Official Series Description


Lab Data Summary

Aggregate lab data for the BANDY soil series. This aggregation is based on all pedons with a current taxon name of BANDY, 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 BANDY 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 BANDY 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 BANDY 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 BANDY 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 BANDY 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 BANDY 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 BANDY 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 BANDY 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.

Click the image to view it full size.

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

Soil series sharing subgroup-level classification with BANDY, 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

No block diagrams are available.

Map Units

Map units containing BANDY 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
Bandy-Blossberg complex, o to 2 percent slopes, rarely flooded844A23801446104vgvmt62119971:24000
Nirling-Bandy complex, 0 to 4 percent slopes, rarely flooded624B14101445324vdbmt62119971:24000
Bandy loam, 0 to 4 percent slopes, rarely flooded814B7141445904vg6mt62119971:24000
Bandy loam, 0 to 4 percent slopes614B5111445294vd7mt62119971:24000
Bandy-Riverwash-Bonebasin complex, 0 to 2 percent slopes606A837615561856xymt62219971:24000
Bandy-Bonebasin loams, 0 to 2 percent slopes605A171115561756xxmt62219971:24000
Bandy-Blossberg complex, 0 to 2 percent slopes, rarely flooded844A17617030121v53wmt63520061:24000
Nirling-Bandy complex, 0 to 4 percent slopes, rarely flooded624B3317030031v53lmt63520061:24000
Histic Endoaquolls-Curlew-Water complex, 0 to 2 percent slopes147A22324226132m9xtmt63819851:24000
Overwhich-Bandy complex, 0 to 2 percent slopes154A19224226172m9xymt63819851:24000
Victor-Bandy complex, 0 to 8 percent slopes345C4924226572m9z7mt63819851:24000
Bandy-Nirling complex, 0 to 4 percent slopes320B1602633670p8czmt64520131:12000
Bandy, occasionally flooded-Curlew, rarely flooded-Water complex, 0 to 2 percent slopes147A971633608p89zmt64520131:12000
Victor-Bandy complex, 0 to 8 percent slopes345C877633687p8djmt64520131:12000
Overwhich-Bandy complex, 0 to 2 percent slopes, rarely flooded154A87215855559zpmt64520131:12000

Map of Series Extent

Approximate geographic distribution of the BANDY 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 .