UPMC Univ Paris 06, Unité Mixte de Recherche 7618, BIOEMCO, F-75005 Paris, France.
Proc Natl Acad Sci U S A. 2013 Nov 5;110(45):18185-9. doi: 10.1073/pnas.1305372110. Epub 2013 Oct 21.
Increasing diffuse nitrate loading of surface waters and groundwater has emerged as a major problem in many agricultural areas of the world, resulting in contamination of drinking water resources in aquifers as well as eutrophication of freshwaters and coastal marine ecosystems. Although empirical correlations between application rates of N fertilizers to agricultural soils and nitrate contamination of adjacent hydrological systems have been demonstrated, the transit times of fertilizer N in the pedosphere-hydrosphere system are poorly understood. We investigated the fate of isotopically labeled nitrogen fertilizers in a three-decade-long in situ tracer experiment that quantified not only fertilizer N uptake by plants and retention in soils, but also determined to which extent and over which time periods fertilizer N stored in soil organic matter is rereleased for either uptake in crops or export into the hydrosphere. We found that 61-65% of the applied fertilizers N were taken up by plants, whereas 12-15% of the labeled fertilizer N were still residing in the soil organic matter more than a quarter century after tracer application. Between 8-12% of the applied fertilizer had leaked toward the hydrosphere during the 30-y observation period. We predict that additional exports of (15)N-labeled nitrate from the tracer application in 1982 toward the hydrosphere will continue for at least another five decades. Therefore, attempts to reduce agricultural nitrate contamination of aquatic systems must consider the long-term legacy of past applications of synthetic fertilizers in agricultural systems and the nitrogen retention capacity of agricultural soils.
地表水和地下水的硝酸盐负荷不断增加,已成为世界上许多农业区的主要问题,导致含水层中饮用水资源受到污染,以及淡水和沿海海洋生态系统的富营养化。尽管已经证明了农业土壤中氮肥施用量与相邻水文系统中硝酸盐污染之间存在经验相关性,但在土壤-水系统中肥料氮的迁移时间还了解甚少。我们研究了在一个长达三十年的原位示踪剂实验中,同位素标记氮肥的命运,该实验不仅量化了植物对肥料氮的吸收和土壤中的保留,还确定了在多大程度上以及在多长时间内,储存在土壤有机质中的肥料氮被重新释放,以供作物吸收或进入水圈。我们发现,61-65%的施入氮肥被植物吸收,而 12-15%的标记肥料氮在示踪剂应用后超过二十五年仍存在于土壤有机质中。在 30 年的观测期内,有 8-12%的施入肥料已经向水圈泄漏。我们预测,从 1982 年示踪剂应用中向水圈继续释放的(15)N 标记硝酸盐将至少再持续五十年。因此,减少农业系统中硝酸盐对水生系统的污染的尝试必须考虑到过去农业系统中合成肥料的长期应用以及农业土壤的氮素保持能力。