Official Series Description


Lab Data Summary

Aggregate lab data for the STUNNER soil series. This aggregation is based on all pedons with a current taxon name of STUNNER, 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 STUNNER 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
5179P036779CO023004Stunner7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.101944,-105.5144424

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the STUNNER 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 STUNNER 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 STUNNER 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 STUNNER 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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Competing Series

Soil series competing with STUNNER 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 STUNNER 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 STUNNER 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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Soil series sharing subgroup-level classification with STUNNER, 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 STUNNER 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
Stunner loam, 3 to 6 percent slopesStC6391508501k248co02320091:24000
Stunner loam, 1 to 3 percent slopesStB3500508500k247co02320091:24000
Stunner loam523100498623jqvmco63019751:24000
Stunner loam, 1 to 3 percent slopesSnB3617498684jqxlco63119721:24000
Stunner loam, 3 to 6 percent slopesSnC780498685jqxmco63119721:24000
Stunner sandy loam, 1 to 8 percent slopes181603106845jpb1co6481:24000
Dahlquist-Stunner very cobbly loams, 15 to 50 percent slopes283233497851jq1qco64919771:24000
Dahlquist-Stunner very cobbly loams, 3 to 15 percent slopes27813497850jq1pco64919771:24000
Stunner, moist-Emlin complex, 1 to 12 percent slopes1827329497149jpb2co68619921:31680
Stunner sandy loam, 1 to 8 percent slopes1812566497148jpb1co68619921:31680
Stunner-Travelers, extremely stony-Luhon association, 2 to 8 percent slopesSVC53382507888k1hhnm67019761:24000
Raton-Stunner-Rock outcrop association, 3 to 40 percent slopesRBE10321507874k1h1nm67019761:24000
Stunner-Luhon association, 1 to 8 percent slopesSUC8019507887k1hgnm67019761:24000
Stunner cobbly loam, 1 to 5 percent slopesStC7790507895k1hqnm67019761:24000
Stunner cobbly loam, 1 to 15 percent slopesStC295727213552tl79nm6721:24000
Raton-Stunner association, moderately steepRBE27327702032v5pvnm6721:24000
Stunner loam, 3 to 6 percent slopesSnC11427701492tl8nnm6721:24000
Stunner sandy loam, 2 to 8 percent slopes22840634501795jv4ywy60119911:24000
Stunner-Borollic Camborthids complex, 2 to 5 percent slopes22921177501797jv50wy60119911:24000
Stunner-Tisworth-Blazon complex, 1 to 6 percent slopes23011450501800jv53wy60119911:24000
Stunner-Urban land complex, 0 to 6 percent slopes231129501802jv55wy60119911:24000
Alcova-Stunner complex, 3 to 15 percent slopes10429330502182jvkfwy62519851:24000
Stunner-Pinelli complex, 3 to 15 percent slopes2807242502416jvszwy62519851:24000

Map of Series Extent

Approximate geographic distribution of the STUNNER 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 .