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RATE OF SUCCESS FOR GROUNDWATER DRILLING TARGETS BASED ON AEM FOR THE GASCOYNE RIVER PROJECT IN WESTERN AUSTRALIA

机译:基于AEM的地下水钻井目标成功率在澳大利亚西澳大利亚汽笛河工程

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In a collaboration between Department of Agriculture and Food, Western Australia (DAFWA) and CSIRO, funded by the Western Australia Government's Royalties for Regions Program and the Gascoyne Foodbowl Project, the Gascoyne River AEM Aquifer and Groundwater Characterization Project was established with the aim of determining whether airborne electromagnetic (AEM) data can be employed to better map attributes of the unconfined alluvial aquifer beneath and adjacent to the ephemeral Gascoyne River. One major aspect of the project was to produce drilling targets, based on interpretation of AEM data, for groundwater production. In a previous presentation delivered at SAGEEP (2015), we explained our method of selecting 71 drill targets. In this presentation, we briefly recapitulate our method and discuss the result of the drilling campaign that ensued. We show that our exploration targets have resulted in overwhelming success in the conversion of exploration wells to production bores; and that the production wells produce greater yields of better quality groundwater than previous campaigns that were conducted through step-out drilling. We also show that the interpretation of the AEM inversions allowed us to map the aquitard layers that define the bottom of the Gascoyne River Old Alluvium aquifer system, determine the extent of the saltwater intrusion from the nearby Indian Ocean, and to calculate the overall volume of the aquifer system. These calculations allow us to provide estimates of total groundwater volume contained in the aquifer for sustainable production.
机译:在农业和食品部之间的合作中,西澳大利亚州西澳大利亚政府政府为地区计划和Gascoyne Foodbowl项目资助的CSIRO资助的汽笛河AEM Aquifer和地下水表征项目的目的是确定的无论是机载电磁(AEM)数据是否可以用于更好地映射下面的非整合的冲积含水层和毗邻短暂的汽笛河流。该项目的一个主要方面是根据AEM数据的解释,为地下水生产产生钻井目标。在Sageep(2015年)交付的先前演示中,我们解释了选择71钻头目标的方法。在本演示文稿中,我们简要介绍了我们的方法,并讨论了随之而来的钻探活动的结果。我们表明,我们的勘探目标导致勘探井转化为生产钻孔的成功压倒性;并且,生产井的产量提高了更好的地下水,比以前通过步进钻探进行的运动。我们还表明,解释AEM反转允许我们映射水流层,这些层定义汽笛河旧的含水层系统的底部,确定附近印度洋的咸水入侵的程度,并计算整体体积含水层系统。这些计算允许我们提供可持续生产含水层中所含地下水体积的估计。

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