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Climate change and the future of freshwater resources of the island: a case study on the Rishiri Island, Japan

机译:气候变化与该岛淡水资源的未来:以日本利ish岛为例

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A comparison of the d-excess values of pre-cipitation and of spring water, streams, groundwater wells and submarine groundwater discharge indicated that the precipitation that occurred during winter season was an important source of groundwater recharge. Due to the steep slope of the island, most of the short duration and high intensity precipitation is lost through direct surface runoff. The comparison indicated that snowmelt is an important resource of groundwater recharge on Rishiri Island. Future climate change will continue to diminish the snowpack, and therefore, reduce groundwater recharge. It may cause the decline of the groundwater level in the coastal area and possibly shift the saline-freshwater boundary on the island. Chloride data indicated that saltwater intrusion is begin-ning to occur on the western flank of the island. A Piper diagram shows that the water samples are characterized by the dominance of the Ca-HC0_3 and Na-Cl type. Their chemistry probably results from sea salt spray and the dissolution of minerals. These results support the need for the effective management of groundwater resources.
机译:对降水和水,溪流,地下水井和海底地下水排放的d-过量值的比较表明,冬季发生的降水是地下水补给的重要来源。由于该岛陡峭的坡度,大部分短时和高强度的降水通过直接地表径流损失掉了。比较表明,融雪是利iri岛上重要的地下水补给资源。未来的气候变化将继续减少积雪,从而减少地下水补给。这可能会导致沿海地区地下水位下降,并可能使岛上的盐水与淡水边界发生偏移。氯化物数据表明,海水入侵开始出现在该岛的西部。派珀图显示水样品的特征是Ca-HC0_3和Na-Cl型占主导地位。它们的化学作用可能是由海盐喷雾和矿物质溶解引起的。这些结果支持有效管理地下水资源的需求。

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