关于铜对全球农田循环的影响的初步证据:元分析
Ahmed S Elrys1, YuHong Wen2, Xiaofeng Qin2
1College of Tropical Agriculture and Forestry, Hainan University, Haikou 570228, China; Soil Science Department, Faculty of Agriculture, Zagazig University, Zagazig 44511, Egypt; Liebig Centre for Agroecology and Climate Impact Research, Justus Liebig University, Giessen, Germany.
Environment international
|February 10, 2024
概括
过多的铜 (Cu) 会损害土壤化和微生物功能. 然而,低水平的铜可以刺激酸盐,而高水平的铜可以减少耕地中的气损失和氧化物排放.
科学领域:
- 土壤科学 土壤科学
- 环境微生物学 环境微生物学
- 生物地质化学生物地质化学
背景情况:
- 铜 (Cu) 在化过程中对氨一氧化酶至关重要.
- 过量的会对土壤微生物和植物生长产生负面影响.
- 对耕地 (N) 循环的全球影响在很大程度上是未知的.
研究的目的:
- 研究Cu对农田土壤中N循环和相关变量的影响.
- 量化Cu添加和污染对土壤N过程的影响.
- 探索Cu度与N转化速率之间的关系.
主要方法:
- 从94个出版物中对1209个配对和319个单独的观察结果进行了元分析.
- 评估了潜在的化,酸盐,酸盐和酶活动的变化.
- 检查了微生物生物质,氨氧化古生物和总N转化率.
主要成果:
- 降低了潜在的化 (33.8%) 和化物 (73.5%),与较低的酶活性和微生物生物质相关.
- 高 (>150毫克/kg-1) 抑制了化 (46.5%),而低刺激了酸盐 (99.0%).
- 增加Cu含量刺激了N矿化,但抑制了化,最终减少了N损失和氧化排放.
结论:
- 铜在调节土壤N的可用性和损失方面发挥着重要作用.
- 的度会影响土壤中的N生产和消费途径.
- 这些发现突显了Cu在土壤N循环中的双重作用,这对减轻N损失有影响.
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