珠江黄茅海河口地貌形态变化及其动力响应

doi:10.11978/2022106

热带海洋学报 ›› 2023, Vol. 42 ›› Issue (2): 9-20.doi: 10.11978/2022106CSTR: 32234.14.2022106

珠江黄茅海河口地貌形态变化及其动力响应

严静¹(), 韦惺¹^,²()

1.中国科学院南海海洋研究所, 广东广州 510301
2.南方海洋科学与工程广东省实验室(广州), 广东广州 511458

收稿日期:2022-05-10 修回日期:2022-06-10 出版日期:2023-03-10 发布日期:2022-06-13
通讯作者: 韦惺。email: wes@scsio.ac.cn
作者简介:
严静(1980—), 女, 广西壮族自治区北海市人, 助理研究员, 从事海洋环境数值模拟研究。email: yanjing@scsio.ac.cn
基金资助:
国家基金重大项目(41890851); 南方海洋科学与工程广东省实验室(广州)人才团队引进重大专项(GML2019ZD0303); 热带海洋环境国家重点实验室自主研究项目(LTOZZ2202)

Geomorphological changes and dynamic responses of the Huangmaohai Estuary in the Pearl River Delta

YAN Jing¹(), WEI Xing¹^,²()

1. South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China
2. Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458, China

Received:2022-05-10 Revised:2022-06-10 Online:2023-03-10 Published:2022-06-13
Contact: WEI Xing. email: wes@scsio.ac.cn
Supported by:
National Natural Science Foundation of China(41890851); Key Special Projects for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)(GML2019ZD0303); Project of State Key Laboratory of Tropical Oceanography(LTOZZ2202)

摘要/Abstract

摘要：

黄茅海是位于珠江三角洲西南部的一个喇叭形溺谷河口湾。近几十年来在自然过程和人类活动共同作用下河口的地貌形态发生了巨大变化。文章基于1972—2016年地形图和卫星遥感影像, 对河口岸线和水下地形的变化进行了量化分析, 并构建了三维水动力模型对河口动力对地貌形态变化的响应进行了讨论。结果显示, 土地围垦使得黄茅河口的口门和岸线急剧向海延伸, 水域面积大面积减少。受此影响, 河口的纳潮量减少了近19.61%, 由1972年的11.13亿m³减少为2016年的8.95亿m³。河口的束窄和形态的变化也使得河口出现水位抬升、径流动力增强, 潮差增加, 涨潮历时缩短, 落潮历时延长等变化。未来, 随着河口的淤积充填, 河口的潮汐动力将受到进一步削弱。

关键词: 黄茅海河口, 地貌形态变化, 动力响应, 数值模拟

Abstract:

The Huangmaohai Estuary (HE) is a horn-shaped estuary in the southwest of the Pearl River Delta. In the last few decades, the morphology of the HE has undergone tremendous changes under the combined action of natural processes and human activities. Based on the historical charts and satellite remote sensing images from 1972 to 2016, this paper quantitatively analyzes the changes of the coastline and underwater topography, and constructs a three-dimensional hydrodynamic model to discuss the dynamic response to the topographic changes. The results showed that land reclamation caused the mouth and coastline of the outlet to extend sharply to the sea, and the water area was greatly reduced. As a result, the tidal volume of the estuary decreased from 1.113 billion cubic meters in 1972 to 895 million cubic meters in 2016, a decrease of nearly 19.61%. At the same time, the narrowing of the estuary also causes changes in the hydrological dynamics, such as the rise of the water level, the enhancement of the runoff power, the reduction of the tidal range, the shortening of the high tide duration, and the extension of the ebb tide duration. In the future, with the silting and filling of the estuary, the tidal power of the estuary will be further weakened.

Key words: Huangmaohai Estuary, Morphological changes, Dynamic response, Numerical modeling

严静, 韦惺. 珠江黄茅海河口地貌形态变化及其动力响应[J]. 热带海洋学报, 2023, 42(2): 9-20.

YAN Jing, WEI Xing. Geomorphological changes and dynamic responses of the Huangmaohai Estuary in the Pearl River Delta[J]. Journal of Tropical Oceanography, 2023, 42(2): 9-20.

