[1]黄雨振,陈秀玲*,吕 镔,等.福建北部闽江流域第四纪红土的磁学特征及其环境意义[J].山地学报,2018,(04):527-535.[doi:10.16089/j.cnki.1008-2786.000349]
 HUANG Yuzhen,CHEN Xiuling*,LYU Bin,et al.Magnetic Characteristics of Quaternary Red Earth Sequence from the Minjiang Drainage Basin in Northern Fujian and Its Environmental Significance[J].Mountain Research,2018,(04):527-535.[doi:10.16089/j.cnki.1008-2786.000349]
点击复制

福建北部闽江流域第四纪红土的磁学特征及其环境意义()
分享到:

《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2018年04期
页码:
527-535
栏目:
山地环境
出版日期:
2018-07-30

文章信息/Info

Title:
Magnetic Characteristics of Quaternary Red Earth Sequence from the Minjiang Drainage Basin in Northern Fujian and Its Environmental Significance
文章编号:
1008-2786-(2018)4-527-09
作者:
黄雨振1陈秀玲12*吕 镔12方 红1朱甜英1
1.福建师范大学 地理研究所,福州 350007; 2.湿润亚热带生态-地理过程教育部重点实验室,福州 350007
Author(s):
HUANG Yuzhen1 CHEN Xiuling12* LYU Bin12 FANG Hong1 ZHU Tianying1
1.Institute of Geography, Fujian Normal University, Fuzhou 350007, China; 2.Key Laboratory of Humid Subtropical Ecosystem and Geography, Ministry of Education, Fuzhou 350007, China
关键词:
红土 磁学特征 第四纪 闽江流域
Keywords:
red earth magnetic characteristics Quaternary Minjiang Drainage Basin
分类号:
P318
DOI:
10.16089/j.cnki.1008-2786.000349
文献标志码:
A
摘要:
南方第四纪红土是记录南方古环境信息的良好载体和第四纪古气候环境研究的重要内容。本文对采自福建北部闽江流域大横第四纪红土剖面的样品进行磁化率、等温剩磁、饱和等温剩磁和代表样品的κ-T 曲线等多磁学参数的详细测量和分析,研究结果表明:大横剖面的磁化率范围为8.87~35×10-8 m3·kg-1,饱和等温剩磁范围为51.77×10-5 ~294.51×10-5 Am2·kg-1,总体偏低,说明大横剖面的磁性矿物含量较低,可能是福建北部化学风化作用强烈且温暖湿润的环境导致的; 频率磁化率、非磁滞磁化率及χARM/SIRM比值说明剖面自上而下,磁性矿物颗粒大小总体上呈现变粗趋势,由SP+SD颗粒到SD+MD颗粒的转变,剖面磁性矿物以磁铁矿为主,并含有磁赤铁矿、赤铁矿和纤铁矿等。本文探讨了红土剖面的不同沉积层磁学特征变化及对环境的指示意义,对认识该地区第四纪红土的风化特征及发育环境有一定借鉴意义。
Abstract:
Quaternary red earth sequences in southern China have been generally considered as potential paleoenvironmental records, because they are one of the most important terrestrial sources of information for reconstructing paleoenvironment and paleoclimate at a regional scale.In this research, the environmental magnetism records from a Quaternary red earth sequence of Daheng(DH)section in the Minjiang Drainage Basin were presented.In practice, detailed measurements and analysis of multi-magnetic parameters were performed with focuses of magnetic susceptibility, isothermal remanence, saturated isothermal remanence and κ-T curves of representative samples collected at the Daheng Quaternary red earth section in the Minjiang River Basin of the northern Fujian, China.The magnetic characteristics of different sedimentary layers in the red earth sections and their implications for the local environment were interpreted for understanding of the weathering characteristics and the associated development environment of the Quaternary red earth in this area.Results showed that the magnetic susceptibility ranged between 8.87×10-8 ~ 35×10-8 m3·kg-1, and the saturation isothermal remanence was within a range of 51.77×10-5 ~ 294.51×10-5 Am2·kg-1.Generally, the obtained values were relatively low in extent, suggesting that there was a low magnetic mineral content at the Daheng sections, possibly caused by a strong, warm and humid environment in the northern part of Fujian.And the frequency susceptibility, non-hysteresis magnetic susceptibility and χARM/SIRM ratio indicated that the values of them increased from base to top, suggesting that the particle size of magnetic mineral may exhibited a decreasing trend from base to top.Investigations of the environmental magnetism records revealed that the particle size of magnetic mineral increased from interval SP+SD to that of SD+MD; and the mass of MD magnetic mineral particles was more than others.Moreover, κ-T curves of selected samples indicated that the magnetite was the dominant magnetic mineral in the DH section, with a secondary component of maghemite, hematite, and lepidocrocite.

