摆动分离筛薯土分离机理分析与参数优化试验

针对摆动分离筛薯土分离机理不明确,作业参数匹配不合理导致明薯率与马铃薯破皮率矛盾突出等问题,利用高速摄像机实时拍摄不同曲柄转速、筛面倾角和机器前进速度时摆动分离筛上薯土混合物的分布状态,统计并分析薯土混合物分布高度的变化规律,揭示薯土分离机理,并获得影响分离筛性能主要因素的取值范围。以明薯率和破皮率为评价指标,采用Box-Behnken响应面试验方法进行试验,建立各指标与因素间的回归数学模型,对影响摆动分离筛性能的结构与工作参数进行优化。结果表明,各因素对明薯率、破皮率影响由大到小为曲柄转速、筛面倾角、机器前进速度。摆动分离筛优化参数组合为:曲柄转速230 r/min,筛面倾角21.1°,机器前进速度2.03 km/h,优化后明薯率和破皮率分别为98.94%和0.21%,明薯率较优化前提高1.68个百分点,破皮率较优化前降低9.6个百分点,参数优化试验结果满足国家标准要求。     

基于OFDM-MIMO移动通信模型的采摘机器人设计

为了提高果树采摘机器人的智能化和自动化水平,提高机器人的实时通信和在线控制能力,实现机器人作业过程的远程控制,在采摘机器人通信系统中引入了OFDM-MIMO模型,并将移动4G技术应用到了机器人的设计中,突破了机器人控制距离限制,实现了机器人的跨区域无线通信。机器人采用视觉传感器和4G网络采集并传输图像,图像数据可以在远程浏览器端实时显示,便于掌握机器人作业信息。当机器人碰撞传感器发出信号时,可以利用OFDM-MIMO信道模型进行图像的高效传输,并将视觉传感器采集的图像信息传送给远程控制端,在采摘出现失误时可以及时地调整机器人的状态,实现果实采摘的在线控制。同时,设计了机器人的实验样机,并对机器人的果实定位能力和通信能力进行了实验和仿真。实验和仿真结果表明:该种机器人可以有效地识别普通果实和套袋果实,并且通信实验测试和仿真测试的结果吻合,从而验证了结果的可靠性及OFDMMIMO模型在采摘机器人通信系统中的可行性。     

考虑分段土壤作用力的振动减阻分析

振动载荷作用下耕作土壤作用力复杂多变,为研究入土角、振幅、振频对土壤作用力、牵引阻力的影响,将耕作土壤视为粘弹性材料,根据深松铲对土壤进行切削、提升、再切削,建立考虑分段土壤作用力的振动深松机-土壤系统的力学模型,采用渐近法与数值积分求解分析该模型,分析表明入土角为45°、振幅为0.001 m、振频为10 Hz时,土壤作用力较小。利用振动深松机进行试验研究,试验数据与仿真数据对比,验证了模型的正确性。试验结果进一步表明利用振动可以减小土壤作用力,降低拖拉机牵引阻力,提高土壤深松质量。     

双定子对称型多泵多速马达理论特性分析

在现有的对称型定量泵、定量马达原理基础上,设计出了双定子对称型结构的多泵/多速马达,在一个壳体内1个转子对应2个定子,使多速马达可以独立同步工作;以双定子对称型双作用多速马达为例,阐述了结构和工作原理,定义了符号表示方法,分析了多泵的输出流量特性、多速马达的输出转速和转矩特性,对多泵多速马达不同组合方式下的多速马达转速进行了分析,结果表明,双定子对称型多速马达能够输出多种不同的转速和转矩,这为双定子多泵/多速马达系统在机床设备、行走机械等领域的应用奠定了基础。     

