Division of Geoenvironmental Science, Graduate School of Life and Environmental Sciences, University of Tsukuba, Advance Research Building-A, Tsukuba City, Ibaraki Prefecture, 305-8572, Japan.
Environ Geochem Health. 2013 Apr;35(2):239-50. doi: 10.1007/s10653-012-9479-6. Epub 2012 Sep 11.
Considering the current poor understanding of the seawater-freshwater (SW-FW) interaction pattern at dynamic hydro-geological boundary of coastal aquifers, this work strives to study tidal effect on groundwater quality using chemical tracers combined with environmental isotopes. In situ measurement data of electrical conductivity and groundwater level along with laboratory measurement data of hydro-chemical species were compared with tidal level data measured by Hydrographic and Oceanographic Department, Saijo City, Japan for time series analysis. Result shows that diurnal tides have significant effect on groundwater level as well as its chemical characteristics; however, the magnitude of effect is different in case of different aquifers. Various scatter diagrams were plotted in order to infer mechanisms responsible for water quality change with tidal phase, and results show that cations exchange, selective movement and local SW-FW mixing were likely to be the main processes responsible for water quality changes. It was also found that geological structure of the aquifers is the most important factor affecting the intensity of tidal effect on water quality.
考虑到当前对沿海含水层动态水文地质边界海水-淡水(SW-FW)相互作用模式的理解不足,本研究旨在使用化学示踪剂结合环境同位素研究潮汐对地下水质量的影响。对电导率和地下水位的现场测量数据以及实验室测量的水化学物质数据与日本爱媛县水上厅测量的潮汐数据进行了时间序列分析。结果表明,昼夜潮汐对地下水位及其化学特性有显著影响;然而,不同含水层的影响程度不同。绘制了各种散点图,以推断潮汐阶段与水质变化之间的机制,结果表明,阳离子交换、选择性迁移和局部 SW-FW 混合可能是导致水质变化的主要过程。还发现,含水层的地质结构是影响潮汐对水质影响强度的最重要因素。