检索规则说明:AND代表“并且”;OR代表“或者”;NOT代表“不包含”;(注意必须大写,运算符两边需空一格)
检 索 范 例 :范例一: (K=图书馆学 OR K=情报学) AND A=范并思 范例二:J=计算机应用与软件 AND (U=C++ OR U=Basic) NOT M=Visual
作 者:李舒[1,2] 李宁波 齐青松 白乐 姚曼飞[3] 刘兵兵 LI Shu;LI Ningbo;QI Qingsong;BAI Le;YAO Manfei;LIU Bingbing(Department of Water Resources,Yellow River Institute of Hydraulic Research,Zhengzhou 450003,China;Henan Key Laboratory of Ecological Environment Protection and Restoration of Yellow River Basin,Zhengzhou 450003,China;School of Water Conservancy,North China University of Water Resources and Electric Power,Zhengzhou 450045,China;College of Hydrology and Water Resources,Hohai University,Nanjing 210098,China)
机构地区:[1]黄河水利科学研究院水资源研究所,河南郑州450003 [2]河南省黄河流域生态环境保护与修复重点实验室,河南郑州450003 [3]华北水利水电大学水利学院,河南郑州450045 [4]河海大学水文水资源学院,江苏南京210098
出 处:《人民黄河》2021年第4期50-53,116,共5页Yellow River
基 金:“十三五”国家重点研发计划项目(2017YFC0403505);河南省自然科学基金资助项目(202300410542)。
摘 要:为了明晰不同人类活动对流域水文情势的影响效果,基于窟野河径流控制站温家川水文站1954—2016年的日径流数据,采用动态时间弯曲(Dynamic Time Warping,DTW)算法分析了不同人类活动影响期的水文情势相似度。结果表明:①水土保持措施和煤矿开采均大幅减小了窟野河的径流量,其中煤矿开采的采空区储存水量减水效应大于水土保持措施涵养水源的作用;②人类活动弱干扰时期(第一时期)、水土保持时期(第二时期)和煤矿开采时期(第三时期)两两之间的DTW距离分别为0.13(第一、二时期)、0.19(第一、三时期)和0.17(第二、三时期),说明水土保持措施和煤矿开采对流域水文情势的影响效果较为相似;③煤矿开采对非汛期流量、基流的影响历时、最大流量出现时间、大/小流量出现次数的影响均比水土保持措施明显。In order to clarify the effects of different human activities on hydrological regime,this paper analyzed the hydrological regime similarity in different anthropogenic influence phases by using Dynamic Time Warping(DTW),based on the daily runoff from 1954 to 2016 in Wenjiachuan Hydrologic Station.The results show that:a)both soil and water conservation and coal mining have made a considerable reduction of the river runoff.The effect of water stored by coal mining goaf is larger than that by soil and water conservation;b)the DTW distance during weak anthropogenic influence(stageⅠ),soil and water conservation(stageⅡ)and coal mining(stageⅢ)is 0.13 between the stageⅠandⅡ,0.19 between the stageⅠandⅢ,and 0.17 between the stageⅡandⅢrespectively;c)and the effect of coal mining is more obvious than that of soil and water conservation in the runoff of nonflood season,effective duration of base flow,the occurrence time of maximum runoff and high or low flow pulse time.
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在链接到云南高校图书馆文献保障联盟下载...
云南高校图书馆联盟文献共享服务平台 版权所有©
您的IP:216.73.216.15