在长期生物炭添加下,在米过渡系统中,从物理化学性质转向微生物驱动的动力学
Zhijie Dong1, Kaixiong Xing2, Yilai Lou3
1Ministry of Education Key Laboratory for Ecology of Tropical Islands, College of Life Science, Hainan Normal University, Haikou, 571158, China; Institute of Environment and Sustainable Development in Agriculture, Chinese Academy of Agricultural Sciences, Beijing, 100081, China.
Journal of environmental management
|June 5, 2025
概括
长期使用生物炭可以改善土壤循环和可用性,特别是在作物过渡期间. 生物炭和的协同作用提高了在性土壤中的可持续性.
科学领域:
- 土壤科学 土壤科学
- 环境科学 环境科学
- 农业学是一种农业学.
背景情况:
- 已知生物炭的应用可以改善微生物介导的 (P) 循环.
- 生物炭对土壤的十年级影响在作物过渡期间的P动态并未得到充分理解.
研究的目的:
- 调查生物炭对土壤P动态在性土壤的作物过渡期间的长期影响.
- 了解生物炭, (N) 施肥和土壤特性在调节P的可用性方面的相互作用.
主要方法:
- 进行了一项为期9年的实地实验,连续种植大米,然后种植玉米.
- 应用了三种生物碳率和两种含量.
- 分析了土壤的物理化学特性,不稳定的P池以及微生物社区的结构和功能.
主要成果:
- 长期使用生物炭显著增强了不稳定的P池,并减轻了N诱导的P限制.
- 物理化学性质调节了大米中的P可用性,而在玉米中,微生物过程成为主导.
- 生物炭增强了玉米土壤中的P矿化网络,并保持了微生物多样性.
结论:
- 长期的生物炭-N协同作用增强了性土壤中P的可持续性.
- 红氧依赖的监管层次 (物理化学与微生物物理化学相互作用) 控制着不同作物系统中的P的可用性.
- 这些发现为优化生物炭使用提供了基础,以提高营养素使用效率并缓解P稀缺.
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