TY - GEN
T1 - The study on profile shaping process of Northern Yellow River delta coast
AU - Ying, Ming
AU - Li, Jiufa
AU - Li, Weihua
AU - Shi, Lianqiang
AU - Chen, Shenliang
PY - 2005
Y1 - 2005
N2 - As terminal reach of Yellow River has changed greatly for 10 times since 1855, the modern Yellow River Delta has been formed. From 1965 to 1976, terminal reach Is Diaokou Channel, mass unconsolidated deposit was produced on front slope of northern Yellow River Delta. After terminal reach's shifting to Qingshuigou in 1976, the seashore was eroded and the coastal line moved back rapidly. This threatened normal production of Shengli Oil Field which is the second largest oil field In China. It is the base of carrying out coastal protection engineering efficaciously to grasp the profile shaping process and law of evolution. Since 1970s, 8 profiles have been observed in the Northern Yellow River delta coast. In order to get rid of dynamic change because of recession, drawback distance is considered to be the metadata for analyze. Time and space shaping characteristic is discussed. The Quasi-equilibrium zone is existent in silt coast profile, and float by dynamic condition.
AB - As terminal reach of Yellow River has changed greatly for 10 times since 1855, the modern Yellow River Delta has been formed. From 1965 to 1976, terminal reach Is Diaokou Channel, mass unconsolidated deposit was produced on front slope of northern Yellow River Delta. After terminal reach's shifting to Qingshuigou in 1976, the seashore was eroded and the coastal line moved back rapidly. This threatened normal production of Shengli Oil Field which is the second largest oil field In China. It is the base of carrying out coastal protection engineering efficaciously to grasp the profile shaping process and law of evolution. Since 1970s, 8 profiles have been observed in the Northern Yellow River delta coast. In order to get rid of dynamic change because of recession, drawback distance is considered to be the metadata for analyze. Time and space shaping characteristic is discussed. The Quasi-equilibrium zone is existent in silt coast profile, and float by dynamic condition.
KW - Profile
KW - Quasi-equilibrium zone
KW - Shaping Process
KW - Yellow River delta
UR - https://www.scopus.com/pages/publications/33745700056
U2 - 10.1109/IGARSS.2005.1525962
DO - 10.1109/IGARSS.2005.1525962
M3 - 会议稿件
AN - SCOPUS:33745700056
SN - 0780390504
SN - 9780780390508
T3 - International Geoscience and Remote Sensing Symposium (IGARSS)
SP - 5404
EP - 5407
BT - 25th Anniversary IGARSS 2005
T2 - 2005 IEEE International Geoscience and Remote Sensing Symposium, IGARSS 2005
Y2 - 25 July 2005 through 29 July 2005
ER -