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Park C, Kim J, Lim W, Lee J. Toward maximum energy density enabled by anode-free lithium metal batteries: Recent progress and perspective. EXPLORATION (BEIJING, CHINA) 2024; 4:20210255. [PMID: 38855623 PMCID: PMC11022618 DOI: 10.1002/exp.20210255] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 02/24/2023] [Accepted: 07/16/2023] [Indexed: 06/11/2024]
Abstract
Owing to the emergenceof energy storage and electric vehicles, the desire for safe high-energy-density energy storage devices has increased research interest in anode-free lithium metal batteries (AFLMBs). Unlike general lithium metal batteries (LMBs), in which excess Li exists to compensate for the irreversible loss of Li, only the current collector is employed as an anode and paired with a lithiated cathode in the fabrication of AFLMBs. Owing to their unique cell configuration, AFLMBs have attractive characteristics, including the highest energy density, safety, and cost-effectiveness. However, developing AFLMBs with extended cyclability remains an issue for practical applications because the high reactivity of Li with limited inventory causes severely low Coulombic efficiency (CE), poor cyclability, and dendrite growth. To address these issues, tremendous effort has been devoted to stabilizing Li metal anodes for AFLMBs. In this review, the importance and challenges of AFLMBs are highlighted. Then, diverse strategies, such as current collectors modification, advanced electrolytes, cathode engineering, and operation protocols are thoroughly reviewed. Finally, a future perspective on the strategy is provided for insight into the basis of future research. It is hoped that this review provides a comprehensive understanding by reviewing previous research and arousing more interest in this field.
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Affiliation(s)
- Cheol‐Young Park
- Chemical and Biomolecular EngineeringKorea Advanced Institute of Science and Technology (KAIST)DaejeonRepublic of Korea
| | - Jinuk Kim
- Chemical and Biomolecular EngineeringKorea Advanced Institute of Science and Technology (KAIST)DaejeonRepublic of Korea
| | - Won‐Gwang Lim
- Chemical and Biomolecular EngineeringKorea Advanced Institute of Science and Technology (KAIST)DaejeonRepublic of Korea
- Present address:
Energy and Environment DirectoratePacific Northwest National Laboratory (PNNL), 902 Battelle BoulevardRichland 99354WashingtonUSA
| | - Jinwoo Lee
- Chemical and Biomolecular EngineeringKorea Advanced Institute of Science and Technology (KAIST)DaejeonRepublic of Korea
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Luo Y, Mi W, Gao Y, Qin L. Provenance Analysis in the Nima Basin during Paleogene and Its Implications for the Decline of the Tibetan Central Valley. ACS OMEGA 2024; 9:13148-13162. [PMID: 38524406 PMCID: PMC10955701 DOI: 10.1021/acsomega.3c09706] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 12/05/2023] [Revised: 02/03/2024] [Accepted: 02/14/2024] [Indexed: 03/26/2024]
Abstract
It is unclear what caused the Bangong Nujiang suture zone in the central Tibetan plateau to rise from less than 2 km in early Cenozoic to more than 4 km at present. The zircon U-Pb ages and trace elements of samples from the Niubao Formation in the Paleogene of the Nima basin were analyzed and tested. Combined with the isostasy theory, the surface uplift height of the Nima Basin during the Cenozoic period was calculated. The zircon U-Pb age results of the Niubao formation are consistent with the ages of the Lhasa terrane on the south side of the basin, the Qiangtang terrane on the north side, and the uplift in central. The zircon Eu/Eu* results show that the crust in central part of Tibetan plateau thickened by ∼20 km in Paleogene, resulting in ∼3 km surface uplift. Sediments created a total of about 1 km of surface uplift throughout the Paleogene, and the deposition rate began to slow down significantly at ∼40 Ma. Therefore, it is inferred that in the early Cenozoic, the uplift of the valley was mainly caused by sedimentation. With the continuous downward subduction of the Indian plate, at about 40 Ma, factors such as crustal shortening dominated the uplift of the central valley, and the uplift caused by deposition only accounted for a very small part. In general, the uplift of the Central Valley in the Paleogene was mainly affected by crustal shortening, but a quarter of the surface uplift was caused by the accumulation of sediments.
