超深水钻井作业隔水管顶张力确定方法   总被引：2，自引：0，他引：2  

鞠少栋  畅元江  陈国明  许亮斌  殷志明 《海洋工程》2011,29(1)

对于深水和超深水钻井作业,确定钻井隔水管系统顶张力是钻前设计非常重要的工作。研究三种隔水管系统顶张力确定方法,分别是理论方法、基于隔水管系统底部残余张力方法和基于下放隔水管系统的最大钩载方法。算例计算与超深水钻井实践对比表明,在相同的隔水管系统配置下,三种方法计算结果都接近于实际钻井作业时的顶张力设定值。但研究认为,基于下放最大钩载的顶张力计算方法简单实用,推荐作为优选方法。  相似文献   

煤田地质超深孔钻探工艺     

孙贵生  张纯峰 《中国煤炭地质》2015,(1):57-61

在对深部煤田地质钻孔钻进工艺研究的基础上,有针对性选择使用聚合物泥浆,解决了基浆配制用水及泥浆抗地表水水质污染问题。通过改变双管钻具长度和改换取心钻头的切削具,满足软硬互层对钻头钻进效率的影响。在煤系地层钻进中,除采用常规的单管钻具钻进外,在见煤预告下过后,采用加长双管取心钻具,既可保证了回次进尺,又可保证岩心的采取。多项措施落实,不仅解决了生产中的一些难题,收到了较好的效果,而且创造了河北省煤田地质局煤田地质单孔钻探深度2 009.12m的新纪录,为今后深部钻孔的施工积累了经验。  相似文献   

http://www.sciencedirect.com/science/article/pii/S167498711300162X     

Fumiko Tajima  Masaki Yoshida  Eiji Ohtani 《地学前缘(英文版)》2015,6(1):79-93

Seismic observations have shown structural variation near the base of the mantle transition zone(MTZ)where subducted cold slabs,as visualized with high seismic speed anomalies(HSSAs),flatten to form stagnant slabs or sink further into the lower mantle.The different slab behaviors were also accompanied by variation of the "660 km" discontinuity depths and low viscosity layers(LVLs) beneath the MTZ that are suggested by geoid inversion studies.We address that deep water transport by subducted slabs and dehydration from hydrous slabs could affect the physical properties of mantle minerals and govern slab dynamics.A systematic series of three-dimensional numerical simulation has been conducted to examine the effects of viscosity reduction or contrast between slab materials on slab behaviors near the base of the MTZ.We found that the viscosity reduction of subducted crustal material leads to a separation of crustal material from the slab main body and its transient stagnation in the MTZ.The once trapped crustal materials in the MTZ eventually sink into the lower mantle within 20-30 My from the start of the plate subduction.The results suggest crustal material recycle in the whole mantle that is consistent with evidence from mantle geochemistry as opposed to a two-layer mantle convection model.Because of the smaller capacity of water content in lower mantle minerals than in MTZ minerals,dehydration should occur at the phase transformation depth,~660 km.The variation of the discontinuity depths and highly localized low seismic speed anomaly(LSSA) zones observed from seismic P waveforms in a relatively high frequency band(~1 Hz) support the hypothesis of dehydration from hydrous slabs at the phase boundary.The LSSAs which correspond to dehydration induced fluids are likely to be very local,given very small hydrogen(H~+) diffusivity associated with subducted slabs.The image of such local LSSA zones embedded in HSSAs may not be necessarily captured in tomography studies.The high electrical conductivity in the MTZ beneath the northwestern Pacific subduction zone does not necessarily require a broad range of high water content homogeneously.  相似文献   

Sound level produced during rock drilling vis-à-vis rock properties     

B. Rajesh Kumar  Harsha Vardhan  M. Govindaraj 《Engineering Geology》2011,(4):333

The process of drilling, in general, always produces sound. Though sound is used as a diagnostic tool in mechanical industry, its application in predicting rock property is not much explored. In this study, an attempt has been made to estimate rock properties such as uniaxial compressive strength, Schmidt rebound number and Young's modulus using sound level produced during rotary drilling. For this purpose, a computer numerical controlled vertical milling centre was used for drilling holes with drill bit diameters ranging from 6 to 20 mm with a shank length of 40 mm. Fourteen different rock types were tested. The study was carried out to develop the empirical relations using multiple regression analysis between sound level produced during drilling and rock properties considering the effects of drill bit diameter, drill bit speed and drill bit penetration rate. The F-test was used to check the validity of the developed models. The measured rock property values and the values calculated from the developed regression model are fairly close, indicating that the developed models could be efficiently used with acceptable accuracy in prediction of rock properties.  相似文献   

