Seepage water of northern Utah

10.3133/wsp7 ◽  
1897 ◽  
Keyword(s):  
Seepage Water ◽  
Northern Utah

Ground-water resources of northern Utah Valley, Utah

1984 ◽  
Author(s):  
D.W. Clark ◽  
C.L. Appel
Keyword(s):  
Water Resources ◽  
Ground Water ◽  
Northern Utah

SPONGE CHERTS AND BIOCALCIFIER BEDS IN THE PERMIAN PARK CITY GROUP, NORTHERN UTAH AND NORTHEASTERN NEVADA

2018 ◽  
Author(s):  
W. Benton Pipkin Franklin ◽  
◽  
Zackery P. Wistort ◽  
Seana C. Hood ◽  
Kathleen A. Ritterbush
Keyword(s):  
Northern Utah ◽  
City Group

THE ORIGIN AND CHEMICAL EVOLUTION OF PRECAMBRIAN BASEMENT UNITS IN NORTHERN UTAH AND SOUTHERN IDAHO

2020 ◽  
Author(s):  
Skadi Kobe ◽  
◽  
Austin Jensen ◽  
Alexander Berniche ◽  
Katherine E. Potter ◽  
...  
Keyword(s):  
Chemical Evolution ◽  
Precambrian Basement ◽  
Northern Utah

scholarly journals The Monitoring-Based Analysis on Deformation-Controlling Factors and Slope Stability of Reservoir Landslide: Hongyanzi Landslide in the Southwest of China

Geofluids ◽  
2018 ◽  
Vol 2018 ◽  
pp. 1-14 ◽  
Author(s):  
Bing Han ◽  
Bin Tong ◽  
Jinkai Yan ◽  
Chunrong Yin ◽  
Liang Chen ◽  
...  
Keyword(s):  
Water Level ◽  
Water Pressure ◽  
Monitoring Program ◽  
Significant Risk ◽  
Controlling Factors ◽  
Seepage Water ◽  
Reservoir Water ◽  
Reservoir Water Level ◽  
Reservoir Area ◽  
Reservoir Landslide

Reservoir landslide is a type of commonly seen geological hazards in reservoir area and could potentially cause significant risk to the routine operation of reservoir and hydropower station. It has been accepted that reservoir landslides are mainly induced by periodic variations of reservoir water level during the impoundment and drawdown process. In this study, to better understand the deformation characters and controlling factors of the reservoir landslide, a multiparameter-based monitoring program was conducted on a reservoir landslide—the Hongyanzi landslide located in Pubugou reservoir area in the southwest of China. The results indicated that significant deformation occurred to the landslide during the drawdown period; otherwise, the landslide remained stable. The major reason of reservoir landslide deformation is the generation of seepage water pressure caused by the rapidly growing water level difference inside and outside of the slope. The influences of precipitation and earthquake on the slope deformation of the Hongyanzi landslide were insignificant.

Chemistry of Water Collected from an Unventilated Drift, Yucca Mountain, Nevada

2006 ◽  
Vol 985 ◽  
Author(s):  
Brian D Marshall ◽  
Thomas A. Oliver ◽  
Zell E. Peterman
Keyword(s):  
Pore Water ◽  
Water Samples ◽  
Conveyor Belt ◽  
Yucca Mountain ◽  
Seepage Water ◽  
Biologic Activity ◽  
Co2 Concentrations ◽  
The Cross ◽  
Chemical Conditions

AbstractWater samples (referred to as puddle water samples) were collected from the surfaces of a conveyor belt and plastic sheeting in the unventilated portion of the Enhanced Characterization of the Repository Block (ECRB) Cross Drift in 2003 and 2005 at Yucca Mountain, Nevada. The chemistry of these puddle water samples is very different than that of pore water samples from borehole cores in the same region of the Cross Drift or than seepage water samples collected from the Exploratory Studies Facility tunnel in 2005. The origin of the puddle water is condensation on surfaces of introduced materials and its chemistry is dominated by components of the introduced materials. Large CO2 concentrations may be indicative of localized chemical conditions induced by biologic activity.

scholarly journals Geochemical and microbial characteristics of seepage water and mineral precipitates in a radwaste disposal facility impacted by seawater intrusion and high alkalinity

2021 ◽  
Vol 285 ◽  
pp. 112087
Author(s):  
Baknoon Ham ◽  
Jang-Soon Kwon ◽  
Maxim I. Boyanov ◽  
Edward J. O'Loughlin ◽  
Kenneth M. Kemner ◽  
...  
Keyword(s):  
Seawater Intrusion ◽  
Seepage Water ◽  
Disposal Facility ◽  
Microbial Characteristics ◽  
High Alkalinity
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