基于QAR数据的民机高高原进近着陆风险评估方法

民机高高原进近着陆是高原飞行高风险阶段。为有效实施高高原进近着陆风险识别和等级判据,提出基于熵权可变模糊识别的长短时记忆网络与深度神经网络(LSTM-DNN)相融合的深度学习风险评估方法。基于快速存取记录器(QAR)记录的高高原飞行数据,借鉴民机飞行品质监控（FOQA）咨询通告和行业QAR监控标准,结合指标重要度分析与Delphi专家调查,提取着陆时航向变化大、航迹低、610～305 m进近时下降率大、接地时垂直加速度及153～15 m进近时下降率大5个关键监控项目作为民机高高原进近着陆风险评估指标。为克服评估指标权重主观性偏差,应用熵权法确定评估指标权重,基于可变模糊识别方法构建风险等级隶属函数,建立基于LSTM-DNN的民机高高原进近着陆风险评估模型。以成都—拉萨进近着陆航段为例,提取QAR数据,对该风险评估模型进行训练与测试,并与Logistic多元回归、支持向量机(SVM)等评估方法进行比较,结果表明：所提方法平均准确率达到94.18%,最高可达94.79%,验证了方法的客观有效性。     

基于自编码器和HMM的民机接地点远事件检测

已有的飞行品质监控（FOQA）标准仅由地速的积分距离判定接地点远事件（LTE）的发生,无法结合多个快速存取记录器（QAR）参数检测并解释发生该事件的原因。通过滑动窗口对包含多个参数的QAR样本进行分段,按照分段位置形成若干分段样本集。由长短时记忆网络（LSTM）自编码器得到QAR样本分段及分段内向量的特征表示,采用K-means分别对这些表示向量进行聚类处理,实现QAR样本及其分段的符号化。使用正常航班QAR样本集的符号序列建立隐马尔可夫模型（HMM）,以检测包含接地点远事件的航班。由发生及未发生接地点远事件的QAR样本各个分段的符号序列构建HMM后,采用Viterbi算法确定接地点远事件在QAR样本分段内的具体位置。在真实QAR数据集上的实验结果表明,与其他多维时间序列异常检测方法相比,所提方法不仅能有效检测接地点远事件,而且可以获得多个QAR参数的异常值,辅助领域专家分析发生该事件的原因。      

Study of satellite retrieved CO2 and CH4 concentration over India

This paper reports a study of spatial and temporal variations of columnar averaged concentration of CO₂ and CH₄ over India using SCanning Imaging Absorption spectroMeter for Atmospheric CHartographY (SCIAMACHY) and Greenhouse gas Observing SATellite (GOSAT) data. Comparison of these data with the global view National Oceanic and Atmospheric Administration (NOAA) land data and also location specific flask data is made. The temporal variation in column averaged global CO₂ is similar to that over India and it is also similar to the NOAA surface flask data and global view. The variation in NOAA surface CH₄ is location dependent and its global view appears to vary seasonally in opposite phase with the column averaged CH₄ values from satellites, reflecting the limited comparability of surface and column averaged data. Over India the CO₂ maximum is in May and minimum in August/September while for CH₄ the maximum is in September and minimum in February/March. The seasonal variation of CH₄ over India is correlated with the eastern coastal rice cultivation.     

Pressure,O2, and CO2, in aquatic Closed Ecological Systems

Pressure increased during net photosynthetic O₂ production in the light and decreased during respiratory O₂ uptake during the dark in aquatic Closed Ecological Systems (CESs) with small head gas volumes. Because most CO₂ will be in the liquid phase as bicarbonate and carbonate anions, and CO₂ is more soluble than O₂, volumes of gaseous CO₂ and gaseous O₂ will not change in a compensatory manner, leading to the development of pressure. Pressure increases were greatest with nutrient rich medium with NaHCO₃ as the carbon source. With more dilute media, pressure was greatest with NaHCO₃, and less with cellulose or no-added carbon. Without adequate turbulence, pressure measurements lagged dissolved O₂ concentrations by several hours and dark respiration would have been especially underestimated in our systems (250–1000 ml). With adequate turbulence (rotary shaker), pressure measurements and dissolved O₂ concentrations generally agreed during lights on/off cycles, but O₂ measurements provided more detail. At 20 °C, 29.9 times as much O₂ will distribute into the gas phase as in the liquid, per unit volume, as a result of the limited solubility of O₂ in water and according to Henry’s Law. Thus even a small head gas volume can contain more O₂ than a larger volume of water. When both dissolved and gaseous O₂ and CO₂ are summed, the changes in Total O₂ and CO₂ are in relatively close agreement when NaHCO₃ is the carbon source. These findings disprove an assumption made in some of Taub’s earlier research that aquatic CESs would remain at approximately atmospheric pressure because approximately equal molar quantities of O₂ and CO₂ would exchange during photosynthesis and respiration; this assumption neglected the distribution of O₂ between water and gas phases. High pressures can occur when NaHCO₃ is the carbon source in nutrient rich media and if head-gas volumes are small relative to the liquid volume; e.g., one “worse case” condition developed 800 mm Hg above atmospheric pressure and broke the glass container. Plastic screw cap closures are likely to leak at high pressures and should not be assumed to seal unless tested at appropriate pressures. Pressure can be reduced by having larger head-gas volumes and using less concentrated nutrient solutions. It is important that pressure changes be considered for both safety and closure, and if total O₂ is used as the measure of net photosynthesis and respiration, the O₂ in the gas phase must be added to the dissolved O₂.     

