热带山地雨林CO2浓度环境的时空梯度特征

基于2000年旱、雨季梯度观测结果叠加分析晴及晴间少云天气,山地雨林垂直CO2浓度雨季在333～350ml/m3的时间空间特征显著即800～1800林内16m至冠顶28m,较旱季浓度分别小10～21、7～20.2ml/n3,夜间呼吸影响空间的最大浓度均在近林地上5m、出现时段有季节性差别.800～1800林冠上CO2浓度梯度、气温梯度表明,大气至林冠的CO2通量和冠层指向大气的热通量特征显著,夜间则梯度值减小、方向相反,且雨季晴天的△Ct/△Z大于旱季,旱季气温梯度大于雨季;林内二氧化碳垂直梯度(△Ct/△Z＜0)昼夜均小于零,即林地指向上层的CO2通量特征显著,且两类天气均表现出雨季的浓度梯度大于相应的旱季.从而,科学地揭示出在28m的山地雨林垂直高度上,植物光合固定CO2最多而导致空间浓度最低的季节、天气、时间和空间,同时证实冠上两个高度实时气温与相应CO2浓度成CCO2.=a10b/T.而山地雨林水汽压时空则较为直观地解释了蒸发、扩散和乱流机制影响的效果以及雨林"雨"形成的特征.     

2005-2009年浙江省不同土地类型上空对 流层NO2变化特征

利用OMI(Ozone Monitoring Instrument, OMI)2005年1月 2009年12月对流层NO₂柱浓度月平均值卫星遥感资料以及浙江省2005年1月 2008年3月由NO₂污染指数数据计算得出的地面NO₂日均值质量浓度,分析了浙江省对流层NO₂的时空分布特征和变化趋势;此外,结合由时间序列的MODIS-EVI数据所获取的浙江省土地利用图,分析不同土地利用类型上空对流层NO₂柱浓度的变化差异。研究发现在2005 2009年间,浙江省对流层NO₂柱浓度呈现显著的增长趋势和季节变化特征,其中NO₂柱浓度最高值出现在冬季,最低值出现在夏季。从区域分布来看,对流层NO₂柱浓度的最高值分布在靠近上海大都市的杭州-嘉兴-湖州平原和宁波地区以及人口密集的西部和东部沿海城市区。此外不同土地利用类型上NO₂柱浓度分布差异显著。农田、水体和城市地区NO₂柱浓度较高,其中城市用地上空的NO₂柱浓度明显高于其他土地利用类型上空的NO₂柱浓度;森林上空NO₂柱浓度值最低。NO₂柱浓度逐年增加趋势主要表现为:在农田、水体和城市居民用地类型上空污染严重的NO₂-Ⅰ类别增加显著,而在森林和草地类型上空,则表现为污染较轻的NO₂-Ⅲ类别增加显著。     

低浓度SO2污染与桃蚜的生长和繁殖

用40或80ppbSO₂熏气处理过的油菜饲养桃蚜(Myzus persicae),研究低浓度SO₂污染对这种蚜虫的影响。与对照组相比,两个处理组若蚜的发育速率显著加快,5天内的平均相对生长速率(MRGR)分别增加22.3%和31.5%。成蚜的繁殖力提高40—90%,导致桃蚜种群的内禀增长率(r_m)分别升高17%和27%。比较了桃蚜和其它3种蚜虫对SO₂污染的反应强度,讨论了SO₂污染促进某些植食性昆虫生长的可能原因。     

低浓度SO2对云杉幼苗中碳水化合物代谢的影响研究

研究了低浓度SO₂对云杉幼苗的光合作用速率及碳水化合物代谢的生理生化过程的影响,测定了CO₂摄取速率、幼苗蔗糖含量、蔗糖磷酸合成酶、蔗糖合成酶和转化酶活性及ATP/ADP值.结果表明,低浓度的SO₂(200μg·m^-3)能瞬时刺激幼苗对CO₂的吸收.与对照组相比,幼苗中的蔗糖含量及蔗糖磷酸酶活性明显下降,ATP/ADP处于低水平.因此,在受到SO₂污染形成可见伤害前,幼苗的生理生化过程可能已受到干扰.     

