6WC-30Y-G型车载式超低容量喷雾机的研制

喷雾机是森林病虫害防治中的主要设备之一,传统的化学防虫不可避免地会造成农药浪费和环境污染。本文综述了基于风送液力式喷雾技术而设计开发的6WC-30Y-G型车载式超低容量喷雾机的主体结构、技术参数和工作原理。     

超导陀螺转子偏移建模与测试方案

根据球形差动电容传感器测量微位移的原理,针对八电极结构的超导陀螺仪分析了每对测量电极上悬浮转子偏移量与电容变化量间的关系.通过无量纲化和微位移范围内线性化处理及利用最小二乘算法,建立了转子偏移测量模型.给出了基于该模型的超导陀螺转子偏移测试方案及其各参数间的关系.分析了影响陀螺转子偏移测量精度的因素.超导陀螺转子偏移测试方案的特点是为保证悬浮转子的零电位而采用4对测试电极的电极分布法,能同时测量出转子偏移的大小和偏移方向.实验结果表明,差动电容传感器的分布电容、陀螺转子的零电位和模型误差等是影响测量精度的主要因素.提出了降低相应因素不良影响的方法及输出电压与转子偏移量呈线性关系模型的适应范围.     

大额牛的群体生存现状与保种措施

本文阐述了大额牛的品种特性、种群现状和保种措施.大额牛保种可采用原产地活体保种,迁地活体保种和现代生物技术保种.大额牛体型较大,产肉性能好、行动敏捷、结构紧凑、肌肉发达、肉质优良、耐粗饲、适应性、繁殖力和抗病力均较强等特点.种群体数量极小.大额牛是云南省一个地方品种,保种工作刻不容缓.     

Spray drift: impact of requirements to protect the environment

Spray drift studies in the US have evaluated the effects of application, meteorological and tank mix variables on spray drift. The data have been incorporated into models to predict drift from aerial applications, and to evaluate worst-case drift from ground rig (boom) and orchard airblast applications. An atomisation model has also been developed to predict droplet size for applications of tank mixes with user-defined or reasonable worst-case physical properties through a wide range of hydraulic nozzles applicable to aerial applications. The database and models help provide the exposure risk input to risk assessments for developing appropriate labelling based on exposure and toxicity risk to non-target sensitive areas. This needs to be balanced with allowing crop protection using careful risk/benefit assessments. Buffers or no spray zones may be based on spray quality, release height and other variables such as wind speed where necessary for protecting specific sensitive areas. The impact of protection measures aimed at minimising the incidence and impact of spray drift is discussed in the present paper.     

语言学理论的发展及其应用

本文对西方语言学发展的各个阶段的主要流派、主要代表人物及其理论作了简要的介绍,同时对各流派理论的应用,包括该理论对中国语言文字比较研究上的应用也作出了简要的评论。     

蒙古羊的群体结构和遗传多态

用随机遗传漂变理论和扩散方程方法分析了蒙古羊的形成发展过程和不同地域群体的遗传多态现象，包括群体有效大小、世代间隔、世代重叠程度、角型、毛色、尾型的遗传变异及其成因。分析结果表明蒙古羊种群总体上属于大群体，群体有效大小约为１００万只，但由于分成许多小群体，因而使群体有效大小明显缩小，基因的随机遗传漂变作用导致各群体中广泛存在遗传多态并且特长期存在。     

古尔班通古特沙漠腹地输沙风能及地貌学意义

根据古尔班通古特沙漠腹地2个气象台站2003-2006年气象资料,分析起沙风况和输沙势,并对其地貌学意义进行探讨。结果表明：沙漠中部全年起沙风出现频率为0.25%,以东北风和西北风为主;南部起沙风出现频率为0.11%,以西北风和西南风为主。沙漠中部和南部均属于低风能环境,中部地区的总输沙势（DP）为66.7VU,合成输...     

