Yonggui Wu

Dr. Yonggui Wu


Research Focus & Metrics

Academic Career Length

12Years (2015-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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14 March 2018 in Environmental Science and Pollution Research
Verified
Journal Article
Closed access
PDF file
YLYoufa Luo
Youfa Luo
YWYonggui Wu
Yonggui Wu
HWHu Wang
Hu Wang
RXRongrong Xing
Rongrong Xing
ZZZhilin Zheng
Zhilin Zheng
LYLian Yang
Lian Yang

12 July 2018 in Journal of Soils and Sediments
Verified
Journal Article
Closed access
PDF file
YLYoufa Luo
Youfa Luo
YWYonggui Wu
Yonggui Wu
JQJing Qiu
Jing Qiu
HWHu Wang
Hu Wang
LYLian Yang
Lian Yang

1 October 2019 in Environmental Pollution
Verified
Journal Article
Closed access
YLYoufa Luo
Youfa Luo
YWYonggui Wu
Yonggui Wu
JSJie Shu
Jie Shu
ZWZhixue Wu
Zhixue Wu

1 January 2022 in Chemosphere
Verified
Journal Article
Closed access
YLYoufa Luo
Youfa Luo
ZZZhilin Zheng
Zhilin Zheng
PWPan Wu
Pan Wu
YWYonggui Wu
Yonggui Wu

1 January 2020 in Chemosphere
Verified
Journal Article
Closed access
MAMing Ao
Ming Ao
XXXiaohang Xu
Xiaohang Xu
YWYonggui Wu
Yonggui Wu
CZChao Zhang
Chao Zhang
BMBo Meng
Bo Meng
Guangle QiuGuangle Qiu
Guangle Qiu

1 January 2021 in Ecotoxicology and Environmental Safety
Verified
Journal Article
Open access
JWJichang Wen
Jichang Wen
YWYonggui Wu
Yonggui Wu
XLXinlong Li
Xinlong Li
QLQian Lu
Qian Lu
YLYoufa Luo
Youfa Luo
CLChunmei Li
Chunmei Li
Lanmuchang mercury-thallium mine, a typical polymetallic mine is located in southwestern Guizhou, China, is the most serious and typical area resulted from multi-metal contamination (Tl, Hg, As, and Sb). After the mercury-thallium mining, a large area of surrounding rocks such as argillaceous sandstone with high contents of Tl, Hg, As, and Sb is exposed to air. Weathering caused the argillaceous sandstone to form different weathering layers, including the grey-black external layer, the brown-yellow middle layer and the gray-white inner layer, and the external layer was enriched with higher heavy metals. However, the reason of heavy metal migration and transformation in argillaceous sandstone caused by weathering is unclear. The objective of this paper was to investigate the migration, transformation and release characteristics of Tl, Hg, As, and Sb in argillaceous sandstone during the weathering. The results indicated that weathering not only promoted an acidic oxidation environment in argillaceous sandstone, but also increased its specific surface area, pore volume and hydrophilicity, which are beneficial to the permeability of oxygen and etching liquids during the process of weathering and leaching. Meanwhile, weathering led to the transformation or decomposition of hydrophilic groups, such as -OH and -C˭O in the grey-black external layer of argillaceous sandstone, resulting in the further release of heavy metals bound to these groups. The concentration of Tl, Hg, As, and Sb in the leaching solution of argillaceous sandstone represented a positive correlation with that of Fe, Ca, Mg at different levels, indicating that Tl, Hg, As, and Sb were released with the dissolution of Fe, Ca and Mg during weathering and leaching. In summary, these results indicated that weathering caused the dissolution and migration of heavy metals in the argillaceous sandstone. Tl, Hg, As, and Sb migrated from the grey-white inner layer to the grey-black external layer and partially adsorbed by free alumina (Ald), jarosite and Ca-bearing minerals, showing enrichment phenomena, partially released into the environment, causing environmental pollution.