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Influence of crop rotation tillage and fertilization on chemical and spectroscopic characteristics of humic acids

机译:轮作耕作和施肥对腐植酸化学和光谱特性的影响

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摘要

The changes in soil organic matter composition induced by anthropogenic factors is a topic of great interest for the soil scientists. The objective of this work was to identify possible structural changes in humic molecules caused by a 2-year rotation of durum wheat with faba bean, lasted for a decade, and conducted with different agricultural practices in a Mediterranean soil. Humic acids (HA) were extracted at three depths (0–30, 30–60 and 60–90 cm) from a Mediterranean soil subjected to different tillage (no tillage, minimum tillage and conventional tillage), crops (faba bean and wheat), and fertilization. The changes in HA quality were assessed by several chemical (ash, yield and elemental analysis) and spectroscopic techniques (solid-state 13C nuclear magnetic resonance, Fourier transform infrared and fluorescence). The results suggest that the different agronomic practices strongly affected the quality of HA. Smaller but more aromatic molecules were observed with depth, while the fertilization induced the formation of simpler and less aromatic molecules due to the enhanced decomposition processes. Under no tillage, more stable humic molecules were observed due to the less soil aeration, while under conventional tillage larger and more aromatic molecules were obtained. Compared to wheat, more aromatic and more oxidized but less complex molecules were observed after faba bean crop. The inorganic fertilization accelerates the decomposition of organic substances rather than their stabilization. At the end of each crop cycle, humic matter of different quality was isolated and this confirms the importance of the rotation practice to guarantee a diversification of the soil organic matter with time. Finally, no tillage induces the formation of more stable humic matter.
机译:人为因素引起的土壤有机质组成的变化是土壤科学家们非常感兴趣的一个话题。这项工作的目的是确定硬粒小麦与蚕豆轮换使用2年,持续10年并在地中海土壤中采用不同的农业实践进行操作,从而导致腐殖质分子的结构变化。从经历了不同耕作(无耕种,最少耕种和常规耕种),农作物(巴西豆和小麦)的地中海土壤的三个深度(0–30、30–60和60–90厘米)中提取腐殖酸(HA)和施肥。 HA质量的变化通过几种化学方法(灰分,产率和元素分析)和光谱技术(固态13C核磁共振,傅立叶变换红外和荧光)进行了评估。结果表明,不同的农艺实践强烈影响着HA的质量。深度观察到更小但更多的芳族分子,而由于增强的分解过程,施肥诱导形成更简单且更少的芳族分子。在免耕条件下,由于土壤通气量较小,因此观察到的腐殖质分子更稳定,而在传统耕作条件下,获得的腐殖质分子更大且更多。与小麦相比,蚕豆种植后观察到更多的芳香和更多的氧化,但是分子却很少。无机肥会加速有机物质的分解,而不是使其稳定。在每个作物周期结束时,分离出不同质量的腐殖质,这证实了轮作的重要性,以确保土壤有机质随时间的多样化。最后,没有耕作引起更稳定的腐殖质的形成。

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