崇明岛种子植物区系及植被资源

崇明岛共有区系植物55科157属198种，区系组成复杂，地理成分多样，涵盖全部15个分布区类型，具有明显的热带-温带过渡性质，落叶树种占木本植物种类的90．5％，属于北亚热带常绿落叶阔叶混交林地带。群落外貌及属的相似性系数分析表明，崇明岛植物区系更接近江苏宜兴，而与临近的大金山岛和佘山差别略大。此外，岛上还有栽培植物和外来植物共235种，其中蔷薇科、菊科、禾本科、豆科、木犀科等科的种类较丰富，以加拿大一枝黄花、臭荠、刺果毛莨、一年蓬、空心莲子草、大米草、互花米草等对当地植被资源和生态系统的影响最大。崇明岛植物群落结构单一，缺乏灌木层，草本层多为广布杂草，其植被资源可以根据功能划分为江防海防林、湿地植被、道路绿化带、庭院景观林、游憩林、大田作物及经济林、水源涵养林等7大类，其中江防海防林及湿地植被是崇明岛植被生态系统的关键成分。提供了崇明岛新纪录野生及外来种子植物名录。     

UASB处理离子交换树脂生产废水的试验研究

本研究主要介绍，尝试采用UASB（Upflow Anaerobic Sludge Bed）反应器厌氧工艺处理某离子交换树脂生产废水试验。研究表明，在中温（37℃±1）环境下，容积负荷在6．0-7．0kgCODcr·m^-3·d^-1时，CODcr去除率维持在80％左右，运行稳定。本试验取得的试验效果，为以后的利用厌氧技术处理离子交换树脂生产废水提供了重要依据。     

催化臭氧氧化法处理甲醛废水

用异丙醇钛盐表面改性法制备TiO2／SiO2催化剂，对甲醛废水进行催化臭氧氧化处理。通过比表面积的BET测定法、X射线衍射和拉曼光谱等分析方法对TiO2／SiO2催化剂进行了表征，考察了TiO2／SiO2催化剂加入量、臭氧流量及溶液pH等因素对甲醛催化臭氧氧化效果的影响。实验结果表明，在SiO2表面，TiO2微晶粒子以锐钛矿型高度分散；在甲醛质量浓度700mg／L、COD1000mg／L、TiO2／SiO2催化剂加入量2．0g、臭氧流量2．5mg／min、溶液pH8．5的条件下，催化臭氧氧化反应30min后，甲醛质量浓度由700mg／L降至39mg／L，COD去除率认到87．5％．     

深圳市新一代暴雨强度公式的研制

首先构造了深圳市新一代暴雨强度公式研制的路线图，重点是利用深圳市气象局1954-2003年50年间的暴雨记录，用指数分布和P-Ⅲ分布进行分布曲线拟合和选优，得到了理论上的雨强-历时-重现期三联表，在此基础上再分别采用最优法、二分搜索法和广义逆法等3种方法求解分公式和总公式参数，根据误差最小的原则确定最优方法。结果表明：由指数分布拟合分布曲线，经过上述步骤求解得到的公式参数，误差最小，符合相关国标要求。     

Effects of aluminum on physiological metabolism and antioxidant system of wheat (Triticum aestivum L.)

We have found that rice bran effectively adsorbed chloroform from tap water. The amount of chloroform adsorbed was plotted against the equilibrium concentration of chloroform in solution on a logarithmic scale. A linear relationship was obtained, indicating that the adsorption reaction was a Freundlich type. The removal of chloroform by rice bran was attributed to the uptake into intracellular particles called spherosomes.     

渤海海域环境现状及保护对策

根据沿海地区陆源污染调查材料,评价了渤海海域的环境质量现状,指出了渤海近岸海域污染严重,生态受到影响,离岸深水海域水质尚好。进而分析了其污染原因,提出了保护渤海环境的对策。      

临界距离老空水下薄煤层联合开采安全性分析

以现场实测结果为基础 ,利用数值模拟与反演方法分析了薄煤层联合开采的顶、底板破坏范围。根据分析的结果评价了临界距离老空水下薄煤层联合开采的安全性。     

特金罕山森林生态系统自然保护区规划研究

本文阐述了建立特金罕山自然保护区的目的、意义和保护对象,对自然保护区的现状进行了详细评价,得出了基本具备省级自然保护区条件的结论。阐述了特金罕山自然保护区规划的原则、目标及功能分区,对自然保护区进行了规划研究。     

负载型催化剂光催化氧化五氯苯酚钠的效果

研究以TiO₂ 为基本活性组分、空心玻璃珠为载体、硅酸钠为粘合剂的负载型催化剂的制备技术 .选取五氯苯酚钠 (PCP-Na)为处理对象 ,结合对催化剂比表面和晶型结构的表征 ,对制备的催化剂进行筛选评价 .实验结果表明 :在适当的条件下 (二氧化钛、空心玻璃珠、40%硅酸钠溶液重量比为 4∶20∶2,650℃下烧 3h)所制备的C3型催化剂不仅光催化活性高 ,且负载牢固 ,易与水分离 .对初始COD_Cr=400mg·L^-1,PCP-Na=10mg·L^-1的反应液 ,在光照强度为 30kW·m^-2下 2hCOD_Cr去除率大于 65% ,PCP-Na去除率大于 92%.试验进一步探讨C3型催化剂投加量、反应液初始浓度、供氧量对催化反应的影响 .     

Variations in global temperature and precipitation for the period of 1948 to 2010

Climate change has impacts on both natural and human systems. Accurate information regarding variations in precipitation and temperature is essential for identifying and understanding these potential impacts. This research applied Mann–Kendall, rescaled range analysis and wave transform methods to analyze the trends and periodic properties of global and regional surface air temperature (SAT) and precipitation (PR) over the period of 1948 to 2010. The results show that 65.34 % of the area studied exhibits significant warming trends (p?<?0.05) while only 3.18 % of the area exhibits significant cooling trends. The greatest warming trends are observed in Antarctica (0.32 °C per decade) and Middle Africa (0.21 °C per decade). Notably, 62.26 % of the area became wetter, while 22.01 % of the area shows drying trends. Northern Europe shows the largest precipitation increase, 12.49 mm per decade. Western Africa shows the fastest drying, ?21.05 mm per decade. The rescaled range analysis reveals large areas that show persistent warming trends; this behavior in SAT is more obvious than that in PR. Wave transform results show that a 1-year period of SAT variation dominates in all regions, while inconsistent 0.5-year bands are observed in East Asia, Middle Africa, and Southeast Asia. In PR, significant power in the wavelet power spectrum at a 1-year period was observed in 17 regions, i.e., in all regions studied except Western Europe, where precipitation is instead characterized by 0.5-year and 0.25-year periods. Overall, the variations in SAT and PR can be consistent with the combined impacts of natural and anthropogenic factors, such as atmospheric concentrations of greenhouse gases, the internal variability of climate system, and volcanic eruptions.