斜向往复水平荷载作用下矩形截面框架柱抗震性能

通过7根矩形截面钢筋混凝土框架柱试验,研究了不同加载角度时低周往复斜向水平荷载作用下,矩形截面框架柱双向受剪承载力的相关性、滞回曲线特性和延性系数。结果表明,低周往复斜向水平荷载作用下矩形截面框架柱的受剪承载力随加载角度的增大而减小;双向受剪承载力的相关关系可以近似用椭圆方程描述;滞回曲线在形状上与正向水平荷载作用下框架柱的滞回曲线并无明显差异;随着加载角度的增大,框架柱的延性系数有降低的趋势。低周往复斜向水平荷载作用下所有框架柱的破坏均为剪切脆性破坏,应加强其抗震设计。     

矿山微地震全波自动定位的层析成像方法(英文)

针对在矿山微地震监测过程中纵横波及其传播速度难以确定的难点,在球坐标系中以波动方程为基础,推导出了矿山微地震全波自动定位的层析成像的计算公式,并给出了参数选择准则,藉此可以获得微地震成像能量最大值及其对应参数。通过判断能量最大值在风险区内的位置,可以将风险区内外的微地震事件区分出来。对于能量最大值位于风险区域内的微地震事件,其震源位置和震动时间以及传播速度与能量最大值对应的坐标参数相同,能量最大值对应于震源函数相对强度;当能量最大值位于风险区域边界上时,微地震事件不在风险区域范围之内。理论模型试算和矿山实际微地震资料的应用表明:层析成像方法无需纵横波识别和传播速度假定,只要给定事故风险区域范围及其传播速度范围,便可完成微地震事件定位,是一种全波全自动定位方法,具有进一步研究价值。     

Magnetic Susceptibility and Heavy Metals Distribution from Risk‐cultivated Soil around the Iron–Steel Plant,China

Magnetic susceptibility is a non‐conventional way that can be used for evaluating proxy soil heavy metals pollution. The paper monitors available heavy metals (Cu, Fe, Zn, and Mn) present in cultivated soils around iron–steel plant by soil magnetic susceptibility. Our study was located in an area with high pollution with small grid density of 250 m in China. Results showed that low field magnetic susceptibility was significantly correlated with available Cu, Zn, and Mn. No clear association exists between magnetic susceptibility and available Fe, soil organic matter, pH. Frequency dependent susceptibility >5% suggests the possible presence of super‐paramagnetic particles, fly ashes produced during coal combustion.     

基于GIS的兰州滑坡与泥石流灾害危险性分析

频繁发生的灾害愈来愈对人类社会造成巨大影响, 遥感、地理信息系统、全球定位系统和网络技术日益在减灾行动中发挥重要的作用. 兰州区域地质岩性、构造断裂、地震活动带、地表侵蚀强烈和地形起伏破碎等因素造成了兰州滑坡与泥石流灾害的发育, 夏季暴雨、人类工程活动等诱发下灾害频繁, 风险加剧. 针对兰州地区滑坡与泥石流等山地灾害对区域社会经济的影响, 通过建立区域滑坡与泥石流灾害的空间数据库, 在GIS技术辅助下实现了专家经验模型和Logistic模型对滑坡与泥石流灾害危险性的预测, 其中滑坡Logistic模型准确性达到85.3%, 专家经验模型准确性达到74.2%; 泥石流Logistic危险性预模型准确性达到80.5%, 专家经验模型准确性达到90.5%. 随着研究的深入, 综合遥感、地理信息系统、全球定位系统和网络技术的灾害研究与应用将在灾害防治中发挥重要的作用.     

大菱鲆2种类胰岛素样生长因子结合蛋白基因克隆及在成鱼和早期发育期中的表达

类胰岛素样生长因子结合蛋白(IGFBP)在调节IGF的生物学功能上起着重要的作用,利用简并引物扩增及RACE克隆技术,首次克隆得到大菱鲆IGFBP-1,-2基因cDNA全长序列。两个基因氨基酸序列都分为保守的N端和C端以及高度特异的L区域3个部分,其中N端和C端共包含18个半胱氨酸残基,N端存在一段保守的(GCGCCXXC)结构,C端存在一段保守的(CWCV)结构,这些结构在与IGF相互作用以及调节与IGF结合的亲和性和稳定性起重要作用。组织表达分析表明,igfbp-1主要在肝脏及脾中大量表达,在其他组织中表达量较少,igfbp-2除在肌肉中没有检测到表达外,在其他组织中均有表达,其中肝脏脑、心、肾、肠中表达量较高。广泛的组织表达模式表明IGFBP是通过自分泌和旁分泌来调节IGF的功能。对于胚胎发育期表达分析表明,igfbp-1在整个发育期均检测到表达,igfbp-2在胚体期开始有表达,结果表明igfbp-1和igfbp-2在胚胎发育过程中的细胞生长以及组织器官分化都起着重要的生理学作用。     

