Loop source transient electromagnetics in an urban noise environment: A case study in Santiago de Chile

Author:

Blanco-Arrué B.1ORCID,Yogeshwar P.1ORCID,Tezkan B.1,Díaz D.2ORCID

Affiliation:

1. University of Cologne, Institute of Geophysics and Meteorology, Pohligstraße 3, Cologne 50969, Germany.(corresponding author); .

2. University of Chile, Department of Geophysics, Blanco Encalada 2002, Santiago de Chile 8370449, Chile..

Abstract

We have developed a transient electromagnetic (TEM) study in the noisy urban environment of the megacity Santiago de Chile. Our investigation characterizes the electrical conductivity structure of the Santiago Basin down to 300 m depth, providing key information about the sedimentary infill, hydrogeologic aspects, and geomorphological units. In total, 52 TEM soundings were recorded over roughly 900 km2. We identified different transient characteristics and noise patterns, spatially correlated to the investigation area. This step allowed classification of the soundings into three groups: highly distorted data, transients severely affected by cultural electromagnetic noise sources, and good-quality data with low noise levels. Conventional 1D inversion techniques were then used to derive resistivity depth models. The models were interpreted using sedimentary units, alluvial fan, static groundwater level information, and also were verified using borehole data. Based on 1D models, different minimum sedimentary thicknesses are observed, ranging between 50 and 300 m in depth. The average derived sedimentary thickness is approximately 210 m. In addition, seven soundings indicated the basement. These are mostly located toward the periphery of the Santiago Basin. We found a high conductive zone toward the north and a low-conductive area toward the south of the basin. The southern area is characterized by the absence of conductive layers at a depth between 100 and 150 m. This is likely related to the presence of a thick gravel layer and the absence of shallow clay layers acting as aquitards. The resistivity distribution and the sedimentary thickness obtained for this noisy and urban environment are key inputs for groundwater research as the water supply becomes more limited, specifically in central Chile. The overall consistency of the derived subsurface models highlights the suitability of the TEM method for investigating urban noise environments.

Funder

Programa de Riesgo Sísmico

DAAD/BECAS Chile, 2018

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

Reference53 articles.

1. ABEM, 2016, Manual WalkTEM – Guideline Geo, https://www.guidelinegeo.com/product/abem-walktem/, accessed August 2018.

2. Araneda, M., M. Avendaño, and C. Merlo, 2000, Gravimetric model of the Santiago basin, third and final phase: IX Congreso Geológico Chileno, Puerto Varas, 2, 404–408.

3. The West Andean Thrust, the San Ramón Fault, and the seismic hazard for Santiago, Chile

4. Brantt, C., 2011, Microzonificación sísmica del sector sur poniente de Santiago, comunas Buin y Paine: B.S. thesis, University of Chile.

5. Brinkhoff, T., 2018, Mayores aglomeraciones de América Latina, City Population, http://www.citypopulation.de, accessed November 2019.

同舟云学术

1.学者识别学者识别

2.学术分析学术分析

3.人才评估人才评估

"同舟云学术"是以全球学者为主线,采集、加工和组织学术论文而形成的新型学术文献查询和分析系统,可以对全球学者进行文献检索和人才价值评估。用户可以通过关注某些学科领域的顶尖人物而持续追踪该领域的学科进展和研究前沿。经过近期的数据扩容,当前同舟云学术共收录了国内外主流学术期刊6万余种,收集的期刊论文及会议论文总量共计约1.5亿篇,并以每天添加12000余篇中外论文的速度递增。我们也可以为用户提供个性化、定制化的学者数据。欢迎来电咨询!咨询电话:010-8811{复制后删除}0370

www.globalauthorid.com

TOP

Copyright © 2019-2024 北京同舟云网络信息技术有限公司
京公网安备11010802033243号  京ICP备18003416号-3