-02).

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Select annual climate data summaries for the BARNES series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2023-10-09).

Click the image to view it full size.

Geomorphic description summaries for the BARNES 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 (updated 2023-10-04).

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.

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

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Soil series sharing subgroup-level classification with BARNES, 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 (updated 2023-10-02).

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. MN-2010-09-08-03 | Becker County - 1998

    Typical pattern of soils and parent material in the Hamerly-Winger-Vallers association (Soil Survey of Becker County, Minnesota; 1998).

  2. MN-2010-09-08-19 | Otter Tail County - 2001

    Typical pattern of soils and parent material in the Barnes-Langhei-Lakepark association (Soil Survey of Otter Tail County, Minnesota; 2001).

  3. ND-2010-09-27-04 | Burke County - 2003

    Typical pattern of soils and parent material in the Barnes-Cresbard association (Soil Survey of Burke County, North Dakota; 2003).

  4. ND-2010-09-27-06 | Griggs County - 2002

    Typical pattern of soils and underlying material in the LaDelle-Buse-Barnes-Edgeley association (Soil Survey of Griggs County, North Dakota; 2002).

  5. ND-2010-09-27-09 | Towner County -

    Typical pattern of soils and underlying material in the Barnes-Hamerly-Buse association (Soil Survey of Towner County, North Dakota).

  6. ND-2010-09-27-10 | Towner County -

    Typical pattern of soils and underlying material in the Hamerly-Barnes-Parnell association (Soil Survey of Towner County, North Dakota).

  7. ND-2012-02-07-06 | Barnes County - June 1990

    Typical pattern of soils and parent material in the Barnes-Svea-Buse association (Soil Survey of Barnes County, North Dakota; June 1990).

  8. ND-2012-02-07-07 | Barnes County - June 1990

    Typical pattern of soils and parent material in the Buse-Barnes-Nutley-Kloten association (Soil Survey of Barnes County, North Dakota; June 1990).

  9. ND-2012-02-07-09 | Bottineau County - May 1982

    Typical pattern of soils and underlying material in the Barnes-Svea association (Soil Survey of Bottineau County, North Dakota; May 1982).

  10. ND-2012-02-07-13 | Cass County Area - 1985

    Typical pattern of soils and underlying material in the Barnes-Svea association (Soil Survey of Cass County Area, North Dakota; 1985).

  11. ND-2012-02-07-22 | Dickey County - May 1993

    Typical pattern of soils and parent material in the Barnes-Svea-Hamerly association (Soil Survey of Dickey County, North Dakota; May 1993).

  12. ND-2012-02-07-23 | Dickey County - May 1993

    Typical pattern of soils and parent material in the Cavour-Barnes association (Soil Survey of Dickey County, North Dakota; May 1993).

  13. ND-2012-02-07-38 | Foster County - July 1995

    Typical pattern of soils and parent material in the Barnes-Svea-Buse association (Soil Survey of Foster County, North Dakota; July 1995).

  14. ND-2012-02-08-01 | Grand Forks County - May 1981

    Typical pattern of soils and parent material in the Svea-Buse-Hamerly association (Soil Survey of Grand Forks County, North Dakota; May 1981).

  15. ND-2012-02-08-17 | Kidder County - March 1988

    Typical pattern of soils and parent material in the Barnes-Towner association (Soil Survey of Kidder County, North Dakota; March 1988).

  16. ND-2012-02-08-18 | Kidder County - March 1988

    Typical pattern of soils and parent material in the Barnes-Buse-Parnell association (Soil Survey of Kidder County, North Dakota; March 1988).

  17. ND-2012-02-08-22 | McHenry County - October 1990

    Typical pattern of soils and parent material in the Barnes-Svea-Buse association (Soil Survey of McHenry County, North Dakota; October 1990).

  18. ND-2012-02-08-23 | McHenry County - October 1990

    Typical pattern of soils and parent material in the Towner-Swenoda-Hecla association (Soil Survey of McHenry County, North Dakota; October 1990).

  19. ND-2012-02-08-26 | McIntosh County - 2001

    Typical pattern of soils and underlying material in the Overly-Nutley-Rusklyn association (Soil Survey of McIntosh County, North Dakota; 2001).

  20. ND-2012-02-08-38 | Nelson County Area - June 1989

    Typical pattern of soils and parent material in the Hamerly-Svea-Tonka association (Soil Survey of Nelson County Area, North Dakota; June 1989).

  21. ND-2012-02-08-39 | Nelson County Area - June 1989

    Typical pattern of soils and parent material in the Svea-Buse-Parnell association (Soil Survey of Nelson County Area, North Dakota; June 1989).

  22. ND-2012-02-08-40 | Nelson County Area - June 1989

    Typical pattern of soils and parent material in the Cresbard-Svea association (Soil Survey of Nelson County Area, North Dakota; June 1989).

  23. ND-2012-02-08-41 | Nelson County Area - June 1989

    Typical pattern of soils and parent material in the Buse-Svea-Barnes association (Soil Survey of Nelson County Area, North Dakota; June 1989).

