水土保持地区人类活动对汛期径流影响的估算

朱恒峰; 赵文武; 康慕谊; 郭雯雯

水土保持地区人类活动对汛期径流影响的估算

1.
北京师范大学资源学院, 地表过程与资源生态国家重点实验室, 北京, 100875;
2.
沈阳航空工业学院经济管理学院, 辽宁, 沈阳, 110034

基金项目: 国家重点基础研究发展计划(973)资助项目(2007CB1068061);国家自然科学基金资助项目(40501002)

详细信息

作者简介:
朱恒峰(1977- ),男,辽宁沈阳人,博士研究生,主要从事水土保持与土地资源管理方面的研究.E-mail:zhfsyln@ires.cn

通讯作者:
赵文武,E-mail:zhaoww@bnu.edu.cn

中图分类号: P333.5

Effect of human activities on flood season runoff in water and soil conservation region

1.
State Key Laboratory of Earth Surface Processes and Resource Ecology, College of Resources Science and Technology, Beijing Normal University, Beijing 100875, China;
2.
College of Economy & Management, Shenyang Institute of Aeronautical Engineering, Shenyang 110034, China

Funds: The study is financially supported by the National Natural Science Foundation of China(No.40501002).

摘要: 人类活动对于流域水文要素时变过程的影响显著,确定人类活动影响下水文要素时序的显著转折点、选出相对"天然"的序列,对于开展水土保持效益评价研究具有重要意义。以延河流域为例,采用数理统计方法推估获取人类活动影响下汛期径流时序的显著转折点,以显著转折点前的数据建立预测模型,对比分析汛期径流量的实测值与预测值,其差值即为人类活动对汛期径流的影响程度。较之传统研究方法,本文以汛期水文数据取代年均数据,以汛期降水径流综合系数代替年径流系数,从而减弱了黄土高原地区降水、径流变化幅度巨大的干扰影响。结果表明,从20世纪50年代末至80年代末,1970年为人类活动下延河流域径流时序的显著转折点,1970年以后人类活动对流域水文的影响更显著,1981年达到最大值,为72.04%。20世纪70、80年代人类活动对延河汛期径流量的影响一直处于负面减流状态。人为因素是延河径流量演变的主要驱动因子。
- 水土保持 /
- 延河流域 /
- 人类活动 /
- 汛期 /
- 径流时序
Abstract: Human activities have great influence on runoff temporal change. The detected distinct transition point and relevant selected "unaffected" hydrological series that have great significance to assessment of soil and water conservation benefits. Taking Yanhe as an example,the distinct transition point of flood season runoff time series by the impacts of human activities has been detected by way of mathematical statistics analysis. And meanwhile,based on the datum before distinct transition point, the forecast model is set up only with the data series before the distinct transition point. The difference between the value derived from the equation and the observed value is right the influence on flood season runoff induced by human activities. Different from traditional methods,using hydrological datum and the synthesis coefficient of precipitation and runoff of flood season instead of annual ones,which could rationally weaken the impact of characteristics on rainfall and runoff in Loess Plateau. The analysis shows that 1970 is the transition point of runoff time series by impacts of human activities from the end of 1950s to 1980s,and human activities have affected significantly on hydrology of Yanhe basin since 1970.And in the year of 1981,human influence on river runoff reached maximum,with its value being 72.04%. In the 1970s and 1980s,flood season runoff was confined to reduced state at all times. So human factors is the primary one for the evolvement of Yanhe runoff.
- soil and water conservation /
- Yanhe basin /
- human activities /
- flood season /
- time series of runoff

