The United States Department of Energy's Regional Carbon Sequestration Partnerships Program Validation Phase

This paper reviews the Validation Phase (Phase II) of the Department of Energy's Regional Carbon Sequestration Partnerships initiative. In 2003, the U.S. Department of Energy created a nationwide network of seven Regional Carbon Sequestration Partnerships (RCSP) to help determine and implement the technology, infrastructure, and regulations most appropriate to promote carbon sequestration in different regions of the nation. The objectives of the Characterization Phase (Phase I) were to characterize the geologic and terrestrial opportunities for carbon sequestration; to identify CO(2) point sources within the territories of the individual partnerships; to assess the transportation infrastructure needed for future deployment; to evaluate CO(2) capture technologies for existing and future power plants; and to identify the most promising sequestration opportunities that would need to be validated through a series of field projects. The Characterization Phase was highly successful, with the following achievements: established a national network of companies and professionals working to support sequestration deployment; created regional and national carbon sequestration atlases for the United States and portions of Canada; evaluated available and developing technologies for the capture of CO(2) from point sources; developed an improved understanding of the permitting requirements that future sequestration activities will need to address as well as defined the gap in permitting requirements for large scale deployment of these technologies; created a raised awareness of, and support for, carbon sequestration as a greenhouse gas (GHG) mitigation option, both within industry and among the general public; identified the most promising carbon sequestration opportunities for future field tests; and established protocols for project implementation, accounting, and management. Economic evaluation was started and is continuing and will be a factor in project selection. During the Validation Phase, the seven regional partnerships will put the knowledge learned during the Characterization Phase into practice through field tests that will validate carbon sequestration technologies that are best suited to their respective regions of the country. These tests will verify technologies developed through DOE's core R&D effort and enable implementation of CO(2) sequestration on a large scale, should that become necessary. Pilot projects will have a site-specific focus to test technology; assess formation storage capacity and injectivity; validate and refine existing CO(2) formation models used to determine the transport and fate of CO(2) in the formation; demonstrate the integrity of geologic seals to contain CO(2); validate monitoring, mitigation, and verification (MMV) technologies; define project costs and compare costs of alternatives; assess potential operational and long-term storage risks; address regulatory requirements; and engage and evaluate public acceptance of sequestration technologies. Field validation tests involving both sequestration in geologic formations and terrestrial sequestration are being developed. The results from the Validation Phase will help to confirm the estimates made during the Characterization Phase and will be used to update the regional atlases and NatCarb. Answers to many questions about the effectiveness and safety of carbon sequestration technologies will be instrumental in planning for a Deployment Phase, in which large volume tests will be planned to further sequestration as an option that can mitigate GHG emissions in the United States.     

Ecosystem carbon budgeting and soil carbon sequestration in reclaimed mine soil

Global warming risks from emissions of green house gases (GHGs) by anthropogenic activities, and possible mitigation strategies of terrestrial carbon (C) sequestration have increased the need for the identification of ecosystems with high C sink capacity. Depleted soil organic C (SOC) pools of reclaimed mine soil (RMS) ecosystems can be restored through conversion to an appropriate land use and adoption of recommended management practices (RMPs). The objectives of this paper are to (1) synthesize available information on carbon dioxide (CO2) emissions from coal mining and combustion activities, (2) understand mechanisms of SOC sequestration and its protection, (3) identify factors affecting C sequestration potential in RMSs, (4) review available methods for the estimation of ecosystem C budget (ECB), and (5) identify knowledge gaps to enhance C sink capacity of RMS ecosystems and prioritize research issues. The drastic perturbations of soil by mining activities can accentuate CO2 emission through mineralization, erosion, leaching, changes in soil moisture and temperature regimes, and reduction in biomass returned to the soil. The reclamation of drastically disturbed soils leads to improvement in soil quality and development of soil pedogenic processes accruing the benefit of SOC sequestration and additional income from trading SOC credits. The SOC sequestration potential in RMS depends on amount of biomass production and return to soil, and mechanisms of C protection. The rate of SOC sequestration ranges from 0.1 to 3.1 Mg ha(-1) yr(-1) and 0.7 to 4 Mg ha(-1) yr(-1) in grass and forest RMS ecosystem, respectively. Proper land restoration alone could off-set 16 Tg CO2 in the U.S. annually. However, the factors affecting C sequestration and protection in RMS leading to increase in microbial activity, nutrient availability, soil aggregation, C build up, and soil profile development must be better understood in order to formulate guidelines for development of an holistic approach to sustainable management of these ecosystems. The ECBs of RMS ecosystems are not well understood. An ecosystem method of evaluating ECB of RMS ecosystems is proposed.     

