冬枣果实对不同贮藏条件的生理反应及耐贮性研究

本文以我国特有的冬枣果实为试材，系统地研究了冬枣果实在室温、低温和不同O2和CO2浓度气调贮藏条件下的生理特性、风味品质和贮藏性，提出了适合于冬枣果实生理特性的气调指标和贮藏时间;分析了冬枣在不同贮藏条件下果实硬度、颜色、叶绿素和花青素、可溶性固形物、可滴定酸、Vc、乙醇和乙酸乙酯等物质成分的含量变化及与果实风味品质的关系;同时也分析了多酚氧化酶（PPO）、苯丙氨酸解氨酶（PAL）、过氧化物酶（POD）、超氧化物歧化酶（SOD）、过氧化氢酶（CAT）、多聚半乳糖醛酸酶（PG）和脂氧合酶（LOX）的活性变化情况以及丙二醛（MDA）含量和膜透性的变化情况，揭示了它们与冬枣果实转红、酒化、褐变、软化、衰老、及耐贮性的关系。对冬枣果实在气调贮藏中的生理反应和品质变化的研究，为形成冬枣果实采后商业化贮藏的系列配套技术提供了理论依据。试验结果表明： 1、冬枣果实在不同贮藏环境下品质的变化：随着贮藏时间的延长，冬枣果实Vc含量呈明显下降的趋势，CA处理能有效地抑制果实Vc含量的下降;不同贮藏条件对冬枣果实SSC影响不大;冬枣果实花青素的含量随贮藏时间逐渐下降，高O2浓度（70%）动态气调与其它处理相比，能更有效保持冬枣果实果皮的颜色及花青素和叶绿素的含量，以及果实的亮度、颜色饱和度和色度;同时，还能降低贮藏前期冬枣果实乙醇释放量。 2、冬枣果实在不同贮藏环境下生理的变化：（1） PG 酶是影响冬枣果实软化的主要因素，冬枣果实中存在内切和外切两种PG 酶，在冬枣果实的成熟过程中，Exo-PG和Endo-PG迅速积累，并呈现较高的活性，多聚半乳糖醛酸酶活性与冬枣果实的软化密切相关。CA贮藏与普通冷藏相比，可有效地抑制冬枣果实多聚半乳糖醛酸酶的活性和延缓果实软化，其中以5% O2的CA贮藏的效果最好。（2）膜质过氧化是造成冬枣果实褐变的主要因素，在室温下冬枣果实细胞膜透性随贮藏时间逐渐上升，CA贮藏在贮藏前中期可有效控制MDA含量的上升和果实褐变的发生，有利于降低膜脂过氧化程度，保护细胞膜结构并延缓果实衰老。冬枣果实褐变与PPO活性关系不大，但与膜透性及膜质过氧化作用的产物—丙二醛（MAD）含量变化显著相关。（3）冬枣果实采收时的SOD活性很低，在25 C下，果实SOD活性急剧上升，低温贮藏条件下，果实SOD活性出现两次高峰，第一次高峰为果实后熟的标志，第二次高峰标志着果实的衰老。（4）在不同贮藏条件下，冬枣果实PAL活性均随贮藏期的延长而呈现下降趋势。 3、影响冬枣果实贮藏性的生理因素：冬枣果实的衰老与活性氧代谢失调和防御体系活力下降有关，随着果实衰老的出现，果实的POD、CAT等保护酶活性均呈现明显下降的趋势。气调贮藏在前期能显著提高冬枣果实POD的活性，而在后期又显著抑制了POD活性的上升，说明POD在果实贮藏初期表现为保护效应，而在后期则表现为伤害效应。 4、冬枣果实适宜的贮藏条件：与普通冷藏相比，气调贮藏（CA）能明显地延缓果实衰老，减少腐烂和褐变，保持风味品质和延长贮藏时间。其中以较高O2浓度的（10% O2 + 0% CO2）气调贮藏效果最好。气调贮藏与杀菌剂配合有利于延长冬枣的贮藏期，0.1%的施保克和0.1%戴挫霉处理能有效控制冬枣果实贮藏期间的腐烂，延长贮藏时间，施保克的防腐效果好于戴挫霉。 5、拮抗菌和病原菌处理对冬枣果实抗性相关酶的诱导：接种拮抗菌+病原菌或只接种病原菌能诱导冬枣果实蛋白含量的显著升高，说明拮抗菌和病原菌处理诱导了果实病原相关蛋白的积累。在常温条件下，拮抗菌和病原菌处理抑制了冬枣果实的CAT酶活性，诱导了SOD和POD活性的上升。同时果实的蛋白含量也显著升高。在低温条件下，CAT和SOD活性受抑制，POD、PPO和 PAL活性被诱导并显著高于正常果实。这说明拮抗菌处理的冬枣果实可能通过加强氧化酶活性的方式来达到抗病的效果。拮抗菌和病原菌处理后，该部分组织的氧化酶活性加强，它们可以分解毒素，促进伤口愈合，抑制病原菌水解酶活性，从而抵抗病害的扩展。PAL是催化莽草酸途径的关键酶，可合成酚、植保素和木质素，而这些物质均与植物抗性有关。

