CAS Key Laboratory of Mountain Ecological Restoration and Bioresource Utilization & Ecological Restoration and Biodiversity Conservation Key Laboratory of Sichuan Province, Chengdu Institute of Biology, Chinese Academy of Sciences, P.O. Box 416, Chengdu, 610041, People's Republic of China.
University of Chinese Academy of Sciences, No. 19A Yuquan Road, Beijing, 100049, People's Republic of China.
Microb Ecol. 2023 Jul;86(1):536-548. doi: 10.1007/s00248-022-02103-8. Epub 2022 Aug 31.
Soil microbial biomass and composition are affected by resource supply and water availability. However, the response of soil microbial communities to nitrogen fertilization under different water availability conditions is unclear. Therefore, this study conducted a 6-year pot experiment comprising five watering regimes (40%, 50%, 60%, 80%, and 100% of field capacity (FC)) and three nitrogen fertilization levels (NHNO solution; 0 [N0], 20 [N1], and 40 [N2] g N m year) to investigate soil microbial biomass, composition, and properties. The results indicated that soil microbial biomass and composition were more strongly affected by nitrogen fertilization compared with water regime. Nitrogen fertilization increased soil microbial biomass and altered soil microbial community composition, especially under low soil water availability. Soil microbial biomass was positively linearly associated with soil water regimes under N0, whereas it responded polynomially to soil water regimes under N1 and N2. The maximal soil microbial biomass was observed at FC80 for N1 and FC60 for N2. Furthermore, the biomass of soil microbial groups with high nitrogen and carbon acquisition ability as well as the enzyme activities of carbon and nitrogen cycling (β-1,4-glucosidase and β-1,4-N-acetyl-glucosaminidase, respectively) were stimulated by nitrogen fertilization. Soil microbial biomass was affected directly by nitrogen fertilization and indirectly by nitrogen and water regimes, via altering soil pH, dissolved inorganic nitrogen (NH-N and NO-N) concentration, and soil organic carbon concentration. This study provides new insights into the effect of interaction between soil nitrogen and water availabilities on soil microbial biomass, composition, and its underlying mechanism.
土壤微生物生物量和组成受资源供应和水分可用性的影响。然而,在不同水分可用性条件下,土壤微生物群落对氮施肥的响应尚不清楚。因此,本研究进行了为期 6 年的盆栽实验,包括 5 种浇水制度(田间持水量的 40%、50%、60%、80%和 100%)和 3 种氮施肥水平(NH4NO3溶液;0[N0]、20[N1]和 40[N2]g N m-2 year-1),以研究土壤微生物生物量、组成和性质。结果表明,与水分制度相比,氮施肥对土壤微生物生物量和组成的影响更大。氮施肥增加了土壤微生物生物量并改变了土壤微生物群落组成,特别是在土壤水分可用性较低的情况下。在 N0 下,土壤微生物生物量与土壤水分制度呈正线性相关,而在 N1 和 N2 下,土壤微生物生物量与土壤水分制度呈多项式相关。在 N1 下,土壤微生物生物量最大的是田间持水量 80%,在 N2 下,土壤微生物生物量最大的是田间持水量 60%。此外,具有高氮和碳获取能力的土壤微生物群的生物量以及碳和氮循环的酶活性(β-1,4-葡萄糖苷酶和β-1,4-N-乙酰-葡萄糖胺酶,分别)受到氮施肥的刺激。土壤微生物生物量受氮施肥的直接影响,通过改变土壤 pH 值、溶解无机氮(NH4+-N 和 NO3--N)浓度和土壤有机碳浓度,间接地受氮和水分制度的影响。本研究为土壤氮和水分可利用性相互作用对土壤微生物生物量、组成及其潜在机制的影响提供了新的见解。