农田固碳措施对温室气体减排影响的研究进展

农田是CO2,CH4和N2O三种温室气体的重要排放源,在全球范围内农业生产活动贡献了约14%的人为温室气体排放量,以及58%的人为非CO2排放,不合理的农田管理措施强化了农田温室气体排放源特征,弱化了农田固碳作用。土壤碳库作为地球生态系统中最活跃的碳库之一,同时也是温室气体的重要源/汇。研究表明通过采取合理的农田管理措施,既可起到增加土壤碳库、减少温室气体排放的目的,又能提高土壤质量。农田土壤碳库除受温度、降水和植被类型的影响外,还在很大程度上受施肥量、肥料类型、秸秆还田量、耕作措施和灌溉等农田管理措施的影响。本文通过总结保护性耕作/免耕,秸秆还田,氮肥管理,水分管理,农学及土地利用变化等农田管理措施,探寻增强农田土壤固碳作用,减少农田温室气体排放的合理途径。农田碳库的稳定/增加,对于保证全球粮食安全与缓解气候变化趋势具有双重的积极意义。在我国许多有关土壤固碳与温室气体排放的研究尚不系统或仅限于短期研究,这也为正确评价各种固碳措施对温室气体排放的影响增加了不确定性。     

中国农业源碳汇估算及其与农业经济发展的耦合分析

农业作为重要的产业部门,在满足人们基本的物质需求的同时具有重要的生态保障和碳汇功能,充分发掘农业的碳汇潜力对于农业绿色化发展和农民增收具有重要意义。本文量化测算了我国1993—2011年的农业源碳汇潜力,并构建农业源浄碳汇与农业经济发展的耦合模型,结果发现农业源碳汇量由1993年的52 318.70万t波动增加到2011年的66 073.77万t,年均增加1.38%,但是农业源的浄碳汇量却呈现波动递减趋势,由1993年的36 691.72万t减少到34 815.67万t,其中粮食作物的CO2吸收总量占据主要部分,经济作物CO2吸收量在农业总的CO2吸收量所占的比重虽小,但是增速较快,年均增幅达到4.15%;从影响因素来看,农业源碳汇和耕地面积关联度不大,农作物单位产量和农业源碳汇呈正相关;农业源浄碳汇与农业经济发展之间处于强负耦合状态,耦合状态不理想,农业产值与农业净碳汇关联度不强,这主要是由高投入、高消耗的农业生产方式引发农业碳排放增加和农业总产出效益提升等原因造成的。最后,本文针对性地提出促进我国农业减排增汇的对策建议:强化政府引导,从农业的规划、生产、消费等多领域进行引导;加大农业减排增汇的技术、资金和人力支持,为农业的减排增汇做好保障;通过林地增汇、农田增汇、草地增汇、综合增汇等多种手段,提升农地的碳汇能力;加快碳市场交易体系建设,以市场杠杆推进农业的减排增汇。     

Global estimates of soil carbon sequestration via livestock waste: a STELLA simulation

It has become increasingly well documented that human activities are enhancing the greenhouse effect and altering the global climate. Identifying strategies to mitigate atmospheric carbon dioxide emissions on the national level are therefore critical. Fossil fuel combustion is primarily responsible for the perturbation of the global carbon cycle, although the influence of humans extends far beyond the combustion of fossil fuels. Changes in land use arising from human activities contribute substantially to atmospheric carbon dioxide; however, land use changes can act as a carbon dioxide sink as well. A soil carbon model was built using STELLA to explore how soil organic carbon sequestration (SOC) varies over a range of values for key parameters and to estimate the amount of global soil carbon sequestration from livestock waste. To obtain soil carbon sequestration estimates, model simulations occurred for 11 different livestock types and with data for eight regions around the world. The model predicted that between 1980 and 1995, United States soils were responsible for the sequestration of 444–602 Tg C from livestock waste. Model simulations further predicted that during the same period, global soil carbon sequestration from livestock waste was 2,810–4,218 Tg C. Our estimates for global SOC sequestration are modest in proportion to other terrestrial carbon sinks (i.e. forest regrowth); however, livestock waste does represent a potential for long-term soil carbon gain. SOC generated from livestock waste is another example of how human activities and land use changes are altering soil processes around the world. Readers should send their comments on this paper to: BhaskarNath@aol.com within 3 months of publication of this issue.     

