QUANTITATIVE ANALYSIS OF THE ECOLOGICAL SEDIMENT REPLENISHMENT AT THE NORTHERN NATURE RESERVE OF YELLOW RIVER DELTA

HUANG Anding; JIANG Xuezhong; CHEN Shenliang

doi:10.16028/j.1009-2722.2019.221

2020 Vol. 36, No. 12

Article Contents

Article navigation > Marine Geology Frontiers > 2020 > 36(12): 15-21

Next Article Previous Article

HUANG Anding, JIANG Xuezhong, CHEN Shenliang. QUANTITATIVE ANALYSIS OF THE ECOLOGICAL SEDIMENT REPLENISHMENT AT THE NORTHERN NATURE RESERVE OF YELLOW RIVER DELTA[J]. Marine Geology Frontiers, 2020, 36(12): 15-21. doi: 10.16028/j.1009-2722.2019.221

Citation:

HUANG Anding, JIANG Xuezhong, CHEN Shenliang. QUANTITATIVE ANALYSIS OF THE ECOLOGICAL SEDIMENT REPLENISHMENT AT THE NORTHERN NATURE RESERVE OF YELLOW RIVER DELTA[J]. Marine Geology Frontiers, 2020, 36(12): 15-21. doi: 10.16028/j.1009-2722.2019.221

QUANTITATIVE ANALYSIS OF THE ECOLOGICAL SEDIMENT REPLENISHMENT AT THE NORTHERN NATURE RESERVE OF YELLOW RIVER DELTA

1.
State Key Laboratory of Estuarine and Coast, East China Normal University, Shanghai 200241, China
2.
School of Urban and Regional Science, East China Normal University, Shanghai 200241, China

More Information

Corresponding author: JIANG Xuezhong, xzjiang@sklec.ecnu.edu.cn

Received Date: 25 December 2019

Publish Date: 31 December 2020

Abstract

Abstract

The northern coast of the Yellow River Delta has lost its sediment supply from the Yellow River basin and experienced continuous erosion under ocean power since the cut-off of Diaokou River in 1976. The ecological resources of wetland in the Yellow River Delta Northern Nature Reserve (YRDNNR), located at the mouth of the Diaokou River, are thus under threat. The erosion of YRDNNR was evaluated by using spatial analysis technique based on the topography data measured on the north bank of the Yellow River Delta in this paper. The results show that from year 1992 to 2015, continuous erosion occurred in this area, the annual erosion volume reached 2 856×10⁴ t, the annual eroded thickness was 9.3 cm, and the erosion rate remained rather stable. Based on the historical runoff of Lijin hydrological station of the Yellow River, the paper tries to put forward a quantitative scheme to compensate the erosion in the YRDNNR. According to the analysis, during the period of water-sediment modulation, water diversion through Diaokou River at a flow rate of 1 200 m³/s for 19 days can effectively alleviate the erosion of the reserve.
- Yellow River Delta /
- coastal erosion /
- sediment replenishment

FullText(HTML)

References

[1]	周云轩,田波,黄颖,等. 我国海岸带湿地生态系统退化成因及其对策[J]. 中国科学院院刊,2016,31(10):1157-1166. Google Scholar
[2]	张晓龙. 现代黄河三角洲滨海湿地环境演变及退化研究[D]. 青岛: 中国海洋大学, 2005. Google Scholar
[3]	李九发, 时连强, 应铭, 等. 黄河河口钓口河流路亚三角洲岸滩演变与抗冲性试验[M]. 北京: 海洋出版社, 2013: 14. Google Scholar
[4]	王开荣,李岩,于守兵,等. 黄河刁口河备用流路现状及保护工程措施探讨[J]. 中国水利,2017(1):15-19. doi: 10.3969/j.issn.1000-1123.2017.01.005 CrossRef Google Scholar
[5]	葛海燕. 刁口河尾闾黄河三角洲自然保护区生态补水效果评估[J]. 山东林业科技,2012,42(5):34-36. doi: 10.3969/j.issn.1002-2724.2012.05.010 CrossRef Google Scholar
[6]	李士国, 李延波. 黄河刁口河流路生态补水试验及效果分析[C]//第三届全国河道治理与生态修复技术交流研讨专刊. 北京: 中国水利技术信息中心, 2015: 13. Google Scholar
[7]	孙莉,司晓磊,廖展强. 黄河三角洲北区湿地生态需水量研究[J]. 人民黄河,2010,32(12):112-113. doi: 10.3969/j.issn.1000-1379.2010.12.046 CrossRef Google Scholar
[8]	FANG H L,XU J. Land cover and vegetation change in the Yellow River Delta nature reserve analyzed with Landsat Thematic Mapper data[J]. Geocarto International,2000,15(4):43-50. doi: 10.1080/10106040008542171 CrossRef Google Scholar
[9]	FAN Y S,CHEN S L,ZHAO B,et al. Monitoring tidal flat dynamics affected by human activities along an eroded coast in the Yellow River Delta,China[J]. Environmental monitoring and assessment,2018,190(7):396. doi: 10.1007/s10661-018-6747-7 CrossRef Google Scholar
[10]	燕峒胜, 蒲高军, 张建华, 等. 黄河三角洲胜利滩海油区海岸蚀退与防护研究[M]. 郑州: 黄河水利出版社, 2006. Google Scholar
[11]	师长兴,章典,尤联元,等. 黄河口泥沙淤积估算问题和方法:以钓口河亚三角洲为例[J]. 地理研究,2003(1):49-59. doi: 10.3321/j.issn:1000-0585.2003.01.006 CrossRef Google Scholar
[12]	陈沈良,谷硕,姬泓宇,等. 新入海水沙情势下黄河口的地貌演变[J]. 泥沙研究,2019,44(5):61-67. Google Scholar
[13]	WANG H J, YANG Z S, 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. Google Scholar
[14]	刘静. 黄河河口三角洲湿地生态补水实践[EB/OL]. https://max.book118.com/html/2018/1022/7012052163001153.shtm, 2019-7-4: 22-24. Google Scholar
[15]	杨作升,李国刚,王厚杰,等. 55年来黄河下游逐日水沙过程变化及其对干流建库的响应[J]. 海洋地质与第四纪地质,2008,28(6):9-18. Google Scholar
[16]	司敬玲,张月明. 黄河三角洲刁口河生态调水实践[J]. 人民黄河,2013,35(2):30-32, 35. doi: 10.3969/j.issn.1000-1379.2013.02.011 CrossRef Google Scholar
[17]	YU Y G,SHI X F,WANG H J,et al. Effects of dams on water and sediment delivery to the sea by the Huanghe (Yellow River):The special role of Water-Sediment Modulation[J]. Anthropocene,2013,3:72-82. doi: 10.1016/j.ancene.2014.03.001 CrossRef Google Scholar
[18]	李国英. 黄河首次调水调沙[J]. 科学,2003,55(1):41-44,2. Google Scholar
[19]	陈沈良,张国安,谷国传. 黄河三角洲海岸强侵蚀机理及治理对策[J]. 水利学报,2004(7):1-6,13. doi: 10.3321/j.issn:0559-9350.2004.07.001 CrossRef Google Scholar
[20]	王建中, 王道席.黄河河口地区生态流量调度初步研究[C]//第三届黄河国际论坛论文集.郑州: 黄河水利出版社, 2007: 3 - 8． Google Scholar
[21]	陈雄波, 雷鸣, 王鹏. 清水沟、刁口河流路联合运用方案比选[J]. 海洋工程, 2014, 32(4):117-123. Google Scholar