低温风干工艺下酱鸭加工过程中品质特性变化规律研究

为改善酱鸭的质地、色泽和风味,本试验在传统酱鸭加工工艺的基础上,引入低温风干工艺制备酱鸭,并研究其加工过程中理化特性(水分含量、色泽、剪切力值、质构特性)和挥发性风味成分的变化。结果表明,在加工过程中,酱鸭水分含量从76.55%降至58.27%(P0.05);与原料肉相比,L~*值在风干6 h显著降低,a~*值在腌制和风干结束下降,b~*值和咀嚼性在酱制阶段增加,杀菌阶段下降,硬度在酱制阶段升高,而弹性和内聚性均在杀菌阶段降低;与风干24 h相比,胶着性在杀菌阶段降低(P0.05),剪切力值先升高后下降。酱鸭挥发性风味成分分析显示,酱鸭成品有70种挥发性风味成分,主要为萜烯类、醛类、呋喃类、酮类、烃类和醇类;其中,莰烯、己醛和2-戊基呋喃是酱鸭成品主要的特征风味成分,分别占总相对含量的16.51%、10.44%和11.88%。本试验结果为低温风干工艺下酱鸭品质变化特征的研究提供了一定的理论依据。     

水体太阳能供电增氧系统及其运行效果

为了快速改善水产养殖水体质量,该文分析了国内水体富营养化的现状和存在的问题,提出了以太阳能电池为动力,采用单片机设计了一套水体增氧系统,重点介绍了硬件组成、结构特点和软件实现方法,并应用在公园鱼池净化和鲤鱼养殖生产中。试验结果表明,该系统能够实时控制鱼池中的溶氧量、pH值,使多环境因子稳定在最佳值附近。为增强水体的自净能力,提高水产养殖水平提供了一种切实可行的技术措施。     

基于改进极限学习机的水体溶解氧预测方法

为了有效地指导水产养殖生产,提高溶解氧浓度预测的精度,提出了基于因子筛选和改进极限学习机（Extreme Learning Machine,ELM）的水产养殖溶解氧预测模型。首先,利用皮尔森相关系数法计算各影响因子与溶解氧浓度间的相关系数,提取强关联因子,降低预测模型的输入量维度;采用偏最小二乘算法（Partial Least Square, PLS）优化传统ELM神经网络,避免网络中隐含层共线性问题,保障输出权值的稳定性;然后,结合新型激活函数,构建水体溶解氧浓度预测模型。最后,将SPLS-ELM（Selection Based Partial Least Square Optimized-Extreme Learning Machine）预测模型应用到江苏省无锡市南泉基地某试验池塘的水体溶解氧预测中。试验结果表明：该模型的预测均方根误差为0.323 2 mg/L,与最小二乘支持向量机（Least Square Support Vector Machine,LSSVM）、BP神经网络、粒子群（Particle Swarm Optimization,PSO）优化LSSVM和遗传算法（Genetic Algorithm, GA）优化BP神经网络相比分别降低40.98%、44.48%、34.73%和44.18%。且该模型的运行时间仅0.623 1s,预测精度和运行效率明显优于其他模型。该模型的溶解氧预测曲线接近真实溶解氧变化曲线,能够满足水产养殖实际生产对水体溶解氧预测的要求。     

The plasma membrane intactness of root-tip cells is a primary factor for Al-tolerance in cultivars of five species

We investigated the role of the cell wall and plasma membrane (PM) of root-tip cells in Al tolerance in Al-tolerant and Al-sensitive cultivars of five plant species (rice, maize, pea, wheat, and sorghum). No correlation was found between the differences in Al tolerance and the cation exchange capacity of cell walls isolated from root-tips (0–1 em). Preliminary exposure to Al for 1 h was sufficient to inhibit subsequent root re-elongation in an Al-free solution, and the inhibitory effect was more pronounced in the Al-sensitive cultivars than in the Al-tolerant ones. Together with the inhibition of root re-elongation, the PM of the root-tip cells of all the Al-sensitive cultivars was more permeabilized than that of the Al-tolerant cultivars, based on the FDA-PI fluorescence staining technique. Exposure for 30 min to Al treatment at 100 µM significantly increased the PM permeability of protoplasts isolated from the root-tips for the Al-sensitive pea cultivar placed in a moderately hypotonic medium. Protoplasts from root-tip portions of all the Al-sensitive cultivars took up more Al than those of the Al-tolerant ones when treated with 100 pM Al under isotonic conditions for 30 min. The co-existence of DNP or hypotonic conditions led to a larger increase of Al uptake by the protoplasts from Al-sensitive maize cultivars. These results suggest that Al ions rapidly alter the PM of the root-tip portion in the Al-sensitive cultivars, irrespective of plant species, resulting in an increase of the PM permeability.     

