Microfacies and multi-isotope records of Anisian sequences from the Upper Yangtze Block: possible responses to tectonics and climate-driven relative sea-level change

Zhong, Yisi; Wang, Licheng; Xu, Yongzhi; Zhang, Yongming; Liu, Chenglin

doi:10.1007/s00531-020-01817-9

Cited by 6 publications

(1 citation statement)

References 62 publications

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“…When Jialingjiang formations deposited, the paleoclimatic was hot and arid, and the South China Marine Transgression provided su cient seawater. As seawater evaporated and concentrated, calcite, dolomite, gypsum, and halite were precipitated successively (Zhong et al 2020). Seawater is rich in seven kinds of ions: Ca 2+ , Mg 2+ , Na + , K + , HCO 3 -, SO 4 2and Cl -.…”

Section: Hydrogeochemical Processmentioning

confidence: 99%

A Method for Quantifying the Role of Carbonate Acid, Sulfuric Acid and Nitric Acid in Carbonate Weathering After Modifying the Effect of Evaporite in Qingjiang Karst Catchment

Zhou

Wan

et al. 2021

Preprint

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Qingjiang river is the second largest tributary of the Yangtze River in Hubei province, it’s also a typical karst catchment. Eighty-two important groundwater samples were collected during high and low water period of 2019. The results show that: (1) The major hydrochemistry types are Ca+Mg-HCO3 and Ca-HCO3, indicate that carbonate weathering is the main source of groundwater chemistry; (2) The results of inverse hydrochemical modeling show that there are two kinds of groundwater-carbonate rock interactions. One is co-dissolution of calcite and dolomite, the other is dedolomitization, and thereinto, dedolomitization is widespread in dolomite aquifers. Furthermore, gypsum has a tendency to dissolve in each aquifer, and the common ion effect of Ca2+ caused by gypsum dissolution promotes dedolomitization. The modeling results suggest that major elements have a good traceability effect on the material source of groundwater. (3) The chemical weathering of carbonate rock is mainly affected by carbonic acid, sulfuric acid and nitric acid. After modifying the impact of evaporite and atmospheric input, the calculations show that the contribution of carbonic acid involved in carbonate weathering is 70.9% (high water period) and 70.0% (low water period). Through statistics of karst springs discharge and contribution of acid involved in carbonate weathering, the two are in a positive relationship. The result can reflect the laws of sulfuric acid and nitric acid under the hydrodynamic condition in different seasons. Therefore, the carbonate weathering should be carefully evaluated in karst areas which have abundant groundwater and the role of groundwater in carbonate weathering is worthy of further study.

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Section: Hydrogeochemical Processmentioning

confidence: 99%