Official Series Description


Lab Data Summary

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

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BROADWATER 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 BROADWATER 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 BROADWATER 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 BROADWATER 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 BROADWATER 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 BROADWATER series and competing. 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 BROADWATER 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 .

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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 BROADWATER, 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-2012-02-13-03 | Garden County - 1999

    Typical pattern of the soils and underlying material in the Ashollow-Tassel association (Soil Survey of Garden County, Nebraska; 1999).

Map Units

Map units containing BROADWATER 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
Broadwater loamy sand, channeled, occasionally flooded5607158922281452dsknne00719881:20000
Broadwater loamy sand, channeled, occasionally flooded560772422196842dhrqne03319891:20000
Broadwater loamy sand, frequently flooded560510522197002dhs7ne03319891:20000
Broadwater loamy sand, channeled, frequently flooded56069522197032dhsbne03319891:20000
Chappell-Bayard-Broadwater complex, 0 to 2 percent slopes13728122196772dhrhne03319891:20000
Chappell-Alice-Broadwater complex, 0 to 3 percent slopes13716322293622dttxne03319891:20000
Chappell-Alice-Broadwater complex, 0 to 3 percent slopes13711435716988001v0r0ne04920001:24000
Broadwater loamy sand, frequently flooded5605436416987981v0qyne04920001:24000
Broadwater loamy sand, channeled, frequently flooded56061024016987311v0nsne06919951:20000
Chappell-Alice-Broadwater complex, 0 to 3 percent slopes1371157922195772dhn8ne10119901:20000
Broadwater loamy sand, channeled, frequently flooded560613122195902dhnpne10119901:20000
Broadwater loamy sand, frequently flooded56052522195832dhngne10119901:20000
Chappell-Bayard-Broadwater complex, 0 to 2 percent slopes13721094916925401tt72ne10520041:24000
Broadwater loamy sand, channeled, occasionally flooded5607720916925381tt70ne10520041:24000
Broadwater loamy sand, channeled, occasionally flooded5607121022203882djhfne12319811:20000
Broadwater loamy sand, channeled, frequently flooded560641922203642djgnne12319811:20000

Map of Series Extent

Approximate geographic distribution of the BROADWATER 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 .