浅谈海原县肉牛繁育现状及对策

本文对现阶段海原县肉牛繁育现状进行总结,即基础母牛饲养量逐年增加,品种趋向良种化;养殖模式由单一散养户逐渐转向规模场(户);养殖技术由原始粗放逐渐转向科学精细化;地方政策支持力度加大,配套体系逐渐健全。并分析了几个制约肉牛良繁的问题：即中大规模养牛场出现本交现象;饲养管理不精准导致“一年一胎”难实现;犊牛成活率低等问题。针对存在的问题从提高冷配繁育技术、母牛规范化饲养管理、提高犊牛成活等方面提出了相应的解决办法。     

不同游泳运动对菊黄东方鲀非特异性免疫的影响

通过水槽实验法,观察了菊黄东方鲀的游泳行为,测量了其爆发游速及临界游速,同时观察了鱼体过氧化氢酶、溶菌酶、超氧化物歧化酶等的活性变化,分析了游泳对菊黄东方鲀免疫力影响,为菊黄东方鲀的健康养殖及科学的增殖放流提供参考。结果表明:体长在（18.1-19.8）cm的菊黄东方鲀的临界游速在45-62cm/s,体长在（18.8-20.6）cm的菊黄东方鲀的爆发游速为（58.5-78.2）cm/s;与对照组相比,爆发游速实验组菊黄东方鲀肝脏过氧化氢酶、溶菌酶、超氧化物歧化酶的活性均高于对照实验组菊黄东方鲀（P?0.05）;临界游速实验组菊黄东方鲀溶菌酶高于对照组（P?0.05）,血液中的超氧化物歧化酶和肝脏过氧化氢酶的活性没有显著变化(P>0.05)。研究表明,急性应激反应对超氧化物歧化酶、过氧化氢酶、溶菌酶的活性影响较大。     

达州市经济作物产业发展现状与对策

通过分析达州市经济作物产业发展现状和存在的问题,提出了促进当地经济作物产业发展的对策建议,为推动地区特色经济作物产业高质量发展提供参考。     

济源市蔬菜产业发展现状与对策

对济源市蔬菜产业的生产、销售、管理等现状进行了调查,指出当前蔬菜产业发展中存在的主要问题,结合济源市蔬菜产业实际情况,提出相应的发展对策。     

膜孔灌肥液自由入渗硝态氮运移特性试验研究

以KNO3为入渗溶液,模拟研究了硝态氮在膜孔灌肥液自由入渗条件下的运移过程.结果表明,在湿润蜂运移的范围内,沿着膜孔水平方向和垂直方向,硝态氮前锋运移速率受土壤含水量的影响较大,并随着土壤含水量的增加而增加;硝态氮前锋运移速率与运移距离有很好的相关性,并随着运移距离的增加呈幂函数衰减变化.硝态氮前锋浓度随着运移距离的增加而升高,其变化趋势呈指数曲线关系,且在湿润锋(土壤干湿交界)面上达到最大值;硝态氮前锋浓度随土壤含水量的增加呈幂函数递减,两者的相关系数也达到了极显著水平.     

新疆奶牛产业化现状与发展对策

针对新疆奶牛业的发展实际,文章分析了新疆奶牛生产目前存在的主要问题及原因,阐述了新疆奶牛业的发展潜力和目标,并从七个方面提出了加快奶业发展的基本思路和关键措施.最后指出要加快奶牛产业化发展,首先应提高认识,重视奶牛品种改良、科技推广、种草养牛和加快奶产品加工流通等,同时政府应给予必要的引导和扶持.     

美国兽医生物制品现状和发展趋势

就近年来美国兽用生物制品的发展现状进行了综述,并在此基础上对未来的发展趋势进行展望。     

Reinvestigation of the scaling law of the windblown sand launch velocity with a wind tunnel experiment

Windblown sand transport is a leading factor in the geophysical evolution of arid and semi-arid regions. The evolution speed is usually indicated by the sand transport rate that is a function of launch velocity of sand particle, whichhasbeen investigated by the experimental measurement and numerical simulation. However, the obtained results in literatures are inconsistent. Some researchers have discovered a relation between average launch velocity and wind shear velocity, while some other researchers have suggested that average launch velocity is independent of wind shear velocity. The inconsistence of launch velocity leads to a controversy in the scaling law of the sand transport rate in the windblown case. On the contrary, in subaqueous case, the scaling law of the sand transport rate has been widely accepted as a cubic function of fluid shear velocity. In order to explain the debates surrounding the windblown case and the difference between windblown and subaquatic cases, this study reinvestigates the scaling law of the vertical launch velocity of windblown transported sand particles by using a dimensional analysis in consideration of the compatibility of the characteristic time of sand particle motion and that of air flow. Then a wind tunnel experiment is conducted to confirm the revisited scaling law, where the sand particle motion pictures are recorded by a high-speed camera and then the launch velocity is solved by the particle tracking velocimetry. By incorporating the results of dimensional analysis and wind tunnel experiment, it can be concluded that, the ratio of saltonsnumber to reptonsnumberdetermines the scaling law of sand particle launch velocity and that of sand transport rate, and using this ratio is able to explain the discrepancies among the classical models of steady sand transport. Moreover, the resulting scaling law can explain the sand sieving phenomenon: a greater fraction of large grains is observed as the distance to the wind tunnel entrance becomes larger.     

Influence of salinity and moisture on the threshold shear velocity of saline sand in the Qarhan Desert,Qaidam Basin of China: A wind tunnel experiment

Determination of the threshold shear velocity is essential for predicting sand transport, dust release and desertification. In this study, a wind tunnel experiment was conducted to evaluate the influence of salinity and moisture on the threshold shear velocity of saline sand. Saline sand samples (mean particle size of 164.50-186.08 μm and the total silt, clay and salt content of 0.80%-8.25%) were collected from three saline sand dunes (one barchan dune and two linear dunes) in the Qarhan Desert, Qaidam Basin of China. Original saline sand samples were placed in two experimental trays for wet and dry processing to simulate deliquescence and desiccation, respectively. Surface moisture content ranging from 0.30% to 1.90% was generated by the steam method so that the saline sand can absorb water in a saturated water vapor environment. The motion of sand particles was determined by the observers with a solid laser. The laser sheet (0.80 cm thick), which was emitted by the solid laser, horizontally covered the sand surface and was bound to the sand. Results show that the cohesion of saline sand results from a combination of salt and water. The threshold shear velocity increases exponentially with the increase in crust thickness for the linear sand dunes. There is a positive linear correlation between the original moisture content and relative threshold shear velocity. The threshold shear velocity of dewatered sand is greater than that of wet sand with the same original moisture content. Our results will provide valuable information about the sand transport of highly saline soil in the desert.