Du Yangong, Shu Kai, Guo Xiaowei, Pengjin Zhu
Qinghai Provincial Key Laboratory of Restoration Ecology for Cold Region, Northwest Institute of Plateau Biology, Chinese Academy of Sciences, Xining, China.
University of Chinese Academy of Science, Beijing, China.
Curr Microbiol. 2019 May;76(5):620-625. doi: 10.1007/s00284-019-01668-x. Epub 2019 Mar 11.
Grasslands are suffering from long-term overgrazing because of the population inflation. Furthermore, nitrous oxide (NO) is a major greenhouse gas that also depletes stratospheric ozone. However, the emission rate of grassland NO and underlying mechanisms remained unclear under different grazing intensities. We conducted a field manipulation under four grazing intensities to compare its NO fluxes and main affected factors. It was indicated that alpine meadow NO emission rates increased from 39.7 ± 3.1 to 47.8 ± 2.3 μg m h (p < 0.05), then decreased to 43.4 ± 4.1 and 32.9 ± 1.4 μg m h with grazing intensity increasing from 4 to 8, 12 and 16 sheep ha-1, respectively. Multiple-stepwise regression analysis indicated that the predominant affected soil factors were separately TN and BD, pH and BD, also pH and BD, SOC and BD. Simple linear regression models revealed that ammonia-oxidizing archaea (AOA) contributed much to NO emission (R = 0.77). Additionally, the R coefficient of linear regression was 0.87 between nosZ genes and NO emission rates in alpine meadow. Much attention should be paid to protecting alpine meadow from degradation to mitigate NO emission source on the Tibetan Plateau.
由于人口增长,草原正遭受长期过度放牧的影响。此外,一氧化二氮(NO)是一种主要的温室气体,它还会消耗平流层臭氧。然而,在不同放牧强度下,草原NO的排放速率及其潜在机制仍不清楚。我们在四种放牧强度下进行了田间操作,以比较其NO通量和主要影响因素。结果表明,随着放牧强度从4只羊/公顷增加到8只羊/公顷、12只羊/公顷和16只羊/公顷,高寒草甸NO排放速率从39.7±3.1增加到47.8±2.3μg m-2 h-1(p<0.05),然后分别降至43.4±4.1和32.9±1.4μg m-2 h-1。多元逐步回归分析表明,主要影响土壤的因素分别是总氮(TN)和容重(BD)、pH值和BD、pH值和BD、土壤有机碳(SOC)和BD。简单线性回归模型显示,氨氧化古菌(AOA)对NO排放贡献很大(R=0.77)。此外,高寒草甸中nosZ基因与NO排放速率之间的线性回归R系数为0.87。应高度重视保护高寒草甸,防止其退化,以减少青藏高原上的NO排放源。