Official Series Description


Lab Data Summary

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

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
53B72ND05500172ND055001Bowdle4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.2730556,-100.8
5481ND03700681ND037006Bowdle3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.0205556,-101.5563889

Water Balance

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

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

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Geomorphic description summaries for the BOWDLE series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

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

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Competing Series

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

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Select annual climate data summaries for the BOWDLE 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 BOWDLE series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

There are insufficient data to create the 2D hillslope position figure.

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

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

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

Soil series sharing subgroup-level classification with BOWDLE, 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. ND-2012-02-07-05 | Adams County - September 1987

    Typical pattern of soils and underlying material in the Straw-Parshall-Bowdle association (Soil Survey of Adams County, North Dakota; September 1987).

  2. ND-2012-02-08-08 | Grant County - September 1988

    Typical pattern of soils and parent material in the Ruso-Straw-Bowdle association (Soil Survey of Grant County, North Dakota; September 1988).

  3. ND-2012-02-08-14 | Hettinger County - May 1990

    Typical pattern of soils and underlying material in the Korchea-Bowdle-Parshall association (Soil Survey of Hettinger County, North Dakota; May 1990).

  4. ND-2012-02-08-29 | McIntosh County - 2001

    Typical pattern of soils and underlying materials in the Amor-Arnegard-Werner association (Soil Survey of McIntosh County, North Dakota; 2001).