[1]	杨新,延军平,刘宝元.无定河年径流量变化特征及人为驱动分析[J].地理科学进展,2005(6):637-642.(YANG Xin,YAN Jun-ping,LIU Bao-yuan.The analysis on the change characteristics and driving forces of Wudinghe River runoff[J].Advances in Earth Science,2005,20(6):637-642.(in Chinese))
[2]	张胜利,于一鸣,姚文艺.水土保持减水减沙效益计算方法[M].北京:中国环境科学出版社,1994.(ZHANG Sheng-li,YU Yi-ming,YAO Wen-yi.Study on calculation methods of benefits of soil and water conservation[M].Beijing:China Environmental Sciences Press,1994.(in Chinese))
[3]	KRITSKIY S N,MENKEL M F.Generalized methods for runoff control computations based on mathematical statistics[J].Journal of Hydrology,1995,172:365-377.
[4]	许炯心,孙季.无定河淤地坝拦沙措施时间变化的分析与对策[J].水土保持学报,2006,20(2):26-30.(XU Jiong-xin,SUN Ji.Study of temporal variation of check dam construction in Wudinghe River basin and some suggestion for some countermeasure[J].Journal of Soil and Water Conservation,2006,20(2):26-30.(in Chinese))
[5]	姚文艺,茹玉英,康玲玲.水土保持措施不同配置体系的滞洪减沙效应[J].水土保持学报,2004,18(2):28-31.(YAO Wen-yi,RU Yu-ying,KANG Ling-ling.Effect of flood retention and sediment reduction with different allocation system of water and soil conservation measures[J].Journal Soil and Water Conservation,2004,18(2):28-31.(in Chinese))
[6]	王国庆,贾西安,陈江南,等.人类活动对水文序列的显著影响干扰点分析[J].西北水资源与水工程,2001(3):13-15.(WANG Guo-qing,JIA Xi-an,CHEN Jiang-nan,et al.Analysis on the transition point of hydrological series impacted by human activities[J].Northwest Water Resources & Water Engineering,2001(3):13-15.(in Chinese))
[7]	汪岗,范昭.黄河水沙变化研究(第二卷)[M].郑州:黄河水利出版社,2002.261-304.(WANG Gang,FAN Zhao.Study on variation of runoff and sediment in Yellow River (Volume 2)[M].Zhengzhou:Yellow River Water Conservancy Press,2002.261-304.(in Chinese))
[8]	王国庆,庞慧,荆新爱,等.清涧河流域的水文情势变化阶段及其特征[J].中国水土保持科学,2005,3(2):23-27.(WANG Guo-qing,PANG Hui,JING Xin-ai,et al.Variation phases and its characteristics of hydrological regime of Qingjianhe River basin[J].Science of Soil and Water Conservation,2005,3(2):23-27.(in Chinese))
[9]	徐建华,李雪梅,李世明,等.延河流域水沙还原计算方法探讨[J].人民黄河,1997(8):21-25.(XU Jian-hua,LI Xue-mei,LI Shi-ming,et al.Study on revivification calculation methods of runoff and sediment in Yanhe River basin[J].Yellow River,1997(8):21-25.(in Chinese))
[10]	SHARMH T C.Stochastic models applied to evaluating hydrologic changes[J].Journal of Hydrology,1985,78:61-81.
[11]	鲁志文,莫小平.采用秩相关系数法分析东江干流CODMn变化趋势[J].人民珠江,2006(1):45-46.(LU Zhi-wen,MO Xiao-ping.Study on variation of CODMn using the method of order relational coefficient in the mainstream of Dongjiang River[J].Pearl River,2006(1):45-46.(in Chinese))
[12]	陈全胜,李凌浩,韩兴国,等.典型温带草原群落土壤呼吸温度敏感性与土壤水分的关系[J].生态学报,2004,24(4):831-836.(CHEN Quan-sheng,LI Ling-hao,HAN Xing-guo,et al.Temperature sensitivity of soil respiration in relation to soil moisture in communities of typical temperate steppe in Inner Mongolia[J].Acta Ecologica Sinica,2004,24(4):831-836.(in Chinese))
[13]	刘秀花,杨军,胡秀锦.黄河宁夏段水质现状及变化趋势分析[J].人民黄河,2006,28(3):57-58.(LIU Xiu-hua,YANG Jun,HU Xiu-jin.Analysis on actuality and trend of water quality of Ningxia section of the Yellow River[J].Yellow River,2006,28(3):57-58.(in Chinese))
[14]	汪岗,范昭.黄河水沙变化研究(第一卷)[M].郑州:黄河水利出版社,2002.717-736.(WANG Gang,FAN Zhao.Study on variation of runoff and sediment in Yellow River (Volume 1)[M].Zhengzhou:Yellow River Water Conservancy Press,2002.717-736.(in Chinese))
[15]	许炯心.无定河流域侵蚀产沙过程对水土保持措施的响应[J].地理学报,2004(6):972-981.(XU Jiong-xin.Response of erosion and sediment producing processes to soil and water conservation measures in the Wudinghe River basin[J].Acta Geographica Sinica,2004,59(6):972-981.(in Chinese))
[16]	徐学选,穆兴民,王炜.基于水土保持的延河流域治理水文响应模型[J].中国水土保持科学,2003(4):20-24.(XU Xue-xuan,MU Xing-min,WANG Wei.Hydrological Response model on soil and water conservation in Yanhe River basin[J].Science of Soil and Water Conservation,2003(4):20-24.(in Chinese))

