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81.
从试验模型、试验材料、试验装置及测试内容等方面制定了工程弃渣型坡面泥石流试验方案,拟定了模型试验过程,降雨历时16-18 h,其中0~13h属于前期降雨阶段,降雨强度控制在6.8 mm/( 10 min),分4次完成,每次降1h,停2h;13h以后属于短历时强降雨阶段,降雨强度控制在16.7 mm/(10 min);分... 相似文献
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电力电子变换装置的重要发展方向是高电压大容量,多电平变换装置以电力电子模块(PEM)为基本单元,是实现高电压大容量的重要途径,可靠性是衡量模块化多电平变换装置优劣的重要性能指标。该文以电力电子模块多电平变换装置的可重构控制途径为基础,分析出了中性点移位加故障模块旁路重构法,计算出了多种故障状态下的中性点移位参数,提出了两种中性点移位载波调制(CPSPWM、SFO-CPSPWM)电力电子模块可重构控制策略,并进行了两种控制策略的对比仿真。仿真结果验证了两种载波调制可重构控制策略的有效性及正确性。 相似文献
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为提高超高速公路行驶安全性,使用结构分析和数学模型的方法研究基于智能路钮的高速公路虚拟轨道系统. 该系统由路面子系统、车载子系统和服务中心子系统组成. 安装车载系统的车辆接近写入路钮时激活虚拟轨道系统,阅读器读取标签路钮的位置坐标和该处道路线形信息,同时数据处理模块读取线形参数并处理得到道路切线与车身角度,读取前轮偏角、车辆速度和相邻两个标签路钮之间的距离,利用计算模型得到车辆在相邻两个标签路钮之间行驶时方向盘的转动角速度,并将控制参数发送给转向电机. 研究结果表明,当超高速公路设计车速分别为140,160,180 km/h时,只要保证路钮间的距离分别小于1.33,1.50,1.69 m,就可保证车辆偏离中心线的距离小于0.5 m. 因此,基于智能路钮的虚拟轨道系统可将车辆限制在虚拟轨道内行驶,保证超高速公路的安全性. 相似文献
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由于烟雾图像场景模糊不清,背景复杂多变,难以捕获到有效特征,导致算法识别误报率和漏报率较高;此外,深度卷积神经网络结构复杂,参数繁多,难以缩短其计算时间至1 ms内,这成为实时火灾预警的一大难题. 为了解决上述问题,提出了一种基于4种Inception结构的轻量级卷积神经网络SInception (sequeeze-and-excitation inception)在此基础上加入SE Block (sequeeze-and-excitation block)用于对烟雾特征进行重新分配;同时,为了避免由于训练样本不足引起的过拟合,原始数据集上采用数据增强技术以及生成对抗网络生成更多训练样本,并在后续实验中采用了融合暗通道先验特征的策略. 实验结果表明:该网络在增强的数据集GAN-Aug-YUAN上将识别误报率降为0的同时将准确率提升至99.65%,且计算时间减少到0.26 ms. 相似文献
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A Pacific basin-wide physical–biogeochemical model has been used to investigate the seasonal and interannual variation of physical and biological fields with analyses focusing on the Sea of Japan/East Sea (JES). The physical model is based on the Regional Ocean Model System (ROMS), and the biogeochemical model is based on the Carbon, Si(OH)4, Nitrogen Ecosystem (CoSiNE) model. The coupled ROMS–CoSiNE model is forced with the daily air–sea fluxes derived from the National Centers for Environmental Prediction (NCEP) and the National Center for Atmospheric Research (NCAR) reanalysis for the period of 1994 to 2001, and the model results are used to evaluate climate impact on nutrient transport in Mixed Layer Depth (MLD) and phytoplankton spring bloom dynamics in the JES.The model reproduces several key features of sea surface temperature (SST) and surface currents, which are consistent with the previous modeling and observational results in the JES. The calculated volume transports through the three major straits show that the Korea Strait (KS) dominates the inflow to the JES with 2.46 Sv annually, and the Tsugaru Strait (TS) and the Soya Strait (SS) are major outflows with 1.85 Sv and 0.64 Sv, respectively. Domain-averaged phytoplankton biomass in the JES reaches its spring peak 1.8 mmol N m− 3 in May and shows a relatively weak autumn increase in November. Strong summer stratification and intense consumption of nitrate by phytoplankton during the spring result in very low nitrate concentration at the upper layer, which limits phytoplankton growth in the JES during the summer. On the other hand, the higher grazer abundance likely contributes to the strong suppression of phytoplankton biomass after the spring bloom in the JES. The model results show strong interannual variability of SST, nutrients, and phytoplankton biomass with sudden changes in 1998, which correspond to large-scale changes of the Pacific Decadal Oscillation (PDO). Regional comparisons of interannual variations in springtime were made for the southern and northern JES. Variations of nutrients and phytoplankton biomass related to the PDO warm/cold phase changes were detected in both the southern and northern JES, and there were regional differences with respect to the mechanisms and timing. During the warm PDO, the nutrients integrated in the MLD increased in the south and decreased in the north in winter. Conversely, during the cold PDO, the nutrients integrated in the MLD decreased in the south and increased in the north. Wind divergence/convergence likely drives the differences in the southern and northern regions when northerly and northwesterly monsoon dominates in winter in the JES. Subjected to the nutrient change, the growth of phytoplankton biomass appears to be limited neither by nutrient nor by light consistently both in the southern and northern regions. Namely, the JES is at the transition zone of the lower trophic-level ecosystem between light-limited and nutrient-limited zones. 相似文献
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