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首页> 外文期刊>Soil Research >Phosphorus loss and speciation in overland flow from a plantation horticulture catchment and in an adjoining waterway in coastal Queensland, Australia.
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Phosphorus loss and speciation in overland flow from a plantation horticulture catchment and in an adjoining waterway in coastal Queensland, Australia.

机译:在澳大利亚昆士兰州沿海的种植园集水区和毗邻的水道中,磷流失和形态变化。

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Phosphorus (P) in overland flow from horticulture farms in coastal Queensland, Australia, could eutrophy coastal freshwater and marine habitats environments nearby. The potential for such eutrophication was investigated in a coastal macadamia plantation under commercial production. During the 13-month study, P losses in overland flow were quantified in a 0.24-ha farm catchment with a 3.1% gradient, during five consecutive storm events. These events were within expected short- and long-term episodic rainfall frequencies and intensities. Runoff occurred when such storms generated between 20-40 mm/h of rainfall for >9 min. Calculated annual losses of total P were 0.32kg/ha.year, comprising dissolved inorganic P (DIP, 0.28 kg/ha.year), particulate P (0.03 kg/ha.year), and dissolved organic P (0.01 kg/ha.year). DIP represented 88% of all losses and this was attributed to excessive fertilisation and untimely applications. Losses of total P were generally higher than those reported in comparable studies. Concentrations of DIP in runoff were 20-200-fold higher than those found in other coastal catchments in Queensland. High concentrations of DIP were present in the topsoil of the non-fertilised, inter-row areas of the farm catchment and this was attributed to transfer and deposition of DIP from adjacent fertilised tree beds during storm flow. Therefore, it can be expected that farm runoff will be enriched with DIP from these areas for an indeterminate period despite any future remediation to fertiliser management. The weighted average of DIP in farm runoff was 2.01 mg/L, whereas it was 0.005 mg/L in a catchment stream bordering the farm, showing a steep concentration gradient between the two ecosystem compartments. Together with nitrogen (N) losses in runoff, reported previously, an N:P molar ratio of 2:1 was contained in the farm runoff. This was well below the growth-limiting threshold for aquatic organisms, as determined by the Redfield ratio of 16:1 (N:P). The entry of nutrient-enriched farm runoff, as detailed in this study, into the catchment stream and the proximity of such waterways (8 km) to the coastline may also have implications for the near-shore (oligotrophic) marine environment during periods of storm flow. Altogether, this work revealed the high risk of eutrophication from farming landscapes such as the one under study.
机译:来自澳大利亚昆士兰州沿海的园艺农场的陆上磷流失,可能使附近的沿海淡水和海洋栖息地环境富营养化。在商业生产的沿海澳洲坚果种植园中研究了这种富营养化的潜力。在为期13个月的研究中,在连续五次暴风雨事件中,以0.23公顷的农场集水量以3.1%的梯度量化了陆流中的磷损失。这些事件在预期的短期和长期情景降雨频率和强度之内。当此类风暴在20-40 mm / h的降水量下持续9分钟以上时,就会发生径流。计算得出的总磷的年度损失为0.32kg / ha.year,包括溶解的无机P(DIP,0.28 kg / ha.year),颗粒P(0.03 kg / ha.year)和溶解的有机P(0.01 kg / ha)。年)。 DIP占所有损失的88%,这归因于过度施肥和不及时施肥。总磷的损失通常高于可比研究中报告的损失。径流中DIP的浓度比昆士兰州其他沿海流域的DIP浓度高20-200倍。农田流域非受精行间区域的表层土壤中存在高浓度的DIP,这归因于暴风雨期间DIP从相邻的施肥树床上转移和沉积。因此,可以预见,尽管将来对肥料管理有任何补救措施,但在不确定的时期内,这些地区的DIP将使农场径流得到丰富。农场径流中DIP的加权平均值为2.01 mg / L,而在与农场接壤的集水径流中的DIP加权平均值为0.005 mg / L,表明两个生态系统区室之间的浓度梯度陡峭。连同先前报道的径流中的氮(N)损失,农场径流中的N:P摩尔比为2:1。这远低于水生生物的生长限制阈值,该阈值由雷德菲尔德比率16:1(N:P)确定。如本研究所述,富含营养的农场径流进入集水区,且此类水道(8公里)靠近海岸线,这也可能对风暴期间的近岸(贫营养)海洋环境产生影响。流。总体而言,这项工作揭示了农业景观(如所研究的景观)富营养化的高风险。

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