长江与黄河河口沉积物磁性特征对比的初步研究

王永红; 沈焕庭; 张卫国

长江与黄河河口沉积物磁性特征对比的初步研究

1.
中国海洋大学海洋地球科学学院山东青岛 266003;
2.
华东师范大学河口海岸国家重点实验室上海 200062

基金项目: 国家自然科学基金课题(批准号:40406015)资助;“引进人才科研启动”基金课题资助;“973”项目“中国典型河口—近海陆海相互作用及其环境效应”(课题编号:2002CB412408)资助

详细信息

作者简介:
王永红女 1969年出生副教授博士河口海岸动力沉积环境

中图分类号: P734.6

计量

文章访问数: 581
HTML全文浏览量: 1
PDF下载量: 941
被引次数: 0

A Preliminary Comparison of Magnetic Properties of Sediments from the Changjiang and the Huanghe Estuaries

1.
Ocean University of China, College of Marine Geosciences, Qingdao,Shandong 266003;
2.
East China Normal University, State Key Laboratory of Estuarine and Coastal Research, Shanghai 200062

摘要

摘要: 根据2001年8月和9月分别采自黄河与长江河口沉积物样品的磁性测量和粒度分析,探讨长江和黄河河口沉积物的磁性特征及其差异。长江河口沉积物中亚铁磁性物质的含量高于黄河口,但长江口与黄河口沉积物中都是亚铁磁性矿物主导了样品磁性特征,亚铁磁性矿物晶粒都以假单畴-多畴为主。相比黄河口沉积物,长江口沉积物不完整反铁磁性物质对磁性特征的的贡献较小。长江与黄河河口的这种磁性特征主要反映了不同的沉积物来源的控制影响。此外,无论是长江口还是黄河口沉积物,磁性参数χARM、χfd%与沉积物细粒级组分存在显著的相关性,表明这两个参数作为粒度的代用指标具有普遍性。
- 磁性特征 /
- 长江 /
- 黄河 /
- 河口沉积物
Abstract: Magnetic properties of sediments from the Changjiang and the Huanghe Estuaries have been studied on the basis of magnetic measurement and grain size analysis. The results show that the magnetic properties of the sediments are dominated by ferrimagnetic magnetite, and higher concentration of ferrimagnetic minerals is observed for the Changjiang Estuary sediments. The pseudo single domain and multi domain particles are the main carriers of the ferrimagetic magnetite of the sediments in the Changjiang and Huanghe Estuaries, and single domain and superparamagnetic particles are also present in the sediments with higher concentration occuring in the Changjiang Estuary. The magnetic properties of sediments from the Changjiang and the Huanghe Estuaries suggested that the provenance of sediments controlled the magnetic features. At the same time, obvious correlation exists between χ ARM、 χ fd % and fine particles of the sediments in the Changjiang and Huanghe estuaries.
- magnetism /
- Changjiang River /
- Huanghe River /
- estuarine sediment

HTML全文

参考文献(22)

