Abstract
Disproportionation of methyltrichlorosilane (MTS) to produce dimethyldichlorosilane (DMCS) was firstly carried out over a bentonite from Zhejiang province (China) after H2SO4 activation. The results demonstrated that the bentonite activated with 30 wt% H2SO4 solution exhibited an excellent activity with 92% conversion of MTS and 41% yield of DMCS at 673 K under atmospheric pressure. The catalysts were characterized by inductively coupled plasma atomic emission spectroscopy (ICP-AES), X-ray powder diffraction (XRD) and N2 absorption–desorption. The acidic sites of these bentonites were studied by in situ FTIR spectra of pyridine adsorption. It revealed that the coexistence of Lewis (L) and Brønsted (B) acidic sites facilitated the formation of DMCS and reaction temperature played important roles in the disproportionation reaction.
GRAPHICAL ABSTRACT
Acknowledgments
This work was supported by the National Natural Science Foundation of China (No. 21062013 and 20562007), the Foundation of Educational Department of Jiangxi Province and the Graduate Innovation Foundation of Jiangxi Province (No.YC09A032).
Notes
aSiO2 content was calculated according to the contents of other compositions.
a Volume ratio of liquid : solid was 3.
b The integral area of d(001) diffraction peak.
c The samples surface area were calculated using the Brunauer–Emmett–Teller (BET) method based on adsorption data in the partial pressure (P/P 0) range of 0.05–0.35.
d The average pore size was obtained from the adsorption data by the Barrett–Joyner–Halenda (BJH) method.