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.     

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).     

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.     

3种苏铁属植物总黄酮、总多糖含量及抗氧化活性研究

为探究锈毛苏铁(Cycas ferruginea)、叉孢苏铁(C.segmentifida)和石山苏铁(C.sexseminifera) 3种苏铁属(Cycas)植物的总黄酮、总多糖含量以及抗氧化活性,本研究采用超声波辅助法对其根、叶柄、叶、雄球花、茎干的总黄酮及总多糖含量进行提取,以DPPH自由基(DPPH·)、羟自由基(·OH)、超氧阴离子自由基(O^-₂·)清除率评价其抗氧化活性,并采用Pearson相关性分析法分析相关性。结果表明：锈毛苏铁、叉孢苏铁和石山苏铁叶的总黄酮含量较高,大小依次为锈毛苏铁(8.61 mg·100 mg^-1)>叉孢苏铁(7.82 mg·100 mg^-1)>石山苏铁(1.04 mg·100 mg^-1);茎干中总多糖含量最高,大小依次为叉孢苏铁(28.32 mg·100 mg^-1)>石山苏铁(24.43 mg·100 mg^-1)>锈毛苏铁(16.59 mg·100 mg^-1<...     

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.     

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.     

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.     

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。     

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.     

Evidence for metasomatic mantle carbonatitic magma extrusion in Mesoproterozoic ore-hosting dolomite rocks in the middle Kunyang rift, central Yunnan, China

The Kunyang rift lying on the western margin of the Yangtze platform is a rare Precambrian Fe-Cu mineralization zone. Wuding- Lufeng basin that is an important part of the zone is located on the west edge in the middle of the rift. The most important ore-hosting rocks are Mesoproterozoic dolomite rocks in the basin controlled by a ring fracture system, which is a fundamental structure of the basin. Plenty of silicate minerals and acicular apatite, feldspar phenocrysts and small vesicular, flown line and flown plane structures, melt inclusion and high temperature fluid inclusion found in most ore-hosting dolomites suggest that this kind of rocks could not be sedimentary dolomite, marble or hydrothermal carbonate rocks. The Zr/Hf and Nb/Ta values of the rocks are identical with those of associated mantle-derived rocks, and vary widely. For the monomineral dolomite, δ^18OSMOW‰=＋5.99 to ＋18.4 and δ^13CPDB‰ = -3.01 to ＋0.94, which fall within the range for all carbonatitic volcanic rocks of the world. As for the accessory minerals, the values of δ^18OSMOW‰ of magnetite （=＋3.47 to ＋5.99‰） are close to that of the mantle （〈5.7%）, and the δ^34S‰ values of sulfides （-5.09 to ＋5.78, averaging ＋1.50） are close to that of meteorite. For all the ore-bearing dolomite rocks, εNd = ＋0.19 to ＋2.27, and the calculated Isr=0.699143, while for the associated mantle-derived rocks, εnd = ＋3.18 to ＋3.72. All the data suggest that the mineral assemblage is not only igneous but also of metasomatic mantle origin. And the presence of acicular apatite indicates that the rocks were formed by magma rapidly cooling. And the phenocryst texture and vesicular, flown and ropy and pyroclastic structures suggest that the igneous rocks were extrusive. Therefore, the ore-bearing dolomite rocks are carbonatitic volcanic rocks. This conclusion implies that most iron and copper ore deposits hosted in the dolomite rocks should be of the carbonatite type.     

四元数矩阵方程AXB+CXD=E的M自共轭解

把实数域上的M对称矩阵的概念推广到四元数体上,形成M自共轭矩阵,然后在四元数体上讨论矩阵方程AXB+CXD=E的M自共轭解及其最佳逼近问题.利用四元数矩阵的实分解和复分解,以及M自共轭矩阵的特征结构,借助Kronecker积把约束四元数矩阵方程转化为实数域上的无约束方程,克服了四元数乘法非交换运算的困难,并得到该方程具有M自共轭解的充要条件及其通解表达式.同时在解集非空的条件下,运用矩阵的分块技术及矩阵的拉直算子,获得与预先给定的四元数矩阵有极小Frobenius范数的最佳逼近解.由于M自共轭矩阵是四元数自共轭矩阵的推广,因此所得结果拓展了该方程的结构解类型.     

