日本海百年来沉积速率及粒度指示意义

宗娴; 石学法; 葛晨东; 邹建军; Sergey Gorbarenko; 乔淑卿; 董智

doi:10.14027/j.cnki.cjxb.2016.03.009

ISSN 1000-0550 CN 62-1038/P

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日本海百年来沉积速率及粒度指示意义

宗娴, 石学法, 葛晨东, 邹建军, Sergey Gorbarenko, 乔淑卿, 董智

文章导航 > 沉积学报 > 2016 > 34(3): 516-522

宗娴, 石学法, 葛晨东, 邹建军, Sergey Gorbarenko, 乔淑卿, 董智. 日本海百年来沉积速率及粒度指示意义[J]. 沉积学报, 2016, 34(3): 516-522. doi: 10.14027/j.cnki.cjxb.2016.03.009

引用本文:

ZONG Xian, SHI XueFa, GE ChenDong, ZOU JianJun, Sergey Gorbarenko, QIAO ShuQing, DONG Zhi. Sedimentation Rate and Implications of Sediment Grain Size of Japan Sea during the Last Hundred Years[J]. Acta Sedimentologica Sinica, 2016, 34(3): 516-522. doi: 10.14027/j.cnki.cjxb.2016.03.009

Citation:

ZONG Xian, SHI XueFa, GE ChenDong, ZOU JianJun, Sergey Gorbarenko, QIAO ShuQing, DONG Zhi. Sedimentation Rate and Implications of Sediment Grain Size of Japan Sea during the Last Hundred Years[J]. Acta Sedimentologica Sinica, 2016, 34(3): 516-522. doi: 10.14027/j.cnki.cjxb.2016.03.009

引用本文:

Citation:

ZONG Xian, SHI XueFa, GE ChenDong, ZOU JianJun, Sergey Gorbarenko, QIAO ShuQing, DONG Zhi. Sedimentation Rate and Implications of Sediment Grain Size of Japan Sea during the Last Hundred Years[J]. Acta Sedimentologica Sinica, 2016, 34(3): 516-522. doi: 10.14027/j.cnki.cjxb.2016.03.009

日本海百年来沉积速率及粒度指示意义

doi: 10.14027/j.cnki.cjxb.2016.03.009

宗娴^1,2,
石学法^2,3,,
葛晨东¹,
邹建军^2,3,
Sergey Gorbarenko⁴,
乔淑卿^2,3,
董智^1,2

1.
南京大学海岸与海岛开发教育部重点实验室/江苏省海岸与海岛开发重点实验室南京 210023;
2.
国家海洋局第一海洋研究所海洋沉积与环境地质国家海洋局重点实验室山东青岛 266061;
3.
青岛海洋科学与技术国家实验室海洋地质过程与环境功能实验室山东青岛 266061;
4.
俄罗斯科学院远东分院太平洋海洋研究所符拉迪沃斯托克 690041

基金项目: “全球变化与海气相互作用”专项项目(GAST-GEOGE-03);国家自然科学基金项目 (41420104005,40710069004);泰山学者项目

详细信息

作者简介:
宗娴,女,1991年出生,硕士研究生,海洋地球化学研究,E-mail:zongxian1991@163.com

通讯作者:
石学法,男,研究员,E-mail:xfshi@fio.org.cn

中图分类号: P736.21

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文章访问数: 613
HTML全文浏览量: 32
PDF下载量: 891
被引次数: 0

Sedimentation Rate and Implications of Sediment Grain Size of Japan Sea during the Last Hundred Years

1.
Key Laboratory of Coast and Island Development, Ministry of Education, Key Laboratory of Coast and Island Development of Jiangsu Province, Nanjing University, Nanjing 210023, China;
2.
Key Laboratory of Marine Sedimentology and Environment Geology, First Institute of Oceanography, State Oceanic Administration, Qingdao, Shandong 266061, China;
3.
Qingdao National Laboratory for Marine Science and Technology, Function Laboratory for Marine Geology and Environment, Qingdao, Shandong 266061, China;
4.
V.I. Il'ichev Pacific Oceanological Institute, Russian Academy of Science, Vladivostok 690041, Russia

Funds: Special Project on Global Change and Ocean-Atmosphere Interations, No. GAST-GEOGE-03; National Natural Science Foundation of China, No. 41420104005,40710069004; Taishan Scholars Program of Shandong

