Trends, prospects and challenges in quantifying flow and transport through fractured rocks
SP Neuman - Hydrogeology Journal, 2005 - Springer
Among the current problems that hydrogeologists face, perhaps there is none as
challenging as the characterization of fractured rock (Faybishenko and Benson 2000). This …
challenging as the characterization of fractured rock (Faybishenko and Benson 2000). This …
Colloid movement in unsaturated porous media: Recent advances and future directions
Investigations of colloid movement through geologic materials are driven by a variety of
issues, including contaminant transport, soil‐profile development, and subsurface migration …
issues, including contaminant transport, soil‐profile development, and subsurface migration …
[KNIHA][B] Characterization, modeling, monitoring, and remediation of fractured rock
National Academies of Sciences, Division on Earth… - 2020 - books.google.com
Fractured rock is the host or foundation for innumerable engineered structures related to
energy, water, waste, and transportation. Characterizing, modeling, and monitoring fractured …
energy, water, waste, and transportation. Characterizing, modeling, and monitoring fractured …
Uranium and Cesium sorption to bentonite colloids under carbonate-rich environments: Implications for radionuclide transport
In the context of geological disposal of radioactive waste, one of the controlling mechanisms
for radionuclide migration through subsurface strata is sorption to mobile colloidal bentonite …
for radionuclide migration through subsurface strata is sorption to mobile colloidal bentonite …
Incorporating cross-scale insights into colloid-facilitated radionuclide transport in fractured rocks: A critical review
Driven by the global imperative for the geological disposal of high-level radioactive waste
(HLW), notable progress has been made in predicting radionuclide transport within fractured …
(HLW), notable progress has been made in predicting radionuclide transport within fractured …
A review of colloid transport in fractured rocks
W Zhang, X Tang, N Weisbrod, Z Guan - Journal of Mountain Science, 2012 - Springer
Recent recognition of colloid and colloida-ssociated transport of strongly sorbing
contaminants in fractured rocks highlights the importance of exploring the transport behavior …
contaminants in fractured rocks highlights the importance of exploring the transport behavior …
Pore‐scale mechanisms of colloid deposition and mobilization during steady and transient flow through unsaturated granular media
The distribution of colloid‐associated contaminants and colloid‐sized microorganisms within
the vadose zone is controlled, in part, by mobilization and retention processes. In this work …
the vadose zone is controlled, in part, by mobilization and retention processes. In this work …
Computer simulation of two‐phase immiscible fluid motion in unsaturated complex fractures using a volume of fluid method
Complex fluid behavior in unsaturated fracture and fracture networks, such as film flow, the
migration, fragmentation, and coalescence of droplets, and rivulet flow with or without …
migration, fragmentation, and coalescence of droplets, and rivulet flow with or without …
Salinity effects on cracking morphology and dynamics in 3‐D desiccating clays
KF DeCarlo, N Shokri - Water Resources Research, 2014 - Wiley Online Library
Saline conditions induce not only chemical but physical changes in swelling clays, and have
a significant influence on the crack dynamics and morphology of desiccating clays. In this …
a significant influence on the crack dynamics and morphology of desiccating clays. In this …
A review on clogging of recirculating steam generators in Pressurized-Water Reactors
G Yang, V Pointeau, E Tevissen, A Chagnes - Progress in Nuclear Energy, 2017 - Elsevier
Corrosion product deposits in the secondary side of nuclear power plant steam generators
may result in Tube Support Plate (TSP) clogging and tube fouling. Magnetite has an inverse …
may result in Tube Support Plate (TSP) clogging and tube fouling. Magnetite has an inverse …