将高纬度地区生态系统的反馈与恢复力引入公司决策

本文讨论了在高纬度地区公司所起的作用,它被概念化为以社会和经济为媒介的生态系统,同时指出了商业环境里其他的一些重要的社会参与者.我们列举了高纬地区企业行为的三个案例并对其中各种共性进行了讨论.特别的,我们认为有必要对商业理论和实践进行革新,以使其不只是停留在社会与经济概念的组织恢复力上,而要把高纬地区的生态恢复力也包括到商业管理的目标之中.同时我们也认为区域生态系统的恢复力应该成为衡量企业可持续管理的一个有意义的指标,企业高层可以据此制定和修改企业的管理策略.最后,文章在结尾处呼吁对高纬地区内的跨国公司和国内公司的作用制定更为详细的研究议程.     

Climate impact from peat utilisation in Sweden

The climate impact from the useof peat for energy production in Sweden hasbeen evaluated in terms of contribution toatmospheric radiative forcing. This wasdone by attempting to answer the question`What will be the climate impact if onewould use 1 m<sup>2</sup> of mire for peatextraction during 20 years?'. Two differentmethods of after-treatment were studied:afforestation and restoration of wetland.The climate impact from a peatland –wetland scenario and a peatland –forestation – bioenergy scenario wascompared to the climate impact from coal,natural gas and forest residues.Sensitivity analyses were performed toevaluate which parameters that areimportant to take into consideration inorder to minimize the climate impact frompeat utilisation. In a `multiple generationscenario' we investigate the climate impactif 1 Mega Joule (MJ) of energy is produced every yearfor 300 years from peat compared to otherenergy sources.The main conclusions from the study are:?The accumulated radiative forcing from the peatland – forestation – bioenergy scenario over a long time perspective (300 years) is estimated to be 1.35 mJ/m²/m² extraction area assuming a medium-high forest growth rate and medium original methane emissions from the virgin mire. This is below the corresponding values for coal 3.13 mJ/ m²/ m² extraction area and natural gas, 1.71 mJ/ m²/ m² extraction area, but higher than the value for forest residues, 0.42 mJ/ m²/ m² extraction area. A `best-best-case' scenario, i.e. with high forest growth rate combined with high `avoided' methane (CH₄) emissions, will generate accumulated radiative forcing comparable to using forest residues for energy production. A `worst-worst-case' scenario, with low growth rate and low `avoided' CH₄ emissions, will generate radiative forcing somewhere in between natural gas and coal.?The accumulated radiative forcing from the peatland – wetland scenario over a 300-year perspective is estimated to be 0.73 –1.80 mJ/ m²/ m² extraction area depending on the assumed carbon (C) uptake rates for the wetland and assuming a medium-high methane emissions from a restored wetland. The corresponding values for coal is 1.88 mJ/ m²/ m² extraction area, for natural gas 1.06 mJ/ m²/ m² extraction area and for forest residues 0.10 mJ/ m²/ m² extraction area. A `best-best-case' scenario (i.e. with high carbon dioxide CO<sub>2</sub>-uptake combined with high `avoided' CH₄ emissions and low methane emissions from the restored wetland) will generate accumulated radiative forcing that decreases and reaches zero after 240 years. A `worst-worst-case' (i.e. with low CO<sub>2</sub>-uptake combined with low `avoided' CH₄ emissions and high methane emissions from the restored wetland) will generate radiative forcing higher than coal over the entire time period.?The accumulated radiative forcing in the `multiple generations' – scenarios over a 300-year perspective producing 1 MJ/year is estimated to be 0.089 mJ/ m<sup>2</sup> for the scenario `Peat forestation – bioenergy', 0.097 mJ/ m² for the scenario `Peat wetland with high CO<sub>2</sub>-uptake' and 0.140 mJ/ m<sup>2</sup> for the scenario `Peat wetland with low CO₂-uptake'. Corresponding values for coal is 0.160 mJ/ m², for natural gas 0.083 mJ/ m² and for forest residues 0.015 mJ/ m². Using a longer time perspective than 300 years will result in lower accumulated radiative forcing from the scenario `Peat wetland with high CO₂-uptake'. This is due to the negative instantaneous forcing that occurs after 200 years for each added generation.?It is important to consider CH₄ emissions from the virgin mire when choosing mires for utilization. Low original methane emissions give significantly higher total climate impact than high original emissions do.?Afforestation on areas previously used for peat extraction should be performed in a way that gives a high forest growth rate, both for the extraction area and the surrounding area. A high forest growth rate gives lower climate impact than a low forest growth rate.?There are great uncertainties related to the data used for emissions and uptake of greenhouse gases in restored wetlands. The mechanisms affecting these emissions and uptake should be studied further.     

浅议促进企业进行环境管理的方法

企业是环境污染的重要源头，企业污染是政府进行环境监督、管理的工作重点。但政府单纯凭借法律、行政和经济手段是不够的，还应该充分调动企业自身进行环境管理、参与环境保护的积极性和主动性，即压力和动力并重。为此，政府应加大对社会、对企业的环保宣传力度，使企业认识到环境效益、社会效益和经济效益存在着一致性和互促性。此外，政府还应加在ISO14000环境管理系列标准的宣传，使企业提早准备、积极行动以提高企业在市场中的竞争力。     

新疆百重7井区油田开发对地下水环境的影响分析

新疆百重7井区为新疆百口腺地下水的汇集径流区,是克拉玛依市生尖生产用水水源之一，在此处进行油田开发，使得保护该区地下水环境成为开发工程的重中之重，由新疆百重7井区油田开发对地下水环境的影响分析可知，正常状况下的油田开发对地下水的影响很小，一旦发生事故，则对地下水的影响很大，必须采取适当措施，保护该区丰富的地下水资源。     

非洲中部生态系统的碳排放及碳截留潜力

<京都议定书>中的<气候变化框架公约共同行动计划>和<清洁开发机制>要求对目前生态系统的碳蓄积、碳通量及碳截留潜力进行科学的理解,特别是对于碳贮库大但碳排放显著的、存在大面积和可重新造林土地的热带生态系统的了解.非洲中部拥有世界上10%的现有热带湿润森林,但有关该地区的碳研究甚少.1980年,非洲中部生态系统地上部分的碳蓄积为28.92Pg,到1990年则减少到24.79Pg.以增加生物量碳密度为目标而改善的森林管理能够截留18.32Pg的碳,到2050年还有超过50万km2原为森林的土地可以重新造林,从而增加截留10Pg的碳.了解生物量碳蓄积及其潜在截留量的空间分布对于通过<共同行动计划>和<清洁开发机制>所启动的碳贸易行动具有重大的意义.     

“十五”环境规划编制方法的改革

在分析中长期环境规划发展趋势的基础上,结合可持续发展的要求,从6个方面探讨了“十五”环境规划编制方法的改革与创新的具体方案。