Co-Innovation Center for Sustainable Forestry in Southern China, Jiangsu Province Key Laboratory of Soil and Water Conservation and Ecological Restoration, Nanjing Forestry University, 159 Longpan Road, Nanjing, Jiangsu 210037, China; Department of Biology, University of Miami, Coral Gables, FL 33124, USA.
Department of Biology, University of Miami, Coral Gables, FL 33124, USA.
Sci Total Environ. 2017 Dec 1;601-602:669-678. doi: 10.1016/j.scitotenv.2017.05.151. Epub 2017 May 31.
Acid rain is mainly caused by dissolution of sulfur dioxide and nitrogen oxides in the atmosphere, and has a significant negative effect on ecosystems. The relative composition of acid rain is changing gradually from sulfuric acid rain (SAR) to nitric acid rain (NAR) with the rapidly growing amount of nitrogen deposition. In this study, we investigated the impact of simulated SAR and NAR on litter decomposition and the soil microbial community over four seasons since March 2015. Results first showed that the effects of acid rain on litter decomposition and soil microbial were positive in the early period of the experiment, except for SAR on soil microbes. Second, soil pH with NAR decreased more rapidly with the amount of acid rain increased in summer than with SAR treatments. Only strongly acid rain (both SAR and NAR) was capable of depressing litter decomposition and its inhibitory effect was stronger on leaf than on fine root litter. Meanwhile, NAR had a higher inhibitory effect on litter decomposition than SAR. Third, in summer, autumn and winter, PLFAs were negatively impacted by the increased acidity level resulting from both SAR and NAR. However, higher acidity level of NAR (pH=2.5) had the strongest inhibitory impact on soil microbial activity, especially in summer. In addition, Gram-negative bacteria (cy19:0) and fungi (18:1ω9) were more sensitive to both SAR and NAR, and actinomycetes was more sensitive to SAR intensity. Finally, soil total carbon, total nitrogen and pH were the most important soil property factors affecting soil microbial activity, and high microbial indices (fungi/bacteria) with high soil pH. Our results suggest that the ratio of SO to NO in acid rain is an important factor which could affect litter decomposition and soil microbial in subtropical forest of China.
酸雨主要是由大气中二氧化硫和氮氧化物的溶解引起的,对生态系统有显著的负面影响。随着氮沉降量的迅速增加,酸雨的相对成分正逐渐由硫酸型(SAR)向硝酸型(NAR)转变。本研究于 2015 年 3 月以来,通过模拟 SAR 和 NAR 处理,在四个季节中研究了它们对凋落物分解和土壤微生物群落的影响。结果表明:在实验的早期阶段,除了对土壤微生物外,酸雨对凋落物分解和土壤微生物的影响是正向的。其次,在夏季,与 SAR 处理相比,NAR 处理下土壤 pH 值随酸雨量的增加而下降更快。只有强酸雨(SAR 和 NAR)能够抑制凋落物分解,其对叶片凋落物的抑制作用强于细根凋落物。同时,NAR 对凋落物分解的抑制作用强于 SAR。第三,在夏季、秋季和冬季,无论是 SAR 还是 NAR,土壤微生物生物量随着酸度的增加而受到负面影响。然而,较高酸度的 NAR(pH=2.5)对土壤微生物活性的抑制作用最强,尤其是在夏季。此外,革兰氏阴性菌(cy19:0)和真菌(18:1ω9)对 SAR 和 NAR 更敏感,放线菌对 SAR 强度更敏感。最后,土壤总碳、总氮和 pH 值是影响土壤微生物活性的最重要土壤性质因素,高土壤 pH 值与高微生物指数(真菌/细菌)相关。我们的结果表明,酸雨的 SO 与 NO 的比例是影响中国亚热带森林凋落物分解和土壤微生物的一个重要因素。