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地貌学家对砾石河河道渠化工程方法的批判:以波兰喀尔巴阡山脉的拉巴河为例

A geomorphologist's criticism of the engineering approach to channelization of gravel-bed rivers: case study of the Raba River, Polish Carpathians.

作者信息

Wyzga B

机构信息

Institute of Nature Conservation, Polish Academy of Sciences, Kraków.

出版信息

Environ Manage. 2001 Sep;28(3):341-58. doi: 10.1007/s0026702454.

DOI:10.1007/s0026702454
PMID:11531237
Abstract

River engineers use sediment transport formulas to design regulated channels in which the river's ability to transport bedload would remain in equilibrium with the delivery of materials from upstream. In gravel-bed rivers, a number of factors distort the simple relationship between particle size and hydraulic parameters at the threshold of sediment motion, inherent in the formulas. This may lead to significant errors in predicting the bedload transport rates in such streams and hence to instability of their regulated channels. The failure to recognize a nonstationary river regime may also result in unsuccessful channelization. Rapid channel incision has followed channelization of the main rivers of the Polish Carpathians in the 20th century. A case study of the Raba River shows that incision has resulted from the increase in stream power caused by channelization and the simultaneous reduction in sediment supply due to variations in basin management and a change in flood hydrographs. Calculations of bedload transport in the river by the Meyer-Peter and Müller formula are shown to have resulted in unrealistic estimates, perhaps because the different degree of bed armoring in particular cross-sections was neglected. It would have been possible to avoid improper channelization if the decreasing trend in sediment load of the Carpathian rivers had been recognized on the basis of geomorphological and sedimentological studies. Allowing the rivers to increase their sinuosity, wherever possible without an erosional threat to property and infrastructure, and preventing further instream gravel mining are postulated in order to arrest channel incision and reestablish the conditions for water and sediment storage on the floodplains.

摘要

河流工程师利用泥沙输运公式来设计整治河道,使河流输运推移质的能力与上游来沙量保持平衡。在砾石河床河流中,一些因素会扭曲公式中固有的泥沙起动临界粒径与水力参数之间的简单关系。这可能导致预测此类河流中推移质输运速率时出现重大误差,进而导致其整治河道不稳定。未能认识到非稳定河流水文情势也可能导致河道整治失败。20世纪波兰喀尔巴阡山脉主要河流进行河道整治后出现了快速的河道下切。对拉巴河的案例研究表明,下切是由于河道整治导致水流功率增加,以及流域管理变化和洪水过程线改变导致泥沙供应量同时减少所致。结果表明,用迈耶 - 彼得和米勒公式计算该河流的推移质输运得出了不切实际的估计值,可能是因为忽略了特定断面不同程度的河床糙化。如果根据地貌学和沉积学研究认识到喀尔巴阡山脉河流泥沙负荷的下降趋势,就有可能避免不当的河道整治。建议尽可能允许河流增加弯曲度,只要不对财产和基础设施造成侵蚀威胁,并防止进一步的河道内砾石开采,以阻止河道下切,并重新建立漫滩蓄水和泥沙淤积的条件。

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