Differences in the lag characteristics of saltwater intrusion in the sub-estuaries of the Pearl River Estuary and their implications for water allocation

IF 2.4 4区 环境科学与生态学 Q3 ECOLOGY Regional Studies in Marine Science Pub Date : 2025-02-01 Epub Date: 2025-01-11 DOI:10.1016/j.rsma.2025.104011
Fei Yuan , Chen Lu , Fang Yang , Zhongyuan Lin , Yugui Yang
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Abstract

The water dispatch during the dry season of the Pearl River Estuary(PRE) has effectively responded to the adverse effects brought by the saltwater intrusion for many years, however, in recent years the saltwater intrusion of the estuary is still further intensified, seriously affected the water supply safety of the estuary and its irradiated area The Guangdong-Hong Kong-Macao Greater Bay Area. In order to manage the water dispatch for preventing the saltwater intrusion more reasonably, it is urgent to study the spatial-temporal characteristics of the saltwater intrusion in the sub-estuaries of the PRE. The wavelet analysis and cross wavelet method used and the results show: there is obvious diurnal, semi-diurnal and semi-lunar cycle of the salinity in most waters of the PRE. The changes in salinity at each sub-estuary are not synchronized with the tidal processes. The semi-monthly periodic changes in salinity typically precede the changes in tidal range, with the salt front appearing 3–4 days before spring tides. The diurnal and semi-diurnal periodic changes in salinity usually lag behind the changes in tidal levels, with the salt front occurring 2–3 hours after high tide. Only at the Hongqi Men sub-estuary does the salt front appear 1 day before spring tides and 8 hours after high tide. The main reason for the differences in lag characteristics may lie in the varying mixing states of saltwater and freshwater in different estuaries. Consequently, the optimal timing for freshwater releases to control salinity intrusion also varies among the sub-estuaries. In the practice of suppressing saltwater intrusions, it is important to choose appropriate timing for water releases based on these lag characteristics and to scientifically manage water allocation to achieve maximum benefits with minimal water usage. We hope that the experience gained from the PRE will be helpful to other coastal regions around the world.
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珠江口次河口海水入侵滞后特征的差异及其对水量分配的影响
珠江口旱季调水多年来有效应对了咸水入侵带来的不利影响,但近年来河口咸水入侵进一步加剧,严重影响了河口及其辐照区域粤港澳大湾区的供水安全。为了更合理地管理水调度,防止咸水入侵,迫切需要研究三峡库区河口河口咸水入侵的时空特征。采用小波分析和交叉小波分析方法,结果表明:PRE大部分海域的盐度存在明显的日、半日、半月周期。各河口下盐度变化与潮汐过程不同步。盐度半年周期性变化通常先于潮差变化,盐锋出现在大潮前3-4 天。盐度的日、半日周期变化通常滞后于潮位变化,盐锋出现在涨潮后2 ~ 3 小时。只有红旗门次河口出现了大潮前1 天、涨潮后8 小时的盐锋。造成滞后特性差异的主要原因可能是不同河口的咸水和淡水混合状态不同。因此,控制盐度入侵的最佳淡水释放时间也因河口而异。在抑制咸水入侵的实践中,根据这些滞后性选择合适的放水时机,科学地管理配水,以最小的用水量实现最大的效益。我们希望从PRE中获得的经验将对世界其他沿海地区有所帮助。
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来源期刊
Regional Studies in Marine Science
Regional Studies in Marine Science Agricultural and Biological Sciences-Ecology, Evolution, Behavior and Systematics
CiteScore
3.90
自引率
4.80%
发文量
336
审稿时长
69 days
期刊介绍: REGIONAL STUDIES IN MARINE SCIENCE will publish scientifically sound papers on regional aspects of maritime and marine resources in estuaries, coastal zones, continental shelf, the seas and oceans.
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