大气氨的多相测量

S.P Singh, G.S Satsangi, P Khare, A Lakhani, K Maharaj Kumari, S.S Srivastava
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引用次数: 42

摘要

在印度郊区对气相、微粒和雨中的氨进行了测量。气相浓度在0.97 ~ 25.5 μg m−3 (57.1 ~ 1500.0 nmol m−3)之间变化,日变化研究表明,NH3浓度在夜间较高,在0600 h(清晨)最低。颗粒相NH4值在1.2 ~ 5.3 μg m−3 (66.7 ~ 294.4 nmol m−3)之间。干沉积通量由模型计算确定。白天NH3通量为8.4±4.0 mg m−2 d−1,夜间NH3通量为2.2±1.2 mg m−2 d−1。颗粒沉降通量为0.2±0.1 mg m−2 d−1,而降水NH4值为0.7 ~ 74.4 μeq l−1。铵态氮浓度随降雨量和沉降量的回归分析表明,铵态氮浓度同时受气体铵和颗粒铵的控制。湿沉积和干沉积的年输入分别为0.34±0.3和3.9±1.9 g m−2 y−1。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Multiphase measurement of atmospheric ammonia

Measurement of ammonia in vapour phase, particulate and rain was made at a suburban site of India. Vapour phase concentrations varied between 0.97 and 25.5 μg m−3 (57.1–1500.0 nmol m−3) and diurnal variation study showed high concentration of NH3 during night time and minimum at 0600 h (early morning). Particulate phase NH4 values ranged between 1.2 and 5.3 μg m−3 (66.7–294.4 nmol m−3). Dry deposition flux was determined from model calculations. Day time NH3 flux was found to be 8.4±4.0 mg m−2 d−1 and that of night 2.2±1.2 mg m−2 d−1. With respect to particulate deposition flux was found 0.2±0.1 mg m−2 d−1 while in precipitation values of NH4 ranged between 0.7 and 74.4 μeq l−1. Regression analysis of ammonium concentration with rain volume and deposition indicates that NH3 concentration is being controlled by both gas and particulate ammonium. Annual inputs for wet and dry deposition were found to be 0.34±0.3 and 3.9±1.9 g m−2 y−1.

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