基于ARIMA和BP神经网络组合模型的我国碳排放强度预测

预测我国碳排放强度的长期变动趋势, 对国家进行宏观经济管理和节能减排工作具有重要的参考价值。运用深入分析自回归移动平均模型和神经网络的特性,并在此基础上建立ARIMA模型和BP神经网络组合模型,将碳排放强度的时间序列的数据结构分解为线性和非线性残差部分,对我国碳排放强度的变化趋势进行了综合分析与预测。结果显示:今后10 a我国碳排放强度总体是逐步下降的,但到2020年我国碳排放强度仅比2005年下降34%,比我国政府提出碳排放强度下降40%~45%的目标还有一定的差距。因此,要在2020年实现我国碳排放强度目标,必须要调整宏观经济政策,采取各种政策措施以实现目标     

特大型城市客运交通碳排放与减排对策研究

本文基于对现有城市交通碳排放测算方法的比较分析,以上海市为例,采用IPCC"自下而上"法对特大型城市客运交通CO2排放进行了测算,结果显示:轨道交通是碳排放效率最高的客运方式,出租车最低;客运交通CO2排放总量增长迅速,且碳源结构发生了较大变化;近年客运交通CO2排放增量主要来自私人载客汽车,同时公务交通在客运交通碳排放中始终占较大比重。由此本文认为,控制客运交通碳排放的关键在于对以私人载客汽车和单位载客汽车为主的个体交通的管理和控制,形成以公共交通为主的交通结构。在此基础上,为了将控制碳排放纳入到城市交通政策目标中去,本文就主要城市交通政策对客运交通碳排放产生的影响进行了深入分析,并得出结论:以往的交通供给、需求管理政策对于抑制客运交通碳排放增长的作用有限;而就目前城市空间发展政策的实施效果而言,也不利于降低居民出行的碳排放水平。文章最后分别从交通供给、需求管理以及城市空间角度给出了控制客运交通碳排放的对策。     

中国西北寒旱区农牧民生活碳排放评估

围绕碳排放权开展的气候谈判愈来愈关注贫困人口与弱势群体的生存权与发展权,一方面由于受制于其薄弱的社会经济水平,贫困人口与弱势群体在气候变化实践中表现出更高的脆弱性,另一方面则因气候变化减缓与适应行动而造成的贫困人口生活成本的增加以及生活水平的下降。然而,对这些地区和人口的排放权判断主要基于国家层面和地区层面宏观数据的分析,其结果掩盖了国家和地区内部不同社会经济水平下的人口排放差异,不能准确揭示贫困人口和脆弱群体的低碳排放事实。本文基于国际碳排放评估对人口生活排放的需求,结合IPCC参考方法,利用投入产出分析模型构建了人口生活碳排放评价指标体系,并用于对甘肃、青海和宁夏干旱-高寒地区农牧民生活碳排放的样本调查和分析。评估表明,中国西北干旱—高寒区人口生活碳排放仅为1.85tCO2/人,其中用于满足基本生活需要的碳排放量达到87.25%。研究发现,生活在更冷(海拔更高)区域内的人口生活排放量更高;随着家庭收入的增长,人口生活排放量也随之上升;家庭成员数量越多,家庭的人均碳排放量就会越低。     

低碳沼气工程建设的生态经济效益核算研究——以广西恭城瑶族自治县为例

在全球气候变暖和快速城市化的背景下,农村地区是能源集约消耗的薄弱区域,其经济、社会、生态的可持续发展一直受到制约。沼气工程作为一种清洁用能方式,在优化用能结构、减少环境污染、节约自然资源、增加农民收入和促进农村经济转型等方面具有较大优势。本文选择广西恭城瑶族自治县这一沼气工程建设全国示范县为案例,针对户用8m3沼气池,对施工建设、运营维护和消费利用全生命周期过程中的碳足迹、减排效益、经济收益和生态价值方面进行核算和评价。结果表明在沼气池的建设与正常使用年限内,该县农户通过替代燃煤、柴薪和秸秆等共可减排CO2约1.24×106t。从户用沼气池建设及生产过程的投入产出价值的来看,仅通过节约炊事燃料和沼液沼渣的回收利用就能为每户节约19 877元,为全县带来1.26亿余元的总收益。因此,沼气工程在该地区的建设普及是发展农村低碳经济、走富农之路的有效措施,可为广大西部地区新农村建设提供借鉴。     

Comprehensive Appraisal of Provincial Low Carbon Development： A Case Study of China

In this research,the Factor Analysis model of measuring provincial low carbon development in China has been constructed.Based on data from 30 provinces,an empirical study was developed to measure comprehensive low carbon development using the Factor Analysis model(Principal Components method and Normalized Varimax Rotation).The results reveal that the provincial marks of low carbon development are generally low and only nine provinces have high marks(more than 0.80).The results also show significant regional disparity.The provincial marks of the eastern region are higher than both the middle and western provinces of mainland China.All of the provinces with high marks(more than 0.90) are located in the eastern region,and those with the lowest marks(0.60) are located in the middle region.Furthermore,regional disparity in low carbon development follows the same pattern as economic development in China.Finally,some suggestions for decision-makers are presented.     

