Grain-size Characteristics and Environmental Significance of Peat Ash in the West Foothill of Changbai Mountain

LI Nan-nan; JIE Dong-mei; YANG Jin-xiu; CHEN Xue-song; CHEN Yu-jie; HU Chu-tian; QIAO Zhi-he

Article Contents

Article Navigation > Acta Sedimentologica Sinica > 2014 > 32(5): 873-883

LI Nan-nan, JIE Dong-mei, YANG Jin-xiu, CHEN Xue-song, CHEN Yu-jie, HU Chu-tian, QIAO Zhi-he. Grain-size Characteristics and Environmental Significance of Peat Ash in the West Foothill of Changbai Mountain[J]. Acta Sedimentologica Sinica, 2014, 32(5): 873-883.

Citation:

Grain-size Characteristics and Environmental Significance of Peat Ash in the West Foothill of Changbai Mountain

1.
School of Geographical Science, Northeast Normal University, Changchun 130024;
2.
Key Laboratory for Wetland Ecology and Vegetation Restoration, Ministry of Environmental Protection, Changchun 130024;
3.
Daqing Normal University, Daqing, Heilongjiang 163712

Received Date: 2013-07-15
Rev Recd Date: 2013-11-28
Publish Date: 2014-10-10

Abstract

In order to recognize the provenances, granularity characteristics of peat ash, and further reveal the paleo-enviromental significance of peat ash. Two peat cores in Hani and Gushantun Peat-land in the west foothill of Changbai Mountain are collected. The results of grain size analysis show that the dominant size of peat ash is 1~350 μm. Which means peat ash is mainly composed of different kinds of silt. What is more, the majority probability cumulative curves for particle size distribution are with two sections. At the same time, frequency distribution curves show unimodal type (10~100 μm), bimodal type (10~100 μm, 100~1 000 μm). These show that the transportation ways of peat ash is suspension and saltation. And the grain sizes changed with the hydrologic condition in the peat land. In the dry season, the water power is weak and the peat ash content is relatively fine. But in the wet season, surface runoff carries the coarse particle into the swamp and deposits. Therefore, the peat ash can be used for rebuilding the evolution of paleo-precipitation and it can be a proxy for the summer monsoon. In addition, 9.2 ka, 8ka and 5ka drought events in Holocene are recognized from the grain size changing curve and the curve also reveals a "dry-wet-dry" cycle in the precipitation history. Because these events correspond to the famous cold events, so we may draw the conclusion that dry and cold, warm and wet may be matched in the process of climate change.
- Changbai Mountain area,
- peat,
- grain-size,
- sedimentary facies,
- summer monsoon

References

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Grain-size Characteristics and Environmental Significance of Peat Ash in the West Foothill of Changbai Mountain

1. School of Geographical Science, Northeast Normal University, Changchun 130024;

2. Key Laboratory for Wetland Ecology and Vegetation Restoration, Ministry of Environmental Protection, Changchun 130024;

3. Daqing Normal University, Daqing, Heilongjiang 163712

Received Date: 2013-07-15

Rev Recd Date: 2013-11-28

Publish Date: 2014-10-10

Key words:

Abstract: In order to recognize the provenances, granularity characteristics of peat ash, and further reveal the paleo-enviromental significance of peat ash. Two peat cores in Hani and Gushantun Peat-land in the west foothill of Changbai Mountain are collected. The results of grain size analysis show that the dominant size of peat ash is 1~350 μm. Which means peat ash is mainly composed of different kinds of silt. What is more, the majority probability cumulative curves for particle size distribution are with two sections. At the same time, frequency distribution curves show unimodal type (10~100 μm), bimodal type (10~100 μm, 100~1 000 μm). These show that the transportation ways of peat ash is suspension and saltation. And the grain sizes changed with the hydrologic condition in the peat land. In the dry season, the water power is weak and the peat ash content is relatively fine. But in the wet season, surface runoff carries the coarse particle into the swamp and deposits. Therefore, the peat ash can be used for rebuilding the evolution of paleo-precipitation and it can be a proxy for the summer monsoon. In addition, 9.2 ka, 8ka and 5ka drought events in Holocene are recognized from the grain size changing curve and the curve also reveals a "dry-wet-dry" cycle in the precipitation history. Because these events correspond to the famous cold events, so we may draw the conclusion that dry and cold, warm and wet may be matched in the process of climate change.

