INTERPRETASI TRANSMISIVITAS UNTUK ANALISA POTENSI AIR BAWAH TANAH BERDASARKAN DRAWDOWN AIR SUMUR CINCIN MENGGUNAKAN METODE PUMPING TEST DI KECAMATAN MARPOYAN DAMAI KOTA PEKANBARU

Rigia Givanny Pritamara, Juandi M, Usman Malik
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Abstract

The most consumption water is groundwater taken through excavated wells or ring wells. An aquifer test can be applied in  pump test in order to find transmissivity of drawdown ring wells.The tested ring wells were located at 25 different locations in the Marpoyan Damai District. In the pumping test on the ring wells data was obtained namely drawdown test data s, times t, rate of discharge Q, and then create a graph of s/Q vs Q. The straight line that cut the s/Q axis the A value with the C gradient and the determinant coefficient d2. The values obtained were then inserted into the transmisivity formula of the Cooper-Jacob method. The A values for t = 3 minutes and t = 7 minutes were selected because their results in C values are close to each other. The C values of t = 3 minutes and t = 7 minutes are 0.1671 and 0.1672 respectively. Transmissivity value obtained is 134.5 m2/day. The value shows a potentially useful groundwater aquifer for the Marpoyan Damai district because the transmissivity value exceeded 50 m2 / day.
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根据北干巴鲁镇和平马波扬地区的抽水测试方法,对地下潜在水的传输解读
消耗最多的水是通过挖井或环井抽取的地下水。为了确定压降环井的透光率,可以在泵试中应用含水层试验。测试的环井位于Marpoyan Damai地区的25个不同位置。在环井的泵送试验中,得到了压降试验数据s,乘以t,流量Q,然后绘制出s/Q vs Q的曲线图,s/Q轴与C梯度和决定系数d2的直线切断a值。然后将所得值代入Cooper-Jacob法的透射率公式。选择t = 3分钟和t = 7分钟的A值是因为它们在C值中的结果非常接近。t = 3分钟和t = 7分钟的C值分别为0.1671和0.1672。所得透射率值为134.5 m2/day。该值显示了马尔波扬达麦地区潜在的有用地下水含水层,因为透过率值超过50 m2 /天。
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