interlamellar water
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Langmuir ◽  
2005 ◽  
Vol 21 (10) ◽  
pp. 4610-4614 ◽  
Author(s):  
Yanli Guo ◽  
Hiroharu Yui ◽  
Hiroyuki Minamikawa ◽  
Mitsutoshi Masuda ◽  
Shoko Kamiya ◽  
...  
Keyword(s):  
Ft Ir ◽  

2004 ◽  
Vol 416 (1-2) ◽  
pp. 105-111 ◽  
Author(s):  
M. Kodama ◽  
M. Abe ◽  
Y. Kawasaki ◽  
K. Hayashi ◽  
S. Ohira ◽  
...  

2000 ◽  
Vol 122 (25) ◽  
pp. 6028-6038 ◽  
Author(s):  
Narayanaswamy Arun ◽  
Sukumaran Vasudevan ◽  
Krishna Venkatachala Ramanathan
Keyword(s):  

2000 ◽  
Vol 40 (supplement) ◽  
pp. S85
Author(s):  
H. Saguchi ◽  
H. Nakamura ◽  
H. Aoki ◽  
M. Kodama

Clay Minerals ◽  
1997 ◽  
Vol 32 (3) ◽  
pp. 463-470 ◽  
Author(s):  
A. Ben Haj Amara

AbstractAn homogenous 8.4 Å hydrate was obtained after washing intercalated KAc- nacrite. X-ray diffraction analysis based on comparison of the experimental and calculated profiles enabled the amount of water (one molecule per Si2Al2O5(OH)4) and the z coordinate along c* (6.5 Å) to be determined. The hydration state was accompanied by a decrease in the coherent domain along c* in the order nacrite > KAc-nacrite > H2O-nacrite. The IR spectrum of the hydrated nacrite showed an evolution of the structure with a shift of ν(OH) from 3702, 3649 and 3630 cm−1 to 3690, 3641 and 3620 cm−1, respectively for the nacrite hydroxyls. The ν(OH) stretching bands of the interlayer water appeared at 3602 and 3545 cm−1 and their bending band at 1655 cm−1. The TGA/DTG analysis of the air-dry hydrated nacrite showed a loss of water at 245°C the weight loss (1 molecule per Si2Al2O5(OH)4) corresponding to the interlamellar water, in agreement with that determined by XRD.


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