外源一氧化氮对NaCl胁迫下番茄幼苗活性氧代谢的影响

研究了在100 mmol/L NaCl胁迫下,外源NO供体硝普钠（SNP）处理对耐盐性不同的2个番茄品种（沪番‘1480’和沪番‘2496’）幼苗叶片活性氧（ROS）水平和保护酶活性的影响。结果表明,外源NO提高了盐胁迫下SOD、POD、CAT和APX活性,AsA和GSH含量以及脯氨酸和可溶性糖含量,降低了MDA含量和O2- 产生速率;与耐盐品种‘1480’相比,NO处理对盐敏感品种‘2496’效果更明显。表明外源NO通过促进盐胁迫下保护酶活性、抗氧化剂和渗透调节物质的提高,降低ROS水平,缓解NaCl胁迫对番茄幼苗生长的抑制作用,增强植株的耐盐能力。     

Dynamics of dissolved oxygen (DO) in ponded water of a paddy field

The transfer of heat and dissolved oxygen (DO) through water is important to understand the phenomenon of ponded water in a paddy soil. The heat from solar radiation is absorbed at the soil surface and transferred into the ponded water by convection. This study clarified the dynamics of DO, as well as the role of convection in water in DO transfer in the ponded water of a paddy field. DO concentration in the ponded water of a paddy field was measured in situ in the daytime and during the night. The results were confirmed in lab-scale model experiments. The DO concentration and temperature profiles in the ponded water of a lab-scale paddy field model were investigated under convective and non-convective conditions using solar radiation and infrared radiation, respectively. Under the ponded condition, solar radiation was absorbed at the soil surface whereas infrared radiation was absorbed at the water surface and thereby convective and non-convective conditions were generated, respectively. The diurnal variation in DO concentration was closely related to the intensity of solar radiation. Oxygen generation by micro-algae and its subsequent circulation by convection resulted in uniform DO concentration profiles, with super-saturated values in the ponded water in the daytime. Eventually oxygen was released to the atmosphere by deaeration until DO in water was depleted to the saturated level. During the night the oxygen moved from the atmosphere into the water surface by reaeration which depends on the oxygen deficit related to saturation. The oxygen deficit is caused by the respiration of microorganisms. The oxygen, that moved from the atmosphere to the water surface, was transferred to the soil surface by convection in the water layer. Thus convection plays an important role in the DO transfer in the ponded water of a paddy field. The DO dynamics is correlated with biological processes in the ponded paddy soil.     

不同增氧水平对夏玉米生长及氮素利用的影响

为探究有利于夏玉米生长和氮素利用的适宜灌溉水溶解氧浓度,本试验以夏玉米为供试作物,采用地下滴灌供水方式,以地下水灌溉为对照,设置10(OA10)、20(OA20)和40(OA40) mg·L^-1灌溉水溶解氧浓度3个增氧水平,研究不同增氧水平对盆栽夏玉米生长、产量和氮素利用的影响。结果表明,增氧地下滴灌显著提高了土壤溶解氧浓度,与对照相比,OA40、OA20和OA10处理土壤溶解氧浓度平均提高14.83%、9.71%和8.00%,表现为作物生长增强,作物产量和氮素利用效率均显著提高(P<0.05)。与对照相比,OA10处理的株高、叶鲜质量和叶干质量分别增加7.39%、16.30%和12.02%;OA40处理叶干质量和茎鲜质量分别增加15.82%和12.43%;OA10、OA20和OA40根系鲜质量分别增加60.00%、17.66%和52.98%,根系体积分别增加34.03%、14.56%和51.32%;OA10和OA20处理根系活力分别增加272.77%和64.44%;OA10和OA40处理产量分别增加24.46%和21.83%,水分利用效率分别提高19.10%和21.61%,百粒重分别增加17.53%和15.14%。OA10和OA40处理籽粒氮素吸收量较对照分别增加63.90%和35.27%,OA10处理籽粒氮素分配比例和氮素吸收效率分别增加21.57%和33.33%。上述差异均具有统计学意义(P<0.05)。综上,增氧地下滴灌可显著提高作物根区溶解氧浓度,促进作物生长,提高产量及氮素吸收利用,以OA10处理效果最为显著。本研究结果为增氧灌溉技术在实际生产中的合理利用提供了理论依据。     

