固定源排气中氮氧化物的测定

由于没有单独测定二氧化氮的方法标准、二氧化氮标准气体和测定二氧化氮便携式(电化学传感器)仪器标准,目前不能利用标准气体评价二氧化氮便携式(电化学传感器)仪器的性能;但是,可采用将NO2还原成NO后用化学发光法、非分散红外线法或电化学传感器法测定氮氧化物。     

线性扫描溶出伏安法同时测定水样中铅镉铜锌

通过多壁碳纳米管-Nafion复合膜修饰电极,建立水样中痕量铅、镉、铜、锌同时测定的线性扫描溶出伏安分析法,优化支持电解质及pH值、修饰剂用量、富集电位及时间等测定条件。实验结果表明,在pH 4.0的NaAc-HAc缓冲液中,-1.20V富集5min后,在电位-1.04V、-0.72V、-0.45V及-0.16V附近分别产生锌、镉、铅、铜的灵敏溶出峰,测定各元素的线性关系良好,相对标准偏差均小于5.4%。该法已成功应用于实际水样中痕量铅、镉、铜、锌的同时测定,加标回收率在93.3%~106.7%之间,结果满意。     

大气红外辐射超高光谱探测仪临边探测—污染气体的反演精度和光谱通道评估

利用RFM模式,模拟计算了在研仪器—大气红外辐射超高光谱探测仪的临边探测模式下大气污染气体体积混合比的权重函数.结合仪器的可探测亮温阈值（0.3 K）,利用权重函数线性化方法,计算并分析了6种大气状态下,气体混合比廓线在不同反演精度条件下可获得的光谱通道数随切点高度的变化,并给出了可用光谱通道在不同切点高度的位置.结果表明,随着相对反演精度的降低,可用光谱通道数量增加,除热带大气外,其它5种大气在10%臭氧反演精度和5%甲烷反演精度条件下有足够的通道,可用于反演4.6 km以上的混合比廓线.CO在15%反演精度条件下,6种大气均能获得反演6.9 km以上廓线的光谱通道.近地面切点高度反演比较困难,很难获得较高的反演精度.可用光谱通道位置与气体吸收线位置特别是峰值区域一致,也与气体模拟亮温高值区一致.     

Projecting Large-Scale Area Changes in Land Use and Land Cover for Terrestrial Carbon Analyses

One of the largest changes in US forest type areas over the last half-century has involved pine types in the South. The area of planted pine has increased more than 10-fold since 1950, mostly on private lands. Private landowners have responded to market incentives and government programs, including subsidized afforestation on marginal agricultural land. Timber harvest is a crucial disturbance affecting planted pine area, as other forest types are converted to planted pine after harvest. Conversely, however, many harvested pine plantations revert to other forest types, mainly due to passive regeneration behavior on nonindustrial private timberlands. We model land use and land cover changes as a basis for projecting future changes in planted pine area, to aid policy analysts concerned with mitigation activities for global climate change. Projections are prepared in two stages. Projected land use changes include deforestation due to pressures to develop rural land as the human population expands, which is a larger area than that converted from other rural lands (e.g., agriculture) to forestry. In the second stage, transitions among forest types are projected on land allocated to forestry. We consider reforestation, influences of timber harvest, and natural succession and disturbance processes. Baseline projections indicate a net increase of about 5.6 million ha in planted pine area in the South over the next 50 years, with a notable increase in sequestered carbon. Additional opportunities to expand pine plantation area warrant study of landowner behavior to aid in designing more effective incentives for inducing land use and land cover changes to help mitigate climate change and attain other goals.     

Twenty five years of industrial development: a study of resource use rates and macro-efficiency indicators for five Asian countries

Economic and population growth in Asia over the last three decades has been unprecedented. While conventional economic indicators have been increasing consistently, indicators of resource and environmental quality have been deteriorating, raising questions about the implications of future growth. Economic growth in the future is considered to be contingent on ensuring a more efficient use of natural resources, while simultaneously striving to reduce environmental impacts. We examine time trends of three efficiency indicators; agricultural efficiency, energy efficiency of economic production and carbon efficiency of energy use, for the five most populous countries in Asia in order to assess whether industrial development has lead to increased resource use efficiency and an associated reduction in total resource use and environmental impacts. Our results indicate that agricultural efficiency has decreased in all five countries. Results are mixed for energy and carbon efficiencies. Where increases in energy and carbon efficiency have occurred, they have been completely overwhelmed by absolute increases in energy use and carbon emissions caused by increases in the scale of economic activity. Based on this analysis, we study the potential for further improvements and policy implications for future food supply, energy consumption and carbon emissions in the region.     