UV-blue upconverted emission from Nd3+-doped InF3-based heavy-metal fluoride glasses for blue upconversion fibre laser

We report spectral properties and thermal stability of Nd3+-doped InF3-based heavy-metal fluoride glasses. Fluoroindate glasses in the chemical compositions (in mol%) of (38-x)InF3-16BaF(2)-20ZnF(2)-20SrF(2)-3GdF(3)-1GaF(3-)2NaF-xNdF(3) (x = 0.1, 0.5, 1, 2, 3) have been prepared under a controlled atmosphere in a dry box. Strong UVblue upconversion emission from a green excitation wavelength has been observed and the involved mechanisms have been explained. Near-infrared emission occurs simultaneously upon excitation of the UV-blue upconversion emissions with a cw Ar(+)laser. The upconversion spectra have revealed four dominant emissions at 354, 380, 412 and 449 nm, which belong to the transitions of D-4(3/2) -> I-4(9/2), D-4(3/2) -> I-4(11/2) and P-2(3/2) -> I-4(9/2), D-4(3/2) -> I-4(13/2) and P-2(3/2) -> I-4(11/2), D-4(3/2) -> I-4(15/2) and P-2(3/2) -> I-4(13/2), respectively.

甜樱桃果实采后生理、耐藏性及褐变机理的研究

本文以我国目前主要栽培的甜樱桃早、中、晚熟品种“红灯”、“佐藤锦”、“那翁”、“拉宾斯”和“砂蜜豆”等为试材，系统地研究了甜樱桃果实在不同O2和CO2浓度气调贮藏条件下的生理特性、风味品质和贮藏性，提出了适合于甜樱桃果实生理特性的气调指标和贮藏时间;分析了甜樱桃在不同贮藏条件下果实中乙烯、多酚氧化酶（PPO）、过氧化物酶（POD）、超氧化物歧化酶（SOD） 和丙二醛（MDA）的变化情况，揭示了它们与甜樱桃果实衰老、褐变及耐贮性的关系;分析了甜樱桃果实在不同贮藏条件下乙醇、色泽、硬度、可溶性固形物、酸和维生素C等物质成分的含量变化及与果实风味品质的关系;同时，还分析了不同甜樱桃品种果皮的结构特征及与耐藏性的关系，以及不同成熟度的甜樱桃果实在气调贮藏中的生理反应和品质变化。为形成甜樱桃果实采后商业化贮藏的系列配套技术提供了理论依据。 本文的主要研究内容包括：不同CO2浓度的气调贮藏对甜樱桃果实采后生理及品质的影响;高O2或高CO2浓度处理对甜樱桃果实褐变、衰老及风味品质的影响;动态气调贮藏和非动态气调贮藏对甜樱桃生理特性、风味品质和耐藏性的影响;不同成熟度及不同品种对甜樱桃耐藏性的影响;不同药剂配合包装处理对甜樱桃果实耐藏性及品质的影响。试验结果表明： 1. 甜樱桃果实适合于较高CO2浓度的CA贮藏：与自发性气调贮藏（MAP）相比，气调贮藏（CA）更能明显地延缓果实衰老，减少腐烂和褐变，保持风味品质和延长1.5~2倍的贮藏时间。其中以较高CO2浓度的（5% O2 + 10% CO2）气调贮藏效果最好，早熟品种“红灯”的贮藏期为60天，而中、晚熟品种“最上锦”、“佐藤锦”、“那翁”、“拉宾斯”和“砂蜜豆” 的贮藏期可达80-100天。果实在25℃下的货架存放时间为2-3天，在低温条件下（3-5℃）的货架时间是6天以上。 2. 高O2浓度气调对甜樱桃果实易造成伤害：用高O2浓度（70% O2 + 0% CO2）气调贮藏甜樱桃，在短期内可以抑制果实腐烂、减少果肉中挥发性代谢产物乙醇含量，但果实中的丙二醛含量上升迅速，褐变加剧，造成高氧伤害。 3. 动态气调贮藏更有利于延长甜樱桃果实的贮藏期：与非动态气调贮藏相比，贮藏前期用较高浓度CO2（20%）处理甜樱桃果实可有效控制维生素C含量的降低，丙二醛含量上升的速率较慢，可明显减少贮藏后期果实褐变和腐烂，保持风味品质。 4. 成熟度较高的甜樱桃果实适合于气调贮藏：成熟度较高（深红色时采收）的甜樱桃果实比成熟度低（鲜红色时采收）的果实耐藏性好。 5. 果实的耐藏性与果皮结构有关：耐藏性强的品种表皮细胞较小，排列紧密，细胞壁和外层蜡脂均较厚，果肉内部的维管束螺纹排列致密，果肉的薄壁细胞也排列得比较致密。 6. MAP与生物药剂配合有利于延长甜樱桃的贮藏期：生物1号药剂与加有TBZ的低密度塑料薄膜袋包装配合使用对控制甜樱桃果实腐烂、抑制果肉乙烯和乙醇生成、保持品质特性和延长贮藏时间都很有效。 7. 膜质过氧化是造成甜樱桃果实褐变的主要因素：甜樱桃果实褐变与PPO活性关系不大，但与膜质过氧化作用的产物—丙二醛（MAD）含量变化显著相关。

