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1.
赵华宣  李强  陈涛  陈浩  苏宁  王虎 《探矿工程》2017,44(2):37-42
研究了空气潜孔锤钻井工艺在贵州省碳酸盐岩地层地热深井中的应用,涉及溶隙、裂隙发育,涌水、漏风、掉块、排渣困难等情况频发的碳酸盐岩地层的10~1100 m井段和φ216~406 mm井径的条件,探讨了在这样环境下空气潜孔锤钻进机具设备配置、钻具组合和钻进参数;分析了空气潜孔锤钻进工艺钻进过程中的常见问题并提出了相应的技术措施;总结了深井碳酸盐岩地层复杂井况的空气潜孔锤钻进效率与经济效益。研究结果表明,通过合理的设备机具配置和技术措施,可有效提高贵州省碳酸岩层空气潜孔锤钻进效率,进而大幅度提高贵州地热深井的钻进效率和经济效益。  相似文献   

2.
空气潜孔锤钻进技术不仅可以提高钻探效率,而且不损害地热储层,因此在地热井中的应用十分广泛,但是仍受到钻探深度和出水量的限制。在湖南永州舜皇山基岩地热深井钻探过程中,常规牙轮钻进与泥浆钻进工艺存在钻进效率低、堵塞储层、影响出水量的可能。应用空气潜孔锤钻进技术实现了钻探深度的突破,钻探深度达到1820 m,实际出水量400 m3/d,出水温度43 ℃,符合设计指标。本文总结了相应的钻进工艺措施,以期促进对该技术在地热深井中的推广应用。  相似文献   

3.
贵州碎屑岩层地热深井空气潜孔锤钻进技术应用研究   总被引:6,自引:0,他引:6  
赵华宣 《地质与勘探》2016,52(5):942-949
本文研究了空气潜孔锤钻井技术在贵州省复杂碎屑岩层地热深井中的应用,涉及结构复杂、软硬互层、软弱夹层多及强水敏性泥页岩地层的56~1029m井段和Φ216~Φ315mm井径的条件,探讨了在这样环境下空气潜孔锤钻进设备机具配置组合、钻进参数;分析了深井碎屑岩层复杂井况的空气潜孔锤钻进效率。结果表明,该设备钻速是牙轮钻进的12.4~35倍,综合成本为198.73~693.93元/米,比牙轮钻进850~950元/米低得多。从复杂碎屑岩的结构特征和空气潜孔锤钻进特性,剖析了钻进中常遇问题的原因,并总结了相应的钻进技术和工艺措施。研究结果表明,合理设备机具的组合配置和钻进工艺措施能有效提高复杂碎屑岩层条件下空气潜孔锤钻进施工效率。  相似文献   

4.
贵州省复杂地层地热深井钻探工艺   总被引:9,自引:0,他引:9  
宋继伟 《地质与勘探》2018,54(5):1024-1037
贵州省地矿局组织实施了“贵州省地热深井钻探技术攻关”项目,研究了喀斯特地区复杂地层情况下地热深井钻探中螺杆钻井工艺和空气钻井工艺的适应性,攻克了两种工艺在该地区应用受地层特性限制的相关技术难题。螺杆马达平均寿命达到200小时以上,螺杆钻井工艺较常规钻井工艺钻进机械钻速提高2~3倍;空气潜孔锤单井应用深度超过1500m,空气潜孔锤钻井工艺较常规钻井工艺机械钻速提高10~29.5倍。同时研究了单井多工艺转换接力钻进技术,以及与上述工艺配套使用的钻井液体系。最终形成了一套适合贵州省地质条件地热深井钻探施工并能显著提高钻井效率和经济效益的组合工艺技术体系。该成果能将1口2000m以上地热深井施工周期由原来的8~12个月缩短至4~6个月,将单井平均施工成本由450万元降低至410万元以下。  相似文献   

