推车式离心雾化喷雾机性能试验研究

对推车式离心雾化喷雾机进行性能试验研究，研究旋转式离心雾化特征、雾滴直径、雾滴沉降分布规律、雾滴沉积密度均匀性、风送低量喷雾效果等，掌握各参数相互匹配关系与工作机理，为进一步优化改进、产业化设计、关键部件精确工艺研究等提供技术支撑。     

Orographic enhancement of wet deposition in the United Kingdom: case studies and modelling

Two field experiments to observe the detailed response of wet deposition to orography in a polluted environment are reported. Rain events were classed as frontal, convective or mixed on the basis of meteorological data. Analysis of the deposition enhancement and cap cloud composition confirmed that for the frontal events the seeder-feeder effect (scavenging of cap cloud by rain drops) dominates. The greater concentration of ions in the water scavenged from the cap cloud than in the rain means that deposition is enhanced for all ions. For marine ions the scavenged water was found to be between five and six times as concentrated as the rain and for anthropogenically produced ions it was about twice as concentrated.A computational model of rainfall incorporating the seeder-feeder effect has been broadly successful in predicting enhancement although some details of the observed pattern remain to be explained.     

Multi-scale system approaches in agronomic research at the landscape level

Spatial multi-scale analyses of actual land use system performance as determined by spatial yield variability reveals the need for landscape research in agronomy. Main ‘drivers’ of spatial yield variability for five different crops in Honduras, Costa Rica and Ecuador were identified. It is demonstrated how they vary with spatial scales and that landscape-related factors often play a large and significant role in when the variability in yield is determined. These results indicate that landscape experiments in agronomy are relevant. Apart from empirical analysis, spatial–temporal explicit modeling of landscape process dynamics such as water and soil redistribution within a landscape can give insight in the performance of agronomic systems within a dynamic landscape context. For a case study in the South of Spain it is demonstrated how within a landscape this type of research can determine the on- and off-site effects of water and soil redistribution in agro-ecosystems. Only after a spatially explicit multi-scale system analysis and explorative landscape process modeling is completed, relevant agronomic landscape experiments can be designed.     

横、顺坡垄作对黑土坡面侵蚀-沉积周期规律的影响

我国东北黑土区的水土流失和土地退化正严重制约着东北地区农业经济发展,威胁国家粮食生产安全。掌握不同垄作方向耕作措施下的东北黑土区土壤侵蚀规律,对合理布设水保措施、控制水土流失等具有重要意义。采用¹³⁷Cs示踪技术并结合小波分析方法,对不同垄作方向坡耕地土壤侵蚀-沉积速率的空间变化规律开展研究。结果表明：(1)横、顺坡垄作坡面¹³⁷Cs平均浓度分别为1 802 Bq·m^-2和1 770 Bq·m^-2,均小于当地背景值2 417 Bq·m^-2,说明在两种垄作方向下均发生了不同程度的土壤侵蚀。(2)横坡垄作的坡面平均侵蚀速率(1 341 t·km^-2·a^-1)小于顺坡垄作(1 477 t·km^-2·a^-1),表明在长期平均条件下前者的水土保持作用优于后者。尽管研究区土壤侵蚀属于轻度侵蚀,但其侵蚀速率远大于黑土区的土壤容许流失量(200 t·km^-2·a^-1     

基于CNN的FDM型3D打印故障诊断方法

热熔堆积(FDM)型3D打印时易受外部环境和参数设置的影响而发生故障,造成打印件的失败。为避免成型过程失败后继续打印,造成材料和时间的浪费,提出热熔堆积型3D打印故障自动诊断方法。该系统基于卷积神经网络(Convolutional Neural Network,CNN)的图像识别技术,通过监视、分析打印成型中零部件表面的图像信息,判断打印进程中是否发生故障。     

固始鸡、罗曼蛋雏鸡和艾维茵肉仔鸡生长、养分沉积、肉质特性的比较研究

通过研究固始鸡、罗曼蛋雏鸡和艾维茵肉仔鸡生长、养分沉积、肉质特性的差异,探讨品种与生长、代谢和肉质间的关系。选用1日龄雄性固始鸡、艾维茵肉仔鸡、罗曼蛋雏鸡各120只,按体重随机分为6个重复,每重复20只,在相同日粮条件下进行8周的生长试验,并进行屠宰试验和肉质测定。结果表明:(1)3种鸡在体重、日增重、采食量、饲料转化率间存在极显著差异(P<0.01),固始鸡低于罗曼蛋雏鸡,罗曼蛋雏鸡低于艾维茵肉仔鸡;(2)固始鸡和罗曼蛋雏鸡的代谢能和粗蛋白质沉积效率显著低于艾维茵肉仔鸡(P<0.05);(3)固始鸡和罗曼蛋雏鸡的肌肉滴水损失、肌纤维直径、羟脯氨酸含量显著低于艾维茵肉仔鸡(P<0.05),固始鸡胸肌和腿肌中超氧化物歧化酶活性则极显著高于蛋鸡(P<0.01),蛋鸡极显著高于肉鸡(P<0.01)。与快速生长的鸡品种相比,慢速生长的固始鸡具有较低的代谢能和粗蛋白质沉积效率,具有较低的肌肉滴水损失、羟脯氨酸含量及较细的肌纤维,并具有较高的肌肉抗氧化水平。     

