Effects of time and temperature of firing on Fe-rich ceramics studied by Mossbauer spectroscopy and two-dimensional 1H-nuclear magnetic resonance relaxometry

被引:6
|
作者
Casieri, Cinzia [1 ,2 ]
De Luca, Francesco [3 ,4 ]
Nodari, Luca [5 ,6 ]
Russo, Umberto [5 ,6 ]
Terenzi, Camilla [7 ]
Tudisca, Valentina [7 ]
机构
[1] Univ Aquila, CNR IPCF UOS Roma, I-67010 Coppito, Laquila, Italy
[2] Univ Aquila, Dipartimento Sci Fis & Chim, I-67010 Coppito, Italy
[3] Univ Roma La Sapienza, CNR IPCF UOS Roma, I-00185 Rome, Italy
[4] Univ Roma La Sapienza, Dipartimento Fis, I-00185 Rome, Italy
[5] Univ Padua, Padova Res Unit, INSTM Consortium, I-35135 Padua, Italy
[6] Univ Padua, Dipartimento Sci Chim, I-35135 Padua, Italy
[7] Univ Roma La Sapienza, Dipartimento Fis, I-00185 Rome, Italy
关键词
ANCIENT CERAMICS; NMR RELAXATION; POROUS-MEDIA; CLAYS; DIFFUSION; SPECTROMETRY; DIFFRACTION; SPECTRA; POTTERY; WATER;
D O I
10.1063/1.4759316
中图分类号
O59 [应用物理学];
学科分类号
摘要
The combined effects of firing temperature and soaking time on the microstructure of iron-rich porous ceramics have been studied by Fe-57-Mossbauer spectroscopy and 2D H-1 nuclear magnetic resonance (NMR) relaxometry using a single-sided probe. Examining water-saturated ceramics using the relaxation correlation method, where longitudinal (T-1) and transverse (T-2) relaxation times are measured concurrently, provides information about firing-induced changes in both porosity (related to T-1) and magnetic properties (related to T-2). Comparing the information obtained from H-1-NMR analyses with that obtained from Mossbauer spectroscopy (which characterizes changes in iron-bearing species) shows that the T-1-T-2 NMR correlation technique is very sensitive to even subtle modifications in the magnetic behavior of Fe-bearing species. Moreover, the single-sided NMR approach allows us to perform millimeter-scale depth-resolved measurements, which can be used to non-invasively study the microstructural heterogeneities associated with non-uniform firing effects inside ceramics. This is in contrast to Mossbauer spectroscopy, which requires that the ceramic samples be ground. (C) 2012 American Institute of Physics. [http://dx.doi.org/10.1063/1.4759316]
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页数:15
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