  24. ND-2012-02-08-42 | Nelson County Area - June 1989

    Typical pattern of soils and parent material in the Kloten-Buse-LaDelle association (Soil Survey of Nelson County Area, North Dakota; June 1989).

  25. ND-2012-02-08-43 | Nelson County Area - June 1989

    Typical pattern of soils and parent material in the Wamduska-Lallie-Mauvais association (Soil Survey of Nelson County Area, North Dakota; June 1989).

  26. ND-2012-02-08-44 | Ramsey County - August 1986

    Typical pattern of soils and underlying material in the Svea-Hamerly-Barnes association (Soil Survey of Ramsey County, North Dakota; August 1986).

  27. ND-2012-02-08-45 | Ramsey County - August 1986

    Typical pattern of soils and underlying material in the Hamerly-Cresbard-Svea association (Soil Survey of Ramsey County, North Dakota; August 1986).

  28. ND-2012-02-08-54 | Stutsman County - June 1995

    Typical pattern of soils and parent material in the Barnes-Buse association (Soil Survey of Stutsman County, North Dakota; June 1995).

  29. ND-2012-02-08-56 | Towner County - 1998

    Typical pattern of soils and underlying material in the Overly-Bearden-Great Bend association (Soil Survey of Towner County, North Dakota; 1998).

  30. ND-2012-02-08-57 | Towner County - 1998

    Typical pattern of soils and underlying material in the Hamerly-Barnes-Tonka association (Soil Survey of Towner County, North Dakota; 1998).

  31. ND-2012-02-08-58 | Towner County - 1998

    Typical pattern of soils and underlying material in the Divide-Brantford-Barnes association (Soil Survey of Towner County, North Dakota; 1998).

  32. ND-2012-02-08-59 | Ward County - 1974

    Relationship of soils to topography and parent material (Soil Survey of Ward County, North Dakota; 1974).

  33. ND-2012-02-08-61 | Wells County - June 1970

    Parent material and position of soils in association 2 (Soil Survey of Wells County, North Dakota; June 1970).

  34. ND-2012-02-08-62 | Wells County - June 1970

    Parent material and position of soils in association 4 (Soil Survey of Wells County, North Dakota; June 1970).

  35. ND-2012-02-08-63 | Wells County - June 1970

    Parent material and position of soils in association 5 (Soil Survey of Wells County, North Dakota; June 1970).

  36. ND-2012-02-08-67 | Wells County - June 1970

    Parent material and position of soils in association 10 (Soil Survey of Wells County, North Dakota; June 1970

  37. ND-2012-02-14-01 | Ward County - 1974

    Relationship of soils to topography and parent material (Soil Survey of Ward County, North Dakota; 1974).

  38. SD-2010-11-01-01 | Brookings County - 2004

    Typical pattern of soils and parent material in the Poinsett-Buse-Waubay association (Soil Survey of Brookings County, South Dakota; 2004).

  39. SD-2010-11-01-03 | Brookings County - 2004

    Typical pattern of soils and parent material in the Barnes association (Soil Survey of Brookings County, South Dakota; 2004).

  40. SD-2010-11-01-04 | Brookings County - 2004

    Typical pattern of soils and parent material in the Buse-Barnes-Lamoure association (Soil Survey of Brookings County, South Dakota; 2004).

  41. SD-2010-11-01-08 | Hamlin County - 2003

    Typical pattern of soils and underlying material in the Poinsett-Waubay-Buse association (Soil Survey of Hamlin County, South Dakota; 2003).

  42. SD-2012-03-14-10 | Brown County - April 1993

    Typical pattern of soils and parent material in the Barnes-Svea association (Soil Survey of Brown County, SD; 1993).

  43. SD-2012-03-14-13 | Clark County - 1999

    Typical pattern of soils and underlying material in the Barnes-Svea-Buse association (Soil Survey of Clark County, SD; 1999).

  44. SD-2012-03-14-14 | Clark County - 1999

    Typical pattern of soils and underlying material in the Buse-Barnes-Southam association (Soil Survey of Clark County, SD; 1999).

  45. SD-2012-03-14-16 | Clark County - 1999

    Typical pattern of soils and underlying material in the Poinsett-Waubay-Buse association (Soil Survey of Clark County, SD; 1999).

  46. SD-2012-03-15-17 | Day County - August 1997

    Typical pattern of soils and underlying material in the Harmony-Aberdee-Nahon and Kranzburg-Brookings associations (Soil Survey of Day County, SD; 1997).

  47. SD-2012-03-15-19 | Day County - August 1997

    Typical pattern of soils and underlying material in the Forman-Buse-Parnell association (Soil Survey of Day County, SD; 1997).

  48. SD-2012-03-15-21 | Day County - August 1997

    Typical pattern of soils and underlying material in the Sioux-Renshaw association (Soil Survey of Day County, SD; 1997).

  49. SD-2012-03-15-62 | Kingsbury County - November 1997

    Typical pattern of soils and underlying material in the Poinsett-Waubay-Buse association (Soil Survey of Kingsbury County, SD; 1997).

