Chemical weathering and the role of sulfuric and nitric acids in carbonate weathering: Isotopes (13C,15N,34S, and18O) and chemical constraints-Reference-Cited by-同舟云学术

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Chemical weathering and the role of sulfuric and nitric acids in carbonate weathering: Isotopes (13C,15N,34S, and18O) and chemical constraints

Published:2016-05 Issue:5 Volume:121 Page:1288-1305
ISSN:2169-8953
Container-title:Journal of Geophysical Research: Biogeosciences
language:en
Short-container-title:J. Geophys. Res. Biogeosci.

Author:

Li Cai¹,Ji Hongbing¹²

Affiliation:

1. School of Civil and Environmental Engineering; University of Science and Technology Beijing; Beijing China

2. State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry; Chinese Academy of Sciences; Guiyang China

Funder

National Natural Science Foundation of China

National Key Basic Research and Development Program

Hundred Talents Programs of Chinese Academy of Sciences

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Atmospheric Science,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry

Reference57 articles.

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2. The natural isotope content of nitrate as an indicator of its origin;Amberger;Geochim. Cosmochim. Acta,1987

3. O2 and H2O are each the source of one O in NO2-produced from NH3 by Nitrosomonas: 15N-NMR evidence;Andersson;FEBS Lett.,1983

4. Seasonal variations of dissolved inorganic carbon and δ13CDIC of surface water: Application of a modified gas evolution technique;Atekwana;J. Hydrol.,1998

5. The contribution of agricultural and urban activities to inorganic carbon fluxes within temperate watersheds;Barnes;Chem. Geol.,2009

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