应用概率统计评价航磁异常

近年来使用基于概率理论的数理统计方法解释物探资料已受到人们的关注,本文通过实例叙述了变质铁矿床区域预测中评价航磁异常所使用的信息量统计方法的原理、变量选择和步骤,并对成果作了分析。     

Wintertime Stratospheric Anomalies-Part I: Warm Pools

The stratospheric worm pools, called the 4-day wave also, are mainly the temperature anomalies in the polar regions of winter hemisphere. It will be shown that their occurrence, propagation speed and specific structure can be explained by the lower frequency coherent heating resulting from the wave interaction in the breaking layers of the stratosphere. Although their vertical phase slope is negligibly small, the warm pools cannot be considered as a barotropic anomaly.     

Life's origin: the cosmic, planetary and biological processes

From elements formed in interstellar furnaces to humans peering back at the stars, the evolution of life has been a long, intricate and perhaps inevitable process. Life as we know it requires a planet orbiting a star at just the right distance so that water can exist in liquid form. It needs a rich supply of chemicals and energy sources. On Earth, the combination of chemistry and energy generated molecules that evolved ways of replicating themselves and of passing information from one generation to the next. Thus, the thread of life began. This chart traces the thread, maintained by DNA molecules for much of its history, as it weaves its way through the primitive oceans, gaining strength and diversity along the way. Organisms eventually moved onto the land, where advanced forms, including humans, ultimately arose. Finally, assisted by a technology of its own making, life has reached back out into space to understand its own origins, to expand into new realms, and to seek other living threads in the cosmos.     

藏北南羌塘盆地毕洛错地区下侏罗统曲色组石膏岩层

对西藏自治区北部南羌塘盆地毕洛错地区下侏罗统曲色组石膏岩层进行了研究。根据岩石地层和生物地层资料,确认毕洛错地区的石膏岩层和油页岩为曲色组的一部分,地质时代为早侏罗世,并确认下侏罗统曲色组在区域上可能是寻找油气、油页岩资源的重要层位之一。     

南美洲7ka来古气候资料中的南方涛动信号

在南半球赤道地区，太平洋东部沿岸的海面温度相对较冷，这些冷水强烈地影响着赤道大陆气候，在由塔西提／达尔文间不规则的高／低气压所定义的南方诗动的减弱价段，这种气候背景型式强烈地受到改变，在南方涛动减弱阶段，厄尔尼诺事件可能会出现，赤道太平洋水团要比通常温暖。     

沿海地区城市发展及地面沉降的系统控制

本文运用系统工程原理,系统论述了地下水合理开发、管理和地面沉降系统控制,这对沿海地区地面沉降控制起到重要的作用。     

长期暴露于高压氮氧环境下人体二氧化碳通气反应的变化

本工作研究了36.5米和50米氮氧饱和暴露对人体二氧化碳通气反应的影响。用重复呼吸法测定了两组共13名健康男性受试者的二氧化碳通气反应。氮氧饱和条件下的氧分压维持在0.30绝对压左右,而测定通气反应时的吸入气中的氧分压是0.98绝对压,二氧化碳分压是0.07绝对压,其余为氮气。此外,还测定了受试者的终末潮气二氧化碳分压。实验结果表明:1.二氧化碳通气反应随压力升高而下降。2.二氧化碳通气反应曲线的截距在不同深度均未见有明显的变化。3.在高压条件下,静息状态的终末潮气二氧化碳分压比常压对照值有明显的增加。高压下的二氧化碳通气反应的下降和终末潮气二氧化碳分压的升高,在减压返回海平面后均能恢复到常压水平。高压下的这些变化,可能是呼吸中枢对二氧化碳敏感性的改变所致,也可能是由于呼吸阻力增加引起的呼吸功增加所致,或是两个因素叠加的结果。