新疆克拉玛依市商业地价空间分布规律研究

城市地价是一个具有时空性质的多维概念,在空间分布上具有较强的关联性和特殊性。但目前对城市地价空间分布规律方面的研究相对较少,还没有形成系统性的理论与方法依据,本文以克拉玛依市2007年土地调查商业用地数据和地价动态监测数据为依据,以ARCGIS软件为平台,采用地统计学的方法,对克拉玛依市商业用地价格的空间分布进行了研究。研究表明:地统计学的理论与方法对城市地价空间分布进行研究具有独特的优越性;城市商业用地地价的分布在空间上既有连续性,也存在变异性,受区域整体趋势的影响明显高于小范围的变异性,属于强空间自相关;商业用地地价分布整体呈现圈层结构,交通道路对地价的空间分布具有重要影响。     

青藏高原盐湖卤水中溴的分布特征及来源初探

溴是完备工业体系的关键必备元素。盐湖卤水是溴的重要来源。青藏高原盐湖众多,富含钾、锂、硼等资源元素,开发潜力巨大。然而,目前针对青藏高原盐湖溴浓度、分布特征及其物源的研究仍然薄弱。本次研究采集了26个青藏高原盐湖表卤水样品并分析其溴浓度,进一步总结其他64个已报道盐湖数据,系统分析了青藏高原盐湖溴浓度分布特征,并进一步探讨了溴的可能物源。结果表明:青藏高原盐湖表卤水溴分布在0.5～246.8 mg/L之间,平均为41.1 mg/L,其中,碳酸盐型盐湖卤水平均溴浓度最高(47.0 mg/L),且集中分布在高原南部,而氯化物型盐湖平均溴浓度最低(30.1mg/L),盐湖溴浓度呈现自南向北降低的趋势;青藏高原盐湖中溴有多种来源,高原南部富溴盐湖溴的来源可能主要与热泉补给有关,而柴达木盆地盐湖高溴来源可能主要与深部地层水(如油田水、背斜构造裂隙孔隙水、砂砾孔隙卤水、气田水等)补给有关。     

桂林岩溶盆地第四纪粘土砾石层沉积与漓江袭夺

通过对桂林岩溶盆地内第四纪粘土砾石层调查研究,认为:①粘土砾石层成因不属冰川沉积或湖相沉积,而是山地河流相沉积和再沉积产物。前者时化属中更新世,后者成因复杂,已发现坡积相、洪积相,时代属晚更新世;②漓江溯源侵蚀过程中发生多次袭夺;③岩溶盆地的发育与漓江袭夺控制和影响粘土砾石层的沉积和再沉积。     

近江牡蛎的染色体组型

以近江牡蛎的担轮幼虫为材料,采用秋水仙素——低渗处理——空气干燥制片法制作染色体标本,对其核型进行分析,结果表明,近江牡蛎体细胞染色体数目2n=20,NF=40,核型公式为20m。     

Analytical scanning and transmission electron microscopy of laboratory impacts on Stardust aluminum foils: Interpreting impact crater morphology and the composition of impact residues

Abstract— The known encounter velocity (6.1 kms^?1) and particle incidence angle (perpendicular) between the Stardust spacecraft and the dust emanating from the nucleus of comet Wild‐2 fall within a range that allows simulation in laboratory light‐gas gun (LGG) experiments designed to validate analytical methods for the interpretation of dust impacts on the aluminum foil components of the Stardust collector. Buckshot of a wide size, shape, and density range of mineral, glass, polymer, and metal grains, have been fired to impact perpendicularly on samples of Stardust Al 1100 foil, tightly wrapped onto aluminum alloy plate as an analogue of foil on the spacecraft collector. We have not yet been able to produce laboratory impacts by projectiles with weak and porous aggregate structure, as may occur in some cometary dust grains. In this report we present information on crater gross morphology and its dependence on particle size and density, the pre‐existing major‐ and trace‐element composition of the foil, geometrical issues for energy dispersive X‐ray analysis of the impact residues in scanning electron microscopes, and the modification of dust chemical composition during creation of impact craters as revealed by analytical transmission electron microscopy. Together, these observations help to underpin the interpretation of size, density, and composition for particles impacted on the Stardust aluminum foils.     

镇泾地区延长组长8油层组基准面旋回与储层非均质性的关系

本文运用高分辨率层序地层学理论,对镇泾地区延长组长8油组储集砂短期基准面叠加样式以及储层非均质性特征进行分析,建立了6种不同的非均质模式;探讨了不同级别的基准面旋回对储层非均质性特征的控制作用,短期旋回控制了储层的层内非均质性特征,中长期旋回控制了储层的层间非均质性特征。     

盐定地区三叠系延长组层序地层特征与生储盖组合

依据地表露头、钻井岩心、测井曲线和地震资料的综合分析,在识别了盐定地区层序界面的基础上,将研究区上三叠统延长组划分为1个超长期、4个长期旋回层序.详细论述了各长期基准面旋回的地层堆砌样式和充填特点,建立研究区高分辨率层序地层格架.对层序与生储盖组合特征进行了详细分析,指出生储盖组合特征与长期基准面旋回关系密切,生油岩和储集层明显受基准面升降和可容空间变化的影响,在长期基准面旋回升降转换面附近是生油岩和盖层发育的有利位置,优质储层主要出现在长期基准面上升半旋回的早中期和下降半旋回的中晚期.在此基础上讨论了研究区上生下储、下生上储的生储盖组合特征.     

古玉器的化学风化机理初探之二——块状模拟实验

在前文粉末态模拟实验基础上,初步模拟古玉埋藏的酸性以及碱性环境,通过对不同材质玉料的块状形态在酸、碱缓冲溶液中的浸泡实验,并与粉末态玉料的浸泡结果进行对比分析,以深化对古玉器风化机理的认识。     

陆地声呐法在探查单个溶洞方面的优势

基于地震反射法的陆地声呐法,在预报探查溶洞等方面成功地进行了2个工区的工作,取得了很好的效果,这是由于其接近于零震-检距的工作布置,用锤击激震可接收10~4 000 Hz的超宽频带的接收等特点所决定。无论在地面上探查中、小溶洞方面(查找的溶洞径深比可小于1∶15),还是在隧道施工地质预报方面都有很大优势。     

Effect of brittle fracture on the rheological structure of the lithosphere and its application in the Ordos

An empirical formula for the fracture strength of the principal rock type in the lithosphere is obtained based on the experimental data from previous studies, in which the effects of the confining pressure, size of the rock sample, temperature, strain rate and the pore pressure are taken into account, the empirical formulae for the effects of them are also presented. By comparing the frictional strength to the fracture strength calculated using the new empirical formula, it is shown that frictional sliding is dominant in the upper crust but brittle fracture is dominant in the lower part of the crust and the lithosphere beneath the crust. Therefore the fracture mechanism must be taken into account in the study of the rheological structure of the lithosphere. The empirical formula for the fracture strength is applied to study the rheological structure of the lithosphere in the Ordos block. Brittle regime in the rheological structure can be divided into two sub-regions, in one of which brittle fracture and in the other frictional sliding are dominant, respectively, unlike previous conventional studies in which frictional sliding is assumed to be the only factor; the magnitude of the rheological strength of the lithosphere calculated by the empirical formula is also lower than that obtained in previous conventional studies.