Official Series Description


Lab Data Summary

Aggregate lab data for the BELFORE soil series. This aggregation is based on all pedons with a current taxon name of BELFORE, 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 BELFORE 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
102C40A2231S1954NE119001Belfore5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.8300018,-97.5772247
102C40A2232S1954NE141001Belfore5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.6708336,-97.5902786
102C40A2058S1954NE179001Belfore6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.1769409,-96.9645004
102C40A2229S1955NE039001Belfore5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.9599991,-96.6483307
102C40A2230S1955NE039002Belfore6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0052795,-96.7480545
102C78P0174S1976NE167025BELFORE6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.8011093,-97.2816696

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BELFORE 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 BELFORE 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 BELFORE 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 BELFORE 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with BELFORE 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 BELFORE 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 BELFORE 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 BELFORE, 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-2012-02-10-15 | Colfax County - January 1982

    Typical pattern of soils and parent material in the Moody-Alcester association (Soil Survey of Colfax County, Nebraska; January 1982).

  2. NE-2012-02-13-61 | Nance County - July 1960

    General soil areas of Nance County from a "bird's-eye view" (Soil Survey of Nance County, Nebraska; July 1960).

  3. NE-2012-02-13-62 | Nance County - July 1960

    Principal soils of Nance County (Soil Survey of Nance County, Nebraska; July 1960).

  4. NE-2012-02-13-63 | Nance County - July 1960

    A cross section along the eastern side of Nance County showing the relationship of the soils to the geological materials (Soil Survey of Nance County, Nebraska; July 1960).

  5. NE-2012-02-13-70 | Platte County - September 1988

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

Map Units

Map units containing BELFORE 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
Belfore silty clay loam, 0 to 2 percent slopes6628724222166492vwbrne01119661:20000
Belfore silty clay loam, terrace, 0 to 2 percent slopes650590534278042vwbsne02119781:20000
Belfore silty clay loam, 0 to 2 percent slopes662857134278032vwbrne02119781:20000
Belfore silty clay loam, 0 to 2 percent slopes662840694278732vwbrne03719801:20000
Belfore silty clay loam, terrace, 0 to 2 percent slopes650524794278742vwbsne03719801:20000
Belfore silty clay loam, 0 to 2 percent slopes6628293854277572vwbrne03919731:20000
Belfore silty clay loam, terrace, 0 to 2 percent slopes650523654277582vwbsne03919731:20000
Belfore-Moody silty clay loams, 1 to 3 percent slopes663011022170062zp2tne03919731:20000
Belfore-Moody silty clay loams, 1 to 3 percent slopes66302722170712zp2tne05119751:20000
Belfore silty clay loam, 0 to 2 percent slopes662883014268702vwbrne05319751:20000
Belfore silty clay loam, terrace, 0 to 2 percent slopes65052222170792vwbsne05319751:20000
Belfore silty clay loam, 0 to 2 percent slopes6628140624273852vwbrne11919811:20000
Belfore silty clay loam, 0 to 2 percent slopes66281029122289832vwbrne12519581:20000
Belfore silty clay loam, 0 to 2 percent slopes6628332804276182vwbrne14119841:20000
Belfore silty clay loam, 0 to 2 percent slopes662840344268132vwbrne16719801:20000
Belfore-Moody silty clay loams, 0 to 1 percent slopes66291247427695gc1mne17319661:20000
Belfore silty clay loam, 0 to 2 percent slopes662837322172872vwbrne17319661:20000
Belfore-Moody silty clay loams, 1 to 3 percent slopes663010322172972zp2tne17319661:20000
Belfore silty clay loam, 0 to 2 percent slopes662822203955242vwbrne17720001:12000
Belfore silty clay loam, terrace, 0 to 2 percent slopes65055963954632vwbsne17720001:12000
Belfore silty clay loam, 0 to 2 percent slopes662879724267742vwbrne17919701:20000
Belfore-Moody silty clay loams, 1 to 3 percent slopes663038664267752zp2tne17919701:20000

Map of Series Extent

Approximate geographic distribution of the BELFORE 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 .