大庆油田深层岩石力学特性参数的试验研究

通过对岩石可钻性、硬度、抗压强度等参数的测量 ,对大庆油田深井不同深度、不同层位、不同岩性的具有广泛代表性的岩心进行试验。并通过线性回归分析 ,建立了适用性较广的钻井岩石力学特性参数预测模型 ,为深井钻头选型提供了依据。     

大红山铜矿岩体结构调查分析

大量工程实践已证明岩体结构是控制岩体稳定性的重要影响因素。为此，以大红山铜矿为研究背景，在选定有代表性调查地段的基础上，引入详细观测线法对其岩体结构进行了详细调查与统计。分析结果表明：调查区域内巷道岩体节理裂隙比较密集和发育，主要发育有倾向N53E、走向N37W、倾角53°，倾向W26S、走向N36W、倾角68°；倾向E1S、走向NIE、倾角89°的三组优势结构面，其中优势结构面第二组和第三组构成不稳定块体，并且断层及软弱夹层比较发育，加剧了巷道的破碎程度，对巷道围岩的稳定性有控制作用。最后提出了在巷道施工中密切注意围岩稳定性变化，避免工程事故的发生的建议。     

塔河油田三叠系水平井地质导向技术研究

针对塔河油田三叠系碎屑岩油气藏油层薄、储集层非均质性较强、泥质和低渗致密夹层纵横向变化大的地质特点，在分析、研究不同区块多口水平井资料的基础上，探讨了水平井不同地质情况下斜井段及目的层砂顶的预测和判别技术，以实例阐述了井眼轨迹调整方法，首次形成了一套适合于该地区碎屑岩非均质薄层油气藏水平井录井地质导向技术，在塔河油田水平井钻探开发中取得了显著的成效。     

Effect of igneous activity on hydrocarbon source rocks in Jiyang sub-basin, eastern China

A 50 m thick diabase sill was found in the Paleogene black mudstone hydrocarbon source rocks in Xia38 well. Within heating aureola of the sill, optical changes of kerogen and signatures of extractable bitumens in the mudstones were investigated. Under effects of high heating rate associated with sill intrusion, the vitrinite reflectance (Ro) has an increasing tendency with decreasing distance to the sill both below and above the sill. However, only within a zone of about 15 m to the diabase sill, the vitrinite reflectance shows significant increase. Above the sill, the Ro values increase gradually from 0.6% to 1.0%, whereas below the sill, the Ro values increase dramatically from 0.8% to 3.8%. The contrasting Ro increasing patterns are attributed to the different heat transferring conditions, the relatively open system above the sill and the relatively close system below. The more mature signatures below the sill are also demonstrated by the n-alkane distribution, carbon predominance index and odd-to-even carbon number predominance of the extracted bitumens. Below the sill, the proportion of the saturated hydrocarbons in the extracted bitumens increases from 34% to 79% towards the sill contact. The bitumens in the two highest rank samples which are closest to the sill are dominated by saturated or saturated + aromatic hydrocarbons.The %20S, %αββ and %Ts biomarker parameters of the extracted bitumens are 46%, 58% and 54%, respectively, at Ro = 1.5%. At Ro = 2.6% or 3.0%, they reach to 52%, 71%, and 71%, respectively, still under or close to their corresponding equilibrium end-points. These samples of high rank, established on the basis of optical assessment (vitrinite reflectance), have less mature biomarker signatures. The remarkable disparities between optical and biomarker parameters can be ascribed to that the aromatization of kerogen to increase Ro was more favored than the isomerization of biomarker in the rapid heating scenario.     

岩石液压致裂中几个问题的研究

论证了流体压力变化与岩石强度变化之间的关系，阐述了流体保持与释放的应力条件和构造环境，总结了两种围岩下的液压致裂模型及其流量方程。     

渤海湾盆地复式油气聚集带高勘探程度区进一步挖潜的领域

渤海湾盆地复式油气聚集区经过了40年的勘探,目前已进入了高勘探程度区.油气聚集的复杂规律表明,渤海湾盆地仍具有巨大的资源潜力,进一步挖潜的领域非常广阔.以第三系为烃源岩的含油气层系的勘探精度仍有待于进一步提高,同时必须将以古生界、中生界和中上元古界为烃源岩的含油气层系作为今后挖潜的重要领域.渤海湾盆地任何层系都可能形成和聚集油气,因此仍有多种复杂的油气藏类型尚待进一步认识和发现.     

新型硬及极硬岩石反井镶齿盘型破岩滚刀的研究

对新型硬及极硬岩石反井镶齿盘型破岩滚刀的总体设计方案、CrMnMo空冷耐磨钢调质处理以及力学性能、镶嵌固齿和过盈量的确定等滚刀设计关键技术,进行了分析、试验和研究,并取得了相应的结论。     

崇礼东坪黄金公司缓倾斜薄矿体采空区综合治理

在采空区调查的基础上,以FLAC工程力学分析软件为手段,应用“诱导崩落和封闭采空区综合治理”理论,进行缓倾斜薄矿体采空区综合治理研究.该项研究与实践为缓薄矿体采空区综合治理提供了可供借鉴的经验,并为矿山创造了可观的经济效益.     

The distribution of nutrient elements in cell wall and other fractions of the herbage of some grasses and legumes

The distribution of 10 nutrient elements was assessed in three fractions of herbage samples of perennial ryegrass, tall fescue, white clover and lucerne. The cell wall fraction, prepared by mechanical disintegration of undried material, contained the following proportions of the total herbage content of the major elements: N, 2.9–16.4%; P, 3.0–6.9%; S, 3.6–17.2%; Ca, 11.3–51.8%; Mg. 6.4–27.6% and K, 0.1–1.7%. Substantial though more variable proportions of the trace element cations, Fe, Mn, Zn and Cu were also present in the cell wall fraction. The extent to which the elements were soluble in water was assessed by analysis of the water-insoluble fraction prepared from freeze-dried samples of each herbage. The proportions of the total herbage content of the major elements soluble in water were: N, 30–57%; P, 80–92%; S, 35–71%; Ca, 48–69%; Mg. 65–83% and K, 90–96%. With the trace element cations the proportions soluble in water were more variable, though they were generally less than 70% of the total. The extent to which the various elements were soluble in 80% aqueous ethanol was assessed by analysis of the insoluble fraction prepared from freeze-dried materials. With each of the major elements, smaller proportions of the total herbage content were soluble in 80% ethanol than in water, which may reflect in part the lower solubility of proteins and pectin. With the trace element cations, the differences in solubility between 80% ethanol and water were generally small and inconsistent.     

辽东含硼岩系条痕状角闪混合岩特征及其找矿意义

痕状角闪混合岩与其围岩变（浅）粒岩为渐变过渡关系.并呈现一些特殊的结构构造.其岩石化学成份变化波动性较大,说明岩石化学成分不稳定,与矿化含量的不稳定性一致.其特殊的岩石化学组成显示为混合岩特征.条痕状角闪混合岩石稀土总量ΣREE的平均值为207.18 ppm;（Ce/ΣY平均值为3.25;La/Yb为平均值为 6.48,δEu平均为 0.48,Eu/Sm平均值为0.16.这些特点与里尔峪组的各种变（浅）粒岩相似,是层状混合花岗岩.