Estimation of Soil Carbon Gains Upon Improved Management within Croplands and Grasslands of Africa

Many agro(eco)systems in Africa have been degraded as a result of past disturbances, including deforestation, overgrazing, and over exploitation. These systems can be managed to reduce carbon emissions and increase carbon sinks in vegetation and soil. The scope for soil organic carbon gains from improved management and restoration within degraded and non-degraded croplands and grasslands in Africa is estimated at 20–43 Tg C year^?1, assuming that 'best' management practices can be introduced on 20% of croplands and 10% of grasslands. Under the assumption that new steady state levels will be reached after 25 years of sustained management, this would correspond with a mitigation potential of 4–9% of annual CO₂ emissions in Africa. The mechanisms that are being put in place to implement the Kyoto Protocol - through C emission trading - and prevailing agricultural policies will largely determine whether farmers can engage in activities that enhance C sequestration in Africa. Mitigation of climate change by increased carbon sequestration in the soil appears particularly useful when addressed in combination with other pressing regional challenges that affect the livelihood of the people, such as combating land degradation and ensuring food security, while at the same time curtailing global anthropogenic emissions.     

土地利用变化及林业温室气体排放核算制度与方法实证

土地利用变化及林业(LUCF)活动是生态固碳最重要手段。研究确定LUCF温室气体排放核算制度和方法,对平衡碳排放、开展全国统一碳市场交易具有重要基础作用。在综述LUCF温室气体核算理论和方法基础上,借鉴IPCC指南和《省级温室气体清单编制指南(试行)》推荐的基本方法,构建了符合地域特色的LUCF温室气体排放核算制度和方法。采用2014年第九次国家森林资源清查数据,以全国低碳试点省陕西省为实证对象,初步核算了陕西省LUCF温室气体的净排放量,并从排放能力、排放结构和空间特征等角度揭示了陕西省LUCF温室气体的排放特征。结果显示:(1)2014年,陕西省LUCF温室气体净吸收量为1 698.42万t CO_2e,其中森林及其他木质生物质碳贮量净吸收1 852.67万t CO2e,森林转化净排放154.25万t CO_2e。(2)乔木林等优势树种,是陕西省LUCF温室气体排放中重要的固碳源(吸收源)。(3)陕南地区是重要固碳贡献区,陕北地区森林固碳能力较差。最后,针对LUCF温室气体排放核算制度和方法不够完善、森林固碳能力差异较大、区域固碳分化严重等问题,提出了健全温室气体核算制度、平衡森林资源空间分布、改善固碳树种结构等加强陕西省LUCF活动应对气候变化统计核算制度和能力建设的基本措施。     

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。     

二氧化碳排放的国际比较及对我国低碳经济发展的启示

首先分析了我国二氧化碳排放的基本情况,指出当前二氧化碳排放增长率虽然有所下降,但环境形势依然严峻。然后从国家碳排放总量、人均CO2排放量、单位GDP二氧化碳排放量、国家累积碳排放和人均累积碳排放几个方面对我国二氧化碳排放水平与国际水平进行了比较,并结合节能减排目标对我国低碳经济的发展提出了相关建议。     

In situ uranium stabilization by microbial metabolites

Microbial melanin production by autochthonous bacteria was explored in this study as a means to increase U immobilization in U contaminated soil. This article demonstrates the application of bacterial physiology and soil ecology for enhanced U immobilization in order to develop an in situ, U bio-immobilization technology. We have demonstrated microbial production of a metal chelating biopolymer, pyomelanin, in U contaminated soil from the Tims Branch area of the Department of Energy (DOE), Savannah River Site (SRS), South Carolina, as a result of tyrosine amendments. Bacterial densities of pyomelanin producers were >10(6) cells per g wet soil. Pyomelanin demonstrated U complexing and mineral binding capacities at pH 4 and 7. In laboratory studies, in the presence of goethite or illite, pyomelanin enhanced U sequestration by these minerals. Tyrosine amended soils in a field test demonstrated increased U sequestration capacity following pyomelanin production up to 13 months after tyrosine treatments.     

