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雅鲁藏布江中游悬移质输沙率的周期性与不均匀性分析

An Analysis of the Periodicity and Inhomogeneity of Suspended Sediment Transport Rates in the Middle Reaches of Yarlung Zangbo River

  • 摘要: 悬移质是河流生源物质输运的重要载体,阐明河流中悬移质输沙率的时间变化特征可为了解河流生态节律提供基础信息。基于雅鲁藏布江中游奴各沙、羊村、奴下水文监测站点1956-2000年共45年逐月悬移质输沙率、流量监测数据,通过建立水沙关系曲线对缺测部分进行插补,采用Morlet小波变换、集中度和集中期分析方法探讨该流域不同时间尺度下的输沙变化特性,结果表明:雅江中游各站点悬移质输沙率序列表现出多时间尺度的周期变化,并在第一主周期19年、第二主周期26年、第三主周期10年,第四主周期6年上保持较高的空间一致性,输沙率短周期变化与太阳活动、气候事件的周期变化存在一定的响应;三个站点最大输沙率主要发生在7、8月,集中度分别为0.83、0.77、0.74,受局部气候差异影响,输沙率在年内的分配不均匀性顺河流方向逐渐降低;受降雨和人类活动影响,输沙率序列在1964年突变,呈现先增大后减小的趋势,降雨对输沙率减小影响的贡献率分别为38.62%、41.04%、-38.15%,人类活动对输沙率减小影响的贡献率分别为61.38%、58.96%、138.15%。研究初步阐明了雅江中游在基本未受大型水利工程干扰情形下悬移质输运过程的多时间尺度变化特征及主要控制因素,可为雅鲁藏布江水生态保护提供水沙过程的天然态参考系。

     

    Abstract: Suspended sediment is an important carrier of river biogenic material transportation. Clarifying the temporal change characteristics of suspended sediment transport rates in rivers can provide basic information for understanding river ecological rhythms. This paper studies the monthly monitoring data of suspended sediment transport rates and discharge from 1956 to 2000 at the Nugesha,Yangcun,and Nuxia hydrological monitoring stations in the middle reaches of the Yarlung Zangbo River. The missing periods are interpolated by using an established water-sediment relationship. Morlet wavelet transforms,concentration degree and concentration period analysis methods are then used to explore the characteristics of sediment transport changes under different time scales in the watershed. The results show that the suspended sediment transport rates series from the three stations all assumed periodic changes in multiple time scales,maintaining a highly spatial consistency with their four major cycles being 19 years,26 years,10 years,and 6 years,respectively. There is a certain response between the short-period changes of sediment transport rates and the periodic changes of solar activity and climate events. The maximum sediment transport rate of the three stations mainly occurs in July and August,and the concentration degrees are 0.83,0.77,0.74,respectively. Affected by differences of local meteorological condition,the uneven distribution of sediment transport rates during the year gradually decrease along the river. Moreover,the sediment transport rate showed an abrupt change in 1964 when an increasing trend changed into a decreasing trend.Precipitation and human activity are believed to contribute to this reduction,with the contribution rate from precipitation in the three stations were 38.62%,41.04%,and-38.15%,respectively,and the contribution rate from human activity were 61.38%,58.96%,and 138.15%,respectively. This study preliminarily clarifies the multi-time-scale variation characteristics and main control factors of the suspended sediments transport process in the middle reaches of the Yarlung Zanbo River when there are no obvious disturbs from large-scale water conservancy projects,which can provide a natural state reference system for ecological protection in the Yarlung Zangbo River.

     

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