Pyrite oxidation under simulated acid rain weathering conditions

被引:23
|
作者
Zheng, Kai [1 ,2 ]
Li, Heping [1 ]
Wang, Luying [1 ,2 ]
Wen, Xiaoying [1 ,2 ]
Liu, Qingyou [1 ]
机构
[1] Chinese Acad Sci, Inst Geochem, Key Lab High Temp & High Pressure Study Earths In, Guiyang 550002, Guizhou, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100039, Peoples R China
关键词
Pyrite; Simulated acid rain; Weathering; pH drainage; ELECTROCHEMICAL-BEHAVIOR; PERCHLORATE SOLUTIONS; SULFIDE MINERALS; MILD-STEEL; CHALCOPYRITE; FLOTATION; ACIDIFICATION; SUBSTANCES; ELECTRODES; RECOVERY;
D O I
10.1007/s11356-017-9804-9
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
We investigated the electrochemical corrosion behavior of pyrite in simulated acid rain with different acidities and at different temperatures. The cyclic voltammetry, polarization curve, and electrochemical impedance spectroscopy results showed that pyrite has the same electrochemical interaction mechanism under different simulated acid rain conditions, regardless of acidity or environmental temperature. Either stronger acid rain acidity or higher environmental temperature can accelerate pyrite corrosion. Compared with acid rain having a pH of 5.6 at 25 degrees C, the prompt efficiency of pyrite weathering reached 104.29% as the acid rain pH decreased to 3.6, and it reached 125.31% as environmental temperature increased to 45 degrees C. Increasing acidity dramatically decreases the charge transfer resistance, and increasing temperature dramatically decreases the passivation film resistance, when other conditions are held constant. Acid rain always causes lower acidity mine drainage, and stronger acidity or high environmental temperatures cause serious acid drainage. The natural parameters of latitude, elevation, and season have considerable influence on pyrite weathering, because temperature is an important influencing factor. These experimental results are of direct significance for the assessment and management of sulfide mineral acid drainage in regions receiving acid rain.
引用
收藏
页码:21710 / 21720
页数:11
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