Department of Plant Sciences, University of California, Davis, CA, United States of America.
Department of Viticulture and Enology, University of California, Davis, CA, United States of America.
Sci Total Environ. 2020 Jun 20;722:137889. doi: 10.1016/j.scitotenv.2020.137889. Epub 2020 Mar 12.
Nitrogen (N) fertilizer use has simultaneously increased global food production and N losses, resulting in degradation of water quality and climate pollution. A better understanding of N application rates and crop and environmental response is needed to optimize management of agroecosystems. Here we show an orchard agroecosystem with high N use efficiency promoted substantial gains in carbon (C) storage, thereby lowering net global warming potential (GWP). We conducted a 5-year whole-system analysis comparing reduced (224 kg N ha yr) and intensive (309 kg N ha yr) fertilizer N rates in a California almond orchard. The intensive rate increased net primary productivity (Mg C ha) and significantly increased N productivity (kg N ha) and net N mineralization (mg N kg soil d). Use of N tracers demonstrated short and long-term mechanisms of soil N retention. These low organic matter soils (0.3-0.5%) rapidly immobilized fertilizer nitrate within 36 h of N application and N in tree biomass recycled back into soil organic matter over five years. Both fertilizer rates resulted in high crop and total N recovery efficiencies of 90% and 98% for the reduced rate, and 72% and 80% for the intensive rate. However, there was no difference in the proportion of N losses to N inputs due to a significant gain in soil total N (TN) in the intensive rate. Higher soil TN significantly increased net N mineralization and a larger gain in soil organic carbon (SOC) from the intensive rate offset nitrous oxide (NO) emissions, leading to significantly lower net GWP of -1.64 Mg CO-eq ha yr compared to -1.22 Mg CO-eq ha yr for the reduced rate. Our study demonstrates increased N cycling and climate mitigation from intensive fertilizer N use in this orchard agroecosystem, implying a fundamentally different result than seen in conventional annual cropping systems.
氮肥(N)的使用在提高全球粮食产量的同时,也导致了 N 的大量流失,从而造成了水质恶化和气候污染。为了优化农业生态系统的管理,我们需要更好地了解氮肥的施用量以及作物和环境的反应。在这里,我们展示了一个果园农业生态系统,该系统具有高氮利用效率,促进了碳(C)储存的大量增加,从而降低了净全球变暖潜力(GWP)。我们进行了为期 5 年的全系统分析,比较了加利福尼亚州杏仁果园中减少(224kgNha yr)和密集(309kgNha yr)施肥氮率。密集施肥率增加了净初级生产力(Mg C ha),并显著增加了 N 生产力(kgNha)和净 N 矿化(mgNkg 土壤 d)。氮示踪剂的使用表明了土壤 N 保持的短期和长期机制。这些低有机质土壤(0.3-0.5%)在施氮后 36 小时内迅速将肥料硝酸盐固定,并在五年内将树木生物量中的 N 回收回土壤有机质中。两种施肥率都导致了高的作物和总 N 回收率,减少施肥率为 90%和 98%,密集施肥率为 72%和 80%。然而,由于密集施肥率土壤总氮(TN)的显著增加,氮损失与氮输入的比例没有差异。较高的土壤 TN 显著增加了净 N 矿化,密集施肥率下土壤有机碳(SOC)的增加幅度更大,从而抵消了氧化亚氮(NO)的排放,使净 GWP 显著降低至-1.64Mg CO-eq ha yr,而减少施肥率为-1.22Mg CO-eq ha yr。我们的研究表明,在这个果园农业生态系统中,密集施用氮肥增加了 N 循环和减缓气候变化,这与传统的一年生作物系统的结果截然不同。