Sand waves near the shelf break of the northern South China Sea: morphology and recent mobility

doi:10.1007/s00367-018-0557-3

CORC > 海洋研究所 > 中国科学院海洋研究所 > 海洋地质与环境重点实验室

	Sand waves near the shelf break of the northern South China Sea: morphology and recent mobility
	Zhang, Hongyun 1,2; Ma, Xiaochuan 1,3; Zhuang, Lihua 1; Yan, Jun 1,3
刊名	GEO-MARINE LETTERS
	2019-02-01
卷号	39 期号:1 页码:19-36
ISSN号	0276-0460
DOI	10.1007/s00367-018-0557-3
通讯作者	Ma, Xiaochuan(mxch@qdio.ac.cn) ; Yan, Jun(jyan@qdio.ac.cn)
英文摘要	Sand waves near the shelf break in the northern South China Sea have not previously been described in detail due to the lack of high-resolution bathymetric data. Their occurrence, however, is important for understanding sand transport and dispersal in the northern South China Sea. Here, using recent bathymetric data, side-scan image, bottom current measurements, and sediment samples collected in 2010 and 2016, we document the distribution, geometry, and mobility of sand waves in five regions along the shelf break of the northern South China Sea. Results show that the sand waves have distinctly different distribution patterns, geometries, and migration behaviors above and below the 145 m isobath. Sand waves at depths greater than 145m are larger and steeper, and mostly occur on slopes steeper than 0.5 degrees. Their crest lines are aligned parallel to the isobaths and their migration direction is toward the southeast (seaward). In comparison, the sand waves on the gentler sloping seabed at water depths <145m migrate toward the northwest with crest lines mostly intersecting the depth contours. Neither the heights nor the wavelengths of the sand waves correlate with water depth, although the two classes of sand wave are restricted to distinct depth intervals. The observed bottom currents, which are characterized by strong velocity pulses, probably relate to internal solitary waves which have the capacity of moving the sediment in the sand wave fields. The height-wavelength relationships of the sand waves correspond to those of subaqueous dunes. The diverging migration directions of the sand waves are interpreted as reflecting the polarity conversion of the internal solitary waves in the northern South China Sea during their propagation onto the shelf. The volume changes of the sand waves from 2010 to 2016 indicate both sediment loss and sediment accretion in various areas, suggesting complex sediment dispersal patterns near the shelf break.
资助项目	National Natural Science Foundation of China[41576056] ; National Natural Science Foundation of China[41876035] ; National Natural Science Foundation of China[41406061]
WOS研究方向	Geology ; Oceanography
语种	英语
出版者	SPRINGER
WOS记录号	WOS:000458181500002
内容类型	期刊论文
源URL	[http://ir.qdio.ac.cn/handle/337002/160852]
专题	海洋研究所_海洋地质与环境重点实验室
通讯作者	Ma, Xiaochuan; Yan, Jun
作者单位	1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao, Peoples R China 2.Univ Chinese Acad Sci, Beijing, Peoples R China 3.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol & Environm, Qingdao, Peoples R China
推荐引用方式 GB/T 7714	Zhang, Hongyun,Ma, Xiaochuan,Zhuang, Lihua,et al. Sand waves near the shelf break of the northern South China Sea: morphology and recent mobility[J]. GEO-MARINE LETTERS,2019,39(1):19-36.
APA	Zhang, Hongyun,Ma, Xiaochuan,Zhuang, Lihua,&Yan, Jun.(2019).Sand waves near the shelf break of the northern South China Sea: morphology and recent mobility.GEO-MARINE LETTERS,39(1),19-36.
MLA	Zhang, Hongyun,et al."Sand waves near the shelf break of the northern South China Sea: morphology and recent mobility".GEO-MARINE LETTERS 39.1(2019):19-36.