白杨派杂种无性系及其亲本光合和生长对盐胁迫的反应

以白杨派单交和双交杂种无性系1年生扦插苗为材料,分析不同盐胁迫条件下无性系的生长及光合系统的反应,并对无性系间的差异进行比较.研究表明:盐胁迫对叶片生长、苗高生长及苗木生物量积累均产生不同程度的影响.随着盐浓度升高,各项生长指标迅速下降,但下降的幅度不同,苗木生物量积累受影响最大.茎叶生长对盐胁迫的敏感性大于根系生长,从而导致根/(茎 叶)生物量随盐胁迫的发展而升高.盐胁迫下4个无性系的净光合速率(Pn)日变化基本上都呈单峰曲线,但随胁迫加强,Pn值迅速降低.盐胁迫下,叶位从幼到老,Pn表现为单峰型变化,中部功能叶Pn值最大,嫩叶和老叶较小,盐胁迫对无性系嫩叶Pn几乎无影响,却显著降低中部功能叶和老叶的Pn值,且随着胁迫时间延长,对叶片Pn的影响加强.盐胁迫降低各无性系的叶绿素含量,且使叶绿素荧光诱导动力学曲线发生明显变化,其参数qN(荧光非光化学猝灭系数)值随盐浓度增加而上升,而qp(荧光光化学猝灭系数)、Fv/Fo(PSⅡ潜在活性)值随盐浓度增加而下降.盐胁迫对双交杂种无性系B430影响最小,单交无性系毛新杨和亲本新疆杨次之,亲本毛白杨对盐胁迫反应最敏感.     

果胶酶降解壳聚糖工艺优化及特性动态变化分析

通过正交试验对果胶酶水解壳聚糖的工艺进行优化，并对降解过程中粘度、还原糖生成量、平均分子量等指标的动态变化进行研究。结果表明，果胶酶在50℃、pH值4．5、酶用量与壳聚糖质量之比为3、壳聚糖脱乙酰度为80％时对壳聚糖降解效果最佳，其中底物脱乙酰度对酶解效果影响极显著。在最适条件下，果胶酶对壳聚糖水解约1h，可控制产物平均分子量在2500左右。果胶酶降解壳聚糖的起始速度非常快，反应30min后粘度下降基本平稳；水解反应进行135min后，产物还原糖生成量逐渐趋于平稳。     

超声波降解苹果汁中展青霉素动力学研究

为了掌握超声波降解苹果汁中展青霉素的动力学特性,在前期超声波降解苹果汁中展青霉素的研究基础上,利用拟一级反应动力学方程对超声波影响因素中超声波功率、频率及温度降解苹果汁中展青霉素的试验数据进行拟合,确定相关参数,进一步建立各影响因素降解速率常数与相关影响因子之间的关系方程。结果表明:超声波功率对苹果汁中展青霉素的降解符合拟一级反应方程,超声波功率为490 W时,降解率最大;功率降解速率常数kP与超声波功率的方程为kP=6×10-5P-0.011 7。超声波频率对展青霉素的降解符合拟一级反应方程,超声波频率为45 k Hz时,降解率最大;频率降解速率常数kf与超声波频率f的关系方程为kf=-8×10-4f2+0.111 9f-2.512 6。温度对苹果汁中展青霉素的降解符合拟一级反应方程,温度为30℃时,降解率最大;温度降解速率常数kT与温度T的关系方程为kT=-1×10-4T2+0.006 1T-0.076 9。     

花生壳活性炭吸附染料废水中结晶紫的研究

利用磷酸处理微波照射制备花生壳活性炭,以一定浓度的结晶紫溶液为模拟染料废水,研究了吸附剂粒径、溶液pH值、结晶紫的初始浓度、吸附剂用量、吸附时间、吸附温度对结晶紫吸附性能的影响。结果表明花生壳活性炭是具有高去除率的廉价吸附剂,最大去除率达96%。结晶紫染料在花生壳活性炭上的吸附过程符合二级动力学模型和Freundlich等温吸附方程。     

3种抗生素对3种常见鱼类病原菌的抑菌活性研究

为研究盐酸恩诺沙星、乳酸恩诺沙星和乳酸诺氟沙星对嗜水气单胞菌(Aeromonas hydrophila)、鳗弧菌(Vibrio anguillarum)和哈维氏弧菌(Vibrioharveyi)的体外抑菌活性,本实验通过测定抑菌圈直径、最小抑菌浓度(MIC)、最小杀菌浓度(MBC)和杀菌曲线,研究3种常用喹诺酮类抗生素药物对3种水产病原菌的体外药效学特性.结果表明:乳酸诺氟沙星对嗜水气单胞菌和哈维氏弧菌抑菌效果最好,MIC分别为0.244μg/mL和1.954μg/mL:盐酸恩诺沙星对鳗弧菌抑菌效果最好,MIC为0.122μg/mL;8 MIC的乳酸诺氟沙星药液在12 h内完全杀灭嗜水气单胞菌,在24 h内也能全部杀灭哈维氏弧菌,8 MIC的盐酸恩诺沙星药液在24 h内全部杀灭鳗弧菌.本研究为3种抗生素在水产养殖中的应用提供实验依据.     

凹凸棒土吸附剂对单宁酸的吸附研究

为探明凹凸棒土吸附剂吸附单宁酸的吸附过程和机理,采用拟一级速率方程和拟二级速率方程,研究其吸附动力学;根据van't Hoff方程,研究其吸附热力学.结果表明:吸附符合拟二级速率方程;温度升高吸附速率常数和初始吸附速率均先增加后减小,单宁酸初始质量浓度增加则吸附速率常数和初始吸附速率均减小;凹凸棒土吸附剂对单宁酸的吸附...     

