1980—2020年鄱阳湖退水期水体滞留时间时空演变特征及对水情响应
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1.南京信息工程大学地理科学学院;2.中国科学院南京地理与湖泊研究所

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基金项目:

国家自然科学基金(U2240219,42371044,42171104)、国家重点研发计划(2022YFC3204104)、江西省科技计划项目(20244BCF61001,20241ZDD02019)、中国科学院国际伙伴计划项目(131432KYSB20200029)和九江市科技计划项目(S2024TDJS0009,S2024QNZZ0006)联合资助


Spatiotemporal variations in residence time and response to hydrological regime during the receding period of Lake Poyang (1980-2020)
Author:
Affiliation:

1.School of Geographical Sciences, Nanjing University of Information Science and Technology;2.Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences

Fund Project:

National Natural Science Foundation of China(U2240219, 42371044, 42171104), National Key Research and Development Program of China(2022YFC3204104), Science and Technology Research Project of Jiangxi Province(20244BCF61001, 20241ZDD02019), International Partnership Program of the Chinese Academy of Sciences(131432KYSB20200029), Jiujiang Science and Technology Program(S2024TDJS0009, S2024QNZZ0006)

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    摘要:

    水体滞留时间是衡量湖泊水体更新速度和交换能力的关键指标,直接影响着污染物的传输和迁移行为,与湖泊水环境密切相关。近年来,鄱阳湖水文情势发生显著变化,其水环境亦受到一定影响。本研究从衡量水环境的动力指标水体滞留时间入手,基于MIKE21水动力数学模型,并耦合示踪剂模块进行数值模拟,定量分析了1980—2020年鄱阳湖退水期滞留时间的时空分布特征及不同区域的年际变化趋势,阐释了退水期水体滞留时间对水情的定量响应关系。结果表明:鄱阳湖退水期水体滞留时间具有极强的时空异质性,全湖水体滞留时间平均为36d,不同区域水体的平均滞留时间为:东部湖湾(93 d)>南部湖区(53 d)>入江通道(38 d)>主湖区(26 d)>吴城碟形湖群(17 d)。从年际变化看,近40年鄱阳湖全湖平均滞留时间呈略微缩短趋势,三峡后(2003—2020年)较三峡前(1980—2002年)平均缩短约4 d;其中入江通道的水体滞留时间降幅最大,较三峡运行前缩短9 d;其次为主湖区缩短5 d;其余湖区变化微弱。从不同水文年来看,水体滞留时间在洪水年显著大于枯水年;在年内的连续退水期,滞留率与退水水位呈显著的正相关关系;退水水位降低、退水速率加快,是鄱阳湖退水期水体滞留时间缩短的主要原因。本研究结果可为鄱阳湖水环境治理和生态修复提供科学依据。

    Abstract:

    Residence time serves as a critical indicator of lake water renewal and exchange, directly influencing pollutant transport and migration processes, and consequently water environment of the lake. In recent years, the hydrological conditions of Poyang Lake have undergone substantial changes, which have significantly influenced its water environment. This study focuses on residence time as a crucial hydrodynamic parameter for assessing water quality. Using the MIKE21 hydrodynamic model coupled with a tracer model, the research quantitatively examines the spatiotemporal distribution characteristics of residence time during the receding period of Poyang Lake from 1980 to 2020. Additionally, the study investigates regional interannual variation trends and clarifies the response relationship between residence time and hydrological conditions. The results reveal that the residence time during the receding period of Poyang Lake is characterized by high spatiotemporal heterogeneity. The average residence time for the entire lake is 36 d, with variations among sub-regions: eastern lake bays (93 d) > southern lake area (53 d) > northern channels (38 d) > main lake area (26 d) > seasonal isolated lakes of Wucheng (17 d). Over the past 40 years, certain areas of Poyang Lake have experienced a slight decreasing trend in average residence time. After the operation of Three Gorges Dam, the average residence time of the entire lake decreases by about 4 d, with the northern channels exhibiting the largest decrease (9 d), followed by the main lake area (5 d); other regions show minimal change. The residence time during the receding period of Poyang Lake is significantly longer in wet years compared to dry years. A strong positive correlation exists between residence rate and water level during the receding period. The shortened residence time during the receding period in Poyang Lake is primarily attributed to the decreased water level and the accelerated recession rate. The results of this study can provide scientific support for the water environment governance and ecological restoration of Poyang Lake.

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  • 收稿日期:2025-04-15
  • 最后修改日期:2025-08-18
  • 录用日期:2025-08-19
  • 在线发布日期: 2025-11-05
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