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245	1	0	_aDehydration and rehydration of palygorskite and the influence of water on the nanopores
490	0		_vClays and Clay Minerals, 52(5), p.635-642, 2004
520	3		_aThe dehydration and rehydration processes of the clay mineral palygorskite (PFI-1)were studied by textural analysis,thermogravimetric analysis connected with mass spectrometry (TGA-MS), and 29Si and 1H solid-state NMR techniques. The TGA-MS results clearly reveal weight losses at maxima of 70°C, 190°C, 430°C and 860°C. PFI-1 is characterized by a micropore area of 93 m 2/g, corresponding to a micropore volume of 47 mm 3/g. These values are also obtained for the sample heated up to 200°C for 20 h. Further heating at 300°C produces a collapse of the structure, as shown by the almost complete loss of microporosity. The 29Si NMR spectra of palygorskite show two main resonances at -92.0 and -97.5 ppm, attributed to one of the two pairs of equivalent Si nuclei in the basal plane. A minor resonance at -84.3 ppm is attributed to Q2(Si-OH)Si nuclei. The resonance at -92.0 ppm is assigned to the central Si position, while the resonance at -97.5 ppm is assigned to the edge Si sites. It is confirmed by solid-state 29Si and 1H NMR that nearly complete rehydration is achieved by exposing palygorskite samples that have been partially dehydrated at 150°C and 300°C, to D2O or water vapor at room temperature, When the rehydration is accomplished with D2O, the atoms are disordered across all the protons sites. © 2004, The Clay Minerals Society.
650	1	4	_aDEHYDRATION
650	1	4	_aMASS SPECTROMETRY
650	1	4	_aMICROPOROSITY
650	1	4	_aNUCLEAR MAGNETIC RESONANCE SPECTROSCOPY
650	1	4	_aRESONANCE
650	1	4	_aSURFACE PROPERTIES
650	1	4	_aTEMPERATURE CONTROL
650	1	4	_aTHERMOGRAVIMETRIC ANALYSIS
700	1	2	_aKuang, W.
700	1	2	_aFacey, G.A.
700	1	2	_aDetellier, C.E
856	4	0	_uhttps://drive.google.com/file/d/1J35bc6BNtYAoDHeXojbZ__6GT4r5SRp-/view?usp=drivesdk _zPara ver el documento ingresa a Google con tu cuenta: @cicy.edu.mx
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