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Experimental water intrusion–extrusion isotherms were performed at room temperature on various 1D channel pure silica AFI, MTW and TON-type zeolites. The water intrusion is obtained by applying a high hydraulic pressure corresponding to the intrusion step. Whatever, the zeosil, when the pressure is released, the water extrusion occurs at a similar pressure to that of the intrusion one. These “zeosil–water”...
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