长北气田山2段小层砂体三维建模

鄂尔多斯盆地长北气田山西组2段为一套海相辫状河三角洲沉积体系,为揭示不同时期小层砂体发育规模及空间分布,以高分辨率层序地层分析为基础,相控建模为指导思想,短期基准面旋回为地层单元,等时地层格架为约束条件,采用序贯指示数学方法对长北气田山2段4个短期层序的水上分流河道、水下分流河道及河口坝微相小层砂体的发育规模及空间分布进行了随机模拟.砂体展布的三维模拟结果表明,河道自北向南沿物源方向延展,其中SSC1～SSC4短期基准面上升时期,河道加宽,小层砂体沉积厚度加大,物性较好,有利储层发育;下降时期河道变窄,小层砂体沉积厚度减小,物性变差.小层砂体的三维模拟结果在该区勘探实践中得到了很好的验证.     

Remaining oil distribution in Ng3^3 bottom water reservoir of Lin 2-6 fault-block in Huimin depression and potential tapping in horizontal well

Oil reservoirs with secondary bottom water in Ng33 members (in Guantao formation, Paleogene system) of Lin2-6 fault block in Huimin depression (Bohai Bay Basin) have entered the late stage of ultra-high water-containing-exploitation. Oil exploita-tion from vertical wells is becoming more and more inefficient. The reservoir type, with water displacing oil and the remaining oil distribution are specifically studied in order to improve the efficiency of the recovery ratio. An integrated scheme for adjusting horizontal wells has been designed and the key technique of the scheme optimized. The study shows that: 1) the positive rhythm of fluvial depositional features is the internal cause of the flooding of oil reservoirs while water injection, injection-production patterns and accumulative petroleum production are the external causes; 2) oil-water driving patterns have transferred from edge water ad-vancing to bottom-water-coning; distribution of the remaining oil mainly concentrates in the upper rhythm and top of the middle rhythm in Ng33 members; 3) a great deal of remaining oil is enriched in high positions of faults, in axes of tiny structures, in stagna-tion areas among water-injection wells and oil-wells and in tectonic saddle areas with sparse wells. Compared with vertical wells, horizontal wells have advantages such as high recovery, high off-take potential, high critical output, large controlling areas and long time of bottom-water breakthrough.     

Characteristics of late cretaceous faults of the eastern segment of the northern Qaidam basin, NW China

The Late Cretaceous tectonic upheaval was an important event during the evolution of the Qaidam Basin, resulting in the omission of the Upper Cretaceous in the whole basin and unconformities between the Paleogene sequence and pre-K2 strata. Inte-grating geological and geophysical data, two different groups of Late Cretaceous faults were recognized in the study area, one group consisting of E-W extending strike-slip faults (e.g., the Maxian and Yema-Jinan faults in the Mahai area, which caused an E-W omission zone of Mesozoic), while the other one has NW-SE thrust faults, resulting in NW-SE fold-and-thrust belts. Consid-ering the different strikes and scale of these two groups, a simple-shear model has been employed to explain this structural phe-nomenon. The NW-SE thrust faults were thought to be subsidiary to the E-W strike-slip faults. Putting this into the framework of the Cretaceous paleogeographic environment of central Asia, it is inferred that this tectonic event of the Qaidam Basin is a response to the continuous northward drifting of the India plate.     

高含硫气藏中元素硫沉积形态和微观分布研究

元素硫沉积是高含硫气藏开采过程中存在而又必须解决的难题之一.随着高含硫气藏储层压力不断下降,元素硫溶解度也不断下降,一旦元素硫溶解度低于元素硫含量,元素硫就会从地层中沉积下来.沉积的元素硫会堵塞地层孔隙,降低渗透率,严重影响气井产能.为了研究元素硫在地层中的沉积形态和沉积特征,利用自主设计的实验流程和实验方法,使TD5-1井高含硫气体通过岩芯,并降低压力让元素硫在岩芯中沉积下来,然后对沉积了元素硫的岩芯进行电镜扫描和能谱分析,首次得到了元素硫在岩芯中的沉积形态,即元素硫主要以膜状形式分布在岩芯孔隙壁面上.该研究结果为深入认识、掌握元素硫沉积规律以及指导高含硫气藏合理开发奠定了基础.     

