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氧气暴露对海洋沉积物侧向输运过程中木质素保存的影响:分子动力学模拟的见解。

Influence of Oxygen Exposure on Lignin Preservation during Sediment Lateral Transport in the Ocean: Insights from Molecular Dynamics Simulations.

机构信息

Frontiers Science Center for Deep Ocean Multispheres and Earth System, and Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education/Institute for Advanced Ocean Studies, Ocean University of China, Qingdao 266100, China.

Laboratory for Marine Geology, Qingdao Marine Science and Technology Center, Qingdao 266237, China.

出版信息

Environ Sci Technol. 2024 Oct 22;58(42):18756-18764. doi: 10.1021/acs.est.4c06185. Epub 2024 Oct 9.

Abstract

Understanding the fate of terrestrial organic carbon (terrOC) preservation in the marine environments is critical for deciphering the biogeochemical processes associated with the global carbon cycle and the Earth's climate change. The mechanisms controlling terrOC preservation are not completely understood, while lateral oxygen exposure time (OET) is considered as a critical controlling factor. Here, we first utilized molecular dynamics simulations to investigate the structural properties of lignin under anoxic, suboxic, and oxic conditions for understanding the mechanisms of terrOC preservation during sediment lateral transport in the ocean. Our finding suggested that oxygen exposure was indispensable for terrOC degradation through influencing the structural stability and reactivity of lignin. Our simulated results showed that in suboxic environments, prolonged OET may enhance terrOC preservation. Our organic geochemical results suggested that terrOC preferably preserved in coarse silts (20-63 μm) than fine silts (<20 μm) in suboxic environments, largely due to hydrodynamics-driven prolonged OET in coarse sediments, which may efficiently reduce CO emissions. Overall, our study sheds new light on the mechanisms of lateral OETs on terrOC preservation in suboxic conditions and, from a unique molecular structural perspective, provides insights into the impact of prolonged OETs on terrOC oxidative degradation in the marine environment.

摘要

理解陆地有机碳(terrOC)在海洋环境中保存的命运对于揭示与全球碳循环和地球气候变化相关的生物地球化学过程至关重要。控制 terrOC 保存的机制尚未完全理解,而侧向氧气暴露时间(OET)被认为是一个关键的控制因素。在这里,我们首先利用分子动力学模拟来研究木质素在缺氧、亚缺氧和有氧条件下的结构特性,以了解海洋沉积物侧向输运过程中 terrOC 保存的机制。我们的发现表明,氧气暴露通过影响木质素的结构稳定性和反应性,对于 terrOC 的降解是必不可少的。我们的模拟结果表明,在亚缺氧环境中,延长 OET 可能会增强 terrOC 的保存。我们的有机地球化学结果表明,在亚缺氧环境中,terrOC 更倾向于保存在粗砂(20-63 μm)中,而不是细砂(<20 μm)中,这主要是由于粗沉积物中由于水动力作用导致的 OET 延长,从而有效地减少了 CO 的排放。总的来说,我们的研究从侧向 OET 对亚缺氧条件下 terrOC 保存的机制提供了新的认识,并从独特的分子结构角度提供了对延长 OET 对海洋环境中 terrOC 氧化降解影响的见解。

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