Abstract

It is important to determine the location, depth and shape (dimensions) of cavities under subsurface in site investigation phase before construction. This study aims to make a study for properties, analysis and comparison of the results of different electrodes configurations that used in 2-D electrical resistivity Tomography surveys to detection subsurface cavities to determining the appropriate and suitable configurations type that must be conduct in the field to obtain best and accurate results. Two-dimensional synthetic models were created for Geoelectrical resistivity of five different geological features, which reflects the common cases of cavities in nature. These models are (narrow, broad, shallow and deep) cavities adding to one model for multiple cavities. RES2DMOD program was used to create these models, while RES2DINV program used in Inversion method to obtain the true 2-D inverted resistivity sections for six configuration types of electrode array for 2D electrical resistivity technique, after adding a Gaussian noise ratio of (5%). Generally, we are noticed the possibilities of most tested configuration types for determine electrical anomalies, because the high contrast between the cavities and the surrounding rocks resistivities values. In addition, RMS ratio overall does not exceed 5%, hence, this ratio is an acceptable and indicates to the quality of the inverse process. The Wenner array have high sensitivity to vertical resistivity variations, and Dipole-dipole array have high sensitivity to lateral resistivity variations. While the Schlumberger-wenner have high sensitivity in both lateral and vertical resistivity variations Also, it was noted that the efficiency of all types decreasing with increasing depth of cavities detecting, due to the low percentage of contrast between the cavities and the surrounding rocks. The Wenner beta (WB) configuration is the best choice in terms of inversing true resistivity values, Secondly the Pole-Dipole (PD). While in term of determining the location and shape (approximately dimensions) of cavities, Dipole-Dipole (DD), Wenner-Schlumberger (WS), Wenner Alpha (WA), Dipole-Pole (DP) respectively. However, in case of noisy areas, Wenner Alpha (WA) configuration gives the best result.

Highlights

  • It is important to determine the location, depth and shape of cavities under subsurface in site investigation phase before construction

  • ‫الكهربائية (‪ )ERT‬فيستخدم الآن على نطاق واسع للكشف عن المشاكل الهندسية والتحريات الموقعية والتحري عن‬ ‫التكهفات والف ارغات والتجاويف تحت السطحية الطبيعية‪ ،‬والأهداف الأثرية ( ;‪; McDonald and Davies, 2003‬‬ ‫‪ .)Cardarelli, et al, 2008; Al-Heety and Shanshal, 2016; Gardi, et al, 2018‬ان تقنية المقاومية‬ ‫الكهربائية التصويرية ‪ ،ERT‬تتيح لنا توزيع المقاومية الكهربائية تحت السطحية عن طريق تسجيل عدد كبير جًدا من‬ ‫القياسات الكهربائية (‪ .)Storez et al, 2000‬حيث ان الاستجابة الجيوكهربائية المتغايرة في منطقة التحري تتيح لنا‬ ‫الحصول على مقاطع ثنائية او ثلاثية الأبعاد لتوزيع المقاومة تحت السطحية‪ ،‬مما يجعلها أداة فعالة للغاية وصديقة‬ ‫للبيئة‪ ،‬لتحليل وتوصيف الظواهر تحت السطحية وعدم الاستم اررية في الطبقات الجيولوجية

  • ‫‪Noise levels (0%) for Wenner alpha array‬‬ ‫‪Noise levels (20%) for Wenner alpha array‬‬

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Summary

Introduction

It is important to determine the location, depth and shape (dimensions) of cavities under subsurface in site investigation phase before construction.

Objectives
Results
Conclusion
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