短期增溫及氮沉降對青藏高原高寒草甸土壤呼吸的影響
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中圖分類號：S812.2 文獻(xiàn)標(biāo)識碼：A 文章編號：1007-0435（2025）05-1445-1：
Abstract： Global climate warming and nitrogen deposition willchange the carbon exchange between grassland ecosystem and atmosphere. However，the response of soil respiration rate and its components to warming and nitrogendeposition in alpine meadows on the Qinghai-Tibet Plateau is unclear. Therefore，this study conducted different levels of warming[ W0 （did not increase temperature）， W1 （air temperature increased by 0.47°C ，soil temperature increased by 0.61°C ）， W2 （air temperature increased by 0.92°C ，soil temperature increased by 1.09°C ）， W3 （air temperature increased by 1.44°C ，soil temperature increased by 1.95°C and nitrogen deposition ！ N16 （ ， experiments in the alpine meadow of the Qinghai-Tibet Plateau.The effects of biotic and abiotic factors on soil respiration and its components under warming and nitrogen deposition were clarified. The results showed that compared with W0 ，soil respiration and its components increased significantly under W3 treatment. Soil temperature and soil N/P ratio under shortterm warming and nitrogen deposition were the key factors affecting soil respiration and soil heterotrophic respiration.Soil autotrophic respiration is afected by soil ammonium nitrogen，soil temperature，soil nitrate nitrogen and plant Shannon-Wiener index. Combined with the above results，warming and nitrogen deposition will change soil physical and chemical properties and plant community characteristics，and then affectthe soil respiration rate and its components of alpine meadow ecosystem.
Key Words：Nitrogen deposition; Warming;Soil respiration rate;Soil heterotrophic respiration;Soil autotrophic respiration;Biological factors;Abiotic factors
土壤呼吸作為陸地生態(tài)系統(tǒng)與大氣之間最大的碳通量之一，其所釋放的二氧化碳量大約是人為化石燃料燃燒排放量的10倍，占年大氣二氧化碳年總輸人的 20%～40%（1] 。（剩余22560字）