Oxidative sulfide weathering and weak mineral attenuation controlling arsenic mobility in a crystalline aquifer.

IF 5.5 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES
Swati Ganveer, Kamal Lochan Pruseth, David Anand Aind
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引用次数: 0

Abstract

This study investigates the source-sink dynamics and hydrogeochemical controls governing arsenic fate and transport within a fractured crystalline aquifer system. The hydrogeologic framework is characterized by spatial heterogeneity in redox conditions and persistent undersaturation with respect to key Fe-, sulfate-, and Ca-bearing mineral phases. Mineralogical characterization identifies arsenopyrite and cobaltite as the primary geogenic sources; oxidative weathering of these sulfide phases drives the continuous release of arsenic. Aqueous speciation modeling reveals a predominance of As(V) and Fe(III) species, with minor As(III) occurring within reducing microenvironments. Persistent undersaturation of Fe- and As-bearing minerals, together with other attenuation-controlling phases, suggests limited potential for secondary mineral precipitation, while allowing arsenic to remain predominantly in the dissolved phase. Weak correlations between arsenic and hydrochemical gradients indicate that contaminant distribution is highly heterogeneous and controlled by the occurrence of mineralized zones. The results demonstrate that persistent arsenic mobility in fractured crystalline aquifers can occur under predominantly oxidizing conditions through sustained sulfide weathering combined with limited attenuation capacity within the aquifer system.

氧化硫化物风化和弱矿物衰减控制砷在结晶含水层中的迁移。
本研究探讨了裂隙结晶含水层系统中砷的源库动力学和水文地球化学控制。水文地质框架的特征是氧化还原条件下的空间异质性和关键含铁、含硫酸盐和含钙矿物相的持续欠饱和。矿物学特征确定毒砂和钴矿为主要成矿源;这些硫化物相的氧化风化作用驱使砷不断释放。水相物种模型揭示了As(V)和Fe(III)的优势,少量As(III)发生在还原性微环境中。含铁和含砷矿物的持续欠饱和,以及其他衰减控制相,表明次生矿物沉淀的潜力有限,同时使砷主要保持在溶解相。砷与水化学梯度之间的弱相关性表明污染物的分布具有高度的非均质性,并受矿化带的产状控制。结果表明,在以氧化为主的条件下,通过持续的硫化物风化和含水层系统内有限的衰减能力,裂隙结晶含水层中砷的持续迁移可能发生。
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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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