爷爷的菜园

正爷爷的菜园不大,种的蔬菜可不少。有穿着紫袍的茄子,它们戴着绿帽子,像是参加晚会的贵妇人一样。玉米的长势最好,一株株像小士兵一样,昂首挺胸地站在田边,神气十足。要是有不认识的人靠近它,它会举起红缨枪,瞄准入侵者。西红柿挂满枝头,像一盏盏红灯笼,照亮了整个菜园。豇豆最文静,像亭亭玉立的少女,一阵风吹来,摆动纤细的身体,翩翩起舞,很是好看。辣椒最威风,它们有的穿着碧绿的外套,有的穿着大红袍,很是耀眼,生怕别人看不到它们美丽的衣裳。朝天椒虽然不太显眼,但可爱炫耀自己了,像骄傲的公主。     

草根的优雅——写在三月,写给这些年的成长

你路过了你的风景,也行使了你应该行使的里程,不要心有不甘,不要挂档倒退,把该记住的记住,该剔除的剔除。三月,注定是属于女人的,草长莺飞,季节变迁,城市里弥漫着对女人的关注和赞美。2010年1月,我获得了成都市2009年度第三届职业丽人提名奖,3月,又获得了2010年十大魅力女川商。同时,又因为工作的原因,获得了总公司记大功的奖励。     

解放思想 高移目标 推动学校事业科学发展

在学校事业发展的新阶段,必须解放思想,高移目标,不断提升人才培养工作水平,不断提升富民强校水平,努力实现办学层次的新提升和办学空间的新拓展。要以科学发展观为指导,坚持稳中求进,坚持好字优先,坚持改革创新,坚持以人为本,夯实基础,彰显特色,增创新的发展优势。要上下团结一心,协调一致,形成合力,共同担负起促进学校事业又好又快发展的重任。     

阿拉斯加——让人钟爱一生的风景地

走进阿拉斯加,仿佛走进了气势恢弘的天然画廊。不同的季节,不同的时辰,这里呈现着不同的景色,有的色彩斑斓,如同浓彩重墨的油画;有的古朴俊秀,犹如水墨丹青的国画;有的刚劲有力,形如对比强烈的版画;有的清新雅致,恰似灵动飘逸的水彩画。无论黄昏还是黎明,无论是晴空万里还是烟雨朦胧,阿拉斯加的每个角落都有一种美丽,让你怦然心动,让你流连忘返,让你想把它放进自己的梦里,千年不醒。     

中国人物

一般来说,知道他,主要是通过两个故事以及这么一个成语——运筹帷幄之中,决胜千里之外。至于他是如何运筹又是如何决胜的,一般人就不会问了,无非权谋计算而已。他的第一个故事是,作为韩国的贵公子,为了替他的韩国报仇,他悉以家财,求得力士,制一百多斤的铁锥,埋伏在那博浪沙,冒险刺杀秦始皇,可惜那     

母爱

春天,母爱犹如和煦的微风,拂过稚嫩的花瓣;夏天,母爱犹如冰冻的冷饮,凉爽炽热的身体;秋天,母爱犹如金黄的落叶,点亮前进的道路;冬天,母爱犹如顽强的种子,等待生     

2009年度中国直销6大庆典

5周年,15周年,50周年……每一次直销企业的周年庆典,都向我们展示着直销企业的一次质变,象征着直销行业的一次成长。走过嗷嗷待哺的年月,走过激情燃烧的岁月,周年庆典的这些数字,都预示着直销企业已步入成熟稳重的中青年时代,开始在中国市场中散发出独特的魅力。周年庆典是实力的展示,是自我的激励,是成长的荣耀,同时也是一个平台:借着一幕幕的精彩表演,甚至是员工自己编排的节目,     

玉树的民风

玉澍偶地名,使人发生一样美感,为什么呢?我国的文人描写女人的漂亮,多喜欢用个玉字,所谓「亭亭玉立,所谓「燕度佳人,美者颜如玉」,都说不了「玉字,所以玉树纵里面的一个玉字,已很容易使人以为它是一个风景美丽的地方,虽不敢奢望如杭州的西湖,至少也如山东的青岛吧,其实单一个玉字,不能尽其妙处,它是玉树呀,玉的树是多么实真的东西呵,所以玉树二字不特     

