TY - JOUR
T1 - Several characteristics of beach aeolian sand transport influenced by tide
T2 - A case study in the Yuandangao beach, Pingtan Island, Fujian Province
AU - He, Yanyu
AU - Liu, Jianhui
AU - Cai, Feng
AU - Li, Bailiang
AU - Wang, Lihui
AU - Zhou, Changmao
N1 - Publisher Copyright:
© 2018, Editorial Office of Haiyang Xuebao. All rights reserved.
PY - 2018/9
Y1 - 2018/9
N2 - Coastal aeolian is a typical product of sea, land and air interaction. Based on a comprehensive observation of beach aeolian sand in the Yuandangao beach of Pingtan Island, Fujian Province, this paper aims to explore and summarize the vertical distribution, entrainment and transport characteristics of beach aeolian sand influenced by tide. The main conclusions are as follows:(1) The vertical distribution of wind-sand flow in intertidal zone is almost entirely(98.9%) in the range of 0–30 cm, and the specific distribution function varies with different particle size; (2) The threshold velocity of beach aeolian sand is significantly higher than that of inland desert, and the changing process of it in the tidal circulation mainly reflects the interaction between average surface moisture and fetch length; (3) The wind-blown sand flux of intertidal zone involves the interaction of average surface moisture, fetch length and wind speed, and the dominant factors of its changing process vary in different stages of ebb and flow; (4) Entrainment of sand from a dry source and transport across a moist surface is one of the typical beach aeolian sand transport mode, with a short delivered distance at a time, and a highly relayed way of overall transport.
AB - Coastal aeolian is a typical product of sea, land and air interaction. Based on a comprehensive observation of beach aeolian sand in the Yuandangao beach of Pingtan Island, Fujian Province, this paper aims to explore and summarize the vertical distribution, entrainment and transport characteristics of beach aeolian sand influenced by tide. The main conclusions are as follows:(1) The vertical distribution of wind-sand flow in intertidal zone is almost entirely(98.9%) in the range of 0–30 cm, and the specific distribution function varies with different particle size; (2) The threshold velocity of beach aeolian sand is significantly higher than that of inland desert, and the changing process of it in the tidal circulation mainly reflects the interaction between average surface moisture and fetch length; (3) The wind-blown sand flux of intertidal zone involves the interaction of average surface moisture, fetch length and wind speed, and the dominant factors of its changing process vary in different stages of ebb and flow; (4) Entrainment of sand from a dry source and transport across a moist surface is one of the typical beach aeolian sand transport mode, with a short delivered distance at a time, and a highly relayed way of overall transport.
KW - Beach aeolian sand
KW - Entrainment
KW - Tide
KW - Transport
KW - Vertical distribution
UR - http://www.scopus.com/inward/record.url?scp=85053079694&partnerID=8YFLogxK
U2 - 10.3969/j.issn.0253-4193.2018.09.008
DO - 10.3969/j.issn.0253-4193.2018.09.008
M3 - Article
AN - SCOPUS:85053079694
SN - 0253-4193
VL - 40
SP - 90
EP - 102
JO - Haiyang Xuebao
JF - Haiyang Xuebao
IS - 9
M1 - 0253-4193(2018)09-0090-13
ER -