Map Units

Map units containing BOWDLE 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
Lehr-Bowdle loams, 2 to 6 percent slopesE4542B17826617232qkxmnd01519671:20000
Bowdle-Lehr loams, 0 to 2 percent slopesE4541A11126617222qkxlnd01519671:20000
Bowdle-Lehr loams, 2 to 6 percent slopesC814B925956362q3gmnd01519671:20000
Lehr-Bowdle loams, 2 to 6 percent slopesE4542B127584922qkxmnd02519811:20000
Bowdle-Lehr loams, 2 to 6 percent slopesC814B953025954432q3gmnd02919791:20000
Bowdle-Lehr loams, 0 to 2 percent slopesC814A924825954412q2h1nd02919791:20000
Bowdle-Lehr loams, 0 to 2 percent slopesE4541A422526618102qkxlnd02919791:20000
Lehr-Bowdle loams, 2 to 6 percent slopesE4542B183326618112qkxmnd02919791:20000
Bowdle loam, 0 to 2 percent slopesC810A116525643072q3glnd02919791:20000
Lehr-Bowdle loams, 6 to 9 percent slopesE4542C57326618122qkxnnd02919791:20000
Bowdle loam, 2 to 6 percent slopesC810B27225642902pwdsnd02919791:20000
Lehr-Bowdle loams, 2 to 6 percent slopesC817B3225958012q2h5nd02919791:20000
Bowdle loam, 0 to 2 percent slopesC810A669425643952q3glnd04319851:20000
Bowdle-Lehr loams, 0 to 2 percent slopesC814A2625966482q2h1nd04319851:20000
Bowdle-Lehr loams, 0 to 2 percent slopesC814A1419325664812q2h1nd04719921:20000
Lehr-Bowdle loams, 2 to 6 percent slopesC817B692825664822q2h5nd04719921:20000
Bowdle loam, 0 to 2 percent slopesC810A152525664892q3glnd04719921:20000
Bowdle-Lehr loams, 0 to 2 percent slopesE4541A126126618762qkxlnd04719921:20000
Lehr-Bowdle loams, 2 to 6 percent slopesE4542B34626618772qkxmnd04719921:20000
Bowdle-Lehr loams, 2 to 6 percent slopesC814B1025967002q3gmnd04719921:20000
Bowdle-Lehr loams, 0 to 2 percent slopesC814A2624925665712q2h1nd05119921:24000
Lehr-Bowdle loams, 2 to 6 percent slopesC817B1184525665722q2h5nd05119921:24000
Bowdle-Lehr loams, 0 to 2 percent slopesE4541A65026620082qkxlnd05119921:24000
Lehr-Bowdle loams, 2 to 6 percent slopesE4542B38626620092qkxmnd05119921:24000
Bowdle-Lehr loams, 2 to 6 percent slopesC814B2225967332q3gmnd05119921:24000
Lehr-Bowdle loams, 2 to 6 percent slopesE4542B237026994032qkxmnd05320031:24000
Bowdle-Lehr loams, 0 to 2 percent slopesE4541A91626994022qkxlnd05320031:24000
Bowdle loam, 0 to 2 percent slopesC810A1880525666542q3glnd05519741:20000
Bowdle-Lehr loams, 2 to 6 percent slopesC814B849225955392q3gmnd05519741:20000
Lehr-Bowdle loams, 2 to 6 percent slopesE4542B50626624842qkxmnd05519741:20000
Bowdle-Lehr loams, 0 to 2 percent slopesE4541A47626624832qkxlnd05519741:20000
Lehr-Bowdle loams, 2 to 6 percent slopesE4542B215826992822qkxmnd05719761:20000
Bowdle-Lehr loams, 0 to 2 percent slopesE4541A158726992492qkxlnd05719761:20000
Lehr-Bowdle loams, 6 to 9 percent slopesE4542C45326992832qkxnnd05719761:20000
Bowdle loam, 0 to 2 percent slopesC810A805325667472q3glnd06119881:24000
Lehr-Bowdle loams, 2 to 6 percent slopesE4542B55026625312qkxmnd06119881:24000
Bowdle-Lehr loams, 0 to 2 percent slopesE4541A41726625302qkxlnd06119881:24000
Bowdle-Lehr loams, 0 to 2 percent slopesC814A8825670842q2h1nd06119881:24000
Bowdle-Lehr loams, 0 to 2 percent slopesE4541A175125260022qkxlnd06519711:20000
Lehr-Bowdle loams, 2 to 6 percent slopesE4542B134425260032qkxmnd06519711:20000
Lehr-Bowdle loams, 6 to 9 percent slopesE4542C36125260042qkxnnd06519711:20000
Bowdle-Lehr loams, 0 to 2 percent slopesC814A276725668312q2h1nd09319901:24000
Bowdle-Lehr loams, 2 to 6 percent slopesC814B173325668392q3gmnd09319901:24000
Bowdle loam, 0 to 2 percent slopesC810A4525670602q3glnd10119671:20000
Bowdle-Lehr loams, 2 to 6 percent slopesC814B425670612q3gmnd10119671:20000
Bowdle loam, 0 to 2 percent slopes2813692339086ccv8nd10519931:24000
Bowdle loam, 0 to 2 percent slopesC810A329925670082q3glnd10519931:24000
Lehr-Bowdle loams, 2 to 6 percent slopesE4542B76626625882qkxmnd10519931:24000
