A simple theoretical approach to the thermal expansion mechanism of salt weathering

CATENA ◽  
2016 ◽  
Vol 147 ◽  
pp. 695-698 ◽  
Author(s):  
Zhen-Ting Wang ◽  
Zhi-Shan An
Author(s):  
Jun Wu ◽  
Honggang Liu ◽  
Zhiyu He ◽  
Hui Luo ◽  
Baojun Chen ◽  
...  

2005 ◽  
Vol 80 (8) ◽  
pp. 2161-2164 ◽  
Author(s):  
Hidehiko Kobayashi ◽  
Ikuo Yanase ◽  
Takashi Mitamura

RSC Advances ◽  
2015 ◽  
Vol 5 (3) ◽  
pp. 1801-1807 ◽  
Author(s):  
Hongping Li ◽  
Shuai Liu ◽  
Lin Chen ◽  
Jiandong Zhao ◽  
Beibei Chen ◽  
...  

We investigate electrical and magnetic properties of an A-site-ordered perovskite SrCu3Fe4O12 and clarify its negative thermal expansion mechanism.


2017 ◽  
Vol 55 (05) ◽  
pp. 351-356
Author(s):  
I. SHTABLAVYI ◽  
S. MUDRY ◽  
U. LIUDKEVYCH

2021 ◽  
Vol 8 (1) ◽  
Author(s):  
Chiaki T. Oguchi ◽  
Swe Yu

AbstractSalt weathering can cause substantial deterioration of natural rocks, building stones, masonry materials, monuments, and engineering structures. Nearly two centuries of salt weathering studies, both theoretically and empirically, have manifested its power as well as its complexity. This paper attempts to unite the kinds of literature assess the various theories in the light of the combined information. The theoretical approaches concerning the most cited mechanisms of salt weathering such as crystallization, hydration and thermal expansion of crystalline salts are thoroughly reviewed. It is understood that there is no universally acceptable hard and sound theoretical information on this topic yet. More precise theories should be developed to elucidate the complications of the mechanisms of salt weathering as well as to interpret the results of empirical studies.


Minerals ◽  
2021 ◽  
Vol 11 (8) ◽  
pp. 911
Author(s):  
Javier Martínez-Martínez ◽  
Anna Arizzi ◽  
David Benavente

This research focuses on the analysis of the influence of two secondary salt weathering processes on the durability of rocks exposed to marine environments: chemical dissolution of rock forming minerals and differential thermal expansion between halite and the hosting rock. These processes are scarcely treated in research compared to salt crystallisation. The methodology followed in this paper includes both in situ rock weathering monitoring and laboratory simulations. Four different calcite-bearing rocks (a marble, a microcrystalline limestone and two different calcarenites) were exposed during a year to a marine semiarid environment. Exposed samples show grain detachment, crystal edge corrosion, halite efflorescences and microfissuring. Crystal edge corrosion was also observed after the laboratory simulation during a brine immersion test. Calcite chemical dissolution causes a negligible porosity increase in all the studied rocks, but a significant modification of their pore size distribution. Laboratory simulations also demonstrate the deterioration of salt-saturated rocks during thermal cycles in climatic cabinet. Sharp differences between the linear thermal expansion of both a pure halite crystal and the different studied rocks justify the registered weight loss during the thermal cycles. The feedback between the chemical dissolution and differential thermal expansion, and the salt crystallisation of halite, contribute actively to the rock decay in marine environments.


RSC Advances ◽  
2016 ◽  
Vol 6 (24) ◽  
pp. 19903-19909 ◽  
Author(s):  
M. P. Attfield ◽  
M. Feygenson ◽  
J. C. Neuefeind ◽  
T. E. Proffen ◽  
T. C. A. Lucas ◽  
...  

Combined Rietveld refinement and pair distribution function analysis of total neutron scattering data unveils the finer details of the negative thermal expansion mechanism of siliceous faujasite.


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