土壤铅和镉溶出伏安法检测中影响因素及其削弱方法研究进展

溶出伏安法具有分析速度快、成本低、灵敏度高等优点被广泛应用于检测土壤重金属含量,但在检测土壤重金属时,溶出伏安检测精度会受到多方面因素的影响。该文在介绍溶出伏安法工作原理的基础上,从伏安参数、试验条件和土壤物质成分三方面阐述溶出伏安法检测土壤Pb2+和Cd2+为的影响因素,解析各因素的影响机理,归纳影响削弱方法的研究进展。研究结论为：方波脉冲阳极溶出伏安法最常用于检测土壤Pb2+和Cd2+,伏安参数包括脉冲幅值、电压增量和脉冲频率,试验条件包括沉积时间、沉积电压和支持电解质种类及其pH值,土壤成分主要干扰因素包括非目标重金属和有机质。针对伏安参数和试验条件的影响可以设计优化试验有效削弱。针对非目标重金属和有机质的干扰影响,目前研究还没有提出有效的削弱方法。最后,展望了溶出伏安法检测土壤重金属的未来发展方向。     

siRNA干涉禽流感病毒PA基因在鸡胚成纤维细胞中的表达

用阳离子脂体质转染试剂将人工合成的小干扰RNA(Small interference RNA,siRNA)转染鸡胚成纤维细胞(CEF).结果表明,针对禽流感病毒(AIV)H5N1亚型核蛋白(NP)基因的siRNA能在AIV感染后1,2,3 h显著抑制NP基因的表达,表达水平分别降低3,1.4和2.5倍.     

碱性蛋白酶产生菌S9发酵条件的研究

为了解大庆地区盐碱土中嗜碱微生物蛋白酶产生情况,对大庆市盐碱土中筛选出的一株碱性蛋白酶菌株S9,通过单因子试验与正交试验确定该菌株的最佳培养基为:葡萄糖2%、硫酸铵2%、酵母浸粉0.5%;最佳培养条件为:温度30 ℃,pH 9.5.     

不同培养条件对微藻总脂含量和脂肪酸组成的影响

微藻细胞中脂类的数量及质量是评价其营养价值的重要指标。大量研究表明,改变培养条件及在不同的时期收获对微藻的脂肪含量和脂肪酸组成有着显著影响。本文主要从培养基成分、光强、温度、通气量和生长期5个方面综述了相关的研究成果,希望能为海洋微藻的研究和开发利用提供有价值的参考。     

鰤鱼诺卡氏菌培养条件及培养基的优化

对鰤鱼诺卡氏菌（Nocardia seriolea）ZJ0503的增菌培养基和生长条件进行优化。研究了温度、盐度、初始pH对鰤鱼诺卡氏菌生长的影响,并通过单因素试验对培养基的碳源、氮源和无机盐成分进行了筛选,采用正交实验法对培养基各主要成分的添加量进行了优化。结果表明,鰤鱼诺卡氏菌最适宜生长条件为温度25 ℃、盐度5、pH 6.5±0.2;经筛选,鰤鱼诺卡氏菌培养基中最佳碳源是葡萄糖,最佳氮源是酵母粉,促生长作用最强的2种无机盐是磷酸氢二钾（K2HPO4）和氯化钙（CaCl2）;确立了培养基优化配方为葡萄糖20 g·L-1,酵母粉15 g·L-1,K2HPO4 0.75 g·L-1,CaCl 20.2 g·L-1（单独灭菌）,氯化钠（NaCl2）5 g·L-1,pH 6.5±0.2。     

Logging pattern and landscape changes over the last century at the boreal and deciduous forest transition in Eastern Canada

Forestry practices associated with the industrial era (since ~1900) have altered the natural disturbance regimes and greatly impacted the world’s forests. We quantified twentieth century logging patterns and regional scale consequences in three sub-boreal forest landscapes of Eastern Canada (117,000, 49,400 and 92,300 ha), comparing forestry maps depicting age and forest cover types for early industrial (1930) and present-day (2000) conditions. Results were similar for the three landscapes, indicating large-scale forest change during the twentieth century. In 1930, previous logging activities had been concentrated in the lowlands and along the main hydrographical network, as compared to a more even distribution over the landscapes in 2000, reflecting a decreasing influence of the environmental constraints on forest harvesting. In 1930, old-aged forests (>100 years) accounted for more than 75% of the unlogged areas of the three landscapes, as compared to less than 15% for the present-day conditions. Logging practices have thus inverted the stand age distribution of the landscapes that are currently dominated by young and regenerating stands. The 1930 forest cover types showed a clear relationship with elevation, with conifers located in the lowlands and mixed and deciduous stands restricted to the upper slopes. Between 1930 and 2000, 58–64% of the conifer areas transformed to mixed and deciduous forests, such that no clear altitudinal relationships remained in 2000. We conclude that twentieth century logging practices have strongly altered the preindustrial vegetation patterns in our study area, to the point that ecosystem-based management strategies should be developed to restore conifer dominance, altitudinal gradients, as well as the irregular structure inspired from old forest stands.     

