GUO LAODONG, GUO JINBAO, LI FAXI. PHYSICOCHEMICAL PROCESSES OF SILICATES IN THE ESTUARINE REGION: Ⅴ. A SIMULATION EXPERIMENT ON THE FORMATION OF AUTHIGENIC SILICATE MINERALS BY ADSORPTION[J]. Acta Oceanologica Sinica, 1986, (1): 70-75.
Citation:
GUO LAODONG, GUO JINBAO, LI FAXI. PHYSICOCHEMICAL PROCESSES OF SILICATES IN THE ESTUARINE REGION: Ⅴ. A SIMULATION EXPERIMENT ON THE FORMATION OF AUTHIGENIC SILICATE MINERALS BY ADSORPTION[J]. Acta Oceanologica Sinica, 1986, (1): 70-75.
GUO LAODONG, GUO JINBAO, LI FAXI. PHYSICOCHEMICAL PROCESSES OF SILICATES IN THE ESTUARINE REGION: Ⅴ. A SIMULATION EXPERIMENT ON THE FORMATION OF AUTHIGENIC SILICATE MINERALS BY ADSORPTION[J]. Acta Oceanologica Sinica, 1986, (1): 70-75.
Citation:
GUO LAODONG, GUO JINBAO, LI FAXI. PHYSICOCHEMICAL PROCESSES OF SILICATES IN THE ESTUARINE REGION: Ⅴ. A SIMULATION EXPERIMENT ON THE FORMATION OF AUTHIGENIC SILICATE MINERALS BY ADSORPTION[J]. Acta Oceanologica Sinica, 1986, (1): 70-75.
PHYSICOCHEMICAL PROCESSES OF SILICATES IN THE ESTUARINE REGION: Ⅴ. A SIMULATION EXPERIMENT ON THE FORMATION OF AUTHIGENIC SILICATE MINERALS BY ADSORPTION
Authigenic silicate minerals similar to Chamosite were synthesized under laboratory conditions, demonstrating that there may exist a geochemical process of authigenic silicate minerals formation by coagulation, adsorption, structural rearrangement and crystallization from dissolved substances in estuarine and marine environments.This also further confirms our previous geochemical removal pattern of dissolved silica in the estuarine region.Results show that the authigenic silicate minerals is one of the significant sinks of the chemical removal of dissolved silica from seawater.
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