安徽省地质碳汇潜力及二氧化碳地质储存
|
摘要
气候变化是当今全球面临的重大挑战,它不仅是重大的科学问题,也是重大的政治问题。遏制气候变暖,拯救地球家园,是全人类共同的使命。我省处于工业化加速期,高能耗行业比重高,未来面临巨大的二氧化碳减排压力。加大产业结构调整、利用低碳技术改造和提升高碳产业固然是非常重要的技术措施,但地质碳汇也是二氧化碳减排的一条重要渠道。岩溶碳汇效应显著,土壤固碳潜力巨大,在二氧化碳减排和缓解温室气体效应的研究计划中,加强地质研究已是不容回避的重大科学问题。
Climate change is a major global challenge to face.It is not only a significant scientific issue,but also a big political issue.It is the mission for all human beings to contain global warming and salvage the earth home.Anhui province is at the stage of industrial acceleration characterized by high percentage of high energy consumption industries facing huge pressure on reduction of carbon dioxide emission in the future.It is an important technical means to enhance industrial restructuring,reconstruct and improve high-carbon industries with low-carbon technology,besides,geological carbon sink is another major approach to reduction of carbon dioxide emission.In this regard karst carbon sink plays a remarkable role and soil has tremendous potential in carbon fixation.It has been an unavoidable major scientific issue to strengthen geological aspect in the research program for reduction of carbon dioxide and alleviating greenhouse effect.
Climate change is a major global challenge to face.It is not only a significant scientific issue,but also a big political issue.It is the mission for all human beings to contain global warming and salvage the earth home.Anhui province is at the stage of industrial acceleration characterized by high percentage of high energy consumption industries facing huge pressure on reduction of carbon dioxide emission in the future.It is an important technical means to enhance industrial restructuring,reconstruct and improve high-carbon industries with low-carbon technology,besides,geological carbon sink is another major approach to reduction of carbon dioxide emission.In this regard karst carbon sink plays a remarkable role and soil has tremendous potential in carbon fixation.It has been an unavoidable major scientific issue to strengthen geological aspect in the research program for reduction of carbon dioxide and alleviating greenhouse effect.
引文
[1]邱冬生,庄大方,胡云峰,等.中国岩石风化作用所致的碳汇能力估算[J].地球科学-中国地质大学学报,2004,29(2),177~190.
[2]李晓明.国土资源部部长徐绍史-中国地质碳汇监测计划启动[N].科学时报,2010.3.
[3]许信旺,潘根兴,侯鹏程.不同土地利用对表层土壤有机碳密度的影响[J].水土保持学报,2005,19(6):193~200.
[4]蒋倩,李心清,丁文慈,等.岩溶水系统对大气CO2的潜在影响[J].矿物岩石地球化学通报,2006,25(3),226~234.
[5]袁道先.地球系统的碳循环和资源环境效应[J].第四纪研究,2001,21(3):223~232.
[6]二氧化碳矿物碳酸化固定的技术进展,中国化工信息网2007-11-6.
[7]Jefferson mortatti,Jean-luci probst.Silicate rock weatheringand atmospheric/Soil CO2 uptake in the Amazon basinestimated from river water geochemistry:seasonal and spatialvariation[J].Chem.Geol.2003,197:177~196.
[8]IPCC-Intergovernmental Panel on Climate Change[c]//MetzB,Davidson O,de Coninck H C,et al,eds.Special Report onCarbon Dioxide Capture and Storage.Cambridge:CambridgeUniversity Press,UK and New York,2005:195~276.
[9]张炜,李义连,郑艳,等.二氧化碳地质封存中的储存容量评估问题和研究进展[J].地球科学进展,2008,23(10),1061~1069.
[10]文冬光,吴登定,孙继潮,等.CO2地质处置研究现状和有关建议[J].中国地质环境信息网,2005-11-7.
[11]刘建栋,胡汉,张龙军.流域化学风化作用的碳汇机制研究进展[J].土壤通报,2007,38(5):998~1002.
[12]张军,李桂菊.二氧化碳封存技术及研究现状[J].能源与环境,2007(2),33~35.
[13]刘玉,刘德深,沈立成.云南维西花岗岩地区水文地球化学特征及形成机制研究[J].地球化学,2007,36(2),161~170.
[14]刘玉,刘德深,沈立成.花岗岩地区碳汇计算及影响因素研究[J].地球化学,2008,37(3),281~28
[2]李晓明.国土资源部部长徐绍史-中国地质碳汇监测计划启动[N].科学时报,2010.3.
[3]许信旺,潘根兴,侯鹏程.不同土地利用对表层土壤有机碳密度的影响[J].水土保持学报,2005,19(6):193~200.
[4]蒋倩,李心清,丁文慈,等.岩溶水系统对大气CO2的潜在影响[J].矿物岩石地球化学通报,2006,25(3),226~234.
[5]袁道先.地球系统的碳循环和资源环境效应[J].第四纪研究,2001,21(3):223~232.
[6]二氧化碳矿物碳酸化固定的技术进展,中国化工信息网2007-11-6.
[7]Jefferson mortatti,Jean-luci probst.Silicate rock weatheringand atmospheric/Soil CO2 uptake in the Amazon basinestimated from river water geochemistry:seasonal and spatialvariation[J].Chem.Geol.2003,197:177~196.
[8]IPCC-Intergovernmental Panel on Climate Change[c]//MetzB,Davidson O,de Coninck H C,et al,eds.Special Report onCarbon Dioxide Capture and Storage.Cambridge:CambridgeUniversity Press,UK and New York,2005:195~276.
[9]张炜,李义连,郑艳,等.二氧化碳地质封存中的储存容量评估问题和研究进展[J].地球科学进展,2008,23(10),1061~1069.
[10]文冬光,吴登定,孙继潮,等.CO2地质处置研究现状和有关建议[J].中国地质环境信息网,2005-11-7.
[11]刘建栋,胡汉,张龙军.流域化学风化作用的碳汇机制研究进展[J].土壤通报,2007,38(5):998~1002.
[12]张军,李桂菊.二氧化碳封存技术及研究现状[J].能源与环境,2007(2),33~35.
[13]刘玉,刘德深,沈立成.云南维西花岗岩地区水文地球化学特征及形成机制研究[J].地球化学,2007,36(2),161~170.
[14]刘玉,刘德深,沈立成.花岗岩地区碳汇计算及影响因素研究[J].地球化学,2008,37(3),281~28
目录