W型永磁电机转矩脉动分析与抑制方法

针对永磁同步电机转矩脉动偏大时电机输出性能较差的问题,对W型永磁同步电机的转矩脉动进行详细分析并研究其抑制方法.首先利用等效磁路法与洛伦兹力定律,推导出电机转矩脉动解析式,基于解析式对W型磁极的位置参数进行优化,并利用有限元软件仿真验证;然后利用转子极面偏心的方法进一步削弱电机转矩脉动,并分析最优偏心距.研究表明,当W...     

Investigations on Several Mechanical Problems in Windblown Sand Movement

It is very necessary for the investigation on mechanism of windblown sand movement to understand and find out effective measures of preventing and reducing danger of windblown sands,which also deals with some general characters and hot spots in the scient     

光纤光谱仪在LED光通量测量中的应用

由于LED的光谱功率分布较窄,而光度测量中采用的光度探头的响应和标准光谱光视效率函数V(λ)很难做到完全匹配,因此在LED光通量测试中极易引入光谱失配误差.现提出了在LED光通量测试仪中引入光纤光谱仪对光通量测试结果进行光谱失配校正.在验证实验中对不同光谱功率分布的LED样品进行了测量,并且与中国计量科学研究院测试的标准光通量进行了比较,实验数据表明,在LED光通量测试中引入光纤光谱仪进行光谱失配校正能够提高测试精度,其中对单色光LED提高最为显著.     

Characterization of MASDs of surface soils in north China and its influence on estimating dust emission

Inordertoquantitivelyevaluateeffectsofdustaerosolonradiativeforcing[1],andtounderstandtheprocessofatmosphericchemistryandbiogeochemistry[2,3],modelingthedustemissionfluxisakindoffundamentalwork.TheDPMmodel[4—6]isidealforpredictingdustemission[7—10]becauseitconsiderseffectsofsurfacefea-tures(MASDofsurfacesoil,roughnesslengthandsoilmoisture,etc)andsandblastingprocess.Italsoprovidesanexplicitphysicalmechanismthatisvalidatedbywindtunnelandfieldexperiments[7—10].Themeandiameterofsurfacesoilsi…     

Preliminary study on land surface characteristics over Huaihe River Basin

The analysis of the flux observation dada from the Huaihe River Basin Experiment (HUBEX) shows that, in semi-humid monsoon regions, latent heat flux is as important as sensible heat flux in most situations. Moreover, it can even dominate the sensible heat flux in cropland and paddy field. This is distinct from that for arid and semi-arid regions where the sensible heat flux is dominant. Under clear sky conditions, the soil temperatures in different vertical layers all exhibit certain diurnal variations, and the magnitude decreases with depth to less than 1°C at a depth of 60 cm. This depth is considered as the transition layer for the soil moisture variation. On the other hand, the vertical profile of soil water content varies with the soil texture and even weather conditions, and the layer with maximum soil water content can also be found in Jiangji station during June 1998.     

磁性水凝胶的制备及其在正渗透中的应用

在Fe3O4纳米磁流体存在的情况下,将强离子型单体2-丙烯酰胺基-2-甲基丙磺酸钠(AMPS)与温敏单体N-异丙基丙烯酰胺(NIPAM)共聚,制备了磁性水凝胶[P(NIPAM-co-AMPS)/MNPs],并将其用作正渗透汲取剂.表征结果证实:磁性水凝胶显示超顺磁性,其饱和磁化强度与Fe3O4磁性纳米粒子(MNPs)含量呈线性关系.正渗透实验结果表明:引入MNPs对磁性水凝胶水通量影响很小,不同MNPs含量的磁性水凝胶在0.5h内平均水通量范围为2.22~2.52L·m-2·h-1;在不同膜方向模式下,磁性水凝胶表现出可忽略的水通量差异,可避免稀释内部浓差极化问题,同时具有重复使用的优点;在温度刺激下(65℃),引入MNPs可提高磁性水凝胶的脱水效率,质量分数为9.0%的MNPs的磁性水凝胶在最初20min内的脱水率是不含MNPs水凝胶的3.2倍.     

关于地下岩盐溶腔利用的特性研究

岩盐的蠕变、卤水的热膨胀以及卤水的渗漏是影响地下岩盐溶腔长期演变过程的三个主要因素．综述了国外在这三个方面的研究现状，以及国外学者所得到的一些结论．由于我国对岩盐溶解机理、岩盐溶腔的利用以及岩盐溶腔长期演变特性的研究相对薄弱，提出了在地下岩盐溶腔利用的过程中的一些建议．     

基于最大流原理的湖泊系统富营养化新模型

针对目前现有的湖泊富营养化模型的不足,以最大流原理为基础,以自组织特征映射神经网络(SOM)为算法实现手段,从复杂系统结构演化的角度提出了一个新的湖泊系统的富营养化模型;进而使用该模型对我国10个湖泊进行了富营养化评价并和以往的评价方法作了详细比较,结果表明该方法具有较好的合理性和可操作性。由于该模型从一定程度上体现了湖泊富营养化系统的演化动力学机理和湖泊系统时空演变特性,因此,不仅在评价上有较大的优越性,在湖泊富营养化发展变化状态的预测上也具有潜力。     

Estimation of components of energy balance on drifting ice over Arctic Ocean

Estimation and simulation were carried out for the components of ice-surface energy balance and tur bulent exchange parameters using the flux-profile method and the sinple biosphere model version 2 (SiB2, hereinafter) respectively based on the measured results for the atmosphere in the near-ice-surface layer, which were observed by the First Arctic Scientific Expedition of China in August, 1999 at a joint ice-research station (75°02′N, 160°51′W) on the drifting ice of Arctic Ocean. Evidence suggests that during the melting period of drifting ice the sum of the ice-released sensible heat and effective melting-consumed heat is greater than the net ice-absorbed radiation on the surface, with the excess heat coming via heat conduction from the deep layers of the ice mass. The simulated net radiation is systematical lv 18% greater than the measured results, while the simulated sensible heat flux is systematically 3% lower than the measured ones; and the simulated ice-surface heat flux differs noticeably from its calculation. Hence, we see that al though the measured sequences are short, the simulations of net radiation and sensible heat fluxes by the SiB2 model are comparatively good, the simulation of other forms of fluxes still needs to be improved.