参考文献/References:

[1] 杨浩,夏应菲,赵其国,等.红土系列剖面的磁化率特征与古气候冷暖变换[J].土壤学报,1995,32(增刊2):195-200 [YANG Hao, XIA Yingfei, ZHAO Qiguo, et al.The character of magnetic susceptibility of red earth profile in South China and paleo-climate changes [J].Acta Pedologica Sinica, 1995, 32(Suppl.2): 195-200]
[2] 卢升高,董瑞斌,俞劲炎,等.中国东部红土的磁性及其环境意义[J].地球物理学报,1999,42(6):764-771 [LU Shenggao, DONG Ruibin, YU Jinyan, et al.Magnetic measurement characterization of red earth profile in eastern China and its environmental implications[J].Chinese Journal Geophysics, 1999, 42(6): 764-771]
[3] 袁大刚,张甘霖.雨花台红土的磁化率特征及其古环境意义[J].土壤,2008,40(1):110-113 [YUANG Dagang, ZHANG Ganlin.Characterization of magnetic susceptibility of red earth at Yuhuatai and its paleoenvironmental implications [J].Soil, 2008, 40(1): 110-113]
[4] 胡雪峰,程天凡,巫和昕.南方网纹红土内是否可能存在多个“沉积-成土”过程的旋回?[J].科学通报,2003,48(9):969-975 [HU Xuefeng, CHENG Tianfan, WU Hexin.Do multiple cycles of Aeolian deposit pedogenesis exist in the reticulate red clay sections in southern China? [J].Chinese Science Bulletin, 2003, 48(9): 969-975]
[5] 朱丽东,姜永见,张明强,等.庐山JL剖面红土磁化率特征及古环境记录[J].山地学报, 2001,29(4):385-394 [ZHU Lidong, JIANG Yongjian, ZHANG Mingqiang, et al.Characteristics of magnetic susceptibility and its paleoenvironmental records from JL red earth section, Lushan area [J].Mountain Research, 2001, 29(4): 385-394]
[6] 邓黄月,郑祥民,杨立辉,等.长江中下游地区第四纪红土磁学特征及其环境意义[J].沉积学报,2015,33(2):285-298 [DENG Huangyue, ZHENG Xiangmin, YANG Lihui, et al.Magnetic properties of quaternary red earth profile in Yangtze River Valley and its paleoenvironmental implications[J].Acta Sedimentologica Sinica, 2015, 33(2): 285-298]
[7] OLDFIELD F.Environmental magnetism-A personal perspective [J].Quaternary Science Reviews, 1991, 10(1): 73-85
[8] MAHER B A.Characterization of soils by mineral magnetic measurements [J].Physics of the Earth & Planetary Interiors, 1986, 42(1-2): 76-92
[9] THOMPSON R, OLDFIELD F.Environmental magnetism [M].London: Allen and Unwin, 1986: 758-759
[10] 曲赞.用于环境研究的磁性参数简介[J].地质科技情报,1994,13(2):98-104 [QU Zan.An introduction of magnetic parameters in environmental studies [J].Geological Science & Technology Information, 1994, 13(2): 98-104]
[11] 符超峰,宋友桂,强小科,等.环境磁学在古气候环境研究的回顾与展望[J].地球科学与环境学报,2009,31(9):312-322 [FU Chaofeng, SONG Yougui, QIANG Xiaoke, et al.Environmental magnetism and its application progress in paleoclimatic and paleoenvironmental changes [J].Journal of Earth Sciences & Environment, 2009, 31(9): 312-322]
[12] MAHER B A.Magnetic properties of some synthetic sub-micron magnetities [J].Geophysical Journal Royal Astronomical Society, 1988, 94(1): 83-96
[13] 刘秀铭,马明明,P.Hesse,等.澳大利亚黄土磁学性质及环境意义[J].第四纪研究,2011,31(5):837-848 [LIU Xiuming, MA Mingming, P.Hesse, et al.Magnetic properties of loess deposit in Australia and its environmental significances [J].Quaternary Sciences, 2011, 31(5): 837-848]
