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Experimental study of the drilling process in hydrate-bearing sediments under different circulation rates of drilling fluid
Huang, Tianjia1,2,3,4; Li, Xiaosen1,2,3; Zhang, Yu1,2,3; Wang, Yi1,2,3; Chen, Zhaoyang1,2,3
刊名JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING
2020-06-01
卷号189页码:12
关键词Hydrate Drilling process Drilling fluid Circulation rate Hydrate dissociation TBAB
ISSN号0920-4105
DOI10.1016/j.petrol.2020.107001
通讯作者Zhang, Yu(zhangyu1@ms.giec.ac.cn)
英文摘要Natural gas hydrate (NGH) is widely considered a potential alternative to traditional energy resources. Some countries are trying to exploit and utilize NGH. However, due to the sensitivity of the hydrate, and a lack of exploitation experience with the NGH, drilling in hydrate reservoirs is considered risky. In order to understand the disturbance effects of drilling fluid with different circulation rates on the hydrate-bearing sediments during the drilling process, a novel hydrate drilling experimental apparatus was used to study the drilling process in the hydrate-bearing sediments. Four drilling experiments were carried out in consolidated sediments containing Tetra-n-butyl ammonium bromide (TBAB) hydrate. The drilling fluid injection rate ranges from 500 to 1800 g/min. The results show that hydrate dissociation can be induced by the circulation of relatively high-temperature drilling fluid when drilling in hydrate-bearing sediments, and that the hydrate dissociation rate is greatly influenced by the circulation rate of the drilling fluid. The drilling fluid invasion area has a maximum as the experiment progresses. Increasing the drilling fluid circulation rate can enhance the sediment temperature rise rate, enlarge the hydrate dissociation region, and increase cumulative TBAB production. Drilling fluid with a relatively low circulation rate is beneficial to wellbore stability. These findings will provide help with drilling design suitable for hydrate-bearing sediments, and provide a scientific basis for achieving safe drilling in hydrate-bearing sediments.
资助项目National Natural Science Foundation of China[51576202] ; National Natural Science Foundation of China[51676190] ; National Natural Science Foundation of China[51736009] ; National Key Research and Development Plan of China[2016YFC0304002] ; National Key Research and Development Plan of China[2017YFC0307306] ; Special project for marine economy development of Guangdong Province[GDME-2018D002] ; Natural Science Foundation of Guangdong Province of China[2017A030313301]
WOS关键词NATURAL-GAS ; WELLBORE INSTABILITY ; MASS-TRANSFER ; MODEL ; HEAT ; DISSOCIATION ; INVASION ; TBAB ; METHANE ; MUD
WOS研究方向Energy & Fuels ; Engineering
语种英语
出版者ELSEVIER
WOS记录号WOS:000522796600043
资助机构National Natural Science Foundation of China ; National Key Research and Development Plan of China ; Special project for marine economy development of Guangdong Province ; Natural Science Foundation of Guangdong Province of China
内容类型期刊论文
源URL[http://ir.giec.ac.cn/handle/344007/26965]  
专题中国科学院广州能源研究所
通讯作者Zhang, Yu
作者单位1.Chinese Acad Sci, Guangzhou Ctr Gas Hydrate Res, Guangzhou 510640, Peoples R China
2.Chinese Acad Sci, Guangzhou Inst Energy Convers, Key Lab Gas Hydrate, Guangzhou 510640, Peoples R China
3.Chinese Acad Sci, Guangdong Prov Key Lab New & Renewable Energy Res, Guangzhou 510640, Peoples R China
4.Univ Chinese Acad Sci, Beijing 10083, Peoples R China
推荐引用方式
GB/T 7714
Huang, Tianjia,Li, Xiaosen,Zhang, Yu,et al. Experimental study of the drilling process in hydrate-bearing sediments under different circulation rates of drilling fluid[J]. JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING,2020,189:12.
APA Huang, Tianjia,Li, Xiaosen,Zhang, Yu,Wang, Yi,&Chen, Zhaoyang.(2020).Experimental study of the drilling process in hydrate-bearing sediments under different circulation rates of drilling fluid.JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING,189,12.
MLA Huang, Tianjia,et al."Experimental study of the drilling process in hydrate-bearing sediments under different circulation rates of drilling fluid".JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING 189(2020):12.
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