Processing and characterization of the microstructure and mechanical properties of Al6061–TiB2 composite

In the present research, aluminum metal matrix composites were processed by the stir casting technique. The effects of TiB2 rein-forcement particles, severe plastic deformation through accumulative roll bonding (ARB), and aging treatment on the microstructural charac-teristics and mechanical properties were also evaluated. Uniaxial tensile tests and microhardness measurements were conducted, and the micro-structural characteristics were investigated. Notably, the important problems associated with cast samples, including nonuniformity of the rein-forcement particles and high porosity content, were solved through the ARB process. At the initial stage, particle-free zones, as well as particle clusters, were observed on the microstructure of the composite. However, after the ARB process, fracturing phenomena occurred in brittle ceramic particles, followed by breaking down of the fragments into fine particles as the number of rolling cycles increased. Subsequently, com-posites with a uniform distribution of particles were produced. Moreover, the tensile strength and microhardness of the ARB-processed com-posites increased with the increase in the reinforcement mass fraction. However, their ductility exhibited a different trend. With post-deforma-tion aging treatment (T6), the mechanical properties of composites were improved because of the formation of fine Mg2Si precipitates.     

不同周围流速和电压下的绝缘子积污特性

为了研究绝缘子在不同电压下表现的积污特性，利用流体力学的相关知识和电场理论，建立了模拟风沙的多物理场仿真模型.研究结果表明，周围流动速度较小时，绝缘子两端的电压增大，积污质量发会有一定程度的增加，且积污与电场力的变化密切相关，结合静电场分析会更准确；周围流动速度较大时，即使电压增大，积污质量也不会发生太大的变化.     

准噶尔盆地乌伦古坳陷中南部石炭系烃源岩生烃潜力分析

目前已在准噶尔盆地乌伦古坳陷石炭系、二叠系、三叠系和侏罗系等发现了工业油气流或油气显示，这些油气主要来源于石炭系烃源岩。但目前研究区石炭系有效烃源岩分布及生烃演化特征不清楚。笔者对比分析了研究区石炭系不同层段、不同岩性类型烃源岩的生烃潜力和热演化特征。结果表明：巴塔玛依内山组凝灰质泥岩、泥岩和姜巴斯套组炭质泥岩有机质丰度较高，有机质类型以Ⅱ2—Ⅲ型为主，处于成熟—过成熟演化阶段，具有倾气性特征。综合应用地球化学实验数据得出姜巴斯套组烃源岩都是有效气源岩，而目前钻井揭示巴塔玛依内山组烃源岩成熟度偏低，未能达到有效气源岩的标准。通过系统对比研究区与滴水泉凹陷石炭系烃源岩地球化学参数，认识到两地区具有高度相似性。可见准噶尔盆地乌伦古坳陷中南部石炭系姜巴斯套组是一套极具潜力的烃源岩，为下一步油气勘探指明方向。     

准噶尔盆地车排子凸起新近系沙湾组重矿物、U-Pb年代学特征及物源分析

综合岩石学特征、砂岩碎屑组分特征、重矿物组合特征和锆石U-Pb年代学特征, 探讨准噶尔盆地车排子凸起新近系沙湾组沙一段的沉积特征和物源演化过程。结果表明, 车排子凸起存在南北双物源体系, 沙一段以粗碎屑沉积为主。在一砂组沉积阶段, 扎依尔山为北部物源区, 发育小规模扇三角洲沉积; 中天山及北天山造山带为南部物源区, 发育辫状河三角洲沉积。在二砂组沉积阶段, 中天山供给减弱, 北天山供给加强, 盆地水体加深, 南部辫状河三角洲前端分布小型滨浅湖滩坝。南部物源变化的主要原因可能是受印度板块和欧亚板块碰撞的远程影响, 天山在新生代中新世中期经历强烈的挤压和抬升过程, 造成北天山隆升, 为车排子凸起提供物源。     

Mechanical behavior of a near α titanium alloy under dynamic compression: Characterization and modeling

Dynamic compression tests under strain rates from 870 s^?1 to 2100 s^?1 were conducted for a near α Ti–8Al–1Mo–1V titanium alloy with equiaxed microstructure. Compression behavior, adiabatic shearing and band microstructure were investigated via characterization and calculation. The results demonstrate that all dynamic constitutive curves exhibited obvious stress fluctuation phenomenon with double increase-decrease changing stages at the primary stage of compression. The dislocation multiplication theory can be used to explain this phenomenon. After the stress fluctuation period, work hardening coexisted with the thermal softening, resulting in the slow hardening tendency in constitutive curves. J-C model was utilized to quantify the dynamic constitutive curves. The deviations between the predicted and experimental curves under high strain rates may be attributed to the over-consideration of thermal softening effect in J-C model. Adiabatic shearing band (ASB) began to form under the strain rate of 2100 s^?1. A total shearing strain of 8.1 within ASB achieved in 8.9 μs, corresponding to a local strain rate of about 9.1 × 10⁵ s^?1 and is over 430 times of the macro strain rate. Post annealing was conducted on ASB before EBSD characterization. Due to the static recrystallization during annealing, the α phase within ASB generally presented as ultra-fine grains less than 1 μm in diameter.     

