scholarly journals Physical Circulation And Spatial Exchange Dynamics In A Shallow Floodplain Wetland

Author(s):  
Z. Sharip ◽  
M.R. Hipsey ◽  
S.S. Schooler ◽  
R.J. Hobbs
Keyword(s):  
2015 ◽  
Vol 120 ◽  
pp. 39-50 ◽  
Author(s):  
Lili Yu ◽  
Adriana García ◽  
Allan R. Chivas ◽  
John Tibby ◽  
Tsuyoshi Kobayashi ◽  
...  

2020 ◽  
Vol 39 (1) ◽  
pp. 33-43
Author(s):  
Malabika Biswas Roy ◽  
Abhishek Kumar ◽  
Arnab Ghosh ◽  
Pankaj Kumar Roy

AbstractThis investigation additionally recognizes partner cooperation issue and furthermore to moderate the real issue through subjective and quantitative appraisal of riverine wetland. Considering a floodplain wetland in rustic West Bengal, the concentration was extended to perceive the type of wetland capacities as per the idea of individuals’ contribution by group examination. Be that as it may, NDVI was connected to ponder the total weeds condition into the wetland to decide the connection between Water Quality Index (WQI) with Normalized Difference Vegatation Index (NDVI) and its impact on valuation. In ANOVA, which is computed by MINITAB programming, centrality level was lower than 0.05 for each case.


2016 ◽  
Vol 47 (S1) ◽  
pp. 293-312 ◽  
Author(s):  
Xiuli Xu ◽  
Qi Zhang ◽  
Yunliang Li ◽  
Xianghu Li

Groundwater plays an important role in supplying water to vegetation in floodplain wetlands. Exploring the effect of water table depth (WTD) on vegetation transpiration is essential to increasing understanding of interactions among vegetation, soil water, and groundwater. In this study, a HYDRUS-1D model was used to simulate the water uptake of two typical vegetation communities, Artemisia capillaris and Phragmites australis, in a floodplain wetland (Poyang Lake wetland, China). Vegetation transpiration was compared for two distinct hydrological conditions: high water table (2012) and low water table (2013). Results showed that vegetation transpiration in the main growth stage (July–October) was significantly influenced by WTD. Under high water table conditions, transpiration of A. capillaris and P. australis communities in the main growth stage totaled 334 and 735 mm, respectively, accounting for over 90% of the potential transpiration. Under low water table conditions, they decreased to 203 and 510 mm, respectively, due to water stress, accounting for merely 55% of the potential transpiration. Scenario simulations found different linear relationships between WTD and the ratio of groundwater contribution to vegetation transpiration. An increase of 1 m in WTD in the main growth stage may reduce the ratio by approximately 25%.


Hydrobiologia ◽  
2018 ◽  
Vol 827 (1) ◽  
pp. 141-153 ◽  
Author(s):  
Kangle Lu ◽  
Haitao Wu ◽  
Zhenshan Xue ◽  
Xianguo Lu ◽  
Darold P. Batzer

2010 ◽  
Vol 393 (3-4) ◽  
pp. 349-361 ◽  
Author(s):  
Chris Bradley ◽  
Andrew Clay ◽  
Nicholas J. Clifford ◽  
John Gerrard ◽  
Angela M. Gurnell

2019 ◽  
Vol 6 ◽  
Author(s):  
Nathan J. Waltham ◽  
Damien Burrows ◽  
Carla Wegscheidl ◽  
Christina Buelow ◽  
Mike Ronan ◽  
...  

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