  50. SD-2012-03-15-63 | Kingsbury County - November 1997

    Typical pattern of soils and underlying material in the Poinsett-Hetland association (Soil Survey of Kingsbury County, SD; 1997).

Map Units

Map units containing BARNES 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
Barnes-Svea-Buse complex, 3 to 15 percent slopesJ119D1147431825182yw63mn00519941:20000
Barnes-Buse complex, 6 to 12 percent slopes, moderately eroded903C237843975772w0lymn00519941:20000
Langhei-Barnes, moderately eroded, complex, 12 to 20 percent slopes942D211783975792w0lwmn00519941:20000
Langhei-Barnes-Darnen complex, 5 to 30 percent slopesJ120E76731825172yw62mn00519941:20000
Langhei-Barnes-Darnen complex, 5 to 30 percent slopesJ120E61931825352yw62mn01119901:20000
Barnes-Svea-Buse complex, 3 to 15 percent slopesJ119D39231825362yw63mn01119901:20000
Langhei-Barnes, moderately eroded, complex, 12 to 20 percent slopesJ37D239924230492w0lwmn02319801:15840
Langhei-Barnes, moderately eroded, complex, 6 to 12 percent slopesJ36C23124230482w0lvmn02319801:15840
Langhei-Barnes, moderately eroded, complex, 6 to 12 percent slopes942C2255503570222w0lvmn02719801:20000
Langhei-Barnes, moderately eroded, complex, 12 to 20 percent slopes942D268933570232w0lwmn02719801:20000
Barnes-Buse complex, 6 to 12 percent slopes, moderately eroded33C213403569592w0lymn02719801:20000
Barnes-Buse complex, 6 to 12 percent slopes, moderately erodedBaC2194913972522w0lymn04119701:12000
Langhei-Barnes, moderately eroded, complex, 12 to 20 percent slopesLgD249723972892w0lwmn04119701:12000
Langhei-Barnes, moderately eroded, complex, 6 to 12 percent slopes942C276283980722w0lvmn05119741:20000
Barnes-Svea-Buse complex, 3 to 15 percent slopesJ119D749131825542yw63mn05119741:20000
Langhei-Barnes, moderately eroded, complex, 12 to 20 percent slopes942D226483980732w0lwmn05119741:20000
Langhei-Barnes-Darnen complex, 5 to 30 percent slopesJ120E151731825532yw62mn05119741:20000
Langhei-Barnes, moderately eroded, complex, 6 to 12 percent slopesJ36C2120029457702w0lvmn06719831:20000
Langhei-Barnes, moderately eroded, complex, 12 to 20 percent slopesJ37D263529457532w0lwmn06719831:20000
Buse-Barnes complex, 2 to 12 percent slopes, extremely stony1865C3559430264gfqhmn07319941:20000
Langhei-Barnes, moderately eroded, complex, 6 to 12 percent slopes942C230484303602w0lvmn07319941:20000
Langhei-Barnes, moderately eroded, complex, 12 to 20 percent slopes220D27454302742w0lwmn07319941:20000
Barnes, occasional saturation-Buse-Svea complex, 1 to 6 percent slopesJ106B3522815423182yyjvmn08120071:12000
Barnes-Buse complex, 6 to 12 percent slopes, moderately erodedJ96C22961811496442wkqtmn08120071:12000
Barnes, occasional saturation-Buse complex, 3 to 6 percent slopesJ96B869311515402yyjgmn08120071:12000
Buse-Barnes-Arvilla complex, 6 to 12 percent slopes, moderately erodedJ235C2108214796071lnn8mn08120071:12000
Barnes, occasional saturation-Buse-Arvilla complex, 2 to 6 percent slopesJ232B106114794782yyj6mn08120071:12000
Renshaw-Barnes complex, 6 to 12 percent slopes, moderately erodedJ81C21139914592yyjfmn08120071:12000
Barnes, occasional saturation-Buse-Svea complex, 1 to 6 percent slopesJ106B2215015423232yyjvmn08320081:12000
Barnes-Buse complex, 6 to 12 percent slopes, moderately erodedJ96C21297214862262wkqtmn08320081:12000
Buse, moderately eroded-Barnes, moderately eroded-Arvilla complex, 6 to 12 percent slopesJ235C2126914862282yyj7mn08320081:12000
Barnes, occasional saturation-Buse-Arvilla complex, 2 to 6 percent slopesJ232B100114862272yyj6mn08320081:12000
Arvilla-Barnes-Buse complex, 2 to 6 percent slopes, eroded904B223185905120dhdmn08320081:12000
Barnes-Buse complex, 6 to 12 percent slopes, moderately eroded903C263643992612w0lymn08719921:20000
Langhei-Barnes, moderately eroded, complex, 12 to 20 percent slopes942D28603992622w0lwmn08719921:20000
