岩土力学
巖土力學
암토역학
ROCK AND SOIL MECHANICS
2013年
3期
639-644
,共6页
关进安%梁德青%吴能友%万丽华%李栋梁%苏正
關進安%樑德青%吳能友%萬麗華%李棟樑%囌正
관진안%량덕청%오능우%만려화%리동량%소정
含水合物沉积物%形成动力学%水合物含量%孔隙水压力%水力参数
含水閤物沉積物%形成動力學%水閤物含量%孔隙水壓力%水力參數
함수합물침적물%형성동역학%수합물함량%공극수압력%수력삼수
hydrate-bearing sediments%kinetics of formation%hydrate content%pore water pressure%hydraulic parameters
沉积物与流体流动的性质是影响水合物形成和聚集的两个重要因素,为研究水合物在沉积地层中的赋存机制必须探明高压环境下含水合物沉积物在非饱和渗流条件下的相互影响关系.以逸度差为水合物反应驱动力,反应动力学常数为Arrhenius 类型,建立了包括非饱和流体流动-沉积物特征-水合物形成动力学耦合的二维模型,从理论上研究了多孔介质内流体与沉积物参数如含水率、去饱和系数、水力分布和水合物饱和度等在孔隙内的相互影响规律.结果表明,在设定的条件下,随着反应的进行孔隙水压力随时间逐渐大,在相同条件下水合物饱和度与温度增加导致孔隙水压力变大,其中水合物饱和度的影响较小,而沉积物基质吸力、去饱和系数与本征动力学常数则与孔隙水压力成反向变化,其中本征动力学常数的影响较大.
沉積物與流體流動的性質是影響水閤物形成和聚集的兩箇重要因素,為研究水閤物在沉積地層中的賦存機製必鬚探明高壓環境下含水閤物沉積物在非飽和滲流條件下的相互影響關繫.以逸度差為水閤物反應驅動力,反應動力學常數為Arrhenius 類型,建立瞭包括非飽和流體流動-沉積物特徵-水閤物形成動力學耦閤的二維模型,從理論上研究瞭多孔介質內流體與沉積物參數如含水率、去飽和繫數、水力分佈和水閤物飽和度等在孔隙內的相互影響規律.結果錶明,在設定的條件下,隨著反應的進行孔隙水壓力隨時間逐漸大,在相同條件下水閤物飽和度與溫度增加導緻孔隙水壓力變大,其中水閤物飽和度的影響較小,而沉積物基質吸力、去飽和繫數與本徵動力學常數則與孔隙水壓力成反嚮變化,其中本徵動力學常數的影響較大.
침적물여류체류동적성질시영향수합물형성화취집적량개중요인소,위연구수합물재침적지층중적부존궤제필수탐명고압배경하함수합물침적물재비포화삼류조건하적상호영향관계.이일도차위수합물반응구동력,반응동역학상수위Arrhenius 류형,건립료포괄비포화류체류동-침적물특정-수합물형성동역학우합적이유모형,종이론상연구료다공개질내류체여침적물삼수여함수솔、거포화계수、수력분포화수합물포화도등재공극내적상호영향규률.결과표명,재설정적조건하,수착반응적진행공극수압력수시간축점대,재상동조건하수합물포화도여온도증가도치공극수압력변대,기중수합물포화도적영향교소,이침적물기질흡력、거포화계수여본정동역학상수칙여공극수압력성반향변화,기중본정동역학상수적영향교대.
Sediments and fluids characteristics are the two important factors affected the formation and accumulation of methane hydrate in deposits. In order to study methane hydrate occurrence in sediments, the influences of unsaturated fluids on hydrate-bearing sedimentary strata under high-pressure seepage environment must be discussed. The difference of fugacity has been adopted to be the driving force in this reaction. The hydrate intrinsic kinetic constant has been written in an Arrhenius-type equation. A two-dimensional (horizontal, vertical) model coupling the aspects of unsaturated flow fluids-sedimentary characteristics-hydrate formation kinetics has been established. The evolution of porous hydraulic parameters such as water content, to-saturation coefficient, pore water pressure and hydrate saturation have been discussed. Under the conditions setting in the simulation, the results show that the pore water pressure becomes larger with time during the reaction proceeding. Under the same conditions, the increase of strata temperature and hydrate saturation will increase the pore water pressure. The hydrate saturation causes less influence; while the sediments matric suction, to-saturation coefficient and hydrate intrinsic kinetic constant will vary inversely with the pore water pressure;and the to-saturation coefficient has more strong effects.