金刚石钻进能量与花岗岩地层风化程度的关系

Relationship between diamond penetrating energy and weathered degree in granite formation

基于钻进过程监测系统在充填土-风化花岗岩地层中对液压旋转钻进的监测数据,对金刚石钻进系统的能量进行了分析.结果表明,钻进系统的能量分布与在普通风化花岗岩地层中的结果一致,黏滞能、动能以及钻进总能量与岩石的风化程度呈负相关,轴力功与岩石的风化程度呈正相关,说明金刚石钻进能量与岩石风化程度具有很好的响应关系.动能、轴力功及黏滞能受钻进方式影响,用于地层识别将受严格的可比条件限制.金刚石钻进比功随岩石风化程度的增强而减少,在不同风化程度的岩层中具有很好的分区性.而且,在充填土及全风化、强风化花岗岩地层中,金刚石旋转钻进比功值明显低于冲击凿碎比功,在微风化的坚硬岩中,旋转钻进比功则明显高于冲击凿碎比功.

Based on experimental data from a drilling process monitoring system instrumented with a hydraulic rotary drill rig in fill-weathered granite formation, the diamond penetrating energy was analyzed. The result shows that the distribution of the penetrating energy in fill-weathered granite formation agrees with that in common weathered granite formation. A negative correlation between the viscous energy, kinetic energy, total penetrating energy and the weathered degree of granite existed, and a positive correlation between the thrust force energy and the weathered degree was presented, which indicates that there is a well response between the penetrating energy and the weathered degree of rock. However, the kinetic energy, thrust force energy and viscous energy are limited in identification of formation because of different effects in various drilling modes. The specific energy of diamond drilling （SEDD） increased with the weathered degree of rock and the values of SEDD can be classified into corresponding range according to the weathered degree of rock. It is shown that the SEDD in rotary drilling is apparently less than the specific energy of percussive drilling （SEPD） in both fill soil and very strongly weathered granite formation. Reversely, the SEDD is much more than the SEPD in lightly weathered hard rock.