渤海湾西部表层沉积物悬移组分元素特征及物源意义

田立柱; 裴艳东; 商志文; 王福; 王宏

doi:10.3724/SP.J.1140.2010.01009

渤海湾西部表层沉积物悬移组分元素特征及物源意义

doi: 10.3724/SP.J.1140.2010.01009

田立柱^1,2,
裴艳东²,
商志文^2,3,
王福²,
王宏^2,3

详细信息

1 中国地质大学海洋学院, 北京 100083;

2 中国地质调查局天津地质调查中心, 天津 300170;

3 中国地质科学院研究生院, 北京 100037

作者简介:
田立柱(1981-),男,博士研究生,主要从事海洋地质学的研究工作,E-mail:tjtlizhu@cgs.gov.cn

基金项目:
国土资源部地质调查项目(1212010540501)

国家海洋局"908"专项(908-TJ-06)
中图分类号: P736.21

ELEMENTS CHARACTERISTICS OF THE SUSPENDED COMPONENT IN SURFACE SEDIMENTS FROM THE WEST BOHAI BAY AND THE PROVENANCE IMPLICATION

More Information

1 School of Marine Sciences, China University of Geosciences, Beijing 100083, China;

2 Tianjin Centre, China Geological Survey, Tianjin 300170, China;

3 School of Graduates, Chinese Academy of Geological Sciences, Beijing 100037, China

摘要: 对渤海湾西部海底表层沉积物样品粒径小于0.063 mm的悬移组分进行16种元素测试,分析了各元素特征及分布规律。元素平均丰度与黄土及渤海泥质沉积物基本一致,说明渤海湾西部表层沉积物悬移组分的物源主要与黄河源区黄土高原的黄土有关。研究区16种元素可分为两类,I类是Sc、Co、Fe、V、Al、Ca、Mg、Th、U、Cr;Ⅱ类是Zr、Hf、Ba、Na、Sr、K。同类元素丰度的平面分布规律相似,呈现正相关性;异类元素丰度的平面分布规律相反且呈负相关性。研究区主要分为两个地球化学分区,两区基本以北纬39°05'线为界,I区位于南部和中部,以高Sc、Co、V、Th、U、Cr、Fe、Al、Mg、Ca等I类元素为特征;而Ⅱ区位于北部,以高Zr、Hf、Ba、Sr、Na、K等Ⅱ类元素为特征。渤海湾西部表层沉积物悬移组分的元素特征及分区,可能与研究区内不同季节沿岸环流方向改变,进而导致不同物源母质沉积物输运混合作用有关。
- 表层沉积物 /
- 悬移组分 /
- 元素 /
- 物源 /
- 渤海湾西部
Abstract: The abundance of 16 elements, analyzed in the suspended component in surface sediments from the west of the Bohai Bay, reveals the element characteristics and distribution patterns. The average elemental abundance in the study area is generally similar to those of the loess and the Bohai mud, indicating the source of the suspension component in the west of the Bohai Bay is related to the provenance of the Yellow River, i.e. the loess on the Loess Plateau. The 16 elements can be divided into Category I (Sc, Co, Fe, V, Al, Ca, Mg, Th, U, and Cr), and Category Ⅱ (Zr, Hf, Ba, Na, Sr, and K). Elements in the same category share the same spatial distribution patterns and show a positive correlation, while elements in the different categories show opposite spatial distribution patterns and a negative correlation. Samples in the study area can be classified into two geochemical provinces, bounded by the latitude of 39°05'N. Province I, the southern and middle part of the study area, is characterized by the comparative concentration of Category I elements:Sc, Co, V, Th, U, Cr, Fe, Al, Mg,and Ca; Province Ⅱ, the northern part of the study area, in contrast, is characterized by the comparative concentration of Category Ⅱ elements:Zr, Hf, Ba, Sr, Na, and K. The element characteristics of the suspended component in surface sediments from the west of the Bohai Bay, are probably associated with the two-way sediment transport mixing of different material elements, caused by the complete changes of coastal circulation directions in different seasons.
- the suspended component of surface sediments /
- elements /
- provenance /
- in the west of the Bohai Bay /