The mechanism of energy storage by shearing the solar magnetic field

In this paper, a complete set of MHD equations have been solved by numerical calculations in an attempt to study the dynamical evolutionary processes of the initial equilibrium configuration and to discuss the energy storage mechanism of the solar atmosphere by shearing the magnetic field. The initial equilibrium configuration with an arch bipolar potential field obtained from the numerical solution is similar to the configuration in the vicinity of typical solar flare before its eruption. From the magnetic induction equation in the set of MHD equations and dealing with the non-linear coupling effects between the flow field and magnetic field, the quantitative relationship has been derived for their dynamical evolution. Results show that plasma shear motion at the bottom of the solar atmosphere causes the magnetic field to shear; meanwhile the magnetic field energy is stored in local regions. With the increase of time the local magnetic energy increases and it may reach an order of 4×10^25 J during a day. Thus the local storage of magnetic energy is large enough to trigger a big solar flare and can be considered as the energy source of solar flares. The energy storage mechanism by shearing the magnetic field can well explain the slow changes in solar active regions.

Ultra-dry oxygen atmosphere to protect tellurite glass fiber from surface crystallization

In this study we report on surface crystallization phenomena and propose a solution for the fabrication of long and robust tellurite glass fibers. The bulk tellurite glasses of interest were prepared by melting and quenching techniques. Tellurite glass preforms and fibers were fabricated by suction casting and rod-in-tube drawing methods, respectively. The surfaces of the tellurite bulk glass samples and of the drawn fibers prepared under different controlled atmospheres were examined by X-ray diffraction. When the tellurite glass fibers were drawn in ambient air containing water vapor, four primary kinds of small crystals were found to appear on the fiber surface, alpha-TeO(2), gamma-TeO(2), Zn(2)Te(3)O(8) and Na(2)Zn(3)(CO(3))(4)center dot 3H(2)O. A mechanism for this surface crystallization is proposed and a solution described, using an ultra-dry oxygen gas atmosphere to effectively prevent surface crystallization during fiber drawing. (C) 2010 Elsevier B.V. All rights reserved.

DISSOCIATIVE RECOMBINATION OF PROTONATED PROPIONITRILE, CH3CH2CNH+: IMPLICATIONS FOR TITAN'S UPPER ATMOSPHERE

The dissociative recombination of protonated propionitrile, CH3CH2CNH+, has been investigated at the heavy ion storage ring, CRYRING, at the Manne Siegbahn Laboratory, Stockholm University, Sweden. The thermal rate coefficient has been deduced to follow k(T) = (1.5 +/- 0.2) x 10(-6) (T/300)(-0.76) (+/-) (0.02) cm(3) s(-1) for electron temperatures ranging from similar to 10 to similar to 1000 K. Measurements of the branching fractions were performed at similar to 0 eV relative kinetic energy. It has been found that in 43% +/- 2% of the reactions the four heavy atoms remain in the same product fragment. An equal portion of the reactions leads to products where one of the heavy atoms is split off from the other three and 14% +/- 1% result in a breakup into two heavy fragments containing two heavy atoms each. We discuss the significance of the data to Titan's upper atmosphere.

