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介绍了SYZX75型绳索取心液动锤在甘肃省肃北县德勒诺尔铁矿区坚硬、破碎地层中的应用情况,总结了该钻具在斜孔施工中的经验。实践表明,使用SYZX75型绳索取心液动锤,大幅度提高了回次进尺和钻进效率;有效克服了破碎地层的岩心堵塞,提高了破碎地层岩心采取率;有助于斜孔施工中的孔斜度控制。 相似文献
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SYZX75绳索取心液动锤在破碎地层中的应用 总被引：4，自引：0，他引：4
SYZX75绳索取心液动锤钻具由双喷嘴复合式液动潜孔锤与绳索取心钻具结合而成。为解决绳索取心在极破碎岩层钻进中的岩心堵塞,从而造成频繁打捞问题,湖北煤炭地质局在宜昌董家堡磷矿勘探区进行了SYZX75绳索取心液动锤钻进的试验应用。为了使试验数据具有对比性,采取了在一个孔内相近地层进行对比试验,从试验所得数据来看,绳索取心液动锤钻进工艺与普通绳索取心工艺相比,平均回次进尺提高了40.5%,平均每日进尺提高了48.1%。据此认为该项技术可在破碎岩层的勘探区中推广应用。 相似文献
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小秦岭金矿田南、北矿带深部找矿钻探施工中,应用SYZX绳索取心液动锤钻进技术,对深孔钻进采取防斜保直钻进,为钻孔的顺利延伸创造了条件,在硬碎地层中钻进,提高回次进尺,提高小时效率,延长钻头寿命,体现出了液动锤技术的优越性,并对液动锤使用中易出现的问题进行了总结。 相似文献
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攀西钒钛磁铁矿区深部及外围普查项目实施中,在破碎、坚硬、打滑地层钻进及大断层、断层破碎带穿越,使用普通绳索取心钻进,施工周期、效率、效益都受到严重影响。项目组尝试多种新型钻进技术工艺及技术关键,2013年优选国土资源部勘探技术研究所研制的SYZX96和SYZX75绳索取心式液动锤,集绳索取芯与液动冲击回转钻进为一体,在坚硬"打滑"地层和破碎地层中具有钻进效率高、钻孔质量好、岩芯采取率高、钻探成本低,钻进技术工艺等方面取得了突破性进展,达到了预期目的,值得推广。 相似文献
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在中国岩金勘查第一深钻ZK96—5钻孔的深部施工中,应用绳索取心液动锤技术在破碎复杂地层中钻进,增加回次进尺,提高时效,延长钻头寿命;在比较完整地层中提高钻速,减少辅助时间,体现了绳索取心液动锤技术的优越性,目前3911．34m的使用深度创造了绳索取心液动锤适应孔深的最新记录。对绳索取心液动锤在深部钻进的优势和易出现的问题进行了分析总结。 相似文献
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曹家口金矿位于甘肃省山丹县大马营乡。2015年宁夏核工业地质勘查院2台全液压动力头钻机在该矿区施工,因地层破碎、坍塌、漏失严重等情况,曾报废4个钻孔。为了提高施工效率和施工质量,采用SYZX96型绳索取心液动潜孔锤,为确保液动潜孔锤能发挥最佳使用效果,对配套冲洗液类型进行了评价研究,并进行了现场应用。应用结果表明,回次进尺平均提高68%,全孔岩心采取率达到95.5%以上,台月效率平均提高21%,没有发生孔内事故,降低了钻探成本,提高了施工质量和施工效率。 相似文献
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针对内蒙古兴和县曹四夭钼矿区构造发育,地层坚硬、岩心破碎,以及钻孔缩径、漏失、坍塌、掉块等复杂情况,总结了该矿区“硬、脆、碎”复杂地层绳索取心深孔钻探施工技术经验,从钻孔结构、泥浆配置和冲洗液选取以及钻探设备、新型SYZX75 2（77）型绳索取心液动锤钻具等方面采取措施,解决了破碎漏失、坍塌掉块及坚硬“打滑”地层的难题。着重阐述了高强度快失水堵漏技术试验,改善了复杂地层的深孔钻进环境,提高了钻探生产效率,保证了钻孔的安全终孔。 相似文献
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考虑核电厂地基-基础的动力相互作用,应用显式动力有限差分法分析了地震作用下极软岩、较软岩、坚硬岩上核电厂建筑结构基础的地震响应特征,比较了岩石坚硬程度对基础加速度反应谱的影响。研究表明：随着岩石坚硬程度的提高,核电厂建筑物结构基础的地震响应有增加的趋势;在周期轴上,基础处的加速度反应谱曲线会随着岩石坚硬程度的提高逐渐向短周期（高频段）方向移动。在高频段,建造于较坚硬岩石上基础结构的加速度反应谱值偏大;在中等频段,建造于较软岩石上基础结构的加速度反应谱值偏大;在低频段,岩石坚硬程度对加速度反应谱的影响不显著。 相似文献
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M. D. Sharma 《Journal of Earth System Science》2004,113(2):247-257
Three dimensional scattering of near-field is studied for dilatation and rotation in the time domain. The perturbation method
is applied to solve the equation of motion for the first order scattering from a weak inhomogeneity in an otherwise homogeneous
medium. The inhomogeneity is assumed close enough to the point source so that the near-field intermediate wave is dominating
over the far-field sphericalP andS pulses. The integral expressions are derived to relate dilatation and rotation of scattering to the radial fluctuations of
velocities and density in the inhomogeneity. These integrals are solved to calculate the strains of scattering from (a part
of) an inhomogeneous spherical shell of arbitrary curvature. Variable curvature may allow the shape of inhomogeneity volume
element to change uniformly from spherical to rectangular. Rotation of scattering from a spherical shell is independent ofP wave velocity inhomogeneity. Dilatation of scattering does not involveS wave velocity inhomogeneity but its gradient. The back scattering results are obtained as a special case. Strains are computed
