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Distribution patterns of salinity and ~(222)Rn in Yatsushiro Inland Sea, Kyushu, Japan

机译:日本九州八代内陆盐度和〜(222)Rn的分布模式

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摘要

Submarine Groundwater Discharge (SGD), as a way through which solutes and nutrients travel from terrestrial areas towards coastal areas, is part of the hydrological cycle. Various methods are used to locate SGD at different scales. Among them, ~(222)Rn has been developed with the viewpoint of accurate local estimations of SGD points indirectly. This research aims to identify SGD areas in the Yatsushiro Sea, southwest Japan, using the ~(222)Rn method, while considering rivers with high ~(222)Rn concentration in the study area. The area is an inland sea with high tidal fluctuations and there is a large contribution between the sea and groundwater, which are greatly affected by rivers. A multi-detector ~(222)Rn survey has been carried out simultaneously with sea water electrical conductivity (EC) and temperature. In addition, several river grab samples were analysed for ~(222)Rn concentration. Considering the sea water radon distribution and river characteristics, several points were selected for future SGD volume estimations.
机译:海底地下水排放(SGD)是溶质和养分从陆地向沿海地区传播的一种方式,是水文循环的一部分。使用各种方法来定位不同规模的SGD。其中,从间接精确地估计SGD点的角度出发,已经开发了〜(222)Rn。这项研究旨在使用〜(222)Rn方法确定日本西南八代海的SGD区域,同时考虑研究区域中〜(222)Rn浓度高的河流。该地区是潮汐波动大的内陆海域,在受河流影响很大的海水与地下水之间有很大的贡献。同时已对海水电导率(EC)和温度进行了多探测器〜(222)Rn测量。另外,分析了几个河流抢夺样品的〜(222)Rn浓度。考虑到海水中ra的分布和河流特征,为将来的SGD量估算选择了几个点。

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