Experimental warming increased soil nitrogen sink in the Tibetan permafrost-Reference-Cited by-同舟云学术

Experimental warming increased soil nitrogen sink in the Tibetan permafrost

Published:2017-07 Issue:7 Volume:122 Page:1870-1879
ISSN:2169-8953
Container-title:Journal of Geophysical Research: Biogeosciences
language:en
Short-container-title:J. Geophys. Res. Biogeosci.

Author:

Chang Ruiying¹,Wang Genxu¹,Yang Yuanhe²,Chen Xiaopeng¹

Affiliation:

1. Key Laboratory of Mountain Environment Evolvement and Regulation; Institute of Mountain Hazards and Environment, Chinese Academy of Sciences; Chengdu China

2. State Key Laboratory of Vegetation and Environmental Change; Institute of Botany, Chinese Academy of Sciences; Beijing China

Funder

National Basic Research Program of China

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

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

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2017JG003827/fullpdf

Reference71 articles.

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2. Abiotic nitrogen uptake in semiarid grassland soils of the U.S. Great Plains;Barrett;Soil Sci. Soc. Am. J.,2002

3. Contributions of nitrification and denitrification to N2O emissions from soils at different water-filled pore space;Bateman;Biol. Fertil. Soils,2005

4. Importance of cryoturbation in redistributing organic carbon in permafrost-affected soils;Bockheim;Soil Sci. Soc. Am. J.,2007

5. Cryopedology

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