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1.
国内聚晶金刚石复合片（ＰＤＣ）传统的生产工艺流程如下：原材料处理→配料→研料→组装→压机合成→毛坯清检→加工→成品检验。其中组装方式直接影响ＰＤＣ的合成效果,最终也决定ＰＤＣ的质量。研究ＰＤＣ的生产工艺,关键在于组装方面。图１是传统的复合片生产组装方... 相似文献
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在ＤＤＣＭＰ应用于实时监控系统通信实践的基础上，对ＤＤＣＭＰ的工程技术问题进行了评估和分析。 相似文献
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两种最新型的PDC钻头 总被引：1，自引：0，他引：1
介绍了两种最新型的ＰＤＣ钻头，即双中心ＰＤＣ钻头和抗旋转ＰＤＣ钻头的特点。它们的出现弥补了ＰＤＣ钻头的不足，为ＰＤＣ钻头的应用又开辟了一个新的天地。 相似文献
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钻井工程用超硬材料及钻头的发展 总被引：10，自引：0，他引：10
介绍了钻井工程用超硬复合材料（包括ＰＤＣ、ＰＣＢＮ、陶瓷和金刚石膜）的发展现状及前景;同时也介绍了以这些材料切削具的钻头制造及应用情况;指出金刚石膜合成技术的发展已使金刚石膜制造钻井工程用切削具成为可能。 相似文献
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PDC钻头的新发展及应用 总被引：7，自引：0，他引：7
聚晶金刚石复合片钻头的发展及应用，大大提高了钻井的机械钻速，减少了钻井时间，降低了钻井成本，本文主要介绍ＰＤＣ钻头的发展与应用概况，几种新型的ＰＤＣ钻头与应用，以及ＰＤＣ钻头的偏转与解决办法。 相似文献
6.
沈健伟 《沉积与特提斯地质》1994,(4)
桂林地区晚泥盆世法门期末，海平面变化表现出高频率的特点，由此产生了５级旋回──ＰＡＣ（ｐｕｎｃｔｕａｔｅｄａｇｇｒａｄａｔｉｏｎａｌｃｙｃｌｅｓ）。ＰＡＣ是一种地层的幕式堆积方式，表现为间断加积的特点。本文讨论了桂林Ｄ／Ｃ界线层的ＰＡＣ，并认为ＰＡＣ中向上变浅之后出现的暴露面加上代表海水陡然加深的的页岩是短距离内不同相地层对比的极好标志，文中以额头村剖面新发现的可形刺：Ｐｓｅｕｄｏｐｏｌｙｇｎａｔｈｕｓｄｅｎｔｉｌｉｎｅａｔｕｓ和Ｐｓｅｕｄｏｐｏｌｙｇｎａｔｈｕｓｃｏｎｔｒａｖｅｒｓｕｓ作为参照物，对额头村剖面和南边村剖面的ＰＡＣ进行对比，从而提高浅水相Ｄ／Ｃ界线的精度。 相似文献
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涡轮钻和改进的ＰＤＣ钻头，在硬岩钻进中的应用Ｒｏｂｅｒｔ Ｃ．Ｂｏｕｄｒｅａｕｘ等马保松译孙友宏校在墨西哥湾地区，采用涡轮钻进配合具有改进的导轨式切削结构的ＰＤＣ钻头，提高了中硬一硬岩层中的钻进效率，与使用容积式马达的回转钻进相比，无论在什么样的钻进... 相似文献
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根据ＰＤＣ钻头的结构特点、破岩原理及现场使用情况，阐明了进行ＰＤＣ钻头井底流场试验研究的必要性和迫切性。结合国外的有关资料，设计出能够进行ＰＤＣ钻头单喷嘴射流特性、井底漫流特性及全尺寸钻头井底液流流动规律试验研究的实验装置。该装置实现了井底流场特性的三维空间测量。 相似文献
10.
PDC无心钻头结构参数与钻进性能的关系 总被引：2，自引：0，他引：2
ＰＤＣ无心钻头结构参数与钻头钻进性能有密切联系，通过全尺寸钻头室内实钻正交试验，研究了各结构参数与钻头钻进速度的关系，确定了ＰＤＣ无心钻头优化结构参数组合。 相似文献
11.
Mineralogical structures of carbon phases within the ureilite North West Africa 4742, a recent find, are investigated at various scales by high-resolution transmission electron microscopy (HRTEM), Raman microspectrometry and X-ray diffraction. Ureilites are the most carbon-rich of all meteorites, containing up to 6 wt.% carbon. Diamond, graphite and so-called “amorphous carbon” are typically described, but their crystallographic relationships and respective thermal histories remain poorly constrained. We especially focus on the origin of “amorphous carbon” and graphite, as well as their relationship with diamond.Two aliquots of carbon-bearing material were extracted: the insoluble organic matter (IOM) and the diamond fraction. We also compare the observed structures with those of laboratory-shocked graphite.Polycrystalline diamond aggregates with mean coherent domains of about 40 nm are reported for the first time in a ureilite and TEM demonstrates that all carbon phases are crystallographically related at the nanometre scale.Shock features show that diamond is produced from graphite through a martensitic transition. This observation demonstrates that graphite was present when the shock occurred and is consequently a precursor of diamond. The structure of what is commonly described as the “amorphous carbon” has been identified. It is not completely amorphous but only disordered and consists of nanometre-sized polyaromatic units surrounding the diamond. Comparison with laboratory-shocked graphite, partially transformed into diamond, indicates that the disordered carbon could be the product of diamond post-shock annealing.As diamond is the carrier of noble gases, whereas graphite is noble gas free, graphite cannot be the sole diamond precursor. This implies a multiple-stage history. A first generation of diamond could have been synthesized from a noble gas rich precursor or environment by either a shock or a condensation process. Thermally-induced graphitization of chondritic-like organic matter could have produced the graphite, which was then transformed by shock processes into polycrystalline nanodiamond aggregates. The formation of the disordered carbon occurred by diamond post-shock back-transformation during post-shock heating. The noble gases in the first generation diamond could then be incorporated directly into the disordered carbon during the transformation. 相似文献
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新型打滑地层钻头的研究 总被引：1，自引：1，他引：0
钻探施工中,经常遇到打滑地层,为了解决打滑地层钻进难题,国内外专家设计了不同类型的金刚石钻头,但都有一定的局限性.金刚石增强型硬质合金复合齿钻头保证了切削齿具有良好的自锐能力、切削齿与岩石接触面的比压大等特点,从本质上提高了钻头对打滑地层的适应性.室内微钻试验表明,金刚石增强型硬质合金复合齿钻头钻进打滑地层时具有高时效的优点. 相似文献
14.
