TY - JOUR
T1 - Evidence of organic N deposition and its anthropogenic sources in China
AU - Zhang, Ying
AU - Zheng, Lixia
AU - Liu, Xuejun
AU - Jickells, Tim
AU - Cape, John Neil
AU - Goulding, Keith
AU - Fangmeier, Andreas
AU - Zhang, Fusuo
PY - 2008
Y1 - 2008
N2 - Organic nitrogen (N) is an important component of the atmospheric deposition of reactive N, but its sources are essentially unknown. Assessing whether this dissolved organic N (DON) is of natural, anthropogenic or mixed origin is critically important in attempting to determine the scale of human perturbation of the global N cycle. Here we report evidence for atmospheric organic N deposition and its anthropogenic sources in China. Precipitation samples were collected and analyzed from 15 rural, suburban and urban sites during 2005 and 2006. The average deposition of DON was 8.6 kg ha-1 yr-1 with a volume-weighted concentration of 111 µmol L-1, which was much higher than in other regions of the world. The contribution of DON to total dissolved N (TDN) was approximately 30% on average, agreeing well with other reported data in the literature. Parallel collections of wet-only and bulk deposition showed wet deposition to be 68% on average, indicating a significant dry deposition component. Combining data from the Chinese sites with those from elsewhere in the world, significant (p
AB - Organic nitrogen (N) is an important component of the atmospheric deposition of reactive N, but its sources are essentially unknown. Assessing whether this dissolved organic N (DON) is of natural, anthropogenic or mixed origin is critically important in attempting to determine the scale of human perturbation of the global N cycle. Here we report evidence for atmospheric organic N deposition and its anthropogenic sources in China. Precipitation samples were collected and analyzed from 15 rural, suburban and urban sites during 2005 and 2006. The average deposition of DON was 8.6 kg ha-1 yr-1 with a volume-weighted concentration of 111 µmol L-1, which was much higher than in other regions of the world. The contribution of DON to total dissolved N (TDN) was approximately 30% on average, agreeing well with other reported data in the literature. Parallel collections of wet-only and bulk deposition showed wet deposition to be 68% on average, indicating a significant dry deposition component. Combining data from the Chinese sites with those from elsewhere in the world, significant (p
U2 - 10.1016/j.atmosenv.2007.12.015
DO - 10.1016/j.atmosenv.2007.12.015
M3 - Article
VL - 42
SP - 1035
EP - 1041
JO - Atmospheric Environment
JF - Atmospheric Environment
SN - 1352-2310
IS - 6
ER -