桂林地区岩溶水SF6年龄研究

2006年10月在桂林地区取地下水、地表水水样5个,空气样品5个,用气相色谱“双阀双柱”法测定了SF6 的浓度,以质量平衡原理为基础建立了计算地下水SF6 年龄的模型。计算结果显示,岩溶裂隙水的SF6 年龄比地下河水的年龄偏老,地下河源头水的SF6 年龄比出口处的年龄偏老,即桂林市丫吉实验场1号洼地岩溶裂隙水SF6 年龄为10年,山脚下地下河出口处水的年龄为8年,冠岩地下河源头水SF6 年龄为9年,出口处的年龄为5年。这可能是与地下河出口处受当年大气降水的影响有关。      

A cloud model of active galactic nuclei: the iron Kα line diagnostics

The origin and the profile of the iron K α line from active galactic nuclei are studied. The model with a quasi-spherical distribution of clouds around a compact galactic nucleus is explored, in which the intrinsic spectral feature around 6–7 keV is substantially affected by Comptonization of primary X-rays. The predicted spectral profiles are influenced mainly by the motion of the clouds in the strong gravitational field of the centre, and by the orientation of the source with respect to the observer. The case of the Seyfert galaxy MCG–6-30-15 is examined in more detail and free parameters of the model are determined. A robust result is obtained: acceptable fits to the observed profile correspond to a spherical distribution of the clouds with strong self-obscuration effects and with a rather high value of ionization parameter. This is a different situation from that considered in the model of a cold illuminated disc. Nevertheless, geometrically flat (disc-type) configurations are not rejected.     

OB association members in the ACT and TRC catalogues

The Hipparcos Catalogue contains members of nearby OB associations brighter than 12th magnitude in V . However, membership lists are complete only to magnitude V =7.3. In this paper we discuss whether proper motions listed in the 'Astrographic Catalogue+Tycho' reference catalogue (ACT) and the Tycho Reference Catalogue (TRC), which are complete to V ∼10.5 mag, can be used to find additional association members. Proper motions in the ACT/TRC have an average accuracy of ∼3 mas yr⁻¹. We search for ACT/TRC stars which have proper motions consistent with the spatial velocity of the Hipparcos members of the nearby OB associations already identified by de Zeeuw et al. These stars are first selected using a convergent-point method, and then subjected to further constraints on the proper-motion distribution, magnitude and colour to narrow down the final number of candidate members. Monte Carlo simulations show that the proper-motion distribution, magnitude, and colour constraints remove ∼97 per cent of the field stars, while at the same time retain more than 90 per cent of the cluster stars.
The procedure has been applied to five nearby associations: the three subgroups of Sco OB2, plus Per OB3 and Cep OB6. In all cases except Cep OB6, we find evidence for new association members fainter than the completeness limit of the Hipparcos Catalogue. However, narrow-band photometry and/or radial velocities are needed to pinpoint the cluster members, and to study their physical characteristics.     

Migmatite gneiss of the Jættedal complex,Liverpool Land,East Greenland: protracted high‐T metamorphism in the overriding plate of the Caledonian orogen

The Greenland Caledonides (GC) formed in the overriding Laurentian plate during the closure of the Iapetus Ocean and the subduction of Baltica, and offer a unique opportunity to study metamorphic patterns, regional structures and the kinematic evolution of the overriding plate of a continental collision. We present new metamorphic petrology and coupled zircon geochronology and geochemistry data from the Jættedal complex in southern Liverpool Land to document the thermal evolution of the orogenic core of the southern GC. Pelitic migmatite gneisses from the Jættedal complex document metamorphic conditions of 850–730 °C at pressures of 11–9.5 kbar. Zircon from these samples yields Archean–Mesoproterozoic detrital cores with positive heavy rare earth element (HREE) slopes, and 440–425 Ma rims with flat HREE slopes are interpreted to date the timing of prograde pelite anatexis. Intercalated mafic assemblages record metamorphic conditions of 860–820 °C at 12–10 kbar. Zircon from mafic gneisses contains cores with ages of c. 458 Ma with positive HREE slopes and 413–411 Ma rims with flat HREE slopes that are interpreted to record the timing of original mafic dyke intrusion and subsequent partial melting respectively. When placed in the context of correlative rocks from the southern GC, these results suggest the development of a thermally weakened lower to middle crust in the Caledonian overriding plate that spanned >200 km perpendicular to orogenic strike during the Silurian. The existing data further suggest Silurian syn‐orogenic channel flow and exhumation occurred at the thrust front, while protracted high‐T metamorphism continued in the orogenic core. These patterns highlight variations in the thermal and rheologic structure of the Caledonian overriding plate along orogenic strike, and have implications for the development and exhumation of high‐ and ultrahigh‐pressure terranes.     

