土壤干湿交替对玉米耗水特性及水分利用的影响

旱地农业与灌溉农业中作物经常面临的土壤干旱与湿润交替变化是实际田间环境[1]。作物在生长发育的不同时期可能会遇上各不相同的土壤缺水胁迫 ,这些不同胁迫会对作物诱导出适应性的生理反应和伤害性影响[2 ,3],对此进行研究和认识 ,可以在节水灌溉中控制作物生长发育不同阶段土壤水分来调节作物生理过程 ,避免伤害性变化的发生 ,而促进适应性变化的产生 ,以改善作物发育后期籽粒形成阶段根系和叶片的功能来提高作物产量、品质和水分利用效率 ,达到高效、优质的目的。本文主要研究玉米在土壤干湿交替过程中的耗水特性和叶水分状况的关系 ,探讨提高水分利用效率的机制 ,为节水农业提供优化供水模式。1　材料与方法于 1 998年在香港浸会大学生物系温室进行 ,将陕单 9号玉米杂交种的种子播入口径 1 6ｃｍ ,高 1 8ｃｍ的生长钵内 ,内装 1 .8ｋｇ混合土 (蛭石、泥炭和沙子按体积 7∶3∶2 )混合 ,加入适量复合肥 ,在 2 6～ 30℃温室中生长 ,用高压钠灯做为光源 ,光合有效辐射 (ＰＡＲ)约为 40 0 μｍｏｌｍ- 2 ｓ- 1 。植株供水良好 ,每钵留两棵生长均匀一致的苗子 ,大约 1个月后 ,待玉米长至 3至 ...

Synthesis of different gold nanostructures by solar radiation and their SERS spectroscopy

In this article, a simple and novel photochemical synthesis of different gold nanostructures is proposed using solar radiation. This method is rapid, convenient and of low cost, and can be performed under ambient conditions. By adjusting the concentration of sodium acetate (NaAc), different morphologies of the products can be easily obtained. Without NaAc, the products obtained are mainly polyhedral gold particles; lower concentration of NaAc (0.05 and 0.1 M) accelerates the formation of flowerlike gold nanostructures; while higher concentration of NaAc (0.5 M) facilitates the formation of a variety of gold nanowires and nanobelts. It is found that the morphology change of gold nanaostructures is the result of the synergistic effect of poly(diallyl dimethylammonium) chloride (PDDA), Ac- ions, and the pH value. In addition, the different gold nanostructures thus obtained were used as substrates for surface-enhanced Raman scattering (SERS) with p-aminothiophenol (p-ATP) as the probe molecule.

Non-isothermal crystallization behavior and kinetics of metallocene short chain branched polyethylene

The non-isothermal crystallization behavior and kinetics of metallocene short chain branched polyethylene were investigated via DSC at cooling rates from 2.5 to 20 degreesC/min, and subsequent heating at rate of 10 degreesC/min. To verify the effect of molecular weight and branching content on crystallization, three group samples were chosen: (1) linear polyethylene with low molecular weight and high molecular weight; (2) low molecular weight polyethylene with low branching content and high branching content; (3) high molecular weight polyethylene with low branching content and high branching content. The results show that crystallization temperature, crystallinity, melting temperature and crystallization rate are highly branching content-dependent. Molecular weight effect is less important, compared to branching content. A dramatic decrease of crystallization temperature, crystallinity, crystallization rate and melting temperature was observed for branched samples. The non-isothermal kinetics was analyzed via the methods, developed by Gupta and Mo Zhi-shen, and good agreement was obtained.

茂金属聚乙烯的非等温结晶行为及其动力学研究

为探索分子量和支链含量对聚乙烯非等温结晶过程的影响 ,选用 3组样品 :(1 )不同分子量的无支链线形聚乙烯 ;(2 )低分子量的支链含量不同的试样 ;(3 )高分子量的支链含量不同的试样 .用 DSC研究了这3组样品的非等温结晶动力学 .结果表明 :(1 )与支链含量相比 ,分子量大小对结晶的影响是次要的 ,但高分子量样品的结晶度比低分子量样品低 ;(2 )支链对聚乙烯的非等温结晶有重要影响 ,在支化聚乙烯中起决定作用 ;(3 )无论是高分子量试样还是低分子量试样 ,支化含量增加 ,聚乙烯的结晶温度、结晶度、结晶动力学以及晶体的熔点等显著降低

Hydrothermal synthesis and crystal structure of Co(En)(3)MoO4

Co(En)(3)MoO4 was synthesized by using the method of hydrothermal synthesis and characterized by elemental analysis, IR, ESR and single-crystal X-ray methods. It crystallizes in hexagonal space group P (3) over bar C1 with a=1.596 4(2) nm, b=1.596 4(2) nm, c = 0.993 5(2) nm, alpha=beta=90 degrees gamma=120 degrees, M-c=399.18, V=2.192 6(6) nm(3), D-c=1.814 g/nm(3), Z=6, F(000)=1 2181 R-1=0.070 3, R-w=0.220 7. According to separation of anion which acted on electrostatic potential, the anion and cation ions formed a type of organic and inorganic material.

