四川盆地中部中二叠统热液白云岩储渗空间类型及成因

近年来,四川盆地川西北地区有多口井在中二叠统栖霞组、茅口组钻获高产气流,展现出该层系巨大的天然气勘探潜力,但有关该盆地中二叠统白云岩储层的成因机理则众说纷纭,一直未达成共识。为此,基于川中地区栖霞组、茅口组岩心及薄片等岩相学特征,以及碳、氧、锶同位素和包裹体均一化温度等地球化学特征,开展了中二叠统热液白云岩储渗空间类型及储渗相特征研究,分析了白云岩储层的成因及其控制因素。结果认为:(1)茅口组、栖霞组石灰岩地层经历了构造控制热液活动,发育萤石、鞍状白云石、天青石的热液矿物组合和膨胀角砾结构;(2)较之于宿主石灰岩,细—中晶云岩和鞍状白云石均呈现出δ18O负偏移、87Sr/86Sr正偏移;(3)中二叠统形成由热液溶孔、热液白云岩晶间孔、热液溶洞、热液扩溶缝等4种储渗空间构成的热液白云岩储渗体。结论认为:(1)热液白云岩储集相发育和分布受深大断裂的控制,呈"透镜状"分布在具"下凹"地震反射特征的区域;(2)中二叠统热液白云岩储集相与下伏烃源岩和上覆封堵层的有机组合可构成有利的天然气勘探目标。     

A novel distributed scheduling approach powered by central databases in optical burst networks

In terms of the growth rate, network capacity is slower than network traffic. To solve the mismatch between them, utilization of available capacity can be maximized to provide “best-fit” service for emerging applications (e.g., eBanking, Peer-to-Peer (P2P) file exchanges, etc.). To satisfy such a requirement, we propose a three-dimensional label scheduling algorithm (TD-LSA), which is a distributed scheduling approach powered by central databases. In the proposal, all connections are provisioned in three dimensions (i.e., space, time and wavelength) in a distributed way and uniquely identified by three-dimensional labels. And in this way a three-dimensional connection is more robust than a single-dimensional connection because the three-dimensional approach can avoid potential scheduling conflicts as much as possible by using central databases in a network. Thus, the central databases can reduce bandwidth consumption and offer “best-fit” service for three-dimensional connections. Furthermore, in order to further reduce bandwidth consumption and to match with a priority of traffic, K-least hop first path (K-LHPF) and a rescheduling mechanism are applied to our proposal. Simulation experiments demonstrate that our proposal achieves the expected performance gain against existing alternates.

PLC在中央空调控制系统中应用及常见故障检修

可编程控制器(PLC)控制系统具有工作稳定、可靠,便于维护,具有价格便宜、控制灵活方便等特点,被广泛应用于各行各业的自动控制系统中。介绍了可编程控制器的控制原理以及其在中央空调制冷系统控制中的应用,并对控制系统故障的检查与维修等相关技术进行了探讨。     

川中地区寒武系龙王庙组沥青成因与油气成藏史

运用有机岩石学、有机地球化学和扫描电镜等方法和技术,深入研究了川中地区寒武系龙王庙组中高演化沥青的成因类型、形成期次和来源;并在此基础上,结合包裹体及构造演化特征等,恢复了安岳气田龙王庙组气藏的成藏史。结果表明:(1)川中地区龙王庙组储层中沥青均来自于下寒武统烃源岩,沥青成因类型多样,以热裂解成因为主;(2)沥青的形成分为3个阶段,第1阶段为氧化水洗型沥青的形成,第2阶段为沉淀型沥青的形成,第3阶段为热裂解成因沥青的形成;(3)安岳气田龙王庙组气藏先后经历了5期的油气充注,包括2期液态烃的充注、晚三叠世—早侏罗世干酪根裂解气的充注、晚侏罗世—早白垩世原油裂解气的充注以及喜马拉雅期圈闭改造调整阶段干气的充注。     

