Mineral distributions in surface sediments of the western South Yellow Sea: implications for sediment provenance and transportation

Jian Lu; Anchun Li; Peng Huang; Yan Li

doi:10.1007/s00343-015-4106-x

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Mineral distributions in surface sediments of the western South Yellow Sea: implications for sediment provenance and transportation

Updated：2023-05-16

- Mineral distributions in surface sediments of the western South Yellow Sea: implications for sediment provenance and transportation
- Journal of Oceanology and Limnology Vol. 33, Issue 2, Pages: 510-524(2015)
- Affiliations：
  
  1. Key Laboratory of Marine Geology and Environment Institute of Oceanology Chinese Academy of Sciences
  2. University of Chinese Academy of Sciences
  3. Yantai Ocean Environmental Monitoring Central Station of State Oceanic Administration
- Author bio：
- Funds：
- DOI：10.1007/s00343-015-4106-x
  CLC：
- Online First：07 November 2014，
  
  Published：2015
- Accepted：
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Lu, J., Li, A., Huang, P. et al. Mineral distributions in surface sediments of the western South Yellow Sea: implications for sediment provenance and transportation., Chin. J. Ocean. Limnol. 33, 510–524 (2015). https://doi.org/10.1007/s00343-015-4106-x
DOI：

Lu, J., Li, A., Huang, P. et al. Mineral distributions in surface sediments of the western South Yellow Sea: implications for sediment provenance and transportation., Chin. J. Ocean. Limnol. 33, 510–524 (2015). https://doi.org/10.1007/s00343-015-4106-x DOI：

摘要

Abstract

The South Yellow Sea (SYS) is strongly influenced by the substantial sediment loads of the Huanghe (Yellow) (including the modern Huanghe and abandoned old Huanghe subaqueous delta) and Changjiang (Yangtze) Rivers. However

the dispersal patterns of these sediments

especially in the western SYS

have not been clearly illustrated. In this study

we have analyzed clay minerals

detrital minerals

and grain sizes for 245 surface sediment samples (0–5 cm) collected from the western SYS. The clay minerals

on average

consist of 67% illite

14% smectite

11% chlorite

and 8% kaolinite. Clay minerals

detrital minerals

and grain size analyses of surface sediments

combined with water mass hydrology analysis

reveal that sediments in the western SYS are mainly derived from the modern Huanghe River

the abandoned subaqueous delta of the old Huanghe River

some material from the Changjiang

and coastal erosion. The clay minerals (especially illite and smectite) and quartz/feldspar ratio distribution patterns

reveal that the influence of modern Huanghe sediments can reach 35°N in the northwestern part of the study area

an influence that can be enhanced especially in winter owing to northerly winds. Conversely

sediments along the Jiangsu coast are mixed

in summer

with material from the Changjiang arriving via northward flow of Changjiang Diluted Water. The Subei Coastal Current carries the refreshed sediments northward into the western SYS. Sediment distribution and transport in the western SYS are mainly controlled by the oceanic circulation system that is primarily related to the monsoon.

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Keywords

references

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