瓦里关山大气CO2及其δ13C本底变化

利用 1991— 2 0 0 1年期间实测资料 ,分析了瓦里关全球基准站大气CO2 及其δ13 C本底特征 ,并探讨了与源汇过程的关系 .结果表明 ,瓦里关大气CO2 及其δ13 C本底变化主要反映了北半球中高纬度大陆自然生态系统源汇的周期性季节特征 ,而海洋的作用相对较弱 ;大气CO2 及其δ13 C本底浓度范围与所处纬度带平均状况基本吻合 ,年平均值以及年际间涨落与全球水平的一致性反映出化石燃料燃烧等人为排放对大气圈的全球性影响 ;瓦里关站提供的主要温室气体本底观测资料 ,既能体现亚洲内陆地域特点又具有全球代表性 ,配合以其它相关资料 ,还可进一步揭示中国内陆高原大气CO2 及其δ13 C本底特征的成因 .     

环境影响评价中清洁生产分析的主要内容及改进

根据清洁生产的基本涵义及环境影响评价中清洁生产分析的原则与目标，分析了清洁生产分析的主要内容，并针对目前存在的问题，提出了改进意见。     

关于排污权交易市场设置的探索研究

排污权交易在我国经过了近30年的探索和实践,仍然停留在试点工作上的原因在于该制度的推广还存在一些困难。本文针对我国部分排污权交易试点地区由于市场容量过小,导致排污权供给不足,出现供不应求情况的问题,以山西省排污权交易开展现状为例,从人口、经济、政策环境等方面对影响市场设置的因素作出初步探索和分析,认为按照省级行政区域来划分市场范围是目前比较合理的选择,可以充分发挥排污权交易机制在市场资源配置方面的作用。     

Insertable thin film thermocouples for in situ transient temperature monitoring in ultrasonic metal welding of battery tabs

Real-time monitoring and control of temperature in ultrasonic joining of battery tabs and coupons are important for the quality improvement and cost reduction of battery assembly. However, there have always been difficulties in accurate and real-time measurement of temperature by conventional sensors for practical implementation. In this study, an innovative method is developed to provide an enabling technology for the in situ transient temperature monitoring, which could provide reliable feedback signals for potential control of ultrasonic joining processes. Micro thin film thermocouples (TFTCs) were fabricated on thin silicon substrates, which were then inserted in the welding anvil as a permanent feature so that the sensors were always located about 100 μm directly under the welding spot during joining of multilayer Ni-coated Cu thin sheets for battery assembly. Good repeatability was demonstrated while a temperature rise of up to 650 °C was obtained due to the closeness of the sensors to the welding spot. The inserts with thin film sensors remained functional after welding experiments. This method has a great potential for in situ transient temperature monitoring, and thus the control of ultrasonic joining processes to realize a practical smart joining system.     

佛山市创建生态市差距分析与策略研究

生态市建设是探索区域生态文明的准备阶段,亦是区域可持续发展道路的重要阶段。成功的生态市创建策略是在充分认识本区域发展现状及创建差距的基础上,抓住重点任务作出科学、合理、可操作的政策措施。佛山市提出了在2015年建成国家生态市的奋斗目标,时间紧任务重,必须尽快制定行之有效的策略。本文重点分析佛山市目前经济、生态环境与社会进步等方面与生态市考核指标要求之间的差异,在此基础上识别佛山市创建生态市的重点任务,进一步研究相应的配套政策需求。     

离子色谱法测定无组织废气中溴化氢浓度

探讨无组织废气中溴化氢的测定方法。采样方法参照环境空气中氯化氢的采样方法,用淋洗液做吸收液,用大型气泡吸收管作收集器,点位设置按照《大气污染物综合排放标准(》GB16297-1996)附录C给出的无组织排放监控点设置方法进行;分析方法使用离子色谱法测定,分离度较高,相对标准偏差为1.7%～1.9%,加标回收率为93.8%～97.6%,溴离子的检测限为0.02μg/ml,当采样体积为60 L时,无组织废气中溴化氢的检出限为0.003 mg/m3。     

湖北郧西县庹家湾剖面粒度组成特征及其环境意义

对湖北省郧西县庹家湾(TJW)剖面的地层序列、年代、磁化率及粒度组成进行研究。结果表明:TJW剖面具有表土(MS)→全新世黄土(L0)→古土壤(S0)→过渡层(Lt)→马兰黄土(L1)→黄土与砂互层(T1-al2)→砾石层(T1-al1)的地层序列;在马兰黄土层上部的黏粒含量、黏粒/粉砂值以及磁化率值明显高于典型马兰黄土,而接近古土壤(S0),其成壤作用明显,属于较典型的弱古土壤层(L1-S1和L1-S2),其年龄在27.3~21.6 ka B.P.之间。此现象反映了在汉江上游地区,晚更新世时期的冰期气候并不是持续稳定的,在27.3~21.6 ka B.P.期间存在相对短暂的温暖湿润阶段,这次气候事件可与黄土高原地区进行良好对比。     

