冲击反循环钻机在大漂石地层中的应用

文章通过对冲击反循环钻进和回转钻进两种施工方法的比较,指出在百色地区大漂石地层使用冲击反循环钻机的优势明显,而在穿越大漂石层后的泥页中扩底以提高桩基承载力时,可再改用回转钻机进行扩大施工比较理想。     

内插管式气举反循环钻进工艺在基岩地热井中的应用

随着地热资源被广泛利用,地热井各种钻井技术新方法不断应用,如何提高地热井施工效率、降低地热井施工成本是地热井项目钻探施工的关键。气举反循环钻进工艺被广泛应用于地热井钻探施工中,然而在基岩浅井和中深井地热项目施工中,使用常规气举反循环钻进工艺存在钻具重量大、结构复杂、双壁密封不严等问题,对钻机提升能力要求较高,中小型钻机难以满足,加大了施工成本。本研究在不改变常规中小型正循环施工钻探设备、钻具的条件下,提出了一种内插管式气举反循环钻进技术,并在沂南智胜汤泉1号基岩地热勘查井施工中进行了应用。试验表明:内插管式气举反循环技术施工工艺,可在无需更换原有钻探设备和钻具的基础上,通过加工部分钻具及部件,便可实现正反循环工艺之间的更换。更换后的气举反循环钻进工艺结构简单、钻具重量轻、双壁密封可靠、施工成本低,提高了设备利用率和钻进效率。在基岩浅井和中深井中,应推广应用内插管式气举反循环钻进工艺。     

贯通式气动潜孔锤反循环钻进初探

贯通式气动潜孔锤反循环钻进是以压缩空气作为碎岩动力和洗井介质，配用双壁钻杆，实现全孔反循环连续取芯（样）的钻进技术。本文在对反循环钻进机理分析的基础上，提出了反循环钻头的设计依据和原则，并依据野外生产试验资料，确定了贯通式气动潜孔锤反循环钻进的设备配套方案、钻进规程参数和工艺技术措施。     

大口径气举反循环钻具提效74%

正日前,由河南省煤田局承担的河南省国土资源厅科技攻关项目"大口径气举反循环钻具研制及应用研究"通过审查验收。项目研制了直径219.1/168.3毫米螺纹联接双壁钻杆、直径168.3毫米内平单壁钻杆、气举反循环水龙头、双壁主动钻杆及反循环钻头等配套器具,经生产性试验证明:该套组合钻具强度高、密封性能好、连接形式独特,可满足直径600毫米~1500毫米的大直径工程井气举反循环钻井施工,在同等技术条件下,比正循环钻进效     

河南省煤田地质局开创国内运用空气反循环动力造穴井先河

近日,河南省煤田地质局二队在黑龙江鹤岗地区,首次运用国际最先进的空气反循环动力造穴工艺打出了一口日排量1400余立方米的煤层气生产试验井。该井的成功施工,填补了国内煤层气空气反循环动力造穴完井的空白。     

晋建文 一片丹心励后人

一把大牙钳,走南闯北;一颗赤诚心,情系地勘。他多次被评为河南省煤田地质局二队及洛阳市的"先进生产者"。已退休十多年,仍一片丹心励后人,他就是不计得失的"拼命三郎"——河南省煤田地质局二队202钻机原机长晋建文。科学施工冲在前晋建文1959年被分配到钻机当钻工,他刻苦学习钻探知识,遇到困难时总是冲锋在前。由于表现突出,1974年他被任命为202钻机的机长。1982年,202钻机在洛阳新安县云顶地区承揽施工6个     

对反循环钻进翼状钻头的分析及改进

反循环钻进与正循环钻进的冲洗液流向不同,同时反循环钻进孔径一般比正循环钻进的孔径大,反循环钻进仍沿用正循环钻进用的开放式翼状钻头,由于孔内冲洗液中心流速高,边沿流速低,孔底边沿排岩屑不畅,特别是在粘土地层钻进常引起糊钻,致使钻进效率受到极大的影响。把钻头的翼板顶部改成封闭(即挡水罩)式,使冲洗液先流到钻头边沿再到中心钻杆,这样孔底排屑较彻底;另外把钻头底唇改成收敛式的(即倒漏斗状),使岩屑翻起的方向与水流方向一致,加强钻头的排岩能力,阻止粘土滞留及粘结钻头的可能性,保持孔底清洁,从而提高了反循环的钻进效率。     

