Water H-O isotopic characteristics of Nandu River estuary and their response to typhoon "Kalmaegi"

LIU Jinqing; YIN Ping; GAO Fei; CHEN Bin; LIAN Ergang

doi:10.16562/j.cnki.0256-1492.2018.01.017

2018 Vol. 38, No. 1

Article Contents

Article navigation > Marine Geology & Quaternary Geology > 2018 > 38(1): 170-177

Next Article Previous Article

LIU Jinqing, YIN Ping, GAO Fei, CHEN Bin, LIAN Ergang. Water H-O isotopic characteristics of Nandu River estuary and their response to typhoon 'Kalmaegi'[J]. Marine Geology & Quaternary Geology, 2018, 38(1): 170-177. doi: 10.16562/j.cnki.0256-1492.2018.01.017

Citation:

LIU Jinqing, YIN Ping, GAO Fei, CHEN Bin, LIAN Ergang. Water H-O isotopic characteristics of Nandu River estuary and their response to typhoon "Kalmaegi"[J]. Marine Geology & Quaternary Geology, 2018, 38(1): 170-177. doi: 10.16562/j.cnki.0256-1492.2018.01.017

Water H-O isotopic characteristics of Nandu River estuary and their response to typhoon "Kalmaegi"

1.
Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology, Ministry of Land and Resources, Qingdao Institute of Marine Geology, Qingdao 266071, China
2.
Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China
3.
Third Institute of Oceanography, State Oceanic Administration, Xiamen 361005, China

More Information

Corresponding author: GAO Fei, gf198712@126.com

Received Date: 31 May 2017

Revised Date: 30 October 2017

Publish Date: 28 February 2018

Abstract

Abstract

Frequent summer typhoon in subtropical regions brings significant impacts on water environment in estuaries. Based on the in-situ hydrographic observation in 2014, this paper portrays the characteristics and changes of water H-O isotope compositions in the Nandu River Estuary during the typhoon Kalmaegi. Results show that atmospheric precipitation, which is mainly derived from the water vapor transported from the tropical Pacific, is the main factor controlling the compositions of the H-O isotope in the typhoon period. After the typhoon, evaporation is strengthened with the decrease in rainfall and increase in temperature, and as the results, the contents of H-O isotopes are increased in water. The large amount of fresh water brought in by the Typhoon Kalmaegi will certainly bring in changes in the estuarine environment. The tidal current limit will move towards the river mouth, water mix strongly, and brackish water front form outside the river mouth. This study provides observational evidence for understanding the impact of typhoon on the water cycle of small-medium rivers in subtropical regions.
- H-O isotope /
- hydrology /
- typhoon Kalmaegi /
- Nandu River

FullText(HTML)

