Hydrogeologic controls on barrier island geomorphology: Insights from electromagnetic surveys

Q2 Earth and Planetary Sciences Leading Edge Pub Date : 2023-09-01 DOI:10.1190/tle42090608.1
Ramadan Abdelrehim, Mohamed Ahmed, Mark E. Everett
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Abstract

Barrier islands provide a first line of defense for coastal communities against storms, hurricanes, and sea-level rise. The geomorphology of barrier islands exerts a major control on storm impact and island recovery. In turn, barrier island geomorphology is affected by subsurface hydrogeologic conditions. In this study, we investigated the relationship between subsurface hydrogeologic conditions and geomorphology of Padre Island, with a focus on the influence of human development. We measured apparent electrical conductivities using frequency-domain electromagnetic (FDEM) surveys and spatially correlated them with the island's morphology. The latter was generated from a 1 m resolution digital elevation model. Four distinct zones were identified from the observed variations in apparent conductivity and elevation, revealing their inverse correlation. The beach area (Zone I) exhibits the highest apparent conductivity (289.7 ± 66.3 mS/m) and the lowest elevations (1.4 ± 0.2 m). These trends are largely due to the proximity of the beach to saline groundwater and maritime floods. Conversely, the foredune area (Zone II) presents the lowest apparent conductivity (19.0 ± 3.4 mS/m) and the highest elevation (4.5 ± 0.4 m) due to a greater distance from saline waters, deeper groundwater levels, and relatively dry soil conditions. Human development has significantly impacted Zones III (east central zone) and IV (west central zone), contributing to an increase in apparent conductivity (Zone III: 40.3 ± 21.8 mS/m; Zone IV: 159.5 ± 83.0 mS/m) and a reduction in elevation (Zone III: 2.1 ± 0.5 m; Zone IV: 1.3 ± 0.4 m). Anthropogenic activities have modified hydrologic patterns, introduced conductive materials, and altered vegetation cover and soil composition. This research elucidates the interplay between subsurface electrical conductivity, surface morphology, and the impact of human development on barrier island geomorphology, providing crucial insights for coastal management and conservation efforts.
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堰洲岛地貌的水文地质控制:来自电磁调查的见解
堰洲岛为沿海社区抵御风暴、飓风和海平面上升提供了第一道防线。障壁岛的地貌对风暴影响和岛屿恢复起着重要的控制作用。堰洲岛的地貌又受到地下水文地质条件的影响。本文研究了帕德雷岛地下水文地质条件与地貌的关系,重点研究了人类发展对其的影响。我们使用频域电磁(FDEM)测量视电导率,并将其与岛屿的形态在空间上相关联。后者是由1米分辨率的数字高程模型生成的。根据观察到的表观电导率和海拔的变化,确定了四个不同的区域,揭示了它们的负相关关系。海滩区(I区)表现出最高的表观电导率(289.7±66.3 mS/m)和最低的海拔(1.4±0.2 m),这些趋势主要是由于海滩靠近含盐地下水和海洋洪水。相反,由于离咸水较远,地下水位较深,土壤条件相对干燥,前沙丘区(II区)的表观电导率最低(19.0±3.4 mS/m),海拔最高(4.5±0.4 m)。人类发展对III区(中东部)和IV区(中西部)产生了显著影响,导致视电导率增加(III区:40.3±21.8 mS/m;IV区:159.5±83.0 mS/m)和海拔降低(III区:2.1±0.5 m;IV区:1.3±0.4 m)。人为活动改变了水文格局,引入了导电物质,改变了植被覆盖和土壤组成。这项研究阐明了地下电导率、表面形态和人类发展对堰洲岛地貌的影响之间的相互作用,为海岸管理和保护工作提供了重要的见解。
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来源期刊
Leading Edge
Leading Edge Earth and Planetary Sciences-Geology
CiteScore
3.10
自引率
0.00%
发文量
180
期刊介绍: THE LEADING EDGE complements GEOPHYSICS, SEG"s peer-reviewed publication long unrivalled as the world"s most respected vehicle for dissemination of developments in exploration and development geophysics. TLE is a gateway publication, introducing new geophysical theory, instrumentation, and established practices to scientists in a wide range of geoscience disciplines. Most material is presented in a semitechnical manner that minimizes mathematical theory and emphasizes practical applications. TLE also serves as SEG"s publication venue for official society business.
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