Numerical and experimental study of the stability of non-circular boreholes in high-permeability formations

Lavrov, Alexandre; Taghipour, Ali; Ytrehus, Jan David; Mårdalen, Jostein; Lund, Halvor; Vrålstad, Torbjørn; Lund, Bjørnar; Carlsen, Inge M.; Saasen, Arild; Wold, Sturla; Abdollahi, Jafar; Torsvoll, Arne; Reyes, Angel Espinosa; Næumann, J.R.; Melchiorsen, J.C.; Skalle, P.

doi:10.1016/j.ijrmms.2014.02.018

Cited by 5 publications

(1 citation statement)

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“…In the field of oil and gas exploitation, extensive analytical, experimental and numerical studies have been carried out on surface borehole instability [2][3][4][5][6][7][8][9]. The relevant research has focused on areas as diverse as the mechanism and regularity of borehole failure due to pre-existing rock fractures, crustal stress, as well as soft or unconsolidated rock formations, the rock failure criteria for predicting borehole shear failure and the drilling technique and method of improving the borehole stability, etc.…”

Section: Introductionmentioning

confidence: 99%

A Case Study of Surface Borehole Wall Dislocation Induced by Top-Coal Longwall Mining

2017

Energies

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Underground coal extraction causes failure and movement of overlying strata, which could also result in the dislocation of vertical surface boreholes. Investigating the correlation between the dislocation of surface boreholes and the broken of overlying strata is of great significance in deducing the mining-induced dynamic movement of overlying strata, which cannot be seen inside the 'black box'. Field measurement, laboratory experiment and theoretical analysis were employed to study the mechanism of the mining-induced dislocation of surface boreholes, and its relationship with the movement of overlying strata. Due to different deflection angles of adjacent strata, the horizontal movement of strata varies, and this contributes primarily to the dislocation of borehole wall. As the development of strata movement from the mining level towards surface, the position of borehole dislocation also occurred upwards, and the highest borehole dislocation occurred at the same position of overlying Key Stratum (KS). In other words, when a KS breaks, borehole dislocation will occur and develop from the bottom of this KS until the bottom of an upper KS. These key findings can provide a theoretical basis for deducing the mining-induced movement of overlying strata, determining the KS position and assessing the water conductivity of broken strata.

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