[1]	McLennan S M, Hemming S, McDaniel D K, et al. Geochemical approaches to sedimentation, provenance, and tectonics[C]//Processes Controlling the Composition of Clastic Sediments. Geological Society of America, 1993, Special Paper 284:21-40.
[2]	Girty G H, Ridge D L, Knaack C, et al. Provenance and depositional setting of Paleozoic chert and argillite, Sierra Nevada, California[J]. J. Sediment. Res, 1996, 66:107-118.
[3]	吕成功, 陈真. 渤海表层沉积物地球化学分析[J]. 青岛海洋大学学报, 1993, 23(3):91-98. [LÜ Chenggong, CHEN Zhen. Geochemical analysis of the surface sediments of the Bohai Sea[J]. Journal of Ocean University of Qingdao, 1993, 23(3):91-98.]
[4]	郭津年, 李健博, 吴景阳. 渤海沉积物中的Fe, Al, Mn分布及某些地球化学特征的研究[J]. 海洋科学, 1983, 4:22-25.[GUO Jinnian, LI Jianbo, WU Jingyang. The distribution of Fe, Al, and Mn in sediments of Bohai Sea and their certain geochemical characteristics[J]. Marine Sciences, 1983 , 4:22-25.]
[5]	Cullers R L. The chemical signature of source rocks in size fractions of Holocene stream sediment derived from metamorphic rocks in the Wet Mountains region, USA[J]. Chem. Geol., 1994., 113:327-343.
[6]	Cullers R L. The geochemistry of shales, siltstones and sandstones of Pennsylvanian Permian age, Colorado, USA:implications for provenance and metamorphic studies[J]. Lithos, 2000, 51:181-203.
[7]	Zhang C, Wang L, Li G, et al. Grain size effect on multi-element concentrations in sediments from the intertidal flats of Bohai Bay, China[J]. Applied Geochemistry, 2002.17:59-68.
[8]	吴明清, 文启忠, 潘景瑜, 等. 中国黄土的平均化学成分上部大陆地壳的一种典型代表[J]. 岩相古地理,1995, 15(2):127-136. [WU Mingqing, WEN Qizhong, PAN Jingyu, et al. Average geochemical composition of loess in China:as a good representative of the upper continental crust[J]. Sedimentary Facies and Palaeogeography,1995, 15(2):127-136.]
[9]	赵一阳, 鄢明才. 中国浅海沉积物地球化学[M]. 北京:科学出版社,1994.[ZHAO Yiyang, YAN Mingcai. Geochemistry of Sediments in Chinese Shallow Sea[M]. Beijing:Science Press,1994.]
[10]	刘昭蜀, 赵焕庭, 范时清,等. 南海地质[M]. 北京:科学出版社, 2002:502.[LIU Zhaoshu, ZHAO Huanting, FAN Shiqing, et al. Geology of South China Sea[M]. Beijing:Science Press. 2002:502.]
[11]	施建堂. 渤海湾西岸的现代沉积[J]. 海洋通报, 1987, 6(1):22-26. [SHI Jiantang. Modern sedimentation in the western Bohai Bay[J]. Marine Science Bulletin, 1987, 6(1):22-26.]
[12]	李建芬, 康慧, 王宏, 等. 渤海湾西岸海岸带现代地质作用及影响因素分析[J]. 地质调查与研究, 2007, 30(4):295-301. [LI Jianfen, KANG Hui, WANG Hong, et al. Modern geological action and discussion of influence factors on the west coast of Bohai Bay, China[J]. Geological Survey and Research, 2007, 30(4):295-301.]