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Affiliation(s)
- Yuhang Luo
- School of Resource and Environmental
Engineering, Inner Mongolia University of
Technology, Inner Mongolia, Hohhot 010051, People’s Republic of China
| | - Wentian Mi
- School of Resource and Environmental
Engineering, Inner Mongolia University of
Technology, Inner Mongolia, Hohhot 010051, People’s Republic of China
| | - Yuan Gao
- School of Resource and Environmental
Engineering, Inner Mongolia University of
Technology, Inner Mongolia, Hohhot 010051, People’s Republic of China
| | - Luqing Qin
- School of Resource and Environmental
Engineering, Inner Mongolia University of
Technology, Inner Mongolia, Hohhot 010051, People’s Republic of China
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The past is key for the future of our freshwater systems. Nat Commun 2023; 14:3971. [PMID: 37414768 DOI: 10.1038/s41467-023-39501-6] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 07/08/2023] Open
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Jin CS, Xu D, Li M, Hu P, Jiang Z, Liu J, Miao Y, Wu F, Liang W, Zhang Q, Su B, Liu Q, Zhang R, Sun J. Tectonic and orbital forcing of the South Asian monsoon in central Tibet during the late Oligocene. Proc Natl Acad Sci U S A 2023; 120:e2214558120. [PMID: 37011203 PMCID: PMC10104490 DOI: 10.1073/pnas.2214558120] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/28/2022] [Accepted: 12/28/2022] [Indexed: 04/05/2023] Open
Abstract
The modern pattern of the Asian monsoon is thought to have formed around the Oligocene/Miocene transition and is generally attributed to Himalaya-Tibetan Plateau (H-TP) uplift. However, the timing of the ancient Asian monsoon over the TP and its response to astronomical forcing and TP uplift remains poorly known because of the paucity of well-dated high-resolution geological records from the TP interior. Here, we present a precession-scale cyclostratigraphic sedimentary section of 27.32 to 23.24 million years ago (Ma) during the late Oligocene epoch from the Nima Basin to show that the South Asian monsoon (SAM) had already advanced to the central TP (32°N) at least by 27.3 Ma, which is indicated by cyclic arid-humid fluctuations based on environmental magnetism proxies. A shift of lithology and astronomically orbital periods and amplified amplitude of proxy measurements as well as a hydroclimate transition around 25.8 Ma suggest that the SAM intensified at ~25.8 Ma and that the TP reached a paleoelevation threshold for enhancing the coupling between the uplifted plateau and the SAM. Orbital short eccentricity-paced precipitation variability is argued to be mainly driven by orbital eccentricity-modulated low-latitude summer insolation rather than glacial-interglacial Antarctic ice sheet fluctuations. The monsoon data from the TP interior provide key evidence to link the greatly enhanced tropical SAM at 25.8 Ma with TP uplift rather than global climate change and suggest that SAM's northward expansion to the boreal subtropics was dominated by a combination of tectonic and astronomical forcing at multiple timescales in the late Oligocene epoch.
