在中国主要的农田中出现了显著的酸化
1College of Resources and Environmental Sciences, China Agricultural University, Beijing 100193, China.
概括
中国的密集农业导致了土壤显著酸化,循环和阴离子吸收是主要的驱动因素. 酸性沉积对这种广泛的农业土壤问题做出的贡献很小.
科学领域:
- 农业科学 农业科学
- 环境科学 环境科学
- 土壤科学 土壤科学
背景情况:
- 土壤酸化是中国密集农业系统的一个关键问题.
- 土壤pH值下降对作物生产和土壤健康构成威胁.
研究的目的:
- 评估中国主要作物生产地区土壤酸度的变化.
- 确定这些农业土壤中土壤酸化的主要驱动因素.
主要方法:
- 利用两个全国性调查来评估土壤pH值的变化.
- 员工在众多地点进行了对比比较,并分析了长期监测数据.
- 循环和基离子吸收对土壤酸化的量化贡献.
主要成果:
- 从20世纪80年代到21世纪,主要农业地区的土壤pH值显著下降 (P<0.001).
- 循环过程每年每公释放20221kmol H+ .
- 基离子的吸收每年每公增加了1520kmol H+.
- 酸沉积的贡献是最小的 (每公每年0.42.0 kmol H+).
结论:
- 强化农业实践,特别是循环和酸盐吸收,是中国土壤酸化的主要驱动因素.
- 酸沉积在中国农业土壤的酸性化中起到较小的作用.
- 需要紧急的管理策略来缓解土壤酸化并维持农业生产率.
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