螺纹桩在软弱地层中的应用

分析了螺纹桩的受力机理,探讨了螺纹桩单桩承载力的确定方法,指出螺纹桩单桩承载力高、节约材料显著、能充分利用地基土的特性,在软弱地层中的应用优势显著,并通过实际工程实例给予具体说明.     

盾构穿越沉降敏感区段的沉降监测及分析

在盾构穿越复合地层沉降敏感区段时,对该区段的施工沉降进行了严密观测,并对监测数据进行了全面分析,总结出上软下硬复合地层的沉降变形的一般规律.在工程实施中采取有针对性的沉降控制措施,确保敏感区段的沉降控制在允许范围之内.     

东营凹陷博兴地区油气成藏动力学研究

运用油气成藏动力学的理论与方法,和对成藏要素——烃源岩、储集层、盖层、运聚史等的描述,对东营凹陷博兴地区油气成藏动力学及其输导体系、地层压力场特征分别进行了研究.认为平面上异常高压区出现在博兴洼陷中心区,纵向上分布层位为砂三中、下亚段和砂四上亚段,异常压力的分布受暗色泥岩分布和生烃作用的控制,并在一定程度上受到砂体输导层、断层等因素的影响.博兴地区输导系统特别发育,由断层、砂体输导层以及不整合面组成,基本控制了全区的油气分布:高青断层、石村断层、博兴断层控制了研究区油气的纵向运移,砂体输导层的分布控制了油气的平面分布,不整合面在局部地区是油气的重要横向运移通道.最后根据地层压力、烃源岩条件和封闭特征将研究区在纵向上分为3个成藏动力学系统,即自源封闭型、他源半封闭型和他源开放型.     

浅埋暗挖地铁车站管棚的数值模拟及其加固效果分析

以北京地铁十号线黄庄站126 m超前大管棚一次性施作作为研究背景,在对管棚作用效果和作用机理分析的基础上,比较了现有管棚计算模型的优劣,提出了在数值计算中采用桩单元模拟管棚的思路;对车站导洞施工过程中管棚变形的动态过程以及管棚注浆和管棚直径对地表沉降的控制效果进行了分析研究.监测数据表明:北京地铁十号线黄庄站管棚施作后,四导洞开挖完成后地表沉降控制在30 mm左右,与四号线黄庄站四导洞完成后地表80 mm的沉降值相比大大减小,起到了良好的控制作用.     

海上浅水三角洲油田砂体构型研究——以渤中19-25地区为例

针对海上浅水三角洲相油田储层展布的复杂现象,建立等时地层格架,分析浅水三角洲砂体的储层构型,确定该地区地层对比的稳定分布标志层。通过五级构型分析认为,发育的浅水体三角洲砂体模式包括:连片状分流河道与河口坝组合模式;条带状分流河道与天然堤组合模式。通过四级构型分析认为,连片状的砂体均由多期次单河道砂体组成。同时,根据单一分流河道识别标志分析,识别出单一分流河道。     

气体钻井地层出水环空携液规律研究

气体钻井在钻井提速、缩短建井周期和保护储层方面具有明显的优势,但钻井过程中也容易发生一些复杂情况,如若气体钻井导致地层出水,会引起携岩规律复杂化、井壁失稳等状况,影响钻井速度、质量及成本。通过对气体在环空中携水机理的研究,建立环空液滴大小模型,并对影响因素进行分析。同时提出环空气体携水量计算模型,利用MATHCAD编程计算出的理论数据与环空气体携水模拟实验数据基本吻合。