The extreme pressure and temperature conditions of the deep Earth,reaching up to∼350 gigapascals(GPa)and 6000 K,pose major challenges for in-situ detection and the investigation of physical and chemical processes[1]....The extreme pressure and temperature conditions of the deep Earth,reaching up to∼350 gigapascals(GPa)and 6000 K,pose major challenges for in-situ detection and the investigation of physical and chemical processes[1].Although numerous theoretical simulations and experiments have been conducted under extreme deep-Earth conditions,a centralized platform with practical tools for predicting the reactivity of substances on Earth and beyond is still lacking.Such tools are crucial for advancing our understanding of Earth’s structure,composition,energy exchange,and long-term evolution.展开更多
基金supported by the National Science and Technology Major Project(2025ZD1010301)the Chinese Academy of Geological Sciences Basal Research Fund(JKYDM2025110)+2 种基金the National Natural Science Foundation of China(42372049,42192502,42302037,92351302,and 62271016)the China Postdoctoral Science Foundation(2023T160007 and 2023M740044)the Regional Special Program(KCX2024003).
文摘The extreme pressure and temperature conditions of the deep Earth,reaching up to∼350 gigapascals(GPa)and 6000 K,pose major challenges for in-situ detection and the investigation of physical and chemical processes[1].Although numerous theoretical simulations and experiments have been conducted under extreme deep-Earth conditions,a centralized platform with practical tools for predicting the reactivity of substances on Earth and beyond is still lacking.Such tools are crucial for advancing our understanding of Earth’s structure,composition,energy exchange,and long-term evolution.
