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Losses of nitrogen in surface runoff from a plantation horticulture farm in coastal Queensland, Australia

机译:澳大利亚昆士兰州沿海的一个园艺园地表径流中的氮损失

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Surface losses of nitrogen from horticulture farms in coastal Queensland, Australia, may have the potential to eutrophy sensitive coastal marine habitats nearby. A case-study of the potential extent of such losses was investigated in a coastal macadamia plantation. Nitrogen losses were quantified in 5 consecutive runoff events during the 13-month study. Irrigation did not contribute to surface flows. Runoff was generated by storms at combined intensities and durations that were 20-40 mm/h for >9min. These intensities and durations were within expected short-term (1 year) and long-term (up to 20 years) frequencies of rainfall in the study area. Surface flow volumes were 5.3pl1.1% of the episodic rainfall generated by such storms. Therefore, the largest part of each rainfall event was attributed to infiltration and drainage in this farm soil (Kandosol). The estimated annual loss of total nitrogen in runoff was 0.26kgN/ha.year, representing a minimal loading of nitrogen in surface runoff when compared to other studies. The weighted average concentrations of total sediment nitrogen (TSN) and total dissolved nitrogen (TDN) generated in the farm runoff were 2.81pl0.77% N and 1.11pl0.27mgN/L, respectively. These concentrations were considerably greater than ambient levels in an adjoining catchment waterway. Concentrations of TSN and TDN in the waterway were 0.11pl0.02% N and 0.50pl0.09mgN/L, respectively. The steep concentration gradient of TSN and TDN between the farm runoff and the waterway demonstrated the occurrence of nutrient loading from the farming landscapes to the waterway. The TDN levels in the stream exceeded the current specified threshold of 0.2-0.3mgN/L for eutrophication of such a waterway. Therefore, while the estimate of annual loading of N from runoff losses was comparatively low, it was evident that the stream catchment and associated agricultural land uses were already characterised by significant nitrogen loadings that pose eutrophication risks. The reported levels of nitrogen and the proximity of such waterways (8km) to the coastline may have also have implications for the nearshore (oligotrophic) marine environment during periods of turbulent flow.
机译:来自澳大利亚昆士兰州沿海的园艺农场的氮表面损失可能使附近的沿海海洋生境富营养化。在沿海澳洲坚果种植园中调查了此​​类损失的潜在程度的案例研究。在为期13个月的研究中,连续5次径流事件中对氮损失进行了量化。灌溉没有促进地表水流。暴风雨以联合强度和持续时间为20-40 mm / h持续9分钟以上的时间产生径流。这些强度和持续时间在研究区域预期的短期(1年)和长期(最多20年)降雨频率范围内。地表流量为此类暴风雨所产生的偶发性降雨的5.3pl1.1%。因此,每个降雨事件的最大部分归因于这种农田土壤(Kandosol)的渗透和排水。估计年径流中总氮的年度损失为0.26kgN / ha.year,与其他研究相比,这表示地表径流中的氮负荷最小。在农场径流中产生的总沉积物氮(TSN)和总溶解氮(TDN)的加权平均浓度分别为2.81pl0.77%N和1.11pl0.27mgN / L。这些浓度大大高于相邻集水道中的环境浓度。水道中TSN和TDN的浓度分别为0.11pl0.02%N和0.50pl0.09mgN / L。农场径流与水道之间的TSN和TDN浓度梯度陡峭,说明了从耕作景观到水道的养分负荷发生。溪流中的TDN含量超过了该水道富营养化的当前指定阈值0.2-0.3mgN / L。因此,尽管从径流损失估算的年度氮含量相对较低,但很明显的是,河流集水区和相关的农业用地已经以大量氮肥为特征,这构成了富营养化的风险。在湍流期间,所报告的氮含量以及此类水道与海岸线之间的距离(8公里)也可能对近岸(贫营养)海洋环境产生影响。

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