Official Series Description


Lab Data Summary

Aggregate lab data for the TEVIS soil series. This aggregation is based on all pedons with a current taxon name of TEVIS, 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 TEVIS 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
43B89P043677MT077308Tevis6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.0648918,-113.0075836

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TEVIS 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 TEVIS 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 TEVIS 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 TEVIS 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 terrace figure.

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with TEVIS 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 TEVIS 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 TEVIS 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 TEVIS, 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 TEVIS 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
Mitten and Tevis families, steep mountain slopes, very stony64QC6140428091242tr6mmt60319891:24000
Mitten and Tevis families, moderately steep mountain slopes30QC5591828090662tr4rmt60319891:24000
Mitten family, extremely stony-Rock outcrop-Tevis family, extremely stony complex, stream breaklands60QC4200428091062tr60mt60319891:24000
Mitten-Tevis families, complex, moderately steep mountain slopes30QG3510128090692tr4vmt60319891:24000
Mitten-Tevis families complex, steep mountain slopes, very stony64QG1926428091272tr6qmt60319891:24000
Mitten family, extremely stony-Rock outcrop-Tevis family, extremely stony complex, dissected stream breaklands61QC1880928091092tr64mt60319891:24000
Tevis-Mitten families, complex, moderately steep mountain slopes30MG776728090612tr4lmt60319891:24000
Afley-Tevis families, complex, broadly convex ridges32QD537728090752tr52mt60319891:24000
Mitten-Tevis complex, 30 to 60 percent slopes71106729955084wd9mt60319891:24000
Tevis family-Rock outcrop complex, stream breaklands60KA93028090972tr5rmt60319891:24000
Tevis family, moderately steep mountain slopes, moderately well weathered granitic substratum30KA54828090522tr49mt60319891:24000
Mitten-Tevis complex, 35 to 60 percent slopes132F5042995555574dmt60319891:24000
Tevis family, moderately steep mountain slopes, well weathered granitic substratum30GA32428090502tr46mt60319891:24000
Tevis gravelly loam, 30 to 60 percent slopes10220029954744w90mt60319891:24000
Tevis gravelly loam, 35 to 60 percent slopes30F1732995580579cmt60319891:24000
Tevis gravelly loam, 15 to 35 percent slopes30E1712995579579bmt60319891:24000
Tevis gravelly loam, dry, 35 to 60 percent slopes31F1492995583579hmt60319891:24000
Tevis gravelly loam, 35 to 60 percent slopes486F11829955384wp8mt60319891:24000
Tevis gravelly loam, dry, 15 to 35 percent slopes31E1102995582579gmt60319891:24000
Tevis family, steep mountain slopes64KA10928091122tr67mt60319891:24000
Tevis-Rock outcrop complex, 30 to 60 percent slopes441F59299561757dvmt60319891:24000
Tevis-Rubble land complex, 40 to 70 percent slopes30G572995581579dmt60319891:24000
Tevis gravelly loam, 15 to 35 percent slopes486E529955374wp7mt60319891:24000
Tevis gravelly loam, dry, 15 to 35 percent slopes31E1319580937mhhxmt61820081:24000
Tevis gravelly loam, 35 to 60 percent slopes30F19515704958f3mt61820081:24000
Tevis gravelly loam, 15 to 35 percent slopes30E14615704858f2mt61820081:24000
Mitten family, extremely stony-Rock outcrop-Tevis family, extremely stony complex, stream breaklands60QC029952962tr60mt62119971:24000
Mitten and Tevis families, steep mountain slopes, very stony64QC029953012tr6mmt62119971:24000
Mitten-Tevis families, complex, moderately steep mountain slopes30QG029953002tr4vmt62119971:24000