References

[1]	Craig H. Isotopic Variations in Meteoric Waters[J]. Science, 1961, 133(3465):1702. doi: 10.1126/science.133.3465.1702 CrossRef Google Scholar
[2]	Dansgaard W. Stable isotopes in precipitation[J]. Tellus, 1964, 16(4):436-468. doi: 10.3402/tellusa.v16i4.8993 CrossRef Google Scholar
[3]	丁悌平, 高建飞, 石国钰, 等.长江水氢、氧同位素组成的时空变化及其环境意义[J].地质学报, 2013, 87(5):661-676. doi: 10.3969/j.issn.0001-5717.2013.05.005 CrossRef Google Scholar DING Tiping, GAO Jianfei, SHI Guoyu, et al. Spacial and temporal variations of H isotope compositions of the Yangtze River water and their environmental implications[J]. Acta Geologica Sinica, 2013, 87(5):661-676. doi: 10.3969/j.issn.0001-5717.2013.05.005 CrossRef Google Scholar
[4]	高建飞, 丁悌平, 罗续荣, 等.黄河水氢、氧同位素组成的空间变化特征及其环境意义[J].地质学报, 2011, 85(4):596-602. Google Scholar GAO Jianfei, DING Tiping, LUO Xurong, et al. δD and δ¹⁸O variations of water in the Yellow River and its environmental signigicance[J]. Acta Geologica Sinica, 2011, 85(4):596-602. Google Scholar
[5]	李小飞, 张明军, 王圣杰, 等.黄河流域大气降水氢、氧稳定同位素时空特征及其环境意义[J].地质学报, 2013, 87(2):269-277. Google Scholar LI Xiaofei, ZHANG Mingjun, WANG Shengjie, et al. Spatial an temporal variations of Hydrogen and Oxygen isotopes in precipitation in the Yellow River Basin and its environmental significance[J]. Acta Geologica Sinica, 2013, 87(2):269-277. Google Scholar
[6]	Kai D, Yang S, Lian E, et al. Three Gorges Dam alters the Changjiang (Yangtze) river water cycle in the dry seasons: Evidence from H-O isotopes[J]. Science of the Total Environment, 2016, 562:89-97. doi: 10.1016/j.scitotenv.2016.03.213 CrossRef Google Scholar
[7]	Li C, Yang S, Lian E, et al. Damming effect on the Changjiang (Yangtze River) river water cycle based on stable hydrogen and oxygen isotopic records[J]. Journal of Geochemical Exploration, 2016, 165:125-133. doi: 10.1016/j.gexplo.2016.03.006 CrossRef Google Scholar
[8]	Zhang J, Letolle R, Martin J M, et al. Stable oxygen isotope distribution in the Huanghe (Yellow River) and the Changjiang (Yangtze River) estuarine systems[J]. Continental Shelf Research, 1990, 10(4):369-384. doi: 10.1016/0278-4343(90)90057-S CrossRef Google Scholar
[9]	赵军鹏, 龚文平, 王道儒.海南岛南渡江河口的盐水入侵[J].海洋学报, 2013, 35(5):14-28. doi: 10.3969/j.issn.0253-4193.2013.05.002 CrossRef Google Scholar ZHAO Junpeng, GONG Wenping, WANG Daoru, et al. Saline intrusion in the Nandu River estuary, Hainan Island[J]. Acta Geologica Sinica, 2013, 35(5):14-28. doi: 10.3969/j.issn.0253-4193.2013.05.002 CrossRef Google Scholar
[10]	龚文平, 吴家信, 莫李帅.用EOF方法分析海口湾东部浅滩区的泥沙来源与泥沙运动[J].泥沙研究, 2004(1):63-69. doi: 10.3321/j.issn:0468-155X.2004.01.010 CrossRef Google Scholar GONG Wenping, WU Jiaxin, MO Lishuai, et al. Using EOF method to analyze the sediment source and transport in the east shallow area of Haikou bay[J]. Journal of Sediment Research, 2004(1):63-69. doi: 10.3321/j.issn:0468-155X.2004.01.010 CrossRef Google Scholar
[11]	谢华亮, 戴志军, 吴莹, 等.海南岛南渡江河口动力沉积模式[J].沉积学报, 2014, 32(5):884-892. Google Scholar XIE Hualiang, DAI Zhijun, WU Ying, et al. Sedimentation dynamic modes of the Nandujiang Estuary, Hainan Island[J]. Acta Sedimentologica Sinica, 2014, 32(5):884-892. Google Scholar
