LIU Shasha, WANG Houjie, ZHANG Yong, BI Naishuang. IMPACTS OF CLIMATE CHANGE AND HUMAN ACTIVITY ON SEDIMENT DISCHARGE IN THE MIDDLE REACH OF THE YELLOW RIVER[J]. Marine Geology & Quaternary Geology, 2014, 34(4): 41-50. DOI: 10.3724/SP.J.1140.2014.04041
Citation: LIU Shasha, WANG Houjie, ZHANG Yong, BI Naishuang. IMPACTS OF CLIMATE CHANGE AND HUMAN ACTIVITY ON SEDIMENT DISCHARGE IN THE MIDDLE REACH OF THE YELLOW RIVER[J]. Marine Geology & Quaternary Geology, 2014, 34(4): 41-50. DOI: 10.3724/SP.J.1140.2014.04041

IMPACTS OF CLIMATE CHANGE AND HUMAN ACTIVITY ON SEDIMENT DISCHARGE IN THE MIDDLE REACH OF THE YELLOW RIVER

More Information
  • Received Date: July 23, 2013
  • Revised Date: October 09, 2013
  • Based on the hydrological study and correlation analysis, yearly/monthly datasets of precipitation, water discharge and sediment load from the main gauging stations of the Yellow River during the period of 1951-2011 are collected. Data suggests that the sediment load during the flood seasons (May to October) of the four phases of 1951-1968, 1969-1986, 1987-1999 and 2000-2011 is 88.46%, 88.79%, 90.41%, 95.94% respectively. And a statistical model denoting the relationship between precipitation and sediment load is built for the base phase and the first phase. According to the estimation of the model, the contribution of anthropogenic activities to the sediment load increases with time. During the latest period (2000-2011), the sediment load was basically contributed by human activities (e. g., the Xiaolangdi Reservoir), and the contribution of climate change (especially the rainfall) was less than 1%. It designates that the Yellow River drainage system has been severely reversed in the past 61 years. Now the sediment budget of the Yellow River is mainly controlled by human activities instead of the nature and it will bring great impact onto the development of the Yellow River delta.
  • [1]
    Milliman J D, Meade R H. World-wide delivery of river sediment to the oceans. Journal of Geology, 1983, 91, 1-21.
    [2]
    Meade R H. River-sediment inputs to major deltas[C]//Sea-Level Rise and Coastal Subsidence. Kluwer, London, 1996.
    [3]
    毕乃双. 黄河三角洲毗邻海域悬浮泥沙扩散和季节性变化及冲淤效应:[博士论文]. 青岛:中国海洋大学. 2009.[BI Naishuang. Suspended sediment dispersal off the Huanghe (Yellow River) Delta and in its adjacent Bohai Sea, its seasonal variation and effect on delta erosion-accumulation[Ph. D thesis], Qingdao:Ocean University of China, 2009.]
    [4]
    WANG H, YANG Z, SAITO Y, et al. Stepwise decreases of the Huanghe (Yellow River) sediment load (1950-2005):Impacts of climate change and human activities[J]. Global and Planetary Change, 2007, 57(3-4):331-354.
    [5]
    Wang Houjie, Yang Zuosheng, Yoshiki Saito, et al. Interannual and seasonal variation of the Huanghe water discharge over the past 50years:Connections to impacts from ENSO events and dams[J]. Global and Planetary Change, 2006, (50):212-225.
    [6]
    Glantz M H, Katz R W, Nicholls N Teleconnections linking World Wide Climatic Anomalies[M]. Cambridge University Press, Cambridge, UK, 1991.
    [7]
    林豆. 黄土区流域径流对水土保持措施响应的时空变化特征:[博士论文]. 北京:中国科学院教育部水土保持与生态环境研究中心, 2010.[LIN Dou. Temporal-spatial responses of river flow to the Water-soil conservation program in the Loess region[Ph. D thesis], Beijing:Institute of Soil and Water Conservation, CAS, 2010.]
    [8]
    周月鲁. 新时期黄河水土保持创新发展的探索与实践[J]. 中国水土保持. 2006(10):5-9.[ZHOU Yuelu. Exploration and practice of advanced soil and water conservation program of the Yellow River[J]. Soil Water Conservation in China, 2006

    , (10):5-9.]
    [9]
    吴保生, 夏军强, 王兆印. 三门峡水库淤积及潼关高程的滞后效应[J]. 泥沙研究. 2006, 2(1):9-16.

