Official Series Description


Lab Data Summary

Aggregate lab data for the TEELER soil series. This aggregation is based on all pedons with a current taxon name of TEELER, 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 TEELER 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
34A08N0275S07WY041001Teeler7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1436653,-110.5504684
34A08N0276S07WY041002Teeler7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1478043,-110.5469742

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TEELER 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 TEELER 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 TEELER 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 TEELER 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 TEELER 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 TEELER 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 TEELER 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 flats position figure.

Soil series sharing subgroup-level classification with TEELER, 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 TEELER 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
Teeler, extremely bouldery-Millerlake, extremely stony complex, 10 to 50 percent slopes54716131068472w8m4co6481:24000
Monida-Mult-Teeler families complex, 15 to 50 percent slopes486137523841852l0y6ut6471:24000
Teeler, extremely stony-Bullo families association, 10 to 30 percent slopesNS10571024960652pv2sut6471:24000
Teeler, extremely stony-Wander-Dromedary families association, 15 to 70 percent slopes49257024212302m8h6ut6471:24000
Morset-Teeler-Tibson complex, 1 to 6 percent slopes2154519522350362f0qywy0411:24000
Morset-Teeler-Delridge complex, 8 to 35 percent slopes216409323761962krmhwy0411:24000
Teeler very gravelly sandy loam, 5 to 40 percent slopes2321522501803jv56wy60119911:24000
Leavitt-Teeler complex, 1 to 15 percent slopes4081155524043892lpyywy6301:24000
Teeler, extremely bouldery-Millerlake, extremely stony complex, 10 to 50 percent slopes547294529134302w8m4wy6301:24000
Teeler-Nathrop-Rock outcrop complex, 20 to 60 percent slopes4601214922337012dzbwwy6351:24000
Babb-Teeler complex, 5 to 35 percent slopes1004986503935jxczwy63819901:24000
Teeler gravelly sandy loam, 1 to 10 percent slopes188845504053jxhswy63819901:24000
Teeler-Nathrop-Rock outcrop complex, 20 to 60 percent slopes460132225154112dzbwwy7231:24000

Map of Series Extent

Approximate geographic distribution of the TEELER 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 .