Barnes, occasional saturation-Buse-Svea complex, 1 to 6 percent slopesJ106B2259415423262yyjvmn10120081:12000
Barnes-Buse complex, 6 to 12 percent slopes, moderately erodedJ96C21180012923192wkqtmn10120081:12000
Barnes, occasional saturation-Buse complex, 3 to 6 percent slopesJ96B696212923182yyjgmn10120081:12000
Barnes, occasional saturation-Buse-Arvilla complex, 2 to 6 percent slopesJ232B179014816572yyj6mn10120081:12000
Buse, moderately eroded-Barnes, moderately eroded-Arvilla complex, 6 to 12 percent slopesJ235C2129414816582yyj7mn10120081:12000
Barnes loam, 3 to 6 percent slopes, eroded33B2986185940920dvymn10120081:12000
Barnes loam, 2 to 4 percent slopes33B787185940820dvxmn10120081:12000
Barnes-Buse loams, 6 to 12 percent slopes, eroded902C2354185945520dxfmn10120081:12000
Buse-Barnes loams, 12 to 18 percent slopes913D100185945820dxjmn10120081:12000
Arvilla-Barnes-Buse complex, 2 to 6 percent slopes904B81185945620dxgmn10120081:12000
Arvilla-Barnes-Buse complex, 6 to 12 percent slopes904C26185945720dxhmn10120081:12000
Renshaw-Barnes complex, 6 to 12 percent slopes, moderately erodedJ81C2179889002yyjfmn10120081:12000
Langhei-Barnes, moderately eroded, complex, 6 to 12 percent slopesLbC219563572462w0lvmn10719701:20000
Langhei-Barnes, moderately eroded, complex, 12 to 20 percent slopesLbD29503572472w0lwmn10719701:20000
Barnes-Buse complex, 6 to 12 percent slopes, moderately erodedBaC27803572032w0lymn10719701:20000
Barnes-Buse complex, 6 to 12 percent slopes, moderately eroded903C294364359642w0lymn11119961:20000
Barnes-Svea-Buse complex, 3 to 15 percent slopesJ119D675531825722yw63mn11119961:20000
Langhei-Barnes, moderately eroded, complex, 12 to 20 percent slopes942D219484359722w0lwmn11119961:20000
Langhei-Barnes-Darnen complex, 5 to 30 percent slopesJ120E62531825712yw62mn11119961:20000
Barnes, occasional saturation-Buse complex, 3 to 6 percent slopesJ96B477712923052yyjgmn11720051:12000
Barnes-Buse complex, 6 to 12 percent slopes, moderately erodedJ96C2328412923082wkqtmn11720051:12000
Barnes, occasional saturation-Buse-Svea complex, 1 to 6 percent slopesJ106B250814815992yyjvmn11720051:12000
Renshaw-Barnes complex, 6 to 12 percent slopes, moderately erodedJ81C215477805182yyjfmn11720051:12000
Barnes-Buse complex, 6 to 12 percent slopes, moderately erodedBbC2216584013202w0lymn12119681:20000
Langhei-Barnes, moderately eroded, complex, 6 to 12 percent slopesLnC2168714013632w0lvmn12119681:20000
Langhei-Barnes, moderately eroded, complex, 12 to 20 percent slopesLnD2144914013642w0lwmn12119681:20000
Langhei-Barnes loams, 2 to 6 percent slopes, erodedLnB23108401362fgn5mn12119681:20000
Barnes-Langhei-Renshaw loams, 6 to 12 percent slopesBdC673401322fglwmn12119681:20000
Langhei-Barnes-Sioux complex, 12 to 18 percent slopes, erodedLoD2490401365fgn8mn12119681:20000
Barnes-Langhei-Renshaw loams, 2 to 6 percent slopes, erodedBdB2414401321fglvmn12119681:20000
Barnes-Svea-Buse complex, 3 to 15 percent slopesJ119D30731825902yw63mn12119681:20000
Langhei-Barnes-Darnen complex, 5 to 30 percent slopesJ120E4631825892yw62mn12119681:20000
Barnes-Buse complex, 6 to 12 percent slopes, moderately eroded421C62374281432w0lymn14519801:15840
Langhei-Barnes, moderately eroded, complex, 12 to 20 percent slopes954D6644281892w0lwmn14519801:15840
Barnes-Svea-Buse complex, 3 to 15 percent slopesJ119D357831826082yw63mn14919661:15840
Barnes-Buse complex, 6 to 12 percent slopes, moderately erodedBbC220454283142w0lymn14919661:15840
Langhei-Barnes-Darnen complex, 5 to 30 percent slopesJ120E96631826072yw62mn14919661:15840
Langhei-Barnes, moderately eroded, complex, 12 to 20 percent slopesBoD26124283212w0lwmn14919661:15840
Langhei-Barnes, moderately eroded, complex, 6 to 12 percent slopesJ36C220584348192w0lvmn15120001:12000
