小麦、玉米控制灌溉技术研究

198 6～ 1998年 ,在山东省的 3个灌溉试验站 ,对冬小麦、秋玉米进行了控制灌溉试验 ,对农作物的多个生育阶段 ,按高产的要求 ,分别给予适时、适量的灌溉水 ,来控制作物不同生长期的根层土壤含水量 ,从而控制作物不同生长期根系对水分的吸收 ,培植农作物的“丰产群体结构”和与之相适应的“高产理想株型” ,适当降低无效的蒸腾量 ,使农作物能在高产的基础上再增产 .该项控制灌溉技术获得了明显的节水、增产效果 ,灌溉水的生产效率超过了 10kg/m3,产量超过了 8t/hm2 .     

CaO—SiO2-FeO—Cl体系中Zn、Pb挥发物的热力学研究

应用FaetSage热力学软件对不同温度下的FeO—CaO—SiO2-Cl体系中Zn、Ph挥发行为进行分析,采用气流携带法对FeO—CaO-SiO2-Cl体系中Zn、Pb挥发物的饱和蒸气压进行测定,并通过试验分析了温度对其体系中Zn、Pb挥发率的影响。结果表明,温度为970～1030K条件下FeO-CaO-SiO2-Cl体系中Zn、Pb主要以氯化物形式存在,氯化物的饱和蒸气压均随着温度的升高而增加,且InP～1／T呈较好的线性关系,其体系中Zn、Pb挥发率亦随着温度的升高而增加。     

FeO-CaO-SiO2-Al2O3-ZnO—PbO-Cl体系中Zn、Pb氯化物饱和蒸气压的测定

采用气流携带法对FeO-CaO-SiO2-Al2O3-ZnO-PbO-Cl体系中Zn、Pb氯化物的饱和蒸气压进行测定,并对温度、渣成分、Cl含量等影响因素进行了分析。结果表明,温度为970～1030K条件下FeO-CaO-SiO2-Al2O3-ZnO-PbO-Cl体系中Zn、Pb氯化物饱和蒸气压均随着温度的升高而增加,且P1）氯化物蒸气压值的对数与温度的倒数之间呈较好的线性关系。碱度、FeO含量均对Zn、Pb氯化物的饱和蒸气压影响很大,低碱度可提高Zn、Pb氯化物的饱和蒸气压,高FeO含量虽可增加ZnCl2饱和蒸气压,却降低了Pb氯化物的饱和蒸气压。Cl含量越高,该体系中Zn、Pb氯化物的饱和蒸气压越大。     

The hydrogen flow characteristics of the multistage hydrogen Knudsen compressor based on the thermal transpiration effect

Multistage hydrogen Knudsen compressor based on the thermal transpiration effect has very exciting prospect for the hydrogen transmission in the micro devices. Understanding of the hydrogen flow characteristic is the key issue for the designs and applications of the hydrogen energy systems. Firstly, the numerical models of the multistage hydrogen Knudsen compressor are established. The distributions of the rarefaction, velocity and temperature at different stages of the hydrogen flow are calculated and presented. Moreover, the dimensional pressure increases of the hydrogen gas flow are analyzed, and the flow behaviors in the microchannel and the connection channel are discussed. Secondly, the numerical simulation at different connection channel height is implemented, and the hydrogen gas flow characteristics in the connection are analyzed. Especially, the performances of the pressure drop in the connection channel under different channel heights are studied, and the hydrogen gas compression characteristics of different cases are compared and discussed. Also, the effect of the connection channel height on the hydrogen gas pressure increase in the microchannel is investigated. The studies presented in this paper could be greatly beneficial for the hydrogen detection and transmission.     

环境因子对土壤水分蒸散的影响

在有作物生长的条件下，土壤散失到大气中的水分主要通过土壤表面蒸发和作物叶面蒸腾两种方式进行，二者之和称为土壤水分蒸散。由于作物冠层的遮荫作用，作物覆盖下土壤水分的蒸发强度与裸土情况下显然不同。本文建立了土壤水分蒸散率的计算公式，并对几个环境因子的影响进行了讨论。计算结果表明，冠层净辐射强度和空气饱和差对蒸散率影响较大，而气温和风速的影响相对较小。当冠层净辐射强度和空气饱和差增大时，蒸散率和日蒸散总量的增加均较为明显。另外，作物的叶面积指数对蒸散也有较大的影响，同时它对蒸发和蒸腾在蒸散中所占的比重影响很大，叶面积指数增大时，叶面蒸腾所占的份额增大，而蒸发所占的份额相应地减小。     

