Role of glycine on sulfuric acid-ammonia clusters formation: Transporter or participator

Glycine(Gly) is ubiquitous in the atmosphere and plays a vital role in new particle formation(NPF).However,the potential mechanism of its on sulfuric acid(SA)-ammonia(A)clusters formation under various atmospheric conditions is still ambiguous.Herein,a(Gly)_x·(SA)_y·(A)_z(z≤x+y≤3) multicomponent system was investigated by using density functional theory(DFT) combined with Atmospheric Cluster Dynamics Code(ACDC) at different temperatures and precursor concentrations.The results show that Gly,with one carboxyl(-COOH) and one amine(-NH_2) group,can interact strongly with SA and A in two directions through hydrogen bonds or proton transfer.Within the relevant range of atmospheric concentrations,Gly can enhance the formation rate of SA-A-based clusters,especially at low temperature,low [SA],and median [A].The enhancement(R) of Gly on NPF can be up to 340 at T=218.15 K,[SA]=10~4,[A]=10~9,and [Gly]=10~7 molecules/cm~3.In addition,the main growth paths of clusters show that Gly molecules participate into cluster formation in the initial stage and eventually leave the cluster by evaporation in subsequent cluster growth at low [Gly],it acts as an important "transporter" to connect the smaller and larger cluster.With the increase of [Gly],it acts as a "participator" directly participating in NPF.     

污染物在地下水毛细饱水带的运移规律浅释

分析了毛细饱水带的水动力学特性，指出在地下水污染研究中，污染物在毛细饱和水带和潜水怪具有相同的水平运动规律，并以实例分析说明该带对污染物运移的重要性。建议在研究和一非饱和条件地下水及污染物运动问题时把毛细饱水带与潜水含水层统一为饱马毛细饱水带顶面作为饱水面。     

Biological complexity confounds the separation of point- and non-point sources of human impact on the natural world

Identifying process from pattern is one of the most vexing tasks inenvironmental monitoring. Given information on the distribution of speciesin a pre-defined area, together with comprehensive data on how environmentalconditions in that area have altered through time, is it possible toidentify the factors controlling the species‘ layout? Here, the practicalsignificance of this quandary is demonstrated using a series ofenvironmentally-degraded coastal lagoons in New South Wales. The TuggerahLakes (33°17′S,151°30′E) have over the last 50 yearsexperienced significant changes in species‘ distributions. Seagrasses,macroalgae, phytoplankton, molluscs, prawns and the jellyfish Catostylus mosaicus have altered in spatial pattern. Two human activitieshave been blamed for these perturbations: (1) agricultural clearance ofnative vegetation from the catchment, with associated input of top-soil andnutrients; (2) the commissioning of a coal-fired power station in 1967, withmassive uptake and recirculation of lake water for cooling purposes. In thispaper, spatial changes in macrophyte distributions over the last 50 yearsare reviewed in an attempt to identify the true source(s) of perturbation.The model adopted assumes that the power station is a point source of impactwhile nutrient inputs from the catchment are a diffuse source of impact;changes in species distributions can hypothetically be related back to thesesources according to whether they are localised or widespread. However,after a comprehensive analysis of available macrophyte data derived frominterviews, aerial photography and line transect methodologyies theconclusion is reached that changes in biogeographical pattern around theTuggerah Lakes cannot be attributed to specific anthropogenic pressures atanything beyond the coarsest of levels. This is considered to be the normfor most coastal management situations where natural background variation(’noise‘) and the complexity of linkages between physical, chemical andbiological components confounds the identification of causal relationships.The practical implications of this conclusion are discussed in the contextof litigation and remedial management design. Emphasis is placed on theneed to adopt an adaptive approach to estuarine management, incorporatingexplicit recognition of the limitations of available data, and to developnew techniques for identifying cause-effect relationships.     

