KClO3对龙眼产期的调控效应

以自行配制、主要有效成份为KClO3的龙眼产期调控剂进行田间试验．结果表明：催花土壤施用剂量以每平方米树冠面积180g效果最佳；不同品种龙眼对药物的敏感程度不同，以石硖、储良龙眼最为敏感，平均抽花率可达80％以上．不同季节和不同梢期施药，龙眼抽花率存在显著差别；药剂干施回泥后淋水、干施淋水后回泥和拌水淋施这3种土壤给药方式的促花效果差异不显著；反季节与正造栽培收获的龙眼相比，果实质量存在一定差异，春季收获的果实个大肉厚，外观较佳，但糖份含量等品质指标则较差．KClO3调控龙眼产期的效果明显，配合相应的树体管理和土壤水分养分调控措施，可实现龙眼产期的人工合理控制．表7参20     

盾壳霉CCTCC M203020的生长特性及其应用潜力

以油菜菌核病病株菌核为诱饵，从油菜地中分离筛选得到一株盾壳霉(Coniothyrium minitans CCTCC M203020)．以生物防治能力好的CBS148．96为对照菌株，比较了两者在油菜叶上对油菜菌核病菌抑制作用和在土壤中对菌核的致腐能力及条件．结果表明：C．minitans CCTCC M203020对油菜菌核病菌的抑制作用及适用的pH范围(4．0～7．0)均优于CBS148．96，适片于油菜菌核病的生物防治．具体表现在：(1)C．minitans CCTCC M203020能够完全限制病原菌在叶面的进一步扩展(已萌发孢子率为800A时)，而CBS148．96则不能；(2)C．minitaras CCTCC M203020与CBS148．96的生长特性及培养条件相近，但其菌体生长和孢子产量分别高出60％和12％，并发现该菌株在PDA上产生孢子的最短周期是3．5～4d，较优培养条件为：20℃、初始pH5．0～6．2、空气湿度90％～97％；敛腐菌核的较优条件为：10^1～10^4孢子／菌核，土壤湿度80％～100％，pH4．0～7．0，图7参19     

UV-B辐射增强对冬小麦生长发育及产量的影响

研究了大田栽培条件下紫外辐射增强对冬小麦孕穗、抽穗、开花、灌浆、结实以及产量的影响。结果表明,UV B辐射增强使小麦植株矮化,叶面积减小,穗重、茎重、叶重减小,灌浆速度变慢,灌浆不充实,此外,UV B辐射增强还使花粉败育率增大。     

Growth and pollution convergence: Theory and evidence

Stabilizing pollution levels in the long run is a pre-requisite for sustainable growth. We develop a neoclassical growth model with endogenous emission reduction predicting that, along optimal sustainable paths, pollution growth rates are (i) positively related to output growth (scale effect) and (ii) negatively related to emission levels (defensive effect). This dynamic law reduces to a convergence equation that is empirically tested for two major and regulated air pollutants – sulfur oxides and nitrogen oxides – with a panel of 25 European countries spanning the years 1980–2005. Traditional parametric models are rejected by the data. More flexible regression techniques confirm the existence of both the scale and the defensive effect, supporting the model predictions.     

地震的社会经济影响

在查阅前人研究成果的基础上,分析了地震造成社会灾害严重、影响地区经济发展的现象,认为地震灾害对一个地区所造成的影响程度与该地区的承灾力有关,并影响地区经济的可持续发展.     

The resource curse revisited and revised: A tale of paradoxes and red herrings

We critically evaluate the empirical basis for the so-called resource curse and find that, despite the topic's popularity in economics and political science research, this apparent paradox may be a red herring. The most commonly used measure of “resource abundance” can be more usefully interpreted as a proxy for “resource dependence”—endogenous to underlying structural factors. In multiple estimations that combine resource abundance and dependence, institutional, and constitutional variables, we find that (i) resource abundance, constitutions, and institutions determine resource dependence, (ii) resource dependence does not affect growth, and (iii) resource abundance positively affects growth and institutional quality.     

Urban expansion and its contribution to the regional carbon emissions: Using the model based on the population density distribution

The method is used for calculating regional urban area dynamics and the resulting carbon emissions (from the land-conversion) for the period of 1980 till 2050 for the eight world regions. This approach is based on the fact that the spatial distribution of population density is close to the two-parametric Γ-distribution [Kendall, M.G., Stuart, A., 1958. The Advanced Theory of Statistics, vol. 1.2. Academic Press, New York; Vaughn, R., 1987. Urban Spatial Traffic Patterns, Pion, London]. The developed model provides us with the scenario of urbanisation, based on which the regional and world dynamics of carbon emissions and export from cities, and the annual total urban carbon balance are estimated. According to our estimations, world annual emissions of carbon as a result of urbanisation increase up to 1.25 GtC in 2005 and begin to decrease afterwards. If we compare the emission maximum with the annual emission caused by deforestation, 1.36 GtC per year, then we can say that the role of urbanised territories (UT) in the global carbon balance is of a comparable magnitude. Regarding the world annual export of carbon from UT, we observe its monotonous growth by three times, reaching 505 MtC. The latter, is comparable to the amount of carbon transported by rivers into the ocean (196–537 MtC). The current model shows that urbanisation is inhibited in the interval 2020–2030, and by 2050 the growth of urbanised areas would almost stop. Hence, the total balance, being almost constant until 2000, then starts to decrease at an almost constant rate. By the end of the XXI century, the total carbon balance will be equal to zero, with the exchange flows fully balanced, and may even be negative, with the system beginning to take up carbon from the atmosphere, i.e., becomes a “sink”. The regional dynamics is somewhat more complex, i.e., some regions, like China, Asia and Pacific are being active sources of Carbon through the studied period, while others are changing from source to sink or continue to be neutral in respect the GCC.