大型海藻与赤潮微藻以及赤潮微藻之间的相互作用研究

研究了2种大型海藻石莼(Ulva pertusa)和江蓠(Gracilaria lemaneiformis)对2种赤潮微藻:东海原甲藻(Prorocentrumdonghaiense)和塔玛亚历山大藻(Alexandum tamarense)生长的影响以及2种微藻之间的相互作用,结果发现:①在大藻(石莼或江蓠)-微藻(东海原甲藻或塔玛亚历山大藻)的共培养体系中,石莼和江蓠均能明显影响与其共培养的微藻的生长,石莼对微藻生长的影响强于江蓠的作用.②在东海原甲藻-塔玛亚历山大藻的双藻培养体系中,东海原甲藻的生长受到明显的抑制作用,最终被完全灭杀;体系中塔玛亚历山大藻的生长未受到明显的影响.另外,塔玛亚历山大藻的培养液滤液能明显抑制东海原甲藻的生长,但东海原甲藻滤液对塔玛亚历山大藻的生长几乎没有影响.实验室条件下模拟二者相互作用的结果显示,塔玛亚历山大藻对东海原甲藻的抑制作用是其被后者抑制作用的17倍左右.③在大藻(石莼或江蓠)-东海原甲藻-塔玛亚历山大藻的多藻培养体系中,东海原甲藻和塔玛亚历山大藻的生长变化与它们在共培养体系中的变化非常类似.半数致死时间(LT50)法的检测结果显示:多藻培养体系对东海原甲藻的联合作用是协同作用,而对塔玛亚历山大藻的作用是相加作用.     

闭坑铅锌矿区地下水—矿坑水水化学特征及成因分析

矿山关闭后,水位迅速回弹升高,区域水动力场发生改变进而影响到水化学场的演变,并伴随着严重的区域水环境问题。为研究闭坑矿区水体水化学特征和成因,系统采集丰水期、枯水期背景点、地下水和矿井水样测定现场参数、δ¹⁸O和δD值、主量离子等,综合利用多元统计分析、同位素示踪和水化学计量分析等分析方法开展不同水体的水化学特征及成因分析。结果表明,(1)δ¹⁸O和δD组成说明研究区地下水和矿井水主要来源为大气降水,且受到了不同程度的蒸发影响;同一季节内背景点、地下水、矿井水同位素组成具有分区聚集性,丰水期同位素相对亏损,枯水期相对富集,表明不同水体水力联系密切;分层聚类分析和水化学同样揭示了不同含水层之间存在密切的水力联系。(2)研究区水化学具有较大差异。背景点、地下水、矿井水TDS取值范围分别为44.18—138.86、43.39—6 917.6、3 329.22—4 174.20 mg·L^-1,从淡水到咸水均有分布;p H取值范围分别为4.39—8.2、2.75—7.9、2.87—2.92,呈酸性、弱酸性、中性、弱碱性。水化学类型...     

重金属Zn、Pb和Cd对可口革囊星虫的急性毒性作用

研究了必需元素Zn及非必需元素Pb、Cd对可口革囊星虫(Phascolosoma esculenda)的急性毒性作用,得到Zn2 的48 h LC50和96 h LC50分别为61.09、10.91 mg/L;pb2 的48 h LC50和96 h LC50分别为29.44、10.59 mg/L;Cd2 的48 h LC50和96hLC50分别为10.69、4.46mg/L.估算得到Zn、Pb和Cd对可口革囊星虫的安全浓度分别为0.55、0.53和0.22mg/L.     

