Dissolution rates of minerals and their relation to surface morphology

Geochimica et Cosmochimica Acta

Volumn 66, Issue 17, 2002, Pages 3055-3062

  Jeschke, Alexander A ^a   Dreybrodt, Wolfgang ^a  

^a UNIVERSITY OF BREMEN   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

AQUEOUS SOLUTION; BOUNDARY LAYER; DISSOLUTION; FRACTAL ANALYSIS; REACTION RATE; SURFACE AREA;

EID: 0036742219     PISSN: 00167037     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0016-7037(02)00893-1     Document Type: Article

References (17)

1. Experimental studies of halite dissolution kinetics. I. The effect of saturation state and the presence of trace metals
2. Surface roughness of minerals and implications for dissolution studies
3. The kinetics of calcite dissolution and precipitation in geologically relevant situations of karst areas. 1. Open system
4. 2 solutions
5. Are quartz dissolution rates proportional to B.E.T. surface areas?
6. Micropore surface area variation with grain size in unweathered alkali feldspars: Implications for surface roughness and dissolution studies
7. Origins of the surface roughness of unweathered alkali feldspar grains
8. Surface controlled dissolution rates of gypsum in aqueous solutions exhibit nonlinear dissolution kinetics
9. -
10. Transport control in crystal growth from solution
11. 2
12. 2-water systems approaching calcite equillibrium
13. Mechanisms of growth and dissolution of sparingly soluble salts