[12]	陈斌, 高飞, 印萍, 等.南渡江河口洪、枯季节水文泥沙变化特征及台风"海鸥"对入海水沙的影响[J].海洋与湖沼, 2015, 46(6):1279-1291. Google Scholar CHEN Bin, GAO Fei, YIN Ping, et al.Variations in hydrodynamics and sedimentation in flood and dry seasons and impact of typhoon kalmaegi on rounoff and sediment discharge in Nandu River Estuary[J]. Oceanologia et Limnologia Sinica, 2015, 46(6):1279-1291. Google Scholar
[13]	吴创收, 杨世伦, 罗向欣, 等.近四十年南渡江水下三角洲的冲淤变化及其主控原因[J].海洋科学进展, 2011, 29(3):339-345. doi: 10.3969/j.issn.1671-6647.2011.03.010 CrossRef Google Scholar WU Chuangshou, YANG Shilun, LUO Shilun, et al.Erosion and accretion of the Nandu River underwater Delta during 1963—2003[J]. Advances in Marine Science, 2011, 29(3):339-345. doi: 10.3969/j.issn.1671-6647.2011.03.010 CrossRef Google Scholar
[14]	罗宪林, 李春初, 罗章仁.海南岛南渡江三角洲的废弃与侵蚀[J].海洋学报, 2000(3):55-60. doi: 10.3321/j.issn:0253-4193.2000.03.008 CrossRef Google Scholar LUO Xianlin, LI Chunchu, LUO Zhangren, et al. Erosion and abandonment of the Nandu River Delta, Hainan Island[J]. Acta Oceanologica Sinica, 2000(3):55-60. doi: 10.3321/j.issn:0253-4193.2000.03.008 CrossRef Google Scholar
[15]	李瑞娴, 李龙兵, 李海朋, 等.南渡江入海径流量变化及其影响因素[J].水力发电, 2015(8):13-16, 57. doi: 10.3969/j.issn.0559-9342.2015.08.004 CrossRef Google Scholar LI Ruixian, LI Longbing, LI Haipeng, et al. Study on variation and influencing factors of discharge into the sea from Nandu River[J]. Water Power, 2015(8):13-16, 57. doi: 10.3969/j.issn.0559-9342.2015.08.004 CrossRef Google Scholar
[16]	龚文平, 王道儒, 赵军鹏, 等.海南岛南渡江河口枯季大小潮的盐度变化特征[J].海洋通报, 2012(6):621-629. Google Scholar GONG Wenping, WANG Daoru, ZHAO Junpeng, et al. Salinity variability during spring-neap tidal cycle in the Nandu River Estuary of Hainan Island in the dry season[J]. Marine Science Bulletin, 2012(6):621-629. Google Scholar
[17]	陈静生, 王忠.海南岛雨水、河水、地下水氢氧稳定同位素特征及其关系[J].地理科学, 1993, 13(3):273-278. Google Scholar CHEN Jingsheng, WANG Zhong. A study on stable isotopes of hydrogen and oxygen in rain water, river water and groundwater from Hainan Island of China[J]. Scientia Geographica Sinica, 1993, 13(3):273-278. Google Scholar
[18]	庞洪喜, 何元庆, 张忠林, 等.季风降水中δ^{^18}O与季风水汽来源[J].科学通报, 2005, 50(20):2263-2266. doi: 10.3321/j.issn:0023-074X.2005.20.014 CrossRef Google Scholar PANG Hongxi, HE Yuanqing, ZHANG Zhonglin, et al. The source of δ¹⁸O in Monsoon precipition and rain water[J]. Chinese Science Bulletin, 2005, 50(20):2263-2266. doi: 10.3321/j.issn:0023-074X.2005.20.014 CrossRef Google Scholar
[19]	陈伟斌, 黄荣成, 屈梅芳, 等.快速台风"海鸥"强度、路径特点及成因分析[J].中国农学通报, 2015, 31(26):200-209. doi: 10.11924/j.issn.1000-6850.casb15050121 CrossRef Google Scholar CHEN Weibin, HUANG Rongcheng, QU Meifang, et al. Analysis of intensity, track characteristics and causes of fast moving typhoon "Kalmaegi"[J]. Chinese Agricultural Science Bulletin, 2015, 31(26):200-209. doi: 10.11924/j.issn.1000-6850.casb15050121 CrossRef Google Scholar
[20]	陈中笑, 程军, 郭品文, 等.中国降水稳定同位素的分布特点及其影响因素[J].大气科学学报, 2010, 33(6):667-679. doi: 10.3969/j.issn.1674-7097.2010.06.004 CrossRef Google Scholar CHEN Zhongxiao, CHENG Jun, GUO Pinwen, et al. Distribution characters and its control factors of stable isotope in precipitation over China[J]. Transactions of Atmospheric Sciences, 2010, 33(6):667-679. doi: 10.3969/j.issn.1674-7097.2010.06.004 CrossRef Google Scholar
[21]	Ye F, Deng W, Xie L, et al. Surface water δ¹⁸O in the marginal China seas and its hydrological implications[J]. Estuarine Coastal & Shelf Science, 2014, 147:25-31. Google Scholar