Saad Ahmed M, Sakr Mohamed A H, Selim Mohamed Sh A, Taalab Sherif A, Zakaly Hesham M H, Aboueldahab Sherif M, Omar Ali E, Zayed Mahmoud, Issa S A M, Awad Hamdy A
Geology Department, Faculty of Science, Al-Azhar University, Cairo, 11884, Egypt.
Arab Consulting Engineers Company (ACE), Cairo, Egypt.
Sci Rep. 2024 Nov 29;14(1):29670. doi: 10.1038/s41598-024-72337-8.
This study aims to evaluate the suitability of subsurface layers for infrastructure development using geophysical and geotechnical studies. Six seismic refraction and six 2D geoelectic profiles were conducted in the study area to analyze the geotechnical characteristics of the subsoil in order to assess its suitability for construction projects. According to the geophysical investigation, there are two main geoelectric strata, each with a different lithology and thickness. The first layer has high resistivity values of more than 200 (Ωm) and its thickness is between 3.5 and 6.3 m. The second layer's resistivity ranges from 0.3 to 200 (Ωm). The findings indicate that the near-surface area of the study site is composed of two layers in addition to the surface layer, which consists of semi-consolidated wadi fill deposits of gravel, sand, and silt with rock fragments. The first layer comprises fractured limestone with clay intercalation, followed by a second layer of marly limestone, which transitions into marl and clay. Both compressional (P) and shear (S) waves were detected and analyzed. The shallow seismic refraction technique indicates that the velocity waves (Vp) in the first and second layers range from 133 to 770 and 790 to 3100 m/s respectively. Various engineering parameters for the second layer were determined, including elastic moduli (bulk modulus, Poisson's ratio, rigidity modulus, and Young's modulus), competence scales (stress ratio, concentration index, material index and density gradient), and bearing capacity (ultimate and allowable). The average Poisson ratio for the first and second layers is 0.235. The ultimate bearing capacity (Qu) of the first layer ranges from 379.1 to 1031.2 gm/cm and between 1040.8 and 1548.5 gm/cm of the second layer. Allowable bearing capacity (Qall) for the first layer is between 126.4 and 343.7 gm/cm, and for the second layer, it is between 346.9 and 516.2 gm/cm. According to the geotechnical investigation's findings, the range of liquid limit (LL) values is between 41.20 and 86.30%, the range of plastic limit (PL) values is between 18 and 35.25%, the range of plasticity index (PI) values is between 14.17 and 51.45%, and the range of free swelling values is between 60 and 170%. However, the study identified high-risk areas in the study area. These zones are located in the first and second layers represented by strongly swelling clay layers and strongly fractured limestone, which will have a major impact on the road and buildings. Therefore, this study recommends addressing these problems before any development to protect these areas from subsidence and collapse.
本研究旨在通过地球物理和岩土工程研究评估地下层对基础设施开发的适用性。在研究区域进行了六条地震折射剖面和六条二维地电剖面,以分析下层土的岩土特性,从而评估其对建设项目的适用性。根据地球物理调查,有两个主要的地电地层,每个地层具有不同的岩性和厚度。第一层具有高于200(Ωm)的高电阻率值,其厚度在3.5至6.3米之间。第二层的电阻率范围为0.3至200(Ωm)。研究结果表明,研究场地的近地表区域除表层外由两层组成,表层由砾石、沙子和粉砂以及岩石碎片的半固结河道充填沉积物组成。第一层包括夹有黏土夹层的裂隙石灰岩,接着是第二层泥灰质石灰岩,其过渡为泥灰岩和黏土。检测并分析了纵波(P波)和横波(S波)。浅层地震折射技术表明,第一层和第二层中的速度波(Vp)分别在133至770米/秒和790至3100米/秒之间。确定了第二层的各种工程参数,包括弹性模量(体积模量、泊松比、刚性模量和杨氏模量)、强度指标(应力比、浓度指数、材料指数和密度梯度)以及承载力(极限承载力和允许承载力)。第一层和第二层的平均泊松比为0.235。第一层的极限承载力(Qu)范围为379.1至1031.2克/平方厘米,第二层的范围为1040.8至1548.5克/平方厘米。第一层的允许承载力(Qall)在126.4至343.7克/平方厘米之间,第二层的允许承载力在346.9至516.2克/平方厘米之间。根据岩土工程调查结果,液限(LL)值范围在41.20%至86.30%之间,塑限(PL)值范围在18%至35.25%之间,塑性指数(PI)值范围在14.17%至51.45%之间,自由膨胀值范围在60%至170%之间。然而,该研究在研究区域识别出了高风险区域。这些区域位于第一层和第二层中,由强膨胀黏土层和强裂隙石灰岩代表,这将对道路和建筑物产生重大影响。因此,本研究建议在任何开发之前解决这些问题,以保护这些区域免受沉降和坍塌的影响。