[14] BLOEMENDAL J, LIU X M.Rock magnetism and geochemistry of two plio-pleistocene Chinese loess-palaeosol sequences-implications for quantitative paleoprecipitation reconstruction [J].Paleogeography Paleoclimatalogy Paleocology, 2005, 226(1-2): 149-166
[15] 刘青松,邓成龙,潘永信.磁铁矿和磁赤铁矿磁化率的温度和频率特性及其环境磁学的意义[J].第四纪研究,2007,27(6):955-962 [LIU Qingsong, DENG Chenglong, PAN Yongxin.Temperature-dependency and frequency-dependency of magnetic susceptibility of magnetite and maghemite and their significance for environmental magnetism [J].Quaternary Sciences, 2007, 27(6): 955-962]
[16] FINE P, SINGER M J.Contribution of ferromagnetic minerals to oxalate and dithionite extractable iron [J].Soil Society of America Journal, 1989, 53(1): 191-196
[17] 胡忠行,朱丽东,张卫国,等.江西九庐公路红土剖面的磁学特征及其反映的风化成土作用[J].地球物理学报,2011,54(5):1319-1326 [HU Zhongxing, ZHU Lidong, ZHANG Weiguo, et al.Magnetic properties of red clay section along the Jiu-Lu highway at Jiujiang, Jiangxi and implications for pedogenesis [J].Chinese Journal Geophysics, 2011, 54(5): 1319-1326]
[18] 卢升高.中国土壤磁性与环境[M].北京:高等教育出版社,2003: 189-190 [LU Shenggao.Magnetism of Soils in China and Its Environment Implication [M].Beijing: Higher Education Press, 2003: 189-190]
[19] 卢升高.中国南方红土环境磁学[J].第四纪研究,2007,27(6):1016-1022 [LU Shenggao.Environmental magnetism of Quaternary red Earth in the southern China [J].Quaternary Sciences, 2007, 27(6): 1016-1022]
[20] 吕厚远,韩家懋,吴乃琴,等.中国现代土壤磁化率分析及其古气候意义[J].中国科学(B辑),1994,24(12):1290-1297 [LV Houyuan, HAN Jiamao, WU Naiqin, et al.Analysis on magnetism and paleoclimate meaning in modern soil of China [J].Science in China(Series B), 1994, 24(12): 1290-1297]
[21] ÖZDEN Özdemir, DUNLOP D J.Thermoremanence and Néel temperature of goethite [J].Geophysical Research Letters, 1996, 23(9): 921-924
[22] XIONG S F, SUN D H, DING Z L.Aeolian origin of the red earth in southeast China [J].Journal of Quaternary Science, 2002, 17(2): 181-191
[23] ZHANG W G, YU L Z, LU M, et al.Magnetic properties and geochemistry of the Xiashu Loess in the present subtropical area of China, and their implications for pedogenic intensity [J].Earth & Planetary Science Letters, 2007, 260(1): 86-97
[24] DING Z L, YANG S L, SUN J M, et al.Iron geochemistry of loess and red clay deposits in the Chinese Loess Plateau and implications for long-term Asian Monsoon evolution in the last 7.0 Ma [J].Earth and Planetary Science Letters, 2001, 185(1/2): 99-109
[25] SCHWERTMANN U, FISCHER W, PAPENDORF H.The influence of organic compounds on the formation of iron oxides [C].Transaction of the Ninth International Congress of Soil Science, Sydey: International Society of soil Science and Angus and Robertson, 1968, 645-655
[26] 张家铭,王明光.台湾红壤及森林土壤中之氧化铁[J].土壤学报, 1995, 32(1):15-22 [ZHANG Jiaming, WANG Mingguang.Iron oxides distributed in red and forest soils of Taiwan [J].Acta Pedologica Sinica, 1995, 32(1): 15-22]

