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上海理工大学能源与动力工程学院 上海 200093
赵巍,女,博士,讲师,上海理工大学能源与动力工程学院,021-55272320,E-mail:zw_cherry@163.com。研究方向:人工造雪技术,自动复叠制冷技术。
收稿日期:2023-12-20,
修回日期:2024-01-22,
录用日期:2024-04-02,
纸质出版日期:2025-06-16
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赵巍, 韩雅倩, 张华, 等. 内混式核子器临界成雪高度的测量分析[J]. 制冷学报, 2025,46(3):91-97.
Zhao Wei, Han Yaqian, Zhang Hua, et al. Measurement and Analysis of the Critical Snow Formation Height of an Internally Mixed Nucleonator[J]. Journal of refrigeration, 2025, 46(3): 91-97.
赵巍, 韩雅倩, 张华, 等. 内混式核子器临界成雪高度的测量分析[J]. 制冷学报, 2025,46(3):91-97. DOI: 10.12465/j.issn.0253-4339.2025.03.091.
Zhao Wei, Han Yaqian, Zhang Hua, et al. Measurement and Analysis of the Critical Snow Formation Height of an Internally Mixed Nucleonator[J]. Journal of refrigeration, 2025, 46(3): 91-97. DOI: 10.12465/j.issn.0253-4339.2025.03.091.
为研究人工造雪机内混式单孔核子器的临界成雪高度,实验测量了在不同气水压力比及环境温度下的临界成雪高度阈值,分析了气水压力比及环境温度对临界成雪高度阈值的影响。结果表明:在气水压力比为0.40 MPa∶0.40 MPa的工况下,当环境温度为-5 ℃和-10 ℃时,临界成雪高度阈值不存在,但环境温度为-15 ℃时,可以实现成雪,临界成雪高度阈值为50~55 cm。当气水压力比为0.50 MPa∶0.45 MPa和0.50 MPa∶0.40 MPa时,-5、-10、-15 ℃环境温度条件下均能成雪,且气水压力比及环境温度对临界成雪高度具有一定的影响。在相同环境温度下,气水压力比越大,临界成雪高度越小;在保持气水压力比不变的情况下,随着环境温度从-5 ℃降至-15 ℃,临界成雪高度则随之减小,且在-10~-5 ℃温度区间变化趋势较为显著。
In this study
the critical snow formation height of a mixed single-aperture nucleator in an artificial snow machine was examined. The threshold values of critical snow formation height were experimentally measured at different air-water pressure ratios and ambient temperatures
and the effects of air-water pressure ratios and ambient temperatures on the threshold values of critical snow formation heights were analyzed. The results showed that the threshold value for the critical height of critical snow formation did not exist at temperatures of -5 ℃ and -10 ℃ under the working conditions with a gas-water pressure ratio of 0.40 MPa∶0.40 MPa
but snow formation could be realized at -15 ℃
and the threshold value for the critical height of critical snow formation was 50-55 cm. When the gas-water pressure ratio is 0.50 MPa∶0.45 MPa or 0.50 MPa∶0.40 MPa
snow can be formed at ambient temperatures of -5 ℃
-10 ℃
and -15 ℃. The gas-water pressure ratio and ambient temperatures have a certain influence on the height of critical snow formation. Under the same ambient temperature
the greater the gas-water pressure ratio
the lower the critical snow height. Provided that the gas-water pressure ratio remains constant
the critical snow height decreases when the ambient temperature lowers from -5 ℃ to -15 ℃
and the trend of the change is more obvious in the temperature interval from -5 ℃ to -10 ℃.
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