Official Series Description


Lab Data Summary

Aggregate lab data for the BOELUS soil series. This aggregation is based on all pedons with a current taxon name of BOELUS, 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 BOELUS 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
102C04N0864S2004NE119005Boelus6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.9464455,-97.6372223

Water Balance

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

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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 BOELUS, 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. NE-2012-02-13-31 | Holt County - March 1983

    Typical pattern of soils in the Dunday-Pivot-Dunn association and their relationship to topography and parent material (Soil Survey of Holt County, Nebraska; March 1983).

  2. NE-2012-02-13-71 | Platte County - September 1988

    Typical landscape pattern of the soils and the underlying material in the Valentine-Thurman association (Soil Survey of Platte County, Nebraska; September 1988).

  3. NE-2012-02-13-80 | Rock County - May 1985

    Typical pattern of soils and parent material in the Valentine-Duday association (Soil Survey of Rock County, Nebraska; May 1985).

  4. NE-2012-02-13-81 | Rock County - May 1985

    Typical pattern of soils and parent material in the Pivot-Valentine association (Soil Survey of Rock County, Nebraska; May 1985).

  5. NE-2012-02-14-15 | Wheeler County - September 1988

    Pattern of soils and parent material in the Valentine association (Soil Survey of Wheeler County, Nebraska; September 1988).

  6. NE-2012-02-14-16 | Wheeler County - September 1988

    Pattern of soils and parent material in the Dunday-Valentine-Boelus association (Soil Survey of Wheeler County, Nebraska; September 1988).

Map Units

Map units containing BOELUS 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
Boelus loamy fine sand, 0 to 2 percent slopes6636367024269342vwbjne00319751:20000
Boelus loamy fine sand, 2 to 6 percent slopes663750024269352vwbkne00319751:20000
Boelus fine sand, 0 to 6 percent slopes66352253426933gb81ne00319751:20000
Boelus loamy sand, 6 to 11 percent slopes66421122159692dcwwne00319751:20000
Boelus loamy fine sand, 0 to 2 percent slopes66364284270222vwbjne01119661:20000
Boelus, Oneill, and Pivot complex, 0 to 3 percent slopes6645189617001021v230ne07920031:12000
Boelus loamy fine sand, 0 to 2 percent slopes6636176811000812vwbjne08919811:20000
Boelus loamy fine sand, 2 to 6 percent slopes663753481000822vwbkne08919811:20000
Boelus loamy sand, gravelly substratum, 0 to 3 percent slopes664331721000843c4jne08919811:20000
Boelus loamy sand, 6 to 11 percent slopes66428751000833c4hne08919811:20000
Boelus-Meadin complex, 6 to 11 percent slopes66486551000853c4kne08919811:20000
Libory-Boelus loamy fine sands43739114997273bs0ne09319681:12000
Libory-Boelus fine sands4372957997263brzne09319681:12000
Boelus loamy fine sand, 2 to 6 percent slopes6637213611442172vwbkne10719891:20000
Boelus loamy sand, 6 to 11 percent slopes6642674114421817dn8ne10719891:20000
Boelus loamy fine sand, 0 to 2 percent slopes663632611442162vwbjne10719891:20000
Boelus sandy substratum-Simeon loamy sands, 0 to 3 percent slopes6644150516995191v1h6ne11519861:20000
Boelus loamy fine sand, sandy substratum, 0 to 3 percent slopes663873316995181v1h5ne11519861:20000
Boelus loamy fine sand, 2 to 6 percent slopes663790914273892vwbkne11919811:20000
Valentine-Boelus loamy fine sands, 3 to 9 percent slopes4854783617096891vd28ne12119781:20000
Valentine-Boelus loamy fine sands, 0 to 3 percent slopes485392317096881vd27ne12119781:20000
Valentine-Boelus loamy fine sands, 3 to 9 percent slopes48543222290002dtg7ne12519581:20000
Boelus-Loretto complex, 2 to 6 percent slopes66478865427547gbwvne13919701:20000
Boelus-Loretto complex, 0 to 2 percent slopes66468044427546gbwtne13919701:20000
Boelus loamy fine sand, 2 to 6 percent slopes663782722171462vwbkne13919701:20000
Boelus loamy fine sand, 0 to 2 percent slopes663621622171812vwbjne13919701:20000
Boelus loamy sand, 6 to 11 percent slopes66422422171692df4lne13919701:20000
Boelus loamy fine sand, 2 to 6 percent slopes66374244276232vwbkne14119841:20000
Boelus loamy sand, 0 to 3 percent slopes664055581002313c98ne14919821:20000
Valentine-Boelus fine sands, 0 to 9 percent slopes485231001002673cbfne14919821:20000
Boelus loamy fine sand, 0 to 3 percent slopes663653516999801v1z2ne16319871:20000
Boelus loamy fine sand, 2 to 6 percent slopes663737874268162vwbkne16719801:20000
Boelus loamy fine sand, 2 to 6 percent slopes6637722173412vwbkne17919701:20000
Boelus loamy fine sand, 0 to 2 percent slopes6636521816998242vwbjne18319841:20000
Boelus loamy fine sand, 2 to 6 percent slopes6637248716998252vwbkne18319841:20000

Map of Series Extent

Approximate geographic distribution of the BOELUS 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 .