Seasonally inundated grasslands of the Mekong Delta Tran Triet - - PowerPoint PPT Presentation

seasonally inundated grasslands of the mekong delta
SMART_READER_LITE
LIVE PREVIEW

Seasonally inundated grasslands of the Mekong Delta Tran Triet - - PowerPoint PPT Presentation

Seasonally inundated grasslands of the Mekong Delta Tran Triet Vietnam National University Ho Chi Minh City floodplains Delta Delta floodplain Hydrology: seasonally inundated by Mekong flood water nutrient-rich


slide-1
SLIDE 1

Seasonally inundated grasslands of the Mekong Delta

Tran Triet Vietnam National University – Ho Chi Minh City

slide-2
SLIDE 2

Delta floodplains

slide-3
SLIDE 3
slide-4
SLIDE 4
slide-5
SLIDE 5

Delta floodplain

  • Hydrology:

– seasonally inundated by Mekong flood water – nutrient-rich

  • Geomorphologic setting:

– flat, low-laying, extensive depression areas on both sides and in between the Mekong and the Bassac channel – acid sulphate soils

  • Vegetation:

– Swamp forest dominated by Melaleuca cajuputi, intermingled with herbaceous marshes – Permanently inundated marshes/pools – Floating vegetation

slide-6
SLIDE 6

U-Minh Thuong

Sea water rise and recede Fresh water arrives

Geology Formation

slide-7
SLIDE 7

Sediment >12,000 yBP (old sediment) Sea water level Sea water level rise Marine sediment deposited and shell appeared Soil formation (> 6,000yBP) 12,000-6,000 yBP

slide-8
SLIDE 8

Sediment contain pyritic materials in 6,000-4,000yBP Marine sediment deposited in 12,000 - 6,000 yBP Sediment > 12,000 yBP (old sediment)

Sea water came

  • ut

Eroded sediment from up-stream of the Mekong river (rich Fe3+) deposited in mixed fresh and saline water (rich SO4=) in unaerobic condition to form Pyrite (FeS2)

Soil formation (6,000 – 4,000yBP)

Fresh water come in

Fe3+ SO4

=

Reduction

Fe2+ S-

FeS2

slide-9
SLIDE 9

Sediment > 12,000 yBP (old sediment)

Fresh water sediment deposited

  • n top to form the delta and build

river levees

Soil formation (<3,000yBP to date)

Marine sediment deposited in 12,000 - 6,000yBP Sediment contain pyritic materials in 6,000-4,000yBP

Water level in the dry season

Flood plain wetlands

slide-10
SLIDE 10

฀yritic ฀yritic materials฀ materials฀ exposed฀to฀the฀air exposed฀to฀the฀air

฀educe ฀xidi฀e

air/bacteria flooding/bacteria Fe(II)(TOXIC) Sulfide Fe(III)-red hydroxide Sulphate H+ (ACIDITY) Jarosite KFe3(SO4)2(OH)6 Aluminium (solid) acid (pH<4) Al3+(aq.)(TOXIC) ฀yrite฀฀e฀2 Potentially ASS Severely & moderately ASS

slide-11
SLIDE 11

A: Horizon with Organic matters Bg: Horizon (with Brown/Red

mottles)

Bj: Horizon (with Brown

and/or Jarosite mottles)

C: Horizon (with Pyritic materials) A typical profile of Acid Sulphate Soil

Ground water level during the dry season

slide-12
SLIDE 12
slide-13
SLIDE 13

Melaleuca swamp forest

slide-14
SLIDE 14

Seasonally inundated grassland

slide-15
SLIDE 15

Eleocharis dulcis

Inundation duration: long Inundation depth: medium to high Acidity: high Salinity: low to medium

slide-16
SLIDE 16

Eleocharis spiralis

Inundation duration: medium Inundation depth: medium Acidity: high Salinity: medium to high

slide-17
SLIDE 17

Lepironia grassland

Inundation duration: medium Inundation depth: medium Acidity: medium Salinity: low to medium