北大别的高温超高压变质作用与多阶段折返     

刘贻灿  古晓锋  邓亮鹏 《岩石学报》2011,27(2):589-600

近期的变质岩石学、地球化学及同位素年代学研究表明,北大别整体经历了高温超高压变质作用和多阶段折返历史,因而表现为广泛发育的多期减压结构和极少保留早期的超高压变质记录。北大别榴辉岩以高温变质作用以及折返期间因麻粒岩相和角闪岩相退变质变质作用而形成的多期后成合晶为显著特征。石榴子石中伴有放射状胀裂纹的单晶和多晶石英包体指示早期柯石英的转变结果,这已被锆石中发现的柯石英残晶所证实。结合北大别北部榴辉岩和片麻岩中发现的金刚石等超高压证据以及三叠纪变质记录,由此证明北大别整体经历过深俯冲和印支期超高压变质作用。北大别榴辉岩的多阶段高温条件主要来自石榴子石-绿辉石矿物对温度计、单斜辉石中紫苏辉石+石英针状矿物出熔体以及金红石中较高的Zr含量和变质锆石中较高的Ti含量等得出的温度证据。此外,多期后成合晶以及石榴子石和单斜辉石等矿物中成分分带的存在,证明该区榴辉岩经历了一个多阶段、快速折返过程;而不同变质阶段的温度、压力和形成时代,却反映该区榴辉岩经历了长时间的高温变质演化与缓慢冷却过程。长时间的高温变质作用与缓慢冷却过程也许正是北大别长期难以发现柯石英和有关超高压记录的重要原因。因此,这些成果为大别山三个不同超高压岩片的差异折返模型的建立提供了新的证据。  相似文献   

创新科技，强化能力，精益管理，努力建设一流钻探队伍——中核地质钻探“十一五”工作回顾及“十二五”工作设想          下载免费PDF全文

姜德英  李成城 《探矿工程》2011,38(1):15-17

从钻探生产、钻探科研、钻探工程管理、钻探能力建设以及钻探队伍建设等方面对中核地质钻探在＂十一五＂期间所取得的成绩和进展作了全面的回顾总结,提出了＂加强人才建设、推进科技创新、加强能力建设、推行精益管理＂的＂十二五＂工作设想。  相似文献   

H020U井钻进所遇问题及处理方法          下载免费PDF全文

张新刚  隆东  向军文  林修阔 《探矿工程》2011,38(1):28-31

土耳其贝帕扎里天然碱矿H020U井在造斜钻进和水平钻进过程中遇到井漏、钻头钻遇硅化灰岩层磨损严重、未绕过第一靶点V020而打中套管、井涌、仪器掉入裸眼、钻遇未知溶腔导致顶角下降,方位偏离而导致未直接连通第二靶点等问题。针对这些问题进行了分析,并提出了相应的处理方法,最后成功地使H020U井连通第一靶点V020井和第二靶点V020U井。  相似文献   

大口径取心工艺在刚果(金)某矿区的应用          下载免费PDF全文

李慧芳 《探矿工程》2011,38(9):46-48

为了满足选冶试验矿样质量的需要,刚果（金）Sicomines铜钴矿区选用了大口径取心（≥Φ325 mm）钻探工艺。实际应用表明,针对完整或破碎地层条件选用不同的筒状钻具及取心工艺是大口径取心工程成功的关键。  相似文献   

梧桐庄矿新增大口径3号排水孔施工技术          下载免费PDF全文

郭再峰 《探矿工程》2011,38(9):83-85

介绍了梧桐庄矿大口径排水孔钻探成井、固井施工技术。该孔设计孔深646 m,终孔直径520 mm,落点坐标水平位移≯5 m,下入重达90余吨的Φ426 mm套管646 m,水泥固井。由于钻孔直径大,垂直度要求高,施工难度大,预防钻孔超斜、确保顺利安全下入Φ426 mm套管并固井是关键。通过采用小口径先导孔钻进再扩孔成井的施工方法,并采取合理的钻具组合和泥浆,制定有效的防斜技术和下套管措施等,顺利完成了施工任务,施工质量满足设计要求。  相似文献   

地层温度对科学超深井井壁稳定的影响          下载免费PDF全文

张培丰 《探矿工程》2011,38(10):1-5

井壁稳定问题包括井壁坍塌和地层破裂2种基本类型,科学超深井钻探的目的层是处于高地应力、高地温和高地层压力的深部岩层,井壁稳定问题更加突出。以12000 m科学超深井为例,从地层温度入手,分析钻井液循环温度变化所引起的当量静态钻井液密度和环空压力当量密度的变化,以及温梯应力、温差应力对井壁稳定的影响。  相似文献