Official Series Description


Lab Data Summary

Aggregate lab data for the BUSE soil series. This aggregation is based on all pedons with a current taxon name of BUSE, 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 BUSE were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). 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
102A87P01791986SD025027Buse5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.0105553,-97.8511124
102AUMN1180S1970MN0511180Buse2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.9795723,-95.9735336
102AUMN1230S1971MN0831230Buse2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.2661247,-96.0119781
102AUMN3195S1979MN1013195Buse3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0402489,-95.7840424
102A93P0767S1993MN111005Buse7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.1722221,-95.9367752
55A82ND06312582ND063125Buse5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.9334137,-98.3790068
55B40A281466ND027011Buse7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.7710876464844,-99.1473922729492
55B87P017886SD025024Buse5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.7700005,-97.7580566
55B94P021393SD115037Buse7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2291679,-98.0513916
55B40A2815S1966ND027012Buse7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.774656,-99.230811

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BUSE 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 BUSE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-10-24), parsed OSD records (updated 2024-10-23) and snapshot of SC database (updated 2024-10-23).

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Select annual climate data summaries for the BUSE 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 2024-10-23).

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Geomorphic description summaries for the BUSE 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 2024-10-23).

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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 BUSE share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2024-10-23) and snapshot of the SC database (updated 2024-10-23).

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Select annual climate data summaries for the BUSE 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 2024-10-23).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the BUSE 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 2024-10-23).

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 BUSE, 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 2024-10-23).

Block Diagrams

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

  1. MN-2010-09-08-19 | 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).

  2. MN-2010-09-08-22 | Otter Tail County - 2001

    Typical pattern of soils and parent material in the Forman-Buse-Peever association (Soil Survey of Otter Tail County, Minnesota; 2001).

  3. MN-2010-09-10-15 | Swift County -

    Tara-Doland-Buse association (Soil Survey of Swift County, Minnesota).

  4. MN-2010-09-27-03 | Lac qui Parle County -

    Typical pattern of soils and underlying material in the Forman-Mehurin-Parnell association (Soil Survey of Lac qui Parle County, Minnesota).

  5. MN-2010-09-27-04 | Lac qui Parle County -

    Typical pattern of soils and underlying material in the Waubay-Poinsett-Colvin association (Soil Survey of Lac qui Parle County, Minnesota).

  6. 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).

  7. 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).

  8. 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).

  9. 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).

  10. 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).

  11. 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).

  12. 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).

  13. ND-2012-02-07-18 | Cavalier County - May 1990

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

  14. ND-2012-02-07-20 | Cavalier County - May 1990

    Typical pattern of soils and parent material in the Svea-Hamerly-Cresbard association (Soil Survey of Cavalier County, North Dakota; May 1990).

  15. 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).

  16. 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).

  17. 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).

  18. 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).

  19. 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).

  20. 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).

  21. 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).

  22. 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).

  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-2012-02-08-47 | Sargent County - January 1964

    Major soils and some minor soils in the undulating Forman-Aastad soil association (Soil Survey of Sargent County, North Dakota; January 1964).

  28. ND-2012-02-08-48 | Sargent County - January 1964

    Rolling landscape in the Forman-Buse soil association (Soil Survey of Sargent County, North Dakota; January 1964).

  29. 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).

  30. ND-2012-02-08-55 | Stutsman County - June 1995

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

  31. 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).

  32. 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).

  33. 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).

  34. 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

  35. 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).

  36. SD-2010-11-01-02 | Brookings County - 2004

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

  37. 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).

  38. 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).

  39. 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).

  40. SD-2010-11-01-09 | Hamlin County - 2003

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

  41. SD-2010-11-01-15 | Spink County - 2009

    Pattern of soils and underlying materials in the Forman-Cresbard-Cavour association (Soil Survey of Spink County, South Dakota; 2009).

  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-2012-03-15-03 | Codington County - December 1966

    Diagram showing the relative position of the major soils in association 4 (Soil Survey of Codington County, SD; 1966).

  47. 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).

  48. SD-2012-03-15-18 | Day County - August 1997

    Typical pattern of soils and underlying material in the Nutley-Sinai and Poinsett-Waubay-Forman associations (Soil Survey of Day County, SD; 1997).