[1]	秦蕴珊,赵一阳,陈丽荣. 黄海地质. 北京:地质出版社,1989 [Qin Yunshan, Zhao Yiyang, Chen Lirong. Geology of the Yellow Sea. Beijing: Geological Publishing House, 1989]
[2]	王腊春,陈晓玲,储同庆黄河、长江泥沙特性对比分析. 地理研究, 1997,16(4):71～79[Wang Lachun, Chen Xiaoling, Chu Tongqing. A contrast analysis on the load character of the Changjiang river and the Yellow river . Geographical Research, 1997, 16(4):71～79]
[3]	Wang Xueye and Xiankun Ke. Grain size characteristics of the extant tidal flat sediments along the Jiangsu coast, China. Sedimentary Geology, 1997, 112/1-2:105～122
[4]	孙白云. 黄河、长江、珠江三角洲沉积物中碎屑矿物的组合特征. 海洋地质与第四纪地质, 1990,10(3):23～34[Sun Beiyun. Detrital mineral assemblages in the Huanghe, Changjiang and Zhujiang River delta sediments. Marine Geology & Quaternary Geology,1990,10(3):23～34]
[5]	杨作升. 黄河、长江、珠江沉积物中粘土矿物组合、化学特征及其与物源区气候环境的关系. 海洋与湖沼, 1988,19(4):336～346 [Yang Zuosheng. Mineralogical assemblages and chemical characteristics of clays from sediments of the Huanghe, Changjiang, Zhujiang Rives and their relationship to the climate environment in their sediment source areas. Oceanologia et Limnologia Sinica, 1988, 19(4): 336～346]
[6]	范德江,李广雪,郭志刚, 等. 黄河入海过程中粘土矿物的沉积作用. 海洋与湖沼, 1997,28(增刊):116～122 [Fan Dejiang, Li Guangxue, Guo Zhigang, et al. Sedimentation of clay minerals during the Huanghe input sea. Oceanologia et Limnologia Sinica, 1997,28 (Suppl.):116～122]
[7]	杨守业,李从先,朱金初. 长江与黄河沉积物中磁铁矿成分标型意义. 地球化学. 2000,29(5):480～484 [Yang Shaoye, Li Congxian, Zhujinchu. Provenance indicator of chemical fingerprint of magnetite from the Yangtze River and the Yellow River sediments. Geochimica,2000,29(5):480～484]
[8]	赵一阳,鄢明才. 黄河、长江、中国浅海沉积物化学元素丰度比较. 科学通报,1992,37(13):1202～1204 [Zhao Yiyang, Yan Mingcai. Compare among the element abundance of sediments from the Huanghe, Changjiang and Chinese shallow sea. Chinese Science Bulletin, 1992,37(13):1202～1204]
[9]	杨守业,李从先. 长江与黄河沉积物REE地球化学及示踪作用. 地球化学, 1999,28(4):374～380 [Yang Shouye, Li Congxian. REE geochemistry and tracing application in the Yangtze River and the Yellow River sediments. Geochimica, 1999,28(4):374～380]
[10]	杨守业,李从先. 长江与黄河沉积物元素组成及地质背景. 海洋地质与第四纪地质,1999,19(2):19～25[Yang Shouye, Li Congxian. Characteristic element compositions of the Yangtze and the Yellow River sediments and their geological background. Marine Geology & Quaternary Geology, 1999,19(2):19～25]
[11]	范德江,杨作升,王文正. 长江、黄河沉积物中碳酸盐组成及差异. 自然科学进展, 2002,12(1): 60～64 [Fan Dejiang, Yang Zuosheng, Wang Wenzheng. Compositions and differences of carbonate in the sediments of the Changjiang river and the Huanghe River. Advance of Natural Science, 2002,12(1): 60～64]
[12]	毛登,范德江,郭志刚. 长江、黄河河口沉积物中生物标志化合物组成的初步分析. 青岛海洋大学学报, 2001, 31(5):747～754 [Mao Deng, Fan Dejiang, Guo Zhigang. Preliminary study on Biomarker in surface sediments from mouths of the Changjiang River and the Huanghe River. Journal of Ocean University of Qingdao, 2001, 31(5):747～754]
[13]	Wright L D, Nittrouer C A. Dispersal of river sediments in coastal seas: six contrasting cases. Estuaries, 1996, 18(3): 494～508
[14]	Oldfield F. Environmental magnetism - a personal perspective. Quaternary Science Research, 1991,10:73～85
[15]	Oldfield F, Yu L. The influence of particle size variations on the magnetic properties of sediments from the northeastern Irish Sea. Sedimentology, 1994,41:1093～1108
[16]	Maher B A. Magnetic properties of some synthetic sub-micromagnetites. Geophysical Journal. 1988, 94:83～96
[17]	Zhang Weiguo, Lizhong Yu, Hutchinson S M. Diagenesis of magnetic minerals in the intertidal sediments of the Yangtze Estuary, China, and its environmental significance . The Science of the Total Environment 2001, 266:169～175
[18]	王建,刘泽纯,姜文英, 等. 磁化率与粒度、矿物学的关系及其古环境意义. 地理学报,1996,51(2):155～163 [Wang Jian, Liu Zechun, Jiang Wenying, et al. A relationship between susceptibility and grain size and minerals and their paleo-environmental implications. Acta Geographica Sinica., 1996,51(2):155～163]
[19]	Clifton J, McDonald P, Plater A, et al. Deviation of a grain size proxy to aid the modeling and prediction of radionuclide activity in salt marshes and mud flats of the Eastern Irish Sea. Estuaries, Coastal and Shelf Science, 1999, 48:511～518
[20]	Oldfield F. Toward the discrimination of fine-grained ferrimagnets by magnetic measurement in lake and nearshore marine sediments. Journal of Geophysical Research, 1994, 99: 9045～9050
[21]	贾玉连,柯贤坤,王艳, 等. 渤海曹妃甸沙坝-泻湖海岸现代沉积的磁化率与粒度、矿物的关系. 海洋通报,2000,19(1):41～50 [Jia Yulian, Ke Xiankun, Wang Yan. Sedimentary characteristics of Caofeidian sand bar-lagoon system. Marine Science Bulletin, 2000,19(1):41～50]
[22]	杨小强,李华梅. 泥河湾盆地沉积物粒度组分与磁化率变化相关性研究. 沉积学报, 2002, 20(4): 675 ～ 679 [Yang Xiaoqiang, Li Huamei. The Correlation between the Content of the Different Grain Size and Magnetic Susceptibility in Lacustrine Sediments, Nihewan Basin. Acta Sedimentologica Sinica, 2002, 20 (4) : 675～679]

