基于点速探头测量的含水层渗透率和宏观分散性随机表征(在博登场址的应用)

IF 5 1区 地球科学 Q2 ENVIRONMENTAL SCIENCES
Gedeon Dagan, Gerardo Severino
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引用次数: 0

摘要

最近发展起来的一项浅层含水层表征技术是基于点速度探针(PVP)。在插入地下的垂直管道的端口处,以厘米尺度测量水流速度。Osorno等人(2022年,https://doi.org/10.1029/2020wr029034)在靠近Sudicky(1986年,https://doi.org/10.1029/wr022i013p02069)进行的输送实验地点的Borden含水层进行了现场试验。其中一个主要目的是通过确定含水层的水力导电性场来验证该方法,并将其与广泛的水力导电性采样确定的结果进行比较(Sudicky, 1986, https://doi.org/10.1029/wr022i013p02069)。沿着垂直平面测量速度,垂直于平均水头梯度,在之前的现场试验区附近,沿着15条垂直线在420个端口测量速度。通过回灌和抽水井,形成了一种强制的稳定流动。Osorno等人(2022,https://doi.org/10.1029/2020wr029034)的分析得出了纵向对数速度的直方图及其横向和垂直半方差图。我们的主要目的是利用这些数据,用一种相对简单和一般的方法,推导出渗透率场的统计矩。我们假设对数电导率是轴对称两点协方差的随机平稳变量。该构造具有测井渗透率均值、方差、横向和纵向积分尺度等特征。横向和垂直速度协方差在理论上以半解析形式导出,根据测井-电导率参数,随后通过与测量结果的最佳拟合来确定。得到的对数电导率方差和积分尺度与Sudicky (1986, https://doi.org/10.1029/wr022i013p02069)的结果相当一致,随后的宏观色散接近输运实验的特征。最后,我们通过简单分析发现PVP是一种很有前途的表征方法。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Stochastic Characterization of Aquifer Permeability and Macrodispersivity Based on Point Velocity Probes Measurements (With Application to Borden Site)
A recently developed technology of characterization of shallow aquifers is based on the point velocity probes (PVP). At ports along vertical tubes which are inserted in the subsurface, water velocity is measured at the centimeter scale. This technique was applied by Osorno et al. (2022, https://doi.org/10.1029/2020wr029034) to a field test at the Borden aquifer, near the site of the transport experiment conducted by Sudicky (1986, https://doi.org/10.1029/wr022i013p02069). One of the main aims was to validate the method by identifying the aquifer hydraulic conductivity field and to compare it with the one determined by the extensive hydraulic conductivity sampling (Sudicky, 1986, https://doi.org/10.1029/wr022i013p02069). The velocities were measured along a vertical plane, normal to the mean head gradient, in the neighborhood of the previous field test area, at 420 ports along 15 vertical lines. A forced steady flow was created by recharging and pumping wells. The analysis of Osorno et al. (2022, https://doi.org/10.1029/2020wr029034) led to the histogram of the longitudinal log-velocities and to their transverse and vertical semi-variograms. Our main aim is to use these data to derive, by a relatively simple and general method, the statistical moments of the permeability field. We assumed that the log-conductivity is a random, stationary variable of axisymmetric two point covariance. The structure is characterized by the log-permeability mean, variance and transverse as well as vertical integral scales. The transverse and vertical velocity covariances were derived theoretically in a semi analytical form, in terms of the log-conductivity parameters, which were subsequently determined by a best fit with measurements. The resulting log-conductivity variance and integral scales were in fair agreement with those of Sudicky (1986, https://doi.org/10.1029/wr022i013p02069) and the ensuing macrodispersivity was close to the one characterizing the transport experiment. Concluding, we found by a simplified analysis that the PVP is a promising characterization methodology.
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来源期刊
Water Resources Research
Water Resources Research 环境科学-湖沼学
CiteScore
8.80
自引率
13.00%
发文量
599
审稿时长
3.5 months
期刊介绍: Water Resources Research (WRR) is an interdisciplinary journal that focuses on hydrology and water resources. It publishes original research in the natural and social sciences of water. It emphasizes the role of water in the Earth system, including physical, chemical, biological, and ecological processes in water resources research and management, including social, policy, and public health implications. It encompasses observational, experimental, theoretical, analytical, numerical, and data-driven approaches that advance the science of water and its management. Submissions are evaluated for their novelty, accuracy, significance, and broader implications of the findings.
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