Vegetation of the water-level fluctuation zone in the Three Gorges Reservoir at the initial impoundment stage

The water-level of Three Gorges Reservoir first reached a normal storage level 175 m in October 2010, resulting in a large-area water-fluctuating zone with an elevation difference of 30 m (145–175 m). We used the Geographic Information System (GIS) technology, the field quadrat survey, the species i...

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Main Authors: Kang-wen Zhu, Yu-cheng Chen, Sheng Zhang, Bo Lei, Zhi-min Yang, Lei Huang
Format: Article
Language:English
Published: Elsevier 2020-03-01
Series:Global Ecology and Conservation
Online Access:http://www.sciencedirect.com/science/article/pii/S2351989419305232
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author Kang-wen Zhu
Yu-cheng Chen
Sheng Zhang
Bo Lei
Zhi-min Yang
Lei Huang
author_facet Kang-wen Zhu
Yu-cheng Chen
Sheng Zhang
Bo Lei
Zhi-min Yang
Lei Huang
author_sort Kang-wen Zhu
collection DOAJ
description The water-level of Three Gorges Reservoir first reached a normal storage level 175 m in October 2010, resulting in a large-area water-fluctuating zone with an elevation difference of 30 m (145–175 m). We used the Geographic Information System (GIS) technology, the field quadrat survey, the species importance value calculation, and literature data to assess the natural environment situation, the vegetation regeneration status, and the ecological benefits of the dominant plant species in terms of mitigating agricultural non-point source pollution of the WLFZ in the Three Gorges Reservoir at the initial impoundment stage. The results showed that: (1) the WLFZ area presented an obvious trend of increasing first and then decreasing from west to east, and the exposed area at the elevation intervals of 145–175 m, 155–175 m, and 165–175 m accounted for 20, 37.49, and 42.51% of the total area, respectively; (2) the WLFZ area gradually decreased with increasing gradient, and the exposed area at the gradient intervals of <15°, 15–25°, 25–35°, 35–60°, and >60° accounted for 60.90, 18.62, 12.03, 8.06, and 0.39%, respectively, of the total area. (3) The vegetated area increased with increasing water level elevation, and the vegetation coverage area at elevation intervals of 145–155 m, 155–165 m, and 165–175 m accounted for 4.96, 16.09, and 44.77%, respectively, of the total area of the corresponding elevation interval. The vegetated area gradually decreased with increasing gradient, and at the sections Jiangjin-Changshou, Fuling-Yunyang, and Fengjie-Yiling, the vegetated area accounted for 15.30, 71, and 12.70%, respectively, of the total vegetation coverage area. (4) The important value calculation results indicate that the dominant species significantly differed among the different elevations in the three belt transects of the Yangtze River main stream (Zhongxian section), the Xiaojiang River (Kaizhou section), and the Xiangxi River (Guizhou section). The dominant annual herb species were Digitaria sanguinalis (Linn.) Scop., Conyza canadensis (Linn.) Cronq., Bidens frondosa Linn., Echinochloa crusgali (Linn.) Beauv., and Setaria viridis (Linn.) Beauv., while the dominant perennial herb species were Cynodon dactylon(Linn.) Pers. and Cyperus rotundus Linn.. (5) The water level elevation was the most important factor affecting vegetation restoration. At the initial impoundment stage, the naturally regenerating plant species Cynodon dactylon(Linn.) Pers. and Cyperus rotundus Linn. could be used to prevent and control regional agricultural non-point source pollution, combined with the establishment of plant hedges using the native species Morus alba L. and Vitex negundo Linn.. We provide a scientific basis for the development of measures to mitigate agricultural non-point source pollution in the Three Gorges Reservoir area, using ecological restoration. Keywords: GIS analysis, Water-level fluctuation zone (WLFZ), Three Gorges reservoir area, Dominant species, Agricultural non-point source pollution