    [WU Baosheng, XIA Junqiang, WANG Zhaoyin. Delayed response of Tongguan's elevation to the sedimentation in Sanmenxia Reservoir[J]. Journal of Sediment Research, 2006, 2(1), 9-16.]
    [10]
    康志强. 退耕还林工程效益评价:[硕士学位论文]. 呼和浩特:内蒙古农业大学, 2011.[KANG Zhiqiang. The cost-benefit analysis after Converting Agricultural Lands to Forest[Master thesis], Hohhot:Inner Mongolia Agricultural University, 2011.]
    [11]
    Lan Yongchao, Kang Ersi, Ma Quanjie, et al. Runoff forecast model for inflow to the Longyangxia Reservoir in the upper Yellow River basin during spring[J]. Journal of Glaciology and Geocryology, 1999, 21(4):391-395.
  • Related Articles

    [1]CHENG Yu, HAO Shefeng, ZOU Xinqing, LUO Ding, GAO Bingfei, YUAN Feng, XU Kang. Millennium-scale coastline changes and sedimentary environment evolution in the incised valley of the Yangtze River Delta since the Holocene[J]. Marine Geology & Quaternary Geology. DOI: 10.16562/j.cnki.0256-1492.2024040701
    [2]ZHENG Siqi, LIN Zhenwen, LI Chu’an, LI Guanhua, ZHUANG Wenming, LI Shiying, LUO Junchao, YANG Feng, LI Yulong. Discussion on the Quaternary initial sedimentary age and sedimentary evolution in the Pearl River Delta[J]. Marine Geology & Quaternary Geology, 2023, 43(6): 145-156. DOI: 10.16562/j.cnki.0256-1492.2023033001
    [3]LU Hongyu, JIANG Shoujun, HUANG Kongwen, CHEN Cong, TANG Yongjie, LI Hongwei, HUANG Ping, HUANG Kangyou. Sedimentary sequences in response to marine transgression during the late Quaternary, Pearl River delta[J]. Marine Geology & Quaternary Geology, 2023, 43(2): 18-30. DOI: 10.16562/j.cnki.0256-1492.2022072102
    [4]ZHANG Shaoxuan, TANG Yongjie, ZHENG Cuimei, CHEN Zhen, ZHENG Zhuo. Holocene sedimentary environment transform and onset time of Pearl River Delta progradation[J]. Marine Geology & Quaternary Geology, 2020, 40(5): 107-117. DOI: 10.16562/j.cnki.0256-1492.2020030701
    [5]WU Yueqin, LIU Chunlian, YANG Xiaoqiang, HANG Yi, YIN Jian, ZHANG Kai. Holocene microfaunal records in the central Pearl River Delta and implications for palaeoenvironmental changes[J]. Marine Geology & Quaternary Geology, 2019, 39(2): 31-43. DOI: 10.16562/j.cnki.0256-1492.2018042801
    [6]ZHOU Yang, XIE Yecai, CHEN Fang, LONG Gui, CHEN Chixin, WU Cong, ZHENG Zhimin, HUANG Xuefei. MICROFAUNAS IN HOLE ZK201-2 AT ZHUJIANG RIVER DELTA SINCE LATE PLEISTOCENE AND THEIR IMPLICATIONS FOR PALEOENVIRONMENTS[J]. Marine Geology & Quaternary Geology, 2015, 35(4): 113-122. DOI: 10.16562/j.cnki.0256-1492.2015.04.012
    [7]PENG Jun, CHEN Shenliang, LI Guqi. SEDIMENTARY INFORMATION OF TIDAL FLAT OF THE YELLOW RIVER DELTA AFTER LAST GLACIAL MAXIMUM AND ITS ENVIRONMENTAL IMPLICATIONS[J]. Marine Geology & Quaternary Geology, 2014, 34(2): 19-26. DOI: 10.3724/SP.J.1140.2014.02019
    [8]WANG Jianhua, CAO Linglong, WANG Xiaojing, YANG Xiaoqiang, YANG Jie, SU Zhihua. EVOLUTION OF SEDIMENTARY FACIES AND PALEOENVIRONMENT DURING THE LATE QUATERNARY IN WANQINGSHA AREA OF THE PEARL RIVER DELTA[J]. Marine Geology & Quaternary Geology, 2009, 29(6): 35-41. DOI: 10.3724/SP.J.1140.2009.06035
    [9]YANG Mu-zhuang, LAI Qi-hong, ZHOU Shun-gui. RELATIONSHIP OF THE SOIL FLUORINE ENRICHMENT AND MARINE INVASION IN THE PEARL RIVER DELTA[J]. Marine Geology & Quaternary Geology, 2008, 28(5): 17-20.
    [10]GAO Fang-lei, YANG Xiao-qiang, DONG Yi-xin, LIANG Qiu-hua, ZHOU Wen-juan. CARBON-NITROGEN RECORD IN SEDIMENTS OF CORE PD IN THE PEARL RIVER DELTA AND THE ENVIRONMENTAL SIGNIFICANCE[J]. Marine Geology & Quaternary Geology, 2006, 26(2): 33-39.
  • Cited by

    Periodical cited type(2)

    1. 张晓洁,肖柳,郭肖伊,南海明,张涵,王飞飞,许博超. 夏季长江口邻近海域活体底栖有孔虫优势种群及分布特征研究. 中国海洋大学学报(自然科学版). 2024(08): 74-82 .
    2. 吴玉琦,陈页,郭远明,袁涛,李铁军,乔玲. 底栖有孔虫对海洋环境的生态响应概述. 地球科学进展. 2024(09): 889-901 .

    Other cited types(2)

Catalog

    Article views (2056) PDF downloads (16) Cited by(4)

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return