摘要
本文根据太平洋中部大洋水物质成分和环境参数的大量实测资料,揭示它们在水深6000m以上的分布态势,概括了大洋水物质模型的两个显著相关的特性,提出重力和溶液质点热运动自扩散力的合力是主控模型形成的主导作用力,并指出其在研究洋底成矿机制和地下水形成理论上的意义。
Based on the large number of data concerning the chemical components and environmental parameters of ocean water in the central part of pacific Ocean, the paper reveals the distribution of chemlcal components within the depth of 6,000 m and summarizes two remarkable correlative properties of ocean-water material model. In addition, the paper puts forward the material model as mainly dominated by the joint force of gravity and self-diffusion brought about by the thermal movement of solution particles and expounds the theoretical significance of the oceanwater material model in studying ocean-floor minerogenic mechanism and formation of groundwater.
出处
《水文地质工程地质》
CAS
CSCD
北大核心
1991年第6期33-36,共4页
Hydrogeology & Engineering Geology
