Читать книгу Groundwater Geochemistry - Группа авторов - Страница 80

Salinity has a profound effect on land subsidence, especially in clay‐dominated coastal soils. Higher salinity in water reduces the interconnectivity of the pores by converting clay fabrics into parallel alignments that induce the fast dissipation of pore water. Hence, consolidation is more pronounced (Sarah et al. 2018).