Paleoenvironment evolution of the East Philippine Sea recorded in the new-type ferromanganese crust since the terminal Late Miocene

From systemic research of microstructure, geochemistry, uranium-series and Be-10 isotope dating on a new-type deepwater ferromanganese crust from the East Philippine Sea, the paleoenvironment evolution of the target area since the terminal Late Miocene was recovered. The vertical section changes of microstructure and chemical composition are consistent in the studied crust, which indicate three major accretion periods and corresponding paleoenvironment evolution of the crust. The bottom crust zone was formed in the terminal Late Miocene (5.6 Ma) with loose microstructure, high detritus content and high growth rate. Reductions of mineral element content, accretion rate and positive Ce-anomaly degree at 4.6 Ma indicate temporal warming, which went against the crust accretion and finally formed an accretion gap in the terminal Middle Pliocene (2.8-2.7 Ma). The more active Antarctic bottom seawaters in the Late Pliocene (2.7 Ma) facilitated the fast transfer to the top pure crust zone. Hereafter, with the further apart of volcanic source and the keeping increase of eolian material (1.0 Ma), although surrounding conditions were still favorable, mineral element content still shows an obvious reducing trend. It thereby offers new carrier and data for the unclear paleoceanographic research of the target area since the terminal Late Miocene.

中国沿海典型区域织纹螺毒性及毒素成分研究

织纹螺（Nassarius spp.）味道鲜美，是中国及其它一些亚洲国家沿海地区居民习惯食用的一种水产品。但是，近几十年来，中国沿海频繁发生食用织纹螺中毒事件，严重威胁着人们的身体健康和生命安全。加之人们对织纹螺体内的毒素成分、来源及其毒性变化规律还没有清晰的认识，因此难以有效预防和控制食用织纹螺引起的中毒事件。本文根据文献报道，在中国沿海食用织纹螺中毒事件多发的典型区域，包括江苏省的连云港市和盐城市、浙江省的舟山市和宁波市、福建省的宁德市、厦门市和莆田市设立了监测点，于2006年和2007年间进行了连续采样，应用小鼠生物测试法调查了织纹螺毒性的消长情况，并利用高效液相色谱-质谱联用（Liquid Chromatography-Mass Spectrometry，LC-MS）和高效液相色谱技术（High Performance Liquid Chromatography，HPLC）对织纹螺体内的毒素成分进行了分析。 实验结果表明，2006年于江苏省盐城市射阳海域采集的织纹螺样品中，阳性样品检出率为56%，毒性在2-5 MU/g组织（湿重）之间变化，在2007年于同地采集的8个样品中，除一个样品毒性为3.14 MU/g组织（湿重）以外，其余样品均表现为阴性；而2007年采集自连云港市赣榆海域的织纹螺样品，在采样期间则呈现出极高的毒性，最高达到846.52 MU/g 组织（湿重），毒性在监测期间呈“M”状波动，在5月和7月下旬出现两个毒性高峰。2006年于浙江省宁波市象山港采集的织纹螺样品中，阳性样品检出率为25%，毒性均在2.5 MU/g组织（湿重）左右；而同年采集自舟山市定海的织纹螺样品中，阳性样品检出率为100%，最高毒性达18.40 MU/g组织（湿重），毒性在监测期间也呈“M”状波动，高峰期出现在6月初和7月底。2006年3-9月采集自福建省宁德霞浦、厦门同安和莆田涵江采集的织纹螺样品中，阳性样品检出率分别为20%、43%和14%，除7月中旬采集自宁德霞浦的一个样品毒性达到16.19 MU/g组织（湿重）之外，其余样品毒性均在2-5 MU/g组织（湿重）间波动。从阳性样品的时间分布规律来看，3月份和6、7月份是阳性样品集中出现的时期。根据以上调查结果可以看出，织纹螺的毒性消长呈现出较明显的地域性和季节性特征，不同地区的织纹螺毒性存在差异，而同一区域织纹螺毒性的消长则表现出明显的季节性集中趋势。除了2007年采集自连云港赣榆的织纹螺样品毒性与其平均个体组织重量有相似的变化趋势以外，其余地区的织纹螺样品毒性和个体大小无明显相关性。 利用LC-MS和HPLC技术对织纹螺样品中的毒素成分进行了分析，确定河豚毒素（tetrodotoxin, TTX）及其同系物（trideoxyTTX，4-epi-TTX，anhydroTTX，oxoTTX）是所采集织纹螺中的主要致毒成分，样品中没有检测到麻痹性贝毒毒素（Paralytic Shellfish Poison, PSP）。自不同地区采集的织纹螺中毒素成分基本一致，但组成存在一定差异。其中，采自江苏省连云港赣榆和浙江省舟山定海的织纹螺样品中，trideoxyTTX是主要的成分，其次是TTX；而从其它采样地点采集的织纹螺中，TTX都是主要的毒素成分，其次才是trideoxyTTX及其它同系物。对采集自江苏省连云港赣榆和浙江舟山定海的织纹螺体内毒素的解剖学分布进行了分析，结果表明肌肉、消化腺和剩余部分中的毒素组成基本一致，其中trideoxyTTX是主要的毒素成分，其次为TTX，但采自浙江舟山的织纹螺剩余部分中的TTX是主要的毒素成分。在监测期间，各组织中的毒素组成没有明显变化，但毒素含量随季节变化表现出了一定的差异。 综上所述，在中国沿海典型区域开展的织纹螺毒性调查结果表明其毒性消长具有一定的地域性和季节性特征。分析结果显示织纹螺体内的毒素成分是河豚毒素及其同系物，采自不同区域的织纹螺体内毒素成分基本一致，但毒素组成稍有差异。对织纹螺中毒素的解剖学分布研究显示，各组织中的毒素含量随季节变化而表现出一定差异，但毒素组成没有明显的季节性变化。这些结果显示中国沿海的织纹螺应具有相似的毒素来源，研究结果将为相关部门有效监测、预防和控制食用织纹螺中毒事件提供有力的科学依据。

