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霍林河中游径流量序列的多时间尺度特征及其效应分析
引用本文:卢晓宁,邓伟,张树清,翟金良.霍林河中游径流量序列的多时间尺度特征及其效应分析[J].自然资源学报,2006,21(5):819-826.
作者姓名:卢晓宁  邓伟  张树清  翟金良
作者单位:1. 中国科学院东北地理与农业生态研究所,长春130012;
2. 中国科学院水利部成都山地灾害与环境研究所,成都610041;
3. 中国科学院,北京100864;
4. 中国科学院研究生院,北京100049
摘    要:霍林河是松嫩平原西部地区科尔沁、向海和查干湖湿地的重要补给水源。通过对其中游白云胡硕水文测站46a的年径流量序列的多时间尺度分析,探讨霍林河径流演变的近似周期性,识别霍林河径流变化对其下游洪泛湿地水源补给的规律,以及这种规律控制下的洪泛湿地环境演变。小波分析表明,霍林河白云胡硕水文站年径流序列主要存在3个尺度的周期变化,不同时间尺度下周期信号的强弱在时频域中的分布具有较强的局部特征,以大于30a尺度的年代际周期变化起主导作用,该尺度下,霍林河径流演变呈现出丰、枯、丰的交替振荡,下游洪泛湿地景观演变相应表现出阶段性特征,1990年代以前尤为突出。能量相对较弱的中、小时间尺度径流量周期性变化,与强烈的人类干扰活动相比,对下游洪泛湿地环境演变的作用效果不明显,突出表现在1990年代以后。

关 键 词:霍林河  洪泛湿地  小波分析  多时间尺度  环境演变  
文章编号:1000-3037(2006)05-0819-08
收稿时间:2006-01-06
修稿时间:2006-03-26

Multiple Time-scale Characteristics of Flow Variations in the Middle Huolin River and Corresponding Effects Analysis
LU Xiao-ning,DENG Wei,ZHANG Shu-qing,ZHAI Jing-liang.Multiple Time-scale Characteristics of Flow Variations in the Middle Huolin River and Corresponding Effects Analysis[J].Journal of Natural Resources,2006,21(5):819-826.
Authors:LU Xiao-ning  DENG Wei  ZHANG Shu-qing  ZHAI Jing-liang
Institution:1. Northeast Institute of Geography & Agricultural Ecology,CAS,Changchun 130012,China;
2. Institute of Mountain Hazards and Environment,CAS,Changdu 610041,China;
3. Graduate University of Chinese Academy of Sciences,Beijing 100049,China;
4. Chinese Academy of Sciences,Beijing 100864,China
Abstract:Huolin River is one of the most important water supply sources for the Xianghai,Kerqin,and Chaganhu wetlands in the west Songnen Plain.A multiple time-scale analysis was used to analyze an annual flow series of 46 years of the Baiyunhushuo hydrologic station,which is located at the middle reaches of Huolin River.Our main objective was to discuss the periodic characteristics of the flow series,and examine the temporal patterns of the Huolin River recharging into floodplain wetlands in its lower reaches,and its corresponding effects exerted on downstream floodplain wetlands environmental evolutions.Wavelet analysis showed that the annual flow of Baiyunhushuo hydrologic station varied mainly in three time scales.The intensity of periodical signals of different time scales was strongly partially distributed in its time-frequency domain.More than 30 years interdecadal variation played a leading role in the temporal pattern,and showed a scale increasing tendency.At this scale,the flow of Baiyunhushuo hydrologic station in the Huolin river presented an alternative fluctuation of rain,draught and rain.Accordingly,the landscape of floodplain wetlands in downstream area presented a periodic feature,it is especially prominent before the 1990s.Compared with intense human activities,the periodic flow patterns of middle and small scales with relative low energy,have unobvious effects on wetlands environmental evolvement,it is especially distinctive after the 1990s.It should be noted that the dual actions of flow evolution of natural factors and human disturbances exerted influences of different degrees on flow signals in different periods.A further discussion should be made regarding the influencing factors,including precipitations,evaporations and human disturbances,for figuring out the reason and role of floodplain wetland landscape evolutions,thereby bringing forward scientific and feasible measures for the protection and restoration of wetland ecosystems.Rationally allocating and managing water resources,reducing river regulation and abstraction actions would be in favor of the protection of the existing wetlands ecosystem and the restoration of degeneration ones in the basin.
Keywords:Huolin River  floodplain wetlands  runoff  wavelet analysis  multiple time scalefeature  environmental evolution
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