安场页岩气井眼轨道优化与地质导向技术

随着安场向斜页岩气井开发的深入,对水平井组的井眼轨迹控制技术、井间井眼轨迹的防碰绕障、防碰分析、定向仪器工具的优选及地质导向技术均提出了更高的要求。为此,针对这些问题,从井眼轨迹控制技术方法、防碰绕障分析的方法、井眼轨迹控制技术和地质导向技术入手开展分析研究,形成了相关技术优化,为安场向斜页岩气井开发提供支撑。     

随钻方位伽马成像测井在鄂尔多斯盆地H井区水平井地质导向中的应用

随钻方位伽马成像测井是水平井地质导向技术的重要组成部分,与常规随钻伽马测井相比,方位伽马成像测井仪利用多个伽马探测器,将带有方位信息的测量数据上传到地面,精确指导井眼轨迹调整,确保维持在目的层的有利位置钻进.根据上下伽马曲线和成像图的8个响应特征将常见的水平井井眼轨迹与地层接触关系划分为简单模式和复合模式,简单模式细分...     

川渝地区复杂储层水平井地质导向技术

复杂储层条件下,尤其是在薄层、低孔渗、缝洞型等储层的油气勘探与开采是油田进入油气勘探开发后期的研究热点与难点。实践证明,水平井地质导向技术正是解决上述难题的有效手段之一。针对川渝地区复杂的地质对象,从复杂储层地质特点、地质导向难点入手,梳理了现场地质导向作业中常见的问题,并针对性地总结了技术对策,提出了针对此类储层在实际地质导向中要解决好的技术要点。以重庆气矿川东高陡复杂构造带云安XX井为例,综合运用测井、钻井、地质、地震等资料进行钻前设计、地质建模、实时导向,地质与工程紧密结合,提高了储层钻遇率,最终试油产气55×10⁴ m³/d,为该区域产量最高井,现场应用效果明显。     

元素录井技术在海陆过渡相页岩气水平井地质导向中的应用

河南省页岩气资源主要发育于上古生界海陆过渡相沉积中,海陆过渡相页岩气层系具有多岩性频繁互层、单层厚度小、纵向变化快的特点,加上局部地区微幅构造发育,使得水平井地质导向中小层识别和水平段钻头方向的判断难度很大。为此,利用研究区优质页岩气层段的X射线荧光元素录井数据,通过统计分析对目的层各小层进行精细刻画,首次提出利用Si、Al、Na、Fe、S、K、Mn和Ti元素含量的变化关系分别建立砂岩、煤岩和泥岩元素交会图版,并利用Ba、Ti、Ca、S和Sr元素组合与深度的关系建立随钻元素定量模型。根据元素交会图版进行目的层小层识别,为水平井入窗提供准确依据;在水平段利用随钻元素定量模型判断钻头穿行方向。该技术在通许隆起中部中深层页岩气水平井钻井过程中进行了现场应用,取得了较好的效果。     

水平井井眼轨迹地质导向技术析

水平井井眼轨迹的地质导向是其综合录井工作中的重点,它决定着水平井钻井工作的成败。本文结合中石化西南分公司在四川中江构造上第一口针对三叠系中统沙溪庙组“D层”砂体的水平井地质导向的成功经验,总结并提出水平井眼轨迹地质导向工作的一些基本方法,旨在为今后的水平井地质导向过程中起到一定的指导作用。     

地质导向钻井技术的现场应用

地质导向钻井是以井下实际地质特征来确定和控制井眼轨迹的钻井技术。使用这一技术,可以精确地控制井下钻具命中最佳地质目标。新疆油田MBHW04水平井是国内第一口使用地质导向钻井技术的井。重点介绍了地质导向钻井技术的具体步骤及其在新疆油田MBHW04井中的应用情况,包括自然伽马测井资料的解释和应用。应用地质导向钻井技术,该井获得良好的油藏开发效果。     

油田钻井的“杀手锏”—地质导向钻井技术

地质导向钻井技术的研发和应用,使石油企业既能拿储量和产量,又能提高钻井时率和降低勘探开发成本,具有广阔的发展前景和很高的实用价值,为低产、低压、低渗透薄油层和难采储层多的国内石油企业带来了新的希望。     

浅析大牛地气田水平井地质导向难点

从地质角度出发,分析了地质导向在水平井施工中的难点,结合录井现场地层对比、钻时、气测和岩性等第一手资料,发挥录井地质导向作用,较好地解决了这一难题。     

浅谈导向钻管道敷设技术在市政通信管道工程中的应用

本文简要介绍了导向钻技术的施工特点和施工过程,并分析了导向钻管道敷设技术在市政通信管道施工中的应用。     

地质导向钻井技术研究与应用

综合介绍了＂地质导向钻井工艺技术研究＂的部分研究成果,并利用初步形成的地质导向现场应用技术成功地实施了地质导向钻井,为薄油层、厚油层顶部剩余油等复杂油气藏开发提供了技术支撑,研究攻关阶段现场试验的25口井,应用效果良好。     

