Xiao Yi, Li Zheng, Huang Rong, Tang Ao-Han, Li Bing, Wang Chang-Quan
College of Resources, Sichuan Agricultural University, Chengdu 611130, China.
Chongqing Key Laboratory of Soil Multi-Scale Interfacial Process, Chongqing 400715, China.
Huan Jing Ke Xue. 2022 Jul 8;43(7):3884-3894. doi: 10.13227/j.hjkx.202108247.
A long-term fertilization experiment with a system of rice-wheat rotation was conducted in Chengdu Plain. Three fertilization treatments including conventional fertilization (T1), pig manure substituting for 50% nitrogen fertilizer (T2), and T2 plus straw (T3) were set up to study the characteristics of microbial carbon source utilization of soil and dissolved organic matter (DOM). The results showed that T3 improved the soil microbial carbon source metabolism in comparison with those of the T1 and T2 treatments; the average color change rate (AWCD) increased by 16% and 48%, respectively. Meanwhile, T3 improved the soil DOM microbial carbon source metabolism, and the AWCD value was 0.43. The highest Shannon, Simpson, and McIntosh indexes of soil and DOM were all found in the T3 treatment, and the Shannon, Simpson, and McIntosh indexes of DOM were 2.73, 0.91, and 3.75, respectively. The results of principal component analysis and enrichment analysis showed that the main carbon sources used by microorganisms of soil and DOM were different under different fertilization treatments. For DOM, the main carbon source used by microorganisms in the T1 and T2 treatments was sugar, whereas T3 increased the utilization of amino acids, carboxylic acids, polymers, and amines. The changes in soil pH and texture were the main factors that caused the difference in soil DOM microbial carbon source metabolism. In conclusion, the application of organic fertilizer (pig manure plus straw) significantly increased the microbial community diversity and carbon source metabolic capacity of soil and DOM and promoted the diversification of microbial carbon source preference.
在成都平原开展了一项稻麦轮作系统的长期施肥试验。设置了三种施肥处理,包括常规施肥(T1)、猪粪替代50%氮肥(T2)以及T2加秸秆(T3),以研究土壤和溶解有机物(DOM)的微生物碳源利用特征。结果表明,与T1和T2处理相比,T3改善了土壤微生物碳源代谢;平均颜色变化率(AWCD)分别提高了16%和48%。同时,T3改善了土壤DOM微生物碳源代谢,AWCD值为0.43。土壤和DOM的香农、辛普森和麦金托什指数在T3处理中均最高,DOM的香农、辛普森和麦金托什指数分别为2.73、0.91和3.75。主成分分析和富集分析结果表明,不同施肥处理下土壤和DOM微生物利用的主要碳源不同。对于DOM,T1和T2处理中微生物利用的主要碳源是糖类,而T3增加了对氨基酸、羧酸、聚合物和胺类的利用。土壤pH值和质地的变化是导致土壤DOM微生物碳源代谢差异的主要因素。总之,有机肥(猪粪加秸秆)的施用显著增加了土壤和DOM的微生物群落多样性和碳源代谢能力,促进了微生物碳源偏好的多样化。