浙闽沿岸泥质区沉积物粒度组分对长江入海输沙量减少的响应

刘胜璟; 高建华; 徐笑梅; 石勇; 舒卓; 吴昊; 元冰瑜; 贾建军

doi:10.12284/hyxb2021025

浙闽沿岸泥质区沉积物粒度组分对长江入海输沙量减少的响应

doi: 10.12284/hyxb2021025

刘胜璟^{1, 2,},
高建华^{1, 2, ,},
徐笑梅^{1, 2},
石勇^{1, 2},
舒卓^{1, 2},
吴昊^{1, 2},
元冰瑜^{1, 2},
贾建军³

1.
南京大学地理与海洋科学学院，江苏南京 210023
2.
海岸与海岛开发教育部重点实验室，江苏南京 210023
3.
华东师范大学河口海岸学国家重点实验室，上海 200062

基金项目: 国家自然科学基金（41776048，41876092）

详细信息

作者简介:
刘胜璟（1995-），男，江苏省连云港市人，研究方向为海洋沉积学。E-mail：shjing_liu@163.com

通讯作者:
高建华（1973-），教授，主要从事海洋沉积动力学研究。E-mail：jhgao@nju.edu.cn

中图分类号: P736.2
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- 被引次数: 0
出版历程
- 收稿日期: 2019-12-09
- 修回日期: 2020-01-27
- 网络出版日期: 2021-02-25
- 刊出日期: 2021-04-23

Response of sediment grain size composition of the Zhe-Min coastal mud to the sediment load reduction of the Changjiang River entering the sea

Liu Shengjing^{1, 2
,},
Gao Jianhua^{1, 2
, ,},
Xu Xiaomei^{1, 2},
Shi Yong^{1, 2},
Shu Zhuo^{1, 2},
Wu Hao^{1, 2},
Yuan Bingyu^{1, 2},
Jia Jianjun³

1.
School of Geography and Ocean Science, Nanjing University, Nanjing 210023, China
2.
Key Laboratory of Coast and Island Development of the Ministry of Education, Nanjing 210023, China
3.
State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062, China

摘要

摘要: 自1950年以来，长江入海输沙量呈阶段性减少趋势；作为长江远端泥，长江入海输沙量的“减沙”效应在浙闽沿岸泥质区是否有相应的沉积信号？若有，该如何进行提取和解译？为探讨以上问题，在浙闽沿岸泥质区采集柱状样5根，进行了高分辨率(2 mm)的粒度测试，并通过端元分析手段分离出4个端元。结合研究区物源及水动力的空间差异，发现各端元有其特定的指示意义：EM1组分(众数粒径约为2 μm)为长江来源的极细粒物质；EM2组分(众数粒径约为10 μm)主要为长江及浙闽沿岸中小河流的细颗粒物质，但以长江为主；EM3组分(众数粒径约为80 μm)主要为台湾暖流带来的较粗粒物质；EM4组分(众数粒径约为200 μm)为长江输运的粗颗粒物质。进一步分析发现，EM1组分对长江入海输沙量的阶段性减少有较好的响应关系：由浙闽泥质区北部至南部响应强度依次降低；在响应时间上存在滞后现象，且从北到南滞后时间增加，由北部的4～6年增加至南部的10～14年。总体来看，细颗粒组分更能反映长江流域变化信息，且泥质区的不同位置对流域变化信息的响应强度差异显著。
- 浙闽泥质区 /
- 粒度 /
- 端元分析 /
- 长江入海输沙量
Abstract: Since 1950, the sediment load of the Changjiang River entering the sea has been stepwise decreasing. As the distal mud of the Changjiang River, whether the signal of “sediment load reduction” was recorded in the Zhe-Min coastal mud? If so, how to extract and interpret these sedimentary information? In order to discussing this scientific problem, 5 sediment cores were collected in the Zhe-Min coastal mud; in addition, high resolution grain size analysis (2 mm) was conducted, and four end members were obtained through end-member (EM) model decomposing. Combined with the analysis of the spatial discrepancy in provenance and hydrodynamics of the study area, the specific indicative significance of each EM was revealed: EM1 (with the modal grain size about 2 μm) is originated from extremely fine-grained sediment of the Changjiang River; EM2’s (with the modal grain size about 10 μm) origin is predominated by the Changjiang River, and small part is contributed by the middle and small sized rivers of Zhe-Min coast; EM3 (with the modal grain size about 80 μm) mainly consists of coarse-grain sediment might be provided by Taiwan Warm Current; EM4 (with the modal grain size about 200 μm) is also characterized by coarse-grain sediment, and may be contributed by the Changjiang River. Further analysis indicated that, the EM1 variation was in agreement with the sediment stepwise reduction of the Changjiang River; however, the response intensity gradually decreased from the north to the south. In addition, the hysteresis existed in response time, and the retardation time increased from 4−6 years in the north to 10−14 years in the south. In general, fine-grained sediment could better reflect the Changjiang River catchment change information, and response intensity exhibited significant difference in different areas of the Zhe-Min coastal mud.
- the Zhe-Min coastal mud /
- sediment grain size /
- end-member (EM) analysis /
- sediment entering into the sea from the Changjiang River

HTML全文

图 1 研究区流系及采样点分布图（★为采样位置）

改绘自文献[23-24]；a：浙闽沿岸流；b：台湾暖流；c：黑潮；d：黑潮入侵分支；e：台湾物质可能的影响区域

Fig. 1 Current systems and sampling distribution of the study area (★ represents the sampling position)

Modified from references [23-24]; a: Zhe-Min Coastal Current; b: Taiwan Warm Current; c: Kuroshio; d: the branch of Kuroshio intrusion; e: possible area of impact of Taiwanese material

下载: 全尺寸图片幻灯片

图 2 各柱状样平均粒径垂向变化

Fig. 2 The mean grain size of each sample column

下载: 全尺寸图片幻灯片

图 3 各柱状样²¹⁰Pb活度的垂向分布

Fig. 3 Vertical distributions of ²¹⁰Pb radioactivity in each sediment core

下载: 全尺寸图片幻灯片

图 4 各端元频率分布

Fig. 4 Frequency distribution of each end member

下载: 全尺寸图片幻灯片

图 5 各柱状样不同端元含量

Fig. 5 Different end member content in each sediment core

下载: 全尺寸图片幻灯片

图 6 长江入海输沙量与EM1组分的变化关系

Fig. 6 The relationship between EM1 composition and the reduction of sediment entering into the sea from the Changjiang River

下载: 全尺寸图片幻灯片

表 1 柱状样信息

Tab. 1 The information of sample columns

柱状样编号	纬度	经度	水深/m	长度/cm
S1	29.55°N	122.80°E	58	38
S2	28.47°N	122.58°E	65	43
S3	27.63°N	121.90°E	65	36
S4	26.82°N	121.23°E	65	41
S5	26.18°N	120.15°E	28	46

下载: 导出CSV

表 2 端元拟合结果

Tab. 2 The results of end member unmixing

No. of EM_S	EM R²	R²	Theta
2	1.742×10⁻⁶	0.956	9.650
3	9.311×10⁻³	0.979	6.723
4	0.0205	0.996	3.044
5	0.182	0.998	1.896
6	0.108	0.999	1.342
注：No. of EM_S为拟合端元数量；EM R²为所有拟合端元之间线性平方相关性的最大值；R²为测量数据集和拟合的端元数据集之间的线性平方相关性；Theta为测量数据集和拟合端元数据集之间的角度距离。

下载: 导出CSV

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