中国省级CO2排放影响因素的空间计量分析

提出面板数据空间误差分量模型,采用基于广义矩1估计的可行广义最小二乘法估计方法,研究1997-2007年间,我国省级CO2排放的影响因素.实证结果表明,我国省级CO2排放量存在显著的正向空间相关性,CO2排放较多的省份往往会影响邻近地区的CO2排放;CO2排放量与人均GDP呈倒N型环境库兹涅兹曲线.未考虑空间相关性时,CO2排放转折点为人均GDP 51 73O元,我国目前仍处于CO2排放量上升期;采用面板数据空间误差分量模型修正后,CO2排放下降转折点为人均GDP约53 237元,较未考虑空间因素时有所提高,省际间的空间相互影响,对CO2排放下降转折点的人均GDP提出更高的要求;实证研究结果同时显示,煤炭消费比重提高及人口数量增大,都将显著增加我国CO2排放量,体现优化能源结构和控制人口增长对抑制CO2排放增长的重要性.     

Energy Use and CO2 Production in Tropical Agriculture and Means and Strategies for Reduction or Mitigation

Carbon dioxide emissions due to fossil fuel consumption are well recognized as a major contributor to climate change. In the debate on dealing with this threat, expectations are high that agriculture based economies of the developing world can help alleviate this problem. But, the contribution of agricultural operations to these emissions is fairly small. It is the clearing of native ecosystems for agricultural use in the tropics that is the largest non-fossil fuel source of CO₂ input to the atmosphere. Our calculation show that the use of fossil energy and the concomitant emission of CO₂ in the agricultural operational sector - i.e. the use of farm machinery, irrigation, fertilization and chemical pesticides - amounts to merely 3.9% of the commercial energy use in that part of the world. Of this, 70% is associated with the production and use of chemical fertilizers. In the absence of fertilizer use, the developing world would have converted even more land for cultivation, most of which is completely unsuitable for cultivation. Current expectations are that reforestation in these countries can sequester large quantities of carbon in order to mitigate excessive emissions elsewhere. But, any program that aims to set aside land for the purpose of sequestering carbon must do so without threatening food security in the region. The sole option to liberate the necessary land for carbon sequestration would be the intensification of agricultural production on some of the better lands by increased fertilizer inputs. As our calculations show, the sequestration of carbon far outweighs the emissions that are associated with the production of the extra fertilizer needed. Increasing the fertilizer use in the developing world (without China) by 20%, we calculated an overall net benefit in the carbon budget of between 80 and 206 Mt yr^?1 dependent on the carbon sequestration rate assumed for the regrowing forest. In those regions, where current fertilizer use is low, the relative benefits are the highest as responding yield increases are highest and thus more land can be set aside without harming food security. In Sub-Saharan Africa a 20% fertilizer increase, which amounts to 0.14 Mt of extra fertilizer, can tie up somewhere between 8 and 19 Mt of CO₂ per year (average: 96 t CO₂ per 1 t fertilizer). In the Near East and North Africa with a 20%-increased fertilizer use of 0.4 Mt yr^-1 between 10 and 24 Mt of CO₂ could be sequestered on the land set aside (40 t CO₂ per 1 t fertilizer). In South Asia this is 22–61 Mt CO₂ yr?1 with an annual additional input of 2.15 Mt fertilizer (19 t CO₂ per 1 t fertilizer). In fact, carbon credits may be the only way for some of the farmers in these regions to afford the costly inputs. Additionally, in regions with already relatively high fertilizer inputs such as in South Asia, an efficient use of the extra fertilizer must be warranted. Nevertheless, the net CO₂ benefit through implementation of this measure in the developing world is insignificant compared to the worldwide CO₂ output by human activity. Thus, reforestation is only one mitigating measure and not the solution to unconstrained fossil fuel CO₂ emissions. Carbon emissions should, therefore, first of all be reduced by the avoidance of deforestation in the developing world and moreover by higher energy efficiency and the use of alternative energy sources.     

Derivation of a screening methodology for evaluating radiation dose to aquatic and terrestrial biota

The United States Department of Energy (DOE) currently has in place a radiation dose standard for the protection of aquatic animals, and is considering additional dose standards for terrestrial biota. These standards are: 10 mGy/d for aquatic animals, 10 mGy/d for terrestrial plants, and, 1 mGy/d for terrestrial animals. Guidance on suitable approaches to the implementation of these standards is needed. A screening methodology, developed through DOE's Biota Dose Assessment Committee (BDAC), serves as the principal element of DOE's graded approach for evaluating radiation doses to aquatic and terrestrial biota. Limiting concentrations of radionuclides in water, soil, and sediment were derived for 23 radionuclides. Four organism types (aquatic animals; riparian animals; terrestrial animals; and terrestrial plants) were selected as the basis for development of the screening method. Internal doses for each organism type were calculated as the product of contaminant concentration, bioaccumulation factor(s) and dose conversion factors. External doses were calculated based on the assumption of immersion of the organism in soil, sediment, or water. The assumptions and default parameters used provide for conservative screening values. The screening methodology within DOE's graded approach should prove useful in demonstrating compliance with biota dose limits and for conducting screening assessments of radioecological impact. It provides a needed evaluation tool that can be employed within a framework for protection of the environment.     

