迎接新时期地质科技革命

当今世界地质科学技术的进步,特别是高新技术在地质工作中的广泛开发和应用正深刻地改变着地质工作的面貌.新世纪,我国地质工作要实现持续、快速、健康发展,必须依靠地质科学理论的不断创新和技术的不断进步.     

银河系分子云总体性质的研究及恒星形成区成协天体的探测

综述了作者通过＾１３ＣＯ观测示研究银河系分子云总体特征和展示大尺度结构，以及探测恒星形成区新成协天体。评述了研究结果及其应用和有关研究课题的深入与发展，并与同类工作作了比较。     

西藏高原大气折射指数的时空分布

利用西藏高原上四个站常规探空资料，应用大气折射指数理论和统计学方法得出：利用两层指数模式拟合实际的大气折射指数垂直分布可保证精度。由于地面气象要素日较差、年较差较大，折射指数日变化、年变化在对流层低层幅度最大。气压、温度、水汽压的分布、变化决定了折射指数的分布变化，不论日际变化，还是年际变化，水汽压都占主导地位。     

Detection and Monitoring of New-Ice in the East Greenland Sea Using the SeaWinds Scatterometer

Space borne radar scatterometers are primarily designed to measure the wind vector over the world ocean; yet they also provide useful information on sea ice type and extent. In this paper, it is shown how the SeaWinds scatterometer can be used to detect new sea ice at the very beginning of its growth. Taking advantage of the very good coverage of the East Greenland Sea by SeaWinds on board the QuikSCAT satellite it has been possible to detect the early stage of formation of the sea ice peninsula, named the Odden, and to monitor its evolution during March 2001. The early sea ice detection has been validated by using RADARSAT Synthetic Aperture Radar scenes. It is also shown that microwave radiometers, such as the Special Sensor Microwave Imager (SSM/I), which are used as standard sensors for sea ice monitoring, do not detect the very early stage of sea ice growth and lag behind new sea ice occurrence by about twelve to twenty four hours.     

Centrifuge modeling of PGD response of buried pipe

A new centrifuge based method for determining the response of continuous buried pipe to PGD is presented. The physical characteristics of the RPI‘s 100 g-ton geotechnical centrifuge and the current lifeline experiment split-box are described: The split-box contains the model pipeline and surrounding soil and is manufactured such that half can be offset, in flight, simulating PGD. In addition, governing similitude relations which allow one to determine the physical characteristics, (diameter, wall thickness and material modulus of elasticity) of the model pipeline are presented. Finally, recorded strains induced in two buried pipes with prototype diameters of 0.63 m and 0.95 m (24 and 36 inch) subject to 0.6 and 2.0 meters (2 and 6 feet) of full scale fault offsets and presented and compared to corresponding FE results.     

IGCP448：岩溶生态系统全球对比研究进展

综述了IGCP 448项目"全球岩溶地质及有关生态系统对比"(2000-2004)执行四年来所取得的学术成果.其中比较重要的新认识有:(1)岩溶地区的植被,常常是涵养水分,增加含水层的贮水能力,改善水文生态环境的重要因素,但在澳大利亚南部岩溶区广泛分布的桉树,则以其强烈的蒸发作用,而被用于降低地下水位,防治土壤盐碱化;(2)在北方(Boreal) 或温带湿润气候生态区,地下岩溶系统则被用于排除沼泽地区过多积水,偏碱性的碳酸盐岩也有利于中和酸性环境,凡是岩溶发育的地方,都成了主要农业基地;(3)通过洞穴探险发现一类完全不同于靠光合作用产生有机质的生物群--化学自养微生物(甲烷菌);(4)中国西南典型岩溶区的研究表明,表层土壤微生物可以加速碳酸盐岩的溶解作用,并揭示了植物根系与土壤微生物是产生碳酸酐酶(CA)的两个重要供给源.     

试论地下热水的铀成矿作用

The studies uranium deposit occurs in a geothermally abnormal area. It has the following four features: 1. Uranium mineralization is observed in a certain temperature zone. 2. The uranium deposit occurs in an area characterized by relatively low but highly varying radioactivity in a regionally high radioactive field. 3. Uranium closely coexists with cubic pyrite of hot water origin. 4. Pitchblende is characteristic of hot water origin. This paper focuses on the relationship between ground hot waters and uranium mineralization. Uranium in the deposit is considered to have come from the host rocks, The possible explanation of the formation of this uranium deposit is that uranium was first leached out of the host rocks by ground hot waters and then transported to where uranium enrichment and deposition were favoured, forming uranium deposit under certain conditions. Based on this explanation, this uranium deposit is believed to be the product of hot water activity in the regionally geothermal abnormal zone.