scholarly journals A swelling pressure cell for X-ray diffraction test

Géotechnique ◽  
2021 ◽  
pp. 1-40
Author(s):  
Hailong Wang ◽  
Hideo Komine ◽  
Takahiro Gotoh
1981 ◽  
Vol 212 (1188) ◽  
pp. 299-304 ◽  

X-ray diffraction has been used to measure the preferred orientation of the collagen fibrils, and their angular distribution within the tissue, as a function of depth from the articular surface in patellar cartilage. Measurements have been made at four different sites chosen to represent differing surface curvatures and régimes of wear. The orientation of fibrils in the surface layer allows it to oppose the swelling pressure exerted by the gel of hydrated glycosaminoglycans within the cartilage. An intermediate layer (where a bimodal distribution of fibrils is sometimes resolved) allows the orientation of the fibrils to change, with increasing depth, until they are roughly perpendicular to the articular surface. In this deep layer the fibrils can tie into the underlying calcified tissue so as to firmly anchor the cartilage. In the plane of the surface the fibrils tend to be aligned in the direction of stress caused by motion.


2010 ◽  
Vol 81 (12) ◽  
pp. 125105 ◽  
Author(s):  
Manja Luzi ◽  
Matthias Girod ◽  
Rudolf Naumann ◽  
Judith M. Schicks ◽  
Jörg Erzinger

2010 ◽  
Vol 81 (6) ◽  
pp. 064103 ◽  
Author(s):  
Nicholas J. Brooks ◽  
Beatrice L. L. E. Gauthe ◽  
Nick J. Terrill ◽  
Sarah E. Rogers ◽  
Richard H. Templer ◽  
...  

2009 ◽  
Vol 80 (3) ◽  
pp. 035107
Author(s):  
Béatrice L. L. E. Gauthé ◽  
Andrew J. Heron ◽  
John M. Seddon ◽  
Oscar Ces ◽  
Richard H. Templer

1996 ◽  
Vol 3 (5) ◽  
pp. 220-224 ◽  
Author(s):  
C. C. Tang ◽  
C. A. Koh ◽  
A. A. Neild ◽  
R. J. Cernik ◽  
R. E. Motie ◽  
...  

Clay Minerals ◽  
1971 ◽  
Vol 9 (2) ◽  
pp. 193-208 ◽  
Author(s):  
J. A. Rausell-Colom ◽  
P. S. Salvador

AbstractVermiculite single crystals swell to the gel state as a consequence of treatment with concentrated solutions of γ-aminobutyric acid.The amount of swelling was determined, by measuring by X-ray diffraction the separation of the elementary silicate layers in the gel-like crystals.By application of pressures into the gels along the swelling direction, a direct measure of the swelling pressure is obtained. The relation between swelling pressures and equilibrium interlayer distances is a function of both cationic concentration and dielectric constant of the solution. Measured swelling pressures are consistent with a model based on formation and interaction of diffuse double layers of aminoacid cations around the silicate particles, these having a Stern layer of an approximate thickness of 5 Å. The specific chemical adsorption potential of the system has been estimated as φ = 3·3 + 0·2 Kcal/mol.


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