Liu Xue-Yan, Xiao Hua-Yun, Liu Cong-Qiang, Li You-Yi, Li Lin
State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China.
Huan Jing Ke Xue. 2008 Jul;29(7):1785-90.
Tissue N concentration and delta15 N signature in epilithic mosses were investigated along 4 directions from urban area to rural area at Guiyang city. Mosses N concentration ranged from 0.85% to 2.97% and showed significant decrease from urban area (2.24% +/- 0.32%) to suburb (1.27% +/- 0.13%), reflecting the level of atmospheric N deposition decreased away from urban. While slightly higher tissue N re-emerged at rural area beyond 25km (mean = 1.33%-1.75%), suggesting increased N deposition occurred in the rural area. Mosses delta15 N values varied from - 12.50 per thousand to - 1.39 per thousand characterized with getting less negative from urban to rural area. More negative delta15 N signatures of urban mosses (mean= - 8.87 per thousand(-) - 8.59 per thousand) mainly indicated the extensive NH3 sources released from excretory wastes and sewage, while mosses growing at farther suburb or rural area had less depleted delta15 N values (mean = - 3.83 per thousand(-) - 2.48 per thousand), indicating the large sources of agricultural NH3 emission connected with fertilizer application. Moreover, the pattern of mosses delta15 N variation in this study was opposite to areas where N deposition was dominated by oxidized form N (NO(x)) with generally positive mosses delta15 N. Accordingly, we concluded that reduced NH, was the dominant N form in atmospheric deposition at Guiyang area, which would be of great value for understanding the spatial variation and sources of atmospheric N deposition.
在贵阳市,沿着从市区到农村的4个方向,对附生苔藓中的组织氮浓度和δ15N特征进行了调查。苔藓的氮浓度范围为0.85%至2.97%,从市区(2.24%±0.32%)到郊区(1.27%±0.13%)显著降低,反映出大气氮沉降水平随着远离城市而降低。而在距离市区超过25公里的农村地区,组织氮含量略有回升(平均值 = 1.33%-1.75%),表明农村地区的氮沉降有所增加。苔藓的δ15N值在-12.50‰至-1.39‰之间变化,其特征是从城市到农村变得不那么负。城市苔藓的δ15N特征更负(平均值 = -8.87‰至-8.59‰),主要表明排泄物和污水中释放出大量氨源,而生长在更远郊区或农村地区的苔藓,其δ15N值贫化程度较低(平均值 = -3.83‰至-2.48‰),表明与肥料施用相关的农业氨排放源较大。此外,本研究中苔藓δ15N的变化模式与以氧化态氮(NO(x))为主的氮沉降地区相反,后者苔藓的δ15N通常为正值。因此,我们得出结论,还原态氨是贵阳地区大气沉降中主要的氮形态,这对于理解大气氮沉降的空间变化和来源具有重要价值。