摘要

摘要: 对日本海中部、北部和西部四个深水多管沉积岩芯中的²¹⁰Pb活度和沉积物粒度进行分析。结果显示百年以来大和海脊、日本海北部和西部陆坡沉积物以粉砂和黏土质粉砂为主。在日本海北部和大和海脊表层沉积物存在显著的生物扰动现象,而在西部陆坡不存在。基于恒定供给速率(CRS)模式建立了4个岩芯的年代框架,并计算了沉积速率。日本海现代平均沉积速率介于0.19~0.42 cm/a,最低值出现在大和海脊。4个岩芯中沉积物平均粒径呈现不同的分布模式,但是在1940年和1980年,沉积物粒度分布模式同时发生了改变,这可能与百年以来北太平洋十年涛动(PDO)及东亚夏季风震荡有关。
- ²¹⁰Pb比活度 /
- 粒度 /
- 沉积速率 /
- 沉积环境 /
- 日本海
Abstract: Both of the ²¹⁰Pb and sediment grain size in four deep-water multicore sediments which are located in the middle, north and west of Japan Sea are analyzed. The result shows that the sediments mainly consist of silt and clayey silt in the Yamato Ridge, northern part and western slope of Japan Sea over the last 100 years. There is a significant biological disturbance phenomenon of surface sediments in Yamato Ridge and the northern part of the Japan Sea, which does not exist in the western slope. According to the model of Constant Rate of Supply (CRS), we determined the age mode and calculated the sedimentation rate in four multicores. The modern average sedimentation rate in the Japan Sea varied between 0.19~0.42 cm/a, with a lowest value in Yamato Ridge. The mean sediment grain size of four cores showed different vertical patterns, but they simultaneously varied at about 1940 and 1980. We think such simultaneous change is closely related to the variations of Pacific Decadal Oscillation (PDO) and East Asian Summer Monsoon over the last 100 years.
- ²¹⁰Pb specific activity /
- sediment grainsize /
- sedimentation rate /
- sedimentary environment /
- Japan Sea

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参考文献(0)

[1]	刘涛, 褚冠宇, 徐慧鹏. 基于风暴潮记录研究红树林淤积速率时间变化 . 沉积学报, 2022, 40(5): 1346-1354. doi: 10.14027/j.issn.1000-0550.2021.042
[2]	胡京九, 张虎才, 常凤琴, 李婷, 蔡萌, 段立曾, 张龙吴, 张扬. 程海表层沉积物粒度空间分布特征及其影响因素 . 沉积学报, 2020, 38(2): 340-348. doi: 10.14027/j.issn.1000-0550.2019.032
[3]	李东义, 徐勇航, 王爱军, 郑斌鑫, 李国刚. 福建安海湾表层沉积物粒度特征及其现代沉积过程分析 . 沉积学报, 2015, 33(4): 724-734. doi: 10.14027/j.cnki.cjxb.2015.04.011
[4]	. 长江水下三角洲向南延伸泥质带浅地层结构及沉积物特征初探——以朱家尖岛以东海域为例 . 沉积学报, 2014, 32(2): 296-305.
[5]	. 乌梁素海湖泊沉积物粒度特征及其环境指示意义 . 沉积学报, 2013, 31(04): 646-652.
[6]	张瑞. 长江河口水下三角洲210Pb分布特征及其沉积速率 . 沉积学报, 2009, 27(4): 704-713.
[7]	段凌云, 王张华, 李茂田, 潘建明, 陈中原, Yishiki Saito, Yutaka kanai. 长江口沉积物²¹⁰Pb分布及沉积环境解释 . 沉积学报, 2005, 23(3): 514-522.
[8]	刘晓东, 鹿化煜, 安芷生. 利用黄土沉积速率与粒度的相关性建立黄土序列年龄的新方法 . 沉积学报, 1999, 17(1): 145-148.
[9]	杨松林, 刘国贤, 杜瑞芝, 张兵. 用²¹⁰Pb年代学方法对辽东湾现代沉积速率的研究 . 沉积学报, 1993, 11(1): 128-135.
[10]	叶崇开. ¹³⁷Cs法和²¹⁰Pb法对比研究鄱阳湖近代沉积速率 . 沉积学报, 1991, 9(1): 106-114.

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文章访问数: 613
HTML全文浏览量: 32
PDF下载量: 891
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日本海百年来沉积速率及粒度指示意义

doi: 10.14027/j.cnki.cjxb.2016.03.009

1. 南京大学海岸与海岛开发教育部重点实验室/江苏省海岸与海岛开发重点实验室南京 210023;

2. 国家海洋局第一海洋研究所海洋沉积与环境地质国家海洋局重点实验室山东青岛 266061;

3. 青岛海洋科学与技术国家实验室海洋地质过程与环境功能实验室山东青岛 266061;

4. 俄罗斯科学院远东分院太平洋海洋研究所符拉迪沃斯托克 690041

基金项目: “全球变化与海气相互作用”专项项目(GAST-GEOGE-03);国家自然科学基金项目 (41420104005,40710069004);泰山学者项目

作者简介:
宗娴,女,1991年出生,硕士研究生,海洋地球化学研究,E-mail:zongxian1991@163.com

通讯作者: 石学法,男,研究员,E-mail:xfshi@fio.org.cn

收稿日期: 2015-08-24
修回日期: 2016-01-19
刊出日期: 2016-06-10

中图分类号: P736.21

关键词:

