Niwa Miki, Suzuki Katsuki, Katada Naonobu, Kanougi Tomonori, Atoguchi Takashi
Department of Materials Science, Faculty of Engineering, Tottori University 4-101, Koyama-minami, Tottori, 680-8552 Japan.
J Phys Chem B. 2005 Oct 13;109(40):18749-57. doi: 10.1021/jp051304g.
Using an IRMS-TPD (temperature programmed desorption) of ammonia, we studied the nature, strength, crystallographic location, and distribution of acid sites of mordenite. In this method, infrared spectroscopy (IR) and mass spectroscopy (MS) work together to follow the thermal behavior of adsorbed and desorbed ammonia, respectively; therefore, adsorbed species were identified, and their thermal behavior was directly connected with the desorption of ammonia during an elevation of temperature. IR-measured TPD of the NH4(+) cation was similar to MS-measured TPD, thus showing the nature of Brønsted acidity. From the behavior of OH bands, it was found that the Brønsted acid sites consisted of two kinds of OH bands at high and low wavenumbers, ascribable to OH bands situated on 12- and 8-member rings (MR) of mordenite structure, respectively. The amount and strength of these Brønsted hydroxyls were measured quantitatively based on a theoretical equation using a curve fitting method. Up to ca. 30% of the exchange degree, NH4(+) was exchanged with Na+ on the 12-MR to arrive at saturation; therefore, in this region, the Brønsted acid site was situated on the large pore of 12-MR. The NH4(+) cation was then exchanged with Na+ on 8-MR, and finally exceeded the amount on 12-MR. In the 99% NH4-mordenite, Brønsted acid sites were located predominantly on the 8-MR more than on the 12-MR. Irrespective of the NH4(+) exchange degree, the strengths deltaH of Brønsted OH were 145 and 153 kJ mol(-1) on the 12- and 8-MR, respectively; that is, the strength of Brønsted acid site on the 8-MR was larger than that on the 12-MR. A density functional theory (DFT) calculation supported the difference in the strengths of the acid sites. Catalytic cracking activity of the Brønsted acid sites on the 8-MR declined rapidly, while that on the 12-MR was remarkably kept. The difference in strength and/or steric capacity may cause such a difference in the life of a catalyst.
我们使用氨的红外质谱 - 程序升温脱附(IRMS - TPD)方法研究了丝光沸石酸位的性质、强度、晶体学位置和分布。在该方法中,红外光谱(IR)和质谱(MS)协同工作,分别跟踪吸附和脱附氨的热行为;因此,可以识别吸附物种,并将它们的热行为与升温过程中氨的脱附直接联系起来。红外测量的NH4(+)阳离子的TPD与质谱测量的TPD相似,从而显示出布朗斯台德酸性的本质。从OH带的行为发现,布朗斯台德酸位由高波数和低波数的两种OH带组成,分别归因于位于丝光沸石结构的12元环和8元环(MR)上的OH带。基于理论方程,使用曲线拟合方法对这些布朗斯台德羟基的数量和强度进行了定量测量。在交换度达到约30%之前,NH4(+)在12元环上与Na+交换直至饱和;因此,在该区域,布朗斯台德酸位位于12元环的大孔上。然后NH4(+)阳离子在8元环上与Na+交换,最终超过了在12元环上的量。在99%的NH4 - 丝光沸石中,布朗斯台德酸位主要位于8元环上,而不是12元环上。无论NH4(+)的交换度如何,12元环和8元环上布朗斯台德OH的强度ΔH分别为145和153 kJ mol(-1);也就是说,8元环上布朗斯台德酸位的强度大于12元环上的。密度泛函理论(DFT)计算支持了酸位强度的差异。8元环上布朗斯台德酸位的催化裂化活性迅速下降,而12元环上的则显著保持。强度和/或空间容量的差异可能导致催化剂寿命出现这种差异。