Official Series Description


Lab Data Summary

Aggregate lab data for the UPTMOR soil series. This aggregation is based on all pedons with a current taxon name of UPTMOR, 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 UPTMOR 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
43A09N115009ID057011Uptmor6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.6812222,-116.5288333

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the UPTMOR 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 UPTMOR 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 UPTMOR 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 UPTMOR 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 terrace figure.

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

Competing Series

Soil series competing with UPTMOR 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 UPTMOR 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 UPTMOR 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 terrace figure.

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

Soil series sharing subgroup-level classification with UPTMOR, 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 UPTMOR 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
Uptmor-Klickson complex, 20 to 40 percent slopesUm211725020812q2sdid05720131:24000
Uptmor silt loam, 7 to 25 percent slopesUm19025020802q2scid05720131:24000
Uptmor silt loam, 7 to 25 percent slopes126726863515570id60919891:24000
Klickson-Uptmor complex, 10 to 40 percent slopes684810796822y6tsid61119941:24000
Uptmor-Klickson complex, 20 to 40 percent slopesUm23327430822q2sdid61119941:24000
Uptmor silt loam, 7 to 25 percent slopes12659271539775570id61719761:24000
Uptmor silt loam, 3 to 7 percent slopes1251229153976556zid61719761:24000
Klickson-Uptmor complex, 10 to 40 percent slopes2y6ts45030988842y6tsid61719761:24000
Uptmor silt loam, 25 to 40 percent slopes1273361539785571id61719761:24000
Cotay-Humarel-Uptmor complex, 30 to 60 percent slopes7343CO5031206091sgb0or60720181:24000
Uptmor-Slaughterhouse complex, 0 to 15 percent slopes7338AO2731206071sg9tor60720181:24000
Uptmor-Cotay-Blackgulch complex, 30 to 60 percent slopes7323CO2631206001sg9jor60720181:24000
Lemonex-Uptmor-Deck complex, 15 to 30 percent slopes7346BO1931206101sgb5or60720181:24000
Lemonex-Uptmor-Deck complex, 15 to 30 percent slopes7346BO49431224011sgb5or62620181:24000
Cotay-Humarel-Uptmor complex, 30 to 60 percent slopes7343CO45831223991sgb0or62620181:24000
Uptmor-Slaughterhouse complex, 0 to 15 percent slopes7338AO29831223951sg9tor62620181:24000
Uptmor-Cotay-Blackgulch complex, 30 to 60 percent slopes7323CO25331223871sg9jor62620181:24000
Lemonex-Uptmor-Deck complex, 0 to 15 percent slopes7346AO18831224001sgb2or62620181:24000
Uptmor-Payraise-Kingbolt complex, 30 to 60 percent slopes7344CO10631221181q70wor62620181:24000
Uptmor-Cotay-Blackgulch complex, 30 to 60 percent slopes7323CO10324868731sg9jor63120181:24000
Uptmor-Payraise-Kingbolt complex, 30 to 60 percent slopes7344CO1824868761q70wor63120181:24000

Map of Series Extent

Approximate geographic distribution of the UPTMOR 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 .