[13]	赵保仁, 庄国文,曹德明,等. 渤海的环流、潮余流及其对沉积物分布的影响[J]. 海洋与湖沼, 1995, 26(5):466-473. [ZHAO Baoren, ZHUANG Guowen, CAO Deming, et al. Circulation, tidal residual currents and their effects on the sedimentations in the Bohai Sea[J]. Oceanologia et Limnologia Sinica, 1995, 26(5):466-473.]
[14]	杨作升. 黄河口毗邻海域细粒级沉积物特征及沉积物入海后的运移[J]. 山东海洋学院学报, 1985, 15, 2, 121-129. [YANG Zuosheng. Characteristics of fine-grained sediment of the shelf area adjacent to the mouth of the Huanghe River and sediment dispersion in that region[J].Journal of Shandong College of Oceanology, 1985, 15(2):121-129.]
[15]	何良彪. 渤海表层沉积物中的黏土矿物[J]. 海洋学报, 1984, 6(2):272-276. [HE Liangbiao. The clay mineral of the surface sediment in Bohai Sea[J]. Acta Oceanolgica Sinica, 1984, 6(2):272-276.]
[16]	赵全基. 渤海表层沉积作用[J]. 黄渤海海洋, 1988, 6(1):45-50. [ZHAO Quanji. Surface sedimentation in the Bohai Sea[J]. Journal of Oceanography of Huanghai & Bohai Sea, 1988, 6(1):45-50.]
[17]	刘彬昌, 卢中发, 张守法. 渤海沉积物地球化学分区的模糊分析[J]. 海洋与湖沼, 1992, 23(5):561-565. [LIU Binchang, LU Zhongfa, ZHANG Shoufa. Fuzzy analysis of geochemical divisions in sediments collected from the Bohai Sea[J]. Oceanologia et limnologia Sinica, 1992, 23(5):561-565.]
[18]	刘兴泉, 缪经榜, 季仲贞. 渤海冬季环流的数值研究[J]. 大气科学, 1989, 13(3):280-288. [LIU Xingquan, MIU Jingbang, JI Zhongzhen. Numerical simulation of the winter-time circulation in the Bohai Sea.[J]. Scientia Atmospherica Sinica, 1989, 13(3):280-288.]
[19]	迟清华, 鄢明才. 应用地球化学元素丰度数据手册[M]. 北京:地质出版社, 2007:1-14.[CHI Qinghua, YAN Mingcai. Handbook of Elemental Abundance for Applied Geochemistry[M]:Beijing:Geological Publishing House, 2007:1 -14.]
[20]	史长义, 鄢明才, 刘崇民, 等. 中国花岗岩类化学元素丰度及特征[J]. 地球化学, 2005, 34(5):470-482. [SHI Changyi, YAN Mingcai, LIU Chongmin, et al. Abundances of chemical elements in granitoids of China and their characteristics[J]. Geochimica, 2005, 34(5):470-482.]
[21]	杨守业, 李从先. 长江与黄河现代表层沉积物元素组成及其示踪作用[J]. 自然科学进展, 1999, 9(10):930-937. [YANG Shouye, LI Congxian. Elements composition of surface sediments from the Changjiang River and the Yellow River and their tracing application[J]. Advances in Natural Science, 1999, 9(10):930-937.]
[22]	刘建国, 李安春, 陈木宏, 等. 全新世渤海泥质沉积物地球化学特征[J]. 地球化学, 2007, 36(6):633-637. [LIU Jianguo, LI Anchun, CHEN Muhong, et al. Geochemical characteristics of sediments in the Bohai Sea mud area during Holocene[J]. Geochimica, 2007, 36(6):633-637.]

