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首页> 外文期刊>Transactions of the ASABE >PREDICTIVE MODEL OF SOIL TEMPERATURE AND MOISTURE DURING SOLARIZATION IN CLOSED GREENHOUSE
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PREDICTIVE MODEL OF SOIL TEMPERATURE AND MOISTURE DURING SOLARIZATION IN CLOSED GREENHOUSE

机译:封闭温室日粮中土壤温度和水分的预测模型

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Soil solarization is a method of non-chemical disease control that employs solar radiation to heat the soil to temperatures that are lethal for soilborne pathogens. Application of this technique in closed greenhouses has allowed it to spread in areas characterized by temperate climate, such as the Mediterranean basin. Optimization of the technique requires knowledge of the physical processes inside the soil-mulch-greenhouse system that determine the thermal regimes in the soil. In this work, a one-dimensional physical model is developed for simulation of the temperature and moisture content in mulched soil during solarization treatment in a closed greenhouse. The model also calculates the air temperature and relative humidity inside the greenhouse. The model includes heat transfer in the soil by both apparent conduction ( which incorporates transfer of latent heat by vapor movement under the influence of a temperature gradient) and enthalpy transport by liquid and vapor flow. The temperature and water content in the soil are calculated using coupled partial differential equations of heat and moisture diffusion. Furthermore, in the calculations of radiative fluxes, infinite reflections are considered. The input variables required are outside air temperature and relative humidity, outside solar radiation flux, wind velocity, soil texture and bulk density, and radiometric properties of the soil as well as of the covering and mulching films. The model is validated using data collected during a soil solarization treatment carried out in a full-scale commercial greenhouse. The results show good agreement between measured and modeled data, especially concerning soil temperature. A sensitivity analysis is also carried out in order to investigate soil temperature changes induced by variations in the radiometric properties of the films. The results show that the highest temperature changes in the soil are determined by the shortwave transmittance of the cover.
机译:土壤日晒是一种非化学疾病控制方法,该方法利用太阳辐射将土壤加热到对土壤传播的病原体具有致命作用的温度。这项技术在封闭式温室中的应用使其能够在具有温带气候特征的地区(例如地中海盆地)传播。技术的优化需要了解土壤覆盖温室系统内部的物理过程,这些过程决定了土壤的热态。在这项工作中,开发了一个一维物理模型,用于模拟封闭温室中日光处理期间覆盖土壤中的温度和水分含量。该模型还计算温室内的空气温度和相对湿度。该模型包括通过表观传导(包括在温度梯度的影响下通过蒸气运动传递潜热的传递)在土壤中的热传递,以及通过液体和蒸气流动的焓传递。土壤中的温度和水分含量是使用热和水分扩散的耦合偏微分方程计算的。此外,在辐射通量的计算中,考虑了无限反射。所需的输入变量是外界空气温度和相对湿度,外界太阳辐射通量,风速,土壤质地和堆积密度,以及土壤以及覆盖和覆盖膜的辐射特性。该模型使用在大型商业温室中进行的土壤日晒处理过程中收集的数据进行了验证。结果表明,实测数据和模型数据之间具有很好的一致性,尤其是在土壤温度方面。还进行了敏感性分析,以研究由薄膜的辐射特性引起的土壤温度变化。结果表明,土壤中最高的温度变化取决于覆盖层的短波透射率。

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