Electrochemical investigations of micro-droplets formed on metals during the deliquescence of salt particles in atmosphere

CORROSION; WATER; SPECTROSCOPY; CHLORIDE; ZINC; NUCLEATION; INTERFACE; ELECTRODE; SURFACES; GROWTH

Phenomenon of micro-droplets formation on metals during the deliquescence of salt particles in atmosphere

CORROSION; MECHANISM; WATER; ZINC

Effects of temperature on CO2 exchange between the atmosphere and an alpine meadow

The alpine meadow ecosystem on the Qinghai-Tibetan Plateau is characterized by low temperatures because of its high elevation. The low-temperature environment may limit both ecosystem photosynthetic CO2 uptake and ecosystem respiration, and thus affect the net ecosystem CO2 exchange (NEE). We clarified the low-temperature constraint on photosynthesis and respiration in an alpine meadow ecosystem on the northern edge of the plateau using flux measurements obtained by the eddy covariance technique in two growing seasons. When we compared NEE during the two periods, during which the leaf area index and other environmental parameters were similar but the mean temperature differed, we found that NEE from 9 August to 10 September 2001, when the average temperature was low, was greater than that during the same period in 2002, when the average temperature was high, but the ecosystem gross primary production was similar during the two periods. Further analysis showed that ecosystem respiration was significantly higher in 2002 than in 2001 during the study period, as estimated from the relationship between temperature and nighttime ecosystem respiration. The results suggest that low temperature controlled the NEE mainly through its influence on ecosystem respiration. The annual NEE, estimated from 15 January 2002 to 14 January 2003, was about 290 g CO2 m(-2) year(-1). The optimum temperature for ecosystem NEE under light-saturated conditions was estimated to be around 15 degrees C.

中国北方表沙无机碳储量及次生碳酸盐固碳潜力研究

This paper selected the Taklamakan Desert and the Badain Jaran Desert as the research areas, tested the carbonate content of surface-sand samples of dunes using Eijkelkamp carbonate goniophotometer, and analyzed the spatial-distribution characteristics of carbonate and estimated the carbonate-stock and secondary carbonate-stock in 1m depth of surface sand in the Taklamakan Desert and the Badain Jaran Desert. In addition, the paper test XRD, SEM, TDA, stable carbon isotope and radioactive strontium isotope of lacustrine deposits in the Taklamakan Desert and carbonates, such as kunkar, root canal, lacustrine deposits, sinter and calcrete, in the Badain Jaran Desert. Resting on the achievements by our predecessors, it analyzed the mineral-composition differences of the carbonates, calculated the contents of secondary carbonate and, furthermore, evaluated their potential of sequestration of CO2 in the atmosphere. The overall goal of this study was to increase our understanding of soil carbonate in the context of carbon sequestration in the arid region in China. That is, to advance our understanding about whether or not secondary carbonate in desert is a sink for atmospheric CO2. The following viewpoints were obtained: 1 Carbonate contents of surface-sand samples decend from the south to the north of the Taklamakan Desert. The minimum lies in the south and the maxmum in the mid. Carbonate content of surface-sand of megadunes in the Badain Jaran Desert has low value generally in the dune-crest and the base of slope, and large value in the mid. The average of Carbonate contents of all sorts of collected samples in the same area of the Taklamakan Desert has small diffetences. The average is about 9%. 2 Using carbonate contents as key parameters, calculate the carbon-stock of carbonates in 1m depth of surface sand in the Taklamakan Desert and the Badain Jaran Deser.They are 1.13Pg and 0.19 Pg respectively. There are 0.53Pg and 0.088Pg carbon-stock of secondary-carbonates in 1m depth of surface sand in the Taklamakan Desert and the Badain Jaran Desert. 3 Through testing data from XRD （X-ray diffraction）and TAD ( Thermal Analysis Data), the most significant conclusion derived from is that the main mineral ingredient is calcite in different carbonate substances in arid regions, From the SEM(Scanning electron microscopy ) images, can obtains the information about the micro environment of different carbonate forms in which they can grow. 4 Selected gas by termal cracking and traditional phosphoric acid method, their δ13C show that δ13C is a good parameter to indicate the micro environment in which different secondary carbonate forms. From the δ13C of the same type samples, if the redeposit degree is hard, theδ13C is light, the redeposit degree is weak, the δ13C is heave. and the δ13C of the different type samples, δ13C is mainly controlled by the micro environment in which secondary formed. if the procedure is characterized by redeposit and dissolve of marine facies carbonate, δ13C is heavy, it is characterized by CO2 which produced by plant respiration,δ13C is light. 5 From the δ13C of lacustrine deposit in the different grain size, there exsit certain differences in their micro environment and secondary degree among different grain size in the same grade. 6 The secondary carbonate content of lacustrine deposits in Taklimakan Desert is 47.26%. And those of root canal, sinter, calcrete, kunkar, lacustrine deposit and surface sand in Badain Jaran Desert are 91.74%, 78.46%, 76.26%, 87.87%, 85.37%and 46.49%, respectively. Of different grain size samples, the secondary carbonate contents of coarse fraction (20-63μm), sub-coarse fraction (5-20μm) and fine fraction (<5μm) are 80.10%, 47.2%and 50.07%, respectively. 7 There is no obvious relevance betweenδ13C of secondary carbonate and the content of secondary carbonate,theδ13C of secondary carbonate mainly reflects the parameters of secondary process, the content of secondary carbonate reflects difference of secondary degree.. 8 Silicates potentially supply 3.4 pencent calcium source during forming process of lacustrine deposits in Taklimakan Desert. If calcium source is mainly supplied by goundwater, it can be calculated that about 5.18 %, 6.13%, 5.68%, 5.64 % and 6.82% silicates supply calcium source respectively for root canal, kunkar, lacustrine deposit, calcrete and sinter, during the forming process of different kinds of carbonates in Badain Jaran Desert.