5.
干热岩试验性开发井钻井施工,在高温硬岩的地层条件下,如何实现高效钻进仍存在很多技术难点。空气潜孔锤钻进技术是解决硬岩地层钻进的有效方法之一,潜孔锤钻头是空气潜孔锤钻进的关键器具。根据青海共和干热岩GH-01井空气潜孔锤钻进技术应用情况,分析探讨了空气潜孔锤钻头断齿、掉齿、磨损严重、使用寿命短等问题,从钻头结构设计、钻头材料选取、钻头冷压固齿工艺等几个方面对空气潜孔锤钻头进行了优化。固齿优化过程中采用有限元分析方法,对钻头冷压固齿过盈量进行仿真分析计算,根据分析计算结果确定最优固齿过盈量。通过对潜孔锤钻头结构、材料、加工等优化,为适用于高温硬岩的空气潜孔锤钻头研制提供了借鉴。为提高空气潜孔锤钻进综合效率,为干热岩钻探开发提供了技术支持和技术储备。  相似文献   

6.
近年来,大直径工程井被广泛应用于煤矿瓦斯抽采、输冰降温、强排水、通风送料等,其施工工艺主要有正循环气动潜孔锤钻井技术和反循环气动潜孔锤钻井技术;前者需要风量大,成本高,后者需要配置全套专用机具,实施难度大。为对现有空气潜孔锤钻井技术进行优化,以王台铺矿大直径抽排水井为例,对单体大直径空气潜孔锤钻井工艺进行研究,单体大直径潜孔锤+跟管钻进技术,解决大直径工程井施工效率低、深度浅、技术装备不完善、施工成本高等难题,可为国内同类型井施工提供借鉴。  相似文献   

7.
2011援鲁抗旱找水打井施工中使用了空气潜孔锤钻进技术,我单位历时41天,成井16口,打井深度均为100 ~ 200米深井,总进尺2981.5m.总出水量为4704m3/d,单孔最深孔深201.7米,终孔孔径在Φ180mm~Φ254mm,可满足居民15647人、牲畜7940头用水,同时可灌溉面积为4200亩.本文通过从空气潜孔锤钻进方面介绍了空气潜孔锤钻进技术及在干旱缺水地区钻探施工的一些实践经验.  相似文献   

8.
详细介绍了在铝土矿区进行空气潜孔锤钻进技术的应用试验。试验结果表明:该技术与普通双管钻进技术相比平均时效提高5.1倍,最高时效可达15.33 m。通过试验得出了几点认识,为在铝土矿区进一步推广应用空气潜孔锤钻进技术积累了实践经验。  相似文献   

9.
分析了清洁、可再生能源干热岩的地质特征以及进行钻井施工可能会遇到的环境温度高、钻井深度大等技术难点,并依据此对液动潜孔锤钻进技术应用于该领域进行了分析。按照目前的技术水平和施工能力,提出干热岩钻井分两步走的思路,目前液动潜孔锤所能达到的指标应用于第一步(井深3000~6000 m,温度150~350 ℃)钻井实践已经基本具备,并对液动潜孔锤需要完善的关键技术提出解决的方案。  相似文献   

10.
空气潜孔锤在松散地层中的钻进试验   总被引:1,自引:0,他引:1       下载免费PDF全文
空气潜孔锤钻探工艺在基岩地区已是首选的一种技术。传统观念认为空气潜孔锤钻进工艺适用于坚硬岩石(硬、脆、碎地层),在松散地层中则需要常规泥浆回转钻进或冲击钻进。通过典型松散地层的试验证明:空气潜孔锤在松散覆盖地层中可以实现正常的钻进,并且具有效率高、成本低、劳动强度小等优点,在粘土和潮湿粘土地层中钻进效率最高可达87和72 m/h。为解决页岩气、地热、煤层气、地下水等能源资源勘探时上覆地层的开孔或一开钻进提供了行之有效的方法,同时,也解决了缺水地区或严重漏失地层钻井液用水困难和传统开孔或一开泥浆回转钻探工艺复杂等问题。  相似文献   

11.
Lithostratigraphy, physicochemical stratigraphy, biostratigraphy, and geochronology of the 77–70 Ma old series bracketing the Campanian–Maastrichtian boundary have been investigated by 70 experts. For the first time, direct relationships between macro- and microfossils have been established, as well as direct and indirect relationships between chemo-physical and biostratigraphical tools. A combination of criteria for selecting the boundary level, duration estimates, uncertainties on durations and on the location of biohorizons have been considered; new chronostratigraphic units are proposed. The geological site at Tercis is accepted by the Commission on Stratigraphy as the international reference for the stratigraphy of the studied interval. To cite this article: G.S. Odin, C. R. Geoscience 334 (2002) 409–414.  相似文献   

