Hydrodynamic effects of reconnecting lake group with Yangtze River in China

The hydrodynamic effects of reconnecting a lake group with the Yangtze River were simulated using a three-dimensional hydrodynamic model. The model was calibrated and validated using the measured water temperature and total phosphorous. The circulation patterns, water temperature, and water exchange...

Full description

Bibliographic Details
Main Authors: Ling Kang, Xiao-ming Guo
Format: Article
Language:English
Published: Elsevier 2011-12-01
Series:Water Science and Engineering
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1674237015301721
id doaj-9a2f4543f1f14e7ea29fa323dd4688f1
record_format Article
spelling doaj-9a2f4543f1f14e7ea29fa323dd4688f12020-11-24T20:54:50ZengElsevierWater Science and Engineering1674-23702011-12-014440542010.3882/j.issn.1674-2370.2011.04.005Hydrodynamic effects of reconnecting lake group with Yangtze River in ChinaLing KangXiao-ming GuoThe hydrodynamic effects of reconnecting a lake group with the Yangtze River were simulated using a three-dimensional hydrodynamic model. The model was calibrated and validated using the measured water temperature and total phosphorous. The circulation patterns, water temperature, and water exchange conditions between sub-lakes were simulated under two conditions: (1) the present condition, in which the lake group is isolated from the Yangtze River; and (2) the future condition, with a proposed improvement in which connecting the lake group with the Yangtze River will allow river water to be diverted into the lake group. The simulation period selected was characterized by extremely high temperature and very little rain. The results show that the cold inflow from the river has a significant effect on the water temperature only near the inlets, and the effect is more obvious in the lower water layers than that in the upper ones. The circulation pattern changes significantly and small-scale vortices only exist in part of the lake regions. The water exchange between sub-lakes is greatly enhanced with the proposed improvement. The water replacement rate increases with water diversion but varies in different sub-lakes. Finally, a new water diversion scheme was proposed to avoid contamination of some lakes in the early stage.http://www.sciencedirect.com/science/article/pii/S1674237015301721hydrodynamic modellake groupDonghu LakeYangtze River
collection DOAJ
language English
format Article
sources DOAJ
author Ling Kang
Xiao-ming Guo
spellingShingle Ling Kang
Xiao-ming Guo
Hydrodynamic effects of reconnecting lake group with Yangtze River in China
Water Science and Engineering
hydrodynamic model
lake group
Donghu Lake
Yangtze River
author_facet Ling Kang
Xiao-ming Guo
author_sort Ling Kang
title Hydrodynamic effects of reconnecting lake group with Yangtze River in China
title_short Hydrodynamic effects of reconnecting lake group with Yangtze River in China
title_full Hydrodynamic effects of reconnecting lake group with Yangtze River in China
title_fullStr Hydrodynamic effects of reconnecting lake group with Yangtze River in China
title_full_unstemmed Hydrodynamic effects of reconnecting lake group with Yangtze River in China
title_sort hydrodynamic effects of reconnecting lake group with yangtze river in china
publisher Elsevier
series Water Science and Engineering
issn 1674-2370
publishDate 2011-12-01
description The hydrodynamic effects of reconnecting a lake group with the Yangtze River were simulated using a three-dimensional hydrodynamic model. The model was calibrated and validated using the measured water temperature and total phosphorous. The circulation patterns, water temperature, and water exchange conditions between sub-lakes were simulated under two conditions: (1) the present condition, in which the lake group is isolated from the Yangtze River; and (2) the future condition, with a proposed improvement in which connecting the lake group with the Yangtze River will allow river water to be diverted into the lake group. The simulation period selected was characterized by extremely high temperature and very little rain. The results show that the cold inflow from the river has a significant effect on the water temperature only near the inlets, and the effect is more obvious in the lower water layers than that in the upper ones. The circulation pattern changes significantly and small-scale vortices only exist in part of the lake regions. The water exchange between sub-lakes is greatly enhanced with the proposed improvement. The water replacement rate increases with water diversion but varies in different sub-lakes. Finally, a new water diversion scheme was proposed to avoid contamination of some lakes in the early stage.
topic hydrodynamic model
lake group
Donghu Lake
Yangtze River
url http://www.sciencedirect.com/science/article/pii/S1674237015301721
work_keys_str_mv AT lingkang hydrodynamiceffectsofreconnectinglakegroupwithyangtzeriverinchina
AT xiaomingguo hydrodynamiceffectsofreconnectinglakegroupwithyangtzeriverinchina
_version_ 1716793528286183424