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spelling doaj.art-bbae4238b88b40ec839fabb18ee27d742022-12-21T18:49:02ZengElsevierGlobal Ecology and Conservation2351-98942020-03-0121Vegetation of the water-level fluctuation zone in the Three Gorges Reservoir at the initial impoundment stageKang-wen Zhu0Yu-cheng Chen1Sheng Zhang2Bo Lei3Zhi-min Yang4Lei Huang5College of Resources and Environment, Southwest University, 400716, ChinaCollege of Resources and Environment, Southwest University, 400716, China; Chongqing Engineering Research Center of Rural Cleaning, Chongqing, 400716, China; Corresponding author. Chongqing Engineering Research Center of Rural Cleaning, Chongqing, 400716, China.Chongqing Academy of Ecology and Environmental Sciences, Chongqing, 401147, China; Corresponding author. Chongqing Academy of Ecology and Environmental Sciences, Chongqing, 401147, China.Chongqing Academy of Ecology and Environmental Sciences, Chongqing, 401147, ChinaCollege of Resources and Environment, Southwest University, 400716, China; Chongqing Engineering Research Center of Rural Cleaning, Chongqing, 400716, ChinaCollege of Resources and Environment, Southwest University, 400716, China; Chongqing Engineering Research Center of Rural Cleaning, Chongqing, 400716, ChinaThe water-level of Three Gorges Reservoir first reached a normal storage level 175 m in October 2010, resulting in a large-area water-fluctuating zone with an elevation difference of 30 m (145–175 m). We used the Geographic Information System (GIS) technology, the field quadrat survey, the species importance value calculation, and literature data to assess the natural environment situation, the vegetation regeneration status, and the ecological benefits of the dominant plant species in terms of mitigating agricultural non-point source pollution of the WLFZ in the Three Gorges Reservoir at the initial impoundment stage. The results showed that: (1) the WLFZ area presented an obvious trend of increasing first and then decreasing from west to east, and the exposed area at the elevation intervals of 145–175 m, 155–175 m, and 165–175 m accounted for 20, 37.49, and 42.51% of the total area, respectively; (2) the WLFZ area gradually decreased with increasing gradient, and the exposed area at the gradient intervals of <15°, 15–25°, 25–35°, 35–60°, and >60° accounted for 60.90, 18.62, 12.03, 8.06, and 0.39%, respectively, of the total area. (3) The vegetated area increased with increasing water level elevation, and the vegetation coverage area at elevation intervals of 145–155 m, 155–165 m, and 165–175 m accounted for 4.96, 16.09, and 44.77%, respectively, of the total area of the corresponding elevation interval. The vegetated area gradually decreased with increasing gradient, and at the sections Jiangjin-Changshou, Fuling-Yunyang, and Fengjie-Yiling, the vegetated area accounted for 15.30, 71, and 12.70%, respectively, of the total vegetation coverage area. (4) The important value calculation results indicate that the dominant species significantly differed among the different elevations in the three belt transects of the Yangtze River main stream (Zhongxian section), the Xiaojiang River (Kaizhou section), and the Xiangxi River (Guizhou section). The dominant annual herb species were Digitaria sanguinalis (Linn.) Scop., Conyza canadensis (Linn.) Cronq., Bidens frondosa Linn., Echinochloa crusgali (Linn.) Beauv., and Setaria viridis (Linn.) Beauv., while the dominant perennial herb species were Cynodon dactylon(Linn.) Pers. and Cyperus rotundus Linn.. (5) The water level elevation was the most important factor affecting vegetation restoration. At the initial impoundment stage, the naturally regenerating plant species Cynodon dactylon(Linn.) Pers. and Cyperus rotundus Linn. could be used to prevent and control regional agricultural non-point source pollution, combined with the establishment of plant hedges using the native species Morus alba L. and Vitex negundo Linn.. We provide a scientific basis for the development of measures to mitigate agricultural non-point source pollution in the Three Gorges Reservoir area, using ecological restoration. Keywords: GIS analysis, Water-level fluctuation zone (WLFZ), Three Gorges reservoir area, Dominant species, Agricultural non-point source pollutionhttp://www.sciencedirect.com/science/article/pii/S2351989419305232
spellingShingle Kang-wen Zhu
Yu-cheng Chen
Sheng Zhang
Bo Lei
Zhi-min Yang
Lei Huang
Vegetation of the water-level fluctuation zone in the Three Gorges Reservoir at the initial impoundment stage
Global Ecology and Conservation
title Vegetation of the water-level fluctuation zone in the Three Gorges Reservoir at the initial impoundment stage
title_full Vegetation of the water-level fluctuation zone in the Three Gorges Reservoir at the initial impoundment stage
title_fullStr Vegetation of the water-level fluctuation zone in the Three Gorges Reservoir at the initial impoundment stage
title_full_unstemmed Vegetation of the water-level fluctuation zone in the Three Gorges Reservoir at the initial impoundment stage
title_short Vegetation of the water-level fluctuation zone in the Three Gorges Reservoir at the initial impoundment stage
title_sort vegetation of the water level fluctuation zone in the three gorges reservoir at the initial impoundment stage
url http://www.sciencedirect.com/science/article/pii/S2351989419305232
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