相似文献/References:

[1]冯志刚,王世杰.中国南方红土古环境重建中存在的几个问题[J].山地学报,2003,(06):641.
[2]靳建辉,李志忠.44ka以来福州盆地红土的沉积地球化学特征[J].山地学报,2016,(06):690.[doi:10.16089/j.cnki.1008-2786.000175]
 JIN Jianhui,LI Zhizhong.Geochemistry Characteristics of Red Earth Sedimentation since 44ka in Fuzhou Intermountane Basin[J].Mountain Research,2016,(04):690.[doi:10.16089/j.cnki.1008-2786.000175]
[3]张祖莲,洪 斌,黄 英,等.降雨作用下红土型坡面径流特性与土壤侵蚀的关系研究[J].山地学报,2017,(04):535.[doi:10.16089/j.cnki.1008-2786.000251]
 ZHANG Zulian,HONG Bin,HUANG Ying,et al.Study on Relationship between Runoff Characteristics and Soil Erosion of Laterite Slope under Rainfall[J].Mountain Research,2017,(04):535.[doi:10.16089/j.cnki.1008-2786.000251]
[4]张祖莲,梁谏杰,黄 英,等.干湿循环作用下云南红土特性与库岸边坡稳定性关系研究[J].山地学报,2018,(02):280.[doi:10.16089/j.cnki.1008-2786.000323]
 ZHANG Zulian,LIANG Jianjie,HUANG Ying,et al.On the Relationship between Characteristics of Yunnan Laterite and Stability of the Bank Slope under Wetting-Drying Cycles[J].Mountain Research,2018,(04):280.[doi:10.16089/j.cnki.1008-2786.000323]
[5]张祖莲,梁谏杰,黄 英,等.库岸边坡倾角及水位变化对红土型库岸稳定性影响研究[J].山地学报,2019,(01):62.[doi:10.16089/j.cnki.1008-2786.000399]
 ZHANG Zulian,LIANG Jianjie,HUANG Ying,et al.Investigation of the Influence of Slope Inclination and Water Level Fluctuation on the Stability of Laterite Reservoir Bank[J].Mountain Research,2019,(04):62.[doi:10.16089/j.cnki.1008-2786.000399]
[6]梁谏杰,张祖莲*,黄 英,等.干湿循环作用下加砂对红土抗剪强度及微结构特性的影响[J].山地学报,2019,(6):848.[doi:10.16089/j.cnki.1008-2786.000475]
 LIANG Jianjie,ZHANG Zulian*,HUANG Ying,et al.Effect of Sand Adding on Shear Strength and Microstructure Characteristics of Laterite under Dry-Wet Cycling Condition[J].Mountain Research,2019,(04):848.[doi:10.16089/j.cnki.1008-2786.000475]

备注/Memo

备注/Memo:
收稿日期(Received date):2017-09-22; 改回日期(Accepted date):2018-05-24
基金项目(Foundation item):福建省自然科学基金(2014J01151); 福建省公益类科研院所基本科研专项项目(2014R1034-2)。[Natural Science Foundation of Fujian Province, China(2014J01151); Fundamental Scientific Research Activities at the Non-profit Research Institutions in Fujian Province, China(2014R1034-2)]
第一作者(Biography):黄雨振(1992-),男,福建莆田人,硕士研究生,主要研究方向:全球变化与第四纪。 [HUANG Yuzhen(1992-), male, born in Putian, Fujian province, M.Sc.candidate, research on global change and quaternary] E-mail: 1204455283@qq.com
*通讯作者(Corresponding author):陈秀玲(1978-),女,博士,副教授,主要研究方向:第四纪环境演变与人类对策。[CHEN Xiuling(1978-), female, Ph.D, associate professor, research on quaternary environmental evolution and human countermeasures] E-mail: xiulingchen@163.com
更新日期/Last Update: 2018-07-30