试验干扰下土壤中微量元素空间变异性研究

[目的]为了解烟草试验站土壤中微量元素的空间变异性,进而为大田试验布局提供依据。[方法]用地统计学方法,分析彭水试验站的耕层土壤养分的空间变异特征。[结果]该站内土壤有效铁、有效铜、有效钙的含量丰富;有效锌和有效锰为中等含量水平,有效硫和有效镁含量从低至高均有分布。各中微量元素间具有显著的相关性。所有元素均可用指数模型和球状模型进行较好拟合;有效锌、有效镁和有效硫由于受结构性因素影响而呈现强空间自相关性;其余元素的空间自相关性由结构性因素和随机因素共同作用而呈现中等空间相关性。Kriging插值显示,东部及东北部较高,中部和西南部区域含量较低;有效铁、有效钙和有效硫的空间分布的规律性差。[结论]该试验站土壤中微量元素含量存在较大的空间变异性。在安排大田试验时,要充分认识这种变异性,合理布局大田试验。     

Deficit irrigations during soybean reproductive stages and CROPGRO-soybean simulations under semi-arid climatic conditions

This study was carried out to determine the effect of water stress on five different generative stages of soybeans and to evaluate the CROPGRO-soybean model under semi-arid climatic conditions. The study was conducted at the Faculty of Agricultural Engineering, Harran University research field in 2003 and 2004 growing seasons. Plants received full irrigation during vegetative stages, after which it was cut off at different reproductive stages (treatments): R_1-2, beginning of flowering and full bloom; R₃, beginning of pod; R₄, full pod; R₅, beginning of seed; and R₆, full seed. The control treatment was full irrigation throughout. Observed yields ranged from 1955 (R₆) to 3684 kg ha⁻¹ (control) in 2003, and from 1867 (R₆) to 3952 kg ha⁻¹ (control) in 2004, respectively. Generally, in both of the years any water stress imposed on soybeans in three different generative stages (R₃, R₅, and R₆) resulted in substantial yield reduction compared with full irrigation; yield reduction was greatest at the R₆ stage. Biomass and 1000 seed weight also showed significant difference. Overall, CROPGRO-soybean simulated parameters from all treatments were higher compared with observed ones. Although simulated yield results were close to measured ones, they could not track observed yield patterns. Generally, the CROPGRO-soybean simulation model failed to satisfactorily mimic observed soybean yield, biomass, and 1000 seed weight and therefore it is suggested not to be used for similar scenarios and climatic conditions.     

异硫氰酸荧光素标记鳗弧菌条件优化及应用条件对荧光信号的影响

为了实现对目标细菌的有效示踪,实验以异硫氰酸荧光素(FITC)为标记物,分别设置FITC标记浓度0.2、2、20、50、100、200μg/mL,标记时间1、15、30、60、120、240 min,研究了FITC标记浓度与标记时间对鳗弧菌标记效果的影响,同时对在不同温度(25、4、-20、-70℃)及不同时间(24、48、96、192 h)存储条件下鳗弧菌标记荧光的稳定性进行了比较,对标记鳗弧菌经甲醛灭活后的荧光变化进行了观察,研究了不同光照条件(0、150、1 500、25 000 lx)对标记鳗弧菌的荧光衰减影响,以及在-20和-70℃条件下反复冻融对标记鳗弧菌荧光强度的影响。结果表明,FITC的最适标记浓度范围为20~100μg/mL,最适标记时间范围60~120 min,储藏在-20和-70℃条件下,标记后的鳗弧菌荧光信号比储藏在4和25℃条件下稳定,标记后的鳗弧菌经甲醛灭活后的荧光信号稳定性优于对照组,不同强度自然光照对标记鳗弧菌的荧光衰减效果不明显,标记细菌经3次冻融,发现在-70℃条件下冻存的细菌荧光信号稳定性保持良好。本研究结果为FITC用于标记海洋细菌提供了实用的技术参数。     

2000—2019年黄土高原地区土壤保持时空变化及影响因素分析

为揭示全球气候变化背景下黄土高原的生态建设成效,以土壤保持量为评估指标,应用美国修正通用土壤流失方程,评估了黄土高原土壤保持服务功能以及植被、气象等因素对其影响,分析了2000年以来植被和气候变化影响下黄土高原土壤保持量时空动态变化特征。结果表明:2000—2019年黄土高原土壤保持量平均值为109.5 t/hm²,并呈增加趋势,平均每年增加2.0 t/hm²,空间分布黄土高原中部和东部土壤保持量增加较明显。2000年以来黄土高原地区植被NPP呈增加趋势,年平均值为330.5 gC/m²,且平均每年增加7.2 gC/m²; 2000年以来植被覆盖度年平均值为29.2%,且以平均每年0.52%的趋势增加。黄土高原地区2000年以来气温和降水量均显著增加,平均年降水量为469.1 mm,且呈增加趋势,平均每年增加3.1 mm,年平均气温为10.2℃,平均每年增加0.03℃。黄土高原生态恢复措施加强,加之区域“暖湿化”有利气候条件,促进了区域生态建设成效显现,成为黄土高原生态恢复、功能提升的重要因素之一。