遮光对红鳞蒲桃幼苗光合特性的影响

为了解红鳞蒲桃（Syzygium hancei）对光能的需求及适应性,以红鳞蒲桃幼苗为材料,设置透光率分别为100.0%、72.3%、48.6%、24.9%的4种光照处理,测定其光合作用参数、光响应参数、叶绿素含量等数据,研究不同遮光处理对其光合特性的影响。结果表明：（1）红鳞蒲桃是喜光树种,红鳞蒲桃幼苗净光合速率（Net Photosynthetic Rate,P_n）、气孔导度（Stomatal Conductance,G_s）日均值随着遮光程度的增加而减小,胞间CO₂浓度（Intercellular Carbon Dioxide Concentration,C_i）日均值随之增大,过度遮光下（透光率为48.6%和24.9%）,蒸腾速率（Transpiration Rate,T_r）日均值显著低于全光照;（2）遮光条件下,红鳞蒲桃幼苗净光合速率下降可能是非气孔限制引起的;（3）红鳞蒲桃幼苗的最大净光合速率（Maximum Net Photosynthetic Rate,P_max）、光补偿点（Light Compensation Point,LCP）、光饱和点（Light Saturation Point,LSP）、暗呼吸速率（Respiration Rate,R_d）均随着光照强度的增加而显著增加;（4）红鳞蒲桃幼苗叶绿素a、叶绿素b及叶绿素（a+b）的含量均随着遮光程度的增加而显著增加,叶绿素a/b的值随之减小。红鳞蒲桃在幼苗期具有较明显的喜光性,因此,在红鳞蒲桃幼苗的培育及种群的恢复过程中,可通过疏伐、修剪枝条等措施来增加林内的透光量,为处于幼苗时期的红鳞蒲桃创造适宜的光照环境,为其自然更新提供良好条件。     

降能片对12C6+束流影响的Geant4模拟

利用Geant4模拟每核子能量在80~360 MeV内碳离子束（¹²C⁶⁺）穿过靶质量厚度为0.5~4.0 g/cm2的有机玻璃、 铝、 铜和铅后的角度歧离值和能量歧离值, 并对比单能碳离子束直接进入水中和经降能片后再进入水中的Bragg峰. 模拟结果表明: 碳离子束的能量越高、 降能片的质量厚度和原子序数越小, 碳离子束经过降能片后的角度歧离和能量歧离值越小, 其Bragg峰所受影响也越小. 即若仅考虑角度歧离和能量歧离, 则低原子序数的材料更适合做降能片.     

三种速生人工林凋落物的持水性能

在广西国营高峰林场界牌分场选择立地条件、营林和管理措施、林分长势基本一致的5年生尾巨桉无性系3229(Eucalyptus3229)、厚荚相思(Acaciac rassicarpa)和马占相思(Acacia mangium)速生人工林,采集林下凋落物测定单位面积储量、持水量、持水率和持水速率,研究3种速生树种人工林下凋落物的持水性能。结果表明,厚荚相思凋落物的持水量和持水率最大,分别达18.40×103kg.hm-2和70%,尾巨桉3229的次之,分别为17.34×103kg.hm-2和50%,马占相思的最小,分别是13.49×103kg.hm-2和45%。厚荚相思和尾巨桉无性系3229的持水性能比马占相思的强。     

Characterizations of <Emphasis Type="Italic">L</Emphasis><Subscript><Emphasis Type="Italic">p</Emphasis></Subscript>(<Emphasis Type="Italic">R</Emphasis>) using tight wavelet frames

In this paper,a Littlewood-Paley function characterization of the spaces L p(R),1相似文献   

邻香草醛缩胱氨酸双Schiff碱的合成及其对粟酒裂殖酵母细胞生长代谢的热动力学研究

用摩尔比为2:1的邻香草醛(C_8H_8O_3)与L-胱氨酸(C_6H_(12)N_2O_4S_2)反应,合成了一种新的双Schiff碱化合物--双{2-[(3-巯基丙酸钠)-2-亚胺基-甲基]-6-甲氧基-苯酚}(OVCS)。通过元素分析、红外光谱、核磁共振等手段对其组成和结构进行了表征,确定其化学式为Na_2(C_(22)H_(22)N_2O_8S_2),采用TAM air微量热仪测定了新合成的Schiff碱化合物(OVCS)在305.15 K时对粟酒裂殖酵母细胞作用的产热曲线;根据产热曲线计算了在OVCS作用下,粟酒裂殖酵母细胞生长代谢的最大发热功率p_(max)、速率常数k、传代时间tG、抑制率I和半抑制浓度C_(I,50)等热动力学参数。通过实验可以发现随着OVCS浓度的增加,粟酒裂殖酵母细胞的生长代谢速率常数k、生长代谢的总热效应Q_(total)、最大发热功率p_(max)均减小,抑制率I、达到生长代谢最大功率所需时间t_(max)、传代时间tG均增加等规律,半抑制浓度C_(I,50)为35.99 mg/L(或9.62×10~(-2)mol/L)。实验结果表明,OVCS对粟酒裂殖酵母细胞有抑制作用,且浓度越大,抑制作用越强。     

