首页> 外文期刊>Journal of the American Chemical Society >PORE SIZE DETERMINATION OF MCM-41 MESOPOROUS MATERIALS BY MEANS OF H-1 NMR SPECTROSCOPY, N-2 ADSORPTION, AND HREM - A PRELIMINARY STUDY
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PORE SIZE DETERMINATION OF MCM-41 MESOPOROUS MATERIALS BY MEANS OF H-1 NMR SPECTROSCOPY, N-2 ADSORPTION, AND HREM - A PRELIMINARY STUDY

机译:H-1 NMR波谱,N-2吸附和HREM介孔法测定MCM-41介孔材料的初步研究

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The aim of the present study is to derive a mathematical pore size distribution function containing a limited number of adjustable parameters. These parameters can be determined exclusively from H-1 NMR measurements. Regular mesoporous MCM-41 materials with different pore sizes, ranging from 20 to 30 Angstrom, were synthesized and characterized by HREM, N-2 adsorption, and H-1 NMR. The pore sizes determined by Nf adsorption and HREM were in good agreement. The H-1 NMR technique was used to determine the freezing point of water enclosed in water-saturated samples. By combining N-2 adsorption and H-1 NMR measurements, a simple relation was found between the freezing point depression (Delta T) and the pore radius (R(p)): Delta T = K/(R(p) - t(f)) with t(f) = 3.49 +/- 0 36 Angstrom. The observation that t(f) not equal 0 is tentatively explained by the formation of a surface layer of nonfreezing water of thickness t(f), which effectively reduces the actual pore radius from R(p) to R(p) - t(f). A mathematical model is derived which enables the pore size distribution to be determined from H-1 NMR intensity vs temperature measurements of water-saturated materials. The pore size distribution of amorphous' silica determined independently by H-1 NMR and N-2 adsorption agreed well. However, the pore size of a microporous VPI-5 material (R(p) = 6.05 Angstrom) could not be predicted by the present model. [References: 41]
机译:本研究的目的是导出包含有限数量的可调参数的数学孔径分布函数。这些参数只能由H-1 NMR测量确定。合成了具有20-30埃的不同孔径的常规介孔MCM-41材料,并通过HREM,N-2吸附和H-1 NMR对其进行了表征。由Nf吸附和HREM确定的孔径大小吻合良好。使用H-1 NMR技术确定含水饱和样品中所含水的凝固点。通过结合N-2吸附和H-1 NMR测量,发现冰点降低(Delta T)与孔半径(R(p))之间的简单关系:Delta T = K /(R(p)-t (f)),其中t(f)= 3.49 +/- 0 36埃。尝试通过形成厚度为t(f)的非冷冻水表面层来解释t(f)不等于0的现象,该表层有效地将实际孔半径从R(p)减小到R(p)-t( F)。推导了数学模型,该数学模型使得可以从H-1 NMR强度与水饱和材料的温度测量值确定孔径分布。通过H-1 NMR和N-2吸附独立确定的非晶态二氧化硅的孔径分布非常吻合。但是,本模型无法预测微孔VPI-5材料的孔径(R(p)= 6.05埃)。 [参考:41]

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