HTD-3型高温堵漏材料研制及性能评价

深海钻探往往伴随着高温、高压,对钻井用堵漏材料提出了新的要求。首先通过对颗粒状、纤维状和片状堵漏材料的耐高温筛选,制作了HTD-3型高温堵漏材料。然后使用DL-3A型高温堵漏评价仪器对该堵漏材料的抗温、承压和封堵性能进行了测试,利用SEM电镜扫描对堵漏材料架桥情况进行了观察和分析,最后以5%梯度浓度进行了配伍性实验。测试结果表明,HTD-3型高温堵漏材料除对钻井液密度影响稍大外,对钻井液其他基本性能影响较小,在该材料中,不同级配的颗粒状材料完成了架桥,纤维状和片状材料完成了充填,形成了强度较高的封堵墙。通过实验证明：HTD-3型高温堵漏材料不仅有着较好的抗温、承压能力,还有较好的封堵效果。HTD-3型高温堵漏材料的研制为未来深海钻探堵漏提供了一种可行的选择。     

PVD and DCM columns combined ground improvement for embankment construction

Acta Geotechnica - Prefabricated vertical drains (PVDs) and deep cement mixing (DCM) columns combined ground improvement with a vacuum pressure for embankment construction on soft clay deposits has...     

皖东北地区农村民居抗震性能调查与研究

皖东北地区位于郯庐断裂带中南段附近,具备发生中强地震的构造背景.本文基于现场调查,并结合汶川地震的震害,对该地区农村民居的结构特点、抗震能力及地震安全农居示范工程现状进行了阐述,对农村民居抗震性能的薄弱环节及对策进行了探讨,以期为该地区抗震设防工作提供参考.     

“天绘一号”卫星工程建设与应用

概括“天绘一号”卫星工程的建设历程和卫星系统的使命任务;介绍了卫星系统和相机载荷的能力与技术参数;重点阐述了“天绘一号”卫星无地面控制条件下的摄影测量关键技术, 包括LMCCD相机体制、航天摄影测量相机参数在轨标定技术以及无地面控制点条件的三线阵EFP影像平差技术等的运用, 通过工程实践, 达到了工程技术指标要求;最后介绍数据应用情况, 提出“天绘一号”卫星的发展设想, 为了解“天绘一号”卫星工程提供了基本参考。     

“天绘一号”卫星地面应用系统设计与实现

介绍了“天绘一号”卫星地面应用系统在中国航天测绘装备建设中的地位和作用, 重点介绍了“天绘一号”卫星地面应用系统的功能、组成、工作流程和产品设计, 以及系统的技术特点、实际运行情况以及测绘能力, 展示了数据处理成果, 为了解天绘卫星工程建设情况, 提供基本参考。     

新疆哈密土屋铜矿床地质和地球化学特征

土屋铜矿床是我国近年来发现的特大型斑岩铜矿床,其独特矿床地质背景和矿床规模已经引起国内外地质学界和矿业界的广泛关注;本文详细叙述该矿床的地质背景,对矿床的地质、地球化学特征进行系统研究和总结,对矿床的成矿作用动力学过程进行探讨。研究表明,该矿床成矿物质具有深部来源特征,而岩浆在侵位过程中受到上地壳物质一定程度的混染;成矿流体以岩浆水为主,天水和岩浆水的混合仅为少量;石英流体包裹体均一温度较低,但盐度较高;含矿斑岩体是多次脉动式侵位的,成岩时代主要集中于早石炭世(367～358 Ma);成矿时代为晚于成岩时代(347.3±2.1 Ma～322.7±3 Ma)。     

Collision criterion for two satellites on Keplerian orbits

This paper analyzes the collision possibility for two satellites on Keplerian orbits. Coplanar and noncoplanar cases are considered, respectively. For each case, the problem of collision possibility analysis can be solved through two steps: First, to determine whether there is any intersection point of the two orbits; if there is no intersection point, the conclusion can be given directly that collision never happens. Secondly, if the two orbits do intersect, the collision possibility in the given time-scale can be studied in terms of the relationship between the two orbital periods and time. Numerical simulations for both cases, each including several situations, are given to prove the validity of the proposed collision criterion.     

莱芜市矿山地质环境保护工作探析

莱芜市成矿地质条件较好,辖区内蕴藏了比较丰富的矿产资源,已发现矿产42种,探明储量的18种,是省内矿产资源总量较丰富,矿种配套较齐全的少数地市之一。近几年,莱芜市大力开展＂治乱、治散、治毁、治本＂工作,矿业开发走上规范化道路。     

Magnetic susceptibility as a proxy for rainfall: Worldwide data from tropical and temperate climate

The magnetic susceptibility of soils has been linked with climate, mainly through rainfall, by numerous investigators. For this study we assembled a worldwide dataset of 272 samples, both published and new, to determine the nature of the relationship between MS and rainfall. On a worldwide basis there is a crude relationship (r² = 0.265) between MS and rainfall. MS increases with increasing rainfall from about 200 mm/yr to 1000–1200 mm/yr. Above 1200 mm/yr, MS decreases as rainfall increases up to about 2000 mm/yr. Under arid and semi-arid conditions, below about 200 mm/yr of rainfall, MS and rainfall exhibit no relationship, likely the result of limited pedogenic activity.When tropical and temperate localities are analyzed separately, the correlation between MS and rainfall exhibits a dramatic improvement, r² = 0.568 and 0.520, respectively. For similar amounts of rainfall tropical localities generally exhibit lower MS values which may be related to differences in the seasonal variation of rainfall. Because the soil environment is highly variable, it is unlikely that a global or even regional equation could accurately estimate rainfall from MS. Using data from Morocco and Mali we demonstrate that local equations using only MS to estimate rainfall produce reasonable results, r² = 0.700 for Morocco and 0.611 for Mali. However, a single independent variable is unlikely to capture the variability of the complex soil system. To the local equations described above we experimented with adding several independent variables in addition to MS including diffuse reflectance spectral data (DRS), x-ray diffraction (XRD), and x-ray fluorescence (XRF). For DRS data, % reflectance and red, yellow, and near-infrared wavelengths appear important; for XRD illite and kaolinite counts are important whereas for XRF Fe₂O₃ is important. The addition of these other independent variables dramatically improves prediction quality. In the case of the Mali transect, estimating rainfall from these variables produces an r² that exceeds 0.9. Based on these data we conclude that MS has the potential to be a reasonable proxy of rainfall for mean annual precipitation values from 200 to 2000 mm/yr, especially if local equations are used. Predictions can be improved by including other independent variables that show sensitivity to climate and are related to MS through the chemistry of the weathering process; we included DRS, XRD, and XRF data with good results.     

内陆湖泊流域的化学风化及气候变化—以内蒙古岱海为例

利用湖泊沉积物中Rb/Sr值来反映受古气候制约的流域陆地化学风化率的变化，并恢复了岱海近400a以来以小冰期为特征的、具有100a准周期（经谱分析）的气候波动历史。通过磁化率、粘土矿物含量和种类的综合分析，确证了湖泊沉积物Rb/Sr值的变化可以用来重建流域内化学风化率与其相应的古气候演化过程，是湖泊沉积记录中具有比磁化率更明显气候意义的有效代用指标。