含外来电的崇明县能源碳排放核算研究

能源消耗是中国最主要的碳排放源,而地方政府是碳管理的基层行政单元,因此,有效控制区域的能源碳排放是碳减排工作的重中之重。区域消耗的能源中,外来电是缓解当地用电压力的重要措施,但一般外来电引起的碳排放易被忽视。将外来电导致的碳排放纳入区域能源碳排放核算体系内,利用部门分析和范围分析法建立了包含外来电分析的能源碳排放核算系统,以上海市崇明县为例进行了应用。研究表明：（1）2000～2009年崇明的能源碳排放增长较快,由181万t增至477万t（CO2当量）;(2）碳排放总量的8212%来自3个部门：工业、建筑业和生活部门;(3）2009年,购买电力导致的间接碳排放达2316%,体现了实施碳管理时考虑外来电力的必要性     

湖南省碳源与碳汇变化的时序分析

在全球气候变暖的背景下,减少温室气体排放、发展低碳经济成为各地区在发展中的普遍共识。以湖南省为研究区域,以1995~2008年为研究时序,从能源消费、主要工业产品生产工艺过程、土地利用变化与牲畜管理、固体废弃物处理与废水处理和排放4个方面综合分析了碳源与碳汇的变化情况。研究表明:1995~2008年,湖南省温室气体排放总量约在220亿t（2000年）至399亿t（2008年）CO2当量之间,14 a间增长了6118%,年均增长374%;碳汇总量约在1754亿t（1995年）至2537亿t（2007年）CO2当量之间,14 a间增长了3607%,年均增长约240%;能源消费与农业部门是湖南省温室气体的主要来源,林地是湖南省碳汇的主要来源;综合碳源与碳汇变化的均衡结果,1995~2008年湖南省呈碳汇盈余状态,净碳汇在2001~2007年持续增加,14 a间增长了31.94%,年均增长2.15%     

CFRP加固高强混凝土梁锚固方式试验研究

高强混凝土梁受拉底面粘贴补强纤维布后,延性降低显著。为提高补强梁的综合性能,利用四点弯曲梁静载试验,在补强加固梁梁端及跨中实施不同的锚固方式,对比不同锚固组合下加固梁的强度和延性。研究表明:端部U锚能改善加固梁破坏模式,提高加固梁的延性和强度及补强纤维布的利用率。端部U锚联合跨中全包锚固能进一步提高加固梁的延性,显著提高补强纤维布的利用率,且能平衡变形性和承载力在安全储备中的比重;在补强纤维布断裂后,能有效限制补强纤维布的剥离和滑移,继续发挥补强作用,使加固梁延性和强度得以恢复;能对包裹区混凝土产生约束作用,提高混凝土的延性。因此端部U锚联合跨中全包锚固是合理且有充分安全储备的锚固方式。     

Role of black carbon in the distribution of polychlorinated dibenzo-p-dioxins/dibenzofurans in aged field-contaminated soils

Floodplain soils containing elevated levels of polychlorinated dibenzo-p-dioxins/dibenzofurans (PCDD/Fs) were collected from several locations along the Tittabawassee River (Michigan, USA). The PCDD/F profiles of these soils exhibited distinct congener patterns consistent with byproducts from either chloralkali manufacturing or chlorophenols productions. Black carbon (BC) particles were isolated for the first time from floodplain soil impacted by PCDD/Fs. Petrographic analysis showed that BC particles, including coal, oxidized coal, metallurgical coke, depositional carbon, coal tar/pitch, cenosphere, and charcoal, comprised approximately 30% by volume of the organic fraction with size range of 250 μm-2000 μm from a typical floodplain soil. The BC particles with anthropogenic origin such as pitch and coke associated with the chloralkali production process served as both the source and subsequent transporter for the highly hydrophobic PCDD/Fs. These anthropogenic BC particles were enriched with high levels of PCDFs, containing approximately 1000-fold the concentration found in the bulk soil. The strong association of PCDD/Fs with anthropogenic BC directly impacts the physicochemical and biological availability thus the risk associated with these hydrophobic organochlorines in soils and sediments.     

Development of a combined isotopic and mass-balance approach to determine dissolved organic carbon sources in eutrophic reservoirs

A combined mass-balance and stable isotope approach was set up to identify and quantify dissolved organic carbon (DOC) sources in a DOC-rich (9 mg L⁻¹) eutrophic reservoir located in Western France and used for drinking water supply (so-called Rophemel reservoir). The mass-balance approach consisted in measuring the flux of allochthonous DOC on a daily basis, and in comparing it with the effective (measured) DOC concentration of the reservoir. The isotopic approach consisted, for its part, in measuring the carbon isotope ratios (δ¹³C values) of both allochthonous and autochthonous DOC sources, and comparing these values with the δ¹³C values of the reservoir DOC. Results from both approaches were consistent pointing out for a DOC of 100% allochthonous origin. In particular, the δ¹³C values of the DOC recovered in the reservoir (−28.5 ± 0.2‰; n = 22) during the algal bloom season (May-September) showed no trace of an autochthonous contribution (δ¹³C in algae = −30.1 ± 0.3‰; n = 2) being indistinguishable from the δ¹³C values of allochthonous DOC from inflowing rivers (−28.6 ± 0.1‰; n = 8). These results demonstrate that eutrophication is not responsible for the high DOC concentrations observed in the Rophemel reservoir and that limiting eutrophication of this reservoir will not reduce the potential formation of disinfection by-products during water treatment. The methodology developed in this study based on a complementary isotopic and mass-balance approach provides a powerful tool, suitable to identify and quantify DOC sources in eutrophic, DOC-contaminated reservoirs.