图/表 12

图1

图2

图3

图4

表1

图5

图6

图7

图8

图9

图10

图11

参考文献 29

[1]	龚文平, 刘欢, 任杰, 等, 2012. 黄茅海河口潮波的传播特征与机理研究[J]. 海洋学报, 34(3): 41-54.
	GONG WENPING, LIU HUAN, REN JIE, et al, 2012. The study of tidal propagation the in Huangmaohai Estuary and its underlying mechanisms[J]. Acta Oceanologica Sinica, 34(3): 41-54. (in Chinese with English abstract) doi: 10.1007/s13131-015-0648-1
[2]	黄方, 叶春池, 温学良, 等, 1994. 黄茅海盐度特征及其盐水楔活动范围[J]. 海洋通报, 13(2): 33-39.
	HUANG FANG, YE CHUNCHI, WEN XUELIANG, et al, 1994. Characteristics of salinity and active range of saline wedge in Huangmaohai Bay[J]. Marine Science Bulletin, 13(2): 33-39. (in Chinese with English abstract)
[3]	贾良文, 罗军, 任杰, 2012. 珠江口黄茅海拦门沙演变及成因分析[J]. 海洋学报, 34(5): 120-127.
	JIA LIANGWEN, LUO JUN, REN JIE, 2012. The analysis of the evolution of a sand bar and its formation in the Huangmao Bay of the Zhujiang Estuary[J]. Acta Oceanologica Sinica, 34(5): 120-127. (in Chinese with English abstract)
[4]	贾良文, 文艺, 2013. 珠江口黄茅海枯季表层沉积物特性及输移研究[J]. 泥沙研究, 1: 60-66.
	JIA LIANGWEN, WEN YI, 2013. Study of characteristics and transport pattern of surface sediment during dry seasons in Huangmao Estuary[J]. Journal of Sediment Research, 1: 60-66. (in Chinese with English abstract)
[5]	蒋陈娟, 周佳楠, 杨清书, 2020. 珠江磨刀门河口潮汐动力变化对人类活动的响应[J]. 热带海洋学报, 39(6): 66-76. doi: 10.11978/2019137
	JIANG CHENJUAN, ZHOU JIANAN, YANG QINGSHU, 2020. Effects of human intervention on tidal dynamics in the Modaomen Estuary, Pearl River[J]. Journal of Tropical Oceanography, 39(6): 66-76. (in Chinese with English abstract) doi: 10.11978/2019137
[6]	李娜, 娄安刚, 张学庆, 等, 2019. 基于MIKE3的渤海三维温盐数值模拟[J]. 海洋湖沼通报, 2: 1-9.
	LI NA, LOU ANGANG, ZHANG XUEQING, et al, 2019. Three dimensional numerical simulation of temperature and salinity in the Bohai Sea based on MIKE3[J]. Transactions of Oceanology and Limnology, 2: 1-9. (in Chinese with English abstract)
[7]	林中源, 龚文平, 贾良文, 2014. 珠江口黄茅海枯季的悬沙变化与泥沙输运[J]. 泥沙研究, 2: 27-37.
	LIN ZHOGNYUAN, GONG WENPING, JIA LIANGWEN, 2014. Spatiotemporal variations of suspended sediment concentration and sediment transport during a dry season in Huangmaohai Estuary, Pearl River Delta[J]. Journal of Sediment Research, 2: 27-37. (in Chinese with English abstract)
[8]	罗丹, 1998. 黄茅海沿岸滩涂发育及岸线变化遥感浅析[J]. 人民珠江, 3: 45-47.
	LUO DAN, 1998. Remote sensing analysis of tidal flat development and coastline changes along the Huangmaohai[J]. Pearl River, 3: 45-47. (in Chinese)
[9]	罗军, 2010. 十年至百年尺度黄茅海地形演变及成因研究[D]. 广州: 中山大学.
	LUO JUN, 2010. Cause analysis of morphological evolution of Huangmaohai Estuary in the decade to century-scale[D]. Guangzhou: Sun Yat-sen University Master Dissertation. (in Chinese with English abstract)
[10]	吴超羽, 1995. 黄茅海河口小尺度动力结构及其沉积作用[J]. 中山大学学报(自然科学版), 34(2): 86-94.
	WU CHAOYU, 1995. Dynamic structures and their sedimentation effects in Huangmaohai Estuary[J]. Acta Scientiarum Naturalium Universitatis Sunyatseni, 34(2): 86-94. (in Chinese with English abstract)
[11]	吴创收, 刘欢, 武亚菊, 等, 2010. 黄茅湾河口沿程异常潮差: Ⅰ-理论模型研究[J]. 海洋科学进展, 28(4): 436-444.
	WU CHUANGSHOU, LIU HUAN, WU YAJU, et al, 2010. Study on abnormal tidal range along coast of Huangmaohai River Estuary: Ⅰ-Theoritical model[J]. Advances in Marine Science, 28(4): 436-444. (in Chinese with English abstract)
[12]	武亚菊, 刘欢, 吴创收, 等, 2011. 黄茅海河口沿程异常潮差数值模拟研究[J]. 海洋科学进展, 29(1): 16-28.
	WU YAJU, LIU HUAN, WU CHUANGSHOU, et al, 2011. Numerical simulation to study abnormal tidal ranges along the river course in Huangmaohai Estuary[J]. Advances in Marine Science, 29(1): 16-28. (in Chinese with English abstract)
[13]	杨美卿, 1993. 河流与海岸动力学[M]. 北京: 水利电力出版社.
	YANG MEIQING, 1993. Introduction to River and Coastal dynamic[M]. Beijing: China Water Conservancy and Hydropower Press. (in Chinese with English abstract)