上海市近地面CO2浓度及其与下垫面特征的定量关系

城市化所带来的土地利用变化和化石燃料燃烧对全球碳循环和气候变化产生了深远影响.明确城市区域CO₂浓度的空间变化特征,对于认识和控制温室气体排放、减少人类活动对全球气候变化的影响具有重要意义.本研究以高强度人类扰动和快速城市化背景下的上海市为研究对象,于2014年春季利用近红外气体分析仪Li 840A开展近地面CO2浓度样带监测,结合遥感数据获取的城市下垫面特征信息,在明确上海市近地面CO₂浓度空间分布格局的基础上,进一步定量分析其对城市下垫面特征的响应机制.结果表明： 上海市近地面CO₂浓度为(443.4±22.0) μmol·mol^-1,城市中心CO₂浓度比郊区平均高12.5%(52.5 μmol·mol^-1).近地面CO₂浓度空间异质性显著,呈现西北高、西南次之、东南低的趋势,总体表现为随着下垫面城市化水平的降低而降低. 城市下垫面植被覆盖率(C_Veg)是城市近地面CO₂浓度的重要指示因子,两者呈现负相关;不透水层覆盖率(C_ISA)次之,两者呈正相关.CO₂浓度（C_CO2）与C_ISA及C_Veg的相关性(R²)在缓冲距离为5 km时同时达到峰值,三者之间的定量关系可通过建立逐步回归方程表征：C_CO2=0.32C_ISA-0.89C_Veg+445.13 (R²=0.66, P<0.01).
     

华北平原农田CO2浓度变化特征

旨在了解农田CO₂浓度长期动态变化特征、趋势、浓度增量分布模式等,收集了2007—2018年中国气象局固城生态与农业气象试验站开路式涡相关CO₂浓度观测数据。研究了华北平原农田CO₂浓度的年际、年内、昼夜和CO₂通量等动态变化特征,对比分析了华北平原农田CO₂浓度与城市站和大气本底站CO₂浓度变化趋势及差异。结果表明,近十多年来华北平原农田CO₂年平均浓度显著升高31.0μmol/mol（r=0.263,P<0.01）,年均增幅（2.58μmol/mol）与全球和瓦里关本底站大气CO₂浓度增幅接近,但农田CO₂浓度年际和年内季节变化波动巨大,日平均浓度和逐时平均浓度标准差分别为33.7、33.5μmol/mol。夜间CO₂平均浓度395.8μmol/mol,比白天高36.2μmol/mol（10.1%）,8月最高差值达到74.4μmol/mol（20.6%）。在作物生长季节,5月和8—9月白天CO₂浓度出现的两个谷值准确地对应了CO₂通量动态变化的两个峰值,表明4—9月昼间CO₂浓度和通量动态变化很好地反映了华北平原冬小麦和夏玉米生长过程、农事活动和农田碳交换的关系。农田CO₂浓度动态变化与城市、湿地和大气本底站的变化特征不同,表明其动态变化的形成机制有差异。农田CO₂浓度昼夜及季节变化特征为研究和评估CO₂浓度升高影响作物生长和产量提供指导依据。     

SO2对蚕豆根尖细胞微核的诱导作用

应用蚕豆根尖微核试验,对SO2的遗传毒性效应进行了研究。结果表明：一定浓度范围内（0.108-14.00mg/m^3）,蚕豆根尖微核细胞数与SO2浓度间呈正相关,太原市大气污染严重的冬季采暖期根尖细胞微核率明显高于非采暖期;SO2浓度0.604mg/m^3处理24h和48h或2.80-28.00mg/m^3熏气处理4h可使蚕豆根尖中具有微核的细胞数明显增加,结果表明,低浓度SO2较长时间接触或高浓度短期接触均可引起蚕豆根尖细胞遗传物质的损伤,应用蚕豆根尖细胞微核实验可对大气SO2污染进行生物监测。SO2（2.80-28.00mg/m^3）熏气实验中,接触时间延长能导致根尖细胞微核率下降,2.80mg/m^3熏气组下降较快,14.00mg/m^3熏气组下降较慢,研究结果提示,在运用蚕豆根尖微核实验监测环境SO2污染时要考虑蚕豆的染毒方式,避免假阴性结果的出现。     

SO2体内衍生物诱发蚕豆根尖细胞微核

以蚕豆为材料 ,研究 SO2 体内衍生物 -亚硫酸钠与亚硫酸氢钠混合液 (3:1)对根尖细胞的遗传毒效应。结果表明 :0 .0 5～2 .0 0 mmol/ L的 SO2 衍生物处理可诱发两品种蚕豆根尖中的微核细胞明显增加 ;不同浓度 (0 .0 5～ 15 .0 0 mmol/ L ) SO2 衍生物处理 12、2 4、36 h后 ,根尖微核细胞率是对照组的 2 .5～ 5 .0倍 ,显著高于对照组。在一定浓度范围内 ,蚕豆根尖细胞微核率与SO2 衍生物浓度之间具有正的线性相关。研究结果表明 ,SO2 衍生物能够破坏蚕豆根尖细胞的遗传稳定性。     