开缝叶片低比转数离心泵空化性能的数值模拟

为了进一步提高低比转数离心泵的空化性能,对离心泵叶轮叶片进口附近的开缝进行研究.考虑开缝的3个参数,设计6组水力模型探究开缝对低比转数离心泵性能的影响.针对离心泵运行过程中产生空化的流动特点,基于Rayleigh-Plesset方程来描述空泡成长和溃灭过程的空泡动力学模型,采用RNG k-ε模型对在相同工况下的离心泵中两相流动进行数值模拟与分析.模拟结果表明:在叶片进口处开缝可以提高泵空化性能,其中第二组模型的空化性能提升比较明显,空化余量由4.447 m下降到3.910 m,降低了12.1%,水力效率由71.56%上升至76.46%;在相同工况下,开缝叶轮流道内的能量分布更加均匀,而扬程在额定流量下只有很小的变化.该模拟结果对研究低比转数离心泵内部流动特性及性能的提升具有一定的参考价值.     

低比转数变曲率叶型离心泵非定常流动分析

运用Fluent流场计算软件,采用修正的RNG k-ε湍流模型、滑移网格技术和二阶隐式时间推进法,用SIMPLEC算法对压力和速度耦合求解,数值模拟了低比转数变曲率叶型离心泵定常压力场、速度场和非定常压力场,设定了不同工况下靠近隔舌区叶轮和蜗壳之间的3个监测点,得到了3点的均压脉动度,并将计算的外特性曲线与试验进行了比对。结果表明,短叶片抑制了工作面流动的分离,改善了叶片上压力分布,叶轮出口处的射流尾迹区得到了明显改善;隔舌附近监测点的压力脉动幅值与监测点到隔舌间的距离成正比;数值计算结果为该泵叶型设计提供了理论依据。     

Earthworm biomass response to soil management in semi-arid tropical Alfisol agroecosystems

Earthworms recorded during 1989–1993 across 15 soil management treatments, comprising three different tillagexthree organic amendments (bare, farmyard manure, and rice straw) and six perennial ley treatments, belonged to two endogeic species, Octochaetona phillotti (Michaelsen) and Lampito mauritii Kinberg, while in a nearby undisturbed natural revegetation area three species were found, including the above two and Octonochaeta rosea (Stephenson). The earthworm biomass showed significant temporal and spatial variations and was higher during the post monsoon period than in the early rainy season. No worm biomass was recorded during the dry season. In the tillage and organic amendment treatments, the biomass was drastically reduced from September 1989 to September 1991 after the application of carbofuran and some herbicides, and was significantly reduced during these two years compared to that of 1992. The maximum monthly earthworm biomass ranged between 2.5 and 17.9 g m^-2 across the treatments and increased several-fold in the nearby natural revegetation area (75.9 g m^-2). It significantly increased in perennial ley treatments compared to annual treatments with organic amendments. Thus the earthworm biomass varied significantly (P<0.01) across the 15 treatments, indicating discernible effects of soil management.Visiting Scientist (under the Rockefeller Foundation Environmental Research Fellowship in International Agriculture)     

Hayland conversion to wheat production in semiarid eastern Montana: tillage, yield and hay production comparisons

When converting grass- and haylands to cultivated crop production, care must be taken to conserve and maintain soil resources while considering economic issues. Methods of breaking sod can have a bearing on erosivity, physical and chemical properties of soils, and cost of production. Our objective was to compare three methods of converting crested wheatgrass [Agropyron desertorum (Fisch. ex Link) Schult.] hayland to wheat (Triticum aestivum L.) production vs. leaving the land for hay production. We initiated a study in 1990 on Dooley sandy loam (fine-loamy, mixed Typic Argiboroll) near Froid in semiarid eastern Montana, USA. Plots, replicated three times, were 12- by 30-m oriented east to west on a north-facing slope. We converted sod to cultivated crop production by: (1) moldboard plow, (2) toolbar with sweeps, (3) herbicides (no-till). Plots were fallowed until spring 1991 and then seeded to spring wheat each of the next four years. All wheat plots were fertilized with 224 kg ha⁻¹ of 18-46-0 in 1991 and 1992, and 34 kg ha⁻¹ nitrogen as 34-0-0 in 1993 and 1994. Grass was either fertilized same as wheat or not fertilized. Wheat yields averaged 2540 kg ha⁻¹ on tilled treatments and 2674 kg ha⁻¹ on no-till. Fertilized grass consistently out-yielded unfertilized, and averaged 3.2 Mg ha⁻¹ vs. 1.8 Mg ha⁻¹. Toolbar with sweeps had highest economic return of US$169.48 ha⁻¹ to pay for land, labor, and management. Moldboard plow had US$162.05 ha⁻¹. Because of herbicide costs, no-till only returned US$148.64 ha⁻¹. Unfertilized grass hay returned US$67.68 ha⁻¹ and fertilized grass hay, US$97.95 ha⁻¹. Results may be tempered because our wheat yields were high: a 2016 kg ha⁻¹ wheat yield would have returned the same as fertilized grass. Before converting grass- and hay-lands to small grains production, consideration must be given to such variables as sod conversion methods, management practices, labor requirements, market conditions, total precipitation and its temporal distribution, soil conditions, growth environment, soil conservation, and economics.     

