This study analysed the temperature and humidity properties of urban soils in the territory of the Mikhailovskaya Embankment Park of Culture and Recreation in Novosibirsk, Russian Federation, in the cold period of the 2018–2019 hydrological year. Data on the temperature of the air and soil at various depths, winter and spring soil moisture and data on the dynamics of snow accumulation and snow distribution were analysed. This study found that, despite high levels of humidity in the autumn and the high snow reserves that accumulated during the winter, a decrease in soil moisture content was observed after the snow had melted. Temperatures in the range of −3 to −7 °С were recorded in the layer of soil from 0 to 30 cm below the ground surface. Systematic clearing of the pedestrian zones of the park of snow during the winter leads to both an increase in snow height and, accordingly, water reserves in the snow in adjacent areas, and to exposure of the surfaces of rabattes, or cement subterranean garden beds, in which perennial ornamental plants are grown. This study also revealed the presence of an additional cooling effect within these rabattes on the temperature regime of the soils within them during the cold period.

本研究分析了 2018-2019 水文年寒冷时期俄罗斯联邦新西伯利亚 Mikhailovskaya 路堤文化休闲公园境内城市土壤的温湿度特性。分析了不同深度的空气和土壤温度数据、冬季和春季土壤湿度数据以及积雪和雪分布的动态数据。这项研究发现，尽管秋季湿度高，冬季积雪量高，但在雪融化后观察到土壤水分含量下降。在地表以下 0 至 30 厘米的土壤层中记录了 -3 至 -7°С 范围内的温度。在冬季系统地清除雪公园的步行区会导致积雪高度增加，从而导致相邻地区积雪中的水储备增加，并导致拉巴特表面或水泥地下花园床的暴露，其中种植多年生观赏植物。这项研究还揭示了在寒冷时期，这些拉巴特土壤对土壤温度状况存在额外的冷却作用。