首页|海洋深水钻井含可燃冰地层物性响应大尺寸高仿真实验

海洋深水钻井含可燃冰地层物性响应大尺寸高仿真实验

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海洋深水钻遇可燃冰地层时,伴随传质传热的钻井液侵入行为会对近井壁地层的力学稳定产生重要影响,对地层物性的改变同时影响后续测井的质量和精度.因此,以墨西哥湾水合物联合工业计划中的Keathley Canyon井151-3井段水合物储层作为研究对象,首先利用压制胶结法制备了物性参数贴近实际的人造地层骨架,然后通过实验研究了原位储层地质与钻井工艺条件下钻井液侵入过程中近井壁地层的物性响应规律,分析了传质传热行为对地层温度、压力和电阻率的影响,得出了温差和压差的影响机理,建立了侵入深度与时间的函数关系.结果表明,通过正交试验优选的人造储层骨架孔隙度和电阻率与原位地层十分接近,分别相差1.29%和4.0%.压力的影响范围远快于温度和电阻率,而三者的影响范围都与时间呈现极强的数学关系.水合物的分解随着侵入深度的增加相继发生,表现为电阻率的变化,分解产生的游离气水向地层深处运移,易在温压变化范围之间区域重新形成水合物,呈现出高饱和水合物带.在地层破裂压力范围内,正压差对保持水合物相稳定起积极作用,从而有利于近井壁地层的稳定,而温差作用则恰为相反.现场钻井过程中,可通过提高钻井液密度、盐度,降低滤失量和添加抑制剂来减小对地层的影响.12 h的电阻率变化深度约为0.65 m,因此,电阻率测井作业中要获取未扰动水合物储层的电阻率数据,应减少钻测井之间的时间间隔,可采用随钻测井,或可采用探测深度合适的测井方法,如深侧向测井.
Large Scale and High Simulation Experimental Study on Physical Property Response of Combustible Ice Formation in Offshore Deepwater Drilling
When deep water drilling meets combustible ice formation,the invasion of drilling fluid accompanied by mass and heat transfer will have an important impact on the mechanical stability of the formation near the wellbore,changing the physical properties of the formation,and affecting the quality and accuracy of subsequent well logging.To address the problem,this paper takes the Gulf of Mexico Gas Hydrate Joint Industry Project(JIP)as the research object.Firstly,the artificial formation skeleton with physical parameters close to the actual is prepared by pressing cementation method.Then,the physical property response law of the formation near the wellbore during the invasion of drilling fluid under the conditions of in-situ reservoir geology and drilling technology is experimentally studied,and the effects of mass transfer and heat transfer behavior on formation temperature,pressure and resistivity are analyzed.The influence mechanism of temperature difference and pressure difference is obtained,and the functional relationship between invasion depth and time is established.The results show that the porosity and resistivity of the artificial reservoir skeleton optimized by orthogonal test are very close to those of the in-situ formation,with the difference of 1.29%and 4.0%respectively.The influence range of pressure is much faster than that of temperature and resistivity,and their influence range has a strong mathematical relationship with time.The decomposition of hydrate occurs successively with the increase of invasion depth,which is manifested in the change of resistivity.The free gas and water produced by decomposition migrate to the deeper,which is easy to reform hydrate in the area between the temperature and pressure variation range,showing a highly saturated hydrate zone.In the range of formation fracture pressure,the positive differential pressure plays a positive role in maintaining the stability of hydrate phase,which is conducive to the stability of near wellbore formation,while the effect of temperature difference is just the opposite.In the process of field drilling,the impact on the formation can be reduced by increasing the density and salinity of drilling fluid,reducing the filtration loss and adding inhibitors.The 12 hours resistivity variation depth is about 0.65 m.Therefore,in order to obtain the resistivity data of undisturbed hydrate reservoir during resistivity logging,the time interval between drilling and logging should be reduced.Logging while drilling or logging methods with appropriate detection depth,such as non-shallow lateral logging,can be used.

deep water drillingcombustible icelarge scale and high simulation experimentdrilling fluidsphysical properties response of the formationresistivity logginggeological engineering

周珂锐、郑明明、王凯、李可赛、王晓宇、陈禺树、刘天乐、吴祖锐

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成都理工大学地质灾害防治与地质环境保护国家重点实验室,四川成都 610059

中国科学院天然气水合物重点实验室(中国科学院广州能源研究所),广东 广州 510640

中国地质大学岩土钻掘与防护教育部工程研究中心,湖北武汉 430074

深水钻井 可燃冰 大尺寸高仿真实验 钻井液 储层物性相应 电阻率测井 地质工程

2024

地球科学
中国地质大学

地球科学

CSTPCD北大核心
影响因子:1.447
ISSN:1000-2383
年,卷(期):2024.49(11)