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A Preliminary Appraisal of the Effect of Pumping on Seawater Intrusion and Upconing in a Small Tropical Island Using 2D Resistivity Technique

机译:利用二维电阻率技术初步评价抽水对热带小岛海水入侵和上冲作用的影响

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摘要

The existing knowledge regarding seawater intrusion and particularly upconing, in which both problems are linked to pumping, entirely relies on theoretical assumptions. Therefore, in this paper, an attempt is made to capture the effects of pumping on seawater intrusion and upconing using 2D resistivity measurement. For this work, two positions, one perpendicular and the other parallel to the sea, were chosen as profile line for resistivity measurement in the coastal area near the pumping wells of Kapas Island, Malaysia. Subsequently, water was pumped out of two pumping wells simultaneously for about five straight hours. Then, immediately after the pumping stopped, resistivity measurements were taken along the two stationed profile lines. This was followed by additional measurements after four and eight hours. The results showed an upconing with low resistivity of about 1–10 Ωm just beneath the pumping well along the first profile line that was taken just after the pumping stopped. The resistivity image also shows an intrusion of saline water (water enriched with diluted salt) from the sea coming towards the pumping well with resistivity values ranging between 10 and 25 Ωm. The subsequent measurements show the recovery of freshwater in the aquifer and how the saline water is gradually diluted or pushed out of the aquifer. Similarly the line parallel to the sea (L2) reveals almost the same result as the first line. However, in the second and third measurements, there were some significant variations which were contrary to the expectation that the freshwater may completely flush out the saline water from the aquifer. These two time series lines show that as the areas with the lowest resistivity (1 Ωm) shrink with time, the low resistivity (10 Ωm) tends to take over almost the entire area implying that the freshwater-saltwater equilibrium zone has already been altered. These results have clearly enhanced our current understanding and add more scientific weight to the theoretical assumptions on the effects of pumping on seawater intrusion and upconing.
机译:现有的有关海水入侵和特别是上行清理的知识,其中两个问题都与抽水有关,完全依赖于理论假设。因此,在本文中,我们尝试使用2D电阻率测量方法来捕获泵送对海水入侵和上冲的影响。在这项工作中,选择了两个位置,一个垂直于海,另一个平行于海,作为马来西亚卡帕斯岛抽水井附近沿海地区电阻率测量的轮廓线。随后,将水同时从两个抽水井中抽出约连续五个小时。然后,在抽水停止后,立即沿两条固定轮廓线进行了电阻率测量。然后在四小时和八小时后进行其他测量。结果表明,沿抽水刚停后沿第一条剖面线在抽水井正下方有一个低电阻率的上冲,约为1–10Ωm。电阻率图像还显示盐水从海水侵入抽水井,其盐水电阻率范围在10至25Ωm之间。随后的测量显示了含水层中淡水的回收以及盐水如何被逐渐稀释或从含水层中挤出。同样,平行于海(L2)的线也显示出与第一条线几乎相同的结果。但是,在第二次和第三次测量中,存在一些明显的变化,这与预期的淡水可能会从含水层中完全冲洗出盐水相反。这两条时间序列线表明,随着电阻率最低的区域(1Ωm)随时间的推移而收缩,低电阻率(10Ωm)趋于占据几乎整个区域,这意味着淡水-盐水平衡区已经改变。这些结果清楚地增强了我们目前的理解,并为有关抽水对海水入侵和向上冲的影响的理论假设增加了更多的科学依据。

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