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温室中雾化微喷对叶片截留水形态及蒸发降温效应的影响

Effects of micro-spray in greenhouses on the leaf interception water types and the evaporative cooling

  • 摘要: 该研究以南方主栽番茄品种合作908为对象,在温室高温环境下设置日间整点1 min雾化微喷处理,系统监测冠层环境因子与叶片光合生理指标,解析雾化微喷调控作物健康生境的效应与机制。结果表明:环境温度是叶片截留水形态的关键调控因子,38~42 ℃时叶片形成“水滴型”截留水(leaf interception in water droplet, LI-WD),42~46 ℃时转变为“水膜型”截留水(leaf interception in water film, LI-WF),42 ℃为形态转换阈值。LI-WD呈线性蒸发特征,可使冠层气温降温效应维持25~30 min、叶片降温维持20~26 min,光系统Ⅱ实际光化学量子产量Y(Ⅱ)提升0.042~0.183,持续25 min;LI-WF呈反“S”形蒸发特征,冠层与叶片降温效应分别维持16~24 min、12~13 min,Y(Ⅱ)提升0.041~0.150,持续16 min。Y(Ⅱ)与叶温呈显著同步变化,叶温可作为雾化微喷生理效应的快速评估指标。研究明确了雾化微喷可形成两种叶片截留水形态及其对应的环境温度阈值,可为温室雾化微喷降温系统的调控及优化应用提供理论支撑。

     

    Abstract: High summer temperatures in greenhouses often induce heat stress in crops, disrupting the balance between photosynthesis and respiration. Micro-spray (MS) is an effective evaporative cooling technology, but its regulatory mechanisms on crop microenvironments and physiological responses remain unclear. This study aimed to investigate how intermittent MS affects leaf surface water interception, canopy cooling, and photosynthetic performance under high-temperature conditions. A greenhouse experiment was conducted with tomato plants (Hezuo 908) grown in a Venlo-type glasshouse in Zhenjiang, Jiangsu Province, China. MS was triggered when indoor air temperature exceeded 30 ℃ and operated for 1 minute at the beginning of each hour from 10:00 to 15:00. Canopy air temperature and humidity were continuously monitored. Leaf surface intercepted water was recorded by time-lapse imaging, while leaf temperature and the actual photochemical quantum yield of photosystem Ⅱ (Y(Ⅱ)) were measured using a chlorophyll fluorescence monitoring system. Two distinct leaf interception forms were observed after MS application: droplet-type (LI-WD) and film-type (LI-WF). LI-WD occurred at canopy temperatures of 30~42 ℃ and vapor pressure deficit (VPD) of 3.0~5.0 kPa, whereas LI-WF occurred at 42~46 ℃ and VPD of 5.0~7.5 kPa. The threshold for the transition between the two forms was approximately 42 ℃. The initial coverage of LI-WD was significantly lower than that of LI-WF (31.6% vs 99.9%). Evaporation dynamics also differed markedly: LI-WD exhibited a linear decline in coverage (R2=0.71), indicating stable evaporation, while LI-WF followed an inverse S-shaped decline (R2=0.97), indicating a rapid but short-lived evaporation process. The two interception forms produced contrasting cooling effects. Under LI-WD, canopy air temperature decreased by 1.72±0.76 ℃ and the cooling effect lasted 25.2±4.1 min; under LI-WF, the decrease was only 0.74±0.21 ℃ and lasted 12.3±2.5 min. Leaf temperature under both forms showed three successive stages (decline, stable low-temperature maintenance, and recovery), but the stable period under LI-WD was significantly longer than that under LI-WF (22.5 min vs. 11.2 min). Notably, leaf temperature responded to MS evaporative cooling earlier than canopy air temperature (by 9~20 min). Y(Ⅱ) increased synchronously with leaf cooling: under LI-WD, the mean Y(Ⅱ) increase was 0.120±0.056 and lasted about 30 min; under LI-WF, the increase was 0.080±0.048 and lasted about 18 min. In conclusion, intermittent MS can generate two distinct evaporative cooling pathways controlled by initial thermal conditions. The droplet-type pathway provides more stable evaporation, longer cooling duration, and stronger physiological protection than the film-type pathway. Leaf temperature can serve as a rapid and reliable indicator for evaluating the physiological effectiveness of greenhouse MS cooling.

     

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