泥石流与主河汇流堆积的数值模拟
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摘要
汶川大地震使震区周围的山体出现大量崩塌、滑坡,为泥石流灾害发育提供了丰富的固体物源.一旦降雨条件适宜,很容易形成山洪泥石流.山洪泥石流来流量大,结构较强,与主河汇流时,难以被主河水流及时冲刷,在汇流区大量堆积,从而引发一系列的灾害.本文在前人的研究成果和相关资料的基础上,对交汇区泥石流与主河水流间的相互作用关系进行了合理简化,采用处理对流项有较好计算稳定性的有限元特征分裂算法,建立了与主河汇流的泥石流堆积数学模型.运用本文模型,再现了文家沟特大山洪泥石流在绵远河的堆积过程,分析了泥石流堆积对主河流路、水深、流速分布等的影响.采用实测堆积地形对计算成果进行了验证,结果表明,本文模型计算泥石流堆积范围,堆积厚度分布,在规律上与实测地形基本一致最后,文章对模型未来改进方向进行了探讨.
引文
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