GHASTLI — Determining physical properties of sediment containing natural and laboratory-formed gas hydrate
By: William J. Winters, William P. Dillon, Ingo A. Pecher, and David H. Mason
Edited by: Michael D. Max
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Abstract
Gas-hydrate samples have been recovered at about 16 areas worldwide (Booth et al., 1996). However, gas hydrate is known to occur at about 50 locations on continental margins (Kvenvolden, 1993) and is certainly far more widespread so it may represent a potentially enormous energy resource (Kvenvolden, 1988). But adverse effects related to the presence of hydrate do occur. Gas hydrate appears to have caused slope instabilities along continental margins (Booth et al., 1994; Dillon et al., 1998; Mienert et al., 1998; Paull & Dillon, (Chapter 12; Twichell & Cooper, 2000) and it has also been responsible for drilling accidents (Yakushev and Collett, 1992). Uncontrolled release of methane could affect global climate (Chapter 11), because methane is 15–20 times more effective as a “greenhouse gas” than an equivalent concentration of carbon dioxide. Clearly, a knowledge of gas-hydrate properties is necessary to safely explore the possibility of energy recovery and to understand its past and future impact on the geosphere.
| Publication type | Book chapter |
|---|---|
| Publication Subtype | Book Chapter |
| Title | GHASTLI — Determining physical properties of sediment containing natural and laboratory-formed gas hydrate |
| Chapter | 24 |
| DOI | 10.1007/978-94-011-4387-5_24 |
| Volume | 5 |
| Year Published | 2003 |
| Language | English |
| Publisher | Springer |
| Contributing office(s) | Coastal and Marine Geology Program |
| Description | 12 p. |
| Larger Work Type | Book |
| Larger Work Subtype | Monograph |
| Larger Work Title | Natural gas hydrate in oceanic and permafrost environments |
| First page | 311 |
| Last page | 322 |
| Google Analytic Metrics | Metrics page |