Applications of well logging techniques to evaluate the groundwater aquifers in the area between southwest Bani Sweif and west Asyoute governorate, upper Egypt.

Safi Eldein.M. Metwally, Shimaa. M. Elska, Fardous M. Zarif, Abdulla. F. Saad
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Abstract

The relevance of detecting aquifer characterization and aquifer potential has risen with the application of well logging techniques as the demand for water has increased. Apart from pumping data, 16 geophysical well logs (resistivity, gamma ray, self-potential, and nuclear logs) are utilized to achieve the main goal of estimating petrophysical parameters (porosity (∅), effective porosity (∅𝑒𝑓𝑓), hydraulic conductivity (k), permeability (K) and shale volume (𝑉𝑠ℎ)) of the Apollonia (Eocene fractured limestone aquifer), Upper and Lower Bahariya (Nubian sandstone aquifer) formations. The findings show that the Eocene fractured limestone aquifer has a carbonate in soft chalk with high K and ∅ as well as high k of 4974.39 mD at well ST-188 (a highly productive aquifer), whereas the Lower Bahariya formation is mostly fine to medium-grained sandstone and clay, suggesting that it formed in shallow marine environments with low K. On the other hand, Upper Bahariya was noted that having poor sand succession. As results shown, K of the most examined wells ranges from 2609.69 to 1486.812 mD at ST-258 and ST-38 wells respectively. The study appears that 𝑉𝑠ℎ, along with ∅ and K features, is regarded as an important attribute in aquifer evaluation where, estimated 𝑉𝑠ℎ over the studied area is ranges between 5.96% and 31.7% at ST-48 and WBS1 wells respectively. Overall, this study provides an important insight into the importance of evaluating groundwater aquifers over time to help in making decisions to save and protect groundwater aquifers in the future.
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测井技术在上埃及Bani Sweif西南部和Asyoute省西部地区地下水含水层评价中的应用
随着对水需求的增加,测井技术的应用提高了探测含水层特征和含水层潜力的相关性。除泵送资料外,还利用16口地球物理测井(电阻率、伽马、自电位、核测井)实现了对Apollonia(初新世裂缝性灰岩含水层)、Bahariya上、下(努比亚砂岩含水层)地层岩石物性参数(孔隙度(∅)、有效孔隙度(∅𝑒𝑓𝑓)、导水率(k)、渗透率(k)、页岩体积(𝑠)的估算。结果表明:始新统裂缝灰岩含水层以高K、∅的软白垩质碳酸盐岩为主,ST-188井高K为4974.39 mD(高产含水层),而下Bahariya组多为细粒至中粒砂岩和粘土,形成于低K的浅海环境;上Bahariya组砂层演替较差。结果表明,ST-258井和ST-38井的K值分别为2609.69 ~ 1486.812 mD。研究表明,ST-48井和WBS1井研究区域的估算值分别为5.96% ~ 31.7%,因此,在含水层评价中,以∅和K为特征的∑𝑠是一个重要的属性。总的来说,这项研究提供了一个重要的见解,即随着时间的推移评估地下水含水层的重要性,有助于在未来做出拯救和保护地下水含水层的决定。
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Kuwait Journal of Science & Engineering
Kuwait Journal of Science & Engineering MULTIDISCIPLINARY SCIENCES-
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