slide-18
SLIDE 18

Ischaemum grassland

Inundation duration: short to medium Inundation depth: low to medium Acidity: low to medium Salinity: low

slide-19
SLIDE 19

Panicum grassland

Inundation duration: short to long Inundation depth: low to medium Acidity: low to high Salinity: low to medium

slide-20
SLIDE 20

Phragmites grassland

Inundation duration: medium Inundation depth: medium Acidity: medium Salinity: low

slide-21
SLIDE 21

Aquatic vegetation in permanently inundated wetlands

slide-22
SLIDE 22
slide-23
SLIDE 23
slide-24
SLIDE 24

Bassac Marsh Boeung Prek Lapouv Tram Chim Ha Tien Plain Lang Sen

slide-25
SLIDE 25

Threats

  • Changing of

floodplain hydrology due to:

– irrigation – flood control

  • Wetland loss due to

agricultural expansion

  • Pollution
slide-26
SLIDE 26

Tram Chim National Park

  • 7,600 ha
  • Mosaic of Melaleuca

forests, grasslands and swamps

  • Critical habitats for

many species of water birds, including the Eastern Sarus crane (Grus antigone sharpii)

slide-27
SLIDE 27
slide-28
SLIDE 28
slide-29
SLIDE 29
slide-30
SLIDE 30

Eastern Sarus crane

slide-31
SLIDE 31

A flagship species of Tram Chim National Park

slide-32
SLIDE 32

Sarus Crane Movements

= KNOWN DRY SEASON LOCATIONS

Mekong Delta ?

slide-33
SLIDE 33

Stung Treng, Cambodia NEST ADULT Tram Chim, Vietnam

slide-34
SLIDE 34

Eleocharis spp. (Cyperaceae)

tubers

slide-35
SLIDE 35

= Water Gate

Hydrological restoration

slide-36
SLIDE 36

Water management

slide-37
SLIDE 37

50 100 150 200 250 300 350 400 450 500

1-Jun-95 1-Aug-95 1-Oct-95 1-Dec-95 1-Feb-96 1-Apr-96 1-Jun-96 1-Aug-96 1-Oct-96 1-Dec-96 1-Feb-97 1-Apr-97 1-Jun-97 1-Aug-97 1-Oct-97 1-Dec-97 1-Feb-98 1-Apr-98 1-Jun-98 1-Aug-98 1-Oct-98 1-Dec-98 1-Feb-99 1-Apr-99 1-Jun-99 1-Aug-99 1-Oct-99 1-Dec-99 1-Feb-00 1-Apr-00 1-Jun-00 1-Aug-00 1-Oct-00 1-Dec-00 1-Feb-01 1-Apr-01 1-Jun-01 1-Aug-01

Water level (cm AMSL)

Water level Ground level

Water level inside the core zone of Tram Chim National Park

slide-38
SLIDE 38

December, 1992 March, 1994 September, 1996 February, 1998

March, 2001

slide-39
SLIDE 39
slide-40
SLIDE 40
slide-41
SLIDE 41

Water birds increased

slide-42
SLIDE 42

Cranes decreased

slide-43
SLIDE 43

469 61 48 89 82 167 34 68 497 365 1052 814 741 665 159 113 302 271 631 503 511 200 400 600 800 1000 1200 1 9 8 6 1 9 8 8 1 9 9 1 9 9 2 1 9 9 4 1 9 9 6 1 9 9 8 2 2 2 2 4 2 6 Highest number of cranes observed

Number of cranes visiting Tram Chim 1986 - 2006

Number of cranes coming to Tram Chim

slide-44
SLIDE 44

200 400 600 800 1000 2001 2002 2003 2004 2005 2006 Number of cranes Mekong Delta Ang Trapeang Thmor Small Wetlands of Open Forest

CRANE POPULATION IN THE LOWER MEKONG BASIN 2001 - 200