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Nitrogen and phosphorous concentrations in runoff from a purple soil in an agricultural watershed

机译:农业流域紫色土壤径流中氮和磷的浓度

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Nutrient loss from purple soils has been reported to increase pollution of the Yangtze River. However, few studies have addressed the variations of nutrient concentration in runoff during natural rainstorms in the regions. Nitrogen and phosphorus concentrations in runoff waters from a small agricultural watershed, in the purple soil region of southwest China, were investigated for four natural rainstorms occurred in a conventional double cropping system (wheat-corn) and another six rainstorms in a new triple cropping system (wheat-corn-sweet potato). The NO concentrations in runoff for the observed rainstorms generally varied from 1.0 to 3.5gmpd, which were noticeably affected by flow rates. A significant logarithmic correlation between NO concentrations and flow rates for each rainstorm was identified. In contrast, the concentrations of NH and dissolved reactive phosphorus (DRP) in runoff fluctuated substantially without a noticeable trend for each rainstorm. Positive linear correlation between the concentrations of DRP and sediment for each rainstorm tested was found under the circumstances of double cropping system. In addition, the ratios of NO to NH for the loss amount in 10 rainstorms varied from 1 to 7 for the triple cropping system and 16-29 for the double cropping system. Furthermore, the ratios of the sum of NO and NH to DRP for the loss amount in 10 rainstorms ranged from 12 to 79 depending on the cropping systems. Nitrate nitrogen was proved to be the main form of inorganic nitrogen loss in runoff water in the purple soil region. Compared with the conventional double cropping system, the new triple cropping system tends to cause more NH loss. These findings would help develop the effective erosion control strategies and select a suitable cropping system to reduce potential pollution hazards.
机译:据报道,紫色土壤的养分流失增加了长江的污染。但是,很少有研究解决该地区自然暴雨期间径流中养分浓度的变化。在中国西南部紫色土壤区域的一个小农业流域,对径流水中的氮和磷浓度进行了调查,调查了常规双作系统(小麦-玉米)中发生的四次自然暴雨,以及新的三作系统中发生的六次暴雨(小麦玉米甜土豆)。对于观测到的暴雨,径流中的NO浓度通常在1.0至3.5gmpd之间变化,这明显受流速的影响。在每次暴雨中,NO浓度和流速之间存在显着的对数相关性。相反,径流中的NH和溶解性活性磷(DRP)的浓度基本没有波动,每次暴雨都没有明显的趋势。在双作制度下,每次暴雨中DRP和沉积物的浓度之间呈正线性关系。此外,在10次暴风雨中,NO与NH的损失量比率在三重种植系统中为1到7,而在二重种植系统中为16-29。此外,根据种植系统的不同,在10次暴风雨中,NO和NH的总和与DRP的损失量之比为12至79。硝酸盐氮被证明是紫色土地区径流水中无机氮损失的主要形式。与传统的双重种植系统相比,新的三次种植系统往往会导致更多的NH损失。这些发现将有助于制定有效的侵蚀控制策略,并选择合适的种植系统以减少潜在的污染危害。

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