对苯二甲酸降解菌固定化生物流化床处理精对苯二甲酸废水

采用微生物筛选、纯化技术,获得了降解对苯二甲酸（TA）的YPC—TA1,YPC—TA2,YPC-TA3,YPC—TA44株菌株。将筛选出的TA降解菌固定化,处理初始TA质量浓度为2650mg／L的模拟废水,降解36h后TA去除率达100％。用TA降解芮在生物流化床反应器中处理PTA废水,最佳容积负荷为6.7kg／（m^3·d）。生物流化床反应器可在容积负荷为6．0～6．5kg／（m^3·d）的较佳条件下长周期稳定运行,COD去除率保持在91％左右,TA去除率保持在94％左右。低pH废水冲击和高容积负荷废水冲击时COD,TA去除率均明显下降,恢复正常讲水后3～4d,COD,TA去除率均恢复正常。     

汉江与嘉陵江源区黄土的风化成土强度及其在土壤系统分类中的归属

以汉江源区(李家河村)和嘉陵江源区(杨家山村)黄土剖面为研究对象,对其粒度、元素组成、团聚体等进行分析与对比,探究两地土壤成土强度与系统分类归属.结果表明两江源区的土壤风化成土特征级类明显不同:(1)两地土壤团聚体主要分布在0.25～1 mm范围内,但汉江源区(LJH)土壤上部的大团聚体含量R0.25值(83.73％)、平均重量直径MWD值(2.17)和几何平均直径GMD值(1.11)均大于嘉陵江源区(YJS)的土壤(其R0.25值为69.81％,MWD和GMD值分别为1.06、0.47),团聚体稳定性更强,而剖面中下部则相反,土体稳定性弱于后者;(2)嘉陵江源区土壤的风化程度仅达到低等向中等强度过渡阶段,与其相比,汉江源区土壤的钾钠比值和残积指数较高、硅铝铁率和淋溶系数较低,钙、钠等易溶元素风化淋失更强,产生的富铝黏土矿物更多,达到中等风化强度,故后者风化成土强度远大于前者;(3)在土壤系统分类中,汉江源区黄土母质发育的土壤可归为斑纹简育湿润淋溶土,嘉陵江源区土壤可归为普通钙积干润淋溶土.     

Analysis of 3-year observations of CFC-11, CFC-12 and CFC-113 from a semi-rural site in China

In-situ measurements of atmospheric chlorofluorocarbons (CFCs) can be used to the assess their global and regional emissions and to check for compliance with phase-out schedules under Montreal protocol and its amendments. The atmospheric mixing ratios of CFC-11 (CCl₃F), CFC-12 (CCl₂F₂) and CFC-113 (CCl₂F–CClF₂) have been measured by an automated in-situ GC-ECDs system at the regional Chinese Global Atmosphere Watch (GAW) station Shangdianzi (SDZ), from November 2006 to October 2009. The time series for these three principal CFCs showed large episodic events and background conditions occurred for approximately 30% (CFC-11), 52% (CFC-12) and 56% (CFC-113) of the measurements. The mean background mixing ratios for CFC-11, CFC-12 and CFC-113 were 244.8 ppt (parts per trillion, 10^?12, molar) 539.6 ppt and 76.8 ppt, respectively, for 2006–2009. The enhanced CFC mixing ratios compared to AGAGE sites such as Trinidad Head (THD), US and Mace Head (MHD), Ireland suggest regional influences even during background conditions at SDZ, which is much closer to highly-populated areas. Between 2006 and 2009 background CFCs exhibited downward trends at rates of ?2.0 ppt yr^?1 for CFC-11, ?2.5 ppt yr^?1 for CFC-12 and ?0.7 ppt yr^?1 for CFC-113. De-trended 3-year average background seasonal cycles displayed small fluctuations with peak-to-trough amplitudes of 1.0 ± 0.02 ppt (0.4%) for background CFC-11, 1.3 ± 2.1 ppt (0.3%) for CFC-12 and 0.2 ± 0.4 ppt (0.3%) for CFC-113. On the other hand, during pollution periods these CFCs showed much larger seasonal cycles of 11.2 ± 10.7 ppt (5%) for CFC-11, 7.5 ± 6.5 ppt (2%) for CFC-12 and 1.0 ± 1.2 ppt (1.2%) for CFC-113, with apparent winter minima and early summer maxima. This enhancement was attributed to prevailing wind directions from urban regions in summer and to enhanced anthropogenic sources during the warm season. In general, horizontal winds from northeast showed negative contribution to atmospheric CFCs loading, whereas South Western advection (urban sector: Beijing) had positive contributions.