跳跃项目起跳动作技术的共性原理--屏气紧身爆发用力

用运动生理学、运动生物力学的原理和方法，分析和研究跳跃项目起跳动作与屏气紧身爆发用力的活动机理。在教学过程中，根据跳跃项目起跳动作技术发力的形式和特点，恰当地结合屏气紧身爆发用力应激活动，以达到加快教学进程和提高教学质量的目的。     

奥灰水文地质条件研究与深部煤炭资源开发

以显德汪井田为例，在剖析奥灰水文地质条件的基础上，从定性与定量两个方面阐述了奥灰水与深部煤炭资源开发的关系，进而提出了奥灰水防治利用的初步设想。     

贵州早二叠世玄武岩喷发环境及其古海洋效应研究

二叠纪是中国南方火山活动较为强烈的时期之一,此时贵州省境内形成了大面积的玄武岩。文章通过岩石学、地球化学、大地构造学研究论证了早二叠世玄武岩喷发时为大陆裂谷环境,从宏观、微观岩石学特征确定了分布区东部的早二叠世玄武岩为海底喷发的产物,并详细研究了它对古海洋沉积学、古海洋地球化学的影响。     

Generation and evolution of cavitation in magma under dynamic unloading

The full system of equations for the problem of rarefaction-wave passage over the magma-melt column in the gravity field is derived with the use of the kinetic theory of phase transformations, and the problem is numerically solved. With allowance for diffusion zones and nucleation frequency as a function of supersaturation, the dependence of the number of cavitation nuclei formed in the course of phase transformations behind the rarefaction-wave front is found. The dynamics of the size distribution of cavitation bubbles along the magma-melt column (1 km) whose viscosity varies dynamically as a function of the concentration of dissolved water is studied.Translated from Prikladnaya Mekhanika i Tekhnicheskaya Fizika, Vol. 46, No. 2, pp. 71–80, March–April, 2005.     

云南腾冲热海热田中金和微量元素的分布特征

热海热田内热泉水和各类热水沉淀物中不同程度地富含Ａｕ、Ａｇ、Ａｓ、Ｓｂ、Ｈｇ、Ｔ１微量元素，金的富集与含黄铁矿的水热角砾岩、硅质泉华更为密切。热田内水热爆炸和沸腾作用广为发育，Ａｕ，Ａｇ、Ａｓ、Ｓｂ、Ｈｇ、Ｔ１微量元素组异常可能是热泉型金矿化浅部的地球化学特征。     

The influence of magnetic field on the physical explosion of a heavy gas cloud

Richtmyer–Meshkov (RM) instability arises during the eruption of heavy gas cloud. In this study, we numerically study the effects of magnetic fields on the RM instability induced by the ionised cylindrical and spherical heavy gas cloud eruption using corner transport upwind + constrained transport algorithm. Our numerical results show that magnetic fields can suppress the formation of spike and bubble structures induced by the eruption in both cylindrical and spherical cases. The magnetic pressure of the interface along the perpendicular direction of magnetic field is the main factor to control the distortion of the interface. Even weak magnetic fields can drastically alter the evolution of the cloud and result in different distributions and amplifications of the magnetic pressure, which will affect further transformation of RM instability during the ionised gas eruption. Meanwhile, the magnetic pressure on the interface decreases gradually when the initial magnetic field is relatively large; when the initial magnetic field is small enough, the opposite results will occur.     

断陷盆地“不对称”火山岩喷发特征与有利储层主控因素探讨

通过大量钻井资料及地震资料的对比研究, 建立松辽盆地不对称火山岩喷发模式, 指出火山岩在断层高部位向低洼区流动, 高部位一翼延伸规模小, 低洼区延伸规模大。在对全区257口钻遇火山岩探井统计的基础上, 明确了火石岭组和营城组火山岩的分布规律, 认为酸性火山岩是优势储层岩类; 火山岩岩相控制优质储层的分布, 近火山口不对称的酸性爆发相为火山岩有利储层发育相带; 裂缝是深部流体运移的重要通道, 能改善渗透条件, 促使次生孔隙发育, 是高产气藏形成的关键, 高角度裂缝和溶蚀孔隙组合带是火山岩储层发育的有利区带。此外, 建设性的成岩表生作用是优质储层形成不可忽视的因素。     

峨眉山绿豆岩的应用及其成因探索

该文对峨眉山龙门洞三叠系中统雷口坡组底部“绿豆岩”运用多种分析手段,了解绿豆岩的物质成分及其在农业上的应用。并结合野外观察,对其形成环境及成因进行初步探索。     

The 4700 aB.P. volcanic signal detected in Vostok BH8 ice core, Antarctica

The detailed electrical conductivity measuremerit （ECM）, trace chemical compositions and microparticles concentration analysis are performed for BH8 ice core from the depth of 126.0m to 130.0m at Vostok Station. At depth 128.7m, a volcanic signal 4726 a B.P. is detected. The volcanic sulphate flux is 95.8 kg·km^-2, sulphate peak concentration 1352.8 ng·g^-1, duration time about 10.1 years, comparable with some well-known volcanic events. The results indicate that it seems to be a relatively large scale, long lasting volcanic signal with farther volcanic origin.