Hydraulic Conductivity and Cation Exchange in Non-prehydrated And Prehydrated Bentonite Permeated with Weak Inorganic Salt Solutions

2004 ◽  
Vol 52 (6) ◽  
pp. 661-679 ◽  
Author(s):  
Ho Young Jo ◽  
Craig H. Benson ◽  
Tuncer B. Edil
Keyword(s):  
Hydraulic Conductivity ◽  
Cation Exchange ◽  
Inorganic Salt ◽  
Salt Solutions

scholarly journals Volume of Space within Cation-exchange Resins Determined by Penetration of Inorganic Salt Solutions

2019 ◽  
Vol 35 (2) ◽  
pp. 141-145 ◽  
Author(s):  
Riou KAWAMURA ◽  
Momoka SATOU ◽  
Takuya YONESAKA ◽  
Akio YUCHI
Keyword(s):  
Cation Exchange ◽  
Inorganic Salt ◽  
Salt Solutions ◽  
Cation Exchange Resins ◽  
Exchange Resins

Long-Term Hydraulic Conductivity of a Geosynthetic Clay Liner Permeated with Inorganic Salt Solutions

2005 ◽  
Vol 131 (4) ◽  
pp. 405-417 ◽  
Author(s):  
Ho Young Jo ◽  
Craig H. Benson ◽  
Charles D. Shackelford ◽  
Jae-Myung Lee ◽  
Tuncer B. Edil
Keyword(s):  
Hydraulic Conductivity ◽  
Inorganic Salt ◽  
Salt Solutions ◽  
Geosynthetic Clay Liner ◽  
Clay Liner

Hydraulic conductivity of compacted clay liners permeated with inorganic salt solutions

2008 ◽  
Vol 26 (5) ◽  
pp. 464-473 ◽  
Author(s):  
Gonca Yılmaz ◽  
Temel Yetimoglu ◽  
Seracettin Arasan
Keyword(s):  
Hydraulic Conductivity ◽  
Inorganic Salt ◽  
Compacted Clay ◽  
Salt Solutions ◽  
Clay Liners

Depression of freezing temperature of water and water solutions in porous materials

1989 ◽  
Vol 54 (10) ◽  
pp. 2644-2647 ◽  
Author(s):  
Petr Schneider ◽  
Jiří Rathouský
Keyword(s):  
Water Vapor ◽  
Porous Materials ◽  
Inorganic Salt ◽  
Freezing Point ◽  
Freezing Temperature ◽  
Inorganic Salts ◽  
Freezing Point Depression ◽  
Salt Solutions ◽  
Water Solutions

In porous materials filled with water or water solutions of inorganic salts, water freezes at lower temperatures than under normal conditions; the reason is the decrease of water vapor tension above the convex meniscus of liquid in pores. The freezing point depression is not very significant in pores with radii from 0.05 μm to 10 μm (about 0.01-2.5 K). Only in smaller pores, especially when filled with inorganic salt solutions, this depression is important.

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