Global Research Trends Related to CO2 Emissions and Their Enlightenment to China

Given the growing awareness of the likely catastrophic impacts of climate change and close association of climate change with global emissions of greenhouse gases (of which carbon dioxide is more prominent) , considerable research efforts have been devoted to the analysis of carbon dioxide (CO2) emissions and its relationship to sustainable development. Now GHG reduction programs have been coming into effect in many developed countries that have more responsibility for historical CO2 emissions, and the studies have become mature. First, the GHG emissions accounting system is more all-inclusive and the methods are more rational with the effort of IPCC from 1995 and all other researchers related. Second, the responsibility allocation is more rational and fair. Along with the clarity of "carbon transfer" and "carbon leakage", the perspective and methodology for allocating regional CO2 emissions responsibility is turning from production base to consumption base. Third, the decomposition method has become more mature and more complex. For example, the decomposition formulas are including KAYA expression and input-output expression and the decomposition techniques are developed from index analysis to simple average divisia and then adaptive-weighting divisia. Fourth, projection models have become more integrated and long-term. The top-down model and bottom-up model are both inter-embedded and synergetic. Trends above give some advice for the research on CO2 in China, such as emissions factors database construction, deeper-going research on emissions responsibility and structure analysis, promotion of modeling technology and technology-environment database.     

晶硅光伏组件出口对中国碳排放的影响

基于文献资料,估算了2004-2009年中国晶硅光伏组件制造过程中的能源消耗和CO2排放强度。研究发现,2004-2009年,晶硅光伏组件制造过程中的能耗强度和CO2排放强度均逐年下降。2009年,单晶、多晶光伏组件制造过程中的能耗强度分别为2 629 kWh/kWp和2 242 kWh/kWp,碳排放强度分别为1 829 gCO2/Wp和1 559 gCO2/Wp。由于晶硅光伏组件的大量出口,中国不仅出口了大量的隐含碳,还损失了数量可观的、潜在的CO2减排能力。2004-2010年,中国的隐含碳净出口量由3万tCO2增加到852万tCO2;如果出口的晶硅电池全部用于国内,在其生命周期内累计可减排CO23.4亿t。除2004年和2010年外,国内安装的晶硅光伏组件在其生命周期内所能减少的CO2排放不足以抵消晶硅光伏行业的CO2排放,晶硅光伏行业对中国CO2减排的贡献为负。在多晶硅全部国产的情况下,中国若维持晶硅电池应用中的CO2减排量与全行业CO2排放量的平衡,至少应将晶硅组件制造的7.2%安装在国内使用。若多晶硅进口比例仍保持在50%左右,则至少应将晶硅组件制造的4.9%安装在国内使用。     

新疆地级市CO_2排放空间特征研究

基于中国高空间分辨率网格数据,建立新疆地级市CO_2排放数据集,探讨新疆CO_2排放的空间特征,为新疆低碳发展的空间布局规划提供一定的依据。研究采用"自下而上"的空间化方法建立排放数据集,并用统计学方法分析排放数据统计特征。研究结果:从整体看,CO_2直接排放总体分散,局部集中,基本沿着天山分为南部和北部,北部地区排放高于南部地区。从区域看,天山北坡经济带CO_2排放最高;丝绸之路经济带的中通道、北通道和南通道排放依次递减。从部门看,服务业与城镇生活CO_2排放相关性最高,间接排放与其他部门排放相关性最弱。从类型看,工业型地级市CO_2人均排放最高,总排放均值略低于服务业型地级市,远高于其他类型地级市;人口规模越大的地级市CO_2排放均值越大,但其人均排放越少。结论与讨论:1新疆CO_2排放空间差异显著,其排放较大的地级市整体效率不高,将是减排的重点区。2工业化、城镇化是新疆CO_2排放的重要影响因素,将是减排的着力点。3省际生态补偿和碳排放指标分配时应适度考虑能源输出引致本地较高CO_2排放的特情。     

