Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.22201/cgeo.20072902e.2019.3.1039 |
Effects of the interaction between an acid solution and pedogenic carbonates: the case of the Buenavista del Cobre Mine, Mexico | |
Yazmin Rivera-Uria, Maria; Martin Romero, Francisco; Sedov, Sergey; Ramos, Daniel; Solleiro-Rebolledo, Elizabeth; Diaz-Ortega, Jaime | |
通讯作者 | Rivera-Uria, MY (corresponding author), Univ Nacl Autonoma Mexico, Inst Geol, Posgrad Ciencias Tierra, Mexico City 04510, DF, Mexico. |
来源期刊 | REVISTA MEXICANA DE CIENCIAS GEOLOGICAS
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ISSN | 1026-8774 |
出版年 | 2019 |
卷号 | 36期号:3页码:308-320 |
英文摘要 | The main purpose of this work was to study and understand the interaction that occurred between an acid solution spilled from Buenavista del Cobre Mine and the soils located in the Bacanuchi River area. The question put forward in this work was: if the soils of the area were able to cushion the impact of the acid solution?. Two soil profiles were examined: Profile 8A, was located on the riverbank and was affected by the spill, whilst Profile 8B, located on the first terrace of the river valley, remained intact . Both soils profiles were chemically characterized. An additional three surface samples (0-30 cm) were taken for gcoavailability tests (RBI, SB2, belonging to Profile 8B, and SB3, belonging to Profile 8A). Two further samples, representing typical unaltered soils of profiles 8A and 8B, were taken for their micromorphological study. The results showed a difference between the two profiles, with profile 8A having more acidic pH, greater electrical conductivity, and higher concentrations of Fe, Pb, Cu and As than profile 8B. The geoavailability test showed that the elements enriched in SB3 were stable and not available to the aqueous phase. The soils of Bacanuchi River contain carbonates, which interacted with the acid solution and stabilized the potentially toxic elements presents in the spilled acid solution. This interaction with carbonates promoted a new minerals formation such as gypsum and copiapite. So, the release of contaminants from soil to surface and ground waters is improbable, unless the redox conditions change or a new spill occurs releasing the potentially toxic elements (PTE) to the environment. In this work we show the importance of pedogenic carbonates in soils of arid and semiarid environments; these carbonates represent a natural geochemical barrier, that can prevent the migration of PTEs in mining areas. |
英文关键词 | soils secondary carbonates acid solution potentially toxic elements |
类型 | Article |
语种 | 英语 |
开放获取类型 | gold |
收录类别 | SCI-E |
WOS记录号 | WOS:000510766200002 |
WOS关键词 | MINING DISTRICT ; TRACE-ELEMENTS ; SOIL ; METALS ; PH ; PRECIPITATION ; CONTAMINATION ; REMEDIATION ; FRACTIONS ; RETENTION |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
来源机构 | Universidad Nacional Autónoma de México |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/369493 |
作者单位 | [Yazmin Rivera-Uria, Maria; Ramos, Daniel] Univ Nacl Autonoma Mexico, Inst Geol, Posgrad Ciencias Tierra, Mexico City 04510, DF, Mexico; [Martin Romero, Francisco; Sedov, Sergey; Solleiro-Rebolledo, Elizabeth; Diaz-Ortega, Jaime] Univ Nacl Autonoma Mexico, Inst Geol, Mexico City 04510, DF, Mexico |
推荐引用方式 GB/T 7714 | Yazmin Rivera-Uria, Maria,Martin Romero, Francisco,Sedov, Sergey,et al. Effects of the interaction between an acid solution and pedogenic carbonates: the case of the Buenavista del Cobre Mine, Mexico[J]. Universidad Nacional Autónoma de México,2019,36(3):308-320. |
APA | Yazmin Rivera-Uria, Maria,Martin Romero, Francisco,Sedov, Sergey,Ramos, Daniel,Solleiro-Rebolledo, Elizabeth,&Diaz-Ortega, Jaime.(2019).Effects of the interaction between an acid solution and pedogenic carbonates: the case of the Buenavista del Cobre Mine, Mexico.REVISTA MEXICANA DE CIENCIAS GEOLOGICAS,36(3),308-320. |
MLA | Yazmin Rivera-Uria, Maria,et al."Effects of the interaction between an acid solution and pedogenic carbonates: the case of the Buenavista del Cobre Mine, Mexico".REVISTA MEXICANA DE CIENCIAS GEOLOGICAS 36.3(2019):308-320. |
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