不同轮伐期对巨尾桉人工林碳固存的影响

【目的】深入探讨不同轮伐期对巨尾桉人工林碳固存的影响,为从应对全球气候变化的视角确定合理轮伐期提供理论依据。【方法】以轮伐期为短(7a)、中(13a)和长周期(21a)的巨尾桉人工林为研究对象,通过对不同轮伐期桉树林分生物量、碳固存、年平均固碳量的分析,揭示不同轮伐期对桉树林分碳固存的影响。【结果】巨尾桉人工林的生物量碳随着轮伐期的延长而逐渐增加,由7a轮伐期的(75.81±5.12)t·C/hm~2增至13a轮伐期的(180.11±19.97)t·C/hm~2以及21a轮伐期的(192.08±16.50)t·C/hm~2,方差分析表明,13a和21a轮伐期的总生物量碳显著高于7a轮伐期,而13a和21a轮伐期之间的差异不显著。巨尾桉人工林土壤有机碳随轮伐期延长而显著降低,由7a轮伐期的(89.99±0.35)t·C/hm~2、13a轮伐期的(85.42±0.76)t·C/hm~2下降到21a轮伐期的(74.64±0.24)t·C/hm~2。7~13a仍是巨尾桉人工林固碳能力迅速增长期,年平均总生物量碳由7a时的10.78t·C/(hm~2·a)迅速提高到13a的19.54t·C/(hm~2·a),增长81%;21a时巨尾桉人工林进入固碳能力下降期,年平均总生物量碳降至3.78t·C/(hm~2·a),固碳能力只是13a的19.34%。【结论】在南亚热带,巨尾桉人工林的最佳轮伐期确定在13a左右较为适宜,这与经济效益的最大化一致。     

Methane emissions from wetlands on the Qinghai-Tibet Plateau

The areal extent of cold freshwater wetlands on the Qinghai-Tibet Plateau (QTP) is estimated at 0.133 × 10⁶ km², suggesting a significant methane potential. Methane fluxes from wet alpine meadows, peatlands,Hippuris vulgaris mires and secondary marshes were 43.18, 12.96, −0.28 and 45.90 mg · m⁻² · d⁻¹, respectively based on the transect flux studies at the Huashixia Permafrost Station (HPS) from July to August 1996. Average CH₄ fluxes in the thaw season were extrapolated at 5.68 g · m⁻² according to the areal percentage of wetland areas in the Huashixia region. The CH₄ fluxes at four fixed sites, representative of similar ecosystems, ranged from −19.384–347.15 mg · m⁻² · d⁻¹, and the average CH₄ fluxes varied from 6.54 to 71.97 mg · m⁻² · d⁻¹ at each site during the observation period from April to September 1997. The CH₄ emissions at each site during the entire thaw season was estimated from 1.21 to 10.65 g · m⁻², displaying strong spatial variations. Seasonal variations of CH₄ fluxes also were observed at four sites: CH₄ outbursts occurred upon the spring thaw in May and June, CH₄ fluxes increased afterwards with rising soil temperatures. Episodic fluxes were observed in summer, which influenced the average CH₄ fluxes considerably. Annual CH₄ emissions from cold wetlands on the QTP were estimated at about 0.7–0.9 Tg based on the distribution of wetlands, representative CH₄ fluxes, and number of thaw days. The centers of CH₄ releasing were located in the sources of the Yangtze and Yellow rivers, and Zoigê Peatlands.     

SNOX法催化脱除模拟烟气中NO○x及SO2实验研究

为了实际考察SNOX方法的工艺条件对烟气中NO○x及SO2的催化脱除效果,针对NO○x的催化还原反应,采用浸渍法制备CuO/γ-Al2O3催化剂,考察了反应温度、空间速度、n(NH3)/n(NO○x)、SO2浓度对NO○x转化率的影响;针对SO2催化氧化反应,采用筛选出的V2O5催化剂,实验考察了反应温度、空间速度、n(O2)/n(SO2)对SO2转化率的影响.以实验研究成果为依据,进行了反应动力学计算.研究结果表明,在实验确定的最佳工艺条件下,NO○x还原率可达87.5%,经两级氧化SO2的转化率达94.3%.