Changing spatial and structural patterns of non-agricultural activities in outward-moving Beijing urban fringe

As responses to metropolitan suburbanization and rural urbanization,the formation and evolution of urban fringes should be understood against the background of overall economic development and spatial reconstruction of entire metropolises.At the same time,however,endogenous interactions between industrial structure and spatial patterns of non-agricultural activities are also worthy of scholarly attention.Since the 1980s,studies on urban fringes in China have been restricted by the lack of micro-level data.This paper investigates the spatial expansion and structural evolution of the urban fringe by taking the case of Beijing and uses systematic firm-level data in 1996 and 2001 from the National Census of Basic Units.The diversity of distribution patterns across industrial sectors brings about two interrelated results.On the one hand,structural adjustment of non-agricultural industries promotes the expansion and spatial evolution of the urban fringe.On the other hand,the stability and dynamics of industrial structure coexist in the moving urban fringe.This study also reveals that the outward-moving urban fringe is the optimal location for manufacturing,especially heavy manufacturing,as well as traditional producer and consumer services.However,industries with spatial stickiness such as tourism and sports have not moved with the fringe.Most advanced services remain concentrated in the city center.The authors argue that it is essential for understanding and managing urban fringes to take into account spatial evolution and industrial structural adjustment together with their interaction with each other.     

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Paleocurrent and fabric analyses of the imbricated fluvial gravel deposits in Huangshui Valley, the northeastern Tibetan Plateau, China

Gravel deposits on fluvial terraces contain a wealth of information about the paleofluvial system. In this study, flow direction and provenance were determined by systematic counts of more than 2000 clasts of imbricated gravel deposits in the Xining Region, northeastern Tibetan Plateau, China. These gravel deposits range in age from the modern Huangshui riverbed to Miocene-aged deposits overlain by eolian sediments. Our major objectives were not only to collect first-hand field data on the fluvial gravel sediments of the Xining Region, but also to the reconstruct the evolution of the fluvial system. These data may offer valuable information about uplift of the northeastern Tibetan Plateau during the late Cenozoic era. Reconstructed flow directions of the higher and lower gravel deposits imply that the river underwent a flow reversal of approximately 130–180°. In addition, the lithological compositions in the higher gravel deposits differ significantly from the lower terraces, suggesting that the source areas changed at the same time. Eolian stratigraphy overlying the gravel deposits and paleomagnetic age determination indicate that this change occurred sometime between 1.55 Ma and 1.2 Ma. We suggest that tectonic activity could explain the dramatic changes in flow direction and lithological composition during this time period. Therefore, this study provides a new scenario of fluvial response to tectonic uplift: a reversal of flow direction. In addition, field observation and statistical analyses reveal a strong relationship between rock type, size and roundness of clasts.     

内蒙古大黄花地区铜多金属矿地质特征及找矿建议

大黄花铜多金属矿区位于赤峰金银多金属成矿带南部,是在近年来开展1：5万数字化区域地质矿产调查野外工作中发现的.区内构造处于赤峰-开原深大断裂带中.含矿围岩主要为石炭系酒局子组地层,又叠加了中生代大规模的火山喷发作用及岩浆侵入活动,具有较好的成矿地质条件.     

华庆地区长63段低渗储层特征及优质储层主控因素

综合运用岩心观察、薄片鉴定、物性分析、压汞分析及试油分析等技术方法,对华庆地区长6₃段低渗储层特征进行了系统研究,分析了低渗储层的成因,并探讨了优质储层的主控因素。结果表明,华庆地区长6₃段储层的厚层块状砂岩主要由具有液化流性质的砂质碎屑流沉积形成的相对较厚块状砂岩纵向叠置组成。岩石类型主要为长石砂岩,其次为岩屑长石砂岩;储层具有低孔特低孔-特低渗透超低渗透特征;储集空间主要包括粒间原生孔隙、次生溶蚀孔隙及晶间微孔隙,为小孔微细喉型孔隙结构。杂基含量高、成分成熟度和结构成熟度差是华庆地区长6₃低渗储层形成的主控因素,压实作用对其形成起到强化作用。沉积鼎盛时期水动力强的主力沉积期次,形成泥质含量较低的砂岩是优质储层形成的主控因素,而较大的储层厚度是优质储层形成的必要条件。