汶川地震断裂带科学钻探孔壁稳定时效特性研究
[Abstract]:Aiming at the problem of borehole wall instability in fault zone strata, this paper takes Wenchuan earthquake fault zone strata as an example to systematically study the time-effect of borehole wall instability. Firstly, the general situation of drilling project, stratum characteristics and in-situ stress distribution characteristics in Wenchuan earthquake fault zone strata are analyzed in detail. Secondly, the material composition and microstructure of rock samples in fault zone are obtained by microscopic test, and the variation of hydration stress and compressive strength of surrounding rock with hydration time are obtained by laboratory test. Based on the establishment and analysis of the mathematical model of formation borehole wall stability aging, the characteristics of drilling borehole wall stability aging in fault zone are studied in depth. The main achievements are as follows: (1) Through field data collection and differential strain analysis, the ground stress of the stratum where the rock sample is located is obtained, and the variation of ground stress with depth is deduced. Formula: _H = 0.098 *H-2.92 (R2 = 0.605), the formula has a certain reference value for the calculation of in-situ stress; (2) A series of laboratory experiments were carried out on rock samples, in which X-ray diffraction and infrared scanning experiments were carried out on rock samples in the fault zone, and the main mineral components of rock samples in the fault zone were analyzed as illite, quartz and chlorite. Stone and other clay minerals exist in the form of degradation, which is easy to destabilize the pore wall due to water swelling. Through scanning electron microscopy observation and analysis, the microstructure of the rock sample is obtained: sheet structure with a large number of micro-cracks and pore throats is the internal structural factor of pore wall instability. (3) According to strain experiment, the hydration stress with hydration time is drawn. The maximum hydration stress and the longest hydration stress time in different solutions are obtained. The hydration process of boreholes is simulated by FLAC3D software. The results show that the great change of rock mechanical strength is basically completed within 15 hours after the slurry immersion. After 15 hours, the curve is smooth and the decrease trend is slow. (4) According to the strength test, the result is obtained. The compressive strength and shear strength of rock samples under different hydration time and different grout types are obtained. The results show that the compressive strength and modulus of elasticity of rock decrease successively with the extension of hydration time, and the compressive strength of rock is especially affected by soaking time. The compressive strength of the core immersed in 2#, 3# drilling fluid decreases greatly, the compressive strength of the core immersed in 2#, 3# drilling fluid decreases minimally, and the compressive strength can still reach 36 MPa. (5) The relationship between hydration strain and hydration time is obtained by swelling test, and the swelling amount and ultimate failure form of the rock sample in different solutions are intuitively understood. Expansion of drilling fluid is restrained to some extent; (6) Based on the previous series of tests, in order to observe and analyze the change of hole wall morphology and the distribution and variation of corresponding stress in the process of instability more clearly and vividly, the in-situ stress, drilling fluid column pressure, pore pressure and hydration stress are analyzed in this project. The stress caused by the force acts on the surrounding rock of the hole wall together, and the stress distribution equation of the surrounding rock of the deep core drilling hole wall in the fault zone is obtained, and the Mohr-Coulomb criterion is selected as the criterion for judging the instability of the surrounding rock of the hole wall in the fault zone. (7) Using COMSOL Multiphysics platform, geomechanics module, porous elastic module and so on are adopted. A self-defined equation module is used to solve the mathematic model of borehole wall stability and aging in coring drilling in fault zone. The variation law of axial stress and radial stress distribution in the surrounding rock of borehole wall in fault zone is obtained, and the pressure distribution of borehole wall at different time is also obtained. (8) Taking the drilling operation in WFSD-1 water-sensitive creep fractured formation as an example, a drilling tool is developed. A modified sulfonated drilling fluid system with high density, low water loss, low permeability and strong lubrication is developed. The basic formula of the system is: 4% bentonite 10.2% soda + 0.5% high viscosity sodium carboxymethyl cellulose (HV-CMC) + 2% dehydrating agent (S-1) + 5% film forming agent (X-1) + 3% sulfonated asphalt (SAS) + 1% chromium-free sulfonated lignite (SMC) + barite powder. The aging problem of hole wall stability.
【学位授予单位】:成都理工大学
【学位级别】:硕士
【学位授予年份】:2017
【分类号】:P634
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