晋建文一片丹心励后人

一把大牙钳,走南闯北;一颗赤诚心,情系地勘。他多次被评为河南省煤田地质局二队及洛阳市的“先进生产者”。已退休十多年,仍一片丹心励后人,他就是不计得失的“拼命三郎”--河南省煤田地质局二队202钻机原机长晋建文。
　　科学施工冲在前
　　晋建文1959年被分配到钻机当钻工,他刻苦学习钻探知识,遇到困难时总是冲锋在前。由于表现突出,1974年他被任命为202钻机的机长。     

论气动潜孔锤钻进在卡斯特灰岩地层使用的适应性

气功潜孔锤钻进是当前钻孔硬岩钻进效率较高的方法之一;对于卡斯特灰岩地层、用正循环气动潜孔锤钻进是不适应的,用CSR堵隔式反循环双管气动潜孔锤钻进或CSR堵隔式双管贯通式反循环气动潜孔锤钻进比较合适:在卡斯特灰岩地层.在水文水井中,气动潜孔锤钻进仍可发挥它高效率、高速度的作用。     

我省钻探进尺效率提高近三成

<正>5月8日,河南省煤田地质局地质三队完成的"大直径工程井气举反循环钻井工艺研究"项目顺利通过专家组的评审验收,钻探进尺效率提高近三成,达到国内领先水平。"大直径工程井气举反循环钻井工艺研究"项目是2013年度省国土资源厅"两权价款"地质科研补助项目。项目通过对岩屑粒径、临界上返速度与最小冲洗量间关系,影响气举反循环排渣能力主要技术参数的分析研究,提出了合理的钻进及扩孔参数(钻压、转速、风压、风量、浸没比),保证了     

Modeling the ocean circulation in the Bering Sea

With parameterized wave mixing, the circulation and the tidal current in the Bering Sea were simulated simultaneously using the three-dimensional Princeton Ocean Model. The simulated circulation pattern in the deep basin is relatively stable, cyclonic, and has little seasonal change. The Bering Slope Current between 200-1000 m isobaths was estimated to be 5 Sv in volume transport. The Kamchatka Current was estimated to be 20 Sv off the Kamchatka Peninsula. The Bering shelf circulations vary with season, driven mainly by wind. These features are consistent with historical esti- mates. A counter current was captured flowing southeastward approximately along the 200 m isobath of the Bering Slope, opposite to the northwestward Bering Slope Current, which needs to be validated by observations. An upwelling current is located in the shelf break （ 120-1000 m） area, which may imply the vertical advection of nutrients for supporting the Bering Sea Green Belt seasonal plankton blooms in the breakslope area. The Bering Slope Current is located in a downwelling area.     

六个顺序脉冲发生器的设计——顺序脉冲宽度是时钟脉冲周期的四倍

本文是关于采用三个TTL D触发器和六个译码器来组成扭形计数器的设计。但是在讨论扭环形计数器之前,要用2个TTL D触发器来组成一个异步计数器,这样处理可以避免在译码时产生的竞争冒险。     

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Preliminary study on the formation mechanism of counter western boundary undercurrents below the thermocline—A conceptual model

Based on a simple conceptual model of stratified ocean, the criterion of the geostrophic velocity inversion in and below the thermocline was derived ash′·ν′<0 and {ie1-1}, meaning that the slopes of the thermocline (h′) and the sea {ie1-2} must be opposite to each other, and thath′ must be strong enough to satisfy the latter inequality. The criterion was applied to discuss the features of the western boundary undercurrents, the counter undercurrents of the western boundary currents below the thermocline, and to discuss the dynamics of their formation finally resulting from the combination of the basin-scale circulation and local geostrophic balance. The formation mechanism, multicore structure, and transport variations of the Mindanao Undercurrent and those of other undercurrents, such as the North Equatorial Undercurrent and the Kuroshio undercurrent, can be satisfactorily explained by the above results. Research supported by the Postdoctoral Research Foundation and the NSFC (No. 49176255 and 49706066). Contribution No. 3405 from the Institute of Oceanology, Chinese Academy of Sciences.     

