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FROZEN HEAT

64

The major advances in understanding the drilling behaviour of in

situ gas hydrates have come through field programs dedicated

specifically to the study of gas hydrates. Substantial resources

have been devoted to gas hydrate research and development

over the past several decades (Collett

et al.

2009), with more

than 100 dedicated gas hydrate wells successfully drilled to date.

Several Integrated Ocean Drilling Program (IODP) expeditions

have investigated gas hydrate occurrences along active and

passive continental margins. Multi-well exploration campaigns

have been undertaken by national gas hydrate research programs

in Canada, China, India, Japan, Korea, and the United States.

In addition, dedicated research and development programs

Box 3.1

Gas hydrate coring and drilling studies

conducted offshore Japan and in permafrost settings in Canada

and Alaska have tested the effectiveness of gas hydrate drilling,

coring, and cementing technologies. The Japanese program

included a short horizontal well in gas-hydrate-bearing strata 350

metres below the sea floor (Takahashi and Tsuji 2005). At the

Mallik site in the Canadian Arctic, a full-scale thermal production

test was completed in 2002 (Dallimore and Collett 2005). Gas

hydrate production by depressurization of the reservoir was

tested there during successive winter programs in 2007 and

2008 (Dallimore

et al.

2012). In Alaska in 2012, an advanced

production test program involving carbon dioxide injection and

pressure drawdown was completed (Schoderbek

et al.

2012).

largely overcome these problems by introducing modifications

to the drilling procedures and equipment, including:

• Chilling the drill mud to reduce thermal disturbance of

the formation;

• Managing the weight of the drill mud to achieve sufficient

downhole pressure to stabilize the in situ gas hydrates,

while remaining below the pressures that might fracture

downhole formations;

• Using chemical additives (or avoiding dissociation-induc-

ing inhibitors such as salts and alcohols) in the drill mud

to maintain gas hydrate stability in the formation and pre-

vent gas hydrate dissociation in the drill cuttings;

Figure TB-3.1:

Notable gas hydrate field programs. This is a general representation of notable hydrate field programs that have

been or are taking place around the world. The compilation is indicative and does not necessarily depict all hydrate field programs.

Prudhoe

Bay area

Mallik test site

Northern Gulf

of Mexico

Blake Ridge

Svalbard

Indian

Ocean

Ulleung Basin

Qilian

Mountains

Eastern

Nankai

Trough

Shenhu

Basin

Gumusut-

Kakap

Taiwan

Messoyahka

New Zealand

Cascadia Margin

Japan Sea

Mexico

Costa Rica

Peru

Selected gas-hydrates study areas