Experimental data are presented for methane hydrate stability conditio
ns in seawater (S almost-equal-to 33.5 part per thousand). For the pre
ssure range of 2.75-10.0 MPa, at any given pressure, the dissociation
temperature of methane hydrate is depressed by approximately -1.1 degr
ees-C relative to the pure methane-pure water system. These experiment
al results are consistent with previously reported thermodynamic predi
ctions and experimental results obtained with artificial seawater. Col
lectively these results provide a minimum constraint concerning depth
ranges over which methane hydrate is stable in the oceanic environment
.