  49. 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).

  50. 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).

  51. SD-2012-03-15-25 | Deuel County - November 1997

    Typical pattern of soils and parent material in the Forman-Aastad-Buse association (Soil Survey of Deuel County, SD; 1997).

  52. SD-2012-03-15-27 | Deuel County - November 1997

    Typical pattern of soils and parent material in the Kranzburg-Brookings association (Soil Survey of Deuel County, SD; 1997).

  53. 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).

  54. 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).

  55. SD-2012-03-15-81 | Minnehaha County - June 1964

    Block diagram showing the geographical association of the soils in association 9. Here, the soils formed in loess and till (Soil Survey of Minnehaha County, SD; 1964).

Map Units

Map units containing BUSE 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
Hokans-Svea-Buse complex, 2 to 12 percent slopesJ118C2164631825152yw5fmn00519941:20000
Barnes-Svea-Buse complex, 3 to 15 percent slopesJ119D1147431825182yw63mn00519941:20000
Hokans-Buse complex, 2 to 6 percent slopes903B89013975762w0lzmn00519941:20000
Barnes-Buse complex, 6 to 12 percent slopes, moderately eroded903C237843975772w0lymn00519941:20000
Forman-Buse complex, 6 to 12 percent slopes, moderately eroded168C226963974872w8dymn00519941:20000
Forman-Buse complex, 12 to 20 percent slopes, moderately eroded168D211013974882w8dzmn00519941:20000
Formdale-Buse-Sandberg complex, 2 to 6 percent slopes1235B1015397448fbkxmn00519941:20000
Hokans-Svea-Buse complex, 2 to 12 percent slopesJ118C427631825332yw5fmn01119901:20000
Barnes-Svea-Buse complex, 3 to 15 percent slopesJ119D39231825362yw63mn01119901:20000
Byrne-Buse complex, 2 to 6 percent slopesJ34B1465024230462mbcsmn02319801:15840
Buse-Doland complex, 6 to 12 percent slopesJ259C378724230692mbdjmn02319801:15840
Hokans-Buse complex, 2 to 6 percent slopesJ35B1524230472w0lzmn02319801:15840
Hokans-Buse complex, 2 to 6 percent slopes903B496163570182w0lzmn02719801:20000
Barnes-Buse complex, 6 to 12 percent slopes, moderately eroded33C213403569592w0lymn02719801:20000
Hokans-Buse complex, 2 to 6 percent slopesBaB2384613972512w0lzmn04119701:12000
Barnes-Buse complex, 6 to 12 percent slopes, moderately erodedBaC2194913972522w0lymn04119701:12000
Forman-Buse complex, 6 to 12 percent slopes, moderately erodedFmC220663972802w8dymn04119701:12000
Hokans-Svea-Buse complex, 2 to 12 percent slopesJ118C831846312yw5fmn04119701:12000
Hokans-Svea-Buse complex, 2 to 12 percent slopesJ118C2042431825512yw5fmn05119741:20000
Barnes-Svea-Buse complex, 3 to 15 percent slopesJ119D749131825542yw63mn05119741:20000
Hokans-Buse complex, 2 to 6 percent slopes903B53143980662w0lzmn05119741:20000
Hokans-Buse complex, 2 to 6 percent slopes954B33213987352w0lzmn06719831:20000
Hokans-Buse complex, 2 to 6 percent slopes902B96044303532w0lzmn07319941:20000
Poinsett-Buse complex, 2 to 6 percent slopes741B6878430338gfswmn07319941:20000
Doland-Buse complex, 3 to 6 percent slopes891B5408430351gft9mn07319941:20000
Buse-Barnes complex, 2 to 12 percent slopes, extremely stony1865C3559430264gfqhmn07319941:20000
Buse-Doland complex, 6 to 12 percent slopes, eroded1309C1623430227gfp9mn07319941:20000
