为改善日光温室内作物生长的热环境,该文研制了一种适用于日光温室的石膏基石蜡/膨胀珍珠岩复合相变储能保温砂浆,其相变温度为25.6℃,相变潜热为89.8 k J/kg。并将50 mm的复合相变保温砂浆用于砖墙日光温室的后墙作为试验温室,与无相...为改善日光温室内作物生长的热环境,该文研制了一种适用于日光温室的石膏基石蜡/膨胀珍珠岩复合相变储能保温砂浆,其相变温度为25.6℃,相变潜热为89.8 k J/kg。并将50 mm的复合相变保温砂浆用于砖墙日光温室的后墙作为试验温室,与无相变材料的原砖墙温室(即对照温室)进行对比试验。在试验周期内,试验温室的室内日最低温度比对照温室平均高出1.5℃,最高可达2.4℃;其中,阴天试验温室的室内温度比对照温室平均高1.6℃;晴天试验温室的室内最高温度比对照温室低1.7℃,室内最大温差比对照温室低3.1℃,夜间(17:00-次日8:00)试验温室室温比对照温室平均高2.7℃;多云期间,试验温室的室内最高温比对照温室低1.4℃,最大温差比对照温室低3.5℃,夜间试验温室室温比对照温室平均高2.3℃;在相同栽培管理条件下,生长旺盛期和坐果期,试验温室的黄瓜植株高度比对照温室分别平均高出17.1和24.6 cm,试验温室内黄瓜的单果质量和单株结果数分别为对照温室的1.4倍和1.3倍,单株产量为对照温室的1.8倍。试验结果表明,复合相变储能保温砂浆具有良好的保温和蓄、放热效果,对日光温室内的热环境具有明显的改善效果,使其更适于黄瓜的生长。展开更多
CH4 and N2O fluxes from soil under a tropical seasonal rain forest in Xishuangbanna, Southwest China were measured for one year using closed static chamber technique and gas chromatography method. Three treatments wer...CH4 and N2O fluxes from soil under a tropical seasonal rain forest in Xishuangbanna, Southwest China were measured for one year using closed static chamber technique and gas chromatography method. Three treatments were set in the studied field： （A） litter-free, （B） with litter, and （C） with litter and seedling. The results showed that the soil in our study was a sink of atmospheric CH4 and source of atmospheric N2O. The observed mean CH4 fluxes from treatments A, B, and C were -50.0 ± 4.0, -35.9 ± 2.8, -31.6 ± 2.8 μgC/（m^2·h）, respectively, and calculated annual fluxes in 2003 were -4.1, -3.1, and -2.9 kgC/hm^2, respectively. The observed mean N2O fluxes from treatments A, B, and C were 30.9 ± 3.1, 28.2 ± 3.5, 50.2±3.7 μgN/（m^2·h）, respectively, and calculated annual fluxes in 2003 were 2.8, 2.6, and 3.7 kgN/hm^2, respectively. Seasonal variations in CH4 and N2O fluxes were significant among all the three treatments. The presence of litter decreased CH4 uptake during wet season （P 〈 0.05）, but not during dry season. There was a similar increase in seedlings-mediated N2O emissions during wet and dry seasons, indicating that seedlings increased N2O emission in both seasons. A strong positive relationship existed between CH4 fluxes and soil moisture for all the three treatments, and weak relationship between CH4 fluxes and soil temperature for treatment B and treatment C. The N2O fluxes correlated with soil temperature for all the three treatments.展开更多
文摘为改善日光温室内作物生长的热环境,该文研制了一种适用于日光温室的石膏基石蜡/膨胀珍珠岩复合相变储能保温砂浆,其相变温度为25.6℃,相变潜热为89.8 k J/kg。并将50 mm的复合相变保温砂浆用于砖墙日光温室的后墙作为试验温室,与无相变材料的原砖墙温室(即对照温室)进行对比试验。在试验周期内,试验温室的室内日最低温度比对照温室平均高出1.5℃,最高可达2.4℃;其中,阴天试验温室的室内温度比对照温室平均高1.6℃;晴天试验温室的室内最高温度比对照温室低1.7℃,室内最大温差比对照温室低3.1℃,夜间(17:00-次日8:00)试验温室室温比对照温室平均高2.7℃;多云期间,试验温室的室内最高温比对照温室低1.4℃,最大温差比对照温室低3.5℃,夜间试验温室室温比对照温室平均高2.3℃;在相同栽培管理条件下,生长旺盛期和坐果期,试验温室的黄瓜植株高度比对照温室分别平均高出17.1和24.6 cm,试验温室内黄瓜的单果质量和单株结果数分别为对照温室的1.4倍和1.3倍,单株产量为对照温室的1.8倍。试验结果表明,复合相变储能保温砂浆具有良好的保温和蓄、放热效果,对日光温室内的热环境具有明显的改善效果,使其更适于黄瓜的生长。
文摘CH4 and N2O fluxes from soil under a tropical seasonal rain forest in Xishuangbanna, Southwest China were measured for one year using closed static chamber technique and gas chromatography method. Three treatments were set in the studied field： （A） litter-free, （B） with litter, and （C） with litter and seedling. The results showed that the soil in our study was a sink of atmospheric CH4 and source of atmospheric N2O. The observed mean CH4 fluxes from treatments A, B, and C were -50.0 ± 4.0, -35.9 ± 2.8, -31.6 ± 2.8 μgC/（m^2·h）, respectively, and calculated annual fluxes in 2003 were -4.1, -3.1, and -2.9 kgC/hm^2, respectively. The observed mean N2O fluxes from treatments A, B, and C were 30.9 ± 3.1, 28.2 ± 3.5, 50.2±3.7 μgN/（m^2·h）, respectively, and calculated annual fluxes in 2003 were 2.8, 2.6, and 3.7 kgN/hm^2, respectively. Seasonal variations in CH4 and N2O fluxes were significant among all the three treatments. The presence of litter decreased CH4 uptake during wet season （P 〈 0.05）, but not during dry season. There was a similar increase in seedlings-mediated N2O emissions during wet and dry seasons, indicating that seedlings increased N2O emission in both seasons. A strong positive relationship existed between CH4 fluxes and soil moisture for all the three treatments, and weak relationship between CH4 fluxes and soil temperature for treatment B and treatment C. The N2O fluxes correlated with soil temperature for all the three treatments.
