期刊
CLAY MINERALS
卷 43, 期 2, 页码 195-203出版社
MINERALOGICAL SOC
DOI: 10.1180/claymin.2008.043.2.04
关键词
palygorskite; Cu; adsorbed site; adsorption; absorption; XPS; FTIR; ESR; XRD
Desorption experiments performed on four CLI-adsorbed palygorskites Suggest that the leached CIA 21 ion originates at the Surface and/or net-like interstice of the palygorskite fibres. The leached fraction, calculated from the quantities of adsorbed Cu 2 before and after desorption, is
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