微孔曝气流量与曝气管长度对水体增氧性能的影响

为了探究曝气流量与曝气管长度对增氧性能的影响,在不同曝气流量、不同曝气管长度条件下进行了室内水体底部微孔曝气增氧试验。分析了曝气流量与曝气管长度对氧体积传质系数、增氧量和氧利用率的影响。研究结果表明,当曝气流量为0.27~0.55 m3/s、曝气管长为0.9~1.5 m时,所对应的氧体积传质系数在0.63~1.1 h-1变化,增氧量在6.8~12.9 g/h变化,氧利用率在6.87%~9.28%变化,且在一定的曝气管长度下,氧体积传质系数、增氧量均与曝气流量成正比,而氧利用率则与其成反比关系;在一定的曝气流量下,曝气管长度对氧体积传质系数产生的影响表现为先高后低再高的趋势;氧体积传质系数与修正的饱和溶解氧浓度是否作为增氧量的主要影响因子取决于曝气管长度;曝气流量对氧利用率较曝气管长度更为敏感。研究还发现,微孔曝气系统中存在着最优曝气管长度,使得增氧性能最佳,并建立了最优曝气管长度与曝气流量、水深、输入压力、最优初始气泡直径的相关关系式,为低碳经济下微孔曝气系统的设计和运行提供了理论依据。     

基于PC-RELM的养殖水体溶解氧数据流预测模型

养殖水体中溶解氧浓度一直是最重要的水质参数之一。为了精准地对水体溶解氧进行调控,提高养殖生产效率,降低养殖风险,该研究考虑外部天气条件对溶解氧的影响以及溶解氧自身的昼夜变化特征,提出一种基于正则化极限学习机（principal component analysis and clustering method optimized regularized extreme learning machine,PC-RELM）的养殖水体溶解氧数据流预测模型。首先,采用主成分分析法判断影响溶解氧浓度的强重要性因子,降低预测模型的数据维度;其次,利用熵权法计算各时刻点的天气环境指数,并利用快速动态时间规整算法（fast dynamic time warping,FastDTW）完成时间序列数据流在不同天气环境下的相似度度量;然后使用k-means算法对时间序列的相似度进行聚类分簇,并基于分簇结果完成正则化极限学习机预测模型的构建,实现溶解氧浓度的估算。最后将PC-RELM模型应用到无锡南泉试验基地养殖池塘的溶解氧预测调控过程中。试验结果表明：PC-RELM的预测均方根误差值（root mean square error, RMSE）为0.961 9,与PLS-ELM（partial least squares optimized ELM）、最小二乘支持向量机（least square support vector machine,LSSVM）以及BP神经网络模型进行对比,其RMSE值分别降低了41.54%、54.58%和67.16%。该预测模型可以有效地捕捉不同天气条件下溶解氧的变化特点,具有较高的预测精度和效率。     

基于空间分布的草原化荒漠地区红砂种群水分利用策略研究

[目的]研究区域尺度上荒漠灌木水分适应与分布格局相呼应关系,揭示干旱半干旱地区植物种群对环境响应的过程与机理,为深入理解植物与环境协同进化规律提供依据。[方法]采用点格局分析方法和氢氧稳定同位素示踪技术,分析了红砂(Reaumuria songarica)种群的空间分布格局、水分利用策略。[结果](1)在完全空间随机零模型下,红砂种群在<3 m尺度内均匀分布,在>32 m尺度内聚集分布,种群内部生态关系由竞争向促进转变;消除生境异质性后,种群在>30 m尺度下呈现随机分布,种内生态关系呈现减弱的趋势。红砂种群空间分布格局的形成过程中生境异质性在大尺度上起到了重要作用。(2)随着多年平均降水量的减少,红砂种群的水分利用深度由0—20 cm加深到60—100 cm;红砂种群的密度与多年降水呈现极显著负相关(p<0.01),样地的植被盖度变化主要受草本盖度影响,红砂植被盖度变化不显著。[结论]随着多年平均降水量的减少,红砂种群的分布格局受环境异质性影响。通过增加植株密度,红砂可以利用更深层的土壤水分适应环境胁迫。