With the rapid development of major infrastructure and urban construction in the Loess Plateau region, the problem of loess subsidence has become an important geological engineering challenge that restricts engineering safety and sustainable development (Figure 1). The compaction method is widely used in loess foundation treatment engineering due to its economy, efficiency, and convenient construction. However, the mechanism by which compaction suppresses loess collapsibility from the perspectives of microstructure and seepage behavior still needs to be explored.
Recently, a geological research team from Northwestern University conducted a systematic geochemical study on the 1.4 billion year old weathering crust in Jixian, North China Craton. Using a divalent iron oxidation kinetic oxygen mass balance model, they estimated that the atmospheric oxygen content at that time could reach 7% of the current oxygen level, providing new evidence for the evolution of atmospheric oxygen in the Mesoproterozoic. The related achievements were published in the international academic journal Science Bulletin under the title "Oxygen rise recorded in a 1.4 Ga paleoweather crust from the North China Craton".
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Reporter:李文帅
Time:2023年4月2日(星期二)15:00
Place:钟健报告厅(系楼218)
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Reporter:常燎 研究员(北京大学地球与空间科学学院)
Time:2024年3月26日(星期二)10:00
Place:钟健报告厅(系楼218)