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[长期施肥对中国浙江省水稻土不同粒径颗粒有机碳稳定性的影响]

[Effect of Long-term Fertilizer Application on the Stability of Organic Carbon in Particle Size Fractions of a Paddy Soil in Zhejiang Province, China].

作者信息

Mao Xia-li, Lu Kou-ping, Sun Tao, Zhang Xiao-kai, He Li-zhi, Wang Hai-long

出版信息

Huan Jing Ke Xue. 2015 May;36(5):1827-35.

PMID:26314136
Abstract

Effects of chemical fertilizers and organic manure on the soil organic carbon (SOC) content in particle size fractions of paddy soil were investigated in a 17-year long-term fertilization field experiment in Zhejiang Province, China. The inherent chemical composition of silt- and clay-associated SOC was evaluated with solid-state 13C-NMR spectroscopy. Compared to CK (no fertilizer treatment), NPKRS (NPK fertilizers plus rice straw) , NPKOM (NPK fertilizers plus organic manure) , NPK (NPK fertilizers) and OM (organic manure alone) treatments significantly (P <0. 05) increased the SOC content of sand- (2-0.02 mm), silt- (0.02-0.002 mm) and clay-sized (< 0.002 mm) fractions. However, no significant difference was observed in the accumulation of silt- and clay-associated SOC between CK and rice straw (RS) treatments. Besides, in comparison with plots applied with NPK fertilizers alone, combined application of organic amendments and NPK fertilizers facilitated the storage of newly sequestered SOC in silt- and clay-sized fractions, which could be more conducive to the stability of SOC. Based on 13C-NMR spectra, both silt and clay fractions were composed of Alkyl-C, O-alkyl-C, Aromatic-C and carbonyl-C. Changes in the relative proportion of different C species were observed between silt and clay fractions: the clay fraction had relatively more Alkyl-C, carbonyl-C and less O-alkyl-C, Aromatic-C than those in the silt fraction. This might be ascribed to the fact that the organic matter complexed with clay was dominated by microbial products, whereas the silt appeared to be rich in aromatic residues derived from plants. The spectra also showed that the relative proportion of different C species was modified by fertilization practices. In comparison with organic amendments alone, the relative proportion of Alkyl-C was decreased by 9.1%-11.9% and 13.7%-19.9% under combined application of organic amendments and chemical fertilizers, for silt and clay, respectively, and that of O-alkyl-C was increased by 2.9%-6.3% and 13.4%-22.1%, respectively. These results indicated that NPKOM and NPKRS treatments reduced the decomposition rate of SOC. The aromaticity, hydrophobicity and, hence, chemical recalcitrance of silt- and clay-associated SOC in the NPK fertilizer treatments were lower than those of the organically amended plots and unfertilized treatments, indicating decreased recalcitrance of SOC against decomposition. We concluded that long-term application of organic manure combined with chemical fertilizers, either through increased accumulation of both recalcitrant compounds and carbohydrates or reduced decomposition of organic matter, was a sustainable strategy for facilitating carbon accumulation of the paddy soil investigated in this study.

摘要

在中国浙江省进行的一项为期17年的长期施肥田间试验中,研究了化肥和有机肥对水稻土不同粒径组分中土壤有机碳(SOC)含量的影响。利用固态13C-NMR光谱对粉砂和黏土结合态SOC的固有化学组成进行了评估。与对照(不施肥处理)相比,NPKRS(NPK化肥加稻草)、NPKOM(NPK化肥加有机肥)、NPK(NPK化肥)和OM(单独施用有机肥)处理显著(P<0.05)提高了砂粒(2-0.02mm)、粉砂粒(0.02-0.002mm)和黏粒(<0.002mm)组分的SOC含量。然而,对照和稻草(RS)处理之间在粉砂和黏土结合态SOC的积累上未观察到显著差异。此外,与单独施用NPK化肥的小区相比,有机改良剂与NPK化肥的联合施用促进了新固存SOC在粉砂和黏粒组分中的储存,这可能更有利于SOC的稳定性。基于13C-NMR光谱,粉砂和黏粒组分均由烷基-C、O-烷基-C、芳香族-C和羰基-C组成。粉砂和黏粒组分之间不同碳物种的相对比例发生了变化:黏粒组分中烷基-C、羰基-C相对较多,O-烷基-C、芳香族-C比粉砂组分中少。这可能归因于与黏土结合的有机质以微生物产物为主,而粉砂似乎富含源自植物的芳香族残基。光谱还表明,不同碳物种的相对比例受施肥措施的影响。与单独施用有机改良剂相比,有机改良剂与化肥联合施用时,粉砂和黏粒中烷基-C的相对比例分别降低了9.1%-11.9%和13.7%-19.9%,O-烷基-C的相对比例分别增加了2.9%-6.3%和13.4%-22.1%。这些结果表明,NPKOM和NPKRS处理降低了SOC的分解速率。NPK化肥处理中粉砂和黏土结合态SOC的芳香性、疏水性以及化学难分解性低于有机改良小区和未施肥处理,表明SOC对分解作用的难分解性降低。我们得出结论,长期施用有机肥与化肥相结合,无论是通过增加难分解化合物和碳水化合物的积累,还是通过降低有机质的分解,都是促进本研究中水稻土碳积累的可持续策略。

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