Multi-lithofacies alluvial characterization via airborne electromagnetic-borehole fusion using ordinary interval kriging and geologic constraints

IF 6.3 1区 地球科学 Q1 ENGINEERING, CIVIL
Yuqi Song , Frank T.-C. Tsai , Burke J. Minsley , Wade H. Kress
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Abstract

Airborne electromagnetic (AEM) survey provides extensive spatial coverage and detailed resolution at the near surface and can be used to develop hydrogeological models. However, utilization of AEM data is not straightforward because AEM resistivity is an indirect measurement for inferring sediment types. This study develops an ordinary interval kriging (OIK) algorithm and a resistivity-to-multi-lithofacies (R2ML) data fusion workflow for multi-lithofacies alluvial characterization. OIK utilizes irregular interval data to construct three-dimensional (3D) resistivity fields from one-dimensional inverted AEM resistivity models. The R2ML workflow maps the resistivity field generated from OIK into a multi-facies lithological model, incorporating geologic constraints derived from well logs and geological observations. The numerical and real-world cases demonstrate that OIK is computationally efficient, accounts for 3D anisotropy, and minimizes the smoothing effect, thereby preserving resistivity contrasts and reducing interpolation uncertainty. The methodology is applied to lithologic characterization of the Mississippi River Valley alluvial aquifer (MRVA) in the Shellmound area, Mississippi, U.S. A frequency-domain AEM survey was conducted to support groundwater studies for the managed aquifer recharge (MAR) to the MRVA. The resulting lithological model, including four types of lithofacies—clay, very fine sand, fine-medium sands, and graveliferous sands, illustrates the geomorphological processes of the MRVA and implies potential MAR. The alignment between the lithological model and existing geological and hydrogeological investigations demonstrates that OIK and R2ML workflow effectively capture the subsurface architecture of the MRVA. The methods have broad applicability for characterizing alluvial aquifers through AEM-borehole data fusion, supporting sustainable groundwater management.
利用普通层段克里格法和地质约束,通过机载电磁-钻孔融合表征多岩相冲积
机载电磁(AEM)测量提供了广泛的空间覆盖范围和近地表的详细分辨率,可用于开发水文地质模型。然而,利用AEM数据并不简单,因为AEM电阻率是推断沉积物类型的间接测量方法。本研究开发了一种普通区间克里格(OIK)算法和一种多岩相电阻率-多岩相(R2ML)数据融合工作流,用于多岩相冲积表征。OIK利用不规则区间数据,从一维反向AEM电阻率模型中构建三维(3D)电阻率场。R2ML工作流程将OIK生成的电阻率场映射到多相岩性模型中,并结合了测井和地质观测得出的地质约束条件。数值和实际案例表明,OIK计算效率高,考虑了三维各向异性,并最大限度地减少了平滑效应,从而保留了电阻率对比度,减少了插值的不确定性。该方法应用于美国密西西比州贝丘地区的密西西比河流域冲积含水层(MRVA)的岩性特征,进行了频域AEM调查,以支持对MRVA的管理含水层补给(MAR)的地下水研究。所得到的岩性模型包括四种类型的岩相——粘土、极细砂、中细砂和含砾砂,说明了MRVA的地貌过程,并暗示了潜在的mara。岩性模型与现有地质和水文地质调查的对比表明,OIK和R2ML工作流程有效地捕捉了MRVA的地下结构。该方法具有广泛的适用性,可以通过aem -钻孔数据融合来表征冲积含水层,支持地下水的可持续管理。
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来源期刊
Journal of Hydrology
Journal of Hydrology 地学-地球科学综合
CiteScore
11.00
自引率
12.50%
发文量
1309
审稿时长
7.5 months
期刊介绍: The Journal of Hydrology publishes original research papers and comprehensive reviews in all the subfields of the hydrological sciences including water based management and policy issues that impact on economics and society. These comprise, but are not limited to the physical, chemical, biogeochemical, stochastic and systems aspects of surface and groundwater hydrology, hydrometeorology and hydrogeology. Relevant topics incorporating the insights and methodologies of disciplines such as climatology, water resource systems, hydraulics, agrohydrology, geomorphology, soil science, instrumentation and remote sensing, civil and environmental engineering are included. Social science perspectives on hydrological problems such as resource and ecological economics, environmental sociology, psychology and behavioural science, management and policy analysis are also invited. Multi-and interdisciplinary analyses of hydrological problems are within scope. The science published in the Journal of Hydrology is relevant to catchment scales rather than exclusively to a local scale or site.
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