scholarly journals Coarse-grained interaction potentials for polyaromatic hydrocarbons

2006 ◽  
Vol 124 (5) ◽  
pp. 054307 ◽  
Author(s):  
O. A. von Lilienfeld ◽  
Denis Andrienko
2006 ◽  
Vol 124 (17) ◽  
pp. 174708 ◽  
Author(s):  
M. Babadi ◽  
R. Everaers ◽  
M. R. Ejtehadi

Author(s):  
R. E. Ferrell ◽  
G. G. Paulson

The pore spaces in sandstones are the result of the original depositional fabric and the degree of post-depositional alteration that the rock has experienced. The largest pore volumes are present in coarse-grained, well-sorted materials with high sphericity. The chief mechanisms which alter the shape and size of the pores are precipitation of cementing agents and the dissolution of soluble components. Each process may operate alone or in combination with the other, or there may be several generations of cementation and solution.The scanning electron microscope has ‘been used in this study to reveal the morphology of the pore spaces in a variety of moderate porosity, orthoquartzites.


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