Environment and Plant Protection Institute, Chinese Academy of Tropical Agricultural Sciences, Key Laboratory of Low-carbon Green Agriculture in Tropical Region of China, Ministry of Agriculture and Rural Affairs, PR China, Haikou, 571101, China; Hainan Danzhou Tropical Agro-ecosystem National Observation and Research Station, Danzhou, 571737, China; Hainan Key Laboratory of Tropical Eco-Circular Agriculture, Haikou, 571101, China; National Agricultural Experimental Station for Agricultural Environment, National Long-term Experimental Station for Agriculture Green Development, Danzhou, 571737, Hainan, China; State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences, Beijing, 100012, China.
Environment and Plant Protection Institute, Chinese Academy of Tropical Agricultural Sciences, Key Laboratory of Low-carbon Green Agriculture in Tropical Region of China, Ministry of Agriculture and Rural Affairs, PR China, Haikou, 571101, China; Hainan Danzhou Tropical Agro-ecosystem National Observation and Research Station, Danzhou, 571737, China; Hainan Key Laboratory of Tropical Eco-Circular Agriculture, Haikou, 571101, China; National Agricultural Experimental Station for Agricultural Environment, National Long-term Experimental Station for Agriculture Green Development, Danzhou, 571737, Hainan, China.
Environ Res. 2024 Dec 1;262(Pt 2):119903. doi: 10.1016/j.envres.2024.119903. Epub 2024 Sep 6.
Fertilization is a critical agronomic measure for croplands in tropical regions, owing to their low fertility. However, the effects of fertilization on the quantity and chemodiversity of latosolic dissolved organic matter (DOM) in tropical regions remain largely unknown. Therefore, in this study, the variations in latosol DOM concentrations and chemodiversity induced by inorganic fertilization and the co-application of inorganic fertilization with straw return, sheep manure, biochar, and vermicompost fertilizers at a molecular level were systematically investigated using multispectral techniques and ultrahigh-resolution mass spectrometry. In line with our expectations, the results showed that combined inorganic-organic fertilization improved soil quality by increasing soil organic carbon content compared to that under inorganic fertilization. However, as the most active and bioavailable organic carbon pool, dissolved organic carbonconcentrations between the fertilization treatments were not significantly different (p = 0.07). However, the dissolved organic carbon concentrations under combined inorganic-organic fertilization treatment (NPK plus straw return, 263.45 ± 37.51 mg/kg) were lower than those under inorganic fertilization treatment (282.10 ± 18.57 mg/kg). Spectral analysis showed that the DOM in the combined inorganic-organic fertilization treatments had a higher degree of humification and lower autogenetic contributions. Furthermore, Fourier transform ion cyclotron resonance mass spectrometry analysis indicated that the combined inorganic-organic fertilization increased the chemodiversity of latosolic DOM and promoted the production of large, oxidized, and stable molecules, including lignin, aromatic, and tannin compounds, which potentially benefits soil carbon sequestration in tropical regions. This study could provide a theoretical basis for elucidating on the potentially relevant ecological functions and environmental effects of DOM under fertilization regimes.
施肥是热带地区农田的一项关键农业措施,因为这些地区的土壤肥力较低。然而,施肥对热带地区土壤中 Latosol 溶解有机物质(DOM)的数量和化学多样性的影响在很大程度上仍不清楚。因此,在这项研究中,我们使用多光谱技术和超高分辨率质谱法,系统地研究了无机肥和秸秆还田、羊粪、生物炭和蚯蚓粪肥的联合施用对 Latosol DOM 浓度和化学多样性变化的影响。正如我们所预期的那样,与单独使用无机肥相比,无机-有机肥的联合施用通过增加土壤有机碳含量来提高土壤质量。然而,作为最活跃和最具生物利用性的有机碳库,不同施肥处理之间的溶解有机碳浓度没有显著差异(p=0.07)。然而,在无机-有机肥联合施用处理下(NPK 加秸秆还田,263.45±37.51mg/kg),溶解有机碳浓度低于单独使用无机肥处理(282.10±18.57mg/kg)。光谱分析表明,联合无机-有机肥处理的 DOM 具有更高的腐殖化程度和更低的自生源贡献。此外,傅里叶变换离子回旋共振质谱分析表明,无机-有机肥的联合施用增加了 Latosol DOM 的化学多样性,并促进了大、氧化、稳定分子的生成,包括木质素、芳香族和单宁化合物,这可能有利于热带地区土壤碳的固存。这项研究可为阐明施肥条件下 DOM 的潜在相关生态功能和环境效应提供理论依据。