Official Series Description


Lab Data Summary

Aggregate lab data for the BOLENT soil series. This aggregation is based on all pedons with a current taxon name of BOLENT, 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 BOLENT 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
6686P026984NE031019Bolent6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.7844429,-101.0502777

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BOLENT 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 BOLENT 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 BOLENT 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 BOLENT 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 BOLENT 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 BOLENT series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the BOLENT 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.

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 BOLENT, 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-2010-09-28-01 | Dundy County -

    Typical pattern of soil and underlying material in the Sanborn-Haigler-Calamus and Bigbend-Munjor-McCook associations (Soil Survey of Dundy County, Nebraska).

  2. NE-2012-02-08-08 | Blaine County - September 1993

    Typical pattern of soils and parent material in the Almeria-Ipage-Fluvaquents association (Soil Survey of Blaine County, Nebraska; September 1993).

  3. NE-2012-02-13-54 | Loup County - October 1990

    Typical pattern of soils and parent material in the Ipage-Valentine-Elsmere and Almeria-Calamus-Bolent associations (Soil Survey of Loup County, Nebraska; October 1990).

  4. NE-2012-02-13-99 | Sherman County - May 1990

    Typical pattern of soils and parent material in the Loup-Bolent-Barney and Gibbon-Wann-Saltine associations (Soil Survey of Sherman County, Nebraska; May 1990).

Map Units

Map units containing BOLENT 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
Platte-Bolent complex, occasionally flooded857041222161212dd1sne00119701:20000
Bolent loam, occasionally flooded42221322160832dd0kne00119701:20000
Bolent loamy sand, occasionally flooded4225140616994752zzbxne00919881:20000
Bolent-Calamus loamy sands, rarely flooded42706326056982qjkyne00919881:20000
Bolent fine sandy loam, occasionally flooded42201176999802zzbrne01719871:20000
Platte-Bolent complex, occasionally flooded8570318122282102dsmrne01919671:20000
Bolent fine sandy loam, occasionally flooded4220133417000801v229ne01919671:20000
Bolent loamy sand, occasionally flooded42253122282012dsmgne01919671:20000
Bolent-Calamus, calcareous loamy fine sands, occasionally flooded422837391003543cf7ne03119951:24000
Bolent loamy fine sand, channeled, occasionally flooded422432001003522zzbvne03119951:24000
Bolent fine sandy loam, rarely flooded42215801003532zzbsne03119951:24000
Bolent-Almeria complex, channeled, frequently flooded42265626686632zzbtne03119951:24000
Calamus-Bolent loamy fine sands, channeled, occasionally flooded42371926686641v26gne03119951:24000
Bolent loamy fine sand, occasionally flooded42231922299702dvgjne04519731:20000
Bolent-Almeria complex, channeled, frequently flooded4226865516990831v114ne05719951:24000
Platte-Bolent complex, occasionally flooded85701844117001711v257ne07920031:12000
Bolent-Calamus complex, occasionally flooded4227495717001061v234ne07920031:12000
Barney-Bolent complex, frequently flooded6322186917001001v22yne07920031:12000
Bolent loam, occasionally flooded4222112917001031v231ne07920031:12000
Bolent loamy sand, occasionally flooded422550617001051v233ne07920031:12000
Bolent fine sandy loam, occasionally flooded422041417001041v232ne07920031:12000
Bolent-Almeria complex, channeled, frequently flooded42266422288482dt9bne08719651:20000
Bolent-Almeria complex, channeled, frequently flooded422694926057052zzbtne09119611:24000
Calamus-Bolent loamy fine sands, channeled, occasionally flooded423745226686751v26gne09119611:24000
Bolent loamy sand, occasionally flooded422514722288992dtbzne09319681:12000
Barney-Bolent complex, channeled, occasionally flooded63212072114569117g5sne10319771:20000
Bolent loamy fine sand, occasionally flooded4223135016995202zzbwne11519861:20000
Bolent loamy sand, occasionally flooded42256122198292zzbxne11519861:20000
Calamus-Bolent loamy fine sands, channeled, occasionally flooded423724717002091v26gne11719661:31680
Platte-Bolent complex, occasionally flooded857067422282642dsphne12119781:20000
Bolent fine sandy loam, occasionally flooded4220622282522dsp3ne12119781:20000
Barney-Bolent complex, frequently flooded6322322282572dsp8ne12119781:20000
Bolent loamy fine sand, occasionally flooded422326761005632zzbwne16119921:20000
Bolent loamy sand, occasionally flooded4225248516999811v1z3ne16319871:20000
Valentine-Bolent complex, 0 to 6 percent slopes48552671700016319ngne16319871:20000
Bolent-Calamus loamy sands, rarely flooded4270145926056682qjkyne17119631:24000
Bolent-Almeria complex, channeled, frequently flooded4226100926056672zzbtne17119631:24000
Bolent-Calamus, calcareous loamy fine sands, 0 to 2 percent slopesT025A26213900181hnf9sd00720041:20000
Bolent loamy fine sand, channeled, occasionally floodedT024A5413900172zzbvsd00720041:20000
Bolent fine sandy loam, rarely floodedT023A3513900162zzbssd00720041:20000
Bolent loamy fine sand, channeled, occasionally floodedT024A26513915672zzbvsd12119671:31680
Bolent-Calamus, calcareous loamy fine sands, 0 to 2 percent slopesT025A16813915681hq19sd12119671:31680
Bolent fine sandy loam, rarely floodedT023A3913915662zzbssd12119671:31680

Map of Series Extent

Approximate geographic distribution of the BOLENT 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 .