Forman-Buse complex, 6 to 12 percent slopes, moderately eroded915C212724303562w8dymn07319941:20000
Buse loam, 12 to 40 percent slopes, extremely stony1865F1168430265gfqjmn07319941:20000
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, eroded-Wilno complex, 12 to 18 percent slopesJ100D25701115044917m48mn08120071:12000
Buse, stony-Wilno complex, 25 to 40 percent slopesJ95F3420115028517lyzmn08120071:12000
Forman-Buse complex, 6 to 12 percent slopes, moderately erodedJ250C22730165023930t1jmn08120071:12000
Buse clay loam, 25 to 40 percent slopesJ73F2195991456128pgmn08120071:12000
Buse-Vienna complex, 6 to 12 percent slopes, moderately erodedJ92C21565991444128p2mn08120071:12000
Buse, stony-Wilno complex, 18 to 25 percent slopesJ95E1488115028417lyymn08120071:12000
Buse-Barnes-Arvilla complex, 6 to 12 percent slopes, moderately erodedJ235C2108214796071lnn8mn08120071:12000
Barnes, occasional saturation-Buse-Arvilla complex, 2 to 6 percent slopesJ232B106114794782yyj6mn08120071:12000
Buse, firm till-Wilno complex, 25 to 40 percent slopesJ238F105916502421sd6mmn08120071:12000
Buse, firm till-Wilno complex, 12 to 18 percent slopesJ238D296716502401sd6kmn08120071:12000
Buse clay loam, 12 to 18 percent slopes, moderately erodedJ73D2588991445128p3mn08120071:12000
Buse, moderately eroded-Sandberg complex, 12 to 18 percent slopesJ227D252114798881lnybmn08120071:12000
Buse clay loam, 18 to 25 percent slopesJ73E505991455128pfmn08120071:12000
Sandberg-Buse-Everts complex, 12 to 40 percent slopesJ83F298991460128plmn08120071:12000
Buse, firm till-Wilno complex, 18 to 25 percent slopesJ238E29216502411sd6lmn08120071:12000
Buse-Sandberg complex, 18 to 40 percent slopesJ227F23914798891lnycmn08120071:12000
Buse, firm till-Wilno-Lamoure, frequently flooded complex, 0 to 40 percent slopesJ242F18916502431sd6nmn08120071:12000
Barnes, occasional saturation-Buse-Svea complex, 1 to 6 percent slopesJ106B2215015423232yyjvmn08320081:12000
Barnes-Buse complex, 6 to 12 percent slopes, moderately erodedJ96C21297214862262wkqtmn08320081:12000
Forman-Buse complex, 6 to 12 percent slopes, moderately erodedJ250C27941165026330t1jmn08320081:12000
Buse, firm till-Wilno complex, 25 to 40 percent slopesJ238F290416502661sd7dmn08320081:12000
Buse, eroded-Wilno complex, 12 to 18 percent slopesJ100D2256714862311lwjymn08320081:12000
Buse, firm till-Wilno complex, 12 to 18 percent slopesJ238D2216616502641sd7bmn08320081:12000
Buse, stony-Wilno complex, 25 to 40 percent slopesJ95F126914862231lwjpmn08320081:12000
Buse, moderately eroded-Barnes, moderately eroded-Arvilla complex, 6 to 12 percent slopesJ235C2126914862282yyj7mn08320081:12000
Buse, firm till-Wilno complex, 18 to 25 percent slopesJ238E122316502651sd7cmn08320081:12000
Barnes, occasional saturation-Buse-Arvilla complex, 2 to 6 percent slopesJ232B100114862272yyj6mn08320081:12000
Buse, stony-Wilno complex, 18 to 25 percent slopesJ95E98214862221lwjnmn08320081:12000
Buse-Sandberg complex, 18 to 40 percent slopesJ227F38514862301lwjxmn08320081:12000
Buse, moderately eroded-Sandberg complex, 12 to 18 percent slopesJ227D235214862291lwjwmn08320081:12000
Buse loam, 18 to 25 percent slopes437E24185904520dh6mn08320081:12000
Arvilla-Barnes-Buse complex, 2 to 6 percent slopes, eroded904B223185905120dhdmn08320081:12000