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Reference (40)

[1]	刘东生, 等. 黄土与环境[M]. 北京:科学出版社, 1985[Liu Tungsheng, et al. Loess and Environment[M]. Beijing: Science Press, 1985]
[2]	胡邦琦, 杨作升, 赵美训, 等. 南黄海中部泥质区7200 年以来东亚冬季风变化的沉积记录[J]. 中国科学(D辑):地球科学, 2012, 42(10):1568-1581[Hu Bangqi, Yang Zuosheng, Zhao Meixun, et al. Grain size records reveal variability of the East Asian Winter Monsoon since the Middle Holocene in the Central Yellow Sea mud area[J]. China Science(Seri. D): Earth Science, 2012, 42(10): 1568-1581]
[3]	张洪岩, 王锡魁, 隋维国, 等. 图们江河口沼泽沉积物的粒度特征及碎屑源分析[J]. 世界地质, 2006, 25(2):147-159[Zhang Hongyan, Wang Xikui, Sui Weiguo, et al. Analysis on grain-size characteristics and fragment sources of deposits in swamps near debouchment of Tumen River[J]. Global Geology, 2006, 25(2): 147-159]
[4]	郑国璋, 岳乐平, 何军锋, 等. 疏勒河下游安西古沼泽全新世沉积物粒度特征及其古气候环境意义[J]. 沉积学报, 2006, 24(5):733-739[Zheng Guozhang, Yue Leping, He Junfeng, et al. Grain-size characteristics of the sediments at palaeoswamp in Anxi County in downstream of Shulehe River during Holocene and its paleoclimatic significance[J]. Acta Sedimentologica Sinica, 2006, 24(5): 733-739]
[5]	王心源, 张广胜, 张恩楼, 等. 巢湖湖泊沉积记录的早-中全新世环境演化研究[J]. 科学通报, 2008, 53(增刊Ⅰ):132-138[Wang Xinyuan, Zhang Guangsheng, Zhang Enlou, et al. Research on early-middle Holocene environment evolution from the records of sediment in Chaohu Lake[J]. Chinese Science Bulletin, 2008, 53(Suppl.Ⅰ): 132-138]
[6]	殷书柏, 吕宪国. "泥炭气候成因说"的探讨[J]. 地理科学, 2006, 26(3):321-326[Yin Shubai, Lü Xianguo. Discussion on "the theory on climate cause of peat forming"[J]. Scientia Geographica Sinica, 2006, 26(3): 321-326]
[7]	赵红艳, 冷雪天, 王升忠. 长白山地泥炭分布、沉积速率与全新世气候变化[J]. 山地学报, 2002, 20:513-518[Zhao Hongyan, Leng Xuetian, Wang Shengzhong. Distribution, accumulation rate of peat in the Changbaishan Mountains and climate change in Holocene[J]. Journal of Mountain Science, 2002, 20: 513-518]
[8]	刘金陵. 长白山区孤山屯沼泽地13000年以来的植被和气候变化[J]. 古生物学报, 1989, 28:495-509[Liu Jinling. Vegetational and climatic changes at Gushantun Bog in Jilin, NE China Since 13, 000 Y.B.P[J]. Acta Palaeontologica Sinica, 1989, 28: 495-509]
[9]	李荣麟, 介冬梅, 刘艳萍, 等. 东北长白山区北部虎山泥炭剖面植硅体的环境指示意义[J]. 微体古生物学报, 2011, 28:329-336[Li Ronglin, Jie Dongmei, Liu Yanpin, et al. Phytolith as an environment indicator of Hushan peat section from northern region in Changbai Mountain[J]. Acta Micropalaeontologica Sinica, 2011, 28: 329-336]
[10]	王金权, 刘金陵. 长白山区全新世大暖期的氨基酸和碳同位素记录[J]. 微体古生物学报, 2001, 18:392-398[Wang Jinquan, Liu Jinling. The records of amino acids and organic carbon isotope for Holocene megathermal in Changbaishan area[J]. Acta Micropalaeontologica Sinica, 2001, 18: 392-398]
[11]	李鸿凯, 卜兆君, 王升忠, 等. 长白山区泥炭地现代有壳变形虫环境意义探讨[J]. 第四纪研究, 2009, 29(4):817-824[Li Hongkai, Bu Zhaojun, Wang Shengzhong, et al. Environmental implications of the modern testate amoebae in the peatlands in Changbai Mountains[J]. Quaternary Sciences, 2009, 29(4): 817-824]
[12]	洪冰, 刘丛强, 林庆华, 等. 哈尼泥炭δ¹⁸O记录的过去14000年温度演变[J]. 中国科学(D 辑):地球科学, 2009, 39:626-637[Hong Bing, Liu Congqiang, Lin Qinghua, et al. Temperature evolution from the δ¹⁸O record of Hani peat, Northeast China, in the last 14000 years[J]. Science China(Seri. D): Earth Science, 2009, 39: 626-637]
[13]	Stuiver M, and Reimer, P J. Extended ¹⁴C database and revised CALIB radiocarbon calibration program[J]. Radiocarbon, 1993, 35: 215-230
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Grain-size Characteristics and Environmental Significance of Peat Ash in the West Foothill of Changbai Mountain

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