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

WANG Yong hong; SHEN Huan ting; ZHANG Wei guo

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Article Navigation > Acta Sedimentologica Sinica > 2004 > 22(4): 658-663

WANG Yong hong, SHEN Huan ting, ZHANG Wei guo. A Preliminary Comparison of Magnetic Properties of Sediments from the Changjiang and the Huanghe Estuaries[J]. Acta Sedimentologica Sinica, 2004, 22(4): 658-663.

Citation:

WANG Yong hong, SHEN Huan ting, ZHANG Wei guo. A Preliminary Comparison of Magnetic Properties of Sediments from the Changjiang and the Huanghe Estuaries[J]. Acta Sedimentologica Sinica, 2004, 22(4): 658-663.

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

Received Date: 2003-10-24
Rev Recd Date: 2004-04-19
Publish Date: 2004-12-10

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

References

[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]

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通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

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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

Received Date: 2003-10-24

Rev Recd Date: 2004-04-19

Publish Date: 2004-12-10

Key words:

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.

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Reference (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]

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

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