why reclamation of nearshore manila bay is a very bad idea part i
DESCRIPTION
Dr. Kelvin Rodlfo's presentation on the hazards of the Manila Bay Reclamation project. Part 1 of 2.TRANSCRIPT
Three reasons why reclamation of nearshore Manila Bay is a VERY BAD IDEA:
1. Rapid subsidence of coastal lands is enhancing the risk of flooding and high tides.
2. Storm surges are an ever-worsening threat, due in part to subsidence, but also from climate change because typhoons are increasing in strength and frequency.
3. Reclaimed coastal areas are the most susceptible to liquefaction during earthquakes.
At Manila’s South Harbor, mean sea level rose at about 2 millimeters per year from 1902 to the early 1960’s. . .
. . . then started rising ten times as fast. WHY?
Groundwater withdrawal!
<20 million liters per day (MLD)
250 MLD
778 MLD
1770 MLD in 2004 (CEST 2004)
989 MLD in 1990 (JICA 1992)
Metro Manila`s
groundwater demand
is still increasing.
Consequently, subsidence
will continue and may even
accelerate!
(Global warming)
January 25, 1999 April 14, 2012
(Pinkish areas are house roofs)
Growth of Metro Manila
More areas below
sealevel
1900 1920 1940 1960 1980 2000 Year
12
10
8
6
4
2
0
Metr
o M
an
ila P
op
ula
tion
, m
illio
ns
GW
Extr
act
ion
, M
illio
n L
iters
per
Day
1800
1600
1400
1200
1000
800
600
400
200
0<20
250
778
989
Metro Manila Ground Water Usage
As population increases, groundwater use increases !!!
Average recharge for Metro Manila = 564
MLD (JICA 1992)
1770
If we use more water than nature
can put back (“recharge”), the land must sink!
Growth of Metro Manila Population
Pumping water too rapidly out of the aquifer reduces the pressure pore spaces between grains of sand and gravel. Water in the clay layers is sucked into the aquifer.
This causes the clay layers to shrink . . .
. . . and the ground surface to sink.
Pipe may appear to rise out of the ground
Pumps extract water from “aquifers” –layers of sand and gravel soaked with water.
How groundwater withdrawal causes land to subside
Loosely packed sand
When water is removed, grains crowd together a little more closely.
Volume is somewhat reduced, so land sinks a little. But sand cannot
compact very much.Clay deposits contains much more water . . .
and can shrink much more.
Our delta sediments are very clayey!
Subsidence from water withdrawal
Benchmarks used for re-leveling (1978 vs 2000) survey (Jacob 2004)
0.95
1.40
1.46
0.76
0.790.1
60.77 0.9
6
0.96
0.88
0.57
0.67
0.95
0.73
0.61
0.59
0.51
0.57
0.43
0.46
0.46
0.46 0.4
7
0.64
Maximum magnitude of subsidence – 1.46 meters or 6.4 centimeters/year (about 2½ inches/year) .
More recently, Lagmay et al. of National Institute of Geological Sciences have measured subsidence using satellite-borne Permanent Scatterer Interferometric Synthetic Aperture Radar
Subsidence in Greater Metro
Manila and vicinity from 2003-2006 from PSInSAR
(precision satellite data)
+ 19.2 mm/y
-43.8 mm/y
0 mm/y
MalolosGuiguinto
Valenzuela
Marilao
Kalookan
Obando
Taguig-Pateros
NavotasMalabon
Manila
Las PiñasMuntinglup
a
Cavite City
KawitRosario
Dasmariñas
San Pedro-Biñan
Mga Ibang Lungsod na Tabing-dagat sa Silangang Asia na Lumulubog Dahil sa Sobrang
Paggamit ng Tubig-poso SUBSIDENCE
LOCATION PERIOD Meters cm/year
Tokyo, 1918-87 4.5 6.5 Japan
Tokyo
Osaka, 1934-68 2.8 8.2 Japan
Osaka Shanghai, 1921-65 2.63 6 China
Shanghai
Yun-Lin, 1989-97 0.66 8.25 Taiwan (Fishpond area!)
Yun-Lin
Hanoi, 1988-93 0.1-0.3 2-6 Vietnam
Hanoi
KAMANAVA 1991-2002 0.3-1 2.7– 9.1
Manila
Bangkok, 1980-90 0.5-1 5-10 Thailand
Bangkok
Jakarta, 1991-99 0.3-0.8 4-10 Indonesia Jakarta
Dahil halos pantay ang lupain sa paligid ng Manila Bay, kahit maliit na pagtaas ng dagat
ay mahalaga.
Ang ibig sabihin nito ay kung tataas ang dagat ng isang metro
lamang, susulong ang tubig-dagat ng 10 o 20 kilometro.
. . . Ang lupa ay nakaangat ng 1 metro lamang mula sa taas ng
dagat.
10 o 20 kilometros mula sa dalampasigan…
Lowering of coasts (land subsidence) makes them increasingly vulnerable to the attack of waves and storm surges.
2. Storm surge
Storm Surge--Typhoon Pedring in Philippines(1).mov
23 September 2011 Super Typhoon Pedring
Roxas Boulevard
[stop the slide show and click the video icon below
before resuming the presentation]