莺歌海盆地底辟构造的成因及石油地质意义

在总结莺歌海盆地底辟构造特征及其伴生的温度和压力异常资料的基础上,提出了流体底辟模式,并进一步讨论了流体底辟在石油地质中的意义.     

Compressive sensing SAR range compression with chirp scaling principle

Compressive sensing(CS) techniques offer a framework for the detection and allocation of sparse signal with a reduced number of measurements.This paper proposes a novel SAR range compression,namely compressive sensing with chirp scaling(CS-CS),achieving the same range resolution as conventional SAR approach,while using fewer range samplings.In order to realize accurate range cell migration correction(RCMC),chirp scaling principle is used to construct reference matrix for compressive sensing recovery.Additionally,error diagrams are designed for measurement of the performance of CS-CS,and some experiments of using real data are performed to deal with the errors caused by three conditions:SNR,sparsity and sampling.     

海量数据库迁移与升级

目前数据库中数据越来越多,应用对数据库在线时间的要求也越来越高,使得数据库迁移和数据库升级成为了一件非常困难的事情.为此,介绍了几种迁移和升级的方法,用以实现以尽可能少的停机时间对TB级数据库完成数据库的迁移和升级.     

化学成分对红黏土界限含水率的影响

为研究桂林地区红黏土中化学成分Fe₂O₃、Al₂O₃、SiO₂含量对其界限含水率的影响,分别采用蒸馏水和乙二胺四乙酸二钠(EDTA二钠)浸泡红黏土土样,对不同浸泡时间的土样进行化学成分XRF测定,同时进行界限含水率测试和比重试验。通过回归分析和路径分析,建立了以Fe₂O₃、Al₂O₃、SiO₂含量为变量的红黏土界限含水率和相对密度的非线性回归模型,红黏土液限与塑限之间、塑性指数与液限之间以及相对密度与塑限之间的线性回归模型,红黏土Fe₂O₃、Al₂O₃、SiO₂含量与液限、塑限、塑性指数和相对密度之间的路径模型,并分析了化学成分对红黏土界限含水率的影响。     

黄河淤积粉土的两种复合稳定方案与性能对比

为探索路基工程中黄河淤积粉土的稳定技术和性能保障方案,针对德州齐河县境内的黄河淤积粉土,在乳化沥青复合稳定粉土(AE稳定土)的研究基础上,采用无机/有机复合材料制备出一种复合固化剂(FG固化剂),研究了AE稳定土和FG稳定土2种稳定方案下粉土的抗压强度性质、水稳定性和抗冻融能力;结合XRD、SEM表征技术,探讨了FG固化剂的稳定机理。研究认为,FG固化剂稳定土较AE稳定土有着更高的无侧限抗压强度、回弹模量和承载能力,水稳定性良好,在抗冻融能力上有着比AE稳定土更好的效果。XRD与SEM分析表明,FG固化剂提供了活性矿物质,其复合胶凝效应和填充增强保障了粉土的抗压强度,高分子物质起到粘结颗粒界面、填塞孔隙的作用,降低了内部孔隙率;两者造成土体的最大干密度变大;与AE稳定土的稳定机理不同。FG固化剂的使用为黄河粉土的稳定和工程应用提供了参考方法。     

突发事件泄漏石油类污染物在水环境中迁移转化研究进展

突发事件泄漏的石油类污染物在水体中的迁移转化规律一直是环境水力学研究的难点。根据石油类污染物的物理、化学特征,针对其在水体中不同阶段的运动动力学特征,分别从油膜在水体表层的扩展迁移过程、水体表层油膜的风化过程、油膜污染物向下层水体的扩散过程、水体中石油类污染物的迁移转化过程、石油类污染物的迁移转化过程物理试验、常用溢油模型6个方面归纳分析了国内外在动力学机制及数学模拟方面的研究进展,并分析了未来研究趋势。     

Comparison of soil moisture at different depths for drought monitoring based on improved soil moisture anomaly percentage index

To better understand the characteristics and mechanisms of droughts at different drought stages, this study selected the Xiangjiang River Basin in China as the study area, and evaluated soil moisture (SM) at different depths for drought monitoring, through SM data simulated with the variable infiltration capacity (VIC) model. To solve the problem of unreasonable drought/wetness classifications based on the soil moisture anomaly percentage index (SMAPI), an improved soil moisture anomaly percentage index (ISMAPI) was developed by introducing the Box–Cox transformation. The drought/wetness frequency generated by ISMAPI demonstrated preferable spatial comparability in comparison with those from SMAPI. The lag time of ISMAPI relative to the standardized precipitation evapotranspiration index was closely related to soil depth, and was characterized by a fast response in shallow soil layers and a relatively slow response in deep soil layers. SM in shallow soil layers provided a measure for monitoring short-term droughts, whereas SM in deep soil layers provided a better measure for long-term persistent drought events. Furthermore, the occurrence and mitigation time of drought events identified by SM in deep soil layers usually lagged behind that identified by SM in shallow soil layers. Compared with deep SM, SM in shallow soil layers responded faster to meteorological anomalies, thereby resulting in shorter periods of SM persistence in shallow soil layers than in deep soil layers. This can explain the differences of SM at different depths in drought monitoring.     

沂沭河底泥中污染物空间分布特征及评价

测定沂沭河底泥的有机质(OM)、总氮(TN)、总磷(TP)及有效磷含量,分析了污染物之间的相关性,评价了沂沭河底泥的污染状况。结果表明:沂沭河流域表层沉积物中TN、TP分布特性相似,沂河中OM含量远低于沭河,OM、TN、TP分布的空间差异较大。有效磷含量约占TP含量的17.7%,表明农田及人类活动对流域水环境造成了一定程度的污染。C/N、N/P及OM与氮、磷含量的回归分析表明,碳、氮具有同源性,底质中OM及氮主要源于生物沉降,而磷主要源于外部输入。经评价,沂沭河底质沉积物环境质量整体较好,污染程度属于清洁水平。     

Regulation of Neutrophil Functions by Hv1/VSOP Voltage-Gated Proton Channels

The voltage-gated proton channel, Hv1, also termed VSOP, was discovered in 2006. It has long been suggested that proton transport through voltage-gated proton channels regulate reactive oxygen species (ROS) production in phagocytes by counteracting the charge imbalance caused by the activation of NADPH oxidase. Discovery of Hv1/VSOP not only confirmed this process in phagocytes, but also led to the elucidation of novel functions in phagocytes. The compensation of charge by Hv1/VSOP sustains ROS production and is also crucial for promoting Ca²⁺ influx at the plasma membrane. In addition, proton extrusion into neutrophil phagosomes by Hv1/VSOP is necessary to maintain neutral phagosomal pH for the effective killing of bacteria. Contrary to the function of Hv1/VSOP as a positive regulator for ROS generation, it has been revealed that Hv1/VSOP also acts to inhibit ROS production in neutrophils. Hv1/VSOP inhibits hypochlorous acid production by regulating degranulation, leading to reduced inflammation upon fungal infection, and suppresses the activation of extracellular signal-regulated kinase (ERK) signaling by inhibiting ROS production. Thus, Hv1/VSOP is a two-way player regulating ROS production. Here, we review the functions of Hv1/VSOP in neutrophils and discuss future perspectives.