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首页> 外文期刊>Applied Magnetic Resonance >Firing-Induced Microstructural Properties of Quasi-Diamagnetic Carbonate-Based Porous Ceramics: a H-1 NMR Relaxation Correlation Study
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Firing-Induced Microstructural Properties of Quasi-Diamagnetic Carbonate-Based Porous Ceramics: a H-1 NMR Relaxation Correlation Study

机译:准磁碳酸盐基多孔陶瓷的烧结诱导微观结构性质:H-1 NMR弛豫相关性研究

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This study deals with the application of two-dimensional proton nuclear magnetic resonance relaxometry (2D H-1 NMR-R) to the characterization of porous ceramics nearly free of magnetic compounds. Different microstructural properties were obtained by firing a diamagnetic mixture of kaolin, calcium, and magnesium carbonate over a wide range of maximum temperatures (600-1100 A degrees C) and firing times at the maximum temperature (soaking times) (0-10 h). The 2D H-1 NMR-R method relies on the correlated measurement of H-1 longitudinal (T (1)) and transverse (T (2)) relaxation times of pore-filling water by which the properties of the interconnected pore space may be investigated. In the absence of significant magnetic susceptibility effect due to para- and ferro-magnetic compounds, the 2D H-1 NMR-R maps allow studying the conjoint effects on pore size distribution and inter-pore coupling due to the variations in both time and temperature of firing. The NMR experiments were performed with a low-field H-1 NMR sensor, which allows non-destructive and in situ analysis. For ceramic specimens fired at 600 and 700 A degrees C, the fraction of smallest pores increases with firing time at the expenses of those with intermediate size. The pore shrinkage occurring at this stage, and likely associated with the transformation of kaolinite in metakaolinite, is affected in a similar way by soaking time and firing temperature, in line with the concept of equivalent firing temperature. At temperatures from 800 to 1100 A degrees C, the structural modifications involving interconnectivity and average pore size are driven primarily by firing temperature and, secondarily, by soaking time. The 2D H-1 NMR-R results are confirmed by more traditional, but destructive, mineralogical, and structural analyses like X-ray powder diffraction, helium pycnometry, mercury intrusion porosimetry, and nitrogen adsorption/desorption method.
机译:这项研究涉及二维质子核磁共振弛豫法(2D H-1 NMR-R)在表征几乎不含磁性化合物的多孔陶瓷中的应用。通过在宽泛的最高温度(600-1100 A摄氏度)范围内烧制高岭土,钙和碳酸镁的反磁性混合物,并在最高温度下烧制时间(均热时间)(0-10 h),可获得不同的微观结构性能。 。 2D H-1 NMR-R方法依赖于孔隙填充水的H-1纵向(T(1))和横向(T(2))弛豫时间的相关测量,通过此弛豫时间可以互连的孔隙空间的性质被调查。在没有由于顺磁性和铁磁性化合物引起的显着磁化率影响的情况下,二维H-1 NMR-R图谱允许研究由于时间和温度的变化而对孔径分布和孔间耦合产生的联合影响射击。 NMR实验是使用低场H-1 NMR传感器进行的,该传感器可以进行无损和原位分析。对于在600和700 A的温度下烧制的陶瓷样品,最小的细孔分数随烧制时间的增加而增加,而中等尺寸的烧损为代价。在此阶段发生的孔收缩,很可能与高岭石在偏高岭石中的转化有关,受浸入时间和烧成温度的影响也类似,这与等效烧成温度的概念一致。在800到1100 A的温度下,涉及互连性和平均孔径的结构改性主要是由烧结温度,其次是保温时间。 2D H-1 NMR-R结果已通过更传统的,但具有破坏性的矿物学和结构分析(如X射线粉末衍射,氦比重瓶法,压汞法和氮吸附/解吸法)得到了证实。

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