%0 Journal Article %1 xia2016dynamic %A Xia, Junqiang %A Deng, Shanshan %A Lu, Jinyou %A Xu, Quanxi %A Zong, Quanli %A Tan, Guangming %D 2016 %I The Author(s) %J Scientific Reports %K MyYangtzeWork china %P 22802 %R 10.1038/srep22802 %T Dynamic channel adjustments in the Jingjiang Reach of the Middle Yangtze River %U https://doi.org/10.1038/srep22802 %V 6 %X Significant channel adjustments have occurred in the Jingjiang Reach of the Middle Yangtze River, because of the operation of the Three Gorges Project (TGP). The Jingjiang Reach is selected as the study area, covering the Upper Jingjiang Reach (UJR) and Lower Jingjiang Reach (LJR). The reach-scale bankfull channel dimensions in the study reach were calculated annually from 2002 to 2013 by means of a reach-averaged approach and surveyed post-flood profiles at 171 sections. We find from the calculated results that: the reach-scale bankfull widths changed slightly in the UJR and LJR, with the corresponding depths increasing by 1.6 m and 1.0 m; the channel adjustments occurred mainly with respect to bankfull depth because of the construction of large-scale bank revetment works, although there were significant bank erosion processes in local regions without the bank protection engineering. The reach-scale bankfull dimensions in the UJR and LJR generally responded to the previous five-year average fluvial erosion intensity during flood seasons, with higher correlations being obtained for the depth and cross-sectional area. It is concluded that these dynamic adjustments of the channel geometry are a direct result of recent human activities such as the TGP operation.

@article{xia2016dynamic, abstract = {Significant channel adjustments have occurred in the Jingjiang Reach of the Middle Yangtze River, because of the operation of the Three Gorges Project (TGP). The Jingjiang Reach is selected as the study area, covering the Upper Jingjiang Reach (UJR) and Lower Jingjiang Reach (LJR). The reach-scale bankfull channel dimensions in the study reach were calculated annually from 2002 to 2013 by means of a reach-averaged approach and surveyed post-flood profiles at 171 sections. We find from the calculated results that: the reach-scale bankfull widths changed slightly in the UJR and LJR, with the corresponding depths increasing by 1.6 m and 1.0 m; the channel adjustments occurred mainly with respect to bankfull depth because of the construction of large-scale bank revetment works, although there were significant bank erosion processes in local regions without the bank protection engineering. The reach-scale bankfull dimensions in the UJR and LJR generally responded to the previous five-year average fluvial erosion intensity during flood seasons, with higher correlations being obtained for the depth and cross-sectional area. It is concluded that these dynamic adjustments of the channel geometry are a direct result of recent human activities such as the TGP operation.}, added-at = {2019-11-06T12:33:56.000+0100}, author = {Xia, Junqiang and Deng, Shanshan and Lu, Jinyou and Xu, Quanxi and Zong, Quanli and Tan, Guangming}, biburl = {https://www.bibsonomy.org/bibtex/29c2022fef4d473c55120747c8cc7bb59/pbett}, description = {Dynamic channel adjustments in the Jingjiang Reach of the Middle Yangtze River | Scientific Reports}, doi = {10.1038/srep22802}, interhash = {f0793384d6eff0d231db841b57a2c1a6}, intrahash = {9c2022fef4d473c55120747c8cc7bb59}, journal = {Scientific Reports}, keywords = {MyYangtzeWork china}, month = mar, pages = 22802, publisher = {The Author(s)}, timestamp = {2019-11-06T12:33:56.000+0100}, title = {Dynamic channel adjustments in the Jingjiang Reach of the Middle Yangtze River}, url = {https://doi.org/10.1038/srep22802}, volume = 6, year = 2016 }