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NUMERICAL STUDY ON THE FORMATION OF THE SOUTH CHINA SEA WARM CURRENT Ⅱ. BAROCLINIC CASE

In this part, Levitus‘ climatological temperature and salinity are incorporated in the numerical model developed in Part I. Diagnostic and prognostic experiment on the thermohaline circulation were conducted. The smooth Levitus‘ data do not include any information on the South China Sea Warm Current (SCSWC), so it is not in the model-produced diagnostic thermohaline circulation. Although the SCSWC does not appear in the wind-driven circulation in the barotropic case, it appears in the prognostic wind-driven circulation in the baroclinic case. This implies that the differing circulation pat-terns between barotropic case and bareclinic case are due to the stratification. The prognostic thermohaline circulation with wind stress and inflow/outflow transports at open boundaries are also discussed. Coupling of density and dynamic forces makes the circulation pattern more complicated, Even though the stratification is not always a direct cause of the formation of the SCSWC, it is at least an indirect cause.     

Development of a High-Resolution Coastal Circulation Model for the Ocean Observatory in Lunenburg Bay

An advanced ocean observatory has been established in Lunenburg Bay of Nova Scotia, Canada as part of an interdisciplinary research project of marine environmental prediction. The development of a high-resolution coastal circulation model is one of important components of the observatory. The model horizontal resolution is 60m and the vertical resolution is about 1 m. The coastal circulation model is used to simulate the semi-diurnal tidal circulation and associated nonlinear dynamics with the M2 forcing specified at the model open boundaries. The model is also used to simulate the storm-induced circulation in the bay during Hurricane Juan in September 2003, with the model forcing to be the combination of tides and remotely generated waves specified at the model open boundaries and wind stress applied at the sea surface. The model results demonstrate strong interactions between the local wind stress, tidal forcing, and remotely generated waves during this period. Comparison of model results with the surface elevation and current observations demonstrates that the coastal circulation model has reasonable skills in simulating the tidal and storm-induced circulation in the bay.     

汶川Ms8.0地震前后青藏块体东北缘的垂直形变

利用区域水准、跨断裂水准资料,分析了2008年汶川8.0级地震前后青藏块体东北缘地壳垂直形变。结果表明：震前近10年,垂直形变具有明显的区域性和差异化特征。其中,祁连 河西地区垂直形变主要反映祁连山下沉、河西走廊相对抬升的逆继承性运动;西吉、海原、固原地区构造运动相对平稳;兰州、天水、漳县 武都以西的岷山隆起抬升速率明显增大并伴有形变高梯度带。这主要反映了震前青藏高原北向推挤作用相对减弱,东向挤压作用明显增强;震后,2008年8—10月的观测显示,垂直形变出现反向大幅变化;2006—2008年岷山隆起区相对临夏呈现逆继承性的快速下沉,反映由于地震的发生,导致青藏高原东向挤压运动减弱;2010年的监测表明,垂直形变幅度减小,2008—2010年合作相对临夏仍呈现反向下沉,但差异运动明显减弱,显示当前包括岷山隆起在内的区域构造活动已基本趋于稳定。     

Optimization of reverse circulation bit based on field experiment

By field experiment in Sandaozhuang W-Mo mining area in Luanchuan of Henan Province, the authors analyzed the Experimental result of reverse circulation bit on the basis of different structures and obtained the following conclusion: the design parameter of reverse circulation bit, the number, diameter and angle of the spurt hole can influence on the reverse circulation effect. The bit with inner spurt hole is better obviously than that one without inner spurt hole in reverse circulation, one or two right and the best choice of inner spurt hole is that the diameter is Φ8, the angle is 30° dip up and the suitable number is two to three.