Isotopic modelling of the significance of bacterial sulphate reduction for phenol attenuation in a contaminated aquifer

A Triassic sandstone aquifer polluted with a mixture of phenolic hydrocarbons has been investigated by means of high-resolution groundwater sampling. Samples taken at depth intervals of 1 m have revealed the presence of a diving pollutant plume with a sharply defined upper margin. Concentrations of pollutant phenols exceed 4 g/l in the plume core, rendering it sterile but towards the diluted upper margin evidence for bacterial sulphate reduction (BSR) has been obtained. Groundwaters have been analysed for both delta34S-SO4 and delta18O-SO4. Two reservoirs have been identified with distinct sulphate oxygen isotope ratios. Groundwater sulphate (delta18O-SO4 = 3-5/1000) outside the plume shows a simple linear mixing trend with an isotopically uniform pollutant sulphate reservoir (delta18O-SO4 = 10-12/1000) across the plume margin. The sulphur isotope ratios do not always obey a simple mixing relation, however, at one multilevel borehole, enrichment in 34SO4 at the plume margin is inversely correlated with sulphate concentration. This and the presence of 34S-depleted dissolved sulphide indicate that enrichment in 34SO4 is the result of bacterial sulphate reduction. Delta34S analysis of trace hydrogen sulphide within the plume yielded an isotope enrichment factor (epsilon) of -9.4/1000 for present-day bacterial sulphate reduction. This value agrees with a long-term estimate (-9.9/1000) obtained from a Rayleigh model of the sulphate reduction process. The model was also used to obtain an estimate of the pre-reduction sulphate concentration profile with depth. The difference between this and the present-day profiles then gave a mass balance for sulphate consumption. The organic carbon mineralisation that would account for this sulphate loss is shown to represent only 0.1/1000 of the phenol concentration in this region of the plume. Hence, the contribution of bacterial sulphate reduction to biodegradation has thus far been small. The highest total phenolic concentration (TPC) at which there is sulphur isotope evidence of bacterial sulphate reduction is 2000 mg/l. We suggest that above this concentration, the bactericidal properties of phenol render sulphate-reducing bacteria inactive. Dissolved sulphate trapped in the concentrated plume core will only be utilised by sulphate reducers when toxic phenols in the plume are diluted by dispersion during migration.     

Reactive transport modeling of processes controlling the distribution and natural attenuation of phenolic compounds in a deep sandstone aquifer

Reactive solute transport modeling was utilized to evaluate the potential for natural attenuation of a contaminant plume containing phenolic compounds at a chemical producer in the West Midlands, UK. The reactive transport simulations consider microbially mediated biodegradation of the phenolic compounds (phenols, cresols, and xylenols) by multiple electron acceptors. Inorganic reactions including hydrolysis, aqueous complexation, dissolution of primary minerals, formation of secondary mineral phases, and ion exchange are considered. One-dimensional (1D) and three-dimensional (3D) simulations were conducted. Mass balance calculations indicate that biodegradation in the saturated zone has degraded approximately 1-5% of the organic contaminant plume over a time period of 47 years. Simulations indicate that denitrification is the most significant degradation process, accounting for approximately 50% of the organic contaminant removal, followed by sulfate reduction and fermentation reactions, each contributing 15-20%. Aerobic respiration accounts for less than 10% of the observed contaminant removal in the saturated zone. Although concentrations of Fe(III) and Mn(IV) mineral phases are high in the aquifer sediment, reductive dissolution is limited, producing only 5% of the observed mass loss. Mass balance calculations suggest that no more than 20-25% of the observed total inorganic carbon (TIC) was generated from biodegradation reactions in the saturated zone. Simulations indicate that aerobic biodegradation in the unsaturated zone, before the contaminant entered the aquifer, may have produced the majority of the TIC observed in the plume. Because long-term degradation is limited to processes within the saturated zone, use of observed TIC concentrations to predict the future natural attenuation may overestimate contaminant degradation by a factor of 4-5.     

苏北地区农业环境问题及管理方案的探讨

配合江苏省“碧海计划”和盐城市海洋经济绿色农业的发展，探讨了现阶段农业环境污染控制的直接政策管理、经济手段和人工生态工程处理三种方案，其中政策管理，如减少化肥农药的施用规定能减少污染，直接经济投入少，但是执行管理成本高，且政策见效慢；经济手段能减少污染，但环境目标达标不确定，且需要完善的市场环境，目前来说，本地区市场机制不完善，会出现“市场失灵”现象；人工湿地生态工程，前期投入大，但管理成本低，环境目标确定，但不能快速削减污染负荷。三种方案各有所长，在实际操作中，应针对不同区域的农业产业状况、方案时间迟度组合使用。     

Microbial reduction of sulfate injected to gas condensate plumes in cold groundwater

Despite a rapid expansion over the past decade in the reliance on intrinsic bioremediation to remediate petroleum hydrocarbon plumes in groundwater, significant research gaps remain. Although it has been demonstrated that bacterial sulfate reduction can be a key electron accepting process in many petroleum plumes, little is known about the rate of this reduction process in plumes derived from crude oil and gas condensates at cold-climate sites (mean temperature <10 degrees C), and in complex hydrogeological settings such as silt/clay aquitards. In this field study, sulfate was injected into groundwater contaminated by gas condensate plumes at two petroleum sites in Alberta, Canada to enhance in-situ bioremediation. In both cases the groundwater near the water table had low temperature (6-9 degrees C). Monitoring data had provided strong evidence that bacterial sulfate reduction was a key terminal electron accepting process (TEAP) in the natural attenuation of dissolved hydrocarbons at these sites. At each site, water with approximately 2000 mg/L sulfate and a bromide tracer was injected into a low-sulfate zone within a condensate-contaminant plume. Monitoring data collected over several months yielded conservative estimates for sulfate reduction rates based on zero-order kinetics (4-6 mg/L per day) or first-order kinetics (0.003 and 0.01 day(-1)). These results favor the applicability of in-situ bioremediation techniques in this region, under natural conditions or with enhancement via sulfate injection.     

