Application of satellite observations to study the changes of hypoxic conditions in near-bottom water in the western part of Peter the Great Bay (the Sea of Japan)

In this paper we explore the possibilities of applying satellite ocean colour (OC) observations and SST to study the changes in the conditions of hypoxia in the near-bottom water in the western part of Peter the Great Bay. Near-bottom water hypoxia occurs in water bodies with increased organic matter influx when the dissolved oxygen (DO) consumed at its oxidation is not restored. Consumption of most DO is usually attributed to the oxidation of organic matter formed as a result of increased algae growth during water eutrophication. Satellite data on indicators of phytoplankton (chlorophyll-a concentration (Chl) and fluorescence (FLH)) allow to analyze the spatial-temporal changes of this substation. Coloured dissolved organic matter (CDOM), non-algal particles (NAP) influence on satellite Chl estimates and also on near-bottom water hypoxia formation. This study analyzes daily, seasonal, and inter-annual changes in the distributions of indicators (Chl, FLH, the coefficients of light absorption by coloured detrital matter (a_CDM) and light backscattering by suspended particles (b_bp)), based on the instant satellite OC data from MODIS-Aqua. Data on the Chl, the sea surface temperature (SST) from the MODIS-Aqua, the precipitation from the TRMM satellite and the hydrometeorological stations (HMSs), the wind speed and direction from HMS “Vladivostok” are used to study the influence of hydrometeorological conditions on the Chl values. These distributions were compared with the literary information based on field observations of the hypoxia cases in the same area and with the changes in the vertical DO, Chl, temperature, salinity distribution obtained by coastal expeditions in October-November 2010 and February-March 2011. Significant interrelations within 95% confidence level between the satellite Chl, FLH values calculated at the MUMM atmospheric correction and in situ Chl values obtained in the autumn of 2010 were reached separately for the cases with winds of northern and southern directions with the correlation coefficients of 0.71, 0.48 and 0.49, 0.71, respectively. Significant dependences of Chl on SST and Chl on wind speed explained by the influence of continental runoff and water ventilation were obtained. Therefore, the changes of Chl reflect the changes of hypoxic conditions in the near-bottom water. In Amursky Bay the onset of hypoxia was at the Chl and SST values equal to 4 mg m^?3 and 13 °C (↑ – at increasing SST); near Furugelm Island it was at 1.6 mg m^?3 and 25 °C (↑), 1 mg m^?3 and 21 °C (↓). The difference in the Chl values was reflected in the hypoxia onset timings that were the beginning of June (2011), August (2013), and September (2014), respectively. The water flow from the eastern coast of Amursky Bay in early August of 2013 recorded from the OC and SST satellite imagers appeared in an additional hypoxic zone. Decreased OC characteristics in the runoff of the Razdolnaya River in August-September of 2014 were a sign of hypoxia at its mouth. Near Furugelm Island the hypoxia destruction (increase in the DO level from 1 to 4.5 ml L^?1) was observed at the Chl of 0.9 mg m^?3 and SST = 18 °C (↓). At the autumn maximum of Chl equal to 1.7 mg m^?3 and SST = 4 °C (↓) in mid-November the DO level here increased to 8 ml L^?1. In Amursky Bay, short-term destructions/weakening of hypoxia manifested themselves in sharp increases of Chl. At that, the ratio between the Chl value and the approximation level was equal to 2 and higher for SST equal to 22–25 °C (↑), to 0.9 and higher for SST equal to 5–13 °C (↓). With the water stratification destruction in temperature and the noticeable weakening of the stratification in salinity (mid-November), the hypoxia destructed (the DO level increased from 2 to 6 ml L^?1). In this case, Chl and SST were about 3 mg m^?3 and 5 °C (↓).     

基于脉冲初值的小推力转移轨道优化研究

针对小推力转移轨道优化过程往往忽略初值多样性的现状,研究了基于不同脉冲初值的小推力转移轨道优化问题。基于直接法的离散思想建立了小推力转移轨道优化模型,提出了基于粒子群和序列二次规划的组合优化算法,以地球1∶1共振近地小行星2016HO3交会任务为例,将3种典型的脉冲轨道作为初值设计了燃料最优小推力转移轨道。仿真结果表明:3种初值轨道优化得到了2个小推力转移发射窗口,两者燃料消耗差距不超过6%。不同的初值对小推力轨道的整体性能指标影响较小,但开关机时刻和推力方向的变化会产生较大差异,从而得到不同的最优控制曲线。     

地面模拟空间环境下磷酸盐涂层的摩擦学行为

针对有机类固体润滑防护涂层长期暴露在空间环境下涂层表面降解、致密性下降、润滑作用失效等问题,设计开发了改性磷酸盐黏结固体润滑防护涂层。通过地面模拟空间综合环境设备系统,分析了改性磷酸盐黏结固体润滑防护涂层在长时间紫外、原子氧、高能质子和电子辐照后的结构变化和真空摩擦学性能。结果表明:紫外和高能粒子辐照对改性磷酸盐黏结固体润滑涂层的力学和真空摩擦磨损性能均无影响;原子氧对涂层表面的二硫化钼具有一定的氧化作用,但并未影响涂层的摩擦磨损性能,涂层经过各种辐照后仍然表现出良好的润滑作用。该涂层有望应用于航天飞行器相关运动部件的润滑与防护。     