塔里木盆地塔中北坡奥陶系碳酸盐岩岩溶储层的形成机理

塔里木盆地塔中北坡奥陶系碳酸盐岩储层已成为该盆地油气勘探的重要目标之一,目前对于该岩溶储层的溶蚀机制尚存在争议。为此,基于沉积、层序与储层综合研究成果,结合微观分析测试与宏观地震资料分析结果,将该区碳酸盐岩岩溶储层划分为石灰岩溶蚀孔洞型、白云岩孔洞型和硅质岩裂缝孔洞型3种类型,并分别探讨了其形成机理。结果表明:(1)石灰岩溶蚀孔洞型储层纵向上分布在中奥陶通鹰山组上段和一间房组,而白云岩孔洞型储层主要发育在下奥陶统蓬莱坝组和鹰山组下段且厚度较大;(2)石灰岩溶蚀孔洞型储层形成于三级层序界面(低位期)岩溶作用,而白云岩孔洞型储层则主要形成于受三级层序界面岩溶作用控制的深埋藏白云石化作用,两者均分布在三级层序界面之下的高位体系域;(3)该区硅质岩储层的发育明显受断裂控制,是深部热液沿断层对石灰岩改造的结果,硅质岩储层及其热液溶蚀缝洞系统分布在断裂附近。进而推测:塔中北坡奥陶系除了发育上述3种储层类型以外,还发育台地边缘礁滩型储层。     

Agreement and reliability in measuring central corneal thickness with a rotating Scheimpflug–Placido system and ultrasound pachymetry

PurposeWe compare the agreement and the reliability in measuring central corneal thickness (CCT) using two different technologies.MethodThe right eyes of 35 healthy individuals who had a negative history of ophthalmic disease, or ocular surgery were examined. The CCT was determined sequentially with a rotating Scheimpflug camera (Sirius; CSO), and an ultrasound pachymeter (P-1; Takagi). For statistical analysis, we used the methods suggested by Bland and Altman.ResultsThe mean values of CCT obtained from Sirius, and ultrasound were 537 ± 28 μm, and 550 ± 35 μm, respectively. There was a high correlation between Sirius and ultrasound (r = 0.92; p < 0.001), but the difference between the two measurements was statistically significant (t = −5.7; p < 0.00001). The precision of Sirius and ultrasound were 9.4 and 15.9 μm; repeatability 13.3 and 22.4 μm, and coefficient of variation 0.9% and 1.5%, respectively. The intraclass correlation coefficient was 0.97 for Sirius and 0.95 for ultrasound.ConclusionsThe average difference between corneal thickness measured with Sirius and ultrasound pachymetry was small but clinically significant. This means that the two instruments cannot be used interchangeably. Sirius showed precision and repeatability almost twice as much as ultrasound pachymetry. Confidence interval of 13.3 μm for Sirius can show variations in corneal thickness with an uncertainty value lower than 2.5% in 95% of cases. The simplicity of use, the possibility to obtain pachymetric maps, and less invasiveness make this instrument potentially useful in contact lens practice.     

基于MT的冀中台陷（京南段）西部Ⅲ级构造单元界限研究

太行山山前断裂是Ⅲ级构造单元太行山隆起与冀中台陷的边界,查明其具体位置对区域的深部热储调查评价具有重要意义。为此,本文在前期区域重力和航磁等物探工作的基础上开展大地电磁勘探工作。通过布设5条大地电磁剖面,实现了对Ⅲ级构造单元界限的详细勘探。通过对4000 m以浅地层进行反演解译,并结合区域重磁勘探成果及地质资料,确定了区域性断裂及其次生断裂的位置、产状、走向等,重新绘制了Ⅲ级构造单元界限。结果显示界限中段向东偏移2 km左右,南段和北段与原界限重合或小有差异。该结果与深地震反射剖面探测结果基本吻合。本文研究成果将对该区域地热勘探工作有一定的指导作用。