marine sediment

基本解释

Microscopic organisms settle to the seafloor and accumulate in marine mud, thus marine sediment was formed.
微生物生存于海底，并聚积在海底的淤泥之中，这样便形成了海洋沉积物。
Significant progress in the establishment of a unified marine sediment dynamics has been made through the joint effort by physical oceanographers, coastal engineers and marine geologists.
海洋沉积动力学正在打破传统，走向海洋工程学、物理海洋学和地质学的联合，共同建立一门综合性的、统一的沉积动力学。
Besides temperature and pressure, the controlling factors for gas hydrate stability also include pore water composition, gas concentration in the fluid and marine sediment types in the seafloor.
海洋天然气水合物的生成除了受温度和压力的影响外，还要受到孔隙水的化学组成、流体中气体的浓度及沉积物类型的影响。

海洋沉积物
Microbial diversity in marine sediment is an important component of marine biodiversity,it plays an important role in geochemical cycle.
海洋沉积物微生物多样性是海洋生物多样性的重要组成部分,在海洋生物地球化学循环中发挥着重要作用。
地球科学
海洋沉积物
Actual marine sediment cores will be used in similar experiments to study the relationship between gas hydrate saturation and acoustic parameters. Parameters of the models determined by experiments will be useful in practical application.
在掌握实验技术的基础上,使用实际的海洋沉积物岩心进行同样的实验,研究水合物饱和度与声学参数的响应关系,确定各理论方程中参数的取值,将得到实际的应用。
海底沉积物
Factors that can influent the distribution and transportation of suspended matter in the surface layer are composed of topography, marine sediment properties, runoffs, thermocline, wind, waves, circulations and so on.
影响表层悬浮体分布和输运的因素包括地形、海底沉积物类型、径流、跃层、风浪以及环流等等,海水中的悬浮体在这些因素的综合作用下呈现出上述的空间分布特征和季节变化规律。
海洋底泥
海相沉积
海洋沉积
海洋沈积物
海相沉积物