城市土壤的压实退化及其环境效应

城市土壤普遍存在严重的压实退化现象。由于压实的影响,土壤物理性质发生了显著的改变:结构破坏、容重和硬度增大、孔隙度和渗透性降低。这些重要的变化对土壤生物活动、土壤物理-化学平衡和氧化还原状况、土壤的过滤和缓冲性能都产生影响。由此对环境产生严重的负面效应:地下水的自然回灌减少,地表径流量增加,降雨的径流洪峰加快、加大,地表水体的污染负荷增加。土壤温度、微生物活动、养分转化都不同于自然土壤,植物的生长也受到严重的影响。     

Kinetics of soil microbial uptake of free amino acids

 Amino acids and proteins typically form the biggest input of organic-N into most soils and provide a readily available source of C and N for soil microorganisms. Amino acids can also be taken up directly by plant roots, providing an alternative source of available soil N. However, the degree to which plants can compete against the soil microbial population for amino acids in soil solution remains poorly understood. The aim of this study was to measure the rate of microbial uptake of three contrastingly charged ¹⁴C-labelled amino acids (glutamate^1–, glycine⁰, lysine^0.9+) over a wide concentration range (0.1–5 mM) and in two contrastingly managed soils varying in their degree of erosion, organic-C content and microbial biomass. Amino acid uptake was concentration dependent and conformed to a single Michaelis-Menten equation. The mean maximum amino acid uptake rate (V _max) for the non-eroded (control) soil (high organic-C, high biomass) was 0.13±0.02 mmol kg^–1 h^–1, while half maximal uptake occurred at a concentration (K _m) of 2.63±0.07 mM. Typically, V _max was fourfold lower and K _m twofold lower in the eroded soil (low available organic-C, low biomass) compared to the non-eroded (control) soil. Amino acid substrate concentration had little effect on the proportion of amino acid utilized in catabolic versus anabolic metabolism and was similar for both. While the results obtained here represent the summation of kinetics for a mixed soil population, they indicate that amino acid uptake is saturated at concentrations within the millimolar range. Because the affinity constants also were similar to those described for plant roots, we hypothesized that competition for amino acids between plants and microbes will be strong in soil but highly dependent upon the spatial distribution of roots and microbes in soil. Received: 2 March 2000     

基于冠层多光谱数据预测水稻氮素营养状况

A soil batch experiment was conducted to investigate both separate and compound effects of three types of surfactants： anionic dodecylbenzene sulfonic acid sodiumsalt （DBSS）, cationic cetyltrimethylammonium bromide （CTAB）, and nonionic nonyl phenol polyethyleneoxy ether （TX-100）, as well as ethylenediaminetetraacetic acid （EDTA） on cadmium solubility, sorption kinetics, and sorption-desorption behavior in purple soil. The results indicated that both individual application of the three types of surfactants and surfactants combined with EDTA could stimulate Cd extraction from the soil with a general effectiveness ranking of EDTA/TX-100 〉 EDTA/DBSS 〉 EDTA/CTAB 〉 EDTA 〉 TX-100 〉 DBSS 〉 CTAB. Further study showed that the compound application of surfactants and EDTA had stronger （P 〈 0.05） effects on Cd solubility than those added individually. The application of surfactants and EDTA to purple soil （P 〈 0.05） decreased the proportion of Cd sorbed, while their effectiveness ranking was similar to that of enhanced solubilization. The sorption kinetics of Cd in purple soil was best described by the double-constant equation, while the Freundlich equation gave an excellent fit to the sorption isotherm curves. Therefore, surfactant-enhanced remediation of Cd contaminated soil is feasible and further research should be conducted.     

l-Asparaginase activity of soils

Summary A simple, precise, and sensitive method to assay l-asparaginase (l-asparagine amidohydrolase, EC 3.5.1.1) activity in soils is described. This method use steam distillation to determine the NH _inf4 ^sup+ produced by l-asparaginase activity when soil is incubated with buffered (0.1 M THAM, pH 10) l-asparagine solution and toluene at 30°C for 2 h. The procedure developed gives quantitative recovery of NH _inf4 ^sup+ -N added to soils and does not cause chemical hydrolysis of l-asparagine. The optimum buffer pH for NH _inf4 ^sup+ -N released by l-asparaginase activity in soils was 10. This enzyme was saturated with 50 mM l-asparagine, and the reaction rate essentially followed zero-order kinetics. The d-isomer of asparagine was also hydrolyzed in soils, but at only 16% of the activity of the l-isomer at a saturating concentration of the substrate. The optimal temperature for the soil l-asparaginase reaction occurred at 60°C and denaturation began at 65°C. The Arrhenius equation plot for l-asparaginase activity in three selected soils was linear between 10 and 50°C. The activation energy values of this enzyme ranged from 20.2 to 34.1 (average 26.6) kJ mol^-1. Application of three linear transformations of the Michaelis-Menten equation showed that the K _m values of l-asparaginase in nine soils ranged from 2.6 to 10.0 (average 6.1) mM and the V _max values ranged from 9 to 131 g NH _inf4 ^sup+ -N released g^-1 soil 2 h^-1. The temperature coefficients (Q ₁₀) for soil l-asparaginase activity ranged from 1.12 to 1.70 (average 1.39). Steam sterilization (121°C for 1 h), formaldehyde, and NaF decreased the activity but the presence of toluene increased the amount of NH _inf4 ^sup+ released. Treatment of soils with dimethylsulfoxide completely destroyed l-asparaginase activity. The use of sulfhydryl reagents indicated that a free sulfhydryl moiety was required to maintain the active enzyme. l-Asparaginase activity in soils was increased by 13 to 18% in the presence of THAM buffer prepared to contain 5 mM Ca²⁺ and Mg²⁺, respectively.