Official Series Description


Lab Data Summary

Aggregate lab data for the TRAG soil series. This aggregation is based on all pedons with a current taxon name of TRAG, 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 TRAG 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
4987P083884CO628002Trag7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.3256111,-104.7547778

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TRAG 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 TRAG 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 TRAG 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 TRAG 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 TRAG 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 TRAG 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 TRAG 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 TRAG, 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 TRAG 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
Falcon-Trag families complex, 5 to 40 percent slopes, extremely stonyFT2199546836bmco62619741:24000
Trag loam, 3 to 12 percent slopes803042496521jnntco62719801:24000
Falcon-Trag families complex, 5 to 40 percent slopes101173496565jnq7co62719801:24000
Teaspoon-Trag families complex, 25 to 40 percent slopes11679496580jnqqco62719801:24000
Teaspoon-Trag families complex, 5 to 25 percent slopes1155496579jnqpco62719801:24000
Teaspoon-Trag families complex, 25 to 40 percent slopes58186498430jqndco63519791:24000
Teaspoon-Trag families complex, 25 to 40 percent slopes716M4567509910k3lqco63620111:24000
Falcon-Trag families complex, 5 to 40 percent slopes506M2158509839k3jfco63620111:24000
Teaspoon-Trag families complex, 5 to 25 percent slopes715M1613509908k3lnco63620111:24000
Trag sandy loam, 9 to 25 percent slopes1533029497433jpm7co64119801:24000
Lininger-Trag sandy loams, 9 to 20 percent slopes871845497535jpqjco64119801:24000
Trag sandy loam, 3 to 9 percent slopes152746497432jpm6co64119801:24000
Lininger-Trag sandy loams, 3 to 9 percent slopes86243497534jpqhco64119801:24000
Trag-Moen complex, 5 to 30 percent slopes11212340497649jpv6co64419801:24000
Lininger-Trag gravelly sandy loams, 15 to 30 percent slopes26407512698k6hnco65320001:24000
Trag gravelly sandy loam, 3 to 15 percent slopes59243512731k6jqco65320001:24000
Garber-Northrim-Trag complex, 3 to 25 percent slopes, very stonyMC617373170476k06zco67619831:24000
Northrim-Garber-Trag complex, 3 to 25 percent slopes, very stonyMC61D513170477k070co67619831:24000
Northrim-Garber-Trag complex, 3 to 25 percent slopes, very stony61D8181506664k070co68019701:31680
Garber-Northrim-Trag complex, 3 to 25 percent slopes, very stony613061506663k06zco68019701:31680
Garber-Northrim-Trag complex, 3 to 25 percent slopes, very stonyMC61263170519k06zco68219861:24000
Trag-Techado-Rock outcrop complex, 3 to 55 percent slopes61511962569431x7wnm68219851:24000
Trag loam, 1 to 8 percent slopes2761906568721x5lnm68219851:24000
Beje-Trag complex732920503764jx6gut61619831:24000
Rottulee family-Trag complex9716018503794jx7fut61619831:24000
Trag-Beje-Senchert complex11710577503691jx43ut61619831:24000
Trag-Croydon complex1186888503692jx44ut61619831:24000
Trag stony loam, 30 to 60 percent slopes1156533503689jx41ut61619831:24000
Trag-Beje-Rottulee family complex1163032503690jx42ut61619831:24000
Trag stony loam, 15 to 60 percent slopes50110019484046j7pdut63419971:24000
Trag-Quincreek families complex, 5 to 25 percent slopes101116332432622zsc9ut6451:24000
Trag-Pino families, complex, 3 to 25 percent slopes20B6952791100vk6cut6511:24000

Map of Series Extent

Approximate geographic distribution of the TRAG 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 .