Official Series Description


Lab Data Summary

Aggregate lab data for the TURNERCREST soil series. This aggregation is based on all pedons with a current taxon name of TURNERCREST, 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 TURNERCREST 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
67A89P081289WY031010Turnercrest7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.1313896,-104.6547241

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TURNERCREST 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 TURNERCREST 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 TURNERCREST 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 TURNERCREST 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 TURNERCREST 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 TURNERCREST 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 TURNERCREST 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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Soil series sharing subgroup-level classification with TURNERCREST, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. WY-2010-11-08-03 | South Converse County -

    (Soil Survey of South Converse County, Wyoming)

Map Units

Map units containing TURNERCREST 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
Turnercrest, moist-Ucross-Sodawells, occasionally flooded complex, 2 to 40 percent slopesP528E1427680992s02nsd01919701:24000
Turnercrest, moist-Ucross-Sodawells, occasionally flooded complex, 2 to 40 percent slopesP528E496427457382s02nwy01119781:24000
Turnercrest-Ucross-Draknab, occasionally flooded complex, cool, 2 to 40 percent slopesQ0819E30724392422mw77wy01119781:24000
Taluce-Turnercrest-Keeline fine sandy loams, 3 to 20 percent slopes19842300349709cqwywy02719931:24000
Taluce-Rock outcrop-Turnercrest complex, 6 to 50 percent slopes195766349703cqwrwy02719931:24000
Terro-Turnercrest sandy loams, 2 to 10 percent slopes20162349712cqx1wy02719931:24000
Taluce, thin solum-Rock outcrop-Turnercrest complex, 6 to 50 percent slopes235472351045903htwwy03119981:24000
Keeline-Taluce-Turnercrest fine sandy loams, 3 to 40 percent slopes179411751045333hs1wy03119981:24000
Taluce-Rock outcrop-Turnercrest complex, moist, 6 to 50 percent slopes237218341045923htywy03119981:24000
Taluce-Turnercrest-Keeline fine sandy loams, 3 to 20 percent slopes242215431045973hv3wy03119981:24000
Keeline-Turnercrest fine sandy loams, 0 to 6 percent slopes180188701045343hs2wy03119981:24000
Taluce-Turnercrest sandy loams, 0 to 6 percent slopes241137301045963hv2wy03119981:24000
Taluce-Badland-Turnercrest complex, 6 to 50 percent slopes236115051045912yv7bwy03119981:24000
Keeline-Turnercrest fine sandy loams, 6 to 10 percent slopes18188681045353hs3wy03119981:24000
Turnercrest-Phiferson-Taluce complex, 0 to 6 percent slopes25136751046033hv9wy03119981:24000
Taluce-Taluce, thin solum-Turnercrest fine sandy loams, 3 to 15 percent slopes2398821045943hv0wy03119981:24000
Tassel-Turnercrest fine sandy loams, 6 to 30 percent slopes111840683493952v09bwy04519841:24000
Terro-Turnercrest sandy loams, 2 to 10 percent slopes11316125349397cqkwwy04519841:24000
Keeline-Turnercrest sandy loams, 2 to 10 percent slopes522848349457cqmtwy04519841:24000
Taluce-Rock outcrop-Turnercrest complex, 6 to 50 percent slopes161221816148461r6ctwy04519841:24000
Turnercrest, moist-Ucross-Sodawells, occasionally flooded complex, 2 to 40 percent slopesP528E141527459822s02nwy04519841:24000
Taluce-Turnercrest-Keeline fine sandy loams, 3 to 20 percent slopes16218116148471r6cvwy04519841:24000
Turnercrest-Keeline-Taluce fine sandy loams, 6 to 30 percent slopes1411483616942wlrvwy04519841:24000
Gateson-Taluce-Turnercrest complex, wooded, 6 to 30 percent slopes1361233616922ztznwy04519841:24000
Turnercrest-Keeline-Taluce fine sandy loams, 6 to 30 percent slopes221178703499212wlrvwy60519951:24000
Gateson-Taluce-Turnercrest complex, wooded, 6 to 30 percent slopes150114613498352ztznwy60519951:24000
Theedle-Turnercrest-Kishona complex, 3 to 15 percent slopes21810481349918cr3pwy60519951:24000
Turnercrest-Wibaux, thin solum-Taluce complex, 6 to 40 percent slopes2221258349922cr3twy60519951:24000
Taluce-Turnercrest-Keeline fine sandy loams, 3 to 20 percent slopes2441808116697402yry6wy60920061:24000
Taluce-Badland-Turnercrest complex, 6 to 50 percent slopes2381378016697382yv7bwy60920061:24000
Keeline-Turnercrest fine sandy loams, 3 to 10 percent slopes1841273616697012yv7gwy60920061:24000
Taluce-Taluce, thin solum-Turnercrest fine sandy loams, 3 to 15 percent slopes241169416697671t1jgwy60920061:24000
Keeline-Turnercrest fine sandy loams, moist, 6 to 10 percent slopes1857616698181t1l3wy60920061:24000
Taluce-Turnercrest-Keeline fine sandy loams, 3 to 20 percent slopes31410713982981hy1dwy62519851:24000
Taluce-Badland-Turnercrest complex, 6 to 50 percent slopes3152413982972yv7bwy62519851:24000
Turnback-Turnercrest complex, 5 to 25 percent slopes39615254453qswy6291:24000
Olney-Turnercrest complex, 0 to 12 percent slopes -- Draft39315254353qrwy6291:24000
Turnercrest fine sandy loam, 0 to 10 percent slopes -- Draft82AC15266853vswy6291:24000
Remmit-Turnercrest complex, 2 to 15 percent slopes534931709342z1z0wy6291:24000
Turnercrest-Keeline-Taluce fine sandy loams, 6 to 30 percent slopes22114298175882wlrvwy70520031:24000
Taluce-Turnercrest-Keeline fine sandy loams, 3 to 20 percent slopes23322114278511jxsqwy70919831:24000
Taluce, thin solum-Rock outcrop-Turnercrest complex, 6 to 50 percent slopes393714148091jh70wy71519741:20000
Taluce-Badland-Turnercrest complex, 6 to 50 percent slopes521914148212yv7bwy71519741:20000
Turnercrest-Keeline-Taluce fine sandy loams, 6 to 30 percent slopes711551713991442wlrvwy71920131:24000
Taluce-Taluce, thin solum-Turnercrest fine sandy loams, 3 to 15 percent slopes16933101049703j74wy72119941:24000

Map of Series Extent

Approximate geographic distribution of the TURNERCREST 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 .