个人信息保护立法亟待提速

“熙熙攘攘,皆为利来,皆为利往”,如此概括中国古代繁荣景象的一组词语,用在这里或许不太合适,但这恰恰成了互联网“泄漏门”利益链条中呈现出来的一个鲜活的画面.这画面很“热闹”,却让所有的网民倍感“揪心”. 看看我们的手机、翻翻我们的邮箱,每天海量的垃圾信息,充斥着我们的眼球.这还不算,更有甚者,接到莫名电话的骚扰,推销奶粉的,卖尿片的、卖治疗仪的、卖房的、投资的、开发票的等等,一度扰乱了一天平静的生活.     

给眼睛装上快门

抬头看看你周围的物体,圆的、方的,短的、长的,远的、近的……物体都是立体的,这就是立体感。当你闭上一只眼睛,或者用手挡住一只眼睛,很难分清物体的远近距离和形状,立体感消失了(如果是熟悉的场景,也许你能分辨出物体的空间感觉,但那不是眼睛看到的,而是大脑"看"到的,主要是     

Dielectric,piezoelectric, and ferroelectric properties of lanthanum-modified PZTFN ceramics

Specimens of Pb_1?1.5xLa_x(Zr_0.53Ti_0.47)_1?y?zFe_yNb_zO₃(x = 0, 0.004, 0.008, 0.012, and 0.016, y = z = 0.01) (PZTFN) ceramics were synthesized by a semi-wet route. In the present study, the effect of La doping was investigated on the structural, microstructural, dielectric, piezoelectric, and ferroelectric properties of the ceramics. The results show that, the tetragonal (space group P4mm) and rhombohedral (space group R3c) phases are observed to coexist in the sample at x = 0.012. Microstructural investigations of all the samples reveal that La doping inhibits grain growth. Doping of La into PZTFN improves the dielectric, ferroelectric, and piezoelectric properties of the ceramics. The hysteresis loops of all specimens exhibit nonlinear behavior. The dielectric, piezoelectric and ferroelectric properties show a maximum response at x ≥ 0.012, which corresponds to the morphotropic phase boundary (MPB).     

Assessment of the uncertainties in temperature change in China during the last century

We have used the China Homogenized Historic Temperature dataset and some long-term station series of the neighbor countries from CRUTEM3, a 5°×5° gridded dataset of monthly mean temperature since 1900, to provide a 107-year record of surface tem-perature trends and variability. We derived a comprehensive set of uncertainty estimates to accompany the data: measurement and sampling errors, uncertainties in temperature bias estimates, and uncertainties arising from limited observational coverage on large-scale averages have all been estimated. We reanalysed the temperature changes during the period of record. The best estimates of trends for 1900–2006 with uncertainties at 95% confidence range are about 0.09±0.017°C/decade for the year as a whole, and 0.14±0.021°C/decade, 0.11±0.021°C/decade, 0.04±0.017°C/decade, and 0.07±0.017°C/decade for winter, spring, summer and autumn respectively. For 1954–2006, the trends for annual, winter, spring, summer and autumn are: 0.26±0.032°C/decade, 0.35±0.046°C/decade, 0.25±0.051°C/decade, 0.16±0.037°C/decade and 0.22±0.055°C/decade. Winter saw the most significant warming trend in both 1900–2006 and 1954–2006, while during the most recent period (the satellite era, 1979–2006), all the seasons show similar warming trends: 0.45±0.13°C/decade, 0.51±0.11°C/decade, 0.52±0.16°C/decade, 0.37±0.10°C/decade and 0.50±0.16°C/decade for annual, winter, spring, summer and autumn. Trends arising from urbanization have been evaluated as less than 5% of the total warming trend for 1951–2001, so this bias was not removed.     