主要营养素在动物体内的分配沉积调控机制研究进展

主要营养素——蛋白质和脂肪在动物体内的分配沉积方式与动物的生长和生产性能密切相关。充分认识主要营养素在动物体内的分配沉积调控机理,将为通过营养调控、基因工程等技术实现定向调控蛋白质和脂肪在动物体内的分配沉积提供重要的理论依据。综述了蛋白质和脂肪在动物体内分配沉积调控机制的研究进展,以便为通过定向调控营养素在动物体内的分配沉积,从而提高动物的生长和生产性能提供参考。     

大气干湿沉降向城市系统输入重金属元素通量特征研究——以沈阳市为例

[目的]探讨大气干湿沉降向城市系统输入重金属元素通量特征.[方法]根据沈阳市不同行政区采样点重金属元素沉降通量,分析沈阳市不同行政区重金属大气干湿沉降污染的空间分布特征.[结果]在不同的采样点,大气干湿沉降中元素的年沉降通量差异较大,但其在沈阳市不同行政区分布规律大致相同.Cd、Pb、Hg的年沉降通量在各地区的分布分别表现为：铁西区＞皇姑区＞沈河区＞和平区＞大东区＞东陵（浑南）区＞于洪区,铁西区＞沈河区＞皇姑区＞和平区＞东陵区＞于洪区＞大东区＞浑南区,铁西区＞沈河区＞皇姑区＞和平区＞大东（东陵）区＞于洪（浑南）区.大气降尘污染的空间分布与污染源地域分布具有一致性,即工业区＞商业区或交通区＞文化区＞居民区＞郊区.[结论]该研究为大气干湿沉降污染的控制与治理提供了理论参考.     

Carbon distribution and losses: erosion and deposition effects

Because of concerns about the eventual impact of atmospheric CO₂ accumulations, there is growing interest in reducing net CO₂ emissions from soil and increasing C storage in soil. This review presents a framework to assess soil erosion and deposition processes on the distribution and loss of C in soils. The physical processes of erosion and deposition affect soil C distribution in two main ways and should be considered when evaluating the impact of agriculture on C storage. First, these processes redistribute considerable amounts of soil C, within a toposequence or a field, or to a distant site. Accurate estimates of soil redistribution in the landscape or field are needed to quantify the relative magnitude of soil lost by erosion and accumulated by deposition. Secondly, erosion and deposition drastically alter the biological process of C mineralization in soil landscapes. Whereas erosion and deposition only redistribute soil and organic C, mineralization results in a net loss of C from the soil system to the atmosphere. Little is known about the magnitude of organic C losses by mineralization and those due to erosion, but the limited data available suggest that mineralization predominates in the first years after the initial cultivation of the soil, and that erosion becomes a major factor in later years. Soils in depositional sites usually contain a larger proportion of the total organic C in labile fractions of soil C because this material can be easily transported. If the accumulation of soil in depositional areas is extensive, the net result of the burial (and subsequent reduction in decomposition) of this active soil organic matter would be increased C storage. Soil erosion is the most widespread form of soil degradation. At regional or global levels its greatest impact on C storage may be in affecting soil productivity. Erosion usually results in decreased primary productivity, which in turn adversely affects C storage in soil because of the reduced quantity of organic C returned to the soil as plant residues. Thus the use of management practices that prevent or reduce soil erosion may be the best strategy to maintain, or possibly increase, the worlds soil C storage.     

SOIL NITROGEN MINERALIZATION UNDER NORTHERN HARDWOOD FORESTS ALONG A SULFATE AND NITRATE DEPOSITION GRADIENT IN THE GREAT LAKES REGION

INTRODUCTIoNChangesinsoilNmineralizationratescouIdbeanearlywarningofsoilNavaila-bilityoreventualforestdeclinesinceNisoftenan.importantnutrientforgrowth(Keeneyl98O;Leaetal.l982;Vitouseketal-l982).Nitrogenmineralizationinvolvestwodistinctprocessesfammonification,inwhichNH:isformedfromorganiccom-pounds,andnitrification,theoxidationofNH:toNO3.ManystudiesofatmosphericdepositionimpactsonforestshavetargetedsoilNmineraIizationusingsimulatedaciddepositionundercontrolledlaboratoryconditions(T…