Department of Crop and Soil Sciences, Cornell University, Ithaca, New York 14853, USA.
Ecol Appl. 2013 Jul;23(5):1017-35. doi: 10.1890/12-0132.1.
Nitrogen (N) leaching to surface waters from grain farms in the Mississippi River Basin (MRB), USA, is the primary cause of hypoxia in the Gulf of Mexico. Regional-scale N mass balances indicate that a small, intensively cropped area of the upper MRB contributes disproportionately to nitrate loading. These aggregate balances miss small-scale variability, especially that caused by differences in farm management. We constructed N mass balances for a gradient of farm types, from corn-soybean monocultures to diversified grain farms that rely on biological N fixation (BNF) as a primary N source, to compare the relative efficiency of diverse farming systems in the MRB. Five-year N balances were calculated for a most and least productive field on each farm using data collected from interviews with 95 grain farmers in Iowa, Ohio, Minnesota, and Wisconsin; from legume biomass and corn grain samples collected from a subset of farms; and published values from the literature. Nitrogen balances ranged from high average annual surpluses (149 kg N x ha(-1) x yr(-1)) to large deficits (80 kg N x ha(-1) x yr(-1)), and differed based on N source and crop rotation. Fields with > 50% of total N additions from legume N sources and fields with complex crop rotations that included both annual and perennial species were approximately in balance (3.7 kg N x ha(-1) x yr(-1) and 5.7 kg N x ha(-1) x yr(-1), respectively) compared to fertilizer-based practices in corn-soybean rotations with average annual surpluses near 35 kg N x ha(-1) x yr(-1). Surplus N was also inversely related to the proportion of total N inputs from BNF for medium (80-160 kg N x ha(-1) x yr(-1)) to high (> 160 kg N x ha(-1) x yr(-1)) N rates. Diversified farmers were more likely to adjust their management practices in response to environmental variability compared to fertilizer-based farmers. Taken together, results from this study suggest that significantly reducing surplus N in agroecosystems will require reducing N inputs and increasing C availability to support the internal biological mechanisms for storing N in farm fields.
美国密西西比河流域(MRB)的谷物农场向地表水中淋滤的氮(N)是墨西哥湾缺氧的主要原因。区域尺度的 N 质量平衡表明,MRB 上游一个小而集约化的作物种植区对硝酸盐负荷的贡献不成比例。这些综合平衡忽略了小规模的可变性,尤其是由农场管理差异引起的可变性。我们构建了从玉米-大豆单一栽培到依赖生物固氮(BNF)作为主要 N 源的多样化谷物农场的梯度的 N 质量平衡,以比较密西西比河流域不同农业系统的相对效率。使用从爱荷华州、俄亥俄州、明尼苏达州和威斯康星州的 95 位谷物农民的访谈中收集的数据、从一组农场采集的豆科植物生物量和玉米谷物样本以及文献中公布的值,为每个农场的最具生产力和最不具生产力的田地计算了五年的 N 平衡。氮平衡从高平均年盈余(149 kg N x ha(-1) x yr(-1))到大量亏缺(80 kg N x ha(-1) x yr(-1))不等,并且因 N 来源和作物轮作而异。具有 >50%的总 N 添加量来自豆科植物 N 源的田地和包括一年生和多年生物种的复杂作物轮作的田地分别接近平衡(分别为 3.7 kg N x ha(-1) x yr(-1)和 5.7 kg N x ha(-1) x yr(-1)),而玉米-大豆轮作中的基于肥料的做法平均每年盈余近 35 kg N x ha(-1) x yr(-1)。剩余的 N 也与中等(80-160 kg N x ha(-1) x yr(-1))到高(>160 kg N x ha(-1) x yr(-1))N 率的总 N 输入中来自 BNF 的比例呈反比关系。与基于肥料的农民相比,多样化的农民更有可能根据环境变化调整他们的管理实践。总的来说,这项研究的结果表明,要显著减少农业生态系统中的过剩 N,就需要减少 N 投入并增加 C 供应,以支持在农田中储存 N 的内部生物机制。