外加气体对等离子体降解CF2ClBr的影响

用等离子体处理难降解大气污染是近国内外产活跃的领域,选用化学方法难解的ＣＦ２ＣｌＢｒ为对象,研究了Ｈｅ,Ｎ２,Ｏ２及空气对等离子体降解ＣＦ２ＣｌＢｒ的影响,实现了ＣＦ２ＣｌＢｒ的常压降解,外加气体为Ｈｅ,Ｎ２时ＣＦ２ＣｌＢｒ的降解情况与纯ＣＦ２ＣｌＢｒ的降解基本相同,外加气体为Ｏ２,空气时的主要降解产物为ＣＦ２Ｏ,Ｂｒ２,Ｃｌ２,外加气体对降糖的影响大小Ｈｅ〈Ｎ２〈Ｏ２空气。     

Heterogeneous oxidation of SO2 by O3-aged black carbon and its dithiothreitol oxidative potential

Ozone (O₃) is an important atmospheric oxidant. Black carbon (BC) particles released into the atmosphere undergo an aging process via O₃ oxidation. O₃-aged BC particles may change their uptake ability toward trace reducing gases such as SO₂ in the atmosphere, leading to different environmental and health effects. In this paper, the heterogeneous reaction process between O₃-aged BC and SO₂ was explored via in-situ diffuse reflectance infrared Fourier transform spectroscopy (DRIFTS). Combined with ion chromatography (IC), DRIFTS was used to qualitatively and quantitatively analyze the sulfate product. The results showed that O₃-aged BC had stronger SO₂ oxidation ability than fresh BC, and the reactive species/sites generated on the surface had an important role in the oxidation of SO₂. Relative humidity or 254 nm UV (ultraviolet) light illumination enhanced the oxidation uptake of SO₂ on O₃-aged BC. The oxidation potentials of the BC particles were detected via dithiothreitol (DTT) assay. The DTT activity over BC was decreased in the process of SO₂ reduction, with the consumption of oxidative active sites.     

华东森林及高山背景区域SO2、NOx、CO本底特征

国家大气背景监测福建武夷山站是中国华东区域背景站点之一,可代表华东森林及高山区域背景状况。为了解该区域的大气背景状况,评估区域污染现状以及污染物输送在区域污染中的作用,选取福建武夷山背景站2011年3月至2012年2月主要气体污染物（SO₂、NO_x、CO）为期1年的监测数据,研究各污染物在不同时间尺度的浓度变化特征和相关关系,以及与气象因子的相关关系,并利用后向轨迹模式探讨区域输送对华东森林及高山背景区域各气体污染物质量浓度的影响。结果表明,武夷山背景点监测期间SO₂、NO_x、CO的平均质量浓度分别为3.9、5.1、409.8 μg/m³,且具有明显的季节变化特征,春、冬季明显高于夏、秋季;三者日变化幅度均很小,呈现出单谷型分布型态,说明武夷山背景点受人为活动的影响很小,主要受气象条件影响;相关性分析结果显示,SO₂与NO_x浓度相关性较好,与湿度有较好的负相关,与风速在冬季具有一定的正相关,NO_x与CO浓度在秋季和冬季的相关性较好,且二者与温度的负相关性较好。后向轨迹分析结果表明,SO₂全年最大浓度峰值主要来自北方采暖季燃煤排放的远距离输送影响,NO_x、CO全年最大值则源于生物质燃烧的远距离输送影响。     

模拟氮沉降和CO2浓度增加对三江平原小叶章群落土壤总有机碳和氮素含量的影响

利用开顶气室(Open-Top Chamber,OTC),设置当前大气CO2浓度(370μmol.mol-1)、中等CO2浓度(550μmol.mol-1)和高CO2浓度(700μmol.mol-1)3个CO2浓度水平和不施氮(N1,0g N.m-2.a-1)、常氮(N2,5g N.m-2.a-1)、高氮(N3,10g N.m-2.a-1)3个氮素水平。研究了不同N沉降水平下,大气CO2浓度升高对以三江平原小叶章群落土壤有机碳和氮素含量的影响。结果表明:CO2浓度升高结合氮沉降连续运行两个生长季后,湿地土壤总有机碳含量没有显著变化,说明较短时间内大气CO2浓度升高和氮沉降不会使三江平原土壤有机碳含量产生变化。氮沉降引起各个土层的土壤全氮、铵态氮和硝态氮的含量增加,施氮水平越高土壤氮增加越多,但是全氮增加量不明显,铵态氮随施氮量的增加呈现极显著差异水平(P<0.01)。0～10cm,10～20cm土层土壤全氮、铵态氮的含量随着CO2浓度升高呈现出先增大后减小的趋势。土壤硝态氮含量在10～20cm土层含量变化与土壤全氮、铵态氮的变化趋势相同。说明大气CO2浓度一定程度的增加可以增加土壤的氮素含量,但是过量的大气CO2浓度反而会使得土壤氮素含量减少。     

Catalytic performance of Fe3O4-CoO/Al2O3 catalyst in ozonation of 2-(2,4-dichlorophenoxy)propionic acid, nitrobenzene and oxalic acid in water

