冻融期不同覆盖和气象因子对土壤导热率和热通量的影响

Influence of different coverage and meteorological factors on soil thermal conductivity and heat flux during freezing and thawing period

为了研究冻融期不同覆盖和气象因子对土壤导热率和土壤热通量的影响,在2015年11月-2016年4月期间,设置了裸地(BL)、自然积雪覆盖(SC)、6 000 kg/hm^2秸秆+积雪覆盖(SM1)、12 000 kg/hm^2秸秆+积雪覆盖(SM2)和18 000 kg/hm^2秸秆+积雪覆盖(SM3)5种不同的处理,测定了20、40、60和100 cm土壤含水率和温度,并计算出土壤导热率和土壤热通量。研究结果发现:在土壤冻结期,土壤导热率随着土壤的冻结而增大,直至完全冻结后基本保持不变,而在土壤融化期则逐渐减小。冻融阶段,积雪和秸秆覆盖会延缓土壤导热率的变化,减小土壤导热率的变化。冻结期,裸地处理的土壤导热率最大,平均为1.55 W/(m×K);融化期,裸地处理的土壤导热率最小,平均为0.79 W/(m×K)。在冻结期,土壤热量向上传递,传递量先增加后减小;在融化期,土壤热量向下传递,传递量逐渐增加。积雪和秸秆覆盖可以减小土壤热通量及其变化。积雪和秸秆覆盖条件下的土壤热通量比裸地少4.73~8.84 W/m^2。裸地处理的土壤导热率与水汽压的相关性最好,相关系数为-0.84,与风速的相关性最差,相关系数为-0.43。积雪和秸秆覆盖条件下的土壤导热率与环境温度的相关性最好,相关系数为-0.67^-0.73,与风速的相关性最差,相关系数为-0.18^-0.25。土壤热通量与太阳辐射的相关性最好,相关系数为-0.88^-0.91,与风速的相关性最差,相关系数为-0.44^-0.53。整体而言,积雪和秸秆覆盖会减小大气环境对土壤导热率和热通量的影响。

In order to study the characteristics of soil thermal conductivity and heat flux under different mulching conditions in freezing and thawing period, we measured the soil temperature with 5 different treatments, i.e. bare land(BL), snow cover(SC), 6 000 kg/hm2 straw mulching + snow cover(SM1), 12 000 kg/hm2 straw mulching + snow cover(SM2), and 18000 kg/hm2 straw mulching + snow cover(SM3), and then calculated the soil thermal conductivity and heat flux. Results showed that the soil thermal conductivity increased when soil was freezing, maintained constant when soil was frozen completely, and decreased when soil was thawing. In the freezing period, straw mulching and snow cover could delay the increase of soil thermal conductivity. In the thawing period, straw mulching and snow cover could delay the decrease of soil thermal conductivity. The rising time of soil thermal conductivity of BL was 7 d earlier than the other 4 treatments in 20 cm soil layer. During the freezing period, the average soil thermal conductivity of BL was the largest, while during the thawing period the average soil thermal conductivity of BL was the lowest. The soil thermal conductivity of BL was 1.55 W/(m?K) in 20 cm soil layer during the freezing period, which was 12%, 26%, 41% and 49% higher than those of SC, SM1, SM2 and SM3, respectively. The thermal conductivity of BL in 20 cm soil layer was 0.78 W/(m?K) in the thawing period, which was 29%, 25%, 22% and 15% smaller than those of SC, SM1, SM2 and SM3, respectively. Straw mulching and snow cover could reduce the range of soil thermal conductivity and the active layer depth of soil thermal conductivity. Soil thermal conductivity had the best correlation with aqueous vapour pressure in BL, and the correlation coefficient was-0.84(P<0.01). Soil thermal conductivity had the worst correlation with wind speed in BL, and the correlation coefficient was-0.43(P<0.05). Soil thermal conductivity had the best correlation with ambient temperature under straw mulching and snow cover, and had the worst correlation with wind speed. Straw mulching and snow cover could reduce the influence of atmospheric environment on soil thermal conductivity. When the environment temperature was higher than-3 ℃, the soil thermal conductivity maintained a lower value and remained unchanged. When the environment temperature was lower than-3 ℃, the soil thermal conductivity maintained a higher value and remained unchanged. During the freezing period, the soil heat transfer upward and the soil heat flux increased first and then decreased; during the thawing period, the soil heat transfer downward and the soil heat flux increased gradually. Straw mulching and snow cover reduced the soil heat flux and its variation. In the whole freezing and thawing period, the average value of soil heat flux of BL was the largest and the soil heat flux of SM3 was the least in the same soil layer. Straw mulching and snow cover could reduce the active layer depth of soil heat flux. The heat flux of surface soil was significantly higher than that of deep soil. Soil heat flux had the best correlation with solar radiation, and all the correlation coefficients were above 0.85 in the 5 treatments. Soil heat flux had the worst correlation with wind speed, and all the correlation coefficients were below 0.55. Straw mulching and snow cover could reduce the influence of atmospheric environment on soil heat flux. The correlation coefficient between solar radiation and soil heat flux of BL was-0.91(P<0.01), while the correlation coefficient of SM3 was only-0.88(P<0.01). The results can provide scientific references for regulation of soil temperature in winter and prediction of soil temperature in spring.