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Land use effect and hydrological control on nitrate yield in subtropical mountainous watersheds

机译:亚热带山区流域土地利用效应与水文控制对硝酸盐产量的影响

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Nitrate export in small subtropical watersheds is rarely observed and the estimation of individual land use nitrate yield from a mixed combination within catchments has scarcely been studied. In this study the nitrate concentrations at 16 nested catchments in the Chi-Chia-Wan watershed in Central Taiwan were measured during 2007-2008. A 3-layer TOPMODEL was applied to estimate daily discharge for ungauged sub-catchments. The observed nitrate concentrations and the simulated discharges were used for nitrate flux estimations through four flux methods. Meanwhile, a new deconvolution computation was developed to resolve the nitrate yield of each land use from within the mixed combinations. The results showed that the observed mean NO _3-N concentration in relatively pristine catchments was approximately 0.145 ± 0.103 mg l ~(-1), which is comparable with other forestry catchments around the world. However, the higher rainfall/runoff, substantial N deposition, and other nitrogen sources resulted in significantly higher annual export of approximately 238-1018 kg-N km ~(-2) yr ~(-1). Our deconvolution computation showed that the background yield of natural forestry was ~351 ±62 kg-N km ~(-2) yr ~(-1). On the other hand, the extremely high nitrate yield of active farmland was ~308, 170 ± 19 241 kg-N km ~(-2) yr ~(-1) due to over-fertilization. The deconvolution computation technique is capable of tracing the mixed signals at the outlet back to the nitrate productions from varied land use patterns. It advances the application of river monitoring network. The typical values of nitrate yields can serve as a guideline for land management. Comparing the nitrogen input and output, we found some nitrogen missing in the cycling which may indicate certain removal processes and we therefore suggest further study to be carried out to fully understand nitrogen cycling in subtropics.
机译:很少观察到亚热带小流域的硝酸盐出口,并且几乎没有研究过流域内混合组合对单个土地利用硝酸盐产量的估算。在这项研究中,对2007年至2008年台湾中部Chi-Chia-Wan流域16个嵌套集水区的硝酸盐浓度进行了测量。应用3层TOPMODEL估算未排水子集水区的日排放量。通过四种通量方法,将观察到的硝酸盐浓度和模拟排放量用于估算硝酸盐通量。同时,开发了一种新的反卷积计算,以解决混合组合中每种土地利用的硝酸盐产量。结果表明,在相对原始的流域中观察到的平均NO _3-N浓度约为0.145±0.103 mg l((-1)),与世界上其他林业流域相近。但是,较高的降雨/径流,大量的氮沉积和其他氮源导致每年的出口量大大增加,约为238-1018 kg-N km〜(-2)yr〜(-1)。我们的反卷积计算表明,天然林的背景产量为〜351±62 kg-N km〜(-2)yr〜(-1)。另一方面,由于过度施肥,活跃农田的硝酸盐产量极高,约为〜308,170±19 241 kg-N km〜(-2)yr〜(-1)。去卷积计算技术能够将出口处的混合信号从各种土地利用方式追溯到硝酸盐生产。它促进了河流监测网络的应用。硝酸盐单产的典型值可以作为土地管理的指南。比较氮的输入和输出,我们发现循环中缺少一些氮,这可能表明某些去除过程,因此,我们建议进行进一步研究以充分了解亚热带的氮循环。

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