Official Series Description


Lab Data Summary

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

Click the image to view it full size.

Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with YOUNGSTON, 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-2012-03-23-01 | Fremont County, East Part and Dubois Area - July 1993

    Soils and their landscape positions as they relate to parent material, precipitation zones, and temperature regimes (Soil Survey of Fremont County, East Part and Dubois Area, WY; 1993).

Map Units

Map units containing YOUNGSTON 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
Youngston loam, 1 to 6 percent slopes784115496743jnwzco68219861:24000
Massadona-Youngston moist, complex, 1 to 8 percent slopes1267345497087jp82co68619921:31680
Youngston loam, well drained, 0 to 3 percent slopes2233420497195jpckco68619921:31680
Youngston loam, cool, 0 to 3 percent slopes2222990497194jpcjco68619921:31680
Youngston clay loamYo927566451wy8nm61819781:63360
Youngston loamy sandYp1225495677jmslnv62219721:24000
Youngston fine sandy loamYr468495678jmsmnv62219721:24000
Yomba-Playas-Youngston association, alkali1624935484937j8m4nv79619841:63360
Youngston-Playas association1801938484941j8m8nv79619841:63360
Youngston-Uffens-Lostwells complex, 1 to 10 percent slopes8460232152133539jwy04319761:24000
Lostwells-Youngston complex, 1 to 10 percent slopes42221011520875381wy04319761:24000
Youngston-Glenton complex, 0 to 3 percent slopes8311242152132539hwy04319761:24000
Stutzman-Persayo association6810743152115538ywy04319761:24000
Youngston clay loam, moderately wet, 0 to 3 percent slo pes818941152130539fwy04319761:24000
Youngston silty clay loam, 0 to 3 percent slopes826343152131539gwy04319761:24000
Lostwells-Youngston complex, wet, 0 to 6 percent slopes4351061520885382wy04319761:24000
Youngston-Uffens complex, 0 to 10 percent slopes -- Draft60124935422pqlpwy6031:24000
Youngston loam, 0 to 10 percent slopes -- Draft48AC24309492mllqwy6031:24000
Youngston loam, 0 to 6 percent slopes -- Draft48AB24309502mllrwy6031:24000
Sayles-Persayo-Youngston complex, 0 to 45 percent slopes -- Draft390CD4065015219553cjwy6031:24000
Youngston loam, 0 to 3 percent slopes -- Draft48A999815223653dvwy6031:24000
Baroid-Las Animas complex, wet, 0 to 3 percent slopes -- Draft509A628115224153f0wy6031:24000
Lostwells-like-Kinnear complex, 3 to 6 percent slopes -- Draft368B243215217953c0wy6031:24000
Binton-Youngston loams, 0 to 10 percent slopes -- Draft363AC133415217453bvwy6031:24000
Youngston-Stutzman complex, 0 to 3 percent slopes -- Draft341A54815216853bnwy6031:24000
Youngston clay loamYo141215741358svwy61319691:20000
Youngston loam, 0 to 3 percent slopes, occasionally flooded -- Draft48A15258953s7wy6291:24000
Youngston-Lostwells complex, 1 to 3 percent slopes0061510815742858tbwy6471:24000
Fluvaquents-Youngston complex, 0 to 3 percent slopes010821415742458t6wy6471:24000
Effington-Youngston loams, 0 to 6 percent slopes2242913637781pdnlwy6471:24000
Frisite-Youngston complex, 1 to 8 percent slopes3021210637782pdnmwy6471:24000
Youngston-Lostwells-Apron complex, 0 to 3 percent slopes199449580427mgzgwy6471:24000
Frisite-Youngston complex, 1 to 8 percent slopes15133240503016jwfbwy71319861:24000
Youngston-Effington loams, 0 to 6 percent slopes22432279503104jwj5wy71319861:24000
Fluvaquents-Youngston complex, 0 to 3 percent slopes14614005503011jwf5wy71319861:24000
Youngston-Lostwells complex, 1 to 3 percent slopes22613794503107jwj8wy71319861:24000
Youngston-Lostwells-Apron complex, 0 to 3 percent slopes2259402503105jwj6wy71319861:24000
Youngston-Persayo loams, rolling2279396503109jwjbwy71319861:24000
Binton-Youngston clay loams, 0 to 3 percent slopes1144242502979jwd4wy71319861:24000

Map of Series Extent

Approximate geographic distribution of the YOUNGSTON 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 .