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- W2376305779 abstract "In accordance with wall of well-bore instability induced by bound water on clays, Infrared spectrum is utilized to determine the types and boundary line of bound water on clays, and the information about chemical-bonding in water and interaction between water and clay-mineral. The results show that clay-minerals adsorb water when they interact with water. The O—H's expanded and contracted frequency v will reduce along with adsorbed water content growth in hydro-clays. The process that O—H's expanded and contracted frequency v changes along with relative vapor pressure p/p s has the characteristics - fast first, slow then, fast again, and steady forever. There are two clear turning points which are p/ps=0.9, 0.98,the two turning points are the special humidity of clay-water system. The relative vapor pressure 0.9 is the boundary line between the strong bound water and the loose bound water(osmotic bound water) on clays, the relative vapor pressure 0.98 is the boundary line between the loose bound water and free water on clays. The results are identical with Ion exchange." @default.
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- W2376305779 date "2001-01-01" @default.
- W2376305779 modified "2023-09-26" @default.
- W2376305779 title "THE DETERMINATION OF BOUND WATER BOUNDARY ON CLAY SURFACE BY INFRARED SPECTRUM" @default.
- W2376305779 hasPublicationYear "2001" @default.
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