概括
三角洲的地形是由沿海的波浪力量和河流排放形成的. 靠近海岸的波浪能量受到水下坡度和沉积物供应的影响,决定了河流或波浪力量是否主导沿海形态.
科学领域:
- 地质形态学 地质形态学
- 海洋学 海洋学 海洋学
- 沉积物学的沉积物学
背景情况:
- 三角洲海岸线呈现出多样化的地形结构.
- 了解河流和海洋过程之间的相互作用对于沿海研究至关重要.
研究的目的:
- 研究波浪气候,河流排水和三角洲地形发展之间的关系.
- 确定控制近岸波浪功率的因素及其对沿海形态的影响.
主要方法:
- 在七个主要的三角洲地区实施了全面的波浪气候计划.
- 分析了深水和近岸波浪功率之间的相关性.
- 评估了水下坡度,大陆架特征和河流沉积物供应的影响.
主要成果:
- 三角洲的构造受到近岸波浪力和相对河流排放的显著影响.
- 靠近海岸的波浪电力主要取决于水下坡度,而不是深水的波浪电力.
- 水下坡度取决于大陆架的特性,最重要的是,取决于河流沉积物供应率.
结论:
- 河流主导的三角洲地形形成时,河流形成平坦的海上配置文件,减少近岸波浪能量.
- 波浪占主导地位的沿海地形占主导地位,在那里的水下坡道允许波浪以不减弱的力量到达岸边.
- 沉积物供应率是水下斜坡的首要控制,因此,在沿海地形上也是如此.
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