中国农业气象 ›› 2022, Vol. 43 ›› Issue (03): 177-193.doi: 10.3969/j.issn.1000-6362.2022.03.002

• 农业生态环境栏目 • 上一篇    下一篇

基于热平衡及热湿参数动态分析红梅杏防霜棚“冷室效应”

姜瑞洋,张维江,马轶,马芳,冯娜,李伟建,姜昌   

  1. 1. 宁夏大学土木与水利工程学院,银川 750021;2. 宁夏红梅杏科技发展有限公司,固原 756000
  • 收稿日期:2021-04-22 出版日期:2022-03-20 发布日期:2022-03-21
  • 通讯作者: 张维江,教授,博士生导师,研究方向为干旱地区水资源调控及水土保持。 E-mail:zwjiang @263.net
  • 作者简介:姜瑞洋,E-mail:469560272@qq.com
  • 基金资助:
    宁夏回族自治区重点研发计划重大(重点)项目“宁南山区生态恢复与水资源潜力开发研究与示范”(2018ZDKJ0040)

Study on “Cold Chamber Effect” of Red Plum Apricot Frost Proof Shed Based on Dynamic Analysis of Heat Balance and Heat and Moisture Parameters

JIANG Rui-yang,ZHANG Wei-jiang,MA Yi,MA Fang,FENG Na,LI Wei-jian,JIANG Chang   

  1. 1. School of civil and hydraulic engineering, Ningxia University, Yinchuan 750021, China;2. Ningxia Hongmei Apricot Technology Development Co. Ltd., Guyuan 756000
  • Received:2021-04-22 Online:2022-03-20 Published:2022-03-21

摘要: 针对宁南地区红梅杏防霜棚夜间棚内环境温度长期低于棚外,即出现了“冷室效应”,未达到预防霜冻效果,依据质、热平衡原理分别研究防霜棚覆盖层、棚内湿空气和土壤层的热量收支情况,以及防霜棚系统在棚布覆盖-次日收拢时段棚内热量蓄积情况;分析棚内主要热湿参数的动态过程,以此探究防霜棚内相对湿度及湿空气状态变化对相变潜热的影响和棚内“冷室效应”的产生机理,为改进设计提供理论依据,以达到有效预防霜冻灾害的目的。结果表明:(1)春、秋季夜间棚内出现“冷室效应”时土壤层和覆盖层均因热损失较高成为失热部分,而棚内湿空气因得到热量较多成为得热部分。(2)春、秋季棚布覆盖-次日收拢时段棚内累计得热量低于累计失热量,导致棚内热量失衡。(3)棚内湿空气热湿参数与棚外热湿参数存在显著差异(春季棚内的饱和水汽压除外);夜间棚内水汽密度与露点温度的动态变化过程均可反映因蒸发及冷凝而产生的潜热变化规律;棚内低温和较高的水汽密度使饱和水汽压与实际水汽压无限接近,导致棚内相对湿度持续偏高。红梅杏防霜棚夜间累计得热量始终小于累计失热量,土壤层和覆盖层为最主要的热损失部分,在热量失衡的情况下出现了“冷室效应”。

关键词: 红梅杏, 冷室效应, 热平衡, 水汽密度, 露点温度, 水汽压

Abstract: A frost-proof shed was designed to prevent perennial frost disaster suffered by red plum apricots in the southern area of Ningxia. During the tests at night, the ambient temperature in the shed was always lower than that outside the shed, resulting in a "cold chamber effect”, and the desired effect was not achieved. Therefore, there was a test that needed to probe into the mechanism of the “cold chamber effect” in the frost-proof shed to provide a theoretical basis for improving the design of the frost-proof shed accurately and prevent frost disaster effectively. According to the principle of mass and heat balance, the test was researched the heat budget of the cover layer, the moist air in the shed, and the soil layer respectively then studied the heat accumulation in the whole system of the frost-proof shed during the period after the covering of the shed cloth to the time before its folding on the next day. Finally, the test explored the influence of relative humidity and the changes of moist air on phase transition latent heat by analyzing the dynamic process of main heat and humidity parameters in the shed. The study results show that: (1) when the “cold chamber effect” occurs at night in spring and autumn, both the soil layer and the cover layer become the part losing heat due to more heat loss, while the moist air in the shed becomes the part gaining heat due to more heat gain. (2) In spring and autumn, the accumulated heat gain is lower than the accumulated heat loss in the shed during the period after the covering of the shed cloth to the time before its folding on the next day, resulting in the heat imbalance in the shed. (3) There is a significant difference in the heat and humidity parameters of the moist air in the shed and those outside the shed (except the saturated water vapor pressure in the shed in spring); The dynamic changes of the water vapor density and the dew point temperature in the shed at night can reflect the change rules of latent heat caused by evaporation and condensation; The low temperature and higher water vapor density in the shed make the saturated water vapor pressure infinitely close to the actual water vapor pressure, resulting in the relative humidity in the shed persistently on the high side. The accumulated heat gain of the frost-proof shed for red plum apricots is always less than the accumulated heat loss at night, and the soil layer and the cover layer are the most important parts losing heat, and thus the “cold chamber effect” appears in the case of heat imbalance.

Key words: Red plum apricots, Cold chamber effect, Heat balance, Water vapor density, Dew point temperature, Water vapor pressure