椭圆极化激光场驱动下氢原子发射高次谐波的特点

通过数值求解两维含时薛定谔方程,研究了在不同波长的椭圆极化激光驱动下氢原子发射高次谐波的特点,得到了氢原子所产生的高次谐波谱截止位置处发射效率随椭偏率的依赖关系.研究结果表明,在激光光强保持不变的情况下,激光波长越大,截止位置处谐波发射效率对椭偏率的依赖越强;而在相同的激光波长驱动下,随着激光光强的增大,氢原子高次谐波谱截止位置处的效率随着驱动场椭偏率的增大下降得更快.最后,利用不同波长下高次谐波发射效率随椭偏率的依赖关系,通过数值计算和拟合研究了电子波包在隧穿电离后的横向扩散速率,研究发现在谐波截止位置附近由ADK模型得到的横向扩散速率比数值求解两维含时薛定谔方程得到的结果约小17%,正是这种横向扩散速率偏小的原因导致由ADK模型计算的谐波发射效率随椭偏率的增大相对于实验结果来说下降的较慢,而数值求解两维模型原子得到的结果与实验结果一致.     

Al2O3对碱硅酸反应的影响

采用分析纯Al2O3和烧铝矾土，以玻璃砂为活性骨料，通过测定砂浆棒的膨胀率及用能谱仪分析砂浆棒中C—S—H凝胶的组成，研究了Al2O3对碱硅酸反应的影响，并分析了其机理。结果显示，Al2O3对碱硅酸反应也有较好的抑制作用。其机理可能为Al^3＋对C—S—H中Si^4＋的取代作用加强了C—S—H对碱的结合能力。     

Indian monsoon influences altitude effect of δ~(18)O in precipitation/river water on the Tibetan Plateau

The δ^18O variation in precipitation acquired from 28 stations within the network of Tibetan Observation and Research Platform （TORP） is studied, with the focus on the altitude effect of δ^18O in river water during monsoon precipitation in an effort to understand the monsoon influence on isotopic composition in annual river water. It is found that δ^18O in precipitation on the Plateau is influenced by different moisture sources, with significant Indian monsoon influence on δ^18O composition in plateau precipitation and river water. The δ^18O of water bodies in the monsoon domain is generally more depleted than that in the westerly domain, suggesting gradual rainout of southwesterly borne marine moisture in the course of long-distance transportation and lifting over the Himalayas. The lapse rate of δ^18O in river water with altitude is the largest during monsoon precipitation, due to the increased temperature vertical gradient over the southern Plateau region controlled by monsoon circulation. The combination of δ^18O in river water in monsoon （wet） and non-monsoon （dry） seasons shows a larger lapse rate than that in non-monsoon （dry） season alone. As the altitude effect of δ^18O in precipitation and river water on the Tibetan Plateau results from the combined effect of monsoon moisture supply and westerly moisture supply, the δ^18O composition and its altitude effect on the Plateau during monsoon seasons should be considered in the reconstruction of paleoelevation of the Tibetan Plateau.     

Chen混沌系统全局指数吸引集和正向不变集的构造性证明及应用

本文利用多个广义正定的Lyapunov函数,给出了Chen混沌系统的全局指数吸引集及正向不变集的构造性证明,解决了"Chen混沌系统是否也像Lorenz混沌系统一样,存在全局指数吸引集"这个长期悬而未决的公开理论难题.本文所提供的方法,对于研究其他形式的混沌系统具有一般性的示范和启迪作用.     

He^＋离子在啁啾激光和高频脉冲组合场中产生的单个阿秒脉冲

利用数值求解含时薛定谔方程的方法,从理论上研究了一维模型He＋离子在波长为1064nm的线性啁啾激光和高频脉冲形成的组合场中产生的高次谐波以及由这种高次谐波构造的阿秒脉冲特征.发现在组合场中,由于啁啾脉冲的作用和在适当的时刻加入了高频脉冲,不仅使高次谐波谱的平台区域能得到很大的扩展,而且谐波转化效率也得到有效地提高,当对第二平台区域的不同范围内高次谐波迭加都可得到单个阿秒脉冲,最短可达21阿秒.最后通过经典分析和时频分析解释了这种高次谐波展宽与阿秒脉冲发射过程的特点.     

利用两束同色激光场与中红外场形成的组合场驱动氦原子产生单个阿秒脉冲

提出了使用两束同色激光场与中红外场形成的组合场驱动一维氦原子产生单个阿秒脉冲的方法. 通过数值模拟研究了氦原子在组合场驱动下发射高次谐波的特点, 谐波谱的截止位置可以拓展到I_p+12.6U_p, 对第二平台区域不同范围内高次谐波叠加均能得到单个阿秒脉冲, 最短脉宽达42 as, 尤其是对平台区域的前端进行叠加, 不仅可以得到单个阿秒脉冲,而且与截止位置附近高次谐波构造的阿秒脉冲相比, 强度提高了3 个数量级. 经过经典和小波分析发现, 中红外场的加入不仅使高次谐波谱平台区域得到了扩展, 同时还抑制了电子长路径对高次谐波的贡献.     

Comparison of a new model with previous models for the low-latitude magnetopause size and shape

In this study, the advantages and the limitations of previous low-latitude magnetopause empirical models are discussed. In order to overcome their limitations and inherit their advantages, a new continuous function for the influence of the interplanetary magnetic field (IMF) Bz on the magnetopause, the Shue model function and the 613 low-latitude magnetopause crossings are used to construct a new low-latitude magnetopause model parameterized by the solar wind dynamic pressure (Dp) and IMF Bz. In comparison ...     

Delamination of lamellar phyllosilicate Magadiite

In this paper, a new delaminated mesoporous material was prepared by swelling the lamellar phyllosilicate Magadiite using cetyltrimethylammonium bromide and tetrapropylammonium hydroxide solution, followed by delamination under the cavitation of ultrasonic treatment. Various characterization tools including XRD, N2 adsorption, NMR, IR, SEM and TEM were employed to observe its structure and morphology. XRD results show that the delaminated material has no long-range crystalline order. Fur-thermore, not only high surface area is obtained, but almost half of it is external surface. The observation for the morphology further reveals that it is made up of the random stacking of single or few layers. All these characters show that this delaminated mesoporous material meets the requirements for application as support in the hydrotreatment of heavy molecules.     

Study of altitudinal lapse rates of δ18O in precipitation/river water with seasons on the southeast Tibetan Plateau

Seasonal δ^18O variation in water on the southeast Tibetan Plateau has been studied, showing the consistent variation pattern of δ^18O with altitude indicative of relevant atmospheric circulation processes. Study shows a similar variation pattern of fixed-site river water δ^18O with that of the precipitation δ^18O in southeast Tibet. δ^18O in regional rivers in southeast Tibet demonstrates a gradual depletion with increasing altitude, though the rates vary seasonally. The most depleted river ^18O occurs during the monsoon period, with the lowest δ^18O/altitude lapse rate. The river ^18O during the westerly period is also depleted, together with low δ^18O/altitude lapse rate. The pre-monsoon rivers witness the most enriched ^18O with least significant correlation coefficient with the linear regression, whilst the postmonsoon rivers witness the largest δ^18O/altitude lapse rate. Different coherence of seasonal δ^18O variation with the altitude effect is attributed to different moisture supplies. Though sampling numbers vary with seasons, the δ^18O-H linear correlation coefficients all reach the 0.05 confidence level, thus witnessing the variation features of δ^18O in seasonal river water due to the influence of atmospheric general circulation and land surface processes revealed from the altitudinal lapse rates.