单轴振动电机横置的高速振动筛理论研究

将单轴振动电机横置于筛体上作为高速振动筛的振动源，通过筛体的动力学分析，建立了筛体的运动微分方程，从中解得筛体的运动方程及筛体的运动轨迹方程。理论分析表明：筛体作由随其质心的平动和绕质心的摆动组成的平面运动，筛面上点的运动轨迹为变化的椭圆，引起筛体摆动的因素是振动电机相对筛体质心在水平和垂直方向的位移以及筛体质心到弹簧支撑面的距离。就振动电机相对筛体质心的位移对筛面运动状态的影响进行了计算机模拟，找出了它们之间的相互关系，从理论上论述了振动电机位移对筛分性能的影响。     

Fine-earth translocation by tillage in stony soils in the Guadalentin, south-east Spain: an investigation using caesium-134

Tillage erosion is increasingly recognised as an important soil erosion process on agricultural land. In view of its potential significance, there is a clear need to broaden the experimental database for the magnitude of tillage erosion to include a range of tillage implements and agricultural environments. The study discussed in this paper sought to address the need for such data by examining tillage erosion by a duckfoot chisel plough in stony soils on steep slopes in a semi-arid environment. Results of the investigation of coarse fraction (rock fragment) translocation by tillage in this environment have been presented elsewhere and the paper focuses on tillage translocation and erosion of the fine earth. Tillage translocation was measured at 10 sites, representing both upslope and downslope tillage by a duckfoot chisel plough on five different slopes, with tangents ranging from 0.02 to 0.41. A fine-earth tracer, comprising fine earth labelled with ¹³⁴Cs, was introduced into the plough layer before tillage. After a single pass of the plough, incremental samples of plough soil were excavated and sieved to separate the fine earth from the rock fragments. Translocation of the fine-earth tracer was established by analysing the ¹³⁴Cs content of the samples of fine earth. These data were used to establish translocation distances for each combination of slope and tillage direction. Translocation distances of the fine earth were not significantly different from translocation distances of the coarse fraction. For all sites, except uphill on the 0.41 slope, translocation distances were found to be linearly related to slope tangent. The soil flux due to tillage for each site was calculated using the translocation distance and the mass per unit area of the plough layer. For slopes with tangents <0.25, the relationship between soil flux and tangent was linear and the soil flux coefficient derived was 520–660 kg m⁻¹ per pass. This is much larger than the coefficients found in other studies and this high magnitude is attributed to the non-cohesive nature and high rock fragment content of the soil in this investigation. A second contrast with previous studies was found in non-linearity in the relationship between soil flux and tangent when steeper slopes were included. This was a product of variation in plough depth between the steepest slopes and the remainder of the study area. On the basis of the study it is suggested that an improved understanding of tillage erosion may be obtained by considering the dual processes of tillage detachment (mass per unit area of soil subject to tillage) and tillage displacement (equivalent to translocation distance per pass) in assessing, comparing and modelling tillage translocation. An improved model is proposed that recognises the complexity of soil redistribution by tillage, provides a framework for process-based investigation of the controls on tillage fluxes, and allows identification of potential self-limiting conditions for tillage erosion.