Five-phase Synchronous Reluctance Machines Equipped with a Novel Type of Fractional Slot Winding

Multi-phase machines are so attractive for electrical machine designers because of their valuable advantages such as high reliability and fault tolerant ability.Meanwhile,fractional slot concentrated windings(FSCW)are well known because of short end winding length,simple structure,field weakening sufficiency,fault tolerant capability and higher slot fill factor.The five-phase machines equipped with FSCW,are very good candidates for the purpose of designing motors for high reliable applications,like electric cars,major transporting buses,high speed trains and massive trucks.But,in comparison to the general distributed windings,the FSCWs contain high magnetomotive force(MMF)space harmonic contents,which cause unwanted effects on the machine ability,such as localized iron saturation and core losses.This manuscript introduces several new five-phase fractional slot winding layouts,by the means of slot shifting concept in order to design the new types of synchronous reluctance motors(SynRels).In order to examine the proposed winding’s performances,three sample machines are designed as case studies,and analytical study and finite element analysis(FEA)is used for validation.

Effects of Trajectory Wind Direction on Ion Concentration of PM_(10)

Objective To study the characterization apportionment of main ion concentrations of PM10 under the influence of trajectory wind direction in London. Methods PM10 samples from 1 May 1995 to 30 October 1995 of Oxford Street of Central London were collected, the metals and anions of which were measured using atomic absorption spectrometry （AAS） and ion chromatography （IC）. Composite trajectories representative of the air mass arriving in London at the same period were calculated based on basic routine back trajectories from the British Atmospheric Data Centre （BADC）. Results Concentration apportionments of main ions were similar when the trajectory was plotted back at 6 h, 12 h, and 24 h, some were obviously different. Mg, Ba, Pb, and Cu had similar peak apportionments at the area 180°-320°, but Zn and Ni at the area of 90°-270°, NO3^- and SO4^2- at the area of 100°-220°. Cl^- concentration peak apportionment was at the area of 220°-300°, which showed that Cl^- mainly came from the North Sea. Conclusion Trajectory wind direction has important effect on ion concentration apportionment of PM10 in London. The ions have similar concentration peak apportionments or their correlation coefficients are statistically significant.

Effects of different poses and wind speeds on flow field of dish solar concentrator based on virtual wind tunnel experiment with constant wind

In order to improve structure performance of the dish solar concentrator,a three-dimensional model of dish solar concentrator was established based on the high-precision numerical algorithms.And a virtual wind tunnel experiment with constant wind is adopted to investigate the pressure distribution of the reflective surface,velocity distribution of the fluid domain for the dish solar concentrator in different poses and wind speeds distribution.Some results about wind pressure distribution before and after dish solar concentrator surface and wind load velocity distribution in the entire fluid domain had been obtained.In particular,it is necessary to point out that the stiffness at the center of the dish solar concentrator should be relatively raised.The results can provide a theoretical basis for the improvement of solar concentrator dish structure as well as the failure analysis of dish solar concentrator in engineering practice.

Satellite-observed trends in the Arctic sea ice concentration for the period 1979–2016

Arctic sea ice cover has decreased dramatically over the last three decades. This study quanti?es the sea ice concentration(SIC) trends in the Arctic Ocean over the period of 1979–2016 and analyzes their spatial and temporal variations. During each month the SIC trends are negative over the Arctic Ocean, wherein the largest(smallest) rate of decline found in September(March) is-0.48%/a(-0.10%/a).The summer(-0.42%/a) and autumn(-0.31%/a) seasons show faster decrease rates than those of winter(-0.12%/a) and spring(-0.20%/a) seasons. Regional variability is large in the annual SIC trend. The largest SIC trends are observed for the Kara(-0.60%/a) and Barents Seas(-0.54%/a), followed by the Chukchi Sea(-0.48%/a), East Siberian Sea(-0.43%/a), Laptev Sea(-0.38%/a), and Beaufort Sea(-0.36%/a). The annual SIC trend for the whole Arctic Ocean is-0.26%/a over the same period. Furthermore, the in?uences and feedbacks between the SIC and three climate indexes and three climatic parameters, including the Arctic Oscillation(AO), North Atlantic Oscillation(NAO), Dipole anomaly(DA), sea surface temperature(SST), surface air temperature(SAT), and surface wind(SW), are investigated. Statistically, sea ice provides memory for the Arctic climate system so that changes in SIC driven by the climate indices(AO, NAO and DA) can be felt during the ensuing seasons. Positive SST trends can cause greater SIC reductions, which is observed in the Greenland and Barents Seas during the autumn and winter. In contrast, the removal of sea ice(i.e., loss of the insulating layer) likely contributes to a colder sea surface(i.e., decreased SST), as is observed in northern Barents Sea. Decreasing SIC trends can lead to an in-phase enhancement of SAT, while SAT variations seem to have a lagged in?uence on SIC trends. SW plays an important role in the modulating SIC trends in two ways: by transporting moist and warm air that melts sea ice in peripheral seas(typically evident inthe Barents Sea) and by exporting sea ice out of the Arctic Ocean via passages into the Greenland and Barents Seas, including the Fram Strait, the passage between Svalbard and Franz Josef Land(S-FJL),and the passage between Franz Josef Land and Severnaya Zemlya(FJL-SZ).