Riverine spawning,long distance larval drift,and floodplain recruitment of a pelagophilic fish: A case study of golden perch (Macquaria ambigua) in the arid Darling River,Australia

1. Pelagic spawning riverine fish (pelagophils) spawn in free‐flowing river habitats with downstream drift of eggs and larvae but the spatial scale is often unknown, and this constitutes a major ecological knowledge gap.
2. In the arid Darling River in south‐eastern Australia, the present objectives were: (i) to determine the potential downstream dispersal distance of young golden perch (Macquaria ambigua); and (ii) to evaluate whether provision of environmental water enhanced dispersal of young fish from Menindee Lakes to the lower Darling River (LDR) while also cueing further spawning in downstream lotic reaches.
3. Golden perch spawned in unregulated lotic tributaries on a flood pulse and larvae drifted or dispersed >1,600 km downstream and entered large ephemeral productive floodplain lake nursery habitats as fully scaled fingerlings.
4. Planned releases of environmental water cued golden perch spawning in the LDR and enabled juvenile fish to disperse downstream from the Menindee Lakes nursery into receiving populations in the LDR, Great Darling Anabranch, and southern Murray River, with some fish potentially completing an active migration of >2,100 km by age 1 year.
5. The Darling River case study highlights the need for a system‐scale approach to the conservation management of pelagophilic fish, along with multi‐year perennial flow strategies to improve ecosystem integrity in large rivers globally.

     

Larval lobster (Homarus americanus) distribution and drift in the vicinity of the Gulf of Maine offshore banks and their probable origins

Surveys for lobster larvae in offshore waters of the north‐eastern Gulf of Maine in 1983, 1987 and 1989 confirm that local hatching occurs mainly at depths <100 m over the banks, including Georges and Browns Banks. Detailed studies in the vicinity of Georges Bank in late July of both 1987 and 1989 indicate that the first and second moult stages were located primarily over the bank whereas stages III and IV lobster were collected both over and off the bank. At times stage IV lobster were more abundant off the bank than over it. The condition of stage III and IV lobster, as measured by a lipid index, was better off than over Georges Bank in 1988 and 1989 indicating a possible physiological advantage to being off the bank. In addition, the higher surface temperatures off Georges Bank would shorten larval development time to settlement. To determine the probable hatch sites of stage IV lobster collected off of Browns Bank in 1983 and off of Georges in 1987 and 1989, a 3‐D circulation model of the Gulf of Maine was used to simulate larval lobster drift backwards in time. In all cases, areas off Cape Cod, MA, and off Penobscot Bay, ME were suggested as the source of the larvae, although most of the larval trajectories never reached these near‐shore waters that are well‐known, larval hatching areas. The model‐projected larval release times match most closely the observed inshore hatch off Massachusetts but model uncertainties mean that coastal Maine cannot be ruled out as a source. Georges Bank is also a potential source because the present model does not take into account short‐term wind events, off‐bank eddy transport or the possibility of directed off‐bank larval swimming. Examination of weather records prior to and during our 1988 and 1989 sampling periods indicates that winds were not of sufficient intensity and duration to induce larval transport off Georges Bank. The shedding of eddies from the northern flank of Georges Bank into the Gulf of Maine are a relatively common phenomenon during summer but not enough is known about them to evaluate their contribution to possible cross‐bank transport of lobster larvae. Directed larval swimming is another possible source for the stage IV lobster found near Georges Bank. Plankton distributions across the northern frontal zone of Georges Bank in 1988 were used as proxies for the scarce larval lobsters. The more surface distribution of the microplankton, in particular, supports the possibility that wind and eddy events may be important in the transport of stage III and IV lobsters off of Georges Bank. Further studies are needed to evaluate these possible additional sources of advanced stage lobster larvae found off of the offshore banks.     

Can drifting objects drive the movements of a vulnerable pelagic shark?

1. Juvenile silky sharks (Carcharhinus falciformis) regularly associate with floating objects yet the reasons driving this behaviour remain uncertain. Understanding the proportion of time that silky sharks spend associated with floating objects is essential for assessing the impacts of the extensive use of fish aggregating devices (FADs) in the tropical tuna purse-seine fisheries, including increased probability of incidental capture and the potential of an ecological trap.
2. Previous studies provided insight into the amount of time that silky sharks spent at an individual FAD but were unable to assess neither the time spent between two associations nor the proportion of time spent associated/unassociated.
3. The percentage of time that juvenile silky sharks spend unassociated with floating objects was estimated through the analysis of horizontal movements of 26 silky sharks monitored with pop-up archival tags. Under the assumption that a high association rate with drifting FADs would align the trajectories of tracked sharks with ocean surface currents, a novel methodology is proposed, based on the comparison of shark trajectories with simulated trajectories of passively drifting particles derived using a Lagrangian model.
4. Results revealed that silky shark trajectories were divergent from surface currents, and thus unassociated with FADs, for at least 30% of their time. The potential of the methodology and the results are discussed in the context of increasing FAD densities in the Indian Ocean.