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Affiliation(s)
- Chun-Sheng Jin
- Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
- Innovation Academy for Earth Science, Chinese Academy of Sciences, Beijing 100029, China
| | - Deke Xu
- Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
- Innovation Academy for Earth Science, Chinese Academy of Sciences, Beijing 100029, China
| | - Mingsong Li
- School of Earth and Space Sciences,Peking University, Beijing 100871, China
| | - Pengxiang Hu
- Research School of Earth Sciences, The Australian National University, Canberra, ACT 0200, Australia
| | - Zhaoxia Jiang
- College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
| | - Jianxing Liu
- Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, China
| | - Yunfa Miao
- Key Laboratory of Desert and Desertification, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China
| | - Fuli Wu
- Key Laboratory of Continental Collision and Plateau uplift, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China
| | - Wentian Liang
- State Key Laboratory of Continental Dynamics, Northwest University, Xi’an 710069, China
| | - Qiang Zhang
- Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
| | - Bai Su
- Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
| | - Qingsong Liu
- Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen 518055, China
| | - Ran Zhang
- Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
| | - Jimin Sun
- Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
- Innovation Academy for Earth Science, Chinese Academy of Sciences, Beijing 100029, China
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Ao H, Liebrand D, Dekkers MJ, Zhang P, Song Y, Liu Q, Jonell TN, Sun Q, Li X, Li X, Qiang X, An Z. Eccentricity-paced monsoon variability on the northeastern Tibetan Plateau in the Late Oligocene high CO 2 world. SCIENCE ADVANCES 2021; 7:eabk2318. [PMID: 34910508 PMCID: PMC8673770 DOI: 10.1126/sciadv.abk2318] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 06/30/2021] [Accepted: 10/28/2021] [Indexed: 06/14/2023]
Abstract
Constraining monsoon variability and dynamics in the warm unipolar icehouse world of the Late Oligocene can provide important clues to future climate responses to global warming. Here, we present a ~4-thousand year (ka) resolution rubidium-to-strontium ratio and magnetic susceptibility records between 28.1 and 24.1 million years ago from a distal alluvial sedimentary sequence in the Lanzhou Basin (China) on the northeastern Tibetan Plateau margin. These Asian monsoon precipitation records exhibit prominent short (~110-ka) and long (405-ka) eccentricity cycles throughout the Late Oligocene, with a weak expression of obliquity (41-ka) and precession (19-ka and 23-ka) cycles. We conclude that a combination of eccentricity-modulated low-latitude summer insolation and glacial-interglacial Antarctic Ice Sheet fluctuations drove the eccentricity-paced precipitation variability on the northeastern Tibetan Plateau in the Late Oligocene high CO2 world by governing regional temperatures, water vapor loading in the western Pacific and Indian Oceans, and the Asian monsoon intensity and displacement.
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Affiliation(s)
- Hong Ao
- State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an, China
- Open Studio for Oceanic-Continental Climate and Environment Changes, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao, China
| | - Diederik Liebrand
- National Oceanography Centre, European Way, SO14 3ZH Southampton, UK
- PalaeoClimate.Science, 27 Granby Grove, SO17 3RY, Southampton, UK
| | - Mark J. Dekkers
- Paleomagnetic Laboratory Fort Hoofddijk, Department of Earth Sciences, Faculty of Geosciences, Utrecht University, Utrecht, The Netherlands
| | - Peng Zhang
- State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an, China
- Open Studio for Oceanic-Continental Climate and Environment Changes, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao, China
| | - Yougui Song
- State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an, China
- Open Studio for Oceanic-Continental Climate and Environment Changes, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao, China
| | - Qingsong Liu
- Centre for Marine Magnetism (CM2), Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen, China
| | - Tara N. Jonell
- School of Geographical and Earth Sciences, University of Glasgow, Glasgow, UK
| | - Qiang Sun
- College of Geology and Environment, Xi’an University of Science and Technology, Xi’an, China
| | - Xinzhou Li
- State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an, China
- Open Studio for Oceanic-Continental Climate and Environment Changes, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao, China
| | - Xinxia Li
