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Chapter 6 The Effects of Soil Phosphorus and Nitrogen and Phosphorus Fertilization on Phosphorus Runoff Losses from Turfgrass

机译:第六章土壤磷,氮和磷的施肥对草坪草磷流失的影响

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Turfgrass accounts for a large percentage of land in urban and suburban areas and thus, it is important to understand the effects of turfgrass on surface water quality. Runoff from natural and simulated rain events was collected from a cool season turfgrass mixture on an undisturbed sandy loam soil for two years. Field plots with runoff collectors had different soil P levels as a result of prior fertilization practices. The treatments for this study were fertilizer application levels and included no fertilizer, nitrogen (N) only, phosphorus (P) only, or both N and P. Runoff volumes were measured and a subsample was saved for dissolved and total P analysis. Phosphorus losses were 0.05% of fertilizer applied for both dissolved and total P. Low mass losses of dissolved P were observed (<0.05 kg ha~(-1) yr~(-1)) and can be attributed to the small amount of precipitation that became runoff. Application of N or P did not affect the amount of runoff from natural or simulated events. Fertilization with N or P increased the concentration of P in the runoff to a similar extent. Soil P levels had no effect on runoff P concentrations or mass losses, despite Morgan extractable soil P levels ranging from 3.7 to 35.6 mg kg~(-1) at the 0-5 cm depth. The simulated events supported the data observed from the natural events in most cases. Significant differences in infiltration rate among treatments were found on 2 of the 6 simulation dates.Significant differences in P loss were only observed when no precipitation fell between a fertilization event and a simulated runoff event. The results of this study suggest that fertilization of established turfgrass does not result in a reduction in runoff volume when visual quality responses to N are similar to those observed in this study. Since increased P runoff concentrations were associated with N and P fertilization, the environmental impacts of turfgrass could be reduced by withholding or limiting N and P fertilizers under these conditions. Soil P level was not a good indicator of P concentration in runoff for this sandy loam and across the range of soil P levels seen in this study. Thus, predictions of runoff P loss based on soil P levels may be misleading or inaccurate for turfgrass areas.
机译:草坪草在城市和郊区占很大比例的土地,因此,重要的是要了解草坪草对地表水质量的影响。在未受干扰的沙质壤土中,从凉爽的草皮草混合物中收集了两年的自然和模拟降雨事件的径流。由于先前的施肥措施,带有径流收集器的田间土壤的磷含量不同。本研究的处理方法为施肥水平,不施肥,仅施氮(N),仅施磷(P)或同时施氮和磷。测量径流量,并保存一个子样本用于溶解和总磷分析。磷的溶解量为总磷的0.05%,溶解磷和总磷的磷损失量为0.05%。观察到溶解磷的质量损失较低(<0.05 kg ha〜(-1)yr〜(-1)),这可归因于降水量少变成了径流。施用N或P不会影响自然或模拟事件的径流量。用氮或磷施肥使径流中磷的浓度增加了相似的程度。尽管在0-5 cm深度处Morgan可提取的土壤P水平范围为3.7至35.6 mg kg〜(-1),但土壤P水平对径流P浓度或质量损失没有影响。在大多数情况下,模拟事件支持从自然事件中观察到的数据。在6个模拟日期中的2个发现处理之间的渗透率存在显着差异。只有在施肥事件和模拟径流事件之间没有降水下降时才观察到P损失的显着差异。这项研究的结果表明,当对N的视觉质量响应与本研究中观察到的相似时,已建立的草皮草的施肥不会导致径流量的减少。由于增加的磷径流浓度与氮和磷的施肥有关,可以通过在这些条件下扣留或限制氮和磷的肥料来减少草皮草对环境的影响。在该研究中,土壤磷水平并不是该砂壤土和整个土壤磷水平范围内径流中磷含量的良好指标。因此,对于草皮草地区,基于土壤磷水平的径流磷损失的预测可能会产生误导或不准确的情况。

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