Methane emissions by alpine plant communities in the Qinghai-Tibet Plateau

For the first time to our knowledge, we report here methane emissions by plant communities in alpine ecosystems in the Qinghai-Tibet Plateau. This has been achieved through long-term field observations from June 2003 to July 2006 using a closed chamber technique. Strong methane emission at the rate of 26.2 +/- 1.2 and 7.8 +/- 1.1 mu g CH4 m(-2) h(-1) was observed for a grass community in a Kobresia humilis meadow and a Potentilla fruticosa meadow, respectively. A shrub community in the Potentilla meadow consumed atmospheric methane at the rate of 5.8 +/- 1.3 mu g CH4 m(-2) h(-1) on a regional basis; plants from alpine meadows contribute at least 0.13 Tg CH4 yr(-1) in the Tibetan Plateau. This finding has important implications with regard to the regional methane budget and species-level difference should be considered when assessing methane emissions by plants.

油气输导体系研究及应用─以准噶尔盆地东部白家海凸起侏罗系为例

Baijiahai uplift is an important hydrocarbon accumulation belt in eastern Jungger Basin, on which Cainan oilfield and lithologic hydrocarbon reservoir named Cai 43 have been discovered and both of them share the same target formation of Jurassic. However, in the subsequent exploration at this region, several wells that designed for lithologic traps of Jurassic were eventually failed, and that indicates the controlling factors of lithologic reservoir distribution are far more complicated than our previous expectation. This dissertation set the strata of the Jurassic in well Cai 43 region as the target, and based on the integrated analysis of structure evolution、fault sealing ability、simulations of sedimentary microfacies and reservoir beds、distribution analysis of high porosity-high permeability carrier beds、drive forces of hydrocarbons、preferential conduit system and conduit model as well as critical values of the reservoir physical properties for hydrocarbon charging, a special method that different from the conventional way to predict favorable lithologic traps was established. And with this method the controlling factors of the hydrocarbon reservoirs formation are figured out, and further more, the favorable exploration targets are point out. At Baijiahai uplift, fault plays as a crucial factor in the process of the hydrocarbon reservoir formation. In this study, it is found out that the availability of a fault that work as the seal for oil and gas are different. The critical value of the lateral mudstone smear factor (Kssf), which is used to measure the lateral sealing ability of fault, for oil is 3.9 while that for gas is 2.1; and the critical value of vertical sealing factor (F), which similarly a measurement for the vertical sealing ability of fault, for oil is 7.3 while that for gas is 5.1. Dongdaohaizi fault belt that possessed well lateral sealing ability since later Cretaceous have bad vertical sealing ability in later Cretaceous, however, it turns to be well now. Based on the comparison of the physical properties that respectively obtained from electronic log calculating、conventional laboratory rock analysis and the additive-pressure bearing laboratory rock analysis, we established the functions through which the porosity and permeability obtained though conventional method can be converted to the values of the subsurface conditions. With this method, the porosity and permeability of the Jurassic strata at the time of previous Tertiary and that in nowadays are reconstructed respectively, and then the characteristics of the distribution of high porosity-high permeability carrier beds in the evolution processes are determined. With the result of these works, it is found that both well Cai 43 region and Cainan oilfield are located on the preferential conduit direction of hydrocarbon migration. This conclusion is consistent with the result of the fluid potential analysis, in which fluid potential of nowadays and that of later Cretaceous are considered. At the same times, experiment of hydrocarbon injection into the addictive-pressure bearing rock is designed and conducted, from which it is found that, for mid-permeability cores of Jurassic, 0.03MPa is the threshold values for the hydrocarbon charging. And here, the conception of lateral pressure gradient is proposed to describe the lateral driving force for hydrocarbon migration. With this conception, it is found that hydrocarbons largely distributed in the areas where lateral pressure gradient is greater than 0. 