[14]	杨名名, 吴加学, 张乾江, 等, 2016. 珠江黄茅海河口洪季侧向余环流与泥沙输移[J]. 海洋学报, 38(1): 31-45.
	YANG MINGMING, WU JIAXUE, ZHANG QIANJIANG, et al, 2016. Lateral residual circulation and sediment transport during the flood season in the Huangmaohai Estuary, Pearl River[J]. Haiyang Xuebao, 38(1): 31-45. (in Chinese with English abstract)
[15]	杨雪舞, 王文介, 1994. 珠江口黄茅海河口湾水动力沉积和泥沙运动的统计研究[J]. 海洋工程, 12(4): 42-51.
	YANG XUEWU, WANG WENJIE, 1994. A statistical study on hydrodynamic sedimentation and sand movement Huangmaohai Estuary Bay[J]. The Ocean Engineering, 12(4): 42-51. (in Chinese with English abstract)
[16]	赵荻能, 2017. 珠江河口三角洲近165年演变及对人类活动响应研究[D]. 浙江: 浙江大学.
	ZHAO DINENG, 2017. Morphological evolution of the Pearl River Delta in the past 165 years and its response to human activities[D]. Zhejiang: Zhejiang University Doctoral Dissertation. (in Chinese with English abstract)
[17]	赵峰, 吴梅桂, 周鹏, 等, 2015. 黄茅海——广海湾及其邻近海域表层沉积物中γ放射性核素含量水平[J]. 热带海洋学报, 34(4): 77-82. doi: 10.11978/j.issn.1009-5470.2015.04.011
	ZHAO FENG, WU MEIGUI, ZHOU PENG, et al, 2015. Radionuclides in surface sediments from the Huangmaohai Estuary-Guanghai Bay and its adjacent sea area of the South China Sea[J]. Journal of Tropical Oceanography, 34(4): 77-82. (in Chinese with English abstract) doi: 10.11978/j.issn.1009-5470.2015.04.011
[18]	自然资源部, 2021. 中国海平面公报[EB/OL][2020-04-28]. 北京: 自然资源部 (https://www.mnr.gov.cn/sj/sjfw/hy/gbgg/zghpmgb/). (in Chinese)
[19]	DHI, 2012. MIKE 3 Flow Model FM Hydrodynamic Module User Guide. DHI Water and Environment, Hørsholm.
[20]	Egbert G D, Erofeeva S Y, 2002. Efficient inverse modeling of barotropic ocean tides[J]. Journal of Atmospheric and Oceanic Technology, 19(2): 183-204. doi: 10.1175/1520-0426(2002)019<0183:EIMOBO>2.0.CO;2
[21]	HE YONG, LIU XIAOJIAN, DUAN ZIHAO, et al, 2022. Long-term morphodynamic evolution in the Modaomen Estuary of the Pearl River Delta, South China[J]. Geomorphology, 398: 108057. doi: 10.1016/j.geomorph.2021.108057
[22]	JIA LIANGWEN, PAN SHUNQI, WU CHAOYU, 2013. Effects of the Anthropogenic Activities on the Morphological Evolution of the Modaomen Estuary, Pearl River Delta, China[J]. China Ocean Engineering, 27(6): 795-808. doi: 10.1007/s13344-013-0065-1
[23]	JOSEPH H, RICARDO D C, 2003. Numerical simulation of the tidal propagation in the coastal region of Santos (Brazil, 24°S46°W)[J]. Continental Shelf Research, 23(16): 1597-1613. doi: 10.1016/S0278-4343(03)00143-2
[24]	WALDMAN S, BASTON S, NEMALIDINNE R, et al, 2017. Implementation of tidal turbines in MIKE 3 and Delft3D models of Pentland Firth & Orkney Waters[J]. Ocean & Coastal Management, 147: 21-36.
[25]	WEI XING, CAI SHUQUN, ZHAN WEIKANG, 2021. Impact of anthropogenic activities on morphological and deposition flux changes in the Pearl River Estuary, China[J]. Scientific Reports, 11(1): 16643. doi: 10.1038/s41598-021-96183-0 pmid: 34404884
[26]	WEI XING, NI PEITONG, ZHAN HAIGANG, 2013. Monitoring cooling water discharge using Lagrangian coherent structures: A case study in Daya Bay, China[J]. Marine Pollution Bulletin, 75(1-2): 105-113. doi: S0025-326X(13)00449-9 pmid: 23972680
[27]	WEI XING, WU XIAOXIN, 2011. Dynamic structures and their sedimentation effects of the Yamen Inlet, Huangmaohai Estuary[J]. Science China Earth Sciences, 54(6): 1-11. doi: 10.1007/s11430-010-4125-6
[28]	WU JIAXUE, SHEN HUANTING, 1999. Estuarine bottom sediment transport based on the ‘Mclaren Model’: A case study of Huangmaohai Estuary, south China[J]. Estuarine, Coastal and Shelf Science, 49(2): 265-279. doi: 10.1006/ecss.1999.0495
[29]	YANG LIUZHU, LIU FENG, GONG WENPIN, et al, 2019. Morphological response of Lingding Bay in the Pearl River Estuary to human intervention in recent decades[J]. Ocean and Coastal Management, 176: 1-10. doi: 10.1016/j.ocecoaman.2019.04.011

