厚壁套管与植物胶用于深厚砂卵砾石层钻进的应用研究

针对大渡河巴底水电站深厚覆盖层钻进过程中遇到的护壁、取心、孔内事故等主要技术问题,采用Ф139mm厚壁套管护壁和SH植物胶取心钻进工艺,有效地提高了取心质量和钻进效率。Ф139mm厚壁套管可以有效克服深厚覆盖层钻进过程中薄壁套管护壁导致孔内事故频发以及跟进深度较浅等致命缺点,也克服了Ф127mm常规厚壁地质管材不能下如薄壁Ф108mm套管的缺点。该工艺不仅提高了取心质量,也极大地提高了钻进效率和保证了成孔概率,节约钻进成本,提高了经济效益。     

深孔绳索取心钻杆质量控制措施

在优化深孔绳索取心钻杆结构设计、选用优质钢材基础上,制定合理的加工工艺和检测规程,配齐相应的检测器具。通过严格的工艺控制,确保钻杆质量稳定,满足深孔绳索取心钻进需要。     

若尔盖复杂地层钻进工艺研究及探讨

川西北高原高寒山区若尔盖铀矿地层“漏失、垮塌、超径、孔斜”,是典型的“五毒俱全”、国内少见的钻探复杂地层。我们通过认真的分析和研究,从工艺技术上改进,采用优质泥浆体系,成功穿越了近300米的炭质板岩层;采用连续造斜器成功实施了深孔定向钻进,为在复杂地层下一基多孔工艺提供了依据。     

浅谈复杂地层科学钻探理念

随着地质找矿方向转向“攻深找盲”,钻探工程施工难度也节节攀升;未来钻孔多以深孔、斜孔为主,面临的地层情况也将越来越复杂,只有坚持科技钻探理念、做好科技钻探理念传承、加强钻探科技发展和更新、做好系统化、标准化、档案化的科学管理,才能为钻探企业注入新的活力,使其能在新的地勘形势下获得更强的生命力。     

富县探区页岩气勘探开发的几点认识

鄂尔多斯盆地中南部“定边-华池-富县”L形页岩气有利发育区,发育大套黑色页岩,有机质含量高、成熟度适中、构造破坏小。特别是富县探区除具有良好的生油条件外,还具有页岩气成藏条件,但其储集层物性差,孔隙度和渗透率极低,自然产能较低,开采难度大,页岩气的经济开采还处于探索起步阶段。针对目前中石化华北分公司在富县区块的工艺试验,在分析国外页岩气开发技术现状的基础上,提出了富县探区页岩气勘探开发的认识和建议。     

松江河石龙电站边坡加固工程施工技术

在松江河石龙电站边坡加固工程中,采用小直径抗滑桩加锚杆的桩锚联合支护体系,替代单纯的大直径抗滑桩,解决了陡峭边坡大型设备无法使用问题。采用潜孔锤跟管钻进工艺,解决了人工填石层钻孔坍塌及不能用水做循环介质的问题。介绍了该边坡治理方案及其施工技术,对陡峭边坡灾害治理工程有实用参考价值。     

φ75 mm双管单动采煤管在薄煤层及粉煤钻探中的应用

在邻水孔家山井田钻探施工中,由于施工区域煤层厚度不稳定,并且煤层主要以粉煤为主,前期技术准备不充分,造成煤层打丢打薄。通过对其原因的分析及采煤工具的选取和采煤工艺的摸索,引入Ф75 mm双管单动采煤管,并确定了一套简单易行的采煤工艺方法。应用表明,该钻具及工艺能够极大地提高煤样的采取率,防止煤层打薄打丢情况的发生。     

小秦岭深部探矿项目某标段钻探施工方法探讨

从钻孔护壁堵漏、钻孔结构、事故预防与处理措施等方面对小秦岭深部探矿项目某标段钻探施工方法进行了探索,特别是强护壁性能的冲洗液和多级大量套管技术的应用取得突破,基本解决了第四系、第三系加断层泥埋藏深度达600～800 m的厚覆盖层钻探施工难题,为该类地层施工提供了经验。     

浅谈全液压履带式水井钻机在水井施工中的应用

为了提高水文水井施工进度、降低施工成本、缩短水文水井施工周期。总结多年来施工水文水井的成功经验及不足,大胆引进新工艺一空气潜孔锤钻探技术及新设备-全液压履带式动力头DL-500型水并钻机、高风压空压机。在同样的钻进工艺下,通过使用DL-500型水井钻机及SPJ-300型水井钻机、XY-4型岩芯钻机施工水文水井的应用效果对比、分析,阐述了全液压履带式动力头DL-500型水井钻机的优越性。     

Geomorphology of carbonate platform‐marginal uppermost slopes: Insights from a Holocene analogue,Little Bahama Bank,Bahamas

As the product of a variety of sediment sources and sedimentation (and re‐sedimentation) and erosion processes, the geomorphology and sedimentology of carbonate slopes are highly variable. The purpose of this study is to describe sub‐bottom profiles and side‐scan sonar, multibeam and optical data acquired by an autonomous underwater vehicle to explore variability in geomorphological and sedimentological character of the present‐day platform‐marginal, uppermost slope environments (< 240 m water depth) on the north, open‐ocean facing flank of Little Bahama Bank, Bahamas. Although at time scales of greater than 100 ka this margin is progradational, the data illustrate a complex juxtaposition of erosional and depositional processes and features. Erosion is evidenced by two prominent escarpments (70 m and 120 m) that expose eroded, bedded rocky outcrops. These escarpments are interpreted to represent relict features, related to past sea‐level positions, although they still may be shedding debris. Aside from erosional remnants, sedimentation and active transport is indicated by several features, including active bedforms (especially above the 70 m escarpment, but ripples occur to depths of ca 200 m), several mass transport complexes that overlie and cover the lower escarpment, gravity flow deposits and rare slump features. Similarly, a thick (up to 20 m) onlapping sediment wedge, interpreted to be Holocene in age, suggests lateral accretion of the slope by more than 75 m in this period. Data illustrate that this open‐ocean margin is distinct from windward margins in the Bahamas, which typically include near‐vertical walls of erosion or bypass, flanked downdip by rubble and talus, and leeward margins, which have onlapping muddy wedges, but that lack marked terraces or escarpments. Collectively, the results provide perspectives into the nature and controls on complex geomorphological patterns of erosion and deposition in Holocene uppermost slope systems, concepts potentially applicable to ancient analogues.