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长江大学地球科学学院,湖北武汉,430100;
摘要:浊流是陆源碎屑向深海/深湖输送的主要重力流类型,与油气储层、海底灾害及全球碳循环密切相关。由于浊流发生的瞬时性与深海观测的高成本,数值模拟已成为揭示其动力学机制的关键手段。本文系统回顾了浊流沉积数值模拟的数学物理基础,包括雷诺平均Navier-Stokes方程、浓度输运方程及k-ε湍流模型的封闭体系,并阐述了侵蚀与沉积通量的经验参数化方法。在此基础上,总结了该方法在油气勘探(鄂尔多斯页岩油)、环境科学(西沙海槽微塑料)及深海地貌演化(南海麻坑-水道系统)三大领域的应用进展。
关键词:浊流;数值模拟;沉积过程;雷诺平均NavierStokes方程
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