Seawater intrusion (SWI) is a natural phenomenon that negatively impacts the potability of
groundwater and is expected to worsen with rising sea levels due to climate change …

Countermeasures against seawater intrusion (SWI) are critical to prevent coastal
groundwater resources from deterioration. Subsurface dams have been recognized as one …

探究水平双裂隙含水层中的海水入侵机制, 对理解裂隙含水层中的海水入侵机制具有重要意义.
本文构建了大型室内砂槽模型, 并通过离散裂隙基质数值模型分析了不同分布形式的水平双裂隙 …

Precipitation of Fe (hydr) oxides (such as Fe (OH) 3) in subterranean estuaries can form a
low-permeable zone, referred to as the “iron curtain”, of which the genesis, distribution, and …

Seawater salt is constantly supplied from the marine environment to coastal underground
brine deposits, meaning that brine has the potential for continuous extraction. There is …

Freshwater injection is a practical and efficient solution to mitigate seawater intrusion in
coastal aquifers, but its thermal impacts on groundwater flow and salt transport are still …

Coastal groundwater dynamics and solute transport were influenced by multiple factors
including aquitards, tides, evaporation, and slope breaks in coastal aquifers. However …

Subsurface dams are now widely used to mitigate seawater intrusion in coastal aquifers.
Previous studies have mostly focused on the optimal design of subsurface dams under …

Evaporated salt accumulated on the surface of tidal flats is an important source of salt for
supplying coastal phreatic brine resources. A clear understanding of the flux and process of …

Unconfined coastal aquifers are a main pathway for land‐sourced solutes to enter the
oceans. The migration of these solutes in aquifers is highly affected by the groundwater flow …