东北哈尼泥炭沼泽中酚酸的组成、酚铁相互作用及其环境意义

邬钰; 向武; 傅先芳; 李启立; 苏靖; 龚文; 王翰

doi:10.3799/dqkx.2016.057

Volume 41 Issue 4

Apr. 2016

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Article Navigation > Earth Science > 2016 > 41(4): 683-691

Wu Yu, Xiang Wu, Fu Xianfang, Li Qili, Su Jing, Gong Wen, Wang Han, 2016. Effect of Phenolic Acids Derived from Peatland on Surface Behavior of Iron and Its Significance:A Case Study in Hani Peatland. Earth Science, 41(4): 683-691. doi: 10.3799/dqkx.2016.057

Citation:

Wu Yu, Xiang Wu, Fu Xianfang, Li Qili, Su Jing, Gong Wen, Wang Han, 2016. Effect of Phenolic Acids Derived from Peatland on Surface Behavior of Iron and Its Significance:A Case Study in Hani Peatland. Earth Science, 41(4): 683-691. doi: 10.3799/dqkx.2016.057

Citation:

Wu Yu, Xiang Wu, Fu Xianfang, Li Qili, Su Jing, Gong Wen, Wang Han, 2016. Effect of Phenolic Acids Derived from Peatland on Surface Behavior of Iron and Its Significance:A Case Study in Hani Peatland. Earth Science, 41(4): 683-691. doi: 10.3799/dqkx.2016.057

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Effect of Phenolic Acids Derived from Peatland on Surface Behavior of Iron and Its Significance:A Case Study in Hani Peatland

doi: 10.3799/dqkx.2016.057

Wu Yu^1
,,
Xiang Wu^{1,2
,
,},
Fu Xianfang¹,
Li Qili¹,
Su Jing¹,
Gong Wen¹,
Wang Han¹

1.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China

Received Date: 2015-09-16
Publish Date: 2016-04-15

Abstract

Abstract

The influence of dissolved organic matters as metal chelators on the bio-available iron input to the ocean has been widely reported by several studies. However, natural dissolved organic matters, especially the phenolics originated from peatlands and geochemical interactions with iron remains poorly understood. Hani peatland, as the national nature reserve in Jilin Province, is located in the central Longgang Mountain on the west side of Changbai Mountains. Physiochemical characteristics of water samples collected from rivers in Hani, including total dissolved iron, ferrous iron, dissolved organic carbon and pH etc., were detected in the field. Inner connections of these indexes were demonstrated through multivariate statistical analysis and simulation experiments on geochemical interactions between iron and phenolic acids were conducted in laboratory. Results show that total dissolved phenol plays an important role in the existence and transportation of ferrous iron. Ten phenolic acid, including protocatechuic acid, caffeic acid, gallic acid, gentisic acid, syringic acid, ferulic acid, p-hydroxybenzoic acid, p-coumaric acid, salicylic acid and vanillic acid, were detected by high performance liquid chromatography. Simulation experiments reveal that phenolics bearing either catechol or galloyl moiety groups (protocatechuic acid, caffeic acid and galllic acid) could chelate ferrous iron, which is the geochemical cause of high concentration of dissolved iron and is crucial for iron transport in peatland. Reducing action of phenolics to Fe(Ⅲ) is also responsible for maintaining high concentration of Fe(Ⅱ) and Fe(Ⅲ) in rivers drained from peatland. Considering the wide distribution of peatlands globally, the higher concentration of Fe in peatlands, and the enhancement of marine organisms by Fe, the complexation and reductive actions between iron and phenolics originated from peatlands are of important significance to global iron cycle coupled with other element cycles, such as carbon and sulfur, which can significantly influence global ecological balance.
- Hani,
- peatland,
- phenolic acid,
- iron,
- environmental geology,
- geochemistry

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References(50)

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