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Updated: Jul 13, 2026

The Benthic Exchange of O2, N2 and Dissolved Nutrients Using Small Core Incubations
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在一个大河口的氧化度和排放的卫星估计

Wenjie Fan1, Zhihao Xu1,2, Yuliang Liu1

  • 1Guangdong Basic Research Center of Excellence for Ecological Security and Green Development, Guangdong Provincial Key Laboratory of Water Quality Improvement and Ecological Restoration for Watersheds, School of Ecology, Environment and Resources, Guangdong University of Technology, Guangzhou 510006, China.

Environmental science & technology
|February 5, 2025
PubMed
概括

河口是氧化 (N2O) 排放的重要来源. 这项研究使用卫星数据和机器学习来绘制珍珠河口N2O动态图,揭示了关键的环境驱动因素.

关键词:
河口排放的排放量温室气体的温室气体是什么可以解释的机器学习.卫星图像 卫星图像 卫星图像时间空间的动态.

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The deep ocean and its underlying sediments represent vast, largely unexplored microbial habitats that extend far beyond the sunlit photic zone. The photic (euphotic) zone typically spans the upper ~100–200 meters of pelagic waters in the open ocean, but its depth varies geographically and seasonally, where sufficient light supports photosynthetic life. Below this lies the deep sea, spanning roughly 1000–6000 meters (bathypelagic to abyssal zones), with deeper hadal trenches extending beyond...