Buse-Barnes complex, 2 to 12 percent slopes, very boulderyJ62C1268434857glhnmn15120001:12000
Langhei-Barnes, moderately eroded, complex, 12 to 20 percent slopesJ37D28834348202w0lwmn15120001:12000
Buse-Barnes complex, 12 to 40 percent slopes, very boulderyJ62F171434858glhpmn15120001:12000
Barnes-Buse complex, 6 to 12 percent slopes, moderately eroded421C3594285432w0lymn15319851:20000
Langhei-Barnes-Darnen complex, 5 to 30 percent slopesJ120E349231826242yw62mn15519861:20000
Barnes-Svea-Buse complex, 3 to 15 percent slopesJ119D61631826252yw63mn15519861:20000
Langhei-Barnes, moderately eroded, complex, 6 to 12 percent slopes942C220843574662w0lvmn16719851:20000
Langhei-Barnes, moderately eroded, complex, 12 to 20 percent slopes942D22163574672w0lwmn16719851:20000
Barnes-Svea-Buse complex, 3 to 15 percent slopesJ119D4231826292yw63mn16719851:20000
Barnes, occasional saturation-Buse-Svea complex, 1 to 6 percent slopesJ106B731316539652yyjvmn17319791:20000
Barnes-Buse complex, 6 to 12 percent slopes, moderately erodedJ96C2482416539412wkqtmn17319791:20000
Buse-Barnes-Arvilla complex, 6 to 12 percent slopes, moderately erodedJ235C252614816791lqt3mn17319791:20000
Barnes, occasional saturation-Buse-Arvilla complex, 2 to 6 percent slopesJ232B34914817092yyj6mn17319791:20000
Barnes-Buse loams, 3 to 6 percent slopesG144B14028525735682pwz2nd00319881:20000
Barnes-Svea loams, 3 to 6 percent slopesG143B10228025735722pwz6nd00319881:20000
Barnes-Svea loams, 0 to 3 percent slopesG143A5753025735732pwz7nd00319881:20000
Barnes-Buse-Langhei loams, 6 to 9 percent slopesG143C4829525735712pwz5nd00319881:20000
Buse-Barnes-Darnen loams, 9 to 35 percent slopesG147F1136025735632pwytnd00319881:20000
Barnes-Sioux complex, 1 to 6 percent slopesG680B828225736572q5w2nd00319881:20000
Barnes-Buse-Langhei loams, 9 to 15 percent slopesG143D827025735702pwz4nd00319881:20000
Barnes-Sioux complex, 3 to 9 percent slopesG680C780025736582q5w3nd00319881:20000
Buse-Barnes-La Prairie, occasionally flooded loams, 6 to 35 percent slopesG148F688025736732q61jnd00319881:20000
Buse-Barnes loams, 15 to 35 percent slopesG143F544325735692pwz3nd00319881:20000
Swenoda-Barnes complex, 3 to 6 percent slopesG732B387025736612q5wrnd00319881:20000
Buse-Barnes-Darnen loams, 3 to 9 percent slopesG147C368025735652pwywnd00319881:20000
Swenoda-Barnes fine sandy loams, 0 to 3 percent slopesG732A241325736602q5wqnd00319881:20000
Barnes-Svea loams, 0 to 6 percent slopes, extremely stonyG614B206025736432q5sgnd00319881:20000
Barnes-Buse-Parnell complex, 0 to 6 percent slopesG146B205225735672pwyznd00319881:20000
Barnes-Cavour loams, 3 to 6 percent slopesG123B179625736712q61fnd00319881:20000
Buse-Barnes-Darnen loams, 6 to 15 percent slopesG147D118925735642pwyvnd00319881:20000
Buse-Barnes-Parnell complex, 0 to 9 percent slopesG146C25525735662pwyynd00319881:20000
Buse-Barnes-La Prairie, occasionally flooded loams, 6 to 15 percent slopesG148D18526382332q61hnd00319881:20000
Buse-Barnes-La Prairie, occasionally flooded loams, 3 to 9 percent slopesG148C8525736722q61gnd00319881:20000
Buse-Barnes-Langhei loams, 4 to 15 percent slopesF1143D1794832476392ykx4nd0051:12000
Barnes-Sioux complex, 3 to 9 percent slopesF680C476325876862q5lhnd0051:12000
Buse-Barnes loams, 15 to 35 percent slopesG143F329725737712pwz3nd0051:12000
Barnes-Cresbard loams, 3 to 6 percent slopesF122B282425877532q4ggnd0051:12000
Barnes-Buse loams, 2 to 6 percent slopesF1144B257632476372ykx2nd0051:12000
Buse-Barnes loams, 3 to 9 percent slopesF1143C207032476382ykx3nd0051:12000
Barnes-Buse loams, 3 to 6 percent slopesG144B201425737232pwz2nd0051:12000
Buse-Barnes-Darnen loams, 9 to 35 percent slopesF147F150225877022q4h8nd0051:12000
Barnes-Svea loams, 0 to 3 percent slopesG143A120125737082pwz7nd0051:12000
Barnes-Buse-Langhei loams, 6 to 9 percent slopesG143C103025737272pwz5nd0051:12000