Buse loam, 25 to 40 percent slopes437F9185904620dh7mn08320081:12000
Hokans-Buse complex, 2 to 6 percent slopes903B321033992602w0lzmn08719921:20000
Barnes-Buse complex, 6 to 12 percent slopes, moderately eroded903C263643992612w0lymn08719921:20000
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
Buse, eroded-Wilno complex, 12 to 18 percent slopesJ100D2188312923201dcrrmn10120081:12000
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
Buse clay loam, 25 to 40 percent slopesJ73F11799888871260lmn10120081:12000
Buse, stony-Wilno complex, 25 to 40 percent slopesJ95F102214816561lqscmn10120081:12000
Barnes-Buse loams, 6 to 12 percent slopes, eroded902C2354185945520dxfmn10120081:12000
Buse, moderately eroded-Sandberg complex, 12 to 18 percent slopesJ227D225314816591lqsgmn10120081:12000
Buse-Vienna complex, 6 to 12 percent slopes, moderately erodedJ92C22349888881260mmn10120081:12000
Buse clay loam, 12 to 18 percent slopes, moderately erodedJ73D21459888891260nmn10120081:12000
Buse-Barnes loams, 12 to 18 percent slopes913D100185945820dxjmn10120081:12000
Sandberg-Buse-Everts complex, 12 to 40 percent slopesJ83F9298890212612mn10120081:12000
Arvilla-Barnes-Buse complex, 2 to 6 percent slopes904B81185945620dxgmn10120081:12000
Arvilla-Barnes-Buse complex, 6 to 12 percent slopes904C26185945720dxhmn10120081:12000
Buse-Sioux complex, 12 to 18 percent slopes917D6185945920dxkmn10120081:12000
Hokans-Buse complex, 2 to 6 percent slopesBaB117223572012w0lzmn10719701:20000
Barnes-Buse complex, 6 to 12 percent slopes, moderately erodedBaC27803572032w0lymn10719701:20000
Hokans-Svea-Buse complex, 2 to 12 percent slopesJ118C1952431825692yw5fmn11119961:20000
Forman-Buse complex, 6 to 12 percent slopes, moderately eroded915C2172294359662w8dymn11119961:20000
Barnes-Buse complex, 6 to 12 percent slopes, moderately eroded903C294364359642w0lymn11119961:20000
Hokans-Buse complex, 2 to 6 percent slopes902B80394359612w0lzmn11119961:20000
Forman-Buse complex, 12 to 20 percent slopes, moderately eroded915D280364359672w8dzmn11119961:20000
Barnes-Svea-Buse complex, 3 to 15 percent slopesJ119D675531825722yw63mn11119961:20000
Barnes, occasional saturation-Buse complex, 3 to 6 percent slopesJ96B477712923052yyjgmn11720051:12000
Buse-Vienna complex, 6 to 12 percent slopes, moderately erodedJ92C23692780287v5ykmn11720051:12000
Barnes-Buse complex, 6 to 12 percent slopes, moderately erodedJ96C2328412923082wkqtmn11720051:12000
Sandberg-Buse-Everts complex, 12 to 40 percent slopesJ83F2510780524v666mn11720051:12000
Barnes, occasional saturation-Buse-Svea complex, 1 to 6 percent slopesJ106B250814815992yyjvmn11720051:12000
Buse clay loam, 12 to 18 percent slopes, moderately erodedJ73D22456780299v5yymn11720051:12000
Buse clay loam, 18 to 25 percent slopesJ73E853780267v5xxmn11720051:12000
Buse clay loam, 25 to 40 percent slopesJ73F724780268v5xymn11720051:12000
Buse, eroded-Wilno complex, 12 to 18 percent slopesJ100D249412923121dcrhmn11720051:12000
Buse, stony-Wilno complex, 25 to 40 percent slopesJ95F39912923101dcrfmn11720051:12000
Buse, stony-Wilno complex, 18 to 25 percent slopesJ95E39112923091dcrdmn11720051:12000
Hokans-Buse complex, 2 to 6 percent slopesBbB2843464013192w0lzmn12119681:20000
