杭州市地面水中多环芳烃污染现状及风险

用HPLC和化学分析法,监测了1999～2002年丰水期和枯水期杭州市地面水中10种多环芳烃(PAHs)的含量和COD、BOD5等常规指标.结果表明,10种PAHs浓度范围为0.989～96.21g/L,平均浓度30.82g/L;BaP平均浓度为1.582g/L,污染较为严重;地面水中PAHs浓度和检出率均为丰水期高于枯水期;COD、BOD₅与PAHs总浓度之间没有相关性,因而不能反映地面水PAHs污染的风险;BeP、BaP与PAHs总浓度之间具有较好的线性相关,可作为水体PAHs污染的代表物.常规的自来水处理工艺不能有效地去除源水中微量PAHs等有机污染物,因此地面水特别是饮用源水PAHs污染存在较大的健康风险.     

对壳牌石油公司HSE管理体系的几点认识

通过介绍壳牌石油公司建立 ＨＳＥ管理体系的背景和目标,对照我国行业标准 ＳＹ／Ｔ６２６７—１９９７,分析了该公司ＨＳＥ体系的技术特点,详细地讨论了危害和影响管理过程（ＨＥＭＰ）在ＨＳＥ管理体系中的地位和作用。指出,壳牌公司在废弃物管理中采用的分级政策和记帐政策颇具特色,值得借鉴。     

推广国际化学品安全卡促进化学工业持续健康发展

国际化学品安全卡（ＩＣＳＣ）是联合国国际化学品;安全规划处（ＩＰＣＳ）与欧洲聪明委员会合作编写的一套权威性化学品信息卡片。文中论述了推广使用ＩＣＳＣ的重要意义,介绍了安全卡的内容以及如何正确使用ＩＣＳＣ。     

浅议废水生物处理过程中环境因子、生物相与运行效果之间的相关性

阐述了在废水生物处理过程中环境因子、生物相与运行效果三者之间存在着一定的相关性,同时指出了生物指示物的局限性,对于工程调试和提高生物处理的效果,有着很重要的指导意义.     

Cryptic prey colouration increases search time in brown trout (<Emphasis Type="Italic">Salmo trutta</Emphasis>): effects of learning and body size

Little is known about how cryptic colouration influences prey search in near-surface aquatic habitats, although such knowledge is critical for understanding the adaptive value of colour crypsis as well as the perceptive constraints influencing foraging behaviour in these environments. This study had two main aims: (1) to investigate how background colour matching by prey affects foraging efficiency by brown trout parr and (2) to investigate how foraging ability on cryptic and conspicuous prey is affected by fish size at age (reflecting dominance). We addressed these questions by training wild brown trout parr to forage individually on live brown-coloured maggots on a cryptic (brown) or conspicuous (green) background. A separate experiment confirmed the absence of trout preference for brown or green substrate. The results show that prey background colour matching increases search time in brown trout. Search time generally decreased by learning, but conspicuous prey remained an easier prey to find throughout the six training trials. Thus, perceptive constraints appear to limit search efficiency for cryptic prey, suggesting that cryptic colouration can confer survival benefits to prey in natural environments. Smaller fish generally found conspicuous prey faster than larger individuals, whereas search time for cryptic prey was not influenced by body size. This suggests that smaller individuals compensate for inferior competitive ability by increasing foraging activity rather than improving cognitive ability. The technique of varying cognitive demands in behavioural tasks could be used more in future studies aimed at distinguishing motivational effects from cognitive explanations for variation in behavioural performance.     

现代生活垃圾卫生填埋场的研究现状及存在的问题

现代生活垃圾卫生填埋场是处理生活垃圾的一个最有效、最安全的方法,国内外学者针对与垃圾填埋场相关的岩土工程问题已经做了大量的研究工作,但是仍然有很多问题没有引起足够的关注。在此总结国内外学者研究现状的基础上提出了需要进一步研究的一系列问题,并在初步研究的基础上提出了一些预防建议。     

电力行业二氧化硫排放控制现状、费用及对策分析

系统地研究了国家级层面上的30多个法规、政策、规划和文件对火电厂二氧化硫排放的控制要求及存在问题,提出了现行政策还不完善之处.通过对典型石灰石-石膏湿法烟气脱硫费用的研究,提出了4个费用估算预测公式.研究表明,煤的含硫量对脱除每kg二氧化硫的费用影响最为敏感.提出清理修订现行法规及政策,加快实施二氧化硫在电力行业内的排放总量平衡和排放权交易政策,鼓励发电企业依法自主选择治理措施;出台火电厂二氧化硫治理优惠经济政策,规范脱硫产业化发展等的建议.      