Barnes-Svea loams, 3 to 6 percent slopesG143B96525737752pwz6nd0051:12000
Buse-Barnes-Darnen loams, 6 to 15 percent slopesF147D89425877282q4h2nd0051:12000
Towner-Barnes complex, 3 to 6 percent slopesF737B75225877142q5m2nd0051:12000
Buse-Barnes-Darnen loams, 3 to 9 percent slopesF147C65425875962q4h1nd0051:12000
Barnes-Buse-Langhei loams, 9 to 15 percent slopesG143D61425737162pwz4nd0051:12000
Barnes-Buse loams, 3 to 9 percent slopes, very stonyF612C55725877332q5dknd0051:12000
Buse-Barnes-La Prairie, occasionally flooded loams, 6 to 35 percent slopesF148F48125877382q4h9nd0051:12000
Towner-Barnes fine sandy loams, 0 to 3 percent slopesG737A16225738092q5wwnd0051:12000
Buse-Barnes-La Prairie, occasionally flooded loams, 6 to 15 percent slopesF148D16125876042q4h4nd0051:12000
Swenoda-Barnes fine sandy loams, 0 to 3 percent slopesF732A12725876922q5lwnd0051:12000
Barnes-Coe complex, 3 to 9 percent slopesG681C10325738272q5w7nd0051:12000
Barnes-Sioux complex, 3 to 9 percent slopesG680C10225737792q5w3nd0051:12000
Buse-Barnes-La Prairie, occasionally flooded loams, 3 to 9 percent slopesF148C9825877662q4h3nd0051:12000
Swenoda-Barnes complex, 3 to 6 percent slopesF732B8825877562q5lxnd0051:12000
Barnes-Buse-Langhei loams, 6 to 9 percent slopesF143C8025876452q4gsnd0051:12000
Barnes-Svea loams, 3 to 6 percent slopesF143B7325876102q4grnd0051:12000
Buse-Barnes-Darnen loams, 3 to 9 percent slopesG147C7125736972pwywnd0051:12000
Barnes-Coe complex, 3 to 9 percent slopesF681C7025876732q5llnd0051:12000
Barnes-Buse loams, 3 to 6 percent slopesF144B4925876622q4gwnd0051:12000
Buse-Barnes-Darnen loams, 9 to 35 percent slopesG147F4525737622pwytnd0051:12000
Towner-Barnes complex, 3 to 6 percent slopesG737B4425736772q5wxnd0051:12000
Barnes-Cresbard loams, 3 to 6 percent slopesG122B3925736952pwzbnd0051:12000
Barnes-Svea loams, 0 to 3 percent slopesF143A1725877222q4gqnd0051:12000
Buse-Barnes-Darnen loams, 6 to 15 percent slopesG147D1325738132pwyvnd0051:12000
Buse-Barnes loams, 15 to 35 percent slopesF143F325876192q4gvnd0051:12000
Barnes loam, 0 to 3 percent slopesF157A507625860112q4hdnd00919811:20000
Barnes-Buse-Langhei loams, 6 to 9 percent slopesF143C505425859352q4gsnd00919811:20000
Barnes-Buse loams, 3 to 6 percent slopesF144B494325859472q4gwnd00919811:20000
Barnes-Cresbard loams, 3 to 6 percent slopesF122B426125860522q4ggnd00919811:20000
Buse-Barnes-Darnen loams, 6 to 15 percent slopesF147D249125860282q4h2nd00919811:20000
Barnes-Svea-Tonka complex, 0 to 3 percent slopesF159A238325859662q3wknd00919811:20000
Barnes-Buse-Langhei loams, 9 to 15 percent slopesF143D194825860312q4gtnd00919811:20000
Buse-Barnes-Darnen loams, 3 to 9 percent slopesF147C193725858742q4h1nd00919811:20000
Buse-Barnes loams, 15 to 35 percent slopesF143F180225859022q4gvnd00919811:20000
Towner-Barnes fine sandy loams, 0 to 3 percent slopesF737A161325859442q5m1nd00919811:20000
Buse-Barnes-Darnen loams, 9 to 35 percent slopesF147F132625859992q4h8nd00919811:20000
Barnes-Svea loams, 3 to 6 percent slopesF143B120425858882q4grnd00919811:20000
Buse-Barnes-La Prairie, occasionally flooded loams, 6 to 35 percent slopesF148F111025860382q4h9nd00919811:20000
Barnes loam, 3 to 6 percent slopesF157B104925858852q4hfnd00919811:20000
Barnes-Svea-Tonka complex, 0 to 6 percent slopesF159B101525860502md2ynd00919811:20000
Buse-Barnes-La Prairie, occasionally flooded loams, 6 to 15 percent slopesF148D62325858842q4h4nd00919811:20000
Barnes-Svea loams, 0 to 3 percent slopesF143A60925860202q4gqnd00919811:20000
Swenoda-Barnes fine sandy loams, 0 to 3 percent slopesF732A50825859822q5lwnd00919811:20000
Buse-Barnes-La Prairie, occasionally flooded loams, 3 to 9 percent slopesF148C30225860732q4h3nd00919811:20000
Buse-Barnes-Parnell complex, 0 to 35 percent slopesF146F6625860622q4h0nd00919811:20000
