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本文介绍了利用同位素单井技术,测定井中各含水层的地下水流速、流向,为枣庄均衡试验场边界的划分及确定边界的性质提供了依据。
This paper introduces the use of isotope single well technology to determine the velocity and direction of groundwater in each aquifer in the well. It provides the basis for the boundary division of Zaozhuang equilibrium test site and the determination of the boundary properties.