Barnes-Buse complex, 6 to 12 percent slopes, moderately erodedBbC2216584013202w0lymn12119681:20000
Hokans-Svea-Buse complex, 2 to 12 percent slopesJ118C185031825872yw5fmn12119681:20000
Forman-Buse complex, 2 to 6 percent slopesFrB23924013482w8dxmn12119681:20000
Barnes-Svea-Buse complex, 3 to 15 percent slopesJ119D30731825902yw63mn12119681:20000
Forman-Buse complex, 6 to 12 percent slopes, moderately erodedFrC2734013492w8dymn12119681:20000
Hokans-Buse complex, 2 to 6 percent slopes421B134964281422w0lzmn14519801:15840
Barnes-Buse complex, 6 to 12 percent slopes, moderately eroded421C62374281432w0lymn14519801:15840
Hokans-Svea-Buse complex, 2 to 12 percent slopesJ118C1068831826052yw5fmn14919661:15840
Hokans-Buse complex, 2 to 6 percent slopesBaB51484283122w0lzmn14919661:15840
Barnes-Svea-Buse complex, 3 to 15 percent slopesJ119D357831826082yw63mn14919661:15840
Barnes-Buse complex, 6 to 12 percent slopes, moderately erodedBbC220454283142w0lymn14919661:15840
Forman-Buse complex, 6 to 12 percent slopes, moderately erodedFuC2824283392w8dymn14919661:15840
Forman-Buse complex, 2 to 6 percent slopesFuB2794283382w8dxmn14919661:15840
Forman-Buse complex, 12 to 20 percent slopes, moderately erodedBuD274283222w8dzmn14919661:15840
Byrne-Buse complex, 2 to 6 percent slopesJ34B12426434815glg9mn15120001:12000
Hokans-Buse complex, 2 to 6 percent slopesJ35B103404348172w0lzmn15120001:12000
Buse-Barnes complex, 2 to 12 percent slopes, very boulderyJ62C1268434857glhnmn15120001:12000
Buse-Barnes complex, 12 to 40 percent slopes, very boulderyJ62F171434858glhpmn15120001:12000
Hokans-Buse complex, 2 to 6 percent slopes421B22234285422w0lzmn15319851:20000
Barnes-Buse complex, 6 to 12 percent slopes, moderately eroded421C3594285432w0lymn15319851:20000
Peever-Buse complex, 2 to 6 percent slopes822B2115357382czwgmn15519861:20000
Hokans-Svea-Buse complex, 2 to 12 percent slopesJ118C90931826232yw5fmn15519861:20000
Barnes-Svea-Buse complex, 3 to 15 percent slopesJ119D61631826252yw63mn15519861:20000
Buse-Formdale clay loams, 6 to 14 percent slopes, eroded915C2570357385czwkmn15519861:20000
Formdale-Buse complex, 2 to 6 percent slopes915B3683573842w8fxmn15519861:20000
Hokans-Buse complex, 2 to 6 percent slopes903B292953574632w0lzmn16719851:20000
Barnes-Svea-Buse complex, 3 to 15 percent slopesJ119D4231826292yw63mn16719851:20000
Hokans-Svea-Buse complex, 2 to 12 percent slopesJ118C1231826282yw5fmn16719851:20000
Barnes, occasional saturation-Buse-Svea complex, 1 to 6 percent slopesJ106B731316539652yyjvmn17319791:20000
Barnes-Buse complex, 6 to 12 percent slopes, moderately erodedJ96C2482416539412wkqtmn17319791:20000
Forman-Buse complex, 6 to 12 percent slopes, moderately erodedJ250C22289165027930t1jmn17319791:20000
Buse, stony-Wilno complex, 25 to 40 percent slopesJ95F115414816851lqt9mn17319791:20000
Buse, firm till-Wilno complex, 12 to 18 percent slopesJ238D287716502731sd7mmn17319791:20000
Buse, eroded-Wilno complex, 12 to 18 percent slopesJ100D284916539431sj20mn17319791:20000
Buse, firm till-Wilno complex, 25 to 40 percent slopesJ238F54216502751sd7pmn17319791:20000
Buse-Barnes-Arvilla complex, 6 to 12 percent slopes, moderately erodedJ235C252614816791lqt3mn17319791:20000
Buse, firm till-Wilno complex, 18 to 25 percent slopesJ238E52616502741sd7nmn17319791:20000