The influence of runoff and wind on the dispersion patterns of suspended sediment in the Zhujiang(Pearl) River Estuary based on MODIS data

Cloud-free moderate-resolution imaging spectroradiometer(MODIS) images of the Zhujiang(Pearl) River Estuary(ZRE) taken between 2002 and 2012 are retrieved and used to study the spatial and temporal patterns of suspended sediment concentrations(SSCs) across the estuary under runoff, wind, and tropical storm conditions.Five typical dispersal patterns of suspended sediments in the estuary are defined: Case I shows generally low SSCs under low dynamics; Case Ⅱ shows a river-dominant dispersal pattern of suspended sediments from the outlets,particularly from Modaomen, Jiaomen, Hengmen, and others; Case Ⅲ shows wind-dominant dispersal of high SSCs derived from the west shoal and southwesterly transport under a strong NE wind; Case IV is the combination of relatively large runoff and wind; and Case V is caused by a strong tropical storm with high river discharge and wind, which is characterized by the high SSCs across the entire estuary that are transported eastward by winddriven and buoyancy currents outside the estuary. Runoff is a dominant factor that controls seasonal and annual SSC variations in the ZRE, with the area of high SSCs being largest in the summer and smallest in the spring. The correlation coefficients between the monthly averaged river-suspended sediment discharge and the area of the high SSCs are approximately 0.6. The wind power over the west shoal increases with a wind speed, which induces more sediment resuspension and shows a close relationship between the wind speed and high SSC area.

The New Minimum of Sea Ice Concentration in the Central Arctic in 2016

In view of the extremely low sea ice concentration(SIC) appeared at high latitudes of the Arctic in the summer of 2010, the changes of SIC in the central Arctic from 2010 to 2017 were investigated in this paper based on the AMSR-E/AMSR-2 SIC products retrieved by the NT2 algorithm. The results show that the extremely low sea ice concentration in the central Arctic not only occurred in 2010 but also occurred again in 2016, and the daily average sea ice concentration(ASIC) reached a minimum of 0.70, which was significantly lower than the value of 0.78 in 2010 and became a new historical low record. A large area of sea ice in the sector 150°E–180° in 2010 disappeared in 2016, which was the most important difference to produce the new minimum. Also, the ice edge in 2016 retreated into the 85°N circle, whereas in 2010 it was far from the central Arctic. In 2010 and 2016, there were high correlations between the wind stress curl and the relative variation rate of ASIC, which indicates that wind stress curl(WSC) drove the divergence of sea ice. It directly leads to the decrease in the SIC and is the main cause of the extremely low SIC events. The results in this paper show that the decline of Arctic sea ice is represented by not only the reduction of sea ice coverage but also the reduction of SICs. The central Arctic has always been covered by large amount of sea ices, so the drastic reduction of SIC will not only change the structure of the ice field, but also lead to critical climatic effects that deserve further attention.

Study on Air Pollutant Concentration inside Railway Tunnels

This paper presents a one-dimensional unsteady flow model and a numerical procedure based on the model. Comparisons between the theory and full scale experiments in a railway tunnel show that the model is capable of produce precise predictions for piston wind and pollutant concentration in railway tunnels.

