两高切变型四川盆地大暴雨天气过程机制研究

利用常规观测和EC数值模式资料,对2020年8月12～13日四川盆地大暴雨天气的环境条件、水汽条件、能量条件、不稳定层结、MCS系统演变进行分析。结果表明：本次盆地大暴雨属于“两高切变”型,是在高能高湿环境条件下,北方干冷空气入侵盆地触发锋线对流系统,盆地南部受地形强迫抬升影响触发对流系统,在高空切变线上合并加强,造成四川盆地大暴雨过程。贵州高原的强水汽输送是此次大暴雨的重要水汽条件,对流云团合并加强是造成局地特大暴雨的重要特征。基于EC数值模式资料分析的盆地暴雨落区比实况探空更加清晰。     

Swift时代伽马射线暴的观测和理论

伽马射线暴是宇宙中最剧烈的爆发现象之一.Swift卫星的快速定位和Fermi卫星的宽、高能段观测,使得伽马暴的观测可以全波段进行.通过Swift的观测可以对伽马暴现象的本质有进一步的理解,而Fermi卫星提供了一些暴高能光子的辐射数据,为进一步研究暴的辐射机制和伽马暴以及它的余辉提供了有力的依据.介绍了Swift和Fermi卫星发射后一些伽马暴的观测和理论研究进展.     

耀变体3C 273在2～10keV的光变特性研究

从RXTE(Rossi X-ray timing explorer)观测原始数据出发,分析了耀变体3C 273在X射线波段2～10 keV从1996年2月2日(MJD 50115)到2007年8月27日(MJD 54339)的数据.一共得到了1 010次观测数据的光子谱指数和相应的流量,平均每次观测时间为1 666.76 s.通过分析3C 273在观测期间2～10 keV硬X射线的能谱变化及光变行为,发现在2000年2月,2003年3、4月,2004年2、3、7月,2006年及2007年,其光子谱指数Γ与流量lgF_(2～10 keV)存在显著反相关.在1999年和2000～2007年观测期间,Γ与lgF_(2～10 keV)月平均行为也同样存在显著反相关.对整个观测期间的光变行为作定量的分析,发现几次较大的光变,并在部分光谱拟合中发现Fe发射线存在的证据,其平均宽度为93.85±21.49 eV.通过分析光变强度与Fe发射线特性,发现3C 273同时具有耀变体与Seyfert星系的一些性质.     

关于Fe-C(H)系高温高压合成金刚石多晶形成机制的一些思考

Fe-C(H)系高温高压金刚石多晶在合成片上呈成堆聚集状、不均匀分布.多晶中的金刚石晶粒多为八面体晶形、随机定向、大小无规律,表面发育"锯齿状"生长台阶,普遍发育塑性形变等缺陷.多晶中的金刚石晶粒间接触界线清晰、呈突变状.无论是利用品体成核、还是晶体长大理论都只能解释多晶中存在的部分现象.利用碳原子配位四面体生长基元模型分析多晶的形成机制值得探索.深入分析Fe-C(H)系高温高压合成金刚石多晶的形成机制不但有利于改善金刚石合成的工艺、提高合成金刚石多晶的品级.而且有利于为人们探讨天然金刚石多晶的形成机制及其深部意义提供科学线索.     

多部委打出“组合拳” 进一步加强楼市调控

对于国家有关部委近日出台多项措施加强楼市调控,打出＂组合拳＂进一步遏制部分城市房价过快上涨,促进房地产市场的健康发展。全国工商联住宅产业商会会长聂梅生在接受中新网房产频道访问时指出,要实现全方面的楼市调控效果,仍需要从体制和机制等方面加大改革力度,措施的出台将使保障性住房政策更为明朗。     

坚定信心 迎接挑战 以机制创新失去资源利用方式和发展方式转变--全国国土资源厅局长座谈会纪实访谈录

一场罕见的浓雾并没有影响全国国土资源厅局长座谈会的如期举行。7月4日,经过两天半的紧张议程,会议落下帷幕,来自全国各省（区、市）国土资源系统的厅局长们带着收获的喜悦,沐浴着灿烂的阳光返程。正在艰难爬坡的国土资源管理工作,仿佛被注入了奋力前行的新活力。     

集体土地所有权登记发证工作中遇到的问题及解决建议

党的十一届三中全会《关于推进农村改革发展若干问题的决定》明确提出：“健全严格规范的农村土地管理制度。……搞好农村土地确权、登记、颁证工作”。天津市于2007年下半年开展了第二次土地调查集体土地所有权登记发证工作。在原土地详查的基础上,由集体土地所有权人提出土地登记申请,经宗地相关的权利主体对宗地界址进行确认、     

以科学发展观为统领 不断探索构建国土资源节约集约利用新机制

节约集约利用国土资源是贯彻落实土地基本国策的长远要求,也是贯彻中央加快经济结构调整和发展方式转变战略部署的现实要求。近几年来,辽宁省坚持以科学发展观为统领,把节约集约作为国土资源改革创新的主线,以资源利用结构调整促进经济结构调整,以资源利用方式转变促进经济发展方式转变。不断探索构建土地资源节约集约利用和矿产资源合理开发利用的新机制。     

Evolution of isotopic compositions in groundwater of the area between the Gulf of Oman and the Arabian Gulf

The stable isotopes of oxygen and hydrogen have been implemented to assess the recharge mechanisms in an area in the UAE bounded to the northwestern part of the Gulf of Oman and the southeastern part of the Arabian Gulf. The conversion of stable isotopes to deuterium excess was utilized as a supportive tool to understand the process of groundwater recharge. The concluding results of this study showed that the origin of moisture is the Mediterranean Sea. The precipitation is the main source of recharge, in which the precipitation having undergone evaporation before recharge occurs. The comparison between regression line for data collected in 1996 and regression line for samples collected in 2006 suggests that the precipitation water which recharged the groundwater, was diluted with groundwater and this dilution is observed from decreasing of the deuterium excess of collected groundwater samples with increasing isotopes of oxygen. The dilution of groundwater with the recharge water suggests modern-day recharge as it is seen from high deuterium excess that exceeded the deuterium excess of LMWL and was close to MMWL.     

Metallogenic mechanisms of super-large Cu and Au deposits in the Dexing region and simulating experiments

Based on the results of previous studies and under the direction of the theory of “ore deposit genesis”, the authors made use of high temperature and high pressure experimental facilities and conditions at the Tectono-geochemistry Research Room under the State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, and put the focus on the multi-source of tectonically controlling ore-forming materials, the characteristics of multi-stage and multi-episode hydrothermal activities and mineralization and the characteristics of multi-genesis and multi-ore deposition so as to shed light on the metallogenic mechanisms of super-large Cu and Au deposits. In addition simulating experiments were made on multi-stage and multi-episode tectonic activities and rock and ore deformation, multi-stage and multi-episode tectonic activities and mobilization and migration of ore-forming materials, and multi-stage and multi-episode tectonic activities and superimposition and enrichment of ore-forming materials. The experimental results showed that under the action of multi-stage and multi-episode tectonic stress the deformation and fragmentation of not only rocks and ores have been intensified, and but also the ore-forming materials originally disbursed in the rocks and ores have been mobilized and migrated and superimposed and enriched. The experimental results also provided the scientific experimental data and grounds for deep-going research on the rules of metallogenesis and geneses of super-large ore deposits in the Dexing region, Jiangxi Province.