Towner-Barnes complex, 3 to 6 percent slopesF737B6025860122q5m2nd00919811:20000
Buse-Barnes-Parnell complex, 0 to 9 percent slopesF146C2825859622q4gznd00919811:20000
Swenoda-Barnes fine sandy loams, 0 to 3 percent slopesF732A187925858422q5lwnd01319911:24000
Swenoda-Barnes complex, 3 to 6 percent slopesF732B137725858592q5lxnd01319911:24000
Buse-Barnes-Darnen loams, 3 to 9 percent slopesF147C43625858162q4h1nd01319911:24000
Barnes-Buse-Langhei loams, 6 to 9 percent slopesF143C27225858312q4gsnd01319911:24000
Buse-Barnes-Darnen loams, 9 to 35 percent slopesF147F16025858442q4h8nd01319911:24000
Barnes-Buse loams, 3 to 6 percent slopesF144B7425858342q4gwnd01319911:24000
Buse-Barnes-La Prairie, occasionally flooded loams, 6 to 35 percent slopesF148F3826246352q4h9nd01319911:24000
Barnes loam, 3 to 6 percent slopesF157B2325858192q4hfnd01319911:24000
Buse-Barnes-Darnen loams, 6 to 15 percent slopesF147D425858512q4h2nd01319911:24000
Barnes-Svea loams, 3 to 6 percent slopesG143B3943325751112pwz6nd01719831:20000
Barnes-Svea loams, 0 to 3 percent slopesG143A3581225750572pwz7nd01719831:20000
Barnes-Buse loams, 3 to 6 percent slopesG144B3250325750672pwz2nd01719831:20000
Barnes-Buse-Langhei loams, 6 to 9 percent slopesG143C628025750712pwz5nd01719831:20000
Barnes-Sioux complex, 1 to 6 percent slopesG680B376425750592q5w2nd01719831:20000
Buse-Barnes-Darnen loams, 3 to 9 percent slopesG147C324325750492pwywnd01719831:20000
Barnes-Sioux complex, 3 to 9 percent slopesG680C226125751132q5w3nd01719831:20000
Buse-Barnes-Darnen loams, 9 to 35 percent slopesG147F160225751032pwytnd01719831:20000
Buse-Barnes-Darnen loams, 6 to 15 percent slopesG147D133025751422pwyvnd01719831:20000
Barnes-Buse-Langhei loams, 9 to 15 percent slopesG143D108025750622pwz4nd01719831:20000
Buse-Barnes loams, 15 to 35 percent slopesG143F99625751092pwz3nd01719831:20000
Barnes-Sioux complex, 6 to 15 percent slopesG680D40825751362q5w4nd01719831:20000
Buse-Barnes-La Prairie, occasionally flooded loams, 3 to 9 percent slopesG148C35825751322q61gnd01719831:20000
Buse-Barnes-La Prairie, occasionally flooded loams, 6 to 15 percent slopesG148D24525750612q61hnd01719831:20000
Barnes-Svea loams, 3 to 6 percent slopesI402B19226408571nyyynd01719831:20000
Barnes-Sioux complex, 6 to 15 percent slopesI462D5526408321tblqnd01719831:20000
Barnes-Buse-Parnell complex, 0 to 6 percent slopesG146B4825750762pwyznd01719831:20000
Swenoda-Barnes complex, 3 to 6 percent slopesG732B4325751192q5wrnd01719831:20000
Barnes-Svea loams, 0 to 3 percent slopesF143A4432725875252q4gqnd01919871:20000
Barnes-Svea loams, 3 to 6 percent slopesF143B2602825875262q4grnd01919871:20000
Barnes-Cresbard loams, 3 to 6 percent slopesF122B1945025875212q4ggnd01919871:20000
Barnes-Buse-Langhei loams, 6 to 9 percent slopesF143C719825875272q4gsnd01919871:20000
Barnes-Buse loams, 2 to 6 percent slopesF1144B533832476582ykx2nd01919871:20000
Barnes-Buse loams, 3 to 6 percent slopesF144B180025875302q4gwnd01919871:20000
Buse-Barnes-La Prairie, occasionally flooded loams, 6 to 35 percent slopesF148F146525875392q4h9nd01919871:20000
Buse-Barnes loams, 3 to 9 percent slopesF1143C137632476592ykx3nd01919871:20000
Barnes-Buse-Langhei loams, 9 to 15 percent slopesF143D122825875282q4gtnd01919871:20000
Buse-Barnes-Darnen loams, 9 to 35 percent slopesF147F113525875382q4h8nd01919871:20000
Buse-Barnes-Langhei loams, 4 to 15 percent slopesF1143D107132476602ykx4nd01919871:20000
Buse-Barnes-Darnen loams, 6 to 15 percent slopesF147D100825875342q4h2nd01919871:20000
Buse-Barnes-Darnen loams, 3 to 9 percent slopesF147C91625875332q4h1nd01919871:20000
Buse-Barnes-La Prairie, occasionally flooded loams, 6 to 15 percent slopesF148D48425875362q4h4nd01919871:20000
Buse-Barnes-La Prairie, occasionally flooded loams, 3 to 9 percent slopesF148C33625875352q4h3nd01919871:20000
