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[半干旱地区土壤呼吸对极端降水的响应]

[Response of Soil Respiration to Extreme Precipitation in Semi-arid Regions].

作者信息

Zhao Man, Wang Rui, Li Ru-Jian, Du Lan-Lan, Wu De-Feng, Sun Qi-Qi, Gao Xin, Guo Sheng-Li

机构信息

College of Resources and Environment, Northwest A & F University, Yangling 712100, China.

Institute of Soil and Water Conservation, Northwest A & F University, Yangling 712100, China.

出版信息

Huan Jing Ke Xue. 2016 Jul 8;37(7):2714-2720. doi: 10.13227/j.hjkx.2016.07.039.

DOI:10.13227/j.hjkx.2016.07.039
PMID:29964483
Abstract

Evaluating the response of soil microbial respiration to extreme precipitation event is significant for a better understanding about the influence of the change of precipitation regime on soil carbon cycling under global warming. A simulated experiment of extreme precipitations was conducted during the rainy season (July-September 2015) in the Changwu State Key Agro-Ecological Station, Shaanxi, China. The treatments consisted of three total precipitations in rainy season (600 mm, 300 mm, and 150 mm) and two precipitation regimes (10 mm, 150 mm; P, P). Soil microbial respiration varied differently in the same single rainfall event among three precipitations. The variation coefficient of soil microbial respiration under 600 mm total precipitation was 36% (P) and 33% (P), and 28% and 22% under 300 mm total precipitation, 43% and 29% under 150 mm total precipitation. Under 600 mm total precipitation, the cumulative soil microbial respiration under P was 20% less than that under P; however, the cumulative soil respiration of P under 150 mm total precipitation was 22% more than that under P; and there was no significant difference between P and P under 300 mm total precipitation. Therefore, the duration in soil water stress must be considered to estimate soil microbial respirations under extreme precipitations.

摘要

评估土壤微生物呼吸对极端降水事件的响应,对于更好地理解全球变暖背景下降水格局变化对土壤碳循环的影响具有重要意义。在中国陕西长武国家重点农业生态站的雨季(2015年7月至9月)进行了极端降水模拟实验。处理包括雨季的三种总降水量(600毫米、300毫米和150毫米)和两种降水格局(10毫米、150毫米;P,P)。在同一单次降雨事件中,三种降水量下土壤微生物呼吸的变化不同。总降水量600毫米时,土壤微生物呼吸的变异系数分别为36%(P)和33%(P),总降水量300毫米时为28%和22%,总降水量150毫米时为43%和29%。总降水量600毫米时,P格局下的土壤微生物累积呼吸量比P格局少20%;然而,总降水量150毫米时,P格局下的土壤累积呼吸量比P格局多22%;总降水量300毫米时,P和P之间没有显著差异。因此,在估算极端降水条件下的土壤微生物呼吸时,必须考虑土壤水分胁迫的持续时间。

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