2、 咸水入侵 ( saltwater intrusion ) : 因地下水位下降或咸水侵入地下淡水层, 使地下淡水咸化。 包括地下淡水层与咸水层串层和海水入侵。
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The sediment environmental transformation is the setting factor of saline water encroachment, and the modern environmental change is the spring factor.
沉积环境变化是咸水入侵产生的背景因素,现代环境变化是咸水入侵产生的主导及驱动因素。
参考来源 - 莱州湾南岸滨海平原沉积环境变化与咸水入侵关系研究The influence degree of the saltwater intrusion upon water resources carrying capacity is obtained through comparative analysis of the two evaluation results.
比较两种情况下的水资源承载能力评价结果,得到咸水入侵对昌邑市水资源承载力的影响程度。
参考来源 - 咸水入侵胁迫下的昌邑市水资源承载能力研究The carrying capacity of water resources of Changyi city under the stress of salt-water intrusion.
咸水入侵胁迫下昌邑市的水资源承载力分析。
参考来源 - 咸水入侵胁迫下的昌邑市水资源承载能力研究Seawater and saltwater intrusion become a serious geological disaster in coastal areas for people exploit groundwater excessively. And in the same time, the proper remedial measures have been taken to protect the groundwater.
由于过量开采地下水,海咸水入侵已经成为滨海地区的一种严重地质灾害现象,很多地区也采取了相应的治理措施。
参考来源 - 滨海地下咸水分布动态特征与治理可行性研究During 1988-1995, which is the time of seawater intrusion developed greatly, land use changes most distinct.
1988~1995年,研究区土地资源、水资源大规模开发时期,也是咸水入侵剧烈发展阶段。
参考来源 - 莱州湾南岸平原土地利用/覆被变化及其驱动机理研究·2,447,543篇论文数据,部分数据来源于NoteExpress
咸水入侵从微观层次上影响土壤质量,从而影响土地利用的变化。
The saltwater intrusion affects the soil quality from the microcosmic aspect, and then affects the LUCC.
本文建立了内陆单斜构造内咸水入侵淡水含水层的三维可混溶溶质运移模型。
This paper presents a three-dimensional miscible solute transport model for salt water intrusion into fresh water aquifers, in an inland monoclinal structure.
古河道构成了咸水入侵的主要通道,其沉积特征差异对咸水入侵方式及速度有较大的影响。
The paleochanles are the main channels of saline water encroachment, the diversity of whose sediment has big influence on the fashion and velocity of saline water encroachment.
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