Official Series Description


Lab Data Summary

Aggregate lab data for the UTLEY soil series. This aggregation is based on all pedons with a current taxon name of UTLEY, 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 UTLEY 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
1011N0357S2009OR023001Utley6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0467262,-119.4800568

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the UTLEY 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 UTLEY 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 UTLEY 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 UTLEY 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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 UTLEY 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 UTLEY 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 UTLEY 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.

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

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

Soil series sharing subgroup-level classification with UTLEY, 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 UTLEY 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
Keerins-Utley complex, 10 to 30 percent south slopes373905534263712lp4yor6181:24000
Keerins-Utley complex, 0 to 12 percent slopes379763234295012lr7cor6181:24000
Gerow-Utley complex, 0 to 5 percent slopes370229634263172lp44or6181:24000
Spikebutte-Utley-Keerins complex, 2 to 12 percent slopes372178934261482lp4wor6181:24000
Utley-Gerow complex, 3 to 12 percent slopes37192734294502lp45or6181:24000
Utley-Izee complex, 10 to 30 percent north slopes37564034264182lp52or6181:24000
Izee-Utley complex, 0 to 20 percent slopes71124934261942pt7vor6181:24000
Gerow-Utley complex, 0 to 5 percent slopes0135AW61633853022lp44or62620181:24000
Izee-Utley complex, 0 to 20 percent slopes711386434260362pt7vor6271:24000
Gerow-Utley complex, 0 to 5 percent slopes370286234263112lp44or6271:24000
Keerins-Utley complex, 10 to 30 percent south slopes373255934263642lp4yor6271:24000
Utley-Izee complex, 10 to 30 percent north slopes375192334264112lp52or6271:24000
Utley-Gerow complex, 3 to 12 percent slopes371169734294462lp45or6271:24000
Keerins-Utley complex, 0 to 12 percent slopes379131934294922lr7cor6271:24000
Utley loam, 8 to 20 percent slopes62D4936136921vnor64819771:24000
Utley channery loam, 10 to 50 percent slopesUtE30006292623gwor66619701:31680
Utley ashy loam, 3 to 20 percent slopes390D498342452426f8or6771:24000
Izee-Utley complex, 0 to 20 percent slopes71119734249912pt7vor6771:24000
Spikebutte-Utley-Keerins complex, 2 to 12 percent slopes37219434247162lp4wor6771:24000

Map of Series Extent

Approximate geographic distribution of the UTLEY 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 .