时间	岸线长度/km	滩涂面积/km²	水域面积/km²	水体体积/km³	平均水深/m
1972	94.27	118.22	562.22	2.82	5.14
2016	115.62	44.90	466.12	2.21	4.79

珠江黄茅海河口地貌形态变化及其动力响应

Geomorphological changes and dynamic responses of the Huangmaohai Estuary in the Pearl River Delta

RichHTML

PDF (PC)

赞

可视化

摘要/Abstract

引用本文

使用本文

图/表 12

参考文献 29

相关文章 15

Metrics

本文评价

推荐阅读 0

[1]	王旭, 屈科, 王梓峻, 杨元平, 王超, 张良斌. 风对波状涌潮海塘越浪水动力特性影响的数值研究[J]. 热带海洋学报, 2024, 43(5): 116-130.
[2]	吴鸿博, 罗锋, 陈治澎, 朱飞, 曾靖伟, 张弛, 李瑞杰. 红树林生态重建效果预测研究新模式[J]. 热带海洋学报, 2024, 43(4): 86-97.
[3]	张哲然, 胡俊洋, 周凯, 张鹏晖, 邢久星, 陈胜利. 不同类型台风气象场对深圳近海海域风暴潮模拟的比较研究—以台风“山竹”为例^*[J]. 热带海洋学报, 2023, 42(6): 1-14.
[4]	张敏, 吴航星, 陆逸彬, 陆迪文, 米婕, 朱冬琳, 陈波. 海岸线围垦对广西钦州湾地形演变的影响分析[J]. 热带海洋学报, 2023, 42(2): 124-131.
[5]	顾靖华, 朱建荣, 金智. 长江口宝钢码头溢油事故油膜漂移扩散数值模拟[J]. 热带海洋学报, 2022, 41(6): 159-170.
[6]	邓国通, 刘敏聪, 邢久星, 申锦瑜, 周凯, 陈胜利. 深圳近海风暴潮影响因素分析[J]. 热带海洋学报, 2022, 41(3): 91-100.
[7]	王仁政, 单正垛, 孟思雨, 宫响. 南海北部次表层叶绿素最大值年际变化特征分析^*[J]. 热带海洋学报, 2021, 40(6): 63-75.
[8]	张华, 温茜茜, 彭世球. 莫桑比克海峡及其邻近海区正压潮流数值模拟与能量收支分析^*[J]. 热带海洋学报, 2021, 40(2): 7-16.
[9]	李娟, 刘军亮, 蔡树群. 台风“康森”产生的海洋近惯性能量的数值模拟研究[J]. 热带海洋学报, 2020, 39(2): 35-43.
[10]	林夏艳, 董昌明, 陈大可. 台湾岛西南部一个暖涡的跨海盆粒子输运[J]. 热带海洋学报, 2018, 37(3): 9-18.
[11]	武文, 严聿晗, 宋德海. 大亚湾的潮汐动力学研究——I.潮波系统的观测分析与数值模拟^*[J]. 热带海洋学报, 2017, 36(3): 34-45.
[12]	严聿晗, 武文, 宋德海, 鲍献文. 大亚湾的潮汐动力学研究——Ⅱ.潮位和潮流双峰现象的产生机制[J]. 热带海洋学报, 2017, 36(3): 46-54.
[13]	马刚, 王云峰, 张晓辉, 顾成明, 钟波, 郭兴亮. 基于梯度信息的微波辐射亮温资料质量控制方法[J]. 热带海洋学报, 2017, 36(2): 86-95.
[14]	罗士浩, 经志友, 齐义泉, 谢强. 南海北部次中尺度过程数值研究^*[J]. 热带海洋学报, 2016, 35(5): 10-19.
[15]	叶丰, 包芸. 层结环境中热液羽流物质输运范围的模拟计算^*[J]. 热带海洋学报, 2016, 35(5): 97-102.