在SO2、Cl2污染环境栽培抗性植物的试验研究

<正> 工业生产排放出的有害气体对大气的污染,不但影响人的健康,而且也影响工厂区的植物生长。植物种类不同,对有害气体反应也不一样。通过试验筛选一批对有害气体具有较强抗性的植物,用以绿化工矿区,不仅可保持环境美化,还可以适当减轻大气污染的危害程度。 筛选抗性植物的科学试验程序包括:现场调查,熏气室试验、现场盆栽试验和现场地栽观测。地栽观测的目的在于取得植物在低浓度、长期和高浓度、短期的大气污染条件下的抗性反应和绿化效应的试验资料。     

粤港澳大湾区PM2.5时空分布特征及其与气象要素的关系

细颗粒物（PM_2.5）污染不仅是现代社会城市化进程中的痛点,也是城市大气环境研究不可忽略的重要焦点。粤港澳大湾区作为世界级城市群,既是城市区域经济社会文化发展的重要体现,更是国家区域发展战略的重要构成与政策实施落脚点,其生态环境的优劣尤其受瞩目。对1999-2016年大湾区地表PM_2.5浓度栅格数据集进行了时空分布特征分析,其中空间自相关分析选取莫兰指数（Moran''I指数）作为度量;并利用多元线性回归模型探讨研究区内PM_2.5与气象要素之间关系。结果表明：粤港澳大湾区1999-2016年历年PM_2.5浓度呈先增加后减小的趋势,2008年为时间拐点,该时间节点之后空气质量显著提高,且1999、2009、2016三年,年平均PM_2.5浓度相似值趋于聚集分布。冷热点分析结果表明：热点区域集中于湾区行政核心区域范围内;冷点集中于核心边缘区域,空气质量较优。利用皮尔森相关分析最终筛选出实际蒸散量（aet）、太阳辐射（srad）、最低温度（tmmn）、蒸汽压（vap）、饱和水汽压差（vpd）、风速（ws）等6个气象因子,利用回归分析判断影响PM_2.5浓度时空分布的显著因子。结果表明：本研究区太阳辐射与PM_2.5浓度关系呈负相关,该结果与其他城市相关研究有较大差异,最小温度与PM_2.5浓度呈正相关,风速与PM_2.5浓度呈负相关,饱和水气压差与PM_2.5浓度呈正相关。     

Stomatal SO2 uptake and sulfate accumulation in needles of Norway spruce stands (Picea abies) in Central Europe

Monthly uptake rates and the annual deposition of gaseous SO₂ via the stomata of six Norway spruce canopies (Picea abies (L.) Karst.) in Germany (Königstein im Taunus, Witzenhausen, Grebenau, Frankenberg, Spessart, Fürth im Odenwald) were calculated (i) from statistical response functions of stomatal aperture depending on meteorological data, and (ii) from the synchronously measured SO₂ immission at these stands. The stomatal response functions had been derived on the basis of thorough stomatal water conductance measurements in the field. Calculations of the SO₂ conductance of spruce twigs and SO₂ uptake rates via stomata need continuously measured complete data sets of the (i) light intensity, (ii) air temperature, (iii) air humidity and (iv) SO₂ concentration in spruce forests from all the year. These data were recorded half hourly in different German spruce forests. The apparent needle water vapour pressure difference and transpiration rates were calculated from meteorological data. Additional use of canopy through flow data in dry years allowed the estimation of the mean stomatal conductance for H₂O and SO₂ of whole spruce canopies. The annual SO₂ uptake of a mean unit needle surface in spruce forests was 32% of the SO₂ uptake rate of exposed needles at the top of spruce crowns. There is significant SO₂ uptake all the year. The mean SO₂ dose at all sites and years received through the stomata was (0.25±0.07) mol SO₂ m^-2 (total needle surface) (nPa Pa^-1)^-1 (annual mean of SO₂ immission; 1 nPa (SO₂) Pa^-1 (air) = 1 ppb) day^-1 (vegetation period per year). Comparison of calculated SO₂ uptake rates into needles with measured SO₄ ^2- accumulation rates in needles from the mentioned sites and additionally from Würzburg, Schneeberg (Fichtelgebirge) and from three sites in the eastern Erzgebirge (Höckendorf, Kahleberg, Oberbärenburg) revealed that oxidative SO₂ detoxification (SO₄ ^2- formation) dominates only at sites with high SO₂ immission and short vegetation periods. Under these conditions 70 to 90% of the annual stomatal SO₂ uptake is detoxified via SO₄ ^2- accumulation in needles. Cations are needed for neutralization of accumulating SO₄ ^2- which are inavailable to support growth. Thus, SO₂ induces a dominant and competitive additional nutrient cation demand, cation deficiency symptoms and enhanced needle loss (spruce decline symptoms) mainly at sites, where the ratio R=(SO₂ immission): (length of the vegetation period) is higher than R=0.07 nPa Pa^-1 day^-1. Correlation analysis of the relative needle loss versus the SO₂-dependent SO₄ ^2- formation rate revealed a significant increase of needle loss at the 98% level (Student). At sites with small SO₂ immission and long vegetation periods (R<0.07 nPa Pa^-1 day^-1) reductive SO₂ detoxification via growth (and/or phloem export of SO₄ ^2-) is not kinetically overburdened. Under these conditions only 30% of the annual SO₂ uptake is detoxified via SO₄ ^2- formation and spruce decline is small or absent. On the basis of the critical value R0.07 nPa Pa^-1 day^-1 recommended SO₂ immission limits can be deduced on a mere ecophysiological basis. These deduced values are close to the proposed SO₂ immission limits of the IUFRO, WHO and the UNECE.     

