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Carbonyl compounds in the atmosphere: A review of abundance, source and their contributions to O3 and SOA formation 期刊论文
Atmospheric Research, 2022
作者:  Qian Liu, Yuan Gao, Weiwen Huang, Zhenhao Ling, ... Xuemei Wang
收藏  |  浏览/下载:19/0  |  提交时间:2022/04/15
Copernican-aged (<200 Ma) Impact Ejecta at the Chang’e-5 Landing Site: Statistical Evidence from Crater Morphology, Morphometry and Degradation Models 期刊论文
Geophysical Research Letters, 2021
作者:  Yuqi Qian;  Long Xiao;  James W. Head;  Christian Wö;  hler;  Roberto Bugiolacchi;  Thorsten Wilhelm;  Stephanie Althoff;  Binlong Ye;  Qi He;  Yuefeng Yuan;  Siyuan Zhao
收藏  |  浏览/下载:12/0  |  提交时间:2021/10/22
An Improved Universal Fusion Algorithm for Constructing 3D Multiscale Porous Media 期刊论文
Water Resources Research, 2021
作者:  Shuaibing Song;  Ming Li;  Qingyi Tu;  Anying Yuan;  Zhenhua Jiao;  Pan Li;  Wenxin Qian;  Hewu Liu;  Nan Xu
收藏  |  浏览/下载:12/0  |  提交时间:2021/08/10
Toroidal polar topology in strained ferroelectric polymer 期刊论文
Science, 2021
作者:  Mengfan Guo;  Changqing Guo;  Jian Han;  Shulin Chen;  Shan He;  Tongxiang Tang;  Qian Li;  Joseph Strzalka;  Jing Ma;  Di Yi;  Ke Wang;  Ben Xu;  Peng Gao;  Houbing Huang;  Long-Qing Chen;  Shujun Zhang;  Yuan-Hua Lin;  Ce-Wen Nan;  Yang Shen
收藏  |  浏览/下载:13/0  |  提交时间:2021/03/12
Stocks and losses of soil organic carbon from Chinese vegetated coastal habitats 期刊论文
Global Change Biology, 2020
作者:  Chuancheng Fu;  Yuan Li;  Lin Zeng;  Haibo Zhang;  Chen Tu;  Qian Zhou;  Kuanxu Xiong;  Jiaping Wu;  Carlos M. Duarte;  Peter Christie;  Yongming Luo
收藏  |  浏览/下载:11/0  |  提交时间:2020/09/30
China's potential SO2 emissions from coal by 2050 期刊论文
Energy Policy, 2020
作者:  Yuan Qian, Laura Scherer, Arnold Tukker, Paul Behrens
收藏  |  浏览/下载:6/0  |  提交时间:2020/09/08
Proton-assisted growth of ultra-flat graphene films 期刊论文
NATURE, 2020, 577 (7789) : 204-+
作者:  Yuan, Guowen;  Lin, Dongjing;  Wang, Yong;  Huang, Xianlei;  Chen, Wang;  Xie, Xuedong;  Zong, Junyu;  Yuan, Qian-Qian;  Zheng, Hang;  Wang, Di;  Xu, Jie;  Li, Shao-Chun;  Zhang, Yi;  Sun, Jian;  Xi, Xiaoxiang;  Gao, Libo
收藏  |  浏览/下载:9/0  |  提交时间:2020/07/03

Graphene films grown by chemical vapour deposition have unusual physical and chemical properties that offer promise for applications such as flexible electronics and high-frequency transistors(1-10). However, wrinkles invariably form during growth because of the strong coupling to the substrate, and these limit the large-scale homogeneity of the film(1-4,11,12). Here we develop a proton-assisted method of chemical vapour deposition to grow ultra-flat graphene films that are wrinkle-free. Our method of proton penetration(13-17) and recombination to form hydrogen can also reduce the wrinkles formed during traditional chemical vapour deposition of graphene. Some of the wrinkles disappear entirely, owing to the decoupling of van der Waals interactions and possibly an increase in distance from the growth surface. The electronic band structure of the as-grown graphene films shows a V-shaped Dirac cone and a linear dispersion relation within the atomic plane or across an atomic step, confirming the decoupling from the substrate. The ultra-flat nature of the graphene films ensures that their surfaces are easy to clean after a wet transfer process. A robust quantum Hall effect appears even at room temperature in a device with a linewidth of 100 micrometres. Graphene films grown by proton-assisted chemical vapour deposition should largely retain their intrinsic performance, and our method should be easily generalizable to other nanomaterials for strain and doping engineering.