史和平：确保旅客走了走好

本刊讯1月12B,副省长史和平带领省有关部门负责人,来到南京的铁路和公路运输窗口,检查春运组织安排情况。他要求,各地、各有关部门和单位要高度重视,切实抓好2009年春运各项工作,确保旅客走得平安有序,走了走好。在中央门汽车站,他勉励工作人员为大家做好春运服务;在板桥汽渡,他要求汽渡方面落实好防冻、防滑等安全措施,发挥好过江通道的保障作用。     

施用不同磷肥对植烟土壤中磷的淋失和有效磷的影响

采用土柱淋溶模拟试验和室内培养试验,研究不同磷肥施入土壤后磷的淋失和有效磷的变化.结果表明,在施磷量为35 mg/kg条件下,整个淋洗期间,钙镁磷肥、磷酸二氢钙、磷酸一氧铵、磷酸二氢铵、磷酸二氢钾5种肥料磷的淋失率很低;各处理从上而下各层土壤的Olsen-P质量比略有增加.施磷量为60 mg/kg、110 mg/kg、170mg/kg、230 mg/kg时.潮砂田肥料磷的淋失率分别为0.26%、0.74%、2.12%和3.17%;灰泥田肥料磷的淋失率分别为0.79%、1.31%、1.60%和1.94%.钙镁磷肥施人各种土壤后,随着培养时间的延长,土壤有效磷质量比逐渐增加,80 d后达到峰值并趋于稳定;磷酸二氢钾、磷酸二氧铵、磷酸一氢铵和磷酸二氢钙施人上壤后,土壤有效磷质量比逐渐降低,至培育60 d后.变化趋于平缓.不同土壤类型对磷的吸附固定率从大到小为潮砂田、灰泥田.     

起升机构正反向接触器故障电动机失电重物失控坠落的保护分析

辽宁清河特殊钢有限公司发生4．18特大事故后,引起全国广泛讨论．怎样从设备本质安全上防止和杜绝类似事故的发生。在此,笔者根据自身的实践,谈谈自己的观点。进行一下分析。     

内分泌干扰物对机体脂质代谢的影响及其机制研究进展

近年来许多动物实验研究表明,内分泌干扰物(endocrine disrupting chemicals,EDCs)暴露除了会损伤生殖、免疫和神经系统等,还能够干扰脂质代谢,增加肥胖、非酒精性脂肪肝和高脂血症等疾病的发病风险.笔者总结了多种EDCs对不同动物模型(哺乳动物、硬骨鱼类、两栖动物)脂质代谢的影响,主要包括促进...     

Aerobic degradation of methyl tert-butyl ether by a Proteobacteria strain in a closed culture system

The contamination of methyl ten-butyl ether （MTBE） in underground waters has become a widely concerned problem all over the world. In this study, a novel dosed culture system with oxygen supplied by H2O2 was introduced for MTBE aerobic biodegradation. After 7 d, almost all MTBE was degraded by a pure culture, a member of β-Proteobacteria named as PMI, in a closed system with oxygen supply, while only 40% MTBE was degraded in one without oxygen supply. Dissolved oxygen （DO） levels of the broth in closed systems respectively with and without H2O2 were about 5-6 and 4 mg/L. Higher DO may improve the activity of monooxygemase, which is the key enzyme of metabolic pathway from MTBE to tert-butyl alcohol and finally to CO2, and may result in the increase of the degrading activity of PM1 cell. The purge and trap GC-MS result of the broth in closed systems showed that tea-butyl alcohol, isopronol and acetone were the main intermediate products.     

Sludge concentration dynamic distribution and its impact on the performance of UNITANK

UNITANK is a biological wastewater treatment process that combines the advantages of traditional activated sludge process and sequencing batch reactor, which is divided into Tank A, B and C. In this study, the sludge distribution and its impact on performance of UNITANK were carried out in Liede Wastewater Plant （WWTP） of Guangzhou, China. Results showed that there was a strong affiliation between Tank A and B of the system in sludge concentration distribution. The initial sludge concentration in Tank A could present the sludge distribution of the whole system. The sludge distribution was mainly influenced by hydraulic condition. Unsteady sludge distribution had an impact on variations of substrates in reactors, especially in decisive reactor, and this could lead to failure of system. Settler could partially remove substrates such as COD and NO3-N, but there was adventure of sludge deterioration. The rational initial sludge concentration in Tank A should be 4000-6000 mg/L MLSS.     

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.