海岸动力地貌中均衡理论模式和扩散理论模式的几个基本特征SOME PRINCIPAL CHARACTERISTICS OF THE EQUILIBRIUM AND DIFFUSSION THEORITICAL MODEL IN COASTAL GEOMORPHOLOGY
崔承琦
摘要(Abstract)：
<正> 多年来各国学者A. R. Emy(1831), E. Beaumont(1845), Cialdi(1866), P. Cornaglia(1891), N. M. Fenneman(1902), В. П. Зенкович(1946, 1962), D. L. Inman, A. J. Bowen(1956), W. A. Price(1969), P. D. Komar(1976)等,分别从海岸动力地貌学、水工学、水文学和地质学等不同学科出发,通过各种途径对波场冲积物运动的基本特征及
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作者(Author): 崔承琦
DOI: 10.16441/j.cnki.hdxb.1983.03.002
参考文献(References)：
- 参见任美锷，最近海滩研究的发展(南京大学科技资料，1975)
- (1) C. A. M. King, Beaches and Coasts(First published, 1959) Printed in Great Britain.
- (2) D. W. Johnson, Shore Processes and Shoreline Development(Columlia University).
- (3) P. D. Komar, Beach Processes and Sedimentation, 1976Prentice-Hall INE., Englewood Cliffs, Wow Jersey. Printed in the United States of America(P288-321) .
- (4) W. A. Price, Variable dispersion and Its Effects on the Movements of Tracers on Beaches. Proc. 11th Conf. on Coast. Eng, PP329-334．
- (5) 1962, (p79～128, p303～426) .
- (6) 1961(p55～142) .
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