空间机器人动力学奇异回避的笛卡尔轨迹规划

针对空间机器人动力学奇异的回避问题,提出一种基于组合函数的笛卡尔轨迹规划方法。将梯形规划与正弦函数相结合,对机械臂末端的位姿进行参数化。机械臂沿着某一轨迹运动时,根据阻尼最小方差法(DLS)的特点,提出一种判断是否发生动力学奇异的方法,并据此进行轨迹规划。该方法可以保证空间机械臂运动过程中不会遇到动力学奇异。此外,将基座姿态扰动和机械臂运动时间作为目标函数的一部分,最终,轨迹规划问题转化为多目标优化问题,并利用混合整数规划的混沌粒子群优化算法(CPSO)进行求解。该优化算法能够改善标准粒子群算法(PSO)的“早熟”现象。仿真结果表明,新方法能够有效处理动力学奇异问题,减小基座姿态扰动及运动时间。     

基于盒粒子滤波的低成本皮纳卫星高效姿态确定算法

针对低成本皮纳卫星姿态确定系统在质量、体积、计算量以及能耗等方面的限制问题,本文基于区间分析理论提出了卫星姿态区间化描述方法并建立了运动学区间化方程,提出了基于盒粒子滤波(BPF)的皮纳卫星姿态确定算法。该算法首先采用双矢量算法对太阳敏感器和磁强计得到的量测进行姿态解算,并将解算出的姿态四元数作为伪量测值输入传递给BPF,从而降低敏感器噪声对估计精度的影响。仿真实验表明,相比于传统粒子滤波的姿态确定算法,本文所提出的BPF姿态确定算法能够在保证姿态确定精度的同时大幅缩短算法运行时间。     

冲蚀条件下炭布橡胶绝热层烧蚀实验与计算

开展了冲蚀条件下一种炭布橡胶类绝热材料的烧蚀实验,研究了颗粒浓度和冲蚀速度对该绝热层烧蚀的影响规律。实验结果表明,实验条件下冲蚀速度是影响绝热层烧蚀的最主要因素;冲蚀速度较低时,即使颗粒浓度很高,烧蚀率也不是很大。在实验基础上建立了一种基于炭化烧蚀模型的烧蚀计算模型,即首先根据实验数据建立冲蚀状态与炭层厚度之间的关系,然后采用传统的炭化烧蚀模型进行烧蚀计算,计算结果与实验结果在一定程度上较为吻合。     

高超声速飞行器非连续点火助推增程弹道设计

针对高超声速飞行器因防热烧蚀而制约整体射程的问题,创新提出了一种非连续点火助推方案,通过增大助推段射程的弹道设计方法提高飞行器整体射程能力,减轻后续段的射程压力。综合考虑动压、过载、控制和终端高度、速度、弹道倾角等约束条件,以助推段射程最大为目标函数,设计了非连续点火助推段飞行程序和纵向平面弹道优化模型,采用改进的梯度粒子群算法进行优化求解。仿真结果表明,改进的梯度粒子群算法能有效解决非连续点火助推弹道设计问题,设计的非连续点火助推弹道方案在满足各项约束的同时,助推段射程比连续点火方案提高了8.7倍,射程达到了4 800 km,增程的效果十分明显。     

复合固体推进剂应力分布的数值模拟及损伤萌生分析

建立了复合推进剂颗粒填充引起应力集中的有限元计算模型，计算了法向应力的分布及其最大应力的位置，讨论了颗粒分数，刚度对应力分布的影响。根据引发微裂纹萌生的力学条件，得到了复合固体推进剂占主导地位的损伤形式为颗粒与界面的显微裂纹损伤。     

微波等离子推力器真空羽流模拟计算

粒子节点－直接模拟蒙特卡罗法（DSMC）是求解稀薄气体流动的数值模拟方法，采用轴对称硬球模型、随机取样频率法对微波等离子推力器（MPT）的真空羽流进行了数值模拟计算，为了提高计算效率和节省计算机内存，采用了随机取样频率法（RSF）和加权技术。对MPT真空羽流的浓度、速度和温度分布进行了计算，并对羽流污染进行了分析。计算结果对以后MPT真空羽流场测试和航天器一体化设计提供了参考。     

同轴送粉喷嘴保护气体流场研究

为解决飞机结构损伤激光在线修复过程中同轴送粉喷嘴气体保护效果不佳的问题,利用粒子图像测速(Particle image velocimetry,PIV)和Fluent软件对喷嘴保护气体流场进行了研究。将喷嘴气流的同轴射流和同轴冲击射流的数值计算结果和实验测量结果进行了比较,分析了喷嘴气流速度变化对流场稳定性的影响。结果表明:喷嘴中心、内环和外环气流流速由内向外递减时可获得稳定的流场;喷嘴中心、内环、外环喷出的气流速度接近一致时,流场比较稳定;喷嘴中心气流速度小于内环和外环的气流速度时,工件表面出现漩涡,破坏了流场的稳定性。