福建九龙江河口湾水下沉积近期变迁的初步研究
AN INITIAL STUDY ON THE RECENT VICISSITUDES OF UNDERWATER DEPOSIT AT THE JIULONG RIVER ESTUARY IN FUJIAN
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摘要: 九龙江是福建省第二大河。该河的河口湾在厦门嵩屿—龙海屿仔尾一线以西及河口三角洲(浒茂洲等)以东的水域,由于处于闽南厦、漳、泉三角地区,毗邻厦门港,其自然变迁情况直接关系着地区的经济开发,有着不少需要研究的课题。例如为制定厦门港扩建规划,就需要了解河口湾砂洲的推移情况,研究水下沉积及其近期变迁的特点。笔者曾在此河口湾参加过两次沉积调查。两次调查季节均属枯水期,相距已有二十年。Abstract: The Jiulong River is the second longest river in Fujian Province. The lower part of the estuary is of sinking type. It lies to the west of the area along Songyu of Xiamen and Yuziwei of Longhai County. Its natural change has a close relation to the economic development of "Thriangular Area"(Xiamen一Zhangzhou一Q uanzhou)in the south of F ujian Province. So. there are quite a few subjects to be studied there For example, it is necessary to know the case of lapse of sandband at the estuary and the changing features of underw ater deposit for m eking plains to transform-the Xiamen Harobur.
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[1] 北京大学、南京大学等地理系合编，1979，地貌学，人民教育出版社。 [2] K,R,Dper, 1982，河口和河口沉积作用，海洋译丛，第3期。 -
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