Impact of plant shoot architecture on leaf cooling: a coupled heat and mass transfer model

Plants display a range of striking architectural adaptations when grown at elevated temperatures. In the model plant Arabidopsis thaliana, these include elongation of petioles, and increased petiole and leaf angles from the soil surface. The potential physiological significance of these architectural changes remains speculative. We address this issue computationally by formulating a mathematical model and performing numerical simulations, testing the hypothesis that elongated and elevated plant configurations may reflect a leaf-cooling strategy. This sets in place a new basic model of plant water use and interaction with the surrounding air, which couples heat and mass transfer within a plant to water vapour diffusion in the air, using a transpiration term that depends on saturation, temperature and vapour concentration. A two-dimensional, multi-petiole shoot geometry is considered, with added leaf-blade shape detail. Our simulations show that increased petiole length and angle generally result in enhanced transpiration rates and reduced leaf temperatures in well-watered conditions. Furthermore, our computations also reveal plant configurations for which elongation may result in decreased transpiration rate owing to decreased leaf liquid saturation. We offer further qualitative and quantitative insights into the role of architectural parameters as key determinants of leaf-cooling capacity.     

基于Matlab语言的温室作物蒸腾模型

为了简单方便地对作物的蒸腾量进行准确的预测,从而按照作物的最佳生长轨迹所要求的蒸腾量给定水分,对作物的生长环境进行调控,以Matlab模糊逻辑工具箱中的图形用户界面(GUI)和命令函数为工具构建了以辐照量和相对湿度为输入的温室作物的模糊蒸腾模型,得到了符合温室作物蒸腾规律的较为满意的仿真结果,证明了模型的合理正确性,并对模型的优化做了简要概述。     

基于Penman-Monteith公式的双源模型的改进

本文在Penman-Monteith公式的基础上，推导出能解析计算冠层蒸腾和土壤蒸发的双源模型，使之能广泛用于农田蒸腾和蒸发的计算.采用玉米田波文比-能量平衡(BREB)观测资料对模型进行检验，模拟的蒸散量与BREB的结果相当一致.模型 主要参数对蒸散的敏感性分析表明，这些参数变化±20%时，蒸散的响应小于±7%.     

苹果树根系吸水研究方法的讨论

介绍了根系吸水模型研究现状;对建立苹果树根系吸水模型所需要的植株蒸腾量、棵间蒸发量、根系密度、土壤含水量等的测定方法进行了探讨．分析了苹果树与作物根系吸水的不同之处．介绍了热脉冲技术测定苹果树蒸腾量、微型蒸渗仪(microlysimeter)测定棵间蒸发量、剖面法测定根系密度、TDR测土壤含水率的技术;最后,探讨了建立苹果树根系吸水模型应注意的具体问题,并进一步提出了利用空间随机场理论研究整个苹果园中苹果树的根系吸水模型的观点,即：将苹果园中的各个苹果树看作小扰动的空间随机变量,然后利用空间随机场理论研究整个苹果园中苹果树的根系吸水情况。     

Significance of Hall effect on heat and mass transport of titanium alloy-water-based nanofluid flow past a vertical surface with IMF effect

In this mathematical presentation, we examined the significance of Hall current on MHD buoyancy-driven boundary layer flow of a Ti₆Al₄V-H₂O based nanofluid past a vertical surface implanted in a uniform permeable region. The vertical surface is considered to be magnetized and induced magnetic field (IMF) impacts are also considered. The nondimensional flow model is solved with the assistance of the two-term perturbation scheme. Various results are obtained by numerical computation for different significant parameters. These results are presented and analyzed in graphical and tabular form. In the boundary layer domain, the transpiration velocity across the surface tends to diminish the main flow, IMF along the main flow, fluid temperature, and concentration. It is remarkably noted that IMF along the main flow grows for incrementing values of volume fraction coefficient of nanofluid. In the magnetic boundary layer domain, the main flow and IMF along the main flow grow with Hall current. Furthermore, it is seen that for the progressing values of magnetic Prandtl number, the main flow reduces while normal flow and IMF along the main flow is induced in the boundary layer domain.