Geochemical evolution of clay pore water as an indicator for palaeoenvironmental variability in the Hebei Plain, northern China
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- 作者：Hong Niu ; Xing Liang ; Menggui Jin ; Zhang Wen ; Jing Li…
- 关键词：Hebei Plain ; Clay pore water ; Geochemical evolution ; Palaeoenvironment
- 刊名：Environmental Earth Sciences
- 出版年：2016
- 出版时间：January 2016
- 年：2016
- 卷：75
- 期：2
- 全文大小：3,807 KB
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Xing Liang (1) (2)
Menggui Jin (1) (3)
Zhang Wen (1)
Jing Li (1)
Bin Ma (1)
Yalei Liu (1)
1. School of Environmental Studies, China University of Geosciences, Wuhan, 430074, China
2. Hubei Key Laboratory of Wetland Evolution & Ecological Restoration, School of Environment Studies, China University of Geosciences, No. 388 Lumo Road, Wuhan, 430074, China
3. State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430074, China - 刊物类别：Earth and Environmental Science
- 刊物主题：None Assigned
- 出版者：Springer Berlin Heidelberg
- ISSN：1866-6299
文摘
In order to elaborate geochemical evolution of clay pore water (CPW) and associated palaeoenvironment in Hengshui, where there is shallow saline water in the area of Hebei Plain, a borehole with a depth of 130 m was drilled in August 2013 in Hengshui city. Q4 sediments occurred above 35 m and Q3 mainly at depth of 130–35 m. Sediment particle size, geochemistry and deuterium and oxygen isotopes of CPW were analyzed. The CPW was generally of meteoric origin and was influenced by evaporation. Total dissolved solids (TDS) in pore water were high, which was mainly controlled by Na+, Mg2+, SO4 2− and Cl−. Ratios of rNa/rCa of CPW were mostly larger than 1, indicating the missing of Ca2+, as a result of evaporation and cation exchange. At depths of 20–10 m, ratios of rNa/rCl were larger than 1, reflecting the accumulation of Na+ during the continent salinization process. The TDS and δ 18O values of CPW above 6 m demonstrated that CPW was primarily affected by human irrigation, as well as by atmospheric precipitation. The mean δ 18O values of CPW were −11.5, −12.1 and −10.6 ‰ at depths of 130–90, 65–29 and 23–0 m, respectively, which were lower than the δ 18O values of groundwater at depths of 90–65 m (−9.8 ‰) and 29–23 m (−8.2 ‰). The depletion in 18O of CPW suggested that the CPW saved the palaeoenvironment media at depths below 6 m. The δ 18O of CPW indicated that the temperature decreased at the depths from 130 to 90 m, and the climate became colder at depths of 65–29 m but evolved to be warm in Holocene at depths of 23–0 m. Keywords Hebei Plain Clay pore water Geochemical evolution Palaeoenvironment