03MPa/100m. Analysis of critical physical properties indicated that the value of the critical porosity and critical permeability varied with burial depth, and it is the throat radius of a certain reservoir bed that works as a key factor in controlling hydrocarbon content. Three parameters are proposed to describe the critical physical properties in this dissertation, which composite of effective oil-bearing porosity、effective oil-bearing permeability and preferential flow coefficient. And found that critical physical properties, at least to some extent, control the hydrocarbon distribution of Jurassic in Baijiahai uplift. Synthesize the content discussed above, this dissertation analyzed the key factors i.e., critical physical properties、driving force、conduit system and fluid potential, which controlled the formation of the lithologic reservoir in Baijiahai uplift. In all of which conduit system and fluid potential determined the direction of hydrocarbon migration, and substantially they are critical physical properties of reservoir bed and the lateral pressure gradient that controlled the eventually hydrocarbon distribution. At the same times, sand bodies in the major target formation that are recognized by reservoir bed simulation are appraised, then predict favorite direction of the next step exploration of lithologic reservoir.

Understanding student information behavior in relation to electronic information services: lessons from longitudinal monitoring and evaluation Part 2

Urquhart, C. & Rowley, J. (2007). Understanding student information behavior in relation to electronic information services: lessons from longitudinal monitoring and evaluation Part 2. Journal of the American Society for Information Science and Technology, 58(8), 1188-1197. Sponsorship: JISC

The Celtic Inscriptions of Britain: Phonology and Chronology, c. 400-1200, Publications of the Philological Society, 37

Sims-Williams, P. (2002). The Celtic Inscriptions of Britain: Phonology and Chronology, c. 400-1200. Publications of the Philological Society, 37. Oxford: Blackwell Publishing. RAE2008

The Rpf/DSF system and the regulation of virulence in the plant pathogen Xanthomonas campestris

The full virulence of Xanthomonas campestris pv. campestris (Xcc) to plants depends upon cell-to-cell signalling mediated by the signal molecule DSF (for diffusible signal factor), that has been characterised as cis-11-methyl-2-dodecenoic acid. DSF-mediated signalling regulates motility, biofilm dynamics and the synthesis of particular virulence determinants. The synthesis and perception of the DSF signal molecule involves products of the rpf (regulation of pathogenicity factors) gene cluster. DSF synthesis is fully dependent on RpfF, which encodes a putative enoyl-CoA hydratase. A two-component system, comprising the complex sensor histidine kinase RpfC and the HD-GYP domain regulator RpfG, is implicated in DSF perception. The HD-GYP domain of RpfG is a phosphodiesterase working on cyclic di-GMP; DSF perception is thereby linked to the turnover of this intracellular second messenger. The full range of regulatory influences of the Rpf/DSF system and of cyclic di-GMP in Xcc has yet to be established. In order to further characterise the Rpf/DSF regulatory network in Xcc, a proteomic approach was used to compare protein expression in the wildtype and defined rpf mutants. This work shows that the Rpf/DSF system regulates a range of biological functions that are associated with virulence and biofilm formation but also reveals new functions mediated by DSF regulation. These functions include antibiotic resistance, detoxification and stress tolerance. Mutational analysis showed that several of these regulated protein functions contribute to virulence in Chinese radish. Interestingly, it was demonstrated that different patterns of protein expression are associated with mutations of rpfF, rpfC and rpfG. This suggests that RpfG and RpfC have broader roles in regulation other than perception and transduction of DSF. Taken together, this analysis indicates the broad and complex regulatory role of Rpf/DSF system and identifies a number of new functions under Rpf/DSF control, which were shown to play a role in virulence.