1. A sedimentary evolvement record and its response to anthropogenic-driven pressure in the shallow Honghu Lake over a century
- Author
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Mingli Zhang, Hao Wang, Yanhua Wang, and Jing Wu
- Subjects
210Pb ,sedimentation rate ,grain size of sediments ,Honghu Lake ,Geology ,QE1-996.5 ,Physical geography ,GB3-5030 - Abstract
Lake sediments record the environment during the lake sedimentation whose characteristics can infer environmental changes and human activities. In this study, the 210Pb chronologies and sedimentation rate of the sediment core in Honghu Lake were calculated by the Constant Rate of Supply model. The characteristics of the sedimentary environment were analysed by using physical and chemical indicators. Four stages were divided as follows: Stage A (before 1900): The relatively low sedimentation rate and nutrient content indicated an extremely stable sedimentary environment. Stage B (1900–1949): With the growth of population, the intensity of land use began to increase, with an averaged sedimentation rate of 0.252 g·cm−2·a−1. Stage C (1949–1980): The sedimentation rate and nutrient content increased markedly. The intense human activity has damaged the surrounding vegetation leading to soil erosion and accelerated sedimentation rate. With the deterioration of the lake water environment, the organic matter source was mainly the internal source represented by algae and bacteria. Stage D (1980–2011): Influenced by the difference in land use types along the coast, the sedimentation rate of HH-A (0.570 g·cm−2·a−1) is higher than that of HH-B (0.445 g·cm−2·a−1). The results are of significance to the management of rural lakes and reservoirs.
- Published
- 2024
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