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Deep soils modify environmental consequences of increased nitrogen fertilizer use in intensifying Amazon agriculture

机译:深层土壤改变了氮肥用量增加对亚马逊农业集约化的环境影响

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摘要

Agricultural intensification offers potential to grow more food while reducing the conversion of native ecosystems to croplands. However, intensification also risks environmental degradation through emissions of the greenhouse gas nitrous oxide (N2O) and nitrate leaching to ground and surface waters. Intensively-managed croplands and nitrogen (N) fertilizer use are expanding rapidly in tropical regions. We quantified fertilizer responses of maize yield, N2O emissions, and N leaching in an Amazon soybean-maize double-cropping system on deep, highly-weathered soils in Mato Grosso, Brazil. Application of N fertilizer above 80 kg N ha−1 yr−1 increased maize yield and N2O emissions only slightly. Unlike experiences in temperate regions, leached nitrate accumulated in deep soils with increased fertilizer and conversion to cropping at N fertilization rates >80 kg N ha−1, which exceeded maize demand. This raises new questions about the capacity of tropical agricultural soils to store nitrogen, which may determine when and how much nitrogen impacts surface waters.
机译:农业集约化提供了种植更多粮食的潜力,同时减少了本地生态系统向农田的转化。但是,集约化还可能通过排放温室气体一氧化二氮(N2O)和硝酸盐渗入地下水和地表水而导致环境退化。在热带地区,集约化管理的耕地和氮肥的使用正在迅速扩大。我们在巴西马托格罗索州的深层,高风化土壤上,对亚马逊大豆-玉米双作系统中玉米产量,N2O排放和氮淋失的肥料响应进行了定量。在80 kg N ha -1 yr -1 以上施氮肥仅能使玉米产量和N2O排放量略有增加。与温带地区不同,氮肥在> 80 kg N ha -1 的施肥条件下,深层土壤中的硝态氮积累量增加,并转化为作物,这超过了玉米的需求。这就提出了有关热带农业土壤储存氮的能力的新问题,这可能决定何时和多少氮影响地表水。

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