Natural variations in calcite dissolution rates in streams: Controls, implications, and open questions-Reference-Cited by-同舟云学术

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Natural variations in calcite dissolution rates in streams: Controls, implications, and open questions

Published:2015-04-28 Issue:8 Volume:42 Page:2836-2843
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Covington M. D.¹²,Gulley J. D.³,Gabrovšek F.²

Affiliation:

1. Department of Geosciences; University of Arkansas; Fayetteville Arkansas USA

2. Karst Research Institute, ZRC SAZU; Postojna Slovenia

3. Department of Geological and Mining Engineering and Sciences; Michigan Technological University; Houghton Michigan USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2015GL063044/fullpdf

Reference54 articles.

1. Some carbonate erosion rates of southeast Alaska;Allred;J. Cave Karst Stud.,2004

2. Hydraulic boundary conditions as a controlling factor in karst genesis: A numerical modeling study on artesian conduit development in gypsum;Birk;Water Resour. Res.,2003

3. The kinetics of calcite dissolution and precipitation in geologically relevant situations of karst areas: 1. Open system;Buhmann;Chem. Geol.,1985a

4. The kinetics of calcite dissolution and precipitation in geologically relevant situations of karst areas: 2. Closed system;Buhmann;Chem. Geol.,1985b

5. Physically based modeling of bedrock incision by abrasion, plucking, and macroabrasion;Chatanantavet;J. Geophys. Res.,2009

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