南海表面海温异常对南海季风影响的数值模拟

采用P-σ混合坐标系区域气候模式模拟了4－7月南海季风的爆发、演变过程，并进行了3组敏感性数值试验，研究南海表面海温异常对南海季风的影响，得到以下结论：（1）南海4月份海温异常对南海季风的爆发日期影响不大，但对季风爆发后的强度有所影响，异常增温造成南海季风增强，异常降温则南海季风减弱。（2）南海季风爆发和强度的变化与南海本身的海温变化情况有密切的关系，尤其是5月份南海海温异常。5月份南海异常增温可以使南海季风提前爆发，季风增强，南海海温异常降低时，南海季风爆发的时间推迟，季风减弱。（3）南海海温持续异常可以影响南海及中国大陆的高低空环流变化，海温持续异常增温可以使南海季风提前爆发，显地加强南海季风，并有利于南海季风向北推进，但当海温在6月份进一步持续增温时，则有利于季风维持在较南地区，阻碍季风向北发展；当海温持续异常降低时，南海季风推迟爆发，且明显减弱。     

Anthropogenic climate change revealed by coral gray values in the South China Sea

The authors analyze the coral growth band from a colony in the northwestern South China Sea. The coral growth band can provide comprehensive environmental information on climate. The trend from the two-century-long annual density of the coral is in a good agreement with that of the global CO2 concentration. Both trends were small prior to the end of the 19th century; after that, trends became clear, more so from the 1960s to the 1990s (the end of the coral record). The overall coral density shows a steady d...     

南海深海塑料垃圾污染

渔业捕捞及商业航运活动的塑料排放是南海深海塑料污染的主要来源。南海深海微塑料污染始于20世纪80年代,具有明显陆源输入的特征,陆架近岸区域微塑料污染严重。陆坡深海峡谷是塑料/微塑料向深海盆地输运的主要通道,近底浊流在输运中发挥了重要作用。综述了南海海底塑料垃圾深潜研究的最新进展,首次提出了深海塑料垃圾生态系统的概念。     

Heat exchange at air-sea interface in the South China Sea during monsoon periods in 1986

Air-sea interaction is achieved by air-sea interface flux exchange. Therefore, general attention has been paid to connective researches of the air-sea interface flux exchange and the burst of the summer monsoon in the South China Sea. Some preliminary res…     

Seasonal features of the Sverdrup circulation in the South China Sea

Based on the Sverdrup relation, using climatological wind stress data, the basin scale Sverdrup transport in the South China Sea(SCS) is calculated and the basic seasonal features of the Sverdrup circulation are obtained. A comparison of these calculated features with observations proves that the wind-driven circulation in the SCS is very important for the formation of the SCS upper oceanic circulation in winter, summer and fall. It is shown that the non-uniform sea surface wind is one of the causes to form multi circulation centers in the basin of the SCS. The westward current at 18°N is caused by the local wind, which is stronger in fall and winter. The seasonal variation of circulation in the southern SCS is much more remarkable than that in the north. The wind in spring is helpful to the seasonal reversal of the circulation in the central SCS. The northward transport of the cyclonic circulation reaches the maximum in fall.     

Upper pycnocline turbulence in the northern South China Sea

The first regional mapping of the averaged turbulent kinetic energy dissipation rate <εp> in the upper pycnocline of the northern South China Sea is presented and discussed.At φ=20°N and to the north of this latitude,<εp> appears to be more than two times larger than that to the south of 20°N.It is suggested that this asymmetry is associated with the predominant northwestward propagation and dissipation of the internal waves originated in the Luzon Strait area.An approximately linear relationship between <εp> and the available potential energy of the waves P IW,suggests a characteristic time of the P IW dissipation of about 6 h.     

南海深部过程的探索

2011—2018年,国家自然科学基金委员会设立"南海深部过程演变"重大研究计划,同时推动实施了三次半的大洋钻探航次,使南海进入国际深海研究的前列,在深海盆洋陆相互作用、边缘海盆地的板缘张裂和气候演变的低纬驱动等3方面取得了突破性进展,挑战了源自西欧、北大西洋的传统观念。深海探索的进展,确立了中国在南海科学上的引导地位,下一轮的深入研究可望将南海建成世界海洋科学的天然实验室,进一步提升中国在海洋基础研究中的国际地位。     

Simulation or meridional overturning in the upper layer of the South China Sea with an idealized bottom topography

The large-scale upper circulations and meridional overturning in the upper layer of the South China Sea (SCS) with idealized bottom topography in winter and summer are investigated. Simulations with the GFDL general circulation model are carried out under the conditions of open or enclosed boundary regarding transport in the Luzon Strait. The intrusion area of Kuroshio, its impact on the meridional overturning in the upper layer of the SCS and seasonal characteristic of this impact are explored, respectively. The model is forced by climatological wind stress and relaxed to monthly mean climatological temperature and salinity. The resultant meridional overturning is non-enclosed, wit htransporting from north to south in the surface and returning to north at the depth of about 500 m in winter, about 200 m in summer, with amplitudes of 10^5 m^3/s. It shows the transporting path of intermediate water of the SCS and offers an idealized reference for further study on dynamics of wind-driven and thermohaline circulation of the SCS.     

Simulation of meridional overturning in the upper layer of the South China Sea with an idealized bottom topography

The South China Sea (SCS) is the largest marginal sea in the northwestern Pacific. Several important water gateways exist around the SCS, such as Luzon Strait, Taiwan Strait, etc., that lie in the northeastern SCS, and others like Kalimantan Strait, Balawan Strait, etc., lie in the south. Luzon Strait connects the SCS and Pacific via the Philippine Sea, and its water exchange has significant impact on the interior circulations of the SCS[1]. Since direct observation data about the …