Official Series Description


Lab Data Summary

Aggregate lab data for the TROJAN soil series. This aggregation is based on all pedons with a current taxon name of TROJAN, 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 TROJAN 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 TROJAN 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 TROJAN 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 TROJAN 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 TROJAN 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 TROJAN 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 TROJAN series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the TROJAN 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 .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

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 TROJAN, 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 TROJAN 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
Trojan-Erig complex, 15 to 30 percent slopes3227135487232jc05ca60419941:24000
Trojan stony sandy loam, 2 to 30 percent slopesTrE192532331142zmrwca61419671:24000
Trojan stony sandy loam, 30 to 50 percent slopesTrF136432331162zmrxca61419671:24000
Trojan-Sattley-Kyburz complex, 30 to 50 percent slopesTTF40932331232zms0ca61419671:24000
Kyburz-Trojan complex, 9 to 30 percent slopesFUE25032330652zmr3ca61419671:24000
Delleker-Kyburz-Trojan complex, 2 to 30 percent slopesDLE9832330632zmr2ca61419671:24000
Kyburz-Rock outcrop-Trojan complex, 2 to 30 percent slopesKRE4832330892zmrgca61419671:24000
Kyburz-Trojan complex, 30 to 50 percent slopesFUF2932330672zmr4ca61419671:24000
Trojan-Kilmerque families association, 2 to 9 percent slopes.19217937470413hshmca70219841:24000
Trojan-Erig complex, 15 to 30 percent slopes322im1703189935421rfhca70319831:24000
Trojan-Inville-Patio families association, 0 to 35 percent slopes.10572231471078ht62ca70819841:24000
Klicker-Trojan families association, 0 to 35 percent slopes.4931190471022ht48ca70819841:24000
Inville-Patio-Trojan families association, 0 to 35 percent slopes.3319927471006ht3rca70819841:24000
Trojan-Inville-Boomtowm families association, 0 to 35 percent slopes.10417762471077ht61ca70819841:24000
Patio-Trojan-De Masters families association, 0 to 35 percent slopes.7110566471044ht4zca70819841:24000
Lithic Haploxerolls-Rock Outcrop-Trojan family association, 0 to 15 percent slopes.569518471029ht4hca70819841:24000
Wintoner-Trojan-De Masters families association, 0 to 15 percent slopes.1228395471095ht6mca70819841:24000
Klicker-Trojan families-Aquolls association,0 to 15 percent slopes.508137471023ht49ca70819841:24000
Klicker family-Klicker family, sedimentary-Trojan family, complex, 0 to 35 percent slopes.s446519471017ht43ca70819841:24000
Trojan-Klicker families, rhyolitic association, 0 to 35 percent slopes.1085414471081ht65ca70819841:24000
Trojan-Klicker families association, 35 to 50 percent slopes.1074070471080ht64ca70819841:24000
Trojan-Kilmerque-Patio families association, 15 to 35 percent slopes.1063735471079ht63ca70819841:24000
Inville-Patio-Trojan families association, 35 to 50 percent slopes.343334471007ht3sca70819841:24000
Trojan family-Lithic Haploxerolls-Rouen family association, 0 to 15 percent slopes.1101769471083ht67ca70819841:24000
Trojan-Klicker-Wintoner families association, 0 to 35 percent slopes.109311471082ht66ca70819841:24000
Trojan-Erig complex, 15 to 30 percent slopes322It8715282561n98lca70819841:24000
Sattley-Shepan-Trojan families complex, 0 to 30 percent slopes.25810508471267htd5ca71319841:24000
Sattley-Shepan-Trojan families complex, 30 to 50 percent slopes.2597775471268htd6ca71319841:24000
Trojan-Sattley families complex, 0 to 30 percent slopes.2785451471287htdtca71319841:24000
Fopiano-Trojan families-Rock outcrop complex, 30 to 50 percent slopes.1653615471174ht95ca71319841:24000
Fopiano-Trojan families complex, 30 to 50 percent slopes.1642265471173ht94ca71319841:24000
Trojan family, 5 to 50 percent slopes.2772045471286htdsca71319841:24000
Trojan-Sattley families complex, 30 to 70 percent slopes.2791812471288htdvca71319841:24000
Klicker family-Klicker family, sedimentary-Trojan family, complex, 0 to 35 percent slopes.sL443115462111nwysca71319841:24000
Kyburz-Trojan complex, 9 to 30 percent slopesFUE1548232330642zmr3ca71919821:24000
Kyburz-Trojan complex, 30 to 50 percent slopesFUF1066532330662zmr4ca71919821:24000
Kyburz-Rock outcrop-Trojan complex, 30 to 50 percent slopesKRF4975464725hll4ca71919821:24000
Kyburz-Rock outcrop-Trojan complex, 2 to 30 percent slopesKRE472732330882zmrgca71919821:24000
Trojan-Sattley-Kyburz complex, 30 to 50 percent slopesTTF369232331222zms0ca71919821:24000
Kyburz-Trojan-Sierraville complex, 2 to 9 percent slopesFUC3243464663hlj4ca71919821:24000
Sierraville-Trojan-Kyburz complex, 2 to 30 percent slopesSIE2534464793hlnbca71919821:24000
Trojan-Sattley-Kyburz complex, 2 to 30 percent slopesTTE2345464813hlnzca71919821:24000
Delleker-Kyburz-Trojan complex, 2 to 30 percent slopesDLE169232330622zmr2ca71919821:24000
Kyburz-Trojan complex, 2 to 30 percent slopes, alteredFUE51611464665hlj6ca71919821:24000
Kyburz-Rock outcrop-Trojan complex, 30 to 50 percent slopes, erodedKRF2610464726hll5ca71919821:24000
Trojan-Sattley-Cryumbrepts, wet complex, 2 to 30 percent slopesTUE512464815hlp1ca71919821:24000
Kyburz-Trojan-Aquolls complex, 2 to 30 percent slopesKVE282464729hll8ca71919821:24000
Trojan stony sandy loam, 30 to 50 percent slopesTrF17932331172zmrxca71919821:24000
Trojan stony sandy loam, 2 to 30 percent slopesTrE8232331152zmrwca71919821:24000
Kyburz-Trojan complex, 30 to 50 percent slopes, terracedFUF656464667hlj8ca71919821:24000
Trojan loam, warm, 0 to 3 percent slopesTnA657506636k063ut60919741:24000
Trojan loam, warm, 8 to 15 percent slopesTnD445506637k064ut60919741:24000

Map of Series Extent

Approximate geographic distribution of the TROJAN 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 .