Official Series Description


Lab Data Summary

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

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Competing Series

Soil series competing with YETULL 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 YETULL 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 YETULL 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 mountains figure.

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

Soil series sharing subgroup-level classification with YETULL, 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 YETULL 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
Busby-Yetull complex, 2 to 15 percent slopes278E2387343364cj98mt01719951:24000
Lihill-Yetull complex, 8 to 35 percent slopes542E345343533cjgqmt01719951:24000
Busby-Yetull complex, 0 to 8 percent slopes961C174343804cjrgmt01719951:24000
Yetull-Busby complex, 0 to 2 percent slopes996A21343840cjsmmt01719951:24000
Busby-Yetull-Rock outcrop complex, 8 to 25 percent slopes847E1343714cjnkmt01719951:24000
Twilight-Yetull complex, 8 to 25 percent slopesDc19090342007cgwhmt02119711:24000
Lambert-Yetull complex, 15 to 65 percent slopesLe17790342019cgwwmt02119711:24000
Yetull-Dimyaw complex, 8 to 80 percent slopesBy7082341999cgw7mt02119711:24000
Twilight-Yetull complex, 2 to 8 percent slopesDb6182342006cgwgmt02119711:24000
Yetull-Busby complex, 2 to 15 percent slopes914D5821342712chm7mt03320021:24000
Busby-Yetull fine sandy loams, 2 to 8 percent slopes915C617339743cdjgmt03320021:24000
Twilight-Yetull fine sandy loams, 8 to 15 percent slopes916D222339751cdjqmt03320021:24000
Chinook-Cozberg-Yetull fine sandy loams, 4 to 15 percent slopes571D4379343995cjymmt04119941:24000
Yetull-Lonesome loamy fine sands, 0 to 8 percent slopes732C3201344046ck08mt04119941:24000
Chinook-Yetull complex, 2 to 10 percent slopes362C2250343922cjw8mt04119941:24000
Yetull-Busby fine sandy loams, 4 to 15 percent slopes701D1964344038ck00mt04119941:24000
Twilight-Yetull fine sandy loams, 8 to 15 percent slopes1424551344341ck9smt05519811:24000
Busby-Yetull fine sandy loams, 2 to 8 percent slopes242073344385ckc6mt05519811:24000
Lihill-Yetull complex, 8 to 35 percent slopes8317073345029cl0zmt07919861:24000
Lihill-Parshall-Yetull complex, 4 to 15 percent slopes815349345024cl0tmt07919861:24000
Busby-Yetull complex, 0 to 8 percent slopes171279344829cktjmt07919861:24000
Yetull-Busby complex, 0 to 2 percent slopes1401187344822ckt9mt07919861:24000
Yetull-Twilight complex, 4 to 15 percent slopes161111424512052n8p4mt07919861:24000
Busby-Yetull-Rock outcrop complex, 8 to 25 percent slopes181104344830cktkmt07919861:24000
Yetull loamy fine sand, 0 to 15 percent slopes73D2582345261cl8gmt10119921:24000
Yetull fine sandYe5881469734xy2mt60019691:24000
Yetull loamy sand, 4 to 20 percent slopes2333332341905cgs6mt61319751:24000
Fleak-Twilight-Yetull complex, 25 to 70 percent slopes653F4942346872cmyfmt61519921:24000
Chinook-Yetull complex, 2 to 10 percent slopes362C4870346712cms8mt61519921:24000
Yetull fine sandy loam, 15 to 45 percent slopes93F4240346985cn22mt61519921:24000
Yetull-Lonesome loamy fine sands, 0 to 6 percent slopes73B2078346903cmzfmt61519921:24000
Yetull-Dune land complex, 15 to 45 percent slopes731F291346902cmzdmt61519921:24000
Yetull-Yetull, stony, complex, 8 to 35 percent slopes858E24315153152p3mt62719981:24000
Yetull loamy fine sand, 2 to 8 percent slopes859C14215153252p4mt62719981:24000
Yetull loamy sand, cool, 2 to 8 percent slopes16041441464374xcsmt63619831:24000
Yetull loamy fine sand, 2 to 8 percent slopes650C290347770cnwdmt64119941:24000
Yetull loamy fine sand, 8 to 15 percent slopes650D66347771cnwfmt64119941:24000
Busby-Yetull complex, 8 to 25 percent slopes515704348083cp6hmt64919851:24000
Busby-Yetull complex, 2 to 8 percent slopes503757348082cp6gmt64919851:24000
Twilight-Yetull-Rock outcrop complex, 8 to 25 percent slopes181E4719348403cpjtmt65719901:24000
Twilight-Chinook-Yetull complex, 2 to 8 percent slopes281C1666348530cpnxmt65719901:24000
Yetull loamy fine sand, 0 to 15 percent slopes42C1628348647cpspmt65719901:24000
Yetull variant loamy sand, 2 to 20 percent slopes -- draft348112423780982ktlvwy6301:24000
Yetull-Figuore complex, 1 to 10 percent slopes53251715823706992kkx5wy6351:24000
Yetull-Figuore complex, 1 to 10 percent slopes53259725154162kkx5wy7231:24000

Map of Series Extent

Approximate geographic distribution of the YETULL 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 .