  
Controls on surface water carbonate chemistry along North American ocean margins 期刊论文
NATURE COMMUNICATIONS, 2020, 11 (1)
作者:  Cai, Wei-Jun;  Xu, Yuan-Yuan;  Feely, Richard A.;  Wanninkhof, Rik;  Jonsson, Bror;  Alin, Simone R.;  Barbero, Leticia;  Cross, Jessica N.;  Azetsu-Scott, Kumiko;  Fassbender, Andrea J.;  Carter, Brendan R.;  Jiang, Li-Qing;  Pepin, Pierre;  Chen, Baoshan;  Hussain, Najid;  Reimer, Janet J.;  Xue, Liang;  Salisbury, Joseph E.;  Martin Hernandez-Ayon, Jose;  Langdon, Chris;  Li, Qian;  Sutton, Adrienne J.;  Chen, Chen-Tung A.;  Gledhill, Dwight K.
收藏  |  浏览/下载:14/0  |  提交时间:2020/06/09
The Mantle Transition Zone Hosts the Missing HIMU Reservoir Beneath Eastern China 期刊论文
GEOPHYSICAL RESEARCH LETTERS, 2020, 47 (9)
作者:  Qian, Sheng-Ping;  Nichols, Alexander R. L.;  Zhang, Le;  Xu, Yi-Gang;  Li, Jie;  Guo, Yu-Long;  Ren, Zhong-Yuan
收藏  |  浏览/下载:10/0  |  提交时间:2020/07/02
late Cenozoic basalts  HIMU component  mantle transition zone  carbonated mantle source  
Millennial-scale hydroclimate control of tropical soil carbon storage 期刊论文
NATURE, 2020, 581 (7806) : 63-+
作者:  Lam, Tommy Tsan-Yuk;  Jia, Na;  Zhang, Ya-Wei;  Shum, Marcus Ho-Hin;  Jiang, Jia-Fu;  Zhu, Hua-Chen;  Tong, Yi-Gang;  Shi, Yong-Xia;  Ni, Xue-Bing;  Liao, Yun-Shi;  Li, Wen-Juan;  Jiang, Bao-Gui;  Wei, Wei;  Yuan, Ting-Ting;  Zheng, Kui;  Cui, Xiao-Ming;  Li, Jie;  Pei, Guang-Qian
收藏  |  浏览/下载:25/0  |  提交时间:2020/05/13

Over the past 18,000 years, the residence time and amount of soil carbon stored in the Ganges-Brahmaputra basin have been controlled by the intensity of Indian Summer Monsoon rainfall, with greater carbon destabilization during wetter, warmer conditions.


The storage of organic carbon in the terrestrial biosphere directly affects atmospheric concentrations of carbon dioxide over a wide range of timescales. Within the terrestrial biosphere, the magnitude of carbon storage can vary in response to environmental perturbations such as changing temperature or hydroclimate(1), potentially generating feedback on the atmospheric inventory of carbon dioxide. Although temperature controls the storage of soil organic carbon at mid and high latitudes(2,3), hydroclimate may be the dominant driver of soil carbon persistence in the tropics(4,5)  however, the sensitivity of tropical soil carbon turnover to large-scale hydroclimate variability remains poorly understood. Here we show that changes in Indian Summer Monsoon rainfall have controlled the residence time of soil carbon in the Ganges-Brahmaputra basin over the past 18,000 years. Comparison of radiocarbon ages of bulk organic carbon and terrestrial higher-plant biomarkers with co-located palaeohydrological records(6) reveals a negative relationship between monsoon rainfall and soil organic carbon stocks on a millennial timescale. Across the deglaciation period, a depletion of basin-wide soil carbon stocks was triggered by increasing rainfall and associated enhanced soil respiration rates. Our results suggest that future hydroclimate changes in tropical regions are likely to accelerate soil carbon destabilization, further increasing atmospheric carbon dioxide concentrations.