[1]	倪和平, 毕磊, 郭玉龙, 何中发, 杨守业. 长江口沉积物化学相态分析及主泓变迁的指示 . 沉积学报, 2023, 41(1): 243-255. doi: 10.14027/j.issn.1000-0550.2021.084
[2]	林旭, 陈济鑫, 吴中海, 刘海金, 张洋. 现代河流碎屑磷灰石原位地球化学分析——对长江物源示踪研究的启示 . 沉积学报, 2022, 40(4): 861-870. doi: 10.14027/j.issn.1000-0550.2021.103
[3]	成沁梓, 王峰, 陈锦, 葛灿, 赵旋琪, 陈莹璐, 年小美, 张卫国, 陈中原, Kam⁃biuLIU. 长江水下三角洲沉积物磁性特征空间差异及其冲淤指示意义 . 沉积学报, 2020, 38(6): 1215-1225. doi: 10.14027/j.issn.1000-0550.2019.119
[4]	李富强, 高红山, 张连科, 李宗盟, 庞红丽, 潘保田. 基于粒度参数特征对黄河后套平原段岩芯沉积环境的分析 . 沉积学报, 2019, 37(6): 1234-1243. doi: 10.14027/j.issn.1000-0550.2019.004
[5]	白雪莘, 张卫国, 董艳, 潘大东, 王张华, 孙千里, 陈静, 陈中原, 刘晋嫣. 长江三角洲全新世地层中潮滩沉积磁性特征及其古环境意义 . 沉积学报, 2016, 34(6): 1165-1175. doi: 10.14027/j.cnki.cjxb.2016.06.014
[6]	. 基于磁学和粒度参数的黄河三角洲刁口叶瓣地区全新世以来的地层演化 . 沉积学报, 2014, 32(3): 518-526.
[7]	. 长江上游水系沉积物锶—钕同位素组成及物源示踪 . 沉积学报, 2014, 32(2): 290-295.
[8]	. 黄河银川平原段河床沉积速率变化特征 . 沉积学报, 2012, 30(3): 565-571.
[9]	乔淑卿. 黄河口及邻近渤海海域悬浮体和沉积物中有机碳、氮的分布特征及其影响因素 . 沉积学报, 2011, 29(2): 354-362.
[10]	何梦颖. 长江流域沉积物黏土矿物组合特征及物源指示意义 . 沉积学报, 2011, 29(3): 544-551.
[11]	付苗苗. 苏州澄湖湖底硬粘土粒度特征及成因初探 . 沉积学报, 2008, 26(5): 828-832.
[12]	樊庆云. 南海湖沉积物重金属形态分布及其对水质影响的研究 . 沉积学报, 2007, 25(4): 612-618.
[13]	邢云. 潮滩表层沉积物磁性特征的季节性变化及其对沉积动力作用的响应：以杭州湾北岸为例 . 沉积学报, 2007, 25(2): 267-273.
[14]	. 长江水系沉积物碎屑矿物组成及其示踪意义 . 沉积学报, 2006, 24(4): 570-578.
[15]	张珂, 刘开瑜, 吴加敏, 杨景春, 蔡剑波. 宁夏中卫盆地的沉积特征及其所反映的新构造运动 . 沉积学报, 2004, 22(3): 465-473.
[16]	王洪宝, 钟建华, 王书宝. 黄河三角洲平原上的气胀构造特征、成因及意义 . 沉积学报, 2003, 21(4): 571-578.
[17]	何江, 李朝生, 王新伟, 孙卫国, 米娜. 多离子体系中黄河沉积物对重金属的竞争吸附研究 . 沉积学报, 2003, 21(3): 500-505.
[18]	张卫国, 俞立中, 丛友滋. 赤道东太平洋C—C区硅质沉积物的磁性特征及细菌合成磁铁矿 . 沉积学报, 2003, 21(3): 467-472.
[19]	韩晓非, 张卫国, 陈满荣, 俞立中. 长江口潮滩植物对沉积物铁的地球化学循环及磁性特征的影响 . 沉积学报, 2003, 21(3): 495-499.
[20]	孙景耀, 陈辉军, 朱明春. 黄河济南以下河段某些异常地质作用及几种典型沉积构造研究 . 沉积学报, 2001, 19(1): 79-84.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 581
HTML全文浏览量: 1
PDF下载量: 941
被引次数: 0