Effect of ambient pressure and radiation reabsorption of atmosphere on the flame spreading over thermally thin combustibles in microgravity

For the flame spread over thermally thin combustibles in an atmosphere, if the atmosphere cannot emit and absorb the thermal radiation (e.g. for atmosphere Of O-2-N-2), the conductive heat transfer from the flame to the fuel surface dominates the flame spread at lower ambient atmosphere. As the ambient pressure increases, the flame spread rate increases, and the radiant heat transfer from the flame to the fuel surface gradually becomes the dominant driving force for the flame spread. In contrast, if the atmosphere is able to emit and absorb the thermal radiation (e.g. for atmosphere Of O-2-CO2), at lower pressure, the heat transfer from flame to the fuel surface is enhanced by the radiation reabsorption of the atmosphere at the leading edge of the flame, and both conduction and thermal radiation play important roles in the mechanism of flame spread. With the increase in ambient pressure, the oxygen diffuses more quickly from ambient atmosphere into the flame, the chemical reaction in the flame is enhanced, and the flame spread rate increases. When the ambient pressure is greater than a critical value, the thermal radiation from the flame to the solid surface is hampered by the radiation reabsorption of ambient atmosphere with the further increase in ambient pressure. As a result, with the increase in ambient pressure, the flame spread rate decreases and the heat conduction gradually dominates the flame spread over the fuel surface.

Numerical simulation of an adaptive optics system with laser propagation in the atmosphere

A comprehensive model of laser propagation in the atmosphere with a complete adaptive optics (AO) system for phase compensation is presented, and a corresponding computer program is compiled. A direct wave-front gradient control method is used to reconstruct the wave-front phase. With the long-exposure Strehl ratio as the evaluation parameter, a numerical simulation of an AO system in a stationary state with the atmospheric propagation of a laser beam was conducted. It was found that for certain conditions the phase screen that describes turbulence in the atmosphere might not be isotropic. Numerical experiments show that the computational results in imaging of lenses by means of the fast Fourier transform (FFT) method agree well with those computed by means of an integration method. However, the computer time required for the FFT method is 1 order of magnitude less than that of the integration method. Phase tailoring of the calculated phase is presented as a means to solve the problem that variance of the calculated residual phase does not correspond to the correction effectiveness of an AO system. It is found for the first time to our knowledge that for a constant delay time of an AO system, when the lateral wind speed exceeds a threshold, the compensation effectiveness of an AO system is better than that of complete phase conjugation. This finding indicates that the better compensation capability of an AO system does not mean better correction effectiveness. (C) 2000 Optical Society of America.

Flow Characteristics and Its Friction Coefficient of Laminar Near-Wall Boundary Layer in Dusty Atmosphere

采用双向耦合的双流体模型,研究了大气悬浮沙尘的存在对大气边界层中层流底层流动特性及摩阻系数的影响,计算并讨论了不同沙尘含量下含尘大气相对于无尘大气摩阻系数的变化。结果表明：摩阻系数的变化取决于悬浮沙尘的初始运动状态和质量载荷率。