To estimation of temperature fluctuations in diamond grains when drilling with diamond bits

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Abstract

Abstract. If we consider the interacting pair: the matrix of a diamond crown, reinforced with protruding diamonds and rock, as a kind of system, then in the process of friction of the matrix against the bottom hole, external mechanical energy is converted into the energy of the heat and matter flows. The main concentration of the flows occurs in places where diamonds protrude above the matrix and take on an additional load. The rubbing system tries to smoothing itself by concentrating pressure and temperature on the diamonds. Diamonds, due to their higher hardness than the destructible medium, are pressed into the rock and destroy it. Since the process of cutting rocks is intermittent, the concentration of energy on diamonds occurs periodically, in the form of “flashes”. Each such “flash” is accompanied by a short-term increase in temperature in the contact zone (temperature fluctuation) and the spalling of a microparticle of the rock. In this work, from the standpoint of thermoelastic instability, the issue of temperature microflashes in single diamonds during the interaction of rough surfaces of the matrix of the diamond crown and the bottom of the borehole is considered, in order to take this factor into account in the mechanism of wear of the diamond of the drill bit. The value of temperature fluctuations on the surface of cutting diamonds was estimated and the size of the flash zone was determined. It is shown that temperature flashes of 400 (С < T* < 3650 (С are observed when drilling granite with a diamond crown on the diamond surface in an area of 5.8(10‑5 m, therefore, the presence of such “microflashes” on the diamond surface in a very small area in the process of interaction with the rock can lead to graphitization of the diamond in this place and separation from the surface of the grain. Such a mechanism should play a certain role in the wear and destruction of diamond surface areas during drilling. The magnitude of temperature fluctuations depends on the physical and mechanical properties of the contacting pair: diamond – rock, operating parameters of the tool and the nature of the placement of diamonds in the crown matrix. In this regard, the study of the assessment of temperature fluctuations in diamond grains when drilling with diamond bits may be of practical interest. Keywords: rock, thermal stresses, intensive cooling, macro- and microcrack system.
用金刚石钻头钻孔时,对金刚石颗粒温度波动的估计
摘要如果我们把相互作用的一对:由突出的钻石和岩石加固的金刚石冠的基体作为一种系统,那么在基体与井底的摩擦过程中,外部机械能被转化为热量和物质流动的能量。这些流动主要集中在钻石突出于基体之上并承担额外载荷的地方。摩擦系统试图通过将压力和温度集中在钻石上来使自己平滑。钻石,由于其硬度高于可破坏介质,被压入岩石并破坏它。由于切割岩石的过程是间歇性的,所以能量集中在钻石上是周期性地以“闪光”的形式发生的。每一次这样的“闪光”都伴随着接触区温度的短期升高(温度波动)和岩石微粒的剥落。本文从热弹性不稳定性的角度出发,研究了钻冠基体粗糙表面与井底相互作用过程中单颗金刚石的温度微闪问题,以便在钻头金刚石磨损机理中考虑这一因素。估计了切割金刚石表面的温度波动值,确定了闪光区的大小。结果表明,在5.8 m (10 - 5 m)的金刚石表面钻钻带有金刚石冠的花岗岩时,可观察到400 (С < T* < 3650 (С))的温度闪光,因此,在金刚石表面与岩石相互作用过程中,在很小的区域内出现这种“微闪光”会导致金刚石在该区域石墨化,并与晶粒表面分离。这种机制对钻削过程中金刚石表面的磨损和破坏应起到一定的作用。温度波动的幅度取决于接触副的物理和机械特性:金刚石-岩石、工具的操作参数和金刚石在冠基体中的放置性质。在这方面,对金刚石钻头钻孔时金刚石颗粒温度波动的评估研究可能具有实际意义。关键词:岩石,热应力,强化冷却,宏微裂纹系统。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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