衡水地区咸水层沉积物粒度及氘氧同位素的古气候指示

牛宏; 梁杏; 李静; 马斌; 葛勤

doi:10.3799/dqkx.2016.041

Volume 41 Issue 3

Mar. 2016

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Article Navigation > Earth Science > 2016 > 41(3): 499-507

Niu Hong, Liang Xing, Li Jing, Ma Bin, Ge Qin, 2016. Paleoclimate Instruction of Sediment Grain Size and Deuterium-Oxygen Isotope in Saline Stratum of Hengshui. Earth Science, 41(3): 499-507. doi: 10.3799/dqkx.2016.041

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Niu Hong, Liang Xing, Li Jing, Ma Bin, Ge Qin, 2016. Paleoclimate Instruction of Sediment Grain Size and Deuterium-Oxygen Isotope in Saline Stratum of Hengshui. Earth Science, 41(3): 499-507. doi: 10.3799/dqkx.2016.041

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Paleoclimate Instruction of Sediment Grain Size and Deuterium-Oxygen Isotope in Saline Stratum of Hengshui

doi: 10.3799/dqkx.2016.041

Niu Hong^1
,,
Liang Xing^{1,2
,
,},
Li Jing¹,
Ma Bin¹,
Ge Qin¹

1.
School of Environmental Studies, China University of Geosciences, Wuhan 430074, China
2.
Key Laboratory of Wetland Evolution & Ecological Restoration, China University of Geosciences, Wuhan 430074, China

Received Date: 2015-09-13
Publish Date: 2016-03-15

Abstract

Abstract

The characteristics of saline stratum in Hengshui have always been concerned. In order to discuss the paleoenvironment and the paleoclimate in Hengshui area, grain size and pore water stable isotope (δD, δ¹⁸O) of clay collected from Hengshui saline stratum(thickness of 130 m) by drilling were analyzed. The standard deviation of sediment grain size shows that the hydrodynamic strength changed from weak to strong and then to weak, there is a deep gravel layer in 90-65 m, which reflects a strong hydrodynamic strength and a humid clime. The TDS and δ¹⁸O reflect the affect of atmospheric precipitation and human irrigation above 6 m, specially for the human irrigation. The mean value of δ¹⁸O at depth of 130-90 m is -11.5‰, and it is -12.1‰ and -10.6‰ at depth of 65-29 m and 23-0 m. The δ¹⁸O of aquifer at 90-65 m is -9.8‰, and -8.2‰ of 29-23 m. The δ¹⁸O of clay pore water is negative compared with the aquifer groundwater, reflecting that the clay pore water saves paleoenvironment information. The δ¹⁸O at depth of 65-29 m firstly increases and than decreases reflecting the temperature firstly increases and than decreases; the δ¹⁸O at depth of 65-29 m reflects a low temperature; the δ¹⁸O at depth of 23-0 m is relatively stable, but is positive overall, indicating a warm climate in Holocene.
- Hengshui,
- sediment grain size,
- clay pore water,
- deuterium-oxygen isotopes,
- paleoclimate

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References(77)

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Paleoclimate Instruction of Sediment Grain Size and Deuterium-Oxygen Isotope in Saline Stratum of Hengshui

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