Mitten and Tevis families, moderately steep mountain slopes30QC029952982tr4rmt62119971:24000
Tevis very gravelly loam, 30 to 60 percent slopes16241891450654vyjmt62919911:20000
Courville-Troybull-Tevis complex, 35 to 75 percent slopes2355F978531648442yywbmt63419881:24000
Tevis-Courville complex, 15 to 60 percent slopes2302F174531648392yyw5mt63419881:24000
Badmedicine-Felixcreek-Tevis complex, 20 to 60 percent slopes2109F171631648462yyvzmt63419881:24000
Mitten-Tevis families complex, steep mountain slopes, very stony64QG2231648612tr6qmt63419881:24000
Afley-Tevis families, complex, broadly convex ridges32QD029953142tr52mt63520061:24000
Mitten-Tevis complex, 30 to 60 percent slopes71354401454924wd9mt63819851:24000
Tevis gravelly loam, 30 to 60 percent slopes102305201453904w90mt63819851:24000
Tevis-Mitten complex, 8 to 30 percent slopes10346571453914w91mt63819851:24000
Tevis-Mitten-Rock outcrop complex, 45 to 70 percent slopes10443051453924w92mt63819851:24000
Mitten-Tevis families, complex, moderately steep mountain slopes30QG84529953352tr4vmt63819851:24000
Mitten family, extremely stony-Rock outcrop-Tevis family, extremely stony complex, stream breaklands60QC38229953572tr60mt63819851:24000
Mitten-Tevis families complex, steep mountain slopes, very stony64QG36229953682tr6qmt63819851:24000
Mitten and Tevis families, steep mountain slopes, very stony64QC31729953652tr6mmt63819851:24000
Mitten and Tevis families, moderately steep mountain slopes30QC9329953322tr4rmt63819851:24000
Afley-Tevis families, complex, broadly convex ridges32QD5229953382tr52mt63819851:24000
Mitten family, extremely stony-Rock outcrop-Tevis family, extremely stony complex, dissected stream breaklands61QC729953592tr64mt63819851:24000
Tevis gravelly loam, 35 to 60 percent slopes486F30701457704wp8mt64419951:24000
Tevis gravelly loam, 15 to 35 percent slopes486E24761457694wp7mt64419951:24000
Tevis gravelly loam, 4 to 15 percent slopes486D7421457684wp6mt64419951:24000
Mitten-Tevis families complex, steep mountain slopes, very stony64QG12529953872tr6qmt64419951:24000
Mitten-Tevis families, complex, moderately steep mountain slopes30QG2729953792tr4vmt64419951:24000
Tevis gravelly loam, 35 to 60 percent slopes30F12377155972579cmt65119971:24000
Mitten-Tevis complex, 35 to 60 percent slopes132F10547155818574dmt65119971:24000
Tevis gravelly loam, 15 to 35 percent slopes30E9485155971579bmt65119971:24000
Tevis gravelly loam, dry, 35 to 60 percent slopes31F3474155976579hmt65119971:24000
Tevis-Rubble land complex, 40 to 70 percent slopes30G2897155973579dmt65119971:24000
Tevis gravelly loam, dry, 15 to 35 percent slopes31E2420155975579gmt65119971:24000
Tevis-Rock outcrop complex, 30 to 60 percent slopes441F105615608057dvmt65119971:24000
Mitten and Tevis families, moderately steep mountain slopes30QC74529954152tr4rmt65119971:24000
Mitten family, extremely stony-Rock outcrop-Tevis family, extremely stony complex, dissected stream breaklands61QC29429954372tr64mt65119971:24000
Mitten and Tevis families, steep mountain slopes, very stony64QC25329954432tr6mmt65119971:24000
Mitten-Tevis families, complex, moderately steep mountain slopes30QG12329954182tr4vmt65119971:24000
Mitten family, extremely stony-Rock outcrop-Tevis family, extremely stony complex, stream breaklands60QC11829954352tr60mt65119971:24000
Tevis-Mitten families, complex, moderately steep mountain slopes30MG9929954122tr4lmt65119971:24000
Tevis-Courville complex, 15 to 60 percent slopes2302F7531648492yyw5mt65119971:24000
Courville-Troybull-Tevis complex, 35 to 75 percent slopes2355F931648522yywbmt65119971:24000

Map of Series Extent

Approximate geographic distribution of the TEVIS 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 .