中国居民及动植物的环境激素暴露研究现状和建议

环境激素污染严重威胁着人类及动植物的健康。综述了EDCs生物危害,简要介绍了美国、日本和欧盟的EDCs研究工作,分析了中国居民和动植物的EDCs暴露现状,归纳了现有的流行病学调查信息,并针对现状提出了建议。     

Nitrogen cycling of atmosphere-plant-soil system in the typical Calamagrostis angustifolia wetland in the Sanjiang Plain, Northeast China

The nitrogen (N) distribution and cycling of atmosphere-plant-soil system in the typical meadow Calamagrostis angustifolia wetland (TMCW) and marsh meadow Calamagrostis angustifolia wetland (MMCW) in the Sanjiang plain were studied by a compartment model. The results showed that the N wet deposition amount was 0.757 gN/(m2·a), and total inorganic N (TIN) was the main body (0.640 gN/(m2·a)). The ammonia volatilization amounts of TMCW and MMCW soils in growing season were 0.635 and 0.687 gN/m2, and the denitrification gaseous lost amounts were 0.617 and 0.405 gN/m2, respectively. In plant subsystem, the N was mainly stored in root and litter. Soil organic N was the main N storage of the two plant-soil systems and the proportions of it were 93.98% and 92.16%, respectively. The calculation results of N turnovers among compartments of TMCW and MMCW showed that the uptake amounts of root were 23.02 and 28.18 gN/(m2·a) and the values of aboveground were 11.31 and 6.08 gN/(m2·a), the re-translocation amounts from aboveground to root were 5.96 and 2.70 gN/(m2·a), the translocation amounts from aboveground living body to litter were 5.35 and 3.38 gN/(m2·a), the translocation amounts from litter to soil were larger than 1.55 and 3.01 gN/(m2·a), the translocation amounts from root to soil were 14.90 and 13.17 gN/(m2·a), and the soil (0-15cm) N net mineralization amounts were 1.94 and 0.55 gN/(m2·a), respectively. The study of N balance indicated that the two plant-soil systems might be situated in the status of lacking N, and the status might induce the degradation of C. angustifolia wetland.     

Topsoil organic carbon mineralization and CO2 evolution of three paddy soils from South China and the temperature dependence

Carbon mineralization and its response to climatic warming have been receiving global attention for the last decade. Although the virtual influence of temperature effect is still in great debate, little is known on the mineralization of organic carbon （SOC） of paddy soils of China under warming. SOC mineralization of three major types of China＇s paddy soils is studied through laboratory incubation for 114 d under soil moisture regime of 70% water holding capacity at 20℃ and 25℃ respectively. The carbon that mineralized as CO2 evolved was measured every day in the first 32 d and every two days in the following days. Carbon mineralized during the 114 d incubation ranged from 3.51 to 9.22 mg CO2-C/gC at 20℃ and from 4.24 to 11.35 mg CO2-C/gC at 25℃ respectively; and a mineralizable C pool in the range of 0.24 to 0.59 gC/kg, varying with different soils. The whole course of C mineralization in the 114 d incubation could be divided into three stages of varying rates, representing the three subpools of the total mineralizable C： very actively mineralized C at 1-23 d, actively tnineralized C at 24--74 d and a slowly mineralized pool with low and more or less stabilized C mineralization rate at 75-114 d. The calculated Q10 values ranged from 1.0 to 2.4, varying with the soil types and N status. Neither the total SOC pool nor the labile C pool could account for the total mineralization potential of the soils studied, despite a well correlation of labile C with the shortly and actively mineralized C, which were shown in sensitive response to soil warming. However, the portion of microbial C pool and the soil C/N ratio controlled the C mineralization and the temperature dependence. Therefore, C sequestration may not result in an increase of C mineralization proportionally. The relative control of C bioavailability and microbial metabolic activity on C mineralization with respect to stabilization of sequestered C in the paddy soils of China is to be further studied.