Official Series Description


Lab Data Summary

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

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Soil series sharing subgroup-level classification with TRAPPS, 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 TRAPPS 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
Trapps channery loam, 25 to 60 percent slopes298F13229955274wkcmt60319891:24000
Trapps channery loam, 4 to 25 percent slopes298D8129955264wkbmt60319891:24000
Trapps channery loam, 60 to 80 percent slopes298G129955284wkdmt60319891:24000
Silverchief-Trapps complex, 8 to 15 percent slopes599D151154953567hmt61620031:24000
Trapps gravelly loam, 35 to 60 percent slopes98F12215519856hdmt61620031:24000
Trapps-Yreka stony loams, 8 to 25 percent slopes198E515463155x3mt61620031:24000
Trapps gravelly loam, 15 to 35 percent slopes98E68441446714vjtmt62119971:24000
Trapps gravelly loam, 35 to 60 percent slopes98F43391446724vjvmt62119971:24000
Silverchief-Trapps complex, 15 to 35 percent slopes599E22241445224vd0mt62119971:24000
Trapps gravelly loam, 60 to 80 percent slopes98G4911446734vjwmt62119971:24000
Trapps gravelly loam, 8 to 15 percent slopes98D3731446704vjsmt62119971:24000
Silverchief-Trapps complex, 35 to 60 percent slopes599F3271445234vd1mt62119971:24000
Silverchief-Trapps complex, 8 to 15 percent slopes599D1661445214vczmt62119971:24000
Trapps-Yreka complex, 4 to 8 percent slopes198C1431442654v3qmt62119971:24000
Trapps-Yreka complex, 8 to 25 percent slopes198E321442664v3rmt62119971:24000
Trapps gravelly loam, 15 to 30 percent slopes16417771450674vylmt62919911:20000
Trapps gravelly loam, 8 to 15 percent slopes1632901450664vykmt62919911:20000
Whitecow, cool-Trapps, dry channery loams, 25 to 60 percent slopes285F43261477714yrtmt63019911:24000
Trapps-Whitecow-Warneke channery loams, 25 to 60 percent slopes985F24121479494yykmt63019911:24000
Trapps channery loam, 25 to 60 percent slopes484F23581478274ytmmt63019911:24000
Trapps stony loam, 8 to 25 percent slopes584D18751478634yvsmt63019911:24000
Trapps-Warneke channery loams, 25 to 60 percent slopes984F13581479484yyjmt63019911:24000
Trapps-Yreka complex, 8 to 25 percent slopes198E208817032421v5c9mt63520061:24000
Silverchief-Trapps complex, 35 to 60 percent slopes599F62117029761v52qmt63520061:24000
Silverchief-Trapps complex, 15 to 35 percent slopes599E31817029751v52pmt63520061:24000
Trapps gravelly loam, 35 to 60 percent slopes98F26917030021v53kmt63520061:24000
Trapps gravelly loam, 15 to 35 percent slopes98E18917030011v53jmt63520061:24000
Trapps gravelly loam, 30 to 60 percent slopes109108811453974w97mt63819851:24000
Trapps gravelly loam, 8 to 30 percent slopes10811931453964w96mt63819851:24000
Wilde-Trapps families complex, mountain uplands and ridges33B3516724226772m9zwmt63819851:24000
Trapps-Wilde families complex, dissected mountain slopes31B392824226712m9zpmt63819851:24000
Trapps gravelly loam, 35 to 60 percent slopes98F44301459804wx1mt64419951:24000
Silverchief-Trapps complex, 15 to 35 percent slopes599E42051458294wr5mt64419951:24000
Trapps gravelly loam, 15 to 35 percent slopes98E39251459794wx0mt64419951:24000
Trapps channery loam, 25 to 60 percent slopes298F30931456494wkcmt64419951:24000
Trapps-Yreka stony loams, 8 to 25 percent slopes198E30771455934whkmt64419951:24000
Trapps channery loam, 4 to 25 percent slopes298D14951456484wkbmt64419951:24000
Silverchief-Trapps complex, 8 to 15 percent slopes599D11991458284wr4mt64419951:24000
Trapps channery loam, 60 to 80 percent slopes298G2421456504wkdmt64419951:24000
Trapps family, dissected mountain slopes31B282075633769p8h5mt64520131:12000
Trapps-Wilde families, complex, dissected mountain slopes31B391643633770p8h6mt64520131:12000
Trapps-Bignell families, complex, steep mountain slopes30B32880754412tb0wmt64520131:12000
Wilde-Trapps families, complex, mountain uplands and ridges33B3541313895551hmycmt64520131:12000
Wilde-Trapps families, complex, steep mountain slopes30B35310757744tfhcmt64520131:12000
Trapps-Wilde families, complex, dissected mountain slopes31B39668415025951c2mt64720071:24000
Trapps-Bignell families, complex, steep mountain slopes30B32456515022851b2mt64720071:24000
Trapps family, dissected mountain slopes31B28317715025751c0mt64720071:24000
Wilde-Trapps families, complex, steep mountain slopes30B35284115023051b4mt64720071:24000
Wilde-Trapps families, complex, mountain ridges33B35135315030051ddmt64720071:24000
Wilde-Trapps-Tolman families, association, dissected mountain slopes31W3511615027551clmt64720071:24000
Trapps-Shawmut complex, 1 to 20 percent slopes, extremely stony330131368402ypn8wy6291:24000
Trapps-Shawmut complex, 1 to 20 percent slopes, extremely stony330132533582ypn8wy65620081:24000

Map of Series Extent

Approximate geographic distribution of the TRAPPS 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 .