12.
Well investigated platforms have been selected in each continent, and the history of Cretaceous transgressions and regressions there is concisely reviewed from the available evidence. The factual records have been summarized into a diagram and the timing of the events correlated between distant as well as adjoining areas.On a global scale, major transgressions were stepwise enlarged in space and time from the Neocomian, via Aptian-Albian, to the Late Cretaceous, and the post-Cretaceous regression was very remarkable. Minor cycles of transgression-regression were not always synchronous between different areas. Some of them were, however, nearly synchronous between the areas facing the same ocean.Tectono-eustasy may have been the main cause of the phenomena of transgression-regression, but certain kinds of other tectonic movements which affected even the so-called stable platforms were also responsible for the phenomena. The combined effects of various causes may have been unusual in the Cretaceous, since it was a period of global tectonic activity. The slowing down of this activity followed by readjustments may have been the cause of the global regression at the end of the Cretaceous.  相似文献   

13.
The Afyon stratovolcano exhibits lamprophyric rocks, emplaced as hydrovolcanic products, aphanitic lava flows and dyke intrusions, during the final stages of volcanic activity. Most of the Afyon volcanics belong to the silica-saturated alkaline suite, as potassic trachyandesites and trachytes, while the products of the latest activity are lamproitic lamprophyres (jumillite, orendite, verite, fitztroyite) and alkaline lamprophyres (campto-sannaite, sannaite, hyalo-monchiquite, analcime–monchiquite). Afyon lamprophyres exhibit LILE and Zr enrichments, related to mantle metasomatism.  相似文献   

14.
正20140751 Guo Xincheng(Geological Party,BGMRED of Xinjiang,Changji 831100,China);Zheng Yuzhuang Determination and Geological Significance of the Mesoarchean Craton in Western Kunlun Mountains,Xinjiang,China(Geological Review,ISSN0371-5736,CN11-1952/P,59(3),2013,p.401-412,8  相似文献   

15.
正20141058 Chen Ling(Key Laboratory of Mathematical Geology of Sichuan Province,Chengdu University of Technology,Chengdu610059,China);Guo Ke Study of Geochemical Ore-Forming Anomaly Identification Based on the Theory of Blind Source Separation(Geosci-  相似文献   

16.
SEISMIC GEOLOGY     
正20141334 Chen Kun(Institute of Geophysics,China Earthquake Administration,Beijing100081,China);Yu Yanxiang Shakemap of Peak Ground Acceleration with Bias Correction for the Lushan,Sichuan Earthquake on April20,2013(Seismology and Geology,ISSN0253-4967,CN11-2192/P,35(3),2013,p.627-633,2 illus.,1 table,9 refs.)Key words:great earthquakes,Sichuan Province  相似文献   

17.
正20141624 Cai Xiongfei(Key Laboratory of Geobiology and Environmental Geology,Ministry of Education,China University of Geosciences,Wuhan 430074,China);Yang Jie A Restudy of the Upper Sinian Zhengmuguan and Tuerkeng Formations in the Helan Mountains(Journal of Stratigraphy,ISSN0253-4959CN32-1187/P,37(3),2013,p.377-386,5 illus.,2 tables,10 refs.)  相似文献   

18.
PALEONTOLOGY     
正20142263Lü Shaojun(Geological Survey of Jiangxi Province,Nanchang 330030,China)Early-Middle Permian Biostratigraphical Characteristics in Qiangduo Area,Tibet(Resources SurveyEnvironment,ISSN1671-4814,CN32-1640/N,34(4),2013,p.221-227,2illus.,2tables,22refs.)Key words:biostratigraphy,Lower Permian,Middle Permian,Tibet  相似文献   

19.
正20142560Hu Hongxia(Regional Geological and Mineral Resources Survey of Jilin Province,Changchun 130022,China);Dai Lixia Application of GIS Map Projection Transformation in Geological Work(Jilin Geology,ISSN1001-2427,CN22-1099/P,32(4),2013,p.160-163,4illus.,2refs.)  相似文献   

20.
GEOCHEMISTRY     
正20140692 Duo Tianhui(No.402 Geological Team,Exploration of Geology and Mineral Resources of Sichuan Authority,Chengdu611730,China);Wang Yongli Computer Simulation of Neptunium Existing Forms in the Groundwater(Computing Techniques for Geophysical and Geochemical Exploration,ISSN1001-1749,CN51-1242/P,35(3),  相似文献   

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