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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Spatial and temporal patterns of nitrogen deposition in China: Synthesis of observational data
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Spatial and temporal patterns of nitrogen deposition in China: Synthesis of observational data

机译:中国氮沉降的时空格局:观测数据综合

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摘要

Anthropogenic nitrous pollutant emissions in China significantly increased during the last decades, which contributed to the accelerated nitrogen (N) deposition. In order to characterize spatial pattern of nitrogen deposition, we employed the kriging technique to interpolate sampling data of precipitation chemistry and ambient air concentration from site-network observations over China. The estimation of wet deposition in China was limited to aqueous NO3 ? and NH4 +, while ambient NO2 was the only species involved in the predicted dry deposition fluxes. To obtain wet deposition fluxes, precipitation concentration was multiplied by 20-year mean precipitation amounts with a resolution of 10 × 10 km. Dry deposition fluxes were products of the interpolated ambient NO2 concentration and deposition velocities modeled for the main vegetation types in China. The total deposition rates of wet and dry deposition peaked over the central south China, with maximum values of 63.53 kg N ha?1 yr?1, and an average value of 12.89 kg N ha?1 yr?1. With ambient NO2 concentration data spanning from the year 1990 through 2003, we detected and evaluated trends in the time series of the annual values of atmospheric NO2 concentration. Significant upward trends at 21 of 102 sites were exhibited, with median percent change of 61.45% over the period 1990–2003. In addition, spatially continuous patterns of dry deposition fluxes based on ambient NO2 measurements in two 5-year phases, 9 years apart, were carried out. On average, there was a rise of 7.66% in NO2 dry deposition during 9 years throughout China.
机译:在过去的几十年中,中国的人为氮氧化物排放量显着增加,这促进了氮(N)的沉积。为了表征氮沉积的空间格局,我们采用了克里格法对来自全国各地站点网络观测的降水化学和环境空气浓度的采样数据进行插值。估计中国的湿沉降仅限于NO3水溶液?和NH4 +,而环境NO2是唯一参与预测的干沉降通量的物质。为了获得湿沉降通量,将降水浓度乘以20年平均降水量,分辨率为10×10 km。干沉降通量是模拟的中国主要植被类型的内插环境NO2浓度和沉降速度的乘积。华南中部地区干湿沉积物的总沉积速率达到峰值,最大值为63.53 kg N ha-1年-1,平均值为12.89 kg N ha-1年-1。利用1990年至2003年的环境NO2浓度数据,我们检测并评估了大气NO2浓度年值时间序列的趋势。在1990年至2003年期间,有102个站点中的21个站点出现了显着的上升趋势,中位百分比变化为61.45%。此外,在两个相隔9年的5年阶段中,根据环境NO2的测量结果,得出了干沉降通量的空间连续模式。在全国范围内,过去9年中,平均NO2干沉降增加了7.66%。

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