碳捕集、利用与封存技术商业模式分析

在2060年碳中和目标的要求下,碳捕集、利用与封存技术将扮演重要角色。目前碳捕集、利用与封存技术在中国尚处于工业示范阶段,面临技术成熟度不足、经济成本高、融资渠道单一、应用领域有限、盈利能力差等障碍,迫切需要建立合理的商业模式以推进技术部署。本文梳理了国际上现有的碳捕集、利用与封存商业化项目和相关支持政策,基于商业模式画布的研究框架,分析了碳捕集、利用与封存商业化部署的现状、特点与障碍,并在此基础上提出了相应建议,包括加强技术研发、完善政策体系、布局基础设施和促进集群建设。     

无锡市碳排放的因素分解模型及实证分析

在计算无锡市2000~2011年二氧化碳排放量的基础上,采用对数平均权重Divisia分解法,建立无锡市人均碳排放的因素分解模型,定量分析能源结构、能源效率、经济发展情况等因素对无锡市人均碳排放的影响。结果显示经济发展对拉动无锡人均碳排放的贡献率呈指数增长趋势,相比之下,能源效率及能源结构对碳排放的抑制作用并不明显。据此提出开发可再生能源,转变能源消费结构,发展清洁煤技术,提高能源利用率等对策。     

冬夏季广州城区碳气溶胶特征及其与O_3和气象条件的关联

2008年1月1日～31日和7月1日～31日在广州城区每天采集1个PM2.5样品,对样品进行碳成分分析,得到有机碳(OC)、元素碳(EC)浓度.同步观测了气象因子以及SO2、NO2、O3气态污染物浓度.结果发现,冬季和夏季PM2.5日均值质量浓度分别为(81.2±61.4)μg.m-3和(53.7±23.2)μg.m-3,OC质量浓度分别为(24.6±19.3)μg.m-3和(14.0±5.6)μg.m-3,EC质量浓度分别为(7.9±5.4)μg.m-3和(4.7±2.2)μg.m-3,OC/EC比值分别为2.9±0.6和3.2±1.0.冬夏季非降雨的稳定天气条件下二次有机碳气溶胶(SOC)浓度分别为(6.1±6.6)μg.m-3和(5.8±5.2)μg.m-3.冬夏季SOC和O3浓度显著相关(p0.01).东南风和西南风条件下,OC、EC浓度普遍较高,表明东莞、江门和佛山地区的工业污染源对广州地区污染物累积和霾天气的形成有一定的贡献.     

Spatial variations in CO2 fluxes in a subtropical coastal reservoir of Southeast China were related to urbanization and land-use types

Carbon dioxide (CO2) emissions from aquatic ecosystems are important components of the global carbon cycle, yet the CO2 emissions from coastal reservoirs, especially in developing countries where urbanization and rapid land use change occur, are still poorly understood. In this study, the spatiotemporal variations in CO2 concentrations and fluxes were investigated in Wenwusha Reservoir located in the southeast coast of China. Overall, the mean CO2 concentration and flux across the whole reservoir were 41.85 ± 2.03 µmol/L and 2.87 ± 0.29 mmol/m2/h, respectively, and the reservoir was a consistent net CO2 source over the entire year. The land use types and urbanization levels in the reservoir catchment significantly affected the input of exogenous carbon to water. The mean CO2 flux was much higher from waters adjacent to the urban land (5.05 ± 0.87 mmol/m2/hr) than other land use types. Sites with larger input of exogenous substance via sewage discharge and upstream runoff were often the hotspots of CO2 emission in the reservoir. Our results suggested that urbanization process, agricultural activities, and large input of exogenous carbon could result in large spatial heterogeneity of CO2 emissions and alter the CO2 biogeochemical cycling in coastal reservoirs. Further studies should characterize the diurnal variations, microbial mechanisms, and impact of meteorological conditions on reservoir CO2 emissions to expand our understanding of the carbon cycle in aquatic ecosystems.     

A model on the carbon cycling in Lake Taihu, China

A model of the carbon cycling in Lake Taihu was developed based on the previous developed model EcoTaihu Model, which couples the hydrology, the nutrient cycling and a number of biological processes. The carbon cycling model (abbreviated CCM) has in addition to the states variables of the EcoTaihu Model, the carbon in phytoplankton, zooplankton, fish, macroplant, hydrogen carbonate carbon, carbonate carbon, dissolved carbon, abiotic organic carbon in water, organic carbon in sediment, soluble organic carbon in pore water, inorganic carbon in sediments, soluble inorganic carbon in pore water and pH. The calibration and validation of the CCM showed that the model results are in good accordance with the observations (from the period February17 to December. 5, 2003). It implies that the model can be used to assess the variation of the carbon dioxide flux at the water-air interface, and to find the pH value of the lake water as function of time. According to the model, the carbon dioxide flux at the water-air interface has clear, diurnal variations. Eutrophied water is a sink for the atmospheric carbon dioxide due to the phytosynthesis during the summer. Due to the terrestrial input of carbon to the lake, Lake Taihu is, however, a source of atmospheric carbon dioxide. The total annual flux is almost equal to the terrestrial input of carbon to the lake.