Official Series Description


Lab Data Summary

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

Competing Series

Soil series competing with DELPHILL 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 DELPHILL 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 DELPHILL 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 .

Click the image to view it full size.

Click the image to view it full size.

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 DELPHILL, 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 DELPHILL 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
Delphill-Abor complex, 5 to 20 percent slopesDhD52751475034yh5mt60919711:24000
Delphill loam, 2 to 5 percent slopesDeB20361475024yh4mt60919711:24000
Monbutte-Delphill families, complex, 3 to 15 percent slopes921346815245wcb7ut6511:24000
Blazon-Delphill complex, 8 to 40 percent slopes3761151324840832pcwqwy0411:24000
Delphill-Alldown-Megonot association, 3 to 25 percent slopes119552186261620j6dwy0411:24000
Blazon-Delphill complex, 20 to 45 percent slopes11616287501643jv01wy60119911:24000
Delphill-Blazon complex, 3 to 20 percent slopes15015675501688jv1hwy60119911:24000
Delphill-Blazon loams, 5 to 30 percent slopes1708538502258jvmwwy62519851:24000
Blazon-Delphill complex, 20 to 45 percent slopes111629598342x8p2wy6301:24000
Delphill-Blazon complex, 3 to 20 percent slopes -- draft452408725730322x8pjwy6301:24000
Delphill-Blazon association. -- draft39045525730412r81wwy6301:24000
Forelle-Blazon, rubbly surface-Cushool complex, 4 to 35 percent slopes5604380014755881ljgmwy6351:24000
Blazon-Delphill complex, 6 to 30 percent slopes1067613503942jxd6wy63819901:24000
Delphill-Iyers-Poposhia complex, 3 to 25 percent slopes1191478503962jxdvwy63819901:24000
Delphill clay loam, 3 to 10 percent slopes714211590545bhswy67719751:24000
Hangmans-Delphill-Rangecreek complex, 15 to 35 percent slopes411332223302ztm2wy7371:24000
Cragosen, extremely flaggy surface-Delphill, rubbly surface, complex, 8 to 35 percent slopes420232222712zdt5wy7371:24000
Piceance-Delphill family-Delplain complex, 4 to 35 percent slopes4228322244030j6mwy7371:24000
Colhill family-Delphill-Manns family, complex, 4 to 20 percent slopes4411322249231335wy7371:24000
Delphill-Blazon association, 6 to 30 percent slopes -- draft20796825723482pb9pwy7371:24000

Map of Series Extent

Approximate geographic distribution of the DELPHILL 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 .