ZHANG Yong-zhi, CHEN Zhe, CHEN Ji-gui, MA Ai-hui, CHEN Yu, TANG Zun-yan, WANG Shi-xiong, GUAN Jin-hong, WANG Wen-ying, ZHOU Hua-kun, XIE Hui-chun, GUO Zhi-ying, JIN Yan-xia, YUN Shi-ming
Acta Agrestia Sinica. 2026, 34(6): 1976-1989.
To investigate whether seasonal freeze-thaw promotes the emission of nitrous oxide (N2O) and accelerates the gaseous loss of nitrogen in the talus plateau vegetation ecosystem, this study focused on the grassland (Thylacospermum caespitosum) pad vegetation at an altitude of 4000-4400 m on the Gangshigacha snow peak in the eastern part of the Qilian Mountains. The soil (0-30 cm) temperature, humidity, nutrient dynamic characteristics, and N2O flux were monitored continuously for two years. The results showed that the soil experienced approximately 70 daily freeze-thaw cycles throughout the year, divided into four periods: unstable thawing period (25 times), stable thawing period, unstable freezing period (45 times), and stable freezing period. For every 100-meter increase in altitude, the average start and end time of soil freeze-thaw was delayed or advanced by 3.88 days. The N2O emission was the most significant during the unstable thawing period (accounting for only 5.5%-6.8% of the entire year), with a cumulative emission (225.97 g·hm-2) accounting for 35.88% of the annual total, a maximum emission rate of 24.52 μg·m-2·h-1, an average flux of 13.63 μg·m-2·h-1, which was 1.39 times the annual average, and the cumulative emission during the non-growing seasons (excluding the stable thawing period) accounted for as high as 74.09%. The emission was dominated by soil water and heat, pH, and substrate scarcity, leading to low production. Under climate warming, the freeze-thaw driven nitrogen gas loss of N2O in the ice margin zone intensified, and further research on the water and heat conditions and nitrogen transformation mechanism is needed.