Study on O2 generation and CO2 absorption capability of four co-cultured salad plants in an enclosed system

The ability to generate O₂ and absorb CO₂ of several co-cultured vegetable plants in an enclosed system was studied to provide theoretical reference for the future man-plant integrated tests. Four kinds of salad plants (Lactuca sativa L. var. Dasusheng, Lactuca sativa L. var. Youmaicai, Gynura bicolor and Cichorium endivia L.) were grown in the CELSS Integration Test Platform (CITP). The environmental factors including O₂ and CO₂ concentration were continuously monitored on-line and the plant biomass was measured at the end of the test. The changing rules of O₂ and CO₂ concentration in the system were basically understood and it was found that the O₂ generated by the plants could satisfy the respiratory needs of 1.75 persons by calculation. It was also found that the plants could absorb the CO₂ breathed out by 2 persons when the light intensity was raised to 550 mmol m⁻² s⁻¹ PPF. The results showed that the co-cultured plants hold good compatibility and excellent O₂-generating and CO₂-absorbing capability. They could also supply some fresh edible vegetable for a 2-person crew.     

多舱段载人航天器CO2去除系统性能仿真分析

多舱段载人航天器通常由主控舱段利用舱间通风对组合体空气环境参数进行集中控制.利用Ecosimpro建立了一种多舱段载人航天器CO₂去除系统性能仿真分析模型,包括舱体模块、乘员模块、CO₂净化模块、舱间通风模块,并对三舱段载人航天器CO₂去除系统性能进行了计算分析.结果表明,当净化装置进风量为0.007 2 kg/s,非主控舱段驻留人数达到6人时,会造成非主控舱段CO₂分压超出700 Pa的指标上限.此时增大舱间通风量对降低非主控舱段CO₂分压的效果并不明显,有效的控制方式是增大净化装置进风量.当净化装置进风量增加至0.011 3 kg/s时,非主控舱段CO₂分压可降至700 Pa以下.该工作有助于加快载人航天器空气环境控制系统的设计和改进流程.     

Cloud optical thickness feedbacks in the CO2 climate problem

A radiative-convective equilibrium model is developed and applied to study cloud optical thickness feedbacks in the CO₂ climate problem. The basic hypothesis is that in the warmer and moister CO₂-rich atmosphere, cloud liquid water content will generally be larger than at present, so that cloud optical thickness will be larger too. For clouds other than thin cirrus, the result is to increase the albedo more than to increase the greenhouse effect. Thus the sign of the feedback is negative: cloud optical properties alter in such a way as to reduce the surface and tropospheric warming caused by the addition of CO₂. This negative feedback can be substantial. When observational estimates of the temperature dependence of cloud liquid water content are employed in the model, the surface temperature change due to doubling CO₂ is reduced by about one half.     

Plasma chemical reactions in C2H2/N2, C2H4/N2, and C2H6/N2 gas mixtures of a laboratory dielectric barrier discharge

Plasma chemical reactions in C₂H₂/N₂, C₂H₄/N₂, and C₂H₆/N₂ gas mixtures have been studied by means of mass spectrometry at a medium pressure of 300 mbar in a laboratory dielectric barrier discharge. A major reaction scheme is production of larger hydrocarbons like C_nH_m with n up to 12 including formation of functional CN groups.     

二维H2/O2混合和流动的直接数值模拟

用高阶精度的紧致差分方法,对低速的随时间发展的二维可压缩H-2/O-2混合层流动编制了直接数值模拟的计算机程序,对雷诺数Re为400、来流马赫数Ma分别为0.4(上部的H₂)和1.57(下部的O₂)的H₂/O₂亚跨超声速混合层流动进行了计算,得到了相应的计算结果,并对结果进行了分析和研究.     

CO2气体保护焊的波形模糊逻辑控制的方法

针对CO2气体保护焊恒流特性控制中弧长稳定性差问题,提出了弧长的波形模糊逻辑控制方案,介绍了波形控制系统工作原理和模糊逻辑控制器设计方法,并进行了试验研究.研究结果表明,此波形模糊逻辑控制系统完全实现了弧长恒定控制,得到焊接过程稳定,飞溅小和焊缝成形好等优良的工艺性能.