大庆市6种绿化树种对SO2、NO2的消减及滞尘效应

城市森林在吸收、滞留大气污染物,改善城市生态环境方面具有重要意义。以大庆市6种常见绿化树种为研究对象,采用水洗-滤膜法和熏气试验探究不同树种对总悬浮颗粒物(TSP)、大颗粒物(PM_>10)、粗颗粒物(PM_3—10)和细颗粒物(PM_1—3)的滞留规律以及对大气中SO₂、NO₂的消减效果。研究结果表明：(1)不同树种的滞尘能力差异显著(P<0.05),对TSP的滞留量从大到小依次为：油松(3.82±0.40)g/m²>红瑞木(1.45±0.12)g/m²>紫丁香(1.22±0.17)g/m²>梣叶槭(1.21±0.13)g/m²>大叶杨(0.93±0.17)g/m²>旱柳(0.54±0.14)g/m²;(2)树种间对不同颗粒物的滞留量具有显著差异(P<0.05),供试树种对不同粒径颗粒物滞留的质量占比表现...     

NIS/H2SO4-Silica: a mild and efficient reagent system for the hydrolysis of thioglycosides

Chemoselective hydrolysis of a variety of thioglycosides in the presence of a wide range of protecting groups has been achieved by using N-iodosuccinimide and H(2)SO(4) immobilized on silica in good to excellent yields.     

H2SO4-silica-promoted 'on-column' removal of benzylidene, isopropylidene, trityl and tert-butyldimethylsilyl groups

H₂SO₄-silica-promoted removal of benzylidene, isopropylidene, trityl and tert-butyldimethylsilyl groups from sugar derivatives was accomplished by following an ‘on-column’ protocol in a virtually waste-free condition.     

The Impact of Indigenous Microorganisms on the Mineral Corrosion and Mineral Trapping in the SO2 Co-injected CO2-Saline-Sandstone Interaction

The impact of indigenous microorganisms on the mineral corrosion and mineral trapping in the SO₂ co-injected CO₂-saline-sandstone interaction was investigated in this study by lab experiments under 55?°C, 15?M pa. The results verified that co-injection of SO₂ resulted in a decrease in biomass and shifts in microbial communities within 90?days, but some microorganisms still could adapt to acidic, high-temperature, high-pressure, and high-salinity environments. Firmicutes and Proteobacteria remained dominant phylum, but phylum Proteobacteria showed better tolerance to the co-injection of SO₂ in the initial period. In the SO₂ co-injected CO₂-saline-sandstone interaction under microbial mediation, acid-producing bacteria further promoted the corrosion of K-feldspar, albite, and clay minerals, meanwhile mobilizing more K⁺, Na⁺, Ca²⁺, Mg²⁺ into solution. The acidogenic effect may be linked to the dominant genus of Bacillus, Paenibacillus, Acinetobacter, Pseudomonas and Exiguobacterium. Co-injection of SO₂ inhibited the carbonates capture, while microbial acid production further reduced the pH, further inhibiting carbonates capture. As a result, no secondary carbonate (e.g., calcite) was observed on a short time scale within 90?days. So, microbial acidogenic effect was not conducive to carbonates capture in short term.     

