Open Access Article
Engineering Construction & Innovation DOI: .
*通讯作者: 无
发布时间: 2026-07-14 总浏览量: 5
运用量化的手段来研究高寒山区泥石流易发程度及时空分布的规律。根据系统的、科学的指标体系,将地形地质、 气候条件以及生态保护等各方面数据进行综合,使用分层评分法评定区域泥石流灾害风险等级。利用历史监测数据和 生态变化趋势,对泥石流事件未来的发展趋向做预测分析。研究成果给该地区灾害防控给予精确的数据支撑与理论 根据。
This paper uses quantitative methods to study debris flow susceptibility and the spatial-temporal distribution patterns of debris flow disasters in high-altitude cold mountainous areas. Based on a systematic and scientific indicator system, data on topography and geology, climatic conditions, ecological protection, and other factors are comprehensively integrated, and the hierarchical scoring method is used to evaluate regional debris flow disaster risk levels. By using historical monitoring data and ecological change trends, the future development trends of debris flow events are predicted and analyzed. The research findings provide accurate data support and theoretical basis for disaster prevention and control in the region.
[1]葛超.错玖沟泥石流运动特征研究及危害评价[J].铁道工程学报,2023,40(12):30-35+54.
[2]顾畛逵,姚鑫,李凌婧,等.河流功率梯度在泥石流空间易发程度调查中的应用:以金沙江流域为例[J].地质力学学报,2023,29(1):87-98.
[3]张鑫.XX 沟谷流域泥石流易发程度分析[J].西部探矿工程,2021,33(12):11-13.
[4]付锦涛.基于神经网络模型的都(江堰)四(姑娘山)线泥石流易发性评价研究[D].西南交通大学,2020.
[5]严松.尼洋河中下游高寒山区泥石流发育规律和危险性评价研究[D].成都理工大学,2018.