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水土保持地区人类活动对汛期径流影响的估算

作者简介:
朱恒峰(1977- ),男,辽宁沈阳人,博士研究生,主要从事水土保持与土地资源管理方面的研究.E-mail:zhfsyln@ires.cn

通讯作者:
赵文武,E-mail:zhaoww@bnu.edu.cn

Effect of human activities on flood season runoff in water and soil conservation region

计量

水土保持地区人类活动对汛期径流影响的估算

1. 北京师范大学资源学院, 地表过程与资源生态国家重点实验室, 北京, 100875;

2. 沈阳航空工业学院经济管理学院, 辽宁, 沈阳, 110034

作者简介:
朱恒峰(1977- ),男,辽宁沈阳人,博士研究生,主要从事水土保持与土地资源管理方面的研究.E-mail:zhfsyln@ires.cn

通讯作者: 赵文武,E-mail:zhaoww@bnu.edu.cn

English Abstract

Effect of human activities on flood season runoff in water and soil conservation region

1. State Key Laboratory of Earth Surface Processes and Resource Ecology, College of Resources Science and Technology, Beijing Normal University, Beijing 100875, China;

2. College of Economy & Management, Shenyang Institute of Aeronautical Engineering, Shenyang 110034, China

全文HTML

目录

留言板

水土保持地区人类活动对汛期径流影响的估算

作者简介: 朱恒峰(1977- ),男,辽宁沈阳人,博士研究生,主要从事水土保持与土地资源管理方面的研究.E-mail:zhfsyln@ires.cn

通讯作者: 赵文武,E-mail:zhaoww@bnu.edu.cn

Effect of human activities on flood season runoff in water and soil conservation region

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出版历程

水土保持地区人类活动对汛期径流影响的估算

1. 北京师范大学资源学院, 地表过程与资源生态国家重点实验室, 北京, 100875; 2. 沈阳航空工业学院经济管理学院, 辽宁, 沈阳, 110034

作者简介: 朱恒峰(1977- ),男,辽宁沈阳人,博士研究生,主要从事水土保持与土地资源管理方面的研究.E-mail:zhfsyln@ires.cn

通讯作者: 赵文武,E-mail:zhaoww@bnu.edu.cn

English Abstract

Effect of human activities on flood season runoff in water and soil conservation region

1. State Key Laboratory of Earth Surface Processes and Resource Ecology, College of Resources Science and Technology, Beijing Normal University, Beijing 100875, China; 2. College of Economy & Management, Shenyang Institute of Aeronautical Engineering, Shenyang 110034, China

全文HTML

目录

作者简介:
朱恒峰(1977- ),男,辽宁沈阳人,博士研究生,主要从事水土保持与土地资源管理方面的研究.E-mail:zhfsyln@ires.cn

通讯作者:
赵文武,E-mail:zhaoww@bnu.edu.cn

1. 北京师范大学资源学院, 地表过程与资源生态国家重点实验室, 北京, 100875;

2. 沈阳航空工业学院经济管理学院, 辽宁, 沈阳, 110034

作者简介:
朱恒峰(1977- ),男,辽宁沈阳人,博士研究生,主要从事水土保持与土地资源管理方面的研究.E-mail:zhfsyln@ires.cn

1. State Key Laboratory of Earth Surface Processes and Resource Ecology, College of Resources Science and Technology, Beijing Normal University, Beijing 100875, China;

2. College of Economy & Management, Shenyang Institute of Aeronautical Engineering, Shenyang 110034, China