自然流和水力发动机厂的遗产
Robert C Walter1, Dorothy J Merritts
1Department of Earth and Environment, Franklin and Marshall College, Post Office Box 3003, Lancaster, PA 17604-3003, USA. robert.walter@fandm.edu
概括
历史上,大西洋中部的河流是湿地中的分支道,而不是曲的河流. 工厂水导致沉积物堆积,创造了人造的洪水平原,挑战了河流恢复模型.
科学领域:
- 地质形态学 地质形态学
- 环境历史 环境历史
- 恢复生态学 恢复生态学
背景情况:
- 石床流被广泛模拟为曲的河流,带有细粒度的洪水平原.
- 这种模式影响了大量的河流恢复工作.
研究的目的:
- 重新评估大西洋中部河流的历史地形学.
- 研究现代洪水平原的形成,并挑战现有的溪流模型.
主要方法:
- 地质地图绘制和河流沉积物的年代.
- 对历史地图和记录进行分析.
主要成果:
- 定居前的河流是湿地内的分支道,储存有机碳.
- 在17世纪至19世纪的磨坊水后面,1-5米的沉积沉积埋葬了这些湿地.
- 大多数大西洋中部的洪水平原被确定为人工填充露台.
结论:
- 流和洪水平原的广泛接受的模型是基于人类改变的景观.
- 历史上切割的道不是流恢复的自然原型.
- 恢复实践可能需要根据定居前的湿地条件重新评估.
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