Official Series Description


Lab Data Summary

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

Soil series sharing subgroup-level classification with TRIDELL, 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 TRIDELL 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
Tridell-Brownsto stony sandy loams, 12 to 50 percent slopes, extremely stony10623680497935jq4fco65519841:24000
Morval-Tridell complex, 12 to 50 percent slopes874652498032jq7kco65519841:24000
Morval-Tridell complex, 6 to 25 percent slopes4515200496787jnydco68319771:24000
Rock outcrop-Boxring-Tridell complex, 10 to 50 percent slopes2662870629967p4jjco68619921:31680
Tridell-Twobears complex, 4 to 40 percent slopes, extremely stony237332125102822q826ut0131:24000
Tridell very cobbly loam, 4 to 25 percent slopes236297025102812q825ut0131:24000
Tridell-Waterhill complex, 2 to 25 percent slopes239172624931902pptnut0131:24000
Tridell gravelly loam, 4 to 15 percent slopes, extremely stony235133229586722swxhut0131:24000
Gash, frequently flooded-Tridell-Lakebench families complex, 2 to 25 percent slopesANF250129729586432wrg2ut0131:24000
Tridell-Rock outcrop complex, 10 to 50 percent slopes, extremely stony23819124931892pptput0131:24000
Tridell-Waterhill association, 3 to 25 percent slopes2398859505516jz0zut04719991:24000
Rock outcrop-Boxring-Tridell complex, 10 to 50 percent slopes1958025505467jyzdut04719991:24000
Tridell-Rock outcrop association, 25 to 50 percent slopes2386688505515jz0yut04719991:24000
Tridell-Ironco association, 15 to 50 percent slopes2373611505514jz0xut04719991:24000
Tridell very cobbly loam, 4 to 25 percent slopes236910505513jz0wut04719991:24000
Tridell cobbly loam, 4 to 15 percent slopes235837505512jz0vut04719991:24000
Tridell cobbly loam, 4 to 25 percent slopes1486967504379jxv9ut63619841:24000
Tridell gravelly loam, moist, 4 to 25 percent slopes1476565504378jxv8ut63619841:24000
Tridell moist-Rock outcrop complex, 25 to 50 percent slopes1493313504380jxvbut63619841:24000
Tridell loam, 2 to 4 percent slopes146584504377jxv7ut63619841:24000
Caballo, extremely stony-Tridell, rubbly-Beenom, rubbly families, complex, 15 to 40 percent slopes83679815236wc9yut6511:24000
Tridell-Emlin complex, 3 to 20 percent slopes1036351186263520j70wy0411:24000
Tridell-Badland-Coyoteflats complex, 8 to 60 percent slopes945632532752ztjnwy6291:24000
Tridell gravelly loam, 3 to 15 percent slopes1901282504057jxhxwy63819901:24000

Map of Series Extent

Approximate geographic distribution of the TRIDELL 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 .