Buse, moderately eroded-Sandberg complex, 12 to 18 percent slopesJ227D246214816861lqtbmn17319791:20000
Buse-Sandberg complex, 18 to 40 percent slopesJ227F42014817101lqv3mn17319791:20000
Barnes, occasional saturation-Buse-Arvilla complex, 2 to 6 percent slopesJ232B34914817092yyj6mn17319791:20000
Buse, stony-Wilno complex, 18 to 25 percent slopesJ95E28914816821lqt6mn17319791:20000
Barnes-Buse loams, 3 to 6 percent slopesG144B14028525735682pwz2nd00319881:20000
Barnes-Buse-Langhei loams, 6 to 9 percent slopesG143C4829525735712pwz5nd00319881:20000
Edgeley-Kloten-Buse loams, 9 to 35 percent slopesG586F1303925736342q5rwnd00319881:20000
Buse-Barnes-Darnen loams, 9 to 35 percent slopesG147F1136025735632pwytnd00319881:20000
Barnes-Buse-Langhei loams, 9 to 15 percent slopesG143D827025735702pwz4nd00319881:20000
Buse-Barnes-La Prairie, occasionally flooded loams, 6 to 35 percent slopesG148F688025736732q61jnd00319881:20000
Buse-Barnes loams, 15 to 35 percent slopesG143F544325735692pwz3nd00319881:20000
Buse-Sioux complex, 9 to 35 percent slopesG680F375025736592q5w5nd00319881:20000
Buse-Barnes-Darnen loams, 3 to 9 percent slopesG147C368025735652pwywnd00319881:20000
Barnes-Buse-Parnell complex, 0 to 6 percent slopesG146B205225735672pwyznd00319881:20000
Lanona-Buse complex, 6 to 9 percent slopesG732C120525736622q5wsnd00319881:20000
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
Buse-Barnes loams, 15 to 35 percent slopesG143F329725737712pwz3nd0051:12000
Buse-Sioux complex, 9 to 35 percent slopesF680F314225876072q5lknd0051:12000
Barnes-Buse loams, 2 to 6 percent slopesF1144B257632476372ykx2nd0051:12000
Buse-Barnes loams, 3 to 9 percent slopesF1143C207032476382ykx3nd0051:12000
Buse-Coe complex, 9 to 35 percent slopesG681F204325737652q5w9nd0051:12000
Barnes-Buse loams, 3 to 6 percent slopesG144B201425737232pwz2nd0051:12000
Buse-Barnes-Darnen loams, 9 to 35 percent slopesF147F150225877022q4h8nd0051:12000
Barnes-Buse-Langhei loams, 6 to 9 percent slopesG143C103025737272pwz5nd0051:12000
Buse-Barnes-Darnen loams, 6 to 15 percent slopesF147D89425877282q4h2nd0051:12000
Buse-Barnes-Darnen loams, 3 to 9 percent slopesF147C65425875962q4h1nd0051:12000
Barnes-Buse-Langhei loams, 9 to 15 percent slopesG143D61425737162pwz4nd0051:12000
Brantford-Bottineau-Buse loams, 15 to 60 percent slopesF690F60625876312q5lrnd0051:12000
Barnes-Buse loams, 3 to 9 percent slopes, very stonyF612C55725877332q5dknd0051:12000
Buse-Barnes-La Prairie, occasionally flooded loams, 6 to 35 percent slopesF148F48125877382q4h9nd0051:12000
Buse-Sioux complex, 9 to 35 percent slopesG680F32225736812q5w5nd0051:12000
Buse-Barnes-La Prairie, occasionally flooded loams, 6 to 15 percent slopesF148D16125876042q4h4nd0051:12000
Edgeley-Kloten-Buse loams, 9 to 35 percent slopesG586F10225736992q5rwnd0051:12000
Buse-Barnes-La Prairie, occasionally flooded loams, 3 to 9 percent slopesF148C9825877662q4h3nd0051:12000
Lanona-Buse complex, 6 to 9 percent slopesF732C9425876702q5lynd0051:12000
Barnes-Buse-Langhei loams, 6 to 9 percent slopesF143C8025876452q4gsnd0051:12000
Buse-Barnes-Darnen loams, 3 to 9 percent slopesG147C7125736972pwywnd0051:12000
Barnes-Buse loams, 3 to 6 percent slopesF144B4925876622q4gwnd0051:12000
Buse-Barnes-Darnen loams, 9 to 35 percent slopesG147F4525737622pwytnd0051:12000