Mining rice new germplasm containing S5n gene by functional molecular marker and sequencing

Inter-subspecific hybrids between indica and japonica varieties yield strong biological heterosis, but it is difficult to utilize the hybrids directly in commercial production due to sterility of F1. A special gene S5^n may overcome the hybrids sterility, which is caused by the interaction between S5 loci. Recently, S5^n had been cloned, and it was revealed containing a large DNA deletion sequence that made the gene nonfunctional, compared to S5^i or S5^j. We designed a pair of primers flanking the deletion sequence of Ssn, and then applied to distinguish the varieties with S5^n or non-S5^n, convincing result suggested that the primers could be served as functional molecular marker to efficiently identify the new germplasm with S5^n, Using the functional marker, we surveyed 197 varieties from China National Micro-core Rice Collection, and found ten of which represented S5^n including following varieties： Haobuka, Sanbangqishiluo, Mubanggu, Xiaohonggu, Mowanggu＇neiza, Laozaogu, Fanhaopi, Feie＇nu02, Baoxie-7B, Teqingxuanhui. Among them, two varieties Sanbangqishiluo and Laozaogu was previously reported to contain S5^n gene. Further sequence analysis on the DNA sequence covering both sides of deletion in S5^n of the 10 varieties confirmed that the detected sequences in above varieties was identical with those of varieties containing S5^n, such as 02428 and Linglun. These results suggested that the gene in S5 locus of the ten varieties was also nonfunctional and it proved the presence of S5^n gene.     

Surface interactions of MoO3/ α-Fe2O3 system

α-Fe₂O₃ -supported molybdena catalysts have been prepared by heating a mixture of MoO₃ and α-Fe₂O₃. XRD, XPS, LRS, TG-DTA and Mössbauer spectroscopy were used to characterize the interactions between MoO₃ and α-Fe₂O₃. The dispersion capacity of MoO₃ on the surface of α-Fe₂O₃ determined by XRD and XPS was 0.8 mmol/100m² α-Fe₂O₃ in the samples calcined at 420 . For the sample with low MoO₃ loading, LRS and FT-IR results showed that Mo⁶⁺ ions were located in the tetrahedral vacant sites on the surface of α-Fe₂O₃, signed as Mo- . The amount of Mo-II species, formed by Mo6+ ions incorporated into the octahedral vacant sites, increased with the MoO₃ loading. Based on the assumption that the (001) plane of α-Fe₂O₃ is preferentially exposed, almost all the Mo⁶⁺ ions of the dispersed molybdena species existed at the surface octahedral sites for the sample with MoO₃ loading close or beyond the dispersion capacity, and formed the Mo-II species. In this case, the capping O^2- ions linking with the incorporated Mo⁶⁺ ions formed a surface epitaxial structure, which was in good agreement with the results predicted by the incorporation model proposed previously. XRD and Mössbauer spectroscopy of the MoO₃ α-Fe₂O₃ samples calcined at different temperatures showed that the calcination temperature could strongly influence the interaction extent: ( i) at 420 , MoO₃ dispersed on the surface of α-Fe₂O₃ and formed surface Mo species; (ii ) at 500 , MoO₃ reacted with the bulk of α-Fe₂O₃ and formed Fe₂(MoO₄)₃ compound.     

Effect of aluminum oxide on the compressive strength of pellets

Analytical-reagent-grade Al₂O₃ was added to magnetite ore during the process of pelletizing, and the methods of mercury intrusion, scanning electron microscopy, and image processing were used to investigate the effect of Al₂O₃ on the compressive strength of the pellets. The results showed that, as the Al₂O₃ content increased, the compressive strength of the pellets increased slightly and then decreased gradually. When a small amount of Al₂O₃ was added to the pellets, the Al₂O₃ combined with fayalite (2FeO·SiO₂) and the aluminosilicate (2FeO·2Al₂O₃·5SiO₂) was generated, which releases some iron oxide and reduces the inhibition of fayalite to the solid phase of consolidation. When Al₂O₃ increased sequentially, high melting point of Al₂O₃ particles hinder the oxidation of Fe₃O₄ and the recrystallization of Fe2O3, making the internal porosity of the pellets increase, which leads to the decrease in compressive strength of the pellets.     

