首页> 外文期刊>Southern Journal of Applied Forestry >Streamside Management Zones Affect Movement of Silvicultural Nitrogen and Phosphorus Fertilizers to Piedmont Streams
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Streamside Management Zones Affect Movement of Silvicultural Nitrogen and Phosphorus Fertilizers to Piedmont Streams

机译:溪流管理区影响造林氮磷肥向皮埃蒙特溪流的迁移

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Forestry best management practices (BMP) recommendations for streamside management zones (SMZs) are based on limited data regarding SMZ width, partial harvests, and nutrient movements after forest fertilization. Agricultural fertilization is commonlylinked to increased stream nutrients. However, less is known about effectiveness of SMZ options for controlling nutrient movements after silvicultural fertilization. Oiammonium phosphate and urea were applied to 12 subwatersheds in 3-year-old loblolly pine [Pinus taeda L) plantations in the Virginia Piedmont. Three replicates of four SMZ treatments were superimposed on 12 subwatersheds in a previous SMZ harvest sediment study (7.6-m SMZ, 15.2-m SMZ thin, 15.2-m SMZ, and 30.5-m SMZ). Surface, near-surface, subsurface, and stream water samples were collected monthly for 1 year and analyzed for nitrate (NO3_3~-), ammonium (NH_4~+), and orthophosphate (orfho-P). Transected measurements from streamside to fertilized plantations allowed interpretations of spatial nutrient measurements across SMZs. When compared with wider SMZs, 7.6-m SMZs had 3-1 Ox surface water NO3_3~-, 3-6x near-surface water NO3_3~-, and l-2x more stream water NO3_3~-. No significant differences were detected for NH_4~+ for any SMZ treatment. The 15.2-m SMZ thin had small but significant increases (2-8x) in surface runoff for ortho-P relative to other SMZ treatments, perhaps because of increased surface water movement along thinning corridors. Across all SMZ treatments, comparisons ofstream edges with fertilized stands indicated NO3_3~- reductions of 33-98%, NNH_4~+ reductions of 68-97%, and ortho-P reductions of 70-98%. A 39% rainfall deficit during the study influenced results, but conventional SMZs > 15.2 m protected streams fromfertilization nutrient increases.
机译:对于河边管理区(SMZ)的林业最佳管理实践(BMP)建议基于有关SMZ宽度,部分采伐和施肥后养分流动的有限数据。农业施肥通常与增加溪流养分有关。但是,对于造林施肥后SMZ控制营养物移动的有效性知之甚少。将磷化ed和尿素施用于弗吉尼亚皮埃蒙特州3年大的火炬松(Pinus taeda L)人工林的12个小流域。在先前的SMZ收获沉积物研究(7.6米SMZ,15.2米SMZ稀薄,15.2米SMZ和30.5米SMZ)中,四个SMZ处理的三个重复叠加在12个小流域上。每月收集地表,近地表,地下和溪流水样品,为期1年,并分析硝酸盐(NO3_3〜-),铵盐(NH_4〜+)和正磷酸盐(orfho-P)。从溪边到施肥人工林的横切测量值可以解释SMZ之间的空间养分测量值。与较宽的SMZ相比,7.6米的SMZ具有3-1 Ox地表水NO3_3〜-,3-6x地表水NO3_3〜-和1-2x的流水NO3_3〜-。对于任何SMZ处理,未检测到NH_4〜+的显着差异。与其他SMZ处理相比,ortho-P的15.2米SMZ薄层的地表径流量小而显着增加(2-8x),这可能是因为沿稀疏走廊的地表水运动增加了。在所有SMZ处理中,将流域边缘与施肥林分进行比较后发现,NO3_3〜-减少了33-98%,NNH_4〜+减少了68-97%,ortho-P减少了70-98%。该研究期间39%的降雨不足影响了结果,但传统的SMZ> 15.2 m可以保护河流免受施肥养分的增加。

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