U MINH PEATSWAMP FORESTS VIETNAM Tran Triet Vietnam National - - PowerPoint PPT Presentation
U MINH PEATSWAMP FORESTS VIETNAM Tran Triet Vietnam National - - PowerPoint PPT Presentation
U MINH PEATSWAMP FORESTS VIETNAM Tran Triet Vietnam National University Ho Chi Minh City Duong Van Ni Can Tho University U Minh Thuong Vo Doi Peat swamps Hydrology: precipitation dominated permanently waterlogged
Vo Doi U Minh Thuong
Peat swamps
- Hydrology:
– precipitation dominated – permanently waterlogged
- Geomorphological setting:
– raised peats
- Vegetation:
– swamp forest dominated by Melaleuca cajuputi – grasslands
Cross section of U-Minh Thuong Peat dome
Colored water C
- l
- r
e d w a t e r Melaleuca forest Marine sediment layer in 12,000-6,000yBP Pyritic sediment layer 6,000-3,000 yBP
Fresh water sediment <3,000 yBP
e at
A B C Rain water Depend on locations, the soil are Non-acid soil (A), Medium acid soil (B), and Severely acid soil (C). Fossil as shell is indicator of marine sediment; Jarosite mottles is indicator of acid soils (Pyritic materials could not see). Water come in to the area is rain water only due high elevation of peat dome.
U Minh Thuong National Park
24,000 ha with 8000 ha core zone One of the two peat swamp forest areas of Vietnam
Peat dome grassland grassland grassland
MIXED SWAMP FOREST
20 40 60 80 100 120 140 160 180 200 1 5 A u g 9 9 1 5 S e p 9 9 1 5 O c t 9 9 1 5 N
- v
9 9 1 5 D e c 9 9 1 5 J a n 1 5 F e b 1 5 M a r 1 5 A p r 1 5 M a y 3 J u n 2 8 J u l 3 A u g 3 S e p 2 5 O c t 3 N
- v
2 8 D e c Elevation in cm (Average mean sea level)
Peat Water table Clay
March – April 2003
Catastrophic fire March-April 2002
Melaleuca regeneration after fire
Buø i Moá p Daá u daà u Traâ m Traø m
B Traø m Buø i Daá u daà u Moá p
C Traø m Daá u daà u
Forest fire
Euodia Alstonia Euginia Melaleuca llex Melaleuca Euodia
Before and after fire
Biodiversity is totally depend on the disturbance of the soil environment. If peat layer was removed (fire) or digging canal to expose the pyritic materials into the air, then oxidation processes will take place and actual acid soils will
- ccurred and biodiversity will be affected by acid water.