上海水源水库产2-MIB生物总量评估方法与应用

本研究开展了蓝藻产2-MIB功能基因mic的qPCR定量分析,对上海水源水库中的mic基因进行长期调研.结果表明,在长江水源水库和黄埔江水源水库中mic基因都有检出.在夏季其丰度达到峰期,基因拷贝数达到10~7～10~8 copies·L~(-1).分析表明mic基因拷贝数与蓝藻、伪鱼腥藻细胞密度、2-MIB浓度之间均存在相关性.因此通过mic基因定量进而推断水中产嗅生物总量的方法,可代替繁琐、重现性低的显微镜镜检过程.应用中还需更多实践,结合其他指标改进准确度.     

油藏厌氧微生物研究进展

地下深层油藏是独特的缺氧环境,目前还没有直接的微生物学证据表明油藏中存在真正意义上的“本源微生物”,但经注水开发后的油藏中确实蕴藏着复杂的微生物区系.油藏性质决定了油藏厌氧微生物特殊的群落结构,而油藏微生物的作用也可以改变油藏的理化及地质学特性.油藏中厌氧微生物按生理类群主要可分为发酵细菌、硝酸盐还原菌、铁还原菌、硫酸盐还原菌和产甲烷古菌.本文综述了国内外近年来油藏微生物学的研究进展,简述了微生物分子生态学在油藏微生物学研究中的应用,并对当前的研究提出了一些思考.图1参37     

Diffuse pollution: A hidden threat to the water environment of the developing world

This Special Section collects eight articles from the 16th IWA International Conference on Diffuse Pollution and Eutrophication （16th DIPCON）, which was held in Beijing on 18 to 23 August, 2013. These articles focus on the diffuse pollution problems encountered in the development process.     

ROAD DE-ICING SALTS IN AN URBAN STREAM AND FLOOD CONTROL RESERVOIR1

ABSTRACT: High concentrations of chloride and sodium were found in the bottom layers of a new flood control reservoir at the beginning of winter thaw periods. The reservoir had a number of significant downstream impacts. After short thaw periods, discharge from the bottom of the reservoir tended to cause higher salt concentrations downstream in comparison with upstream sites. During long thaw periods or when large quantities of rain fell, downstream salt concentrations were considerably less than upstream values. Average chloride and sodium content of soil at the bottom of the reservoir more than doubled as a result of impounding runoff waters for one winter.     

华中地区水库沉积物重金属抗性基因的赋存特征及影响因素分析

环境中重金属抗性基因（Metal resistance genes,MRGs）的迁移转化作为环境及生态领域的重要研究内容近年来备受关注,但目前环境中重金属是否是MRGs的重要驱动因素则尚不明确.本研究采用宏基因组技术对华中地区水库沉积物MRGs进行了定量,并分析了不同形态重金属在MRGs迁移转化过程中起到的作用.结果表明,trcop （抗Cu基因）及arsM （抗砷基因）是水库环境中的主要MRGs,供水水库之间MRGs分布并无地域性差异.czrA （多抗基因）的潜在宿主菌较为广泛,trcop及arsM很可能位于同一种可移动遗传元件上进行水平转移.重金属总量与MRGs之间并无明显联系,而可交换态及碳酸盐结合态（B1）则是环境中MRGs的重要驱动因素.     

高铁酸盐预处理湖泊水库水的研究进展

从高铁酸钾的性质出发,概述了高铁酸钾及其复合药剂预处理湖泊水库水的影响因素,展望了这一领域的发展情况.     

MANGANESE OXIDATION RELATED TO THE RELEASES FROM RESERVOIRS1

ABSTRACT: Stratified reservoir waters frequently contain objectionable quantities of dissolved manganese. The oxidation and removal of dissolved manganese during transport below Normandy Dam, Tennessee, was shown to be much more rapid than expected from chemical oxidation. Oxidation took place in only a day of travel time rather than months or years. Laboratory studies showed that removal was associated with a slime found on rock surfaces below the dam and led to the development of column technology as a possible method of treating natural waters containing manganese. Hydraulic loadings on the columns in the range of 390–780 m³/hr.ha accomplished a 90 percent removal rate of soluble manganese over an influent concentration range of 2 to 15 mg/l.     

PRELIMINARY HYDROLOGIC DESIGN OF SMALL FLOOD DETENTION RESERVOIRS1

ABSTRACT. Flood detention reservoir design is a common problem encountered by engineers and others involved with water resources problems. This paper presents a method by which the volume of flood storage required for a single reservoir or a series of reservoirs may be estimated without using numeric flood-routing techniques. The proposed procedure requires a minimum of computations and is most applicable to preliminary design situations where a high degree of accuracy is not required.     

PRIMARY PRODUCTIVITY AND PLANKTON COMMUNITIES IN A TWO-RESERVOIR SERIES1

ABSTRACT: It is suggested that new impoundments undergo an initial period of trophic upsurge lasting one to three years because of organic detritus and inorganic nutrients from the inundated basin. The new Monksville Reservoir in Passaic County, New Jersey, provided an opportunity to study the accelerated transformation of the Wanaque River into a 200-ha lake and to compare productivity with the older Wanaque Reservoir located immediately downstream. A one-year investigation of both reservoirs was conducted during 1988. The primary productivity (0.547 g C m^?2 d^?1) of the new Monksville Reservoir was not significantly different from that of the established Wanaque Reservoir (0.668 g C m^?2 d^?1). Mean surface chlorophyll a concentrations were similar (3.0–4.0 μg 1^?1), although the Monksville Reservoir exhibited more pronounced chlorophyll peaks in spring and late autumn. Phytoplankton and zooplankton populations were consistently larger and fluctuated sharply in the Monksville Reservoir. Both reservoirs became thermally stratified, but only the Monksville Reservoir developed a metalimnetic dissolved oxygen minimum. The results demonstrated that the predicted trophic upsurge in the new reservoir did not occur in the first year therefore, the ecosystem dynamics did not fit the model for larger reservoirs.