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Response of sediment grain size composition of the Zhe-Min coastal mud to the sediment load reduction of the Changjiang River entering the sea
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Shengjing Liu1, 2, Jianhua Gao1, 2, *, Xiaomei Xu1, 2, Yong Shi1, 2, Zhuo Shu1, 2, Hao Wu1, 2, Bingyu Yuan1, 2, Jianjun Jia3
Haiyang Xuebao | 2021, 43(3) : 105 - 115
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Haiyang Xuebao | 2021, 43(3): 105-115
Article
Response of sediment grain size composition of the Zhe-Min coastal mud to the sediment load reduction of the Changjiang River entering the sea
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Shengjing Liu1, 2, Jianhua Gao1, 2, *, Xiaomei Xu1, 2, Yong Shi1, 2, Zhuo Shu1, 2, Hao Wu1, 2, Bingyu Yuan1, 2, Jianjun Jia3
Affiliations
  • 1School of Geography and Ocean Science, Nanjing University, Nanjing 210023, China
  • 2Key Laboratory of Coast and Island Development of the Ministry of Education, Nanjing 210023, China
  • 3State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062, China
Published: 2021-03-25 doi: 10.12284/hyxb2021025
Outline
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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
Shengjing Liu, Jianhua Gao, Xiaomei Xu, Yong Shi, Zhuo Shu, Hao Wu, Bingyu Yuan, Jianjun Jia. Response of sediment grain size composition of the Zhe-Min coastal mud to the sediment load reduction of the Changjiang River entering the sea[J]. Haiyang Xuebao, 2021 , 43 (3) : 105 -115 . DOI: 10.12284/hyxb2021025
Year 2021 volume 43 Issue 3
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Article Info
doi: 10.12284/hyxb2021025
  • Receive Date:2019-12-09
  • Online Date:2026-02-26
  • Published:2021-03-25
Article Data
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History
  • Received:2019-12-09
  • Revised:2020-01-27
Funding
Affiliations
    1School of Geography and Ocean Science, Nanjing University, Nanjing 210023, China
    2Key Laboratory of Coast and Island Development of the Ministry of Education, Nanjing 210023, China
    3State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062, China
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表12种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)

Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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