Migration behavior of naturally occurring radionuclides at the Nopal I uranium deposit, Chihuahua, Mexico

Oxidation of pyrite at the Nopal I uranium deposit, Peña Blanca district, Chihuahua, Mexico has resulted in the formation of Fe-oxides/hydroxides. Anomalous U concentrations (i.e. several hundred to several thousand ppm) measured in goethite, hematite, and amorphous Fe-oxyhydroxides in a major fracture that crosscuts the deposit and the absence of U minerals in the fracture suggest that U was retained during secondary mineral growth or sorbed on mineral surfaces. Mobilization and transport of U away from the deposit is suggested by decreasing U concentrations in fracture-infilling materials and in goethite and hematite with distance from the deposit. Greater than unity ²³⁴U/²³⁸U activity ratios measured in fracture-infilling materials indicate relatively recent ( < 1 Ma) U uptake from fluids that carried excess ²³⁴U. Systematic decreases in ²³⁴U/²³⁸U activity ratios of fracture materials with distance from the deposit suggest a multistage mobilization process, such as remobilization of U from ²³⁴U-enriched infill minerals or differential or diminished transport of U-bearing solutions containing excess ²³⁴U.     

Molecular characterization of effluent organic matter in secondary effluent and reclaimed water: Comparison to natural organic matter in source water

Municipal wastewater reclamation is becoming of increasing importance in the world to solve the problem of water scarcity. A better understanding of the molecular composition of effluent organic matter(Ef OM) in the treated effluents of municipal wastewater treatment plants(WWTPs) is crucial for ensuring the safety of water reuse. In this study, the molecular composition of Ef OM in the secondary effluent of a WWTP in Beijing and the reclaimed water further treated with a coagulation–sedimentation–ozonation process were characterized using a non-target Fourier transform ion cyclotron resonance mass spectrometry(FT-ICR MS) method and compared to that of natural organic matter(NOM) in the local source water from a reservoir. It was found that the molecular composition of Ef OM in the secondary effluent and reclaimed water was dominated by CHOS formulas, while NOM in the source water was dominated by CHO formulas. The CHO formulas of the three samples had similar origins. Anthropogenic surfactants were responsible for the CHOS formulas in Ef OM of the secondary effluent and were not well removed by the coagulation-sedimentation-ozonation treatment process adopted.     

2013—2017年《自然资源学报》办刊进展

论文基于2013—2017年中国科学技术信息研究所发布的《中国科技期刊引证报告（核心版）》和《中国科技期刊引证报告（扩刊版）》,《中国学术期刊（光盘版）》电子杂志社有限公司、中国科学文献计量评价研究中心和清华大学图书馆联合发布的《中国学术期刊影响因子年报》以及中国科学院文献情报中心的中国科学引文数据库（CSCD）中统计的《自然资源学报》的总被引频次、影响因子等相关引证指标,分析了近5年来《自然资源学报》一些重要引证指标的变化;同时梳理了《自然资源学报》近5年来被数据库收录情况、获奖情况以及发表的学术论文获奖和被媒体报道、转载情况,总结了2013—2017年间《自然资源学报》的办刊进展。结果表明：1）《自然资源学报》2016年核心影响因子、扩展影响因子和复合影响因子分别达到1.912、2.565、3.250,近5年来的增长率分别达到47.0%、46.4%、33.8%,在资源科学期刊领域排名稳居前列;2）《自然资源学报》已被国内重要数据库和检索系统全部收录,并在2016年被收录在EBSCO最新研发的数据库Academic Search Ultimate;3）2013—2017年间,《自然资源学报》共获得了15项学术期刊领域奖项,2013—2017年连续获得中国科协精品科技期刊工程项目支持,并于2014、2015年获得中国科学院科学出版三等基金资助;4）2013—2017年间,《自然资源学报》共有65篇论文入选中国精品科技期刊顶尖学术论文,多篇论文被媒体报道和转载。通过对2013—2017年《自然资源学报》发展状况的分析,为期刊未来的发展提供科学依据,为我国资源科学期刊质量的提升提供参考。     

工频电磁场环境管理目标值的研究

介绍了国外工频电磁场对人体影响的最新研究进展,收集了国内外工频电磁场的限制标准,结合南方沿海某城市近年来工频电磁场投诉的热点和难点,针对问题研究防治对策,提出了深圳市工频电磁场的环境管理目标值。     

浅谈节约型城市的构建

构建节约型社会是实现城市可持续发展的必然要求。节约型城市的构建应通过转变经济增长模式、推行循环经济、加强节能科技的创新,发展替代能源,同时结合政策手段、宣传教育和法律手段来实现。