Randomly interstratified illite-vermiculite from weathering of illite in red earth sediments in Xuancheng, southeastern China

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• 作者：Hanlie Hong ; Gordon Jock Churchman ; Ke Yin ; Rongbiao Li ; Zhaohui Li
• 关键词：Red earth ; Clay minerals ; Mixed-layer illite&ndash ; vermiculite (I/V) ; Pedogenesis ; Palaeoclimate
• 刊名：Geoderma
• 出版年：February, 2014
• 年：2014
• 卷：214-215
• 期：Complete
• 页码：42-49
• 全文大小：1100 K

文摘

Mixed-layer illite-vermiculite (I/V) clays of the Xuancheng red earth were investigated using X-ray diffraction (XRD), Fourier-transform infrared (FTIR) spectrometer, and high-resolution transmission electron microscopy (HRTEM) methods. The XRD results indicated that the mixed layer I/V clays were characterized by the broad 10-14 脜 peak with a maximum intensity at ~ 12 脜 in air-dried sample, which decomposed into two peaks at 10 脜 and 14 脜 peaks respectively after ethylene glycol treatment. After K⁺ saturation, the 14 脜 peak changed to 10 脜, which reverted back to 14 脜 after saturation with Mg^2 + with a notable decrease in intensity of the 10 脜 peak. The broad 10-14 脜 peak collapsed to 10 脜 on heating to 400 掳C. These suggested that the broad 10-14 脜 peak resulted from randomly interstratified illite-vermiculite clays together with discrete illite and also vermiculite. HRTEM observation showed that straight 10 脜 illite layers were interstratified with 12 脜 vermiculite layers, suggesting that transformation of illite to vermiculite involves an exchange of K⁺ by hydrated cations associated with a swelling of the illite. The (060) spacing of I/V clay is 1.50 脜, indicating a dioctahedral precursor of illite and thus reinforcing the transformation from illite to vermiculite. FTIR analysis suggested that most band positions of vermiculite and illite in mixed-layer I/V did not change in comparison with those of the discrete clay species, indicating that the basic crystal structure of mixed-layer illite-vermiculite remains the same as the discrete clays. The interlayer cations in the interlayer region of vermiculite layers of the I/V clays are mainly Ca and minor Mg, Al, and Fe. The abundant Ca makes the I/V clays to behave like I/S on glycolated and thermal treatment, while the Mg, Al, and Fe complex ions in the interlayer region cause the vermiculite layer to lose its expandability and to behave like chlorite. The mixed-layer I/V clays were widely formed in late Quaternary alluvial fans in subtropical to tropical areas, where the sediments experienced synchronous pedogenic modification. The syndepositional pedogenesis process leads to an incomplete transformation of illite to vermiculite and causes the formation of metastable intermediates of mixed-layer illite-vermiculite.