College of Environmental Science and Engineering, Beijing Forestry University, Beijing 100083, China.
Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, A11, Datun Road, Chaoyang District, Beijing 100101, China.
Sci Total Environ. 2023 Dec 15;904:166403. doi: 10.1016/j.scitotenv.2023.166403. Epub 2023 Aug 18.
With exogenous nitrogen (N) input into soil, phosphorus (P) could become a limiting nutrient for plant growth. Soil microbes play a crucial role in regulating soil P cycle and availability. P functional genes, further, regulate soil P availability. It is unclear how the addition of N in different chemical forms and rates influences the composition of soil microbes associated with P cycling and the abundance of P functional genes. A long-term experiment of N addition in three chemical forms with two levels in a temperate forest was performed to reveal the influences and the underlying mechanisms. We found that both chemical N forms and N rates selected for different P-solubilizing microbes. Ammonia form-N increased the abundances of P-solubilizing bacteria at low and high rates. Continuous N deposition included a significant decrease in soil pH and inhibited the viability and activity of bacterial communities in soil, especially the P-solubilizing bacteria. Thus, it restricted inorganic P mobilization and led to a decrease in soil available P. In addition, ammonium-N enhanced the relative abundance of most of the functional genes related to organic P mineralization, while nitrate-N presented a decrease trend. Ammonium-N significantly decreased most of the functional genes relevant to P transportation, whereas the other chemical N forms did not change them. Although N-addition consistently decreased the functional genes relevant to inorganic P solubilization, two of them (ppx and ppa) were the exceptions and showed an increase trend. N addition also decreased soil pH and altered soil properties, and indirectly contributed to the changes in community composition of P-solubilizing microbes and the abundances of multiple P functional genes. Our results provide a mechanistic explanation for the regulation of microbes on N-induced available P limitation via tuning the compositions of P-solubilizing microbes and the abundances of multiple P functional genes.
随着外源氮(N)输入土壤,磷(P)可能成为植物生长的限制养分。土壤微生物在调节土壤 P 循环和有效性方面起着至关重要的作用。此外,P 功能基因调节土壤 P 的有效性。目前尚不清楚不同化学形式和速率的 N 添加如何影响与 P 循环相关的土壤微生物组成和 P 功能基因的丰度。在温带森林中进行了一项 N 添加的长期实验,该实验涉及三种化学形式和两个水平,以揭示其影响和潜在机制。我们发现,两种化学 N 形式和 N 速率都选择了不同的 P 溶解微生物。氨氮形式-N 在低浓度和高浓度下增加了 P 溶解细菌的丰度。连续的 N 沉积包括土壤 pH 值的显著下降,抑制了土壤中细菌群落的活力和活性,特别是 P 溶解细菌。因此,它限制了无机 P 的动员,导致土壤有效 P 减少。此外,氨氮增强了与有机 P 矿化相关的大多数功能基因的相对丰度,而硝酸盐氮呈现下降趋势。氨氮显著降低了与 P 运输相关的大多数功能基因,而其他化学 N 形式则没有改变它们。尽管 N 添加一致降低了与无机 P 溶解相关的功能基因,但其中两个(ppx 和 ppa)是例外,呈上升趋势。N 添加还降低了土壤 pH 值并改变了土壤性质,这间接导致了 P 溶解微生物群落组成和多个 P 功能基因丰度的变化。我们的研究结果为微生物通过调节 P 溶解微生物的组成和多个 P 功能基因的丰度来调节 N 诱导的有效 P 限制提供了一种机制解释。