卡特里娜和丽塔风造成的湿地沉积
R Eugene Turner1, Joseph J Baustian, Erick M Swenson
1Coastal Ecology Institute, Louisiana State University, Baton Rouge, LA 70803, USA. euturne@lsu.edu
概括
卡特里娜和里塔风在路易斯安那州沿海湿地沉积了超过1.31亿公 (MT) 的无机沉积物. 这种由风驱动的沉积堆积量很大,可能支持健康的盐沼.
科学领域:
- 沿海地质的地质学
- 沉积物学的沉积物学
- 环境科学环境科学
背景情况:
- 2005年,卡特里娜和里塔风对路易斯安那州的海岸造成了重大影响.
- 了解沉积物动态对于沿海湿地恢复和弹性至关重要.
研究的目的:
- 为了量化路易斯安那州沿海湿地在风卡特里娜和丽塔之后的无机沉积物的积累.
- 为了将风驱动的沉积物负载与其他沉积物来源进行比较,包括密西西比河和湿地恢复工作.
主要方法:
- 根据卡特里娜和丽塔风报告的数据计算沉积物积累.
- 风沉积物负载与密西西比河悬浮负载和历史上岸洪水数据的比较.
- 评估沉积物对修建的河流转移用于湿地恢复的贡献.
主要成果:
- 超过131×106米 (MT) 的无机沉积物直接从卡特里娜和丽塔风中积累在沿海湿地.
- 每次风每年的沉积积量是密西西比河悬浮载荷的12%.
- 风沉积物负载是风前海平面上岸洪水的5.5倍,是恢复河流转移的227倍.
结论:
- 风引起的沉积沉积是沿海湿地环境的重要因素.
- 这些风沉积的沉积物体积足以解释健康的盐沼中发现的无机沉积物.
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