Hydrogeochemistry characterization of an overexploited municipal, agricultural, and industrial aquifer, central Mexico

Amézaga-Campos, Blanca Sofia; Villanueva-Estrada, Ruth Esther; Carrillo-Chávez, Alejandro; Morales-Arredondo, José Iván; Morán-Ramírez, Janete

doi:10.1016/j.apgeochem.2022.105310

Cited by 9 publications

(1 citation statement)

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“…Another important source of Early-Middle Triassic altered volcanic ash is the chemical weathering of F-rich volcanic rocks in the vicinity of the basin. High fluorine concentrations have always been found in felsic igneous rocks (Chowdhury et al, 2019;Liu et al, 2020;Amézaga-Campos et al, 2022). In this study, the altered volcanic ashes were considered to be derived from the eruption of episodic volcanism (e.g., Xiao and Hu, 2005;Lin et al, 2020;Feng M. S. et al, 2021).…”

Section: The Formation Process Of F-rich Bentonitesmentioning

confidence: 99%

Fluorine speciation and origin of Early-Middle Triassic bentonite deposits in Sichuan Basin, South China

Lin

Zheng²,

Zhang³

et al. 2023

Front. Earth Sci.

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Fluorine (F) is one of the most important environmentally harmful elements released by volcanic activity, and the bentonite deposits that formed from volcanic ashes are potentially harmful to the environment. However, the mechanisms governing F-rich bentonite formation and its F speciation composition remain enigmatic. The F-rich bentonite deposits are widely distributed in the Early-Middle Strata of the Sichuan Basin, South China. Detailed mineralogical and geochemical studies were conducted on the bentonite deposits from five sections of the Sichuan Basin. X-ray diffraction (XRD) analyses indicate that the F-rich bentonites mainly contain quartz, carbonates (calcite and dolomite) or gypsum, and clay minerals, while the clay minerals are dominated by illite and illite/smectite (I/S). Clay mineralogical studies suggest that bentonites were transformed from volcanic ashes during diagenesis by smectite illitization. The major and trace element distribution in F-rich bentonite deposits altered from volcanic ashes is most likely derived from felsic magmas, and alteration of the parent rocks (e.g., rhyolites) to bentonite is associated with leaching and subsequent removal of F. The total fluorine content (FTOT) of the bentonite samples ranged from 1,162 mg/kg to 2,604 mg/kg (average = 1773 mg/kg), well above the average FTOT contents of soils in the world. The results of the sequential extraction experiments show that the highest content is residual-fluorine (Fres), followed by carbonate-fluorine (Fcar) with a mean value of 1,556 mg/kg and 186 mg/kg, indicating carbonate is an important F sink in bentonite deposits. The average fluorine value of organic fluorine (For), Fe/Mn oxide-fluorine (Ffm) and exchangeable fluorine (Fex) are relatively low with an average value of 17.5 mg/kg, 6.8 mg/kg and 4.1 mg/kg, respectively. However, water-soluble fluorine (Fws) has a mean value of 4.0 mg/kg, which is higher than the corresponding average value in soils in an area susceptible to endemic fluorosis in China. Based on the characteristic of fluorine speciation, the fluorine in bentonite deposits may pose a risk to the environment. This study makes an important contribution to a better understanding of the characteristic of fluorine speciation in bentonites and the formation mechanism that governs fluorine enrichment in bentonites.

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