Recent decreases in fossil-fuel emissions of ethane and methane derived from firn air

Methane and ethane are the most abundant hydrocarbons in the atmosphere and they affect both atmospheric chemistry and climate. Both gases are emitted from fossil fuels and biomass burning, whereas methane (CH(4)) alone has large sources from wetlands, agriculture, landfills and waste water. Here we use measurements in firn (perennial snowpack) air from Greenland and Antarctica to reconstruct the atmospheric variability of ethane (C(2)H(6)) during the twentieth century. Ethane levels rose from early in the century until the 1980s, when the trend reversed, with a period of decline over the next 20?years. We find that this variability was primarily driven by changes in ethane emissions from fossil fuels; these emissions peaked in the 1960s and 1970s at 14-16 teragrams per year (1?Tg = 10(12)?g) and dropped to 8-10?Tg yr(-1) by the turn of the century. The reduction in fossil-fuel sources is probably related to changes in light hydrocarbon emissions associated with petroleum production and use. The ethane-based fossil-fuel emission history is strikingly different from bottom-up estimates of methane emissions from fossil-fuel use, and implies that the fossil-fuel source of methane started to decline in the 1980s and probably caused the late twentieth century slow-down in the growth rate of atmospheric methane.     

铑催化剂上CO的吸附态及其加氢反应

用红外光谱法测定表明：各种硅胶负载仲进型铑催化剂上，线ＣＯ／桥ＣＯ红外吸收强度比值与金属助剂（Ｍ）的关系变化顺序为（５０：１）（Ｒｈ－Ｍｎ）〉（２２：１）（Ｒｈ－Ｌｉ）〉（９．１：１）（Ｒｈ－Ｍｎ－Ｆｅ－Ｌｉ）〉（３．５：１）（Ｒｈ－Ｆｅ）〉２．８：１）（Ｒｈ）。在各种Ｒｈ－Ｍ／ＳｉＯ２催化剂上，线、桥ＣＯ吸附态的加氢原位ＦＴＩＲ跟踪实验表明：随着加氢的进行，线ＣＯ／桥ＣＯ吸收强度比值均逐渐减少…