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在印度恒河平原及其周边地区,二氧化硫(SO2)、二氧化氮(NO2)和一氧化碳(CO)排放的季节性特征。

Seasonal characteristics of SO2, NO2, and CO emissions in and around the Indo-Gangetic Plain.

机构信息

Space and Atmospheric Sciences Division, Physical Research Laboratory, Navrangpura, Ahmedabad, 380009, India.

出版信息

Environ Monit Assess. 2014 Feb;186(2):1295-310. doi: 10.1007/s10661-013-3458-y. Epub 2013 Oct 5.

Abstract

Anthropogenic emissions of sulfur dioxide (SO2), nitrogen dioxide (NO2), and carbon monoxide (CO) exert significant influence on local and regional atmospheric chemistry. Temporal and spatial variability of these gases are investigated using surface measurements by the Central Pollution Control Board (India) during 2005-2009 over six urban locations in and around the Indo-Gangetic Plain (IGP) and supported using the satellite measurements of these gases. The stations chosen are Jodhpur (west of IGP), Delhi (central IGP), Kolkata and Durgapur (eastern IGP), Guwahati (east of IGP), and Nagpur (south of IGP). Among the stations studied, SO2 concentrations are found to be the highest over Kolkata megacity. Elevated levels of NO2 occur over the IGP stations of Durgapur, Kolkata, and Delhi. Columnar NO2 values are also found to be elevated over these regions during winter due to high surface concentrations while columnar SO2 values show a monsoon maximum. Elevated columnar CO over Guwahati during pre-monsoon are attributed to biomass burning. Statistically significant correlations between columnar NO2 and surface NO2 obtained for Delhi, Kolkata, and Durgapur along with very low SO2 to NO2 ratios (≤0.2) indicate fossil fuel combustion from mobile sources as major contributors to the ambient air over these regions.

摘要

人为排放的二氧化硫(SO2)、二氧化氮(NO2)和一氧化碳(CO)对当地和区域大气化学产生重大影响。本研究使用印度中央污染控制委员会在 2005-2009 年期间在印度恒河平原(IGP)及其周边的六个城市地区进行的地面测量来研究这些气体的时间和空间变化,并利用这些气体的卫星测量结果提供支持。选择的站点是焦特布尔(IGP 以西)、德里(IGP 中心)、加尔各答和杜尔加布尔(IGP 东部)、古瓦哈蒂(IGP 以东)和那格浦尔(IGP 以南)。在所研究的站点中,发现加尔各答大都市的 SO2 浓度最高。NO2 浓度在杜尔加布尔、加尔各答和德里的 IGP 站点较高。由于表面浓度高,冬季这些地区的柱 NO2 值也较高,而柱 SO2 值则显示出季风最大值。在季风前期间,古瓦哈蒂的柱 CO 升高归因于生物质燃烧。在德里、加尔各答和杜尔加布尔获得的柱 NO2 与地面 NO2 之间存在显著的统计相关性,以及非常低的 SO2 与 NO2 比值(≤0.2)表明,这些地区的大气环境中主要来自移动源的化石燃料燃烧。

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