Barnes-Sioux complex, 3 to 9 percent slopesF680C12925875862q5lhnd01919871:20000
Buse-Barnes loams, 15 to 35 percent slopesF143F2925875292q4gvnd01919871:20000
Barnes-Buse-Parnell complex, 0 to 6 percent slopesF146B1725875312q4gynd01919871:20000
Barnes-Coe complex, 3 to 9 percent slopesF681C625875872q5llnd01919871:20000
Barnes-Svea loams, 0 to 3 percent slopesG143A9735925752542pwz7nd02119891:20000
Barnes-Svea loams, 3 to 6 percent slopesG143B6393825752532pwz6nd02119891:20000
Barnes-Cavour loams, 3 to 6 percent slopesG123B2757325753832q61fnd02119891:20000
Barnes-Cresbard loams, 3 to 6 percent slopesG122B1800725752562pwzbnd02119891:20000
Barnes-Buse loams, 3 to 6 percent slopesG144B1589025752492pwz2nd02119891:20000
Barnes-Buse-Langhei loams, 6 to 9 percent slopesG143C1144125752522pwz5nd02119891:20000
Swenoda-Barnes fine sandy loams, 0 to 3 percent slopesG732A945825753732q5wqnd02119891:20000
Barnes-Buse-Parnell complex, 0 to 6 percent slopesG146B460125752482pwyznd02119891:20000
Buse-Barnes-Darnen loams, 9 to 35 percent slopesG147F383925752452pwytnd02119891:20000
Buse-Barnes-Darnen loams, 3 to 9 percent slopesG147C379725752472pwywnd02119891:20000
Barnes-Gardena loams, 0 to 3 percent slopesG711A324825753702q5wjnd02119891:20000
Barnes-Sioux complex, 3 to 9 percent slopesG680C167225753682q5w3nd02119891:20000
Buse-Barnes-Darnen loams, 6 to 15 percent slopesG147D103925752462pwyvnd02119891:20000
Barnes-Buse-Langhei loams, 9 to 15 percent slopesG143D92725752512pwz4nd02119891:20000
Buse-Barnes loams, 15 to 35 percent slopesG143F30525752502pwz3nd02119891:20000
Buse-Barnes-La Prairie, occasionally flooded loams, 6 to 15 percent slopesG148D12325753852q61hnd02119891:20000
Buse-Barnes-La Prairie, occasionally flooded loams, 3 to 9 percent slopesG148C6425753842q61gnd02119891:20000
Barnes-Coe complex, 3 to 9 percent slopesG681C2125753692q5w7nd02119891:20000
Swenoda-Barnes complex, 3 to 6 percent slopesG732B1225753742q5wrnd02119891:20000
Barnes-Buse loams, 3 to 9 percent slopes, very stonyG612C525753652q5sfnd02119891:20000
Barnes-Svea loams, 3 to 6 percent slopesG143B391325753952pwz6nd0271:12000
Barnes-Svea loams, 0 to 3 percent slopesG143A188125753962pwz7nd0271:12000
Barnes-Buse-Langhei loams, 6 to 9 percent slopesG143C155425753942pwz5nd0271:12000
Buse-Barnes-Darnen loams, 9 to 35 percent slopesG147F95825753872pwytnd0271:12000
Towner-Barnes fine sandy loams, 0 to 3 percent slopesG737A78025763492q5wwnd0271:12000
Barnes-Buse-Langhei loams, 9 to 15 percent slopesG143D59225753932pwz4nd0271:12000
Towner-Barnes complex, 3 to 6 percent slopesG737B45625763502q5wxnd0271:12000
Buse-Barnes loams, 15 to 35 percent slopesG143F21825753922pwz3nd0271:12000
Barnes-Buse loams, 3 to 9 percent slopes, very stonyG612C20725763402q5sfnd0271:12000
Buse-Barnes-Darnen loams, 3 to 9 percent slopesG147C16625753892pwywnd0271:12000
Buse-Barnes-Darnen loams, 6 to 15 percent slopesG147D12225753882pwyvnd0271:12000
Buse-Barnes-Parnell complex, 0 to 9 percent slopesG146C11325753902pwyynd0271:12000
Barnes-Buse-Parnell complex, 0 to 6 percent slopesG146B8025753912pwyznd0271:12000
Swenoda-Barnes fine sandy loams, 0 to 3 percent slopesG732A525763482q5wqnd0271:12000
Barnes-Buse loams, 3 to 6 percent slopesG144B1993525763672pwz2nd03119901:20000
Barnes-Svea loams, 0 to 3 percent slopesG143A1671325763722pwz7nd03119901:20000
Barnes-Svea loams, 3 to 6 percent slopesG143B1352225763712pwz6nd03119901:20000
Barnes-Buse-Langhei loams, 6 to 9 percent slopesG143C817825763702pwz5nd03119901:20000
Towner-Barnes complex, 3 to 6 percent slopesG737B261025764712q5wxnd03119901:20000
Barnes-Buse-Langhei loams, 9 to 15 percent slopesG143D222925763692pwz4nd03119901:20000

Map of Series Extent

Approximate geographic distribution of the BARNES 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 (updated 2023-10-04).