利用探地雷达监测蒙古地下水

Q. Lu, Motoyuki Sato
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引用次数: 6

摘要

在蒙古乌兰巴托市的一个水源进行了控制采水,以评估探地雷达探测和监测地下动态地下水运动的有效性。乌兰巴托市区的地下水位在2米至10米之间。这种相对较浅的深度使其成为GPR探测的合适目标。2001年在乌兰巴托用100兆赫天线进行了实地试验。我们测量了抽水井周围的地下水位,然后监测了水泵停止后地下水位的变化。地下水位约5米。当生产井水位变化65cm时,我们可以检测到地下水变化约50cm。通过对天线位置的精确定位,可以获得高相干的雷达廓线,可以清晰地看到地下水的运移。为了确定地下水表面的反射,在同一地点也使用了CMP。发现CMP和速度分析能很好地反映土壤中地下水饱和度的深度变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Groundwater monitoring by GPR in Mongolia
A controlled water production was performed at a water source of Ulaanbaatar city, Mongolia to evaluate the effectiveness of ground penetrating radar for detecting and monitoring dynamic groundwater movements in the subsurface. The groundwater level in Ulaanbaatar city area is between 2m-10m. This relatively shallow depth makes it a suitable target for detection by GPR. Field experiments in Ulaanbaatar were carried out in 2001 with 100 MHz antennae. We measured the groundwater level around a pumping well, then we monitored the change of the level after the pump was stopped. The groundwater level was about 5m. We could detect the groundwater change about 50cm, when the water level in the production well changed by 65cm. If we acquire the data by locating the antenna positions very accurately, we can obtain radar profiles with very high coherency, and we could see the groundwater migration clearly. The CMP was also used in the same site in order to determine the reflection from the groundwater surface. It was found that CMP and velocity analysis give a good information about the depth variation of the groundwater saturation in soil.
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