Bowdle-Lehr loams, 0 to 2 percent slopesE4541A75526625872qkxlnd10519931:24000
Lehr-Bowdle loams, 2 to 6 percent slopes, shalyC809B85227656042rsqlsd01319871:20000
Lehr-Bowdle loams, 0 to 2 percent slopesC817A17027656052rsqqsd01319871:20000
Lehr-Bowdle loams, 2 to 6 percent slopesC817B16427655622q2h5sd01319871:20000
Bowdle loam, 0 to 2 percent slopesC810A3727655642q3glsd01319871:20000
Bowdle loam, 0 to 2 percent slopesC810A659927978762q3glsd02119781:20000
Bowdle loam, 2 to 6 percent slopesC810B481427978562pwdssd02119781:20000
Bowdle loam, 3 to 6 percent slopes34B837354706cx34sd02119781:20000
Bowdle loam, 0 to 3 percent slopes34A366354705cx33sd02119781:20000
Bowdle-Wabek loams, 2 to 6 percent slopesC811B6227979382rsqmsd02119781:20000
Bowdle-Lehr loams, 0 to 2 percent slopesC814A4427978682q2h1sd02119781:20000
Bowdle-Wabek loams, 6 to 9 percent slopesC811C827979392rsqnsd02119781:20000
Wabek-Bowdle complex, 2 to 9 percent slopesC878C527979402rsqzsd02119781:20000
Lehr-Bowdle loams, 2 to 6 percent slopesC817B443727985532q2h5sd04519731:20000
Wabek-Bowdle complex, 2 to 9 percent slopesC878C265327986142rsqzsd04519731:20000
Bowdle loam, 0 to 2 percent slopesC810A147827985572q3glsd04519731:20000
Bowdle loam, 2 to 6 percent slopesC810B114727985482pwdssd04519731:20000
Wabek-Bowdle loams, 6 to 15 percent slopesWbC148354291cwnrsd04519731:20000
Wabek-Bowdle complex, 6 to 15 percent slopesC878D5227985872qyg4sd04519731:20000
Wabek-Bowdle complex, 2 to 6 percent slopesC878B1627986052rsq0sd04519731:20000
Bowdle-Wabek loams, 6 to 9 percent slopesC811C627986122rsqnsd04519731:20000
Bowdle loam, 0 to 2 percent slopesC810A293827986272q3glsd04919811:20000
Wabek-Bowdle loams, 3 to 9 percent slopesWbC338355200cxm2sd04919811:20000
Wabek-Bowdle complex, 2 to 6 percent slopesC878B31927986752rsq0sd04919811:20000
Wabek-Bowdle complex, 2 to 9 percent slopesC878C4627986792rsqzsd04919811:20000
Lehr-Bowdle loams, 2 to 6 percent slopesC817B2798127986982q2h5sd08919801:20000
Wabek-Bowdle complex, 2 to 9 percent slopesC878C1789727987802rsqzsd08919801:20000
Bowdle loam, 0 to 2 percent slopesC810A501127987062q3glsd08919801:20000
Bowdle loam, 2 to 6 percent slopesC810B80927986892pwdssd08919801:20000
Wabek-Bowdle complex, 6 to 15 percent slopesC878D21927987542qyg4sd08919801:20000
Bowdle-Lehr loams, 0 to 2 percent slopesC814A7927986962q2h1sd08919801:20000
Lehr-Bowdle loams, 0 to 2 percent slopesC817A1827987782rsqqsd08919801:20000
Bowdle loam, 0 to 2 percent slopesC810A145527994542q3glsd10719831:20000
Bowdle loam, 2 to 6 percent slopesC810B49527994462pwdssd10719831:20000
Lehr-Bowdle loams, 2 to 6 percent slopesC817B11727994492q2h5sd10719831:20000
Bowdle-Lehr loams, 2 to 6 percent slopesC814B10927994552q3gmsd10719831:20000
Lehr-Bowdle loams, 0 to 2 percent slopesC817A54227995222rsqqsd11519971:24000
Lehr-Bowdle loams, 2 to 6 percent slopesC817B48227994922q2h5sd11519971:24000
Bowdle loam, 0 to 2 percent slopesC810A449928000832q3glsd12919751:20000
Bowdle loam, 2 to 6 percent slopesC810B273928000702pwdssd12919751:20000
Bowdle-Wabek loams, 2 to 6 percent slopesC811B225128001462rsqmsd12919751:20000
Bowdle-Wabek loams, 6 to 9 percent slopesC811C196828001472rsqnsd12919751:20000
Bowdle-Wabek loams, 6 to 9 percent slopesBxC668354480cwvvsd12919751:20000
Lehr-Bowdle loams, 2 to 9 percent slopesLbB504354506cwwpsd12919751:20000
Bowdle-Wabek loams, 2 to 6 percent slopesBxB371354479cwvtsd12919751:20000
Bowdle-Wabek loams, 9 to 15 percent slopesBxD340354481cwvwsd12919751:20000
Lehr-Bowdle loams, 2 to 6 percent slopesC817B15728000782q2h5sd12919751:20000
Wabek-Bowdle complex, 2 to 9 percent slopesC878C8328001482rsqzsd12919751:20000
Wabek-Bowdle complex, 6 to 15 percent slopesC878D6628001172qyg4sd12919751:20000

Map of Series Extent

Approximate geographic distribution of the BOWDLE 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 .