Official Series Description


Lab Data Summary

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

Click the image to view it full size.

Geomorphic description summaries for the THERIOT 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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Click the image to view it full size.

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 THERIOT, 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 THERIOT 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
Sanpete-Theriot families complex, 5 to 60 percent slopes.15927609471575htq3ca76319841:24000
Sanpete-Theriot families-Rock outcrop, limestone association, 60 to 80 percent slopes.1609697471576htq4ca76319841:24000
Theriot family-Rock outcrop, limestone association, 60 to 80 percent slopes.1745559471590htqlca76319841:24000
Theriot family-Rock outcrop, limestone assiciation, 30 to 60 percent slopes.1734405471589htqkca76319841:24000
Theriot-Kyler-Rock outcrop association250ec6123904652l7gsca76319841:24000
Theriot family-Rock outcrop, limestone association, 15 to 30 percent slopes.17234471588htqjca76319841:24000
Boxspring-Theriot-Rock outcrop association MLRA 29BTR5736538842whmcnv61119671:24000
Boxspring-Theriot-Rock outcrop association MLRA 291811269574781502whmcnv75419921:24000
Izamatch-Theriot association152110949478652j22dnv76619941:24000
Theriot-Izamatch association15308611478654j22gnv76619941:24000
Theriot-Zimbob association8706461478507j1xqnv76619941:24000
Theriot-Rock outcrop association15324375478656j22jnv76619941:24000
Theriot-Izamatch-Rock outcrop association15313726478655j22hnv76619941:24000
Theriot-Findout-Rock outcrop association9104142476689j012nv77019951:24000
Theriot-Theriot, very steep-Rock outcrop association2030142424768522v421nv77419851:24000
Theriot, moist-Kyler-Rock outcrop association203244404768542v433nv77419851:24000
Blacktop-Rodad-Theriot association124331914767412s226nv77419851:24000
Theriot-Eaglepass-Rock outcrop association20312577476853j06cnv77419851:24000
Rodad-Theriot-Kyler association210016924768642v41knv77419851:24000
Blacktop-Rodad-Theriot association111752604849052s226nv79619841:63360
Rodad-Theriot-Kyler association112596834849122v41knv79619841:63360
Theriot-Slatery-Rock outcrop association2536287484971j8n7nv79619841:63360
Theriot-Rock outcrop association25146544849692v42bnv79619841:63360
Theriot-Kyler-Rock outcrop association25042304849682v432nv79619841:63360
Rodad-Theriot-Rock outcrop association11213918484908j8l6nv79619841:63360
Theriot-Rodad-Leo association2541819484972j8n8nv79619841:63360
Rodad-Roic-Theriot association11231613484910j8l8nv79619841:63360
Theriot-Kyler-Leo association2521244484970j8n6nv79619841:63360
Rodad-Ardivey-Theriot association11221153484909j8l7nv79619841:63360
Pintwater-Theriot-Wardenot association411949485032j8q6nv79619841:63360
Theriot-Theriot, very steep-Rock outcrop association3803984776392v421nv79919911:24000
Theriot-Rock outcrop complex, 15 to 70 percent slopes65A2066482175j5r1ut61119921:24000

Map of Series Extent

Approximate geographic distribution of the THERIOT 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 .