Kinetic modeling of microbially-driven redox chemistry of radionuclides in subsurface environments: coupling transport, microbial metabolism and geochemistry

Microbial reactions play an important role in regulating pore water chemistry as well as secondary mineral distribution in many subsurface systems and, therefore, may directly impact radionuclide migration in those systems. This paper presents a general modeling approach to couple microbial metabolism, redox chemistry, and radionuclide transport in a subsurface environment. To account for the likely achievement of quasi-steady state biomass accumulations in subsurface environments, a modification to the traditional microbial growth kinetic equation is proposed. The conditions for using biogeochemical models with or without an explicit representation of biomass growth are clarified. Based on the general approach proposed in this paper, the couplings of uranium reactions with biogeochemical processes are incorporated into computer code BIORXNTRN Version 2.0. The code is then used to simulate a subsurface contaminant migration scenario, in which a water flow containing both uranium and a complexing organic ligand is recharged into an oxic carbonate aquifer. The model simulation shows that Mn and Fe oxyhydroxides may vary significantly along a flow path. The simulation also shows that uranium(VI) can be reduced and therefore immobilized in the anoxic zone created by microbial degradation.     

Mobilization of soil organic matter by complexing agents and implications for polycyclic aromatic hydrocarbon desorption

Complexing agents are frequently used in treatment technologies to remediate soils, sediments and wastes contaminated with toxic metals. The present study reports results that indicate that the rate and extent of soil organic matter (SOM) as represented by dissolved natural organic carbon (DNOC) and polycyclic aromatic hydrocarbon (PAH) desorption from a contaminated soil from a manufactured gas plant (MGP) site can be significantly enhanced with the aid of complexing agents. Desorption of DNOC and PAH compounds was pH dependent, with minimal release occurring at pH 2-3 and maximal release at pH 7-8. At pH-6, chelate solutions were shown to dissolve large amounts of humic substances from the soil compared to controls. The complexing agents mobilized polyvalent metal ions, particularly Fe and Al from the soil. Metal ion chelation may disrupt humic (metal ion)-mineral linkages, resulting in mobilization of SOM and accompanying PAH molecules into the aqueous phase; and/or reduce the degree of cross-linking in the soil organic matter phase, which could accelerate PAH diffusion.     

Photocatalytic activity of TiO2 films grown on different substrates

Titanium dioxide films were prepared on glass, indium-tin oxide (ITO) glass and p-type monocrystalline silicon and studied for the photocatalytic degradation of rhodamine B in an aqueous medium. Raman, AFM, and XPS spectroscopic investigations of these films indicated that microstructure of titanium oxide films were greatly affected by the substrate materials. Rutile was confirmed to be easily formed on the surface of ITO glass, and TiO2 tended to grow as closely packed particles that were elongated strips with an average size of 20 nm, and had lovely contrast with the perfectly round particles grown on p-type monocrystalline silicon. Charge transfer between the film and silicon substrate was verified by surface photovoltage spectra. This may be the real reason why the films grown on ITO glass and silicon substrates exhibit higher photocatalytic reactivity than the film on glass substrate. Moreover, the different surface properties also seem to be responsible for the different activity.     

Detection and Molecular Characterization of Human Noroviruses in Korean Groundwater Between 2008 and 2010

RT-PCR, nucleotide sequencing, and phylogenetic analysis were performed for genotyping and molecular characterization of noroviruses isolated from Korean groundwater. Among 160 samples collected from 80 sites between 2008 and 2010, 14 samples (8.7?%) from 12 sites were positive for noroviruses (NoVs). The percentages of NoV-positive samples in 2008, 2009, and 2010 were 22.2, 3.2, and 0?%, respectively, representing a yearly decrease. GII-positive samples (n?=?9, 5.6?%) outnumbered GI-positive samples (n?=?5, 3.1?%). The genotypes of the GI NoVs were GI.2, GI.5, and GI.6, and the genotypes of the GII NoVs were all GII.4. One sample, HM623465, was very similar to CUK-3 and CBNU2 and two GII.4 sequences isolated from the stool of Korean gastroenteritis patients. A BLASTN search revealed several nucleotide sequences highly similar to those of NoVs isolated in this study. The original isolation sources for these similar NoVs were mostly stool (n?=?731, 80.0?%) and groundwater (n?=?135, 14.8?%), and all the countries from which they were isolated were almost in Asia (96.0?%); specifically, China (n?=?192, 21.0?%), Japan (n?=?383, 41.9?%), Korea (n?=?296, 32.4?%), and other Asian countries (n?=?6, 0.7?%). These results suggest that Korean groundwater might be contaminated with NoVs from the stool of infected patients and that these NoVs in turn cause new cases of gastroenteritis through a typical fecal-oral route with region-specific circulation. Therefore, it is important to properly treat sewage, which may include waterborne viruses and manage point sources in groundwater for national health and sanitation. In addition, continuous molecular surveillance remains important for understanding circulating NoVs.     