The Observed Low CO_2 Concentration in the Rongbuk Valley on the Northern Slope of Mt. Everest

In the summers of 2006 and 2007, the atmospheric CO2 concentration and the wind speed in the Rongbuk Valley on the northern slope of Mr. Everest were measured by an ultrasonic anemometer with an Li-7500 CO2/H2O gas analyzer. The average CO2 concentration was 370.23±0.59 and 367.45±1.91 ppm in June of 2006 and 2007, respectively. The values are much lower than those at sites with similar latitudes and altitudes worldwide. The observed atmospheric CO2 concentration in Rongbuk Valley can be affected by the transportation of prevailing down-valley winds from the up-valley direction to the observation site. Our results suggest that the Mt. Everest region could be ideal for background atmospheric and environmental studies.

Detecting sand-dust storms using a wind-profiling radar

Sand-dust storm is a type of disastrous weather, typically occurring in arid and semi-arid climates. This study selected a region in the hinterlands of the Taklimakan Desert, called the Tazhong region, as the experimental area to quantitatively estimate the particle concentrations of sand-dust storms using the boundary layer wind-profiling radar. We thoroughly studied the radar echo signals and reflectivity factor features during the sand-dust storms. The results indicate that（1） under sand-dust storm conditions, boundary layer wind-profiling radar cannot capture the complete information regarding horizontal wind velocity and direction, but it can obtain the backscattering intensity of sand-dust storms; and（2） during sand-dust storms particle size distributions in the surface layer closely resemble log-normal distributions, with sand-dust particles sizes of 90–100 μm accounting for the maximum particle probability. Retrieved particle size distributions at heights of 600, 800, and 1000 m follow log-normal distributions, and the expected value of particle diameter decreases gradually with increasing height. From the perspective of orders of magnitude, the retrieved results for particle number concentrations and mass concentrations are consistent with previous aircraft-detected results, indicating that it is basically feasible to use boundary layer wind-profiling radar to quantitatively detect the particle concentrations of dust storms.

一种基于直流式风洞的火星尘暴模拟装置

为了研究火星表面尘暴环境对探测器及人类活动的影响,研制了一种基于低密度直流式风洞的火星尘暴环境模拟装置:采用超声速引射器作为风洞动力源,结合具备多工况动态调节能力的大抽气量真空系统,实现了引射气量精准调控,可模拟100~1500 Pa低气压下的5~100 m/s大跨度风速;针对低气压下沙尘浓度难以精确控制的问题,采用振动式喂料、逆向螺旋式喷嘴设计以及大周期滞后串级调节方式,实现了0.1~1 g/m^(3)的沙尘浓度精确控制。该装置可用于研究火星尘暴环境对材料和机构的影响,同时还可用于火星气动力研究。

综掘工作面风流调控下风速及瓦斯粉尘浓度融合预测模型研究

针对综掘工作面传统的通风总量控制管理模式不能根据实际需求进行风流调控,造成瓦斯及粉尘聚集和污染隐患等问题,对风流调控下的风速及瓦斯粉尘浓度多源数据融合神经网络预测模型进行了研究。采用欧拉-拉格朗日法建立了风流调控下的瓦斯及粉尘气固耦合模型并进行了测试验证,模拟分析瓦斯和粉尘颗粒在综掘巷道的分布情况,获取大量不同风流调控方案下的风速及瓦斯粉尘浓度样本数据。采用多层感知器神经网络技术建立预测模型结构,选取对瓦斯及粉尘浓度具有较大影响的风流调控等参数作为输入层,根据风速及瓦斯粉尘的隐患位置确定输出层,对样本数据进行预处理,通过引入差分进化算法搜索最佳隐藏层节点数和学习率,利用TensorFlow框架搭建多源数据融合神经网络预测模型。以陕北某矿综掘工作面为研究对象,对不同风流调控方案进行预测和井下实测验证。结果表明:该模型相对误差最大值为9.7%,具有较高的准确性;选取出风口距端头最短距离5 m和最远距离10 m这2种工况下的最佳调控方案,与调控前相比,风速符合规范要求,端头死角区瓦斯体积分数分别降低34%和35%,回风侧人行处平均粉尘质量浓度分别降低40%和41%,司机处粉尘质量浓度分别降低38%和36%,研究可为风流调控提供参考。