Polycrystalline stishovite, synthesized in a multi-anvil apparatus at 15 GPa and 1200°C, contains numerous dislocations. The
microstructures of the recovered material have been investigated using Transmission Electron Microscopy (TEM). The Burgers
vectors of the dislocations were determined using Large Angle Convergent Beam Electron Diffraction (LACBED). We find that
<100>, <001>, <110> and <101> dislocations were activated in the stishovite during the synthesis experiments. Dislocation
microstructures, indicative of dislocation glide, suggest that plastic deformation occurred during quench. Subgrain boundaries
that are present in some grains indicate that some recovery occurred. As recovery is unlikely during quench, deformation also
occurred during synthesis.
Received: 6 October 1997 / Revised, accepted: 8 February 1998 相似文献
15.
J. Graham 《Rock Mechanics and Rock Engineering》1972,4(4):191-202
SummaryDamage Induced by a Sliding Diamond — an Approach to Hard Rock Drilling Optical methods were used to evaluate the early stages of damage caused by a loaded spherical diamond moving over a smooth surface, as a function of speed, radius, load and lubrication, for several homogeneous materials. New types of cracking patterns and abraded tracks have been observed. The statistical variation from track to track, and even within one track, is so great that quantitative conclusions are not possible at this stage, although some general effects of the variables are noted. Application to hard rock drilling is not straightforward and will probably have to await an evaluation of material removed.With 10 Figures 相似文献
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通过显微镜下观察充填红宝石内外部的充填特征、次生玻璃的形态,结合在Diamond ViewTM荧光成像仪下观察红宝石基底及次生玻璃体的发光情况,对红宝石中玻璃质材料充填的"量"进行了判断.将红宝石的充填程度分为轻微充填、中度充填、明显充填3等,建议对应定名为红宝石(备注可见轻微充填现象)、红宝石(备注可见中度充填现象)、充填处理红宝石. 相似文献
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金刚石是地球上最坚硬、对形成环境要求最苛刻的矿物之一。金刚石的矿物学特征、包裹体特征及碳稳定同位素组成记录了金刚石生长、熔蚀、搬运等地质过程中的温度、压力及物质成分等信息,是探索金刚石物质来源、形成过程和地球深部物理化学环境的重要研究对象。总结了国内外金刚石矿物学特征、包裹体特征和碳稳定同位素组成的相关研究成果,发现金刚石晶形和组合及其颜色可大致区分金刚石来源; 金刚石表面特征是区分原生金刚石与砂矿金刚石的重要鉴别特征; 金刚石包裹体类型及组合、包裹体年代学及金刚石碳稳定同位素研究,可分析金刚石物质来源和地球深部物理化学环境,确定金刚石形成时代,为研究金刚石成因、地幔岩石圈深部作用过程以及壳幔相互作用提供重要依据。 相似文献
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金刚石是地球上最坚硬、对形成环境要求最苛刻的矿物之一。金刚石的矿物学特征、包裹体特征及碳稳定同位素组成记录了金刚石生长、熔蚀、搬运等地质过程中的温度、压力及物质成分等信息,是探索金刚石物质来源、形成过程和地球深部物理化学环境的重要研究对象。总结了国内外金刚石矿物学特征、包裹体特征和碳稳定同位素组成的相关研究成果,发现金刚石晶形和组合及其颜色可大致区分金刚石来源; 金刚石表面特征是区分原生金刚石与砂矿金刚石的重要鉴别特征; 金刚石包裹体类型及组合、包裹体年代学及金刚石碳稳定同位素研究,可分析金刚石物质来源和地球深部物理化学环境,确定金刚石形成时代,为研究金刚石成因、地幔岩石圈深部作用过程以及壳幔相互作用提供重要依据。 相似文献
20.
某软基砂井堆载预压失效原因分析 总被引：2，自引：0，他引：2
谢秋兰 《地质灾害与环境保护》2005,16(3):325-327
在某防洪工程的软基砂井堆载预压处理中,两预压段虽然采用相同的预压加固设计方案．但在预压加固后的检测中发现.其中一预压段预压效果良好,达到设计要求,另一预压段软土特性未能得以明显改善。通过比较分析后认为,砂井堆载预压效果影响因素有井径、井距、砂料、垫层及软土成分等因素,通过合理的设计和施工,能有效地对软基进行加固处理。 相似文献