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渤海湾西部表层沉积物悬移组分元素特征及物源意义

doi: 10.3724/SP.J.1140.2010.01009

1 中国地质大学海洋学院, 北京 100083;

2 中国地质调查局天津地质调查中心, 天津 300170;

3 中国地质科学院研究生院, 北京 100037

作者简介:
田立柱(1981-),男,博士研究生,主要从事海洋地质学的研究工作,E-mail:tjtlizhu@cgs.gov.cn

ELEMENTS CHARACTERISTICS OF THE SUSPENDED COMPONENT IN SURFACE SEDIMENTS FROM THE WEST BOHAI BAY AND THE PROVENANCE IMPLICATION

1 School of Marine Sciences, China University of Geosciences, Beijing 100083, China;

2 Tianjin Centre, China Geological Survey, Tianjin 300170, China;

3 School of Graduates, Chinese Academy of Geological Sciences, Beijing 100037, China

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渤海湾西部表层沉积物悬移组分元素特征及物源意义

doi: 10.3724/SP.J.1140.2010.01009

1 中国地质大学海洋学院, 北京 100083;

2 中国地质调查局天津地质调查中心, 天津 300170;

3 中国地质科学院研究生院, 北京 100037

作者简介:
田立柱(1981-),男,博士研究生,主要从事海洋地质学的研究工作,E-mail:tjtlizhu@cgs.gov.cn

English Abstract

ELEMENTS CHARACTERISTICS OF THE SUSPENDED COMPONENT IN SURFACE SEDIMENTS FROM THE WEST BOHAI BAY AND THE PROVENANCE IMPLICATION

1 School of Marine Sciences, China University of Geosciences, Beijing 100083, China;

2 Tianjin Centre, China Geological Survey, Tianjin 300170, China;

3 School of Graduates, Chinese Academy of Geological Sciences, Beijing 100037, China

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渤海湾西部表层沉积物悬移组分元素特征及物源意义

doi: 10.3724/SP.J.1140.2010.01009

1 中国地质大学 海洋学院, 北京 100083; 2 中国地质调查局 天津地质调查中心, 天津 300170; 3 中国地质科学院 研究生院, 北京 100037

作者简介: 田立柱(1981-),男,博士研究生,主要从事海洋地质学的研究工作,E-mail:tjtlizhu@cgs.gov.cn

ELEMENTS CHARACTERISTICS OF THE SUSPENDED COMPONENT IN SURFACE SEDIMENTS FROM THE WEST BOHAI BAY AND THE PROVENANCE IMPLICATION

1 School of Marine Sciences, China University of Geosciences, Beijing 100083, China; 2 Tianjin Centre, China Geological Survey, Tianjin 300170, China; 3 School of Graduates, Chinese Academy of Geological Sciences, Beijing 100037, China

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渤海湾西部表层沉积物悬移组分元素特征及物源意义

doi: 10.3724/SP.J.1140.2010.01009

1 中国地质大学 海洋学院, 北京 100083; 2 中国地质调查局 天津地质调查中心, 天津 300170; 3 中国地质科学院 研究生院, 北京 100037

作者简介: 田立柱(1981-),男,博士研究生,主要从事海洋地质学的研究工作,E-mail:tjtlizhu@cgs.gov.cn

English Abstract

ELEMENTS CHARACTERISTICS OF THE SUSPENDED COMPONENT IN SURFACE SEDIMENTS FROM THE WEST BOHAI BAY AND THE PROVENANCE IMPLICATION

1 School of Marine Sciences, China University of Geosciences, Beijing 100083, China; 2 Tianjin Centre, China Geological Survey, Tianjin 300170, China; 3 School of Graduates, Chinese Academy of Geological Sciences, Beijing 100037, China

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关于我们

1 中国地质大学海洋学院, 北京 100083;

2 中国地质调查局天津地质调查中心, 天津 300170;

3 中国地质科学院研究生院, 北京 100037

作者简介:
田立柱(1981-),男,博士研究生,主要从事海洋地质学的研究工作,E-mail:tjtlizhu@cgs.gov.cn

1 School of Marine Sciences, China University of Geosciences, Beijing 100083, China;

2 Tianjin Centre, China Geological Survey, Tianjin 300170, China;

3 School of Graduates, Chinese Academy of Geological Sciences, Beijing 100037, China

1 中国地质大学海洋学院, 北京 100083;

2 中国地质调查局天津地质调查中心, 天津 300170;

3 中国地质科学院研究生院, 北京 100037

作者简介:
田立柱(1981-),男,博士研究生,主要从事海洋地质学的研究工作,E-mail:tjtlizhu@cgs.gov.cn

1 School of Marine Sciences, China University of Geosciences, Beijing 100083, China;

2 Tianjin Centre, China Geological Survey, Tianjin 300170, China;

3 School of Graduates, Chinese Academy of Geological Sciences, Beijing 100037, China