铁路运输过程控制模拟实验系统中列车运行仿真模型的研究

阐述了一种基于离散事件系统模拟的列车运行仿真模型它综合考虑了列车运行过程中可能遇到的种种情况，在应用于铁路运输过程控制模拟实验系统中，收到了很好的效果．     

基于RBF函数状态离散化的激励学习

介绍了激励学习和两类学习算法：Q学习和SARSA学习，提出一类基于RBF函数的特征状态离散化方法，并对该方法进行了初步的实验比较．     

江西高等职业教育发展趋势分析及对策

江西高等职业教育从八十年代初发展至今,取得了可喜的成绩,面对江西经济的高速发展,面对江西高等职业教育发展的新形势、新环境,及时明确江西高等职业教育的发展趋势,并采取相应的措施是非常有必要的.本文对江西省高等职业教育的发展趋势进行了分析,并提出相应的措施和对策,促进江西高等职业教育的发展.     

高压静电场处理油菜种子的品质影响及模型探讨

研究了高压静电场处理种子在大田生长条件下的长期效应 .结果表明 ,较低电压的处理可提高硫甙含量显著降低含油量 ,而较高电压的处理可降低硫甙含量 ,极显著降低芥酸含量 .采用平面类脂双层模型分析外加高压静电场对植物细胞跨膜电位的影响 ,并探讨其微观机理 ,一定程度上可以解释相关的实验结果     

沙坡头铁路防护体系防护效益系统仿真研究

在风洞实验、野外观测的基础上，采用系统仿真方法，对沙坡头铁路风沙防护体系防护效益、结构配置、防护宽度进行了研究．风洞实验测定了流沙输沙率、栅栏阻沙率、草方格阻沙率、植被阻沙率，与风洞实验模型相似的野外观测，确定了风洞实验数据与野外观测数据转换系数．以风洞实验、野外观测数据为基础，对防护体系三种不同配置结构的防护宽度，进行了系统仿真研究，阻沙栅栏 草方格 植被的防护体系结构防护宽度90-95m，阻沙栅栏 草方格的防护体系结构防护宽度100-105m，2道阻沙栅栏 草方格 植被的防护体系结构防护宽度50-55m，可以达到流沙输沙与防护系统阻沙量理论平衡，研究所得结论对风沙区交通线路防护体系设计具有借鉴意义，所采用的方法，对风沙工程研究有普遍适用意义。     

Computer simulation for the precipitation process of Ni75Al7.5V17.5 alloy

The precipitation mechanism of Ni75Al7.5V17.5 alloy above the L12 instability line, between the L12 and D022 instability lines and below the D022 instability line are studied using microscopic phase-field kinetic equation. This paper is aimed at investigating the effect of temperature on precipitation mechanism and morphological evolution of the alloy. Our simulations demonstrate that the precipitation is a mixed mechanism of non-classical nucleation growth and spinodal decomposition above the L12 instability line. It needs certain thermal fluctuations for nucleation and the number of θ phases is small at this temperature. The precipitation mechanism of γ'phase is congruent ordering followed by spinodal decomposition, and θ phase is a mixed mechanism of non-classical nucleation growth and spinodal decomposition between the L12 and D022 instability lines. The mechanism below the D022 instability line is similar to that between the L12 and D022 instability lines. With the decrease of the temperature, ordering and phase separation becomes fast, the dimension of γ'phase becomes small, the shape transforms from equiaxed to block, the dimension of θ phase becomes large and the shape transforms from strip to circle.     

Development of the CAS-IBB single-particle microbeam for localized irradiation of living cells

A single-particle microbeam facility has been constructed at the Key Laboratory of Ion Beam Bioengineering (LIBB), Chinese Academy of Sciences (CAS). The system was designed to deliver a defined numbers of hydrogen ions, produced by a van de Graaff accelerator, in an energy range of 2.0-3.0 MeV, into an area smaller than that of the nucleus of an individual living cell. The beam is collimated by a borosilicate glass capillary that forms the beam-line exit. An integrated computer program recognizes the cells and locates them one by one over the microbeam exit for irradiation. We present technical details of the CAS-LIBB microbeam facility, particularly on the collimator, hardware, control program, as well as cell irradiation protocols available. Various factors contributing to the targeting and positioning precision are discussed along with accuracy measurement results.     

盐岩储库腔底堆积物空隙体积试验与计算

受建库盐层本身地质特点影响,造腔结束后,底部一般会堆积大量不溶物。堆积物的存在既浪费了有效库容体积,又为整体建库施工带来了诸多不利因素。为科学评价该堆积物并进行有效处理或转变利用以增大库容体积,对其分布特征及堆积空隙体积进行了研究。通过室内溶腔实验获取了堆积不溶物样品,采用筛分法实验测定了其颗粒分布,并根据分形分布理论对其粒度分布特征进行了分析,进而基于可压缩堆积模型对堆积空隙体积进行了数值及模型研究。应用实例进行计算并与现场数据进行了对比评价验证,结果表明,在双对数坐标系下,腔底堆积物颗粒尺寸与累积数量呈线性相关,即其粒度分布可用分形分布函数进行表征,且分形维数作为分布特征参量能较好地描述颗粒均匀程度与集中性。     

钴掺杂对二氧化钛晶粒尺寸及相变的影响

通过溶胶凝胶法制备了纯Ti O_2与不同Co浓度掺杂的Ti O_2纳米粉体,并对样品进行了450、550、650℃保温2 h的热处理.采用X射线衍射仪对制得的纳米粉体进行了晶体结构表征,研究了热处理温度以及Co掺杂浓度对Ti O_2晶粒尺寸以及锐钛矿金红石相变的影响.结果表明:纯Ti O_2与Co-Ti O_2在450℃时为单一的锐钛矿;550℃时,纯Ti O_2有微量金红石生成,Co-Ti O_2仍然全部为锐钛矿;650℃时纯Ti O_2大部分转变为金红石,当Co掺杂量较低时,Co能促进锐钛矿相向金红石相的转变,而当掺杂浓度为8%时,Co抑制锐钛矿相向金红石相的转变;热处理温度升高以及Co掺杂浓度增加有利于Co Ti O_3相的生成,相同温度下,Co掺杂后Ti O_2晶粒尺寸减小.     

Benthic foraminiferal δ~(13)C minimum events in the southeastern Okhotsk Sea over the last 180 ka

A total of six d13C minimum events,i.e.,VI,V,IV,III,II,and I,were observed via a stable carbon and oxygen isotope analysis of infaunal benthic foraminifera Uvigerina spp.in gravity core OS03-1 in the southeastern Okhotsk Sea over the last 180 ka.These events occurred at112–109,102–90,85–76,57–54,44–40,and 17–10 ka BP.The largest negative excursions reached 2.5%in event V and were greater than 1%in the other events.We proposed that all d13C minimum events were caused by the increase in sea surface water productivity,the weakened formation of Okhotsk Sea intermediate water,and the enhancement of the oxygen minimum zone.The negative excursions were unaffected by methane hydrate destabilization and subsequent methane release based on the results obtained by using archaeal lipid markers.