KL油田沙三下亚段混合沉积特征及演化

针对目前莱州湾凹陷南斜坡带KL油田沙河街组三段下亚段陆源碎屑与碳酸盐岩混合沉积形成条件、沉积特征及模式认识程度较低的问题，利用该区壁芯、薄片及扫描电镜等资料，结合构造演化、古气候和古地貌背景，在层序格架约束下研究沉积环境，分析其沉积特征。结果表明，研究区发育混合沉积，形成于宽缓斜坡、亚热带湿润气候，兼具湖平面、物源、水动力条件周期性变化等条件；该混合沉积包括相缘渐变混合与原地混合两种沉积类型，互层式和组分式两种混合模式，以及4种混合样式。两种混合沉积类型沉积机理不同，混合模式及组合样式表现较大差异，因而具有不同的储层微观特征。     

苏里格气田马家沟组膏模孔型储层特征及成因

含“膏模”孔泥粉晶云岩是鄂尔多斯盆地马家沟组上组合地层重要储集岩类型，其形成时间和成因对于该类型储层的认识具有重要意义。研究利用苏里格东区丰富的取芯资料，根据岩芯、薄片等观察手段，结合常规物性测试分析，综合研究含“膏模”孔型储层特征及其成因。结果表明，“膏模”孔主要发育于泥粉晶白云岩中，位于向上变浅序列中部，常可见未充填—半充填型与全充填型两类。储层特征方面，该类储集岩主要发育“膏模”孔充填残余孔、渗流粉砂间微孔和基岩晶间溶蚀微孔3类储集空间，物性测试显示储集性能优越，平均孔隙度可达5.34%，平均渗透率为1.02 mD。纵向沉积序列显示“膏模”孔发育受沉积旋回控制，旋回中部“膏模”孔内存在溶蚀，内为云质渗流粉砂充填，旋回顶部具有暴露特征，且可见下一次海侵泥质灌入岩溶系统内，各类特征均指示“膏模”孔形成与准同生期岩溶相关，即“膏模”孔形成于准同生期，而非传统认识的表生阶段。     

基于隐马尔可夫模型的公交乘客出行链识别方法

以公交IC卡数据为基础,结合公交站点周边土地类型及乘客时空转移序列构建隐马尔可夫模型对乘客的出行目的进行识别,继而实现完整乘客公交出行链的提取。采用石家庄某一工作日的公交IC卡数据来实现模型,并与同日期的公交乘客出行调查数据对比,结果表明模型与实际调查结果较为吻合,工作日公交乘客出行链以通勤类出行链为主,总占比达81.87%,通勤活动具有很强的时效性。本文模型为公交IC卡数据的深度研究提供了一定的基础。     

渤海特高含水期油田剩余油分布规律及挖潜策略

油田进入特高含水期后,受储层韵律性、平面非均质性、断层边界及纵向夹层等影响,油层水淹规律及剩余油分布十分复杂。为进一步提高油田采收率,结合新钻井水淹层测井解释成果、密闭取心、生产动态及油藏数值模拟等资料,对渤海Q油田水淹特征和剩余油分布规律进行深入研究,并提出相应的调整井挖潜策略。认为油层底部、井点附近及边水油藏注采主流线水淹严重,油层中上部、井间区域、遮挡带附近和底水油藏边部水淹较弱或未水淹,纵向上井间区域水淹层占比为8%～65%,平面上生产井有效动用半径为70～150 m。提出利用水平井进行井间加密、边部完善井网、垂向穿夹层动用屋檐油及井网调整等挖潜策略。结果表明:利用水平井挖潜特高含水期剩余油,可有效改善开发效果,提高油田采收率,并为海上类似油田的调整挖潜提供借鉴。     

川中地区南充构造成因机制探讨

南充构造处于川中隆起斜坡位置,又是龙门山构造带、大巴山构造带和华蓥山构造带等不同方向不同时期构造交汇叠置地区。为研究分析川中地区南充构造,基于区域地质资料、地震资料及物理模拟实验对南充构造成因机制进行分析。研究表明,南充构造形成于燕山晚期,在喜马拉雅期改造定型,通过设计实施构造物理模拟实验,验证了在隆升作用下南充构造形成的可能性。