College of Resources and Environment, Huazhong Agricultural University, Wuhan 430070, China.
Hubei Province Key Laboratory for Geographical Process Analysis and Simulation, Central China Normal University, Wuhan 430079, China; Department of Ecohydrology, Leibniz Institute of Freshwater Ecology and Inland Fisheries, Berlin 12587, Germany.
Water Res. 2023 Sep 1;243:120398. doi: 10.1016/j.watres.2023.120398. Epub 2023 Jul 22.
Nitrate-nitrogen (NO-N) loss is a significant contributor to water quality degradation in agricultural catchments. The amount of nitrogen (N) fertilizer input in citrus orchard is relatively large and results in significant NO-N loss, compared to cropland. To promote sustainable N fertilizer management, it is crucial to identify the sources of runoff NO-N loss in citrus orchards catchments. Particularly, we poorly know the sources of NO-N and the mitigation mechanisms in these areas, which are highly polluted with NO-N in water bodies. In this study conducted in central China, we conducted a field experiment with four treatments (CK: no N fertilizer; CF: conventional N fertilizer, 371.3kg N ha yr urea; OM: CF with organic manure; GM: CF with legume green manure) and a catchment-scale experiment in two citrus orchards (34.3%; 51.6%) catchments. To determine the source of runoff NO-N loss, we used the dual isotope tracer method (δN and δO of NO) to identify the sources of NO-N, and a 15-day incubation experiment to determine the potential and rate of soil N mineralization. Our findings revealed that soil organic nitrogen (SON) mineralization was the primary contributor to runoff NO-N loss, and soil N mineralization potential (0.65) and rate (0.54) were the key factors impacting NO-N loss. Interestingly, organic manure significantly increased 29.0% of NO-N loss derived from SON in the runoff by enhancing soil N mineralization potential (+36.6%) and rate (+77.1%). But green manure mulching significantly reduced the soil N mineralization rate (-18.6%) compared to organic manure application, making it the most effective measure to reduce NO-N loss (-12.4%). Our study highlights the critical role of regulating SON mineralization in controlling NO-N pollution in surface waters in citrus orchard catchments.
硝酸盐氮(NO-N)的流失是农业集水区水质恶化的一个重要因素。与农田相比,柑橘园的氮肥投入量相对较大,导致大量的 NO-N 流失。为了促进可持续的氮肥管理,确定柑橘园集水区径流水中 NO-N 流失的来源至关重要。特别是,我们对这些高度受水体中 NO-N 污染的地区的 NO-N 来源和缓解机制知之甚少。在本研究中,我们在中国中部进行了一项田间实验,其中包括四个处理(CK:不施氮肥;CF:常规氮肥,施 371.3kg N ha yr 尿素;OM:CF 加有机肥;GM:CF 加豆科绿肥)和两个柑橘园(34.3%和 51.6%)集水区的流域尺度实验。为了确定径流水中 NO-N 流失的来源,我们使用双同位素示踪法(δN 和 δO of NO)来确定 NO-N 的来源,并进行了为期 15 天的培养实验来确定土壤氮矿化的潜力和速率。我们的研究结果表明,土壤有机氮(SON)矿化是径流水中 NO-N 流失的主要来源,土壤氮矿化潜力(0.65)和速率(0.54)是影响 NO-N 流失的关键因素。有趣的是,有机肥显著增加了 29.0%的 SON 衍生的径流水中 NO-N 流失,这是由于其提高了土壤氮矿化潜力(增加了 36.6%)和速率(增加了 77.1%)。而绿肥覆盖显著降低了土壤氮矿化速率(减少了 18.6%),与有机肥相比,是减少 NO-N 流失的最有效措施(减少了 12.4%)。本研究强调了调控 SON 矿化在控制柑橘园集水区地表水中 NO-N 污染中的关键作用。