复苏促进因子辅助单细胞分离筛选青藏高原低温联苯降解潜力菌

微生物资源的挖掘一直是研究关注的重点.在传统微生物分离培养中,因优势菌群竞争及培养条件限制等原因,存在庞大的不可培养微生物群体,单细胞分离培养可排除种间竞争的影响,添加复苏促进因子蛋白可提高低活性、慢生长微生物的分离效率.青藏高原拥有着巨大的微生物资源储备量,同时也因为脆弱的生态环境而受到原油、持久性有机污染物等的威胁,在高原长期的低温条件下,挖掘本土微生物资源对冷环境污染修复具有重要意义.本研究利用单细胞分离与复苏促进因子添加培养相结合的方法,从青藏高原不同海拔表层土壤样品中,分离培养低温联苯降解潜力菌,并探究分离菌株对复苏促进因子的响应情况.共获得24株可在低温条件下以联苯为唯一碳源生长的菌株,其中18株来自复苏促进因子添加组,分属于Microbacterium等9个属,多数筛选菌株对复苏促进因子的响应明显.本研究建立了一种新的功能菌分离筛选方法,具有高效率、低成本、易推广的特点,为“微生物暗物质”挖掘提供了一种新方案.     

增升装置中的流动控制技术

阐述了襟翼涡流发生器、主翼后缘偏折技术、Zhu’s襟翼、自激励运动襟翼、零质量射流、等离子体技术以及动力增升等各类主动控制技术的工作原理及其增升效果分析和具体应用情况.结果表明,这些流动控制新技术对于进一步提高民用飞机的增升效果具有巨大的潜力.     

青藏高原生态环境恶化及其影响

青藏高原东西长约2700千米，南北宽约1400千米，面积约240万平方千米，平均海拔高度4500～5000米，是我国最大的高原，也是世界上最高的高原，有“世界屋脊”之称。     

500kV并联电抗器升流

针对目前500kV并联电抗CT二次回路检查的现状,分析了可采用的两种方法,并着重介绍了一次升流的方法,同时也对未来电流二次回路的发展作出了预测。     

高原鸟岛

在我国的青藏高原上,有一个很神秘的湖泊,那里水天一色,群鸟飞翔,就如天使的国度,它就是我国内陆的第一大湖——青海湖。 青海湖位于青海省共和县西部,面积约4635平方千米,平均水深19米。这里是青海省最大的自然风景区,每年都吸引数以万计的国内外游客前来观光揽胜。     

A high-resolution environmental change record since 19 cal ka BP in Pumoyum Co,southern Tibet

A 380-cm-long sediment core was acquired from the deep water area of Pumoyum Co, southern Tibet. Twenty-five plant residue samples were selected, and organic carbon stable isotopes were obtained using the AMS ¹⁴C chronological method. The ¹⁴C age and carbon reservoir effect were calibrated with surface sedimentation rate measurements using ²¹⁰Pb dating. Results showed that the core sediment deposited over 19 cal ka BP. Based on a multi-proxy analysis of TOC and IC contents, grain size and pollen assemblage data, the palaeoclimatic evolution of Pumoyum Co was reconstructed since the last glacial. Pumoyum Co was a shallow lake prior to 16.2 cal ka BP; although the glacier around the lake began to melt due to increasing temperatures, climate was still cold and dry. In the interval of 16.2–11.8 cal ka BP, the sedimentary environment fluctuated drastically and frequently. Two cold-events occurred at 14.2 and 11.8 cal ka BP, and these may correspond to the Older Dryas and the Younger Dryas events, respectively. After 11.8 cal ka BP, Pumoyun Co developed into the deep lake as it is now. The lake water temperature was relatively lower at that time because of influx of cold water from glacial meltwater entering the lake. As a result, the multi-proxy indicators showed no sign of warm conditions. Comparisons between the sedimentary record of Pumoyum Co with that of other lakes of the same age in southern Tibet indicate a warmer climate following the last deglaciation influenced the southeastern Tibetan Plateau. These results imply that the southwest Asian monsoon gradually became stronger since the deglaciation during its expansion to the inner plateau. The glacial-supplied water of the lake responded sensitively to cold-events. The entire southern Tibet region was dominantly influenced climatically by the southwest Asian monsoon during the Holocene.     

奇特的藏族水文化

在藏族文化中。其中的水文化占有较大比重。水广泛存在于青藏高原的神山圣迹之间．水神则活跃在藏族民众的精神世界里。西藏除了有四座神山外,还有三个备受广大藏族同胞崇敬的圣湖：玛旁雍错湖、纳木错秋莫和羊卓雍错。这三个湖是全藏的守护神。西藏的山山有神,湖湖有龙,听藏族老人们说,雪域的每座山、每个湖,甚至每块石头,都是有灵魂的。     

新生代全球变冷背景下北部青藏高原变冷和干旱化事件:西宁盆地早第三纪沉积物中正构烷烃和孢粉的记录

位于青藏高原西北部的西宁盆地沉积了年代序列跨度非常长的连续的新生代地层. 这些地层序列记录了有关青藏高原隆升历史及其相关气候变化的丰富信息. 本研究获得了西宁盆地谢家剖面较高分辨率的正构烷烃生物标志化合物和孢粉记录. 整合正构烷烃和古孢粉记录揭示: 在50.2~28.2 Ma 之间, 西宁盆地经历了长期的降温过程, 明显的生态事件发生在 37.5~32.7 Ma 之间. 自此盆地中的植被呈现显著的垂直地带性变化: 较低海拔处生长旱生灌草类植物, 中海拔地带生长亚热带阔叶树, 高海拔带生长针叶林. 这些植被和气候的变化有可能是对始新世早期气候最适宜期之后长期的全球降温事件和早新生代北部青藏高原周围山地隆升事件的共同响应.