Water management for agricultural production in a coastal province of the Mekong River Delta under sea-level rise.

Author(s):  
D Ngo ◽  
T Chu ◽  
Q Tran ◽  
V Nguyen ◽  
D Tran ◽  
...  
PLoS ONE ◽  
2020 ◽  
Vol 15 (3) ◽  
pp. e0229464 ◽  
Author(s):  
SongYi Paik ◽  
Dung Thi Phuong Le ◽  
Lien Thi Nhu ◽  
Bradford Franklin Mills

2020 ◽  
Vol 12 (24) ◽  
pp. 10356
Author(s):  
Pham Thi Oanh ◽  
Makoto Tamura ◽  
Naoko Kumano ◽  
Quang Van Nguyen

This study evaluated inundation impacts and the economic damage resulting from sea level rise (SLR) in the Vietnamese Mekong River Delta (VMRD), and identified the effectiveness of mixing gray and green infrastructures using cost-benefit analysis. The results showed that the VMRD could potentially be heavily affected by SLR. Without the implementation of proper adaptations, more than 90% of this area could be below sea level and nearly 20 million people could be affected by inundation by the end of the 21st century. The total economic damage could reach more than 22,000 billion US$ (2010 real value) by 2100 with no discount rate. These threats may increase the pressure on the region to ensure well-being, equity, and progress towards achieving sustainable development goals. However, achieving these goals will require the implementation of adaptations for upgrading and restoring in the region. This study assessed the effectiveness of adaptations and demonstrated that mixing gray and green infrastructures could benefit coastal inhabitants at a cost of 12 to 19 billion US$.


2012 ◽  
Vol 78 (2) ◽  
pp. 386-399 ◽  
Author(s):  
Zhen Li ◽  
Yoshiki Saito ◽  
Limi Mao ◽  
Toru Tamura ◽  
Zhen Li ◽  
...  

AbstractMiddle Holocene vegetation and mangrove successions are clearly evident in the palynological records of two cores from the upper Mekong River delta in Cambodia. Spanning from ~ 9.4 to 6.3 cal ka BP, the cores mainly record a transgressive sequence from floodplain freshwater marsh to tidal flat, which was overlain by mangrove. Corresponding to the decelerated sea-level rise at ~ 8.3 cal ka BP, pioneer mangrove species Sonneratia alba and Sonneratia caseolaris appeared in the sediments, and then was replaced by regressive mangrove succession containing upward-increasing abundances of Rhizophora apiculata and Bruguiera spp. High salinity- and flooding-tolerant community S. alba was developed at the western core site PSG at ~ 8.2 cal ka BP, and the eastern core site PK at ~ 7.5 cal ka BP. The time difference of S. alba appearance between the two sites might be resulted from the complexity of sedimentary environment, where a higher sediment supply was provided to the western floodplain than to the eastern floodplain. After 7.5 cal ka BP, aggradational stacking of intertidal sediments, of which the thickness is larger than the present maximum tidal range, may have resulted from continuous sea-level rise during 7.5–7.0 cal ka BP.


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