CS1000P6L型钻机在地表水平钻孔中的应用研究

通过对CS1000P6L型钻机主要技术参数的分析,认为其在0°～45°的倾角范围内实现岩心钻探施工具有一定的可行性。通过对钻机的主要部件——动力头的进一步研究后,选取了一个具体的项目进行了应用实验,针对实验过程中发现的问题,进行了认真分析并加以解决,从而验证了该钻机在0°～45°倾角条件下工作性能的可靠性。还通过对钻机在水平孔施工时的相关配套研究,不仅解决了施工人员的操作平台及钻杆钻具的摆放问题,还解决了钻机在工作中位移控制问题。实践证明,该设备完全可以在0°～45°的倾角范围内实现岩心钻探的施工工作,为该型设备的拓展应用提供了可靠依据,在岩心钻探领域具有良好的推广价值和现实意义。     

草鱼(Ctenopharyngodon idellus)呼肠孤病毒(GCRV)VP6相互作用蛋白的筛选

为筛选与草鱼呼肠孤病毒GCRV096 VP6发生相互作用的宿主蛋白,先将VP6基因的PCR扩增产物,克隆至酵母表达载体p GBKT7以构建其诱饵质粒(p GBKT7-VP6);再将酵母菌Y2HGold(含p GBKT7-VP6)与酵母菌Y187[含草鱼肾脏细胞(CIK)c DNA文库质粒]进行人工诱导融合,然后经选择培养筛选阳性克隆。结果共筛选到4株阳性克隆,经测序、生物信息学分析,分别属于两条不同的核苷酸序列,其中之一所编码的产物与GAPDH(3-磷酸甘油醛脱氢酶)同源性较高。可见,该酶极可能在GCRV096侵染宿主的初期发挥着重要作用。     

SPOT6遥感图像融合方法比较研究

SPOT6是2012年法国新发射的遥感卫星,具有空间分辨率高、数据采集能力强等特点,但目前在国土资源监管中,尚未形成完善的SPOT6数据处理技术体系。针对SPOT6卫星图像的特点,借助ENVI,ERDAS和PCI等遥感图像处理软件平台,选取相位恢复(Gram-Schmidt)变换法,高通滤波(HPF)法,超分辨率贝叶斯(Pansharp)法和Pan Sharpening法等4种图像融合方法进行融合对比实验,并从3个方面对融合效果进行了评价:首先对融合结果进行图像质量的定性评价;其次,构建了平均值、标准差、信息熵、平均梯度和相关系数等5个评价指标,对融合效果进行定量评价;最后,借助地物分类精度评价方法,进行了融合后图像的应用效果评价。分析结果表明,对于不同的应用要求,应选择不同的图像融合方法,以期达到最好的应用效果,从而为SPOT6图像在国土资源监管中的应用提供技术支持。     

山区地表太阳辐照度随时空变化的模拟分析

在光学遥感数据的应用过程中,地表太阳辐照度的量化问题对于遥感数据的获取和地表地物特性的反演等工作都是一个非常重要的环节,而地表太阳辐照度的定量计算又依赖于辐射源、目标物和传感器三者之间的几何关系以及目标地物的地表特征。利用山区地表太阳辐照度的计算模型,对不同时间、不同山区地形下的地表太阳辐照度进行了定量模拟,用三维图的方式分析了地表太阳辐照度随时间、地形坡度、坡向的变化规律,为光学遥感中地表太阳辐照度随时空变化的量化关系分析提供了更直观的依据。     

柴达木盆地大浪滩地区表层芒硝的形成时代及环境意义

通过对柴达木盆地大浪滩地区的两次实地勘查,发现小梁山多处可见芒硝—碳酸盐粘土互层的露头,选取了完整沉积的D26剖面进行研究。比较盐湖学的研究表明,芒硝是典型的冷相盐类矿物;而碳酸盐粘土和石膏则反映了相对温暖潮湿和温暖的环境。本文通过对芒硝—碳酸盐粘土互层的矿物鉴定,石膏的铀系不平衡法定年,以及结合碳酸盐粘土的碳氧同位素分析,首次揭示出大浪滩地区在倒数第二次冰期（MIS 6阶段）前后经历了偏暖潮湿期（＞195.1 ka BP）→寒冷干旱期（195.1 ~ 169.9 ka BP）→偏暖湿期（169.9 ka BP ka BP）→冷暖交替时期（169.9 ka BP ~ 118 ka BP）→偏暖湿期（118 ka BP）的气候演变序列。经与黄土剖面,深海氧同位素和区域研究资料的对比表明,自中晚更新世以来,大浪滩地区不仅受到区域地质活动的影响,也与全球的气候变化同步响应。     

云南富源—弥勒1∶5万化探异常的发现及意义

1∶5万水系沉积物测量表明,该区属浅成低温热液型金多金属成矿区,除受构造控制外,岩浆岩、地层亦有控矿作用。金矿主要分布在裂谷带中,成矿潜力巨大,测区西部杨梅山中部支壁找铜金、东南部大得克找铅锌有较好前景。