城市产业部门CO2排放三层次核算研究

城市是人类生产和生活的中心,超过75%的温室气体从城市产生,其中又以城市产业部门能源消费和工业过程非能源产生的CO2为主。本文基于投入产出模型,评价城市产业部门3个不同层次的CO2排放。以重庆为案例,核算其2002-2008年产业部门三个层次的CO2排放,包括能源消费直接排放、购买电力间接排放和全生命周期排放,并进行多层次对比。结果显示传统能源消耗和购买电力为对象的核算方法低估了产业部门CO2排放水平。2002-2008年,重庆各产业部门排放量逐年增加,碳排放强度整体呈现下降趋势。煤炭开采和洗选业、非金属矿采选业、非金属矿物制品业、电力、热力的生产和供应业,化学工业、金属冶炼及压延加工业、交通运输、仓储及邮电通讯业部门共7大行业是重庆碳排放的重点行业。部门交通设备制造业是重庆的优势产业,排放总量大,但是排放强度却相对较小,因此应大力发展该产业以促进重庆市低碳经济的发展。     

无锡市能源消费、碳排放与经济增长关系分析

经济增长对资源消耗存在很大的依赖性,研究能源消费、碳排放与经济增长关系,可为经济增长方式转变和低碳城市建设提供重要科学依据。基于IPCC国家温室气体排放清单指南中的方法估算了无锡市能源消费碳排放,并建立“脱钩”模型探讨能源消费、碳排放与经济增长之间的关系。结果表明：（1）2000~2010年,无锡市碳排放从84335万t增加到2 52804万t,总量不断增加,但趋势有所减缓,且各县市碳排放特征差异显著;（2）无锡市碳排放与经济增长整体处于弱脱钩状态,且脱钩状态有不断增强的趋势,市区经济发展已不依赖于能源消费,朝着环境友好方向发展,江阴和宜兴节能减排压力仍然很大;（3）优化产业结构、调整工业结构和提高能源利用效率是改善无锡市能源消费、碳排放和经济增长关系的有效途径,各县市根据具体情况,侧重点有所不同     

中国城市产业结构与CO_2排放的耦合关系

产业结构与CO_2排放量之间的相互作用形成产业结构与CO_2排放量的耦合关系。本文基于2012年中国1 km高空间分辨率网格CO_2排放数据(CHRED),运用耦合度模型,分析了中国288个城市产业结构与CO_2排放量的耦合特征。研究发现,中国产业结构和CO_2排放量之间正处于中度耦合一致性阶段,以资源型为主的城市产业结构和CO_2排放量处于极度耦合一致性阶段;工业型城市耦合度和一致性均高于服务业型城市;其他类型城市则分布比较分散没有呈现一定的规律性,而在其他类型的城市中,工业占比相对较高的城市耦合度和一致性往往高于农业和服务业占比较高的城市。根据产业结构和CO_2排放量的耦合度和一致性关系,将现有的城市分为4种类型,分别是产业结构与CO_2排放耦合一致性相关关系极强的城市,产业结构与CO_2排放耦合一致性相关关系较高的城市、产业结构和CO_2排放耦合一致性相关关系一般的城市以及产业结构和CO_2排放耦合一致性相关关系较弱的城市。通过对4种类型城市进行特征分析,4种类型城市在空间分布上具有明显的聚集效应,而且第二产业与碳排放之间的耦合一致性较高。     

基于IPCC方法的湖南省温室气体排放核算及动态分析

为温室气体减排提供决策参考,基于IPCC和中国《省级温室气体清单编制指南》,核算了1995~2011年湖南省温室气体排放,并对其动态作了分析。结果表明: 2011年湖南省温室气体排放总量为594.7 Mt CO₂e,主要温室气体CO₂、CH₄和N₂O的排放量分别为471.3、100.8和22.6 Mt CO₂e,占排放总量的比例依次为79.25%、16.95%和3.79%。能源消费是温室气体排放的主要来源,2011年的排放量达421.5 Mt CO₂e,占排放总量的70.87%。林业呈现为碳汇效应,2011年的值为18.2 Mt CO₂e,消解温室气体排放量的3.06%。研究时段内温室气体从241.7 Mt CO₂e增长为594.7 Mt CO₂e,年均增长率达9.12%,可分为3个阶段,其中,1995~1999年波动降低,1999~2003年缓慢上升,2003~2011年快速增长,变化率依次为-3.32%、4.69%和17.37%。能源利用效率明显提高,万元GDP温室气体排放量由10.64 t CO₂e/万元减少到2.93 t CO₂e/万元,年均减少7.75%,但人均温室气体排放量由3.65 t CO₂e增加到8.07 t CO₂e,年均增长5.08%,减排压力较大。