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Experimental studies on the possible influences of composition changes of pore water on the stability conditions of methane hydrate in marine sediments

机译:孔隙水组成变化对海洋沉积物中甲烷水合物稳定性条件可能影响的实验研究

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摘要

Experiments with a set of electrolyte solutions have been carried out to investigate the effects of pore water composition changes on the stability conditions of methane hydrate in marine sediments. The results reveal that (1) SO_4~(2-) and CP concentration changes can affect hydrate stability slightly, (2) the changes in both the type and the concentration of cations, which occur in normal diagenetic processes, do not exert a significant influence on the methane hydrate stability conditions, and (3) the shift of hydrate stability in pore water can be expressed as a function of the Cl~- concentration only. Based on the results above, an empirical equation ΔT (K)=0.00206 Cl~- (mmol/dm~3) has been obtained for estimating the shift in the equilibrium temperature of methane hydrate in pore water at a given pressure.
机译:已经进行了一系列电解质溶液的实验,以研究孔隙水组成变化对海洋沉积物中甲烷水合物稳定性条件的影响。结果表明:(1)SO_4〜(2-)和CP浓度的变化对水合物的稳定性有轻微的影响;(2)正常成岩过程中发生的阳离子类型和浓度的变化都没有显着影响。对甲烷水合物稳定性条件的影响,以及(3)孔隙水中水合物稳定性的变化只能表示为Cl〜-浓度的函数。基于以上结果,获得了经验公式ΔT(K)= 0.00206 Cl〜(mmol / dm〜3),用于估算给定压力下孔隙水中甲烷水合物平衡温度的变化。

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