Numerical modeling of the effects of beach slope on water-table fluctuation in the unconfined aquifer of Donghai Island, China

Numerical modeling of the effects of beach slope on water-table fluctuation in the unconfined aquifer of Donghai Island, China
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东海岛无承压含水层滩坡对地下水位波动影响的数值模拟

DOI:
10.1007/s10040-013-1045-5
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发表时间:
2014-03
影响因子:
2.8
通讯作者:
Ming Li
Ming Li
中科院分区:
地球科学3区
文献类型:
--
作者:
Pengpeng Zhou;Guomin Li;Yaodong Lu;Ming Li

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海滩坡度是影响滨海潜水层水位波动的重要因素。然而,关于海滩坡度对地下水位波动影响的研究还很有限,特别是对于缓坡地。为了解海滩坡度对海滩地下水动态的影响,建立了数值模型,并利用东海岛的实测数据进行了校正,模拟了观测到的地下水动态。进行敏感性分析,以评估地下水位波动的敏感性参数和模型的概念化。分析表明,地下水位波动对导水率和给水度特别敏感,模型区域的水平长度会影响地下水位波动的幅度。此外,还发现当滩坡角在1.5 ° ~ 45 °范围内变化时,振幅的变化更为明显,特别是在1.5 ° ~ 5 °范围内。了解海滩坡度对潮汐引起的地下水位动态的影响,可以帮助建模者在海滩地下水流模型中更好地处理坡度。[出版物摘要]
Beach slope is an important factor influencing the tide-induced water-table fluctuation in coastal unconfined aquifers. However, research about the effect of beach slope on water-table fluctuation is limited, especially for gentle slopes. To understand the effect of beach slope on beach groundwater dynamics, a numerical model, calibrated with field monitoring data from Donghai Island (China), was built to simulate the observed water-table fluctuation. Sensitivity analysis was performed to assess the sensitivity of water-table fluctuation to the parameters and conceptualization of the model. The analysis indicated that the water-table fluctuation was especially sensitive to the hydraulic conductivity and specific yield, and the horizontal length of the model domain could affect the amplitude of the water-table fluctuation. Moreover, it is found that the variation of the amplitude is more evident when the beach-slope angle changes in the range from 1.5 to 45, especially in the range from 1.5 to 5. Understanding the effect of beach slope on tide-induced water-table dynamics could help modelers deal with the slope better in their beach groundwater flow models.[PUBLICATION ABSTRACT]
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