论生物多样性的价值

从经济学角度论述了生物多样性的价值 ,并从三方面论述了生物多样性受到的威胁可能会给人类带来的危害 ,从经济价值角度揭示了保护生物多样性的重要意义。     

安徽张八岭地区构造演化及动力学

对张八岭地区的构造特征、演化及其动力学有不同解释。通过1：5万张八岭幅、珠龙幅区域地质调查．从地层、岩石组合、岩石化学、岩浆岩、构造变形和变质等研究认为．该区从中新元古代起，经历了成谷、沉积．下沉、顺层剪切、深部熔融、塑性流动、层间褶皱．叠加折劈、宽缓褶曲、逆掩推覆，壳层滑动、熔融成浆、聚浆热隆、侵入或喷发．剥蚀夷平、堆积充填等铸成现今地貌景观．引起上述构造特征和演化的动力源自重力、热力和地球自转速率变化的惯性离心力等的结合与转化，它们在每个阶段各自所起的作用不同，就产生不同构造特征，推动区域构造演化．     

Differential N uptake by maize cultivars and soil nitrate dynamics under N fertilization in West Africa

Nitrate is prone to leaching in the sandy soils of the West African moist savannas. Better management of nitrogen (N) resources and maize cultivars with enhanced genetic capacity to capture and utilize soil and fertilizer N are strategies that could improve N-use efficiency. In two field experiments conducted at Zaria, northern Nigeria, five maize (Zea mays L.) cultivars planted early in the season were assessed under various N levels for differences in N uptake, soil N dynamics, and related N losses. Cultivar TZB-SR accumulated more N in the aboveground plant parts in both years than the other cultivars. All, except the semi-prolific late (SPL) variety, met about 50–60% of their N demand by the time of silking (64–69 DAP). In both years, SPL had the greatest capacity to take up N during the grain filling period, and it had the highest grain-N concentration and the least apparent N loss through leaching in the second year. There were no significant differences in soil N dynamics among cultivars in both years. At harvest, the residual N in the upper 90 cm of the profile under all the cultivars ranged from 56 to 72 kg ha⁻¹ in the first year and from 73 to 83 kg ha⁻¹ in the second year. Apparent N loss from 0 to 90 cm soil profile through leaching ranged from 35 to 122 kg ha⁻¹ in both years. N application significantly increased N uptake by more than 30% at all sampling dates in the second year of the experiment, but had no effect on apparent N loss. Results indicate that the use of maize cultivars with high N uptake capacity during the grain filling period when maximum leaching losses occur could enhance N recovery and may be effective in reducing leaching losses of mineral N in the moist savanna soils.     

环境模型的统计评价

系统地探讨了评价模型的统计指标,并在BOD反应动力学模型中使用,取得了较好的效果。     

长江三角洲生态系统的近代演化特征及其生态与环境问题分析

长江三角洲主要生态系统类型包括河流生态系统、河口海岸湿地生态系统、农林生态系统、城市生态系统、湖泊生态系统以及近海海域生态系统，、长江三角洲是人类和自然相互作用的结果．具有明显的生态边缘效应．支持了长江三角洲丰富的动植物区系。文章分析了长江三角洲地区主要生态系统的演化特征及其相互关系：阐述了长江三角洲地区主要生态系统在城市化进程中所面临的生态与环境问题．从系统生态学的角度对长江三角洲地区主要自然生态系统的修复和保护提出了对革。同时分析了流域治理和区域治理的重要性．这对于长江三角洲地区社会和经济的可持续发展具有重要的指导意义。     

电催化氧化技术处理硝基苯废水的试验研究

用实验室自制的活性炭粒子填充电极电催化氧化反应器对模拟硝基苯废水进行了降解处理。初步探讨电催化氧化反应的机理,考察了电流强度、反应时间、进水浓度等对硝基苯去除率的影响。用一元线性回归方程对不同初始浓度和电流强度降解后硝基苯的相对残余浓度对反应时间的相关性进行了分析,结果发现相关系数大于临界相关系数,硝基苯的降解符合表观一级反应动力学模型,求出了各反应条件下的一级速率常数。通过用spss软件分析,表明不同的初始浓度和电流强度下ln(C0/C)对时间的相关性显著。实验结果表明,在本实验条件下,硝基苯的去除率达到95%以上,能有效的催化降解硝基苯。