姓名
邮箱
手机号码
标题
留言内容
验证码

留言板

长江与黄河河口沉积物磁性特征对比的初步研究

作者简介:
王永红女 1969年出生副教授博士河口海岸动力沉积环境

计量

A Preliminary Comparison of Magnetic Properties of Sediments from the Changjiang and the Huanghe Estuaries

计量

目录

长江与黄河河口沉积物磁性特征对比的初步研究

1. 中国海洋大学海洋地球科学学院山东青岛 266003;

2. 华东师范大学河口海岸国家重点实验室上海 200062

作者简介:
王永红女 1969年出生副教授博士河口海岸动力沉积环境

English Abstract

A Preliminary Comparison of Magnetic Properties of Sediments from the Changjiang and the Huanghe Estuaries

1. Ocean University of China, College of Marine Geosciences, Qingdao,Shandong 266003;

2. East China Normal University, State Key Laboratory of Estuarine and Coastal Research, Shanghai 200062

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

长江与黄河河口沉积物磁性特征对比的初步研究

作者简介: 王永红 女 1969年出生 副教授 博士 河口海岸动力沉积环境

计量

出版历程

A Preliminary Comparison of Magnetic Properties of Sediments from the Changjiang and the Huanghe Estuaries

计量

出版历程

目录

长江与黄河河口沉积物磁性特征对比的初步研究

1. 中国海洋大学海洋地球科学学院 山东青岛 266003; 2. 华东师范大学河口海岸国家重点实验室 上海 200062

作者简介: 王永红 女 1969年出生 副教授 博士 河口海岸动力沉积环境

English Abstract

A Preliminary Comparison of Magnetic Properties of Sediments from the Changjiang and the Huanghe Estuaries

1. Ocean University of China, College of Marine Geosciences, Qingdao,Shandong 266003; 2. East China Normal University, State Key Laboratory of Estuarine and Coastal Research, Shanghai 200062

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
王永红女 1969年出生副教授博士河口海岸动力沉积环境

1. 中国海洋大学海洋地球科学学院山东青岛 266003;

2. 华东师范大学河口海岸国家重点实验室上海 200062

作者简介:
王永红女 1969年出生副教授博士河口海岸动力沉积环境

1. Ocean University of China, College of Marine Geosciences, Qingdao,Shandong 266003;

2. East China Normal University, State Key Laboratory of Estuarine and Coastal Research, Shanghai 200062