Ca5Zn3相稳定性和物理性质的第一性原理研究

利用基于密度泛函理论的第一性原理方法对Ca_5Zn_3化合物的晶格常数、形成焓、弹性常数、以及电子态密度等进行计算研究。为了获得Ca_5Zn_3化合物的结构稳定性,考虑了Cr_5B_3、W_5Si_3以及Mn_5Si_3 3种结构类型,计算得到的形成焓表明:具有Cr5B3结构类型的Ca_5Zn_3最稳定,其次为Mn_5Si_3型,最后是W_5Si_3型。对该化合物的弹性常数、电子态密度和电荷密度差进行了计算。最后利用德拜模型,对Ca_5Zn_3的热物理性能进行了计算,获得体积、体积模量、热膨胀系数以及等容热容随温度和压强变化的规律,为该化合物在热电方面的应用提供了理论依据。     

Variability and reduction of atmospheric pollutants in Beijing and its surrounding area during the Beijing 2008 Olympic Games

The Beijing-Tianjin-Hebei Atmospheric Environment Monitoring Network was established by the Institute of Atmospheric Physics, Chinese Academy of Sciences. The goals of the network were to monitor and provide warnings of the atmospheric quality in Beijing and its surrounding area during the Beijing 2008 Olympic Games. The results showed that the atmospheric complex pollution exhibited high concentrations of ozone and fine particles and oxidation in summer, with a ubiquitous regional source. The regional mean concentrations of SO₂, PM_2.5, NO₂, and O_{3_8h max} (the maximum daily 8 h mean) and O_x were 22±11, 90±40, 25±5, 136±35 and 112±21 μg/m³ in summer, respectively. During the Olympic Games, the mean concentration of SO₂, PM_2.5, NO_{2, O3_8h} max, and O_x were 12.5±4, 56±28, 23±4, 114±29, 95±17 μg/m³ in the region, respectively, and fell by 51.0%, 43.7%, 13%, 20.2%, and 18.9%, respectively, compared to the prophase mean before the Olympic Games. The concentration of atmospheric pollutants declined significantly and achieved the “Green Olympics” control goal of air quality. After the Olympic Games, SO₂, PM_2.5 and NO_x increased significantly as the temporary atmospheric pollution control measures were terminated.     

Coral reef ecosystems in the South China Sea as a source of atmospheric CO<Subscript>2</Subscript> in summer

Field measurements of air-sea CO2 exchange in three coral reef areas of the South China Sea (i.e. the Yongshu Reef atoll of the Nansha Islands, southern South China Sea (SCS); Yongxing Island of Xisha Islands, north-central SCS; and Luhuitou Fringing Reef in Sanya of Hainan Island, northern SCS) during the summers of 2008 and 2009 revealed that both air and surface seawater partial pressures of CO2 (pCO2) showed regular diurnal cycles. Minimum values occurred in the evening and maximum values in the morning. Air pCO2 in each of the three study areas showed small diurnal variations, while large diurnal variations were ob-served in seawater pCO2. The diurnal variation amplitude of seawater pCO2 was ~70 μmol mol–1 at the Yongshu Reef lagoon, 420–619 μmol mol–1 on the Yongxing Island reef flat, and 264–579 μmol mol–1 on the reef flat of the Luhuitou Fringing Reef, and 324–492 μmol mol–1 in an adjacent area just outside of this fringing reef. With respect to spatial relations, there were large differences in air-sea CO2 flux across the South China Sea (e.g. ~0.4 mmol CO2 m–2 d–1 at Yongshu Reef, ~4.7 mmol CO2 m–2 d–1 at Yongxing Island, and ~9.8 mmol CO2 m–2 d–1 at Luhuitou Fringing Reef). However, these positive values suggest that coral reef ecosystems of the SCS may be a net source of CO2 to the atmosphere. Additional analyses indicated that diurnal variations of surface seawater pCO2 in the shallow water reef flat are controlled mainly by biological metabolic processes, while those of deeper water lagoons and outer reef areas are regulated by both biological metabolism and hydrodynamic factors. Unlike the open ocean, inorganic metabolism plays a significant role in influencing seawater pCO2 variations in coral reef ecosystems.