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Tide-induced Air Pressure Fluctuation in Coastal Unsaturated Zones

机译:沿海不饱和区潮汐引起的气压波动

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Air pressure in coastal unsaturated aquifers fluctuates with sea tides, as does the groundwater level. Tide-induced air pressure fluctuations in coastal subsurface systems, however, are not well addressed in literature. Significant diurnal air pressure fluctuations are observed below the asphalt pavement in a coastal reclamation area of Hong Kong. A two-dimensional cross-sectional model is built to describe the air-water two-phase flow in the unsaturated zone of the area. TOUGH2, a general-purpose numerical simulation program for multi-dimensional fluid and heat flows of multiphase, multicomponent fluid mixtures in porous and fracture media, is used to obtain the numerical solutions. The numerical simulation reveals that the significant air pressure fluctuation results from a combination of various factors such as asphalt pavement of extremely low permeability, soil structures of the reclamation area, and rainfall intensity during spring tides. Numerical simulation also reveals that the air pressure is approximately proportional to the tidal rate. A great amplitude of the sea level fluctuation will not necessarily lead to high air pressure, if the sea level changes slowly. Coastal unsaturated zones inhale and exhale as the tidal level falls and rises. The paper goes on to discuss various engineering and environmental implications of air pressure fluctuations in coastal aquifers.
机译:沿海非饱和含水层中的气压随着海潮而波动,地下水位也一样。但是,在沿海地下系统中,潮汐引起的气压波动并未在文献中得到很好的解决。在香港沿海填海区的沥青路面下,观察到明显的每日气压波动。建立了一个二维截面模型来描述该地区非饱和区内的空气-水两相流。 TOUGH2是一种通用数值模拟程序,用于求解多孔介质和压裂介质中多相,多组分流体混合物的多维流体和热流,从而获得了数值解。数值模拟表明,明显的气压波动是由多种因素共同导致的,例如极低渗透性的沥青路面,开垦区的土壤结构以及春季潮汐期间的降雨强度。数值模拟还表明,气压大约与潮汐速度成正比。如果海平面变化缓慢,则海平面波动幅度较大并不一定会导致气压升高。随着潮汐水位下降和上升,沿海不饱和区会吸气和呼气。本文继续讨论沿海含水层中气压波动的各种工程和环境影响。

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