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A GLOBAL OUTLOOK ON METHANE GAS HYDRATES

39

Figure 2.4-b:

Gas hydrates resource potential by global regions.

Estimates of the methane held in hydrates worldwide. Early

estimates for marine hydrates (encompassed by the green

region), made before hydrate had been recovered in the marine

environment, are high because they assume gas hydrates exist

in essentially all the world’s oceanic sediments. Subsequent

estimates are lower, but remain widely scattered (encompassed

by the blue region) because of continued uncertainty in the non-

uniform, heterogeneous distribution of organic carbon from which

the methane in hydrate is generated, as well as uncertainties in the

efficiency with which that methane is produced and then captured

in gas hydrate. Nonetheless, marine hydrates are expected to

contain one to two orders of magnitude more methane than exists

in natural gas reserves worldwide (brown square) (U.S. Energy

Information Administration 2010). Continental hydrate mass

estimates (encompassed by the pink region) tend to be about 1 per

cent of the marine estimates (Figure modified from Boswell and

Collett (2011)). Estimates are given in Gigatonnes of carbon (GtC)

for comparison with other organic hydrocarbon reservoirs. At

standard temperature and pressure, 1 GtC (Gigatonnes of carbon)

represents 1.9 Tcm (trillion cubic meters) of methane which has an

energy equivalent of approximately 74 EJ (exajoules).

the Gulf of Mexico (Frye

et al.

2008), and the eastern Nankai

Trough (Fujii

et al.

2008) provide insight into the resources that

might be available as sand-hosted gas hydrates. These studies

informed a recent global review by Johnson (2011), which pro-

vides a rough first-order estimate of the share of global in-place

resources of gas hydrates that could occur in sand reservoirs

(Figure 2.4). The estimate suggests significant potential tech-

nically recoverable resource (TRR) of gas hydrates in every re-

gion of the globe, with a cumulative mean estimate of in-place

resources within sand reservoirs of more than 1 217 trillion

cubic metres of gas. That value represents roughly 5 per cent of

the typical mid-range estimate for global gas hydrate in-place

resources. However, these estimates are highly speculative and

require significant field confirmation. The following sections

review a range of the best-studied occurrences of gas hydrates

in both coarse-grained and fine-grained reservoirs.

1

10

10

2

10

3

10

4

10

5

10

6

10

7

Global natural

gas reserves

(conventional)

First observation of marine hydrate

Estimates of the methane held

in hydrates worldwide

Gigatonnes carbon

1970 1975 1980 1985 1990 1995 2000 2005 2010

Methane in marine

gas hydrates

Methane in permafrost

gas hydrates

Methane in marine hydrates (based

only on the pressure and temperature

requirements for hydrate stability)

1

10

10

2

10

3

10

4

10

5

10

6

10

7

Global natural

gas reserves

(conventional)

First observation of marine hydrate

Estimates of the methane held

in hydrates orld ide

Gigatonnes carbon

1970 1975 1980 1985 1990 1995 2000 2005 2010

Methane in marine

gas hydrates

Methane in permafrost

gas hydrates

Methane in marine hydrates (based

only on the pressure and temperature

requirements for hydrate stability)