局部高水分进口大豆发热及热量传递研究

    Study on heat and heat transfer of imported soybean with local high moisture

    • 摘要: 进口大豆因运输条件恶劣及储藏过程中的湿热传递,易造成局部水分升高进而引起局部发热,为做到发热后的及时处理,减少进口大豆在储藏过程中的经济损失,将水分含量为20%、不同质量的大豆包埋于安全水分含量的大豆中,布置9根电缆,每天记录温度变化,模拟大豆在运输及实仓储藏中局部水分偏高引起的发热现象,研究大豆的发热及热量传递。结果表明:包埋高水分的大豆,即使较少质量也会引起发热,控制高水分大豆入仓极为重要。包埋高水分大豆中层先发热,中层发热后,会迅速向上转移,造成上层温度持续升高并高于中下层,高水分大豆质量越大,上、下两层发热越快,发热点出现所用的时间越短,发热扩散的区域越广。包埋高水分大豆为120、60、30、15 kg的粮堆,分别在储存1、1、2、3 d后开始发热,高水分大豆上层(c3)分别以2.26、1.57、1.47、0.49℃/d的速度升温,达到的最高温度分别为52.1、43.2、41.4、29.1℃。研究结果可为进口大豆安全储藏提供参考。

       

      Abstract: 90% of China's soybeans are imported. Imported soybeans are transported by sea, and since the transportation season is hot and rainy, beans are stocked in a humid environment for a long time. In addition, due to the transfer of moisture and heat, moisture migration, and condensation caused by the alternation of seasons during the storage, local moisture and temperature rise. In order to deal with the heat in time and reduce the economic loss of imported soybean during storage, soybeans with 20% moisture content and different qualities were embedded in soybeans with safe water content stored in a simulated warehouse with the arrangement of 9 cables. The temperature change was recorded every day to simulate the heating phenomenon caused by high moisture content in the transportation and storage of soybean, as well as the heating and heat transfer law of soybean. With the data analysis and application of Origin, the heating trend and heating range of soybean were obtained. The results showed that:even if the mass was small, high moisture content would cause heat in the soybeans, so it is very important to control the warehousing of soybeans with high moisture content. The middle layer of high moisture soybeans was heated first, then the heat will quickly move upward, causing the temperature of the upper layer of the grain pile to continue to rise and exceed the middle and lower layer. The higher the weight of high moisture soybeans, the faster the heating of upper and lower layers, the shorter the time it takes for the hot spot to appear, and the wider the area of heating diffusion. Grain heaps with high moisture content of 120 kg, 60 kg, 30 kg and 15 kg began to heat after 1 d, 1 d, 2 d and 3 d, respectively. The upper layer of high moisture soybeans (c3) increased at the speed of 2.26℃/d, 1.57℃/d, 1.47℃/d and 0.49℃/d, respectively. The highest temperatures could reach at 52.1℃, 43.2℃, 41.4℃ and 29.1℃, respectively. After the center of the grain pile heated, the heat gradually spread to the surrounding area, and the speed of spreading to the upper layer was faster than that around the grain pile, and the affected area of the upper layer was larger than that around the wet grain. The temperature cable should be set in the warehouse. It is suggested to increase the temperature measuring points in the vertical direction. The distance between the temperature measuring points should be small, and the temperature of soybeans should be monitored in real time. In case of heating, it should be handled in time.

       

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