²¹⁰Pb比活度 /

粒度 /

沉积速率 /

沉积环境 /

日本海

摘要: 对日本海中部、北部和西部四个深水多管沉积岩芯中的²¹⁰Pb活度和沉积物粒度进行分析。结果显示百年以来大和海脊、日本海北部和西部陆坡沉积物以粉砂和黏土质粉砂为主。在日本海北部和大和海脊表层沉积物存在显著的生物扰动现象,而在西部陆坡不存在。基于恒定供给速率(CRS)模式建立了4个岩芯的年代框架,并计算了沉积速率。日本海现代平均沉积速率介于0.19~0.42 cm/a,最低值出现在大和海脊。4个岩芯中沉积物平均粒径呈现不同的分布模式,但是在1940年和1980年,沉积物粒度分布模式同时发生了改变,这可能与百年以来北太平洋十年涛动(PDO)及东亚夏季风震荡有关。

English Abstract

Sedimentation Rate and Implications of Sediment Grain Size of Japan Sea during the Last Hundred Years

1. Key Laboratory of Coast and Island Development, Ministry of Education, Key Laboratory of Coast and Island Development of Jiangsu Province, Nanjing University, Nanjing 210023, China;

2. Key Laboratory of Marine Sedimentology and Environment Geology, First Institute of Oceanography, State Oceanic Administration, Qingdao, Shandong 266061, China;

3. Qingdao National Laboratory for Marine Science and Technology, Function Laboratory for Marine Geology and Environment, Qingdao, Shandong 266061, China;

4. V.I. Il'ichev Pacific Oceanological Institute, Russian Academy of Science, Vladivostok 690041, Russia

Received Date: 2015-08-24
Rev Recd Date: 2016-01-19
Publish Date: 2016-06-10

Keywords:

Abstract: Both of the ²¹⁰Pb and sediment grain size in four deep-water multicore sediments which are located in the middle, north and west of Japan Sea are analyzed. The result shows that the sediments mainly consist of silt and clayey silt in the Yamato Ridge, northern part and western slope of Japan Sea over the last 100 years. There is a significant biological disturbance phenomenon of surface sediments in Yamato Ridge and the northern part of the Japan Sea, which does not exist in the western slope. According to the model of Constant Rate of Supply (CRS), we determined the age mode and calculated the sedimentation rate in four multicores. The modern average sedimentation rate in the Japan Sea varied between 0.19~0.42 cm/a, with a lowest value in Yamato Ridge. The mean sediment grain size of four cores showed different vertical patterns, but they simultaneously varied at about 1940 and 1980. We think such simultaneous change is closely related to the variations of Pacific Decadal Oscillation (PDO) and East Asian Summer Monsoon over the last 100 years.

引用本文:

Citation:

ZONG Xian, SHI XueFa, GE ChenDong, ZOU JianJun, Sergey Gorbarenko, QIAO ShuQing, DONG Zhi. Sedimentation Rate and Implications of Sediment Grain Size of Japan Sea during the Last Hundred Years[J]. Acta Sedimentologica Sinica, 2016, 34(3): 516-522. doi: 10.14027/j.cnki.cjxb.2016.03.009

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日本海百年来沉积速率及粒度指示意义

doi: 10.14027/j.cnki.cjxb.2016.03.009

作者简介:
宗娴,女,1991年出生,硕士研究生,海洋地球化学研究,E-mail:zongxian1991@163.com

通讯作者:
石学法,男,研究员,E-mail:xfshi@fio.org.cn

计量

Sedimentation Rate and Implications of Sediment Grain Size of Japan Sea during the Last Hundred Years

计量

目录

日本海百年来沉积速率及粒度指示意义

doi: 10.14027/j.cnki.cjxb.2016.03.009

作者简介:
宗娴,女,1991年出生,硕士研究生,海洋地球化学研究,E-mail:zongxian1991@163.com

通讯作者: 石学法,男,研究员,E-mail:xfshi@fio.org.cn

English Abstract

Sedimentation Rate and Implications of Sediment Grain Size of Japan Sea during the Last Hundred Years

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日本海百年来沉积速率及粒度指示意义

doi: 10.14027/j.cnki.cjxb.2016.03.009

作者简介: 宗娴,女,1991年出生,硕士研究生,海洋地球化学研究,E-mail:zongxian1991@163.com

通讯作者: 石学法,男,研究员,E-mail:xfshi@fio.org.cn

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Sedimentation Rate and Implications of Sediment Grain Size of Japan Sea during the Last Hundred Years

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日本海百年来沉积速率及粒度指示意义

doi: 10.14027/j.cnki.cjxb.2016.03.009

作者简介: 宗娴,女,1991年出生,硕士研究生,海洋地球化学研究,E-mail:zongxian1991@163.com

通讯作者: 石学法,男,研究员,E-mail:xfshi@fio.org.cn

English Abstract

Sedimentation Rate and Implications of Sediment Grain Size of Japan Sea during the Last Hundred Years

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
宗娴,女,1991年出生,硕士研究生,海洋地球化学研究,E-mail:zongxian1991@163.com

通讯作者:
石学法,男,研究员,E-mail:xfshi@fio.org.cn

作者简介:
宗娴,女,1991年出生,硕士研究生,海洋地球化学研究,E-mail:zongxian1991@163.com