空气过滤棉荷尘阻力特性的实验研究

为研究复合式空气过滤棉的阻力特性,选择3层复合空气过滤棉作为主要研究对象,通过实验系统地研究荷尘速率对其阻力变化的影响,并与过滤纸进行对比。研究结果表明:在相同过滤风速下,荷尘质量浓度越低,过滤棉阻力上升速度越快;过滤棉等级越低,荷尘质量浓度对其阻力增长影响越大,归一化阻力随单位面积荷尘质量的增长越快;过滤风速对过滤棉归一化阻力的增长有影响,过滤风速越大,归一化阻力增长越缓慢,但对效率较高的过滤棉影响不大。相同荷尘条件下,相较于过滤纸,过滤棉的归一化阻力上升更慢;基于实验归纳得到3层复合空气过滤棉的阻力增长特性方程。研究结果可为其使用寿命预测提供参考。

齿调制作用下转子开槽对永磁电机电磁振动影响

为了研究齿调制作用下转子表面开槽对永磁同步电机电磁振动的影响,以小功率分数槽集中绕组(FSCW)内置永磁同步电机(IPMSM)为研究对象,通过麦克斯韦应力张量法推导径向电磁力波的频率及空间阶数特征。分析齿调制作用在FSCW-IPMSM中将空间高阶电磁力波调制为低阶电磁力波的过程,并给出转子表面开槽在齿调制作用影响下与电磁振动间的联系。研究表明,转子表面开槽结构的改变会使各次谐波磁场发生变化,进而改变以极数阶电磁力波为代表的高阶电磁力波的幅值。在齿调制作用下,这些高阶电磁力波会被调制为幅值较高的低阶电磁力波,并引起不同幅度的低阶振动。然后建立C型、V型两种不同转子表面开槽结构的10极12槽FSCW-IPMSM电磁及结构有限元分析模型并进行仿真分析。结果表明,极数阶即10阶电磁力波会被调制为2阶并引起2阶振动,且两种不同开槽结构间的电磁振动存在着高达22.1%的差异。最后,在一台10极12槽样机上进行振动实验,验证理论与仿真分析结果。

结构保温一体化墙体加厚免拆模板连接性能分析

增加结构保温一体化墙体免拆模板的保温层厚度可实现更高的节能目标,然而增加保温层厚度后,现有连接件不能很好满足锚固要求。本文提出适用于较厚保温层免拆模板的连接件,对其连接性能进行分析,以实际工程为研究案例,通过ANSYS将增厚墙体中的连接件替换成改良连接件,对一体化墙体、加厚免拆模板的整体性和改良连接件自身受力及变形情况进行分析。经计算结果分析,一体化墙体整体锚固与改良前相比效果明显,免拆模板与现浇墙体协调变形,改良连接件改进部位符合受力规律,穿出免拆模板背面产生的应力集中不会对模板造成破坏,风压增高的情况下锚固效果优于普通连接件。结构保温一体化墙体加厚免拆模板连接性能较好。

重载列车车速对隧道入口段扬尘特征的影响模拟

为掌握重载列车车速对隧道入口段风流运移及扬尘特征的影响,为铁路隧道抑尘提供技术支持,以梁家山隧道为研究对象,模拟分析了重载列车以不同车速进入隧道时入口段压力场、风流场的演变规律,探究了隧道入口段煤尘颗粒运移轨迹及其浓度分布规律。结果表明:重载列车驶入隧道过程中,车速越大,列车运行前方正压场及车身周边的负压场越强,隧道入口段产生的涡流区及风速越大;重载列车完全驶入隧道后,空间内的煤尘颗粒以内旋和外旋两种运移方式呈高速无序地扩散,同一尾流区断面上,列车不同位置处监测点的煤尘浓度和最大煤尘浓度对应的时间分布有差异。该研究成果有助于理解重载列车运行速度对隧道入口段风流运移及扬尘特征的影响,对梁家山隧道入口段的煤尘防治有指导意义。

超厚结构保温一体化墙体免拆模板受力性能研究

随着各省绿色建筑政策的发布,结构保温一体化墙体面对高要求节能目标难以胜任,超200 mm厚度保温层成为未来满足节能水平主要途径之一,以实际工程为研究案例,通过ANSYS有限元软件进行风载下仿真模拟,对比研究结构保温一体化墙体中220 mm厚免拆模板在框剪结构中受力情况,结果表明免拆模板厚度增加、自重增大时,其变形也成倍数增加,且在高层建筑中不同构件交界处以及阴阳角部位易发生应力集中,是免拆模板易损部位,现有连接件不能满足超厚结构保温一体化墙体免拆模板使用要求,需根据受力特性进行改进。

