Dep. of Soil and Crop Sciences, Texas A&M Univ., 370 Olsen Blvd., College Station, TX 77843-2474, USA.
J Environ Qual. 2010 Sep-Oct;39(5):1762-70. doi: 10.2134/jeq2010.0032.
Managing manure in no-till systems is a water quality concern because surface application of manure can enrich runoff with dissolved phosphorus (P), and incorporation by tillage increases particulate P loss. This study compared runoff from well-drained and somewhat poorly drained soils under corn (Zea mays, L.) production that had been in no-till for more than 10 yr. Dairy cattle (Bos taurus L.) manure was broadcast into a fall planted cover crop before no-till corn planting or incorporated by chisel/disk tillage in the absence of a cover crop. Rainfall simulations (60 mm h(-1)) were performed after planting, mid-season, and post-harvest in 2007 and 2008. In both years and on both soils, no-till yielded significantly less sediment than did chisel/disking. Relative effects of tillage on runoff and P loss differed with soil. On the well-drained soil, runoff depths from no-till were much lower than with chisel/disking, producing significantly lower total P loads (22-50% less). On the somewhat poorly drained soil, there was little to no reduction in runoff depth with no-till, and total P loads were significantly greater than with chisel/disking (40-47% greater). Particulate P losses outweighed dissolved P losses as the major concern on the well-drained soil, whereas dissolved P from surface applied manure was more important on the somewhat poorly drained soil. This study confirms the benefit of no-till to erosion and total P runoff control on well-drained soils but highlights trade-offs in no-till management on somewhat poorly drained soils where the absence of manure incorporation can exacerbate total P losses.
免耕系统中粪肥管理是一个水质关注点,因为粪肥的地表施用会使径流中溶解态磷(P)富化,而耕作的翻耕会增加颗粒态 P 的损失。本研究比较了在免耕 10 年以上的玉米(Zea mays,L.)生产下,排水良好和排水不良的土壤的径流水。在免耕玉米种植前,将奶牛(Bos taurus L.)粪肥撒播到秋季种植的覆盖作物中,或者在没有覆盖作物的情况下用凿耕/圆盘耕翻进行翻耕。在 2007 年和 2008 年种植后、生长中期和收获后进行了 60 毫米/小时的降雨模拟。在这两年和两种土壤中,免耕的泥沙流失量明显少于凿耕/圆盘耕翻。耕作对径流和 P 损失的相对影响因土壤而异。在排水良好的土壤中,免耕的径流深度远低于凿耕/圆盘耕翻,产生的总 P 负荷明显较低(低 22-50%)。在排水不良的土壤中,免耕几乎没有减少径流深度,总 P 负荷明显高于凿耕/圆盘耕翻(高 40-47%)。在排水良好的土壤中,颗粒态 P 流失是主要关注点,超过了溶解态 P 流失,而在排水不良的土壤中,表面施用粪肥中的溶解态 P 更为重要。本研究证实了免耕对排水良好土壤的侵蚀和总 P 径流控制的益处,但突出了免耕管理在排水不良土壤中的权衡,其中粪肥翻耕的缺失会加剧总 P 流失。