水溶性有机物电子转移能力与荧光峰强度的关系研究

以不同来源的水溶性有机物（DOM）为供试材料,采用电化学方法和荧光光谱法研究了DOM电子转移能力及其与荧光峰强度的关系.采用库仑安培法测定DOM电子转移能力,其中测得的电子接受能力为635.6～1 049.3μmol.（g.C）-1,电子供给能力为27.3～42.3μmol.（g.C）-1.利用循环伏安法研究DOM电化学活性,发现其氧化还原电位在-731～-996 mV（vs.Ag/AgCl）之间.经过电位跃阶法三次氧化还原循环后电子转移能力仍可维持在232.1～897.2μmol.（g.C）-1之间,电子循环率为36.7%～78.2%,说明DOM具有重复利用、反复转移电子的特性.采用荧光激发发射光谱法（EEMS）测定DOM的类富里酸荧光峰强度并比较其与DOM电子转移能力的关系,发现DOM的类富里酸荧光峰强度与DOM的电子循环率具有显著相关（r2=0.92）.实验结果为理解DOM在元素循环、污染物降解以及生物地球化学循环中的作用提供科学依据.     

Effects of long-term nitrogen addition and precipitation changes on CH4 flux in an alpine steppe北大核心CSCD

土壤是甲烷(CH4)重要的源和汇.氮沉降和降水格局变化正在急剧改变土壤碳循环,进而可能对土壤CH4通量造成深刻影响.高寒生态系统是巨大的碳库,对氮沉降和降水变化十分敏感.然而,目前多数研究集中在短期实验上,缺乏对长期氮沉降和降水变化背景下CH4通量的响应及其调控因素的认识.以青藏高原高寒草原为研究对象,在2013年搭建模拟氮沉降和降水格局改变实验平台.基于静态箱–气相色谱法测定2020年生长季(5-10月)土壤CH4通量.结果显示,高寒草原土壤呈CH4的汇.氮添加没有显著改变生长季和植物生长高峰CH4通量.然而,降水变化显著改变了生长季和植物生长高峰CH4通量,其中降水增加(+50%降水)降低了CH4的吸收(分别为–16%和–45%),降水减少(–50%降水)增强了CH4的吸收(分别为+73%和+33%).进一步研究发现,与植物属性和功能基因丰度相比,土壤环境因子主导了CH4通量变化(解释率>90%).其中CH4通量与土壤含水量和温度显著正相关,与土壤pH显著负相关.综上所述,在未来全球变化情景下,降水格局改变更能调节青藏高原高寒草原CH4通量的变化.(图6表1参37)     

Interannual variation of ichthyoplankton density and species composition in the waters off northeastern Taiwan

The ichthyoplankton in the waters of northeastern Taiwan have been studied since 1989. Based on collections in August 1989 to 1991, this report treats primarily the annual variation of ichthyoplankton density, species composition and assemblage diversity among the waters of the East China Sea, the Kuroshio and the mixing zone. The ranges of average densities found for fish eggs were 7 to 3897 ind 1000 m^-3 and 0.02 to 1.43 g 1000 m^-3, for ichthyoplankton 154 to 1364 ind 1000 m^-3 and 0.33 to 3.23 g 1000 m^-3, and for zooplankton 52 to 532 g 1000 m^-3. An interannual comparison indicates a tendency towards a decrease in ichthyoplankton density from 1989 to 1991. In total, 5803 individuals assigned to at least 91 families and 254 taxa at species level were collected. Lantern fish form the most common species group (Benthosema pterotum: 12.1%; Diaphus pacificus: 4.2%). The other species in order of frequency are: gobies (5.8%); Callionymus sp. (3.4%); Auxis spp. (3.1%); Trachinocephalus myops (3.0%); Nibea sp. (2.8%); Synagrops philippinensis (2.3%); Priacanthus macracanthus (2.2%); and percophid (2.0%). The relative frequency of the ten most abundant taxa fluctuated annually. Neither interannual distinction nor interannual correlation was confirmed by statistical analysis, but intra-annual rank correlations were established among the water masses. A weak tendency towards increasing diversity from 1989 to 1990 and little diversity in the mixing zone were observed. We conclude that there is a complex inter-dependence of assemblages from the waters of northeastern Taiwan.