Institute of Biochemistry, College of Life Sciences, Zhejiang University, Hangzhou, 310058, China.
College of Animal Sciences, Zhejiang University, Hangzhou, Zhejiang Province, 310058, China.
Environ Pollut. 2019 Jun;249:686-695. doi: 10.1016/j.envpol.2019.03.091. Epub 2019 Mar 24.
Although fertilization plays an important role in determining the contents of soil dissolved organic matters or water-extractable organic matter (DOM, WEOM), knowledge regarding the dynamics, biodegradability, and microbial community shifts of WEOM in response to different fertilization treatments is very limited, particularly in rice-wheat cropping soil. Thus, in the present study, we performed biodegradation experiments using WEOM extracted from samples of soil that had been subjected to four different fertilization treatments: unfertilized control (CK), chemical fertilizer (CF), 50% chemical fertilizer plus pig manure (PMCF), and 100% chemical fertilizer plus rice straw (SRCF). UV spectrum and fluorescence 3D excitation-emission matrix analyses applied to investigate the chemical composition of WEOM revealed that all examined WEOMs were derived from microbial activity and the dominant portion comprised humic acid-like compounds. After the incubation, 31.17, 31.63, 43.47, and 33.01% of soil WEOM from CK, CF, PMCF, and SRCF treatments, respectively, were biodegraded. PMCF- derived WEOM had the highest biodegradation rate. High-throughput sequencing analyses performed to determine the microbial community before and after the incubation indicated that Sphingomonas, Bacillus, and Flavisolibacter were the predominant bacterial genera in the original inoculum derived from the four fertilization treatments. Following biodegradation, we observed that the dominant bacteria differed according to fertilization treatments: Curvibacter (43.25%) and Sphingobium (10.47%) for CK, Curvibacter (29.68%) and Caulobacter (20.00%) for CF, Azospirillum (23.68%) and Caulobacter (13.29%) for PMCF, and Ralstonia (51.75%) for SRCF. Canonical correspondence analysis revealed that, shifts in the microbial community were closely correlated with pH and specific UV absorbance at 254 nm. We speculated that the inherent traits of different WEOM and the properties of soil solutions under different fertilization treatments shaped the soil microbial community structure, thereby influencing the biodegradation of WEOM.
尽管受精在决定土壤溶解有机物质或水可提取有机物质(DOM、WEOM)的含量方面起着重要作用,但关于 WEOM 对不同施肥处理的动态、生物降解性和微生物群落变化的知识非常有限,特别是在水稻-小麦轮作土壤中。因此,本研究采用从经过四种不同施肥处理(未施肥对照(CK)、化肥(CF)、化肥+猪粪(PMCF)和化肥+稻草(SRCF)的土壤样品中提取的 WEOM 进行生物降解实验。应用紫外光谱和荧光三维激发-发射矩阵分析来研究 WEOM 的化学成分,结果表明所有检查的 WEOM 均源自微生物活性,主要部分由腐殖酸样化合物组成。培养后,CK、CF、PMCF 和 SRCF 处理的土壤 WEOM 分别有 31.17%、31.63%、43.47%和 33.01%被生物降解。PMCF 衍生的 WEOM 具有最高的生物降解率。培养前后进行高通量测序分析以确定微生物群落,结果表明,在来自四种施肥处理的原始接种物中,Sphingomonas、Bacillus 和 Flavisolibacter 是主要的细菌属。生物降解后,我们观察到不同施肥处理下优势细菌不同:CK 为 Curvibacter(43.25%)和 Sphingobium(10.47%),CF 为 Curvibacter(29.68%)和 Caulobacter(20.00%),PMCF 为 Azospirillum(23.68%)和 Caulobacter(13.29%),SRCF 为 Ralstonia(51.75%)。典范对应分析表明,微生物群落的变化与 pH 和 254nm 处的特定紫外吸光度密切相关。我们推测,不同 WEOM 的固有特性和不同施肥处理下土壤溶液的性质塑造了土壤微生物群落结构,从而影响 WEOM 的生物降解。