Optimization of H2SO4-catalyzed hydrothermal pretreatment of rapeseed straw for bioconversion to ethanol: Focusing on pretreatment at high solids content

A central composite design of response surface method was used to optimize H₂SO₄-catalyzed hydrothermal pretreatment of rapeseed straw, in respect to acid concentration (0.5–2%), treatment time (5–20 min) and solid content (10–20%) at 180 °C. Enzymatic hydrolysis and fermentation were also measured to evaluate the optimal pretreatment conditions for maximizing ethanol production. The results showed that acid concentration and treatment time were more significant than solid content for optimization of xylose release and cellulose recovery. Pretreatment with 1% sulfuric acid and 20% solid content for 10 min at 180 °C was found to be the most optimal condition for pretreatment of rapeseed straw for ethanol production. After pretreatment at the optimal condition and enzymatic hydrolysis, 75.12% total xylan and 63.17% total glucan were converted to xylose and glucose, respectively. Finally, 66.79% of theoretical ethanol yielded after fermentation.     

Synthesis of a tetrasaccharide related to the repeating unit of the O-antigen from Escherichia coli K-12

Synthesis of a tetrasaccharide related to the repeating unit of the O-antigen from Escherichia coli K-12 is reported in the form of its octyl glycoside. Syntheses of the 1,2-cis glycosidic linkages have been accomplished by using NIS in conjunction with H₂SO₄-silica, and it was found to be stereoselective and productive. The synthesized tetrasaccharide will be utilized as the substrate for galactofuranosyltransferase, WbbI.     

Determination of sulphite in mineral soils

Summary Two methods were evaluated to determine the concentration of sulphite in sandy loam soils. Use of p-rosaniline-formaldehyde reagent and sodium tetrachloromercurate as extractant proved effective only if a wide soil to extractant ratio was employed. Use of Ellman's reagent in conjunction with this extractant was however, unsatisfactory. Soils exposed to heavy atmospheric pollution differed in sulphite concentration only marginally compared with relatively unpolluted soils. The effect of soil water content on the stability of sulphite in soil was also determined.     

城市小型景观水体CO2与CH4排放特征及影响因素

淡水生态系统被认为是大气温室气体排放的重要来源,尤其在人类活动影响下,其排放强度可能进一步增强。城市小型景观水体是城市生态系统的重要组成,具有面积小、数量大以及人类干扰强的特征,其温室气体排放特征及影响因素尚不清楚。选择重庆市大学城8个景观水体和周边2个自然水体为对象,于2019年1、4、7、10月,利用漂浮箱和顶空法分析了水体CO₂与CH₄的溶存浓度及排放通量,旨在揭示城市小型景观水体CO₂与CH₄排放强度、时空变异特征以及影响因素。结果表明,10个小型水体CO₂、CH₄的溶存浓度范围分别为10.75-116.25 μmol/L和0.09-3.61 μmol/L（均值分别为（47.6±29.3）μmol/L、（1.13±0.56）μmol/L）,均为过饱和状态;漂浮箱法实测的8个景观水体CO₂和CH₄排放通量均值分别为（72.7±65.9）mmol m^-2 d^-1和（2.31±3.48）mmol m^-2 d^-1（顶空法估算值为（69.7±82.0）mmol m^-2 d^-1和（3.69±2.92）mmol m^-2 d^-1）,是2个自然水体的3.5-6.1和2.0-4.5倍,呈较强的CO₂、CH₄排放源;居民区景观水体CO₂和CH₄排放略高于校园区,均显著高于对照的自然水体;CO₂排放夏季最高,秋季次之,冬、春季最低,CH₄呈夏季>秋季≈春季>冬季的季节模式,温度和水体初级生产共同影响CO₂和CH₄排放的季节模式;水生植物分布对景观水体CO₂、CH₄排放有显著影响,有植物分布的水域比无植物水域平均高1.97和2.94倍;漂浮箱法和顶空法测得气体通量线性关系较好,但顶空法测得CO₂通量在春季明显偏低,而CH₄则普遍偏高。相关分析表明,景观水体碳、氮浓度、pH值以及DO等对CO₂排放具有较好的指示性,CH₄排放通量主要与水体中碳、磷浓度有关。城市小型景观水体CO₂、CH₄排放通量远高于大部分已有自然水体的研究结果,呈一种较强的大气温室气体排放源,在区域淡水系统温室气体排放清单中具有重要贡献,未来研究中应给以更多关注。