Spatio-temporal patterns of hydrological processes and their responses to human activities in the Poyang Lake basin, China

• Published in: Hydrological sciences journal Vol. 56; no. 2; pp. 305 - 318
• Main Authors: Zhang, Qiang, Sun, Peng, Jiang, Tao, Tu, Xinjun, Chen, Xiaohong
• Format: Journal Article
• Language: English
• Published: Wallingford Taylor & Francis 30.03.2011; IAHS Press; Taylor & Francis Ltd
• Subjects: activités humaines; anthropogenic activities; charge sédimentaire; China; deforestation; Earth sciences; Earth, ocean, space; Exact sciences and technology; freshwater; humaines; human activities; Hydrology. Hydrogeology; Lac Poyang; Lakes; linear models; patron spatio-temporel; Poyang Lake; regression analysis; rivers; sediment load; sediments; spatio-temporal pattern; stream flow; streamflow; water reservoirs; watersheds; Yangtze River; écoulement en rivière; Great Britain; Asia; Europe; Avon England; China; England; United Kingdom; Far East; Western Europe; Yangtze River; rivers; floods; attenuation; reservoirs; inundations; human activity; sedimentation; deforestation; precipitation; discharge; erosion; construction; lakes; soils; fresh water; flow
• ISSN: 2150-3435; 0262-6667; 2150-3435
• DOI: 10.1080/02626667.2011.553615

Poyang Lake is the largest freshwater lake in China, and plays a major role in flood mitigation, restoration and conservation of the ecological environment in the middle Yangtze River basin. Sediment load and streamflow variations in Poyang Lake basin are important for the scouring and deposition changes of this lake. However, these hydrological processes are heavily influenced by human activities, such as construction of water reservoirs, and land-use/land cover changes. By thorough analysis of long series of sediment and streamflow obtained from five major hydrological stations, we systematically investigated the spatial and temporal patterns of these hydrological processes and the hydrological responses to human activities using the Mann-Kendall trend test, the double cumulative mass curve and the linear regression method. The results show: (1) no significant change in streamflow followed by an increasing tendency after the 1990s that turns to be decreasing about 2000; and (2) a sharp increase of sediment load during the late 1960s and 1970s triggered by extensive deforestation (during the “Cultural Revolution” in China) followed by a tendency to decrease after the early 1980s. Construction of water reservoirs has greatly reduced the sediment load of the Poyang Lake basin, and this is particularly the case in the Ganjiang River, where the sediment load changes may be attributed to the trapping effects of the Wan'an Reservoir, the largest water reservoir within the Poyang Lake basin. There is no evidence to corroborate the influence of water reservoirs on the streamflow variations. It seems that the streamflow variations are subject mainly to precipitation changes, but this requires further analysis. The current study may be of scientific and practical benefit in the conservation and restoration of Poyang Lake, as a kind of wetland, and also in flood mitigation in the middle Yangtze River basin that is under the influence of human activities.Citation Zhang, Q., Sun, P., Jiang, T. & Chen, X.-H. (2011) Spatio-temporal patterns of hydrological processes and their hydrological responses to human activities in the Poyang Lake basin, China. Hydrol. Sci. J.56(2), 305–318.