基于空间极对数宽频带耦合的双转子同步风力发电机电磁特性分析

【目的】针对传统大型永磁同步风力发电机无法实现励磁磁场的调节、传统双馈发电机无法实现直驱且存在后期维护等问题,设计了一种模块化双转子同步风力发电机。【方法】该发电机定子绕组为分数槽集中绕组(FSCW);双转子绕组均为集中绕组且采用直流激励;定子激励产生的两个主导极分别与两个转子的主导极进行磁通匝链。首先,介绍了所设计发电机的基本结构与工作原理;其次,建立了该类发电机的数学模型,并依托于FSCW理论分析其磁链、感应电动势等电磁特性;最后,建立有限元仿真模型,将仿真与理论结果进行对比分析。【结果】结果表明:定、转子齿部导磁面正对位置处磁链计算较为准确,而定、转子齿部偏移处由于含有气隙漏感存在一定的计算偏差。【结论】仿真与理论结果基本吻合,验证了所设计的模块化双转子同步风力发电机的正确性。

直升机涵道尾桨永磁同步电机设计与仿真

针对直升机涵道尾桨机械传动系统传动链长、噪声大、结构复杂、传动轴刚度差和安装维护周期长等缺陷,设计一种适用于直升机涵道尾桨的永磁同步电机。通过探究悬停工况下电机主要尺寸与尾桨桨叶长度、宽度以及安装角度的关系,明确一定范围内电机主要尺寸最小时的功率、转矩和转速;采用分数槽集中绕组进一步提升了功率密度,基于14极18槽完成了电机设计。建立电磁场和温度场有限元仿真模型,验证电磁设计的合理性以及永磁体分段降温的有效性。与未分段相比,当永磁体沿周向分4段时,永磁体平均温度降低了55.43%。结果表明:该电机功率密度较高,输出特性良好并且温升较低,能够长时间可靠运行。

南极宇航员海夏季水文结构变化特征研究

本文基于中国南极考察(CHINARE37-38)在宇航员海获取的海洋综合站位观测数据,结合海冰密集度、WOA23和ERA5再分析资料等,分析了该海域主要水文结构及其变化特征。结果表明:宇航员海夏季水团包括南极表层水(分为夏季表层水与冬季残留水)、绕极深层水、变性绕极深层水和南极底层水。夏季表层水均分布在表层50 m深度以浅,呈现出南冷北暖的趋势。66°S以南的冬季残留水最厚,最深可达200 m左右。绕极深层水向南侵入的趋势明显,CHINARE-38绕极深层水向上涌升的高度较CHINARE-37高出10~20 m。夏季表层水的高温高盐核心位于中心海域无冰区,因为无冰海域的表层海水长时间接收太阳短波辐射而温度较高。近岸海域因冰融水导致局部夏季表层水降温淡化。宇航员海中心海域海面风场维持低气压气旋式环流,次表层水体通过Ekman抽吸上升冷却表层暖水,导致表层与次表层水体混合加强,绕极深层水向南侵入并向上涌升。

固定式打磨台排风除尘效果研究

在固定式打磨台上进行高精细度的金属打磨已成为机械制造工艺中的重要环节。为改善某公司固定式打磨台的排风除尘效果,提出了2种优化方案。采用CFD-DPM相互耦合的数值模拟方法,对打磨过程中固定式打磨台上的粉尘质量浓度分布情况进行分析,并对原固定式打磨台及2种优化方案的固定式打磨台排风除尘效果进行对比研究。研究结果表明,原固定式打磨台的排风除尘效果较差,而2种优化方案都能在一定程度上降低打磨过程中的粉尘质量浓度。当排风孔数量增加到4个和5个(上2下3)时,排风除尘效果较佳。在此基础上,通过在固定式打磨台安装风幕,对比得出安装风幕的4个排风孔固定式打磨台的排风除尘效果最佳,其呼吸带高度粉尘质量浓度和最大粉尘质量浓度相比未安装风幕分别降低了99.88%和91.81%,值得在相关工业实践中推广使用。