不同水分和黑页岩含量对黄土电阻率影响的研究

IF 3.5 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES
Jishi Geng , Hao Huang , Qiang Sun , Jianjun Hu , Qingmin Shi , Chao Lyu
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引用次数: 0

摘要

土壤退化以土壤物理和化学性质恶化、养分流失和有毒物质增加为特征,是采矿活动中的一个主要生态问题。本研究探讨了如何利用矿业开发过程中产生的废弃黑页岩作为黄土添加剂,以增强矿区复垦的土壤特性。研究包括对不同黑页岩和水含量的改良复垦黄土进行电阻率和有机碳含量测试。此外,还研究了这些改良土壤在不同交流频率下的电特性。结果表明,土壤塑性和 1.5% 的黑页岩含量对改良黄土的电特性有重要影响。水分含量和黑页岩会影响土壤导电路径和电阻率的变化。由于阳离子在水中的吸附作用以及在电场作用下的定向传输,黑页岩中丰富的粘土矿物在改变土壤电阻率方面起着至关重要的作用。考虑到土壤的三相组成和弥散双层结构,该研究阐明了改良复垦黄土电特性变化背后的机理,并考虑了水和黑页岩的含量。这项研究证明了使用黑页岩作为土壤添加剂的可行性,并强调了电阻率测试(ERT)测量对改良再生土壤的无损评估潜力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Study on the influence of different water and black shale content on the resistivity of loess

Study on the influence of different water and black shale content on the resistivity of loess

Soil degradation, characterized by the deterioration of soil physical and chemical properties, nutrient loss, and an increase in toxic substances, is a key ecological concern in mining activities. This study explores the use of waste black shale from mining development as an additive to loess to enhance soil properties for reclamation in mining areas. The research includes resistivity and organic carbon content tests on modified reclaimed loess with varying black shale and water contents. Additionally, the electrical properties of these modified soils are investigated across different AC frequencies. The results highlight the significance of soil plasticity and a 1.5% black shale content in influencing reclaimed loess's electrical properties. Moisture content and black shale influence changes in soil conductive paths and resistivity. The abundance of clay minerals in black shale plays a crucial role in altering soil electrical resistivity due to the adsorption of cations in water and the directional transport under an electric field. Considering soil's three-phase composition and diffuse bilayer structure, the study elucidates the mechanism behind changes in the electrical properties of improved reclaimed loess, accounting for water and black shale content. This research demonstrates the feasibility of using black shale as a soil additive and emphasizes the non-destructive assessment potential of electrical resistivity test (ERT) measurements for modified reclaimed soils.

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来源期刊
Journal of contaminant hydrology
Journal of contaminant hydrology 环境科学-地球科学综合
CiteScore
6.80
自引率
2.80%
发文量
129
审稿时长
68 days
期刊介绍: The Journal of Contaminant Hydrology is an international journal publishing scientific articles pertaining to the contamination of subsurface water resources. Emphasis is placed on investigations of the physical, chemical, and biological processes influencing the behavior and fate of organic and inorganic contaminants in the unsaturated (vadose) and saturated (groundwater) zones, as well as at groundwater-surface water interfaces. The ecological impacts of contaminants transported both from and to aquifers are of interest. Articles on contamination of surface water only, without a link to groundwater, are out of the scope. Broad latitude is allowed in identifying contaminants of interest, and include legacy and emerging pollutants, nutrients, nanoparticles, pathogenic microorganisms (e.g., bacteria, viruses, protozoa), microplastics, and various constituents associated with energy production (e.g., methane, carbon dioxide, hydrogen sulfide). The journal''s scope embraces a wide range of topics including: experimental investigations of contaminant sorption, diffusion, transformation, volatilization and transport in the surface and subsurface; characterization of soil and aquifer properties only as they influence contaminant behavior; development and testing of mathematical models of contaminant behaviour; innovative techniques for restoration of contaminated sites; development of new tools or techniques for monitoring the extent of soil and groundwater contamination; transformation of contaminants in the hyporheic zone; effects of contaminants traversing the hyporheic zone on surface water and groundwater ecosystems; subsurface carbon sequestration and/or turnover; and migration of fluids associated with energy production into groundwater.
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