Dickey-Buse-Embden complex, 3 to 9 percent slopesG738C3725737892q5wynd0051:12000
Buse-Barnes-Darnen loams, 6 to 15 percent slopesG147D1325738132pwyvnd0051:12000
Buse-Barnes loams, 15 to 35 percent slopesF143F325876192q4gvnd0051:12000
Dickey-Buse-Embden complex, 3 to 9 percent slopesF738C225876602q5m3nd0051:12000
Bottineau-Buse loams, 9 to 25 percent slopesF184E575425858752q3x0nd00919811:20000
Barnes-Buse-Langhei loams, 6 to 9 percent slopesF143C505425859352q4gsnd00919811:20000
Barnes-Buse loams, 3 to 6 percent slopesF144B494325859472q4gwnd00919811:20000
Svea-Buse-Tonka complex, 0 to 6 percent slopesF145B258025860482q4gxnd00919811:20000
Buse-Barnes-Darnen loams, 6 to 15 percent slopesF147D249125860282q4h2nd00919811:20000
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
Buse-Barnes-Darnen loams, 9 to 35 percent slopesF147F132625859992q4h8nd00919811:20000
Buse-Barnes-La Prairie, occasionally flooded loams, 6 to 35 percent slopesF148F111025860382q4h9nd00919811:20000
Buse-Barnes-La Prairie, occasionally flooded loams, 6 to 15 percent slopesF148D62325858842q4h4nd00919811:20000
Buse-Barnes-La Prairie, occasionally flooded loams, 3 to 9 percent slopesF148C30225860732q4h3nd00919811:20000
Buse-Barnes-Parnell complex, 0 to 35 percent slopesF146F6625860622q4h0nd00919811:20000
Buse-Barnes-Parnell complex, 0 to 9 percent slopesF146C2825859622q4gznd00919811:20000
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
Buse-Barnes-Darnen loams, 6 to 15 percent slopesF147D425858512q4h2nd01319911:24000
Barnes-Buse loams, 3 to 6 percent slopesG144B3250325750672pwz2nd01719831:20000
Barnes-Buse-Langhei loams, 6 to 9 percent slopesG143C628025750712pwz5nd01719831:20000
Buse-Barnes-Darnen loams, 3 to 9 percent slopesG147C324325750492pwywnd01719831:20000
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
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-Buse-Parnell complex, 0 to 6 percent slopesG146B4825750762pwyznd01719831:20000
Svea-Buse loams, 3 to 6 percent slopesF154B4842025875372q4h7nd01919871:20000
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
Buse-Barnes loams, 15 to 35 percent slopesF143F2925875292q4gvnd01919871:20000
Barnes-Buse-Parnell complex, 0 to 6 percent slopesF146B1725875312q4gynd01919871:20000
Barnes-Buse loams, 3 to 6 percent slopesG144B1589025752492pwz2nd02119891:20000
Barnes-Buse-Langhei loams, 6 to 9 percent slopesG143C1144125752522pwz5nd02119891:20000
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
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-Buse loams, 3 to 9 percent slopes, very stonyG612C525753652q5sfnd02119891:20000
Edgeley-Kloten-Buse loams, 9 to 35 percent slopesG586F195925763342q5rwnd0271:12000
Barnes-Buse-Langhei loams, 6 to 9 percent slopesG143C155425753942pwz5nd0271:12000
Buse-Barnes-Darnen loams, 9 to 35 percent slopesG147F95825753872pwytnd0271:12000
Barnes-Buse-Langhei loams, 9 to 15 percent slopesG143D59225753932pwz4nd0271:12000
Buse-Barnes loams, 15 to 35 percent slopesG143F21825753922pwz3nd0271:12000
Barnes-Buse loams, 3 to 9 percent slopes, very stonyG612C20725763402q5sfnd0271:12000

Map of Series Extent

Approximate geographic distribution of the BUSE 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 2024-10-30).