Official Series Description


Lab Data Summary

Aggregate lab data for the ULYMEYER soil series. This aggregation is based on all pedons with a current taxon name of ULYMEYER, 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 ULYMEYER 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 ULYMEYER 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 ULYMEYER 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 ULYMEYER 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 ULYMEYER 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with ULYMEYER 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 ULYMEYER 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 ULYMEYER 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.

Click the image to view it full size.

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

Soil series sharing subgroup-level classification with ULYMEYER, 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 ULYMEYER 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
Ulymeyer gravelly loamy coarse sand, moist, 5 to 15 percent slopes335bo147122291832dtn4ca73219981:24000
Ulymeyer-Rovana complex, slightly moist, 5 to 15 percent slopes340bo100722291872dtn8ca73219981:24000
Ulymeyer-Rovana complex, moist, 5 to 15 percent slopes339bo95022291862dtn7ca73219981:24000
Ulymeyer gravelly loamy coarse sand, 5 to 15 percent slopes334bo61222291822dtn3ca73219981:24000
Rovana-Ulymeyer complex, 5 to 15 percent slopes304bo31922291722dtmsca73219981:24000
Ulymeyer-Rovana complex, 5 to 15 percent slopes338bo11422291852dtn6ca73219981:24000
Watterson-Conway-Ulymeyer complex, 0 to 15 slopes slopes354bo6422291972dtnlca73219981:24000
Ulymeyer gravelly loamy coarse sand, slightly moist, 5 to 15 percent slopes337bo522291842dtn5ca73219981:24000
Ulymeyer-Rovana complex, slightly moist, 5 to 15 percent slopes340bo12322300562dvk9ca74019961:24000
Ulymeyer-Rovana complex, slightly moist, 5 to 15 percent slopes340bo38023841042l0vlca76319841:24000
Ulymeyer gravelly loamy coarse sand, 5 to 15 percent slopes334bo5323841012l0vhca76319841:24000
Ulymeyer-Rovana complex, moist, 5 to 15 percent slopes339bo4123841032l0vkca76319841:24000
Ulymeyer gravelly loamy coarse sand, moist, 5 to 15 percent slopes335bo523841022l0vjca76319841:24000
Ulymeyer-Rovana complex, slightly moist, 5 to 15 percent slopes34010367488302jd3pca80219961:24000
Ulymeyer gravelly loamy coarse sand, moist, 5 to 15 percent slopes3357941488297jd3jca80219961:24000
Ulymeyer-Rovana complex, moist, 5 to 15 percent slopes3397742488301jd3nca80219961:24000
Ulymeyer gravelly loamy coarse sand, 5 to 15 percent slopes3344575488296jd3hca80219961:24000
Ulymeyer-Rovana complex, 5 to 15 percent slopes3382615488300jd3mca80219961:24000
Ulymeyer gravelly loamy coarse sand, slightly moist, 5 to 15 percent slopes3372125488299jd3lca80219961:24000
Ulymeyer-Ulymeyer very cobbly-Rovana complex, 0 to 5 percent slopes341965488303jd3qca80219961:24000
Watterson-Conway-Ulymeyer complex, 0 to 15 slopes slopes354655488316jd44ca80219961:24000
Rovana-Ulymeyer complex, 5 to 15 percent slopes304618488261jd2cca80219961:24000
Ulymeyer gravelly loamy coarse sand, slightly dry, 5 to 15 percent slopes336344488298jd3kca80219961:24000

Map of Series Extent

Approximate geographic distribution of the ULYMEYER 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 .