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Estimating hydraulic parameters of the Acu-Brazil aquifer using the computer analysis of micrographs

机译:使用显微照片的计算机分析估算Acu-巴西含水层的水力参数

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The conventional way of obtaining hydraulic parameters of aquifers is through the interpretation of aquifer tests that requires a fairly complex logistics in terms of equipment and personnel. On the other way, the,processing and analysis of digital images of two-dimensional rock sample micrographs presents itself as a promising (simpler and cheaper) alternative procedure for obtaining estimates for hydraulics parameters. This methodology involves the sampling of rocks, followed by the making and imaging of thin rock samples, image segmentation, three-dimensional reconstruction and flow simulation. This methodology was applied to the outcropping portion of the Acu aquifer in the northeast of Brazil, and the computational analyses of the thin rock sections of the acquired samples produced effective porosities between 11.2% and 18.5%, and permeabilities between 52.4 mD and 1140.7 mD. Considering that the aquifer is unconfined, these effective porosity values can be used effectively as storage coefficients. The hydraulic conductivities produced by adopting different water dynamic viscosities at the temperature of 28 degrees C in the conversion of the permeabilities result in values in the range of [6.03 x 10(-7),1.43 x 10(-5)] m/s, compatible with the local hydrogeology. (C) 2016 Elsevier B.V. All rights reserved.
机译:获取含水层水力参数的常规方法是通过解释含水层试验,这需要在设备和人员方面进行相当复杂的后勤工作。另一方面,二维岩石样品显微照片的数字图像的处理和分析本身是获得水力学参数估计的有希望的(更简单,更便宜)的替代方法。这种方法包括对岩石进行采样,然后对薄岩石样品进行制作和成像,图像分割,三维重建和流量模拟。该方法应用于巴西东北部Acu含水层的露头部分,对所采集样品的薄岩段进行的计算分析得出有效孔隙率在11.2%至18.5%之间,渗透率在52.4 mD至1140.7 mD之间。考虑到含水层是无限制的,这些有效孔隙率值可以有效地用作储水系数。通过在28摄氏度的温度下采用不同的水动力粘度进行渗透率转换而产生的水力传导率的值范围为[6.03 x 10(-7),1.43 x 10(-5)] m / s ,与当地水文地质兼容。 (C)2016 Elsevier B.V.保留所有权利。

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