numerically, for hypothetical models to study the effects of various parameters viz., velocity inhomogeneity, distance of
source from inhomogeneity and from receiver, and thickness of inhomogeneity. The curvature of the spherical shell is varied
to study the effects of the shape of inhomogeneous volume element on scattering. 相似文献
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地震次生地质灾害风险评估集对态势分析 总被引：2，自引：0，他引：2
5．12四川汶川8级强震引发了大量次生地质灾害,加剧了灾情并严重影响抗震救灾。地震次生地质灾害受多重因素制约,其孕育与致灾过程具有不确定性。利用集对分析原理与方法,对地震次生地质灾害进行同异反态势分析,拟定了风险评估的集对分析同一度、差异度、对立度等指标体系的构建原则与赋值标准,对承灾体系统的不确定性及其作用作了刻画与分析,建立了不同风险分区代表性的集对分析联系度表达式,为地震灾害研究提供了可资借鉴的新思路和技术方法。 相似文献
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Ivan V. BRAGIN Georgy A. CHELNOKOV Oleg V. CHUDAEV Natalia A. KHARITONOVA Sergey V. VYSOTSKIY 《《地质学报》英文版》2016,90(1):276-284
Studied waters belong to warm(T=30-50℃),alkaline(pH=8.9-9.3),low mineralized(TDS235 mg/1)Na-HCO_3 or Na-SO_4-HCO_3 thermal waters with high content of SiO_2(up to 81 mg/l)and F(up to 3.9 mg/1),occur on modern volcano-tectonic rejuvenated areas of Eastern Sikhote-Alin orogenic belt.Low~3He concentration as well as N_2/O_2 and N_2/Ar ratios exclude influence of deep mantle fluid.New rare earth element data constrain our understandmg of water-rock interaction occurring in the water source region.Meteoric origin of waters is proved by stable isotope values varying from-71‰to-136.1‰and from-10.8‰to-18.8‰forδ~2U andδ~(18)O respectively.REE patterns reflect high pH,resultfing from water-rock interaction and oxidative conditions.Calculations of deep aquifer temperature using Na-K and quartz geothermometers show 116.8-131.1°C and 82.2-125.8℃respectively.Presence of deep faults both with abnormal thermal gradient(~45-50 K/km)define unique geochemical shape of thermal waters of Sikhote-Alin,area,where no present volcanic activity is registered. 相似文献
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下扬子区三叠纪古地理演化 总被引：2，自引：2，他引：0
下扬子区在三叠纪期间接受了早-中三叠世海相碳酸盐沉积、中-晚三叠世海陆交互相和陆相湖沼沉积.沉积相带的空间分布和古地理格局的变迁明显地受到区域构造的控制.区内盆地发育与演化是在华南板块与扬子板块、扬子板块与华北板块相互作用的背景下进行的.早-中三叠世末期的印支运动是下扬子区构造-古地理格局改变的决定性因素,使下扬子海盆闭合,沉积类型由海相沉积变为陆相沉积.下扬子区三叠纪古地理的演化特征也为板块碰撞提供了沉积证据. 相似文献
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Isothermal thermogravimetric experiments have been carried out to determine the reaction kinetics of the dehydration processes
in fuller's earth, a natural Ca-montmorillonite. Dehydration in swelling clays is a complex reaction, and analysis of the
thermogravimetric data using empirical rate equations and time-transformation analysis reveals that the nature of the rate
controlling mechanism is dependent upon both the temperature regime of the sample as well as the extent of reaction. For fuller's
earth, we find that the dehydration kinetics are dominated by a nucleation and growth mechanism at low temperatures and fractions
transformed (stage I), but above 90 °C the last stages of the reaction are diffusion controlled (stage II). The activation
energy for dehydration during stage I is around 35 kJ · mol−1, whereas the removal of water during stage II requires an activation energy of around 50 kJ · mol−1. These two stages of dehydration are associated with primary collapse of the interlayer (stage I) and movement of water that
is hydrated to cations within the interlayer (stage II).
Received: 28 August 1998 / Revised, accepted: 27 January 1999 相似文献