- School of Earth Sciences, China University of Geosciences (Wuhan), Wuhan, China
| | - Xiaoke Qiang
- State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an, China
| | - Zhisheng An
- State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an, China
- Open Studio for Oceanic-Continental Climate and Environment Changes, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao, China
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Paleogeography control of Indian monsoon intensification and expansion at 41 Ma. Sci Bull (Beijing) 2021; 66:2320-2328. [PMID: 36654458 DOI: 10.1016/j.scib.2021.07.023] [Citation(s) in RCA: 3] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/03/2021] [Revised: 06/20/2021] [Accepted: 06/22/2021] [Indexed: 02/03/2023]
Abstract
As a crucial part of the Asian monsoon stretching from tropical India to temperate East Asia, the Indian monsoon (IM) contributes predominant precipitation over Asian continent. However, our understanding of IM's onset, development and the underlying driving mechanisms is limited. Increasing evidence indicates that the IM began in the Eocene or even the Paleocene and was unexceptionally linked to the early rise of the Tibetan Plateau (TP). These were challenged by the heterogeneous and diachronous uplift of the TP and all the reported records were confined to tropical zone under tropical monsoon driven by the Intertropical Convergence Zone (ITCZ) that is irrelevant to the TP. Therefore, reliable paleoclimatic records from the extra-tropical IM region is crucial to reveal how the tropical IM expanded to subtropical and temperate zones and what driving factors might be related to it. Here we present robust Eocene paleoenvironmental records from central Yunnan (~26°N) in subtropical East Asia. The multiproxy results of two sites demonstrate a consistent sudden switch from a dry environment in the early Eocene to a seasonally wet one at 41 Ma, suggesting a jump of the tropical IM to the southern subtropical zone at 41 Ma. The full collision of India with Asia, and the resulting changes in paleogeography at 41 Ma (closure of the Neotethys sea, retreat of the Paratethys seas, fast northward movement of the southern margin of the TP and rise of the central TP), aided by synchronous Antarctic cooling, might have worked together to drive the IM enhancement and northward expansion.
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Thomson JR, Holden PB, Anand P, Edwards NR, Porchier CA, Harris NBW. Tectonic and climatic drivers of Asian monsoon evolution. Nat Commun 2021; 12:4022. [PMID: 34188033 PMCID: PMC8242090 DOI: 10.1038/s41467-021-24244-z] [Citation(s) in RCA: 11] [Impact Index Per Article: 3.7] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/26/2020] [Accepted: 05/26/2021] [Indexed: 11/23/2022] Open
Abstract
Asian Monsoon rainfall supports the livelihood of billions of people, yet the relative importance of different drivers remains an issue of great debate. Here, we present 30 million-year model-based reconstructions of Indian summer monsoon and South East Asian monsoon rainfall at millennial resolution. We show that precession is the dominant direct driver of orbital variability, although variability on obliquity timescales is driven through the ice sheets. Orographic development dominated the evolution of the South East Asian monsoon, but Indian summer monsoon evolution involved a complex mix of contributions from orography (39%), precession (25%), atmospheric CO2 (21%), ice-sheet state (5%) and ocean gateways (5%). Prior to 15 Ma, the Indian summer monsoon was broadly stable, albeit with substantial orbital variability. From 15 Ma to 5 Ma, strengthening was driven by a combination of orography and glaciation, while closure of the Panama gateway provided the prerequisite for the modern Indian summer monsoon state through a strengthened Atlantic meridional overturning circulation.
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Affiliation(s)
| | - Philip B Holden
- School of Environment, Earth & Ecosystem Sciences, The Open University, Milton Keynes, UK.
| | - Pallavi Anand
- School of Environment, Earth & Ecosystem Sciences, The Open University, Milton Keynes, UK
| | - Neil R Edwards
- School of Environment, Earth & Ecosystem Sciences, The Open University, Milton Keynes, UK
- Cambridge Centre for Energy, Environment and Natural Resource Governance, University of Cambridge, Cambridge, UK
| | - Cécile A Porchier
- School of Environment, Earth & Ecosystem Sciences, The Open University, Milton Keynes, UK
- Department of Geography, University College London, London, UK
| | - Nigel B W Harris
- School of Environment, Earth & Ecosystem Sciences, The Open University, Milton Keynes, UK
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