Seasonal variations in trace elements and influencing factors in drip water from Kaiyuan Cave, Shandong Province

CHENG Ke; WANG Qing; ZHENG Zhihui; ZHAN Chao; ZHOU Houyun; CHI Hong

doi:10.16562/j.cnki.0256-1492.2017032801

Marine Geology & Quaternary Geology > 2019 > 39(1): 154-162. > DOI: 10.16562/j.cnki.0256-1492.2017032801

CHENG Ke, WANG Qing, ZHENG Zhihui, ZHAN Chao, ZHOU Houyun, CHI Hong. Seasonal variations in trace elements and influencing factors in drip water from Kaiyuan Cave, Shandong Province[J]. Marine Geology & Quaternary Geology, 2019, 39(1): 154-162. DOI: 10.16562/j.cnki.0256-1492.2017032801

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Seasonal variations in trace elements and influencing factors in drip water from Kaiyuan Cave, Shandong Province

1.
School of Geography, South China Normal University, Guangzhou 510631, China
2.
Coast institute of Ludong University, Yantai 264025, China

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Received Date: March 27, 2017
Revised Date: May 21, 2018

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Abstract

Abstract

Drip water samples for 15 months were collected from the Kaiyuan Cave, Zibo City of Shandong Province, a cave located in a semi-humid monsoon climatic zone in coastal North China. Geochemical information suggests that: (1) the variations in dripping rates respond rapidly to the atmospheric precipitation outside the cave. (2) Although the Ca²⁺, Mg²⁺, Sr²⁺ and Ba²⁺ concentrations display significant seasonal variations, their behaviors and influencing mechanisms are rather different. (3) The Sr/Ca and Ba/Ca ratios of the drip water may respond to certain degree to the atmospheric precipitation outside of the cave, and, especially, the Mg/Ca, Sr/Ca and Mg/Sr ratios may well indicate heavy rainfall. However, the variations in Mg/Sr in the drip water do not respond obviously to surface air temperature.
- drip water,
- trace elements,
- seasonal variations,
- influencing factors,
- Kaiyuan Cave

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References

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Seasonal variations in trace elements and influencing factors in drip water from Kaiyuan Cave, Shandong Province