Fe3O4-CoO/Al2O3 catalyst was prepared by incipient wetness impregnation using Fe(NO3) 3·9H2O and Co(NO3) 2·6H2O as the precursors,and its catalytic performance was investigated in ozonation of 2-(2,4-dichlorophenoxy) propionic acid(2,4-DP) ,nitrobenzene and oxalic acid.The experimental results indicated that Fe3O4-CoO/Al2O3 catalyst enabled an interesting improvement of ozonation eciency during the degradation of each organic pollutant,and the Fe3O4-CoO/Al2O3 catalytic ozonation system followed a radical-type mechanism.The kinetics of ozonation alone and Fe3O4-CoO/Al2O3 catalytic ozonation of three organic pollutants in aqueous solution were discussed under the mere consideration of direct ozone reaction and OH radical reaction to well investigate its performance.In the catalytic ozonation of 2,4-DP,the apparent reaction rate constants(k) were determined to be 1.456×10-2 min-1 for ozonation alone and 4.740×10-2 min-1 for O3/Fe3O4-CoO/Al2O3.And O3/Fe3O4-CoO/Al2O3 had a larger Rct(6.614×10-9) calculated by the relative method than O3 did(1.800×10-9) ,showing O3/Fe3O4-CoO/Al2O3 generated more hydroxyl radical.Similar results were also obtained in the catalytic ozonation of nitrobenzene and oxalic acid.The above results demonstrated that the catalytic performance of Fe3O4-CoO/Al2O3 in ozonation of studied organic substance was universal to a certain degree.     

草地退化对三江源区高寒草甸生态系统CO2通量的影响及其原因

为了揭示草地退化对三江源地区高寒草甸生态系统碳通量的影响,利用涡度相关技术,于2006年12月1日~2007年11月30日对三江源地区的退化高寒草甸生态系统的碳通量及生物和环境因子进行观测.结果发现:草地退化对高寒草甸生态系统的碳通量产生了深刻影响,与未退化的高寒草甸生态系统相比,退化高寒草甸生态系统全年总初级生产力(GPP)下降了36.6%,全年生态系统呼吸(Reco)下降了7.9%,全年净生态系统CO2交换(NEE)也由退化前的负值(碳吸收)转变为正值(碳排放),二者相差132.5gC/(m2·a),生态系统由原来的碳汇转变为目前的碳源.这些变化与高寒草甸退化后,生态系统植物地上生物量锐减、植物生长期缩短(NEE<0的天数)、植物多样性下降、土壤含水量降低等因素密切相关.     

Contrasting responses of seed yield to elevated carbon dioxide under field conditions within Phaseolus vulgaris

The rising concentration of carbon dioxide [CO₂] in the atmosphere represents an increase in a growth-limiting resource for C₃ crop species. Identification of lines or characteristics of lines which have superior yield at elevated [CO₂] could aid in adaptation to this global change. While intraspecific variation in responses to elevated [CO₂] has been found in several species, intraspecific differences in crop yield responses to elevated [CO₂] under field conditions have seldom been documented. In this 4-year study, the responses of photosynthesis, growth, pod number, seed number and size, and seed yield to the elevation of [CO₂] to 180 μmol mol⁻¹ above the current ambient concentration were examined in four varieties of Phaseolus vulgaris in the field, using open-top chambers. There was a significant variety by [CO₂] interaction for seed yield, with seed yield at elevated [CO₂] ranging from 0.89 to 1.39 times that at ambient [CO₂] (mean 1.17×) in the different varieties, when averaged over 4 years. The highest yielding variety at elevated [CO₂] was not the highest yielding variety at ambient [CO₂]. The varieties with the largest and smallest yield responses both had an indeterminate growth habit. Down-regulation of photosynthesis at elevated [CO₂] only occurred in the two indeterminate varieties, and there was no significant correlation between the response of single leaf photosynthetic rate and the response of seed yield to elevated [CO₂] among varieties, nor between the responses of stem mass and seed yield. The change in the number of pods at elevated [CO₂] was the primary determinant of the response of seed yield. These results indicate that significant variation in the response of seed yield to elevated [CO₂] under field conditions does exist among varieties of P. vulgaris, and that variation in the response of pod and seed number may be more important than variation in photosynthetic response.     

青海湖东北岸天然草地CO2 通量变化特征

采用涡度相关法对青海湖东北岸地区草甸化草原生态系统的CO₂ 通量进行了观测,结果表明： 在生长季节(5~9 月),就日变化,08:00~19:00 为CO₂ 净吸收,20:00~07:00 为CO₂ 净排放,CO₂ 通量 净吸收峰值一般出现在12:00 时,7 月份12:00 时CO₂ 净吸收峰值为1.41 g·(m2·h)^-1;就月变化,7 月 是生长季CO₂ 净吸收最高月份,月CO₂ 净吸收量达到162.70 g·m^-2,整个生长季CO₂ 净吸收的总量达 468.07 g·m^-2。非生长季节(1~4 月及10~12 月),CO₂ 通量日变化振幅极小,最大CO₂ 净排放通量出现 在3 月,为0.29 g·(m2·h)^-1,除12 月和1 月各时段CO₂ 通量接近于零,其余月份各时段CO₂ 净排放在 0.02~0.29 g·(m2·h)^-1;3 月是全年CO₂ 净排放的最高月份,全月CO₂ 净排放量为72.33 g·m^-2,整个非生 长季CO₂ 净排放为319.78 g·m^-2。结果表明,无放牧条件下青海湖东北岸地区草甸化草原,全年CO₂ 净吸收量达148.30 g·m^-2,是显著的CO₂ 汇。