富硫沉积生境中微生物群落的垂直分布特征

为探讨富硫沉积环境中特定微生物类群对硫循环的贡献,人工建立富含硫酸盐的模型,对模型中各种环境化学参数进行监测,并采用不依赖于培养的微生物分子生态学技术对微生物群落垂向分布特征进行解析.结果表明,以沉积物-水界面为分界线,上层水相为好氧环境,硫化物浓度较底;而沉积物相中硫化物浓度较高,为厌氧生境.微生物群落分布与环境特征具有很好的吻合性,沉积物相中微生物群落相似性较高,多样性相对较低,而水相中微生物多样性较高,且与沉积物中微生物分离距离较大.在水-沉积物垂向剖面中,细菌域中的变形菌门(Protebacteria)(丰度为7.6%~32.8%)、绿弯菌门(Chloroflexi)(13.6%~22.3%)以及古菌域中的广古菌门(Euryarchaeota)(19.3%~29.2%)是微生物群落中的绝对优势类群.在该生境中,存在微生物主导的硫循环过程,在厌氧沉积物表层,δ变形菌纲(Deltaprotebacteria)中的硫酸盐还原细菌还原硫酸盐产生硫化物,同时降解有机质.硫化物向上层扩散时,被Thiobacillus、Acidithiobacillus和Halothiobacillus等属的硫氧化微生物氧化为单质硫,并进一步氧化为硫酸盐,在硫循环过程中有机质被逐渐降解.特定微生物种群的富集需要在不同的环境因素,多种微生物共同参与硫循环过程,完成有机质降解.     

桂南地下热水系统中氟的分布及迁移富集规律

选取广西桂南地区地下热水系统为研究对象,利用氢氧同位素及锶同位素研究手段,对研究区内地下热水中氟的空间分布规律及其控制因素进行研究。结果表明:研究区内地下热水中氟含量变化范围为0.01~17.93mg/L,其中43%地下水样品中氟含量超过饮用水氟骨症临界值1.5mg/L,高氟地下热水的主要水化学类型为Na-HCO3型,水体中氟含量与温度呈明显正相关性;地下热水氢氧同位素特征显示,研究区地下热水的主要来源为大气降水,同时受一定程度蒸发浓缩及水-岩作用影响,地下热水锶同位素特征显示,研究区地下热水水化学组成明显受长石、云母等铝硅酸盐风化及碳酸盐岩溶解影响;对地下热水水化学开展的因子分析结果显示,研究区地下热水系统中影响氟迁移释放的主要因素为萤石的溶解与沉淀过程。     

过氧化氢除藻及相关环境条件优化

采用室内培养的方式,通过正交试验研究了H_2O_2质量浓度、光照、pH值和温度4个因素复合作用对铜绿微囊藻去除的影响。结果表明,在所设置的各因素梯度范围内,对去除铜绿微囊藻影响最大的因素是H_2O_2质量浓度;光照和pH值对藻细胞数和叶绿素a的去除,以及H_2O_2残留量的影响各不相同;温度对藻细胞数的影响最小,对H_2O_2残留量的影响较小,对叶绿素a质量浓度的影响较大。除藻的最佳组合为A_1B_2C_3D_2,即光照为1 500 lx,H_2O_2质量浓度为50mg/L,pH值为8.5,温度为25℃。     

Endogenous formation of hydrogen cyanide during distillation for the determination of total cyanide

This paper describes how organic compounds and nitrogen compounds induce the formation of hydrogen cyanide during the distillation process. Hydrogen cyanide formation was confirmed by X‐ray diffraction. The formation scheme for hydrogen cyanide from organic compounds is proposed.     

化工生产中硫化氢泄漏事故的预防和处置对策

通过发生在昆明市安宁齐天化肥有限公司的硫化氢中毒事故,提出硫化氢泄漏事故的预防措施及相应的处置方法,同时总结经验教训,提出整改措施,以避免类似事故的再次发生.     

Biogeochemistry of two types of permeable reactive barriers, organic carbon and iron-bearing organic carbon for mine drainage treatment: Column experiments

Permeable reactive barriers (PRBs) are an alternative technology to treat mine drainage containing sulfate and heavy metals. Two column experiments were conducted to assess the suitability of an organic carbon (OC) based reactive mixture and an Fe⁰-bearing organic carbon (FeOC) based reactive mixture, under controlled groundwater flow conditions. The organic carbon mixture contains about 30% (volume) organic carbon (composted leaf mulch) and 70% (volume) sand and gravel. The Fe⁰-bearing organic carbon mixture contains 10% (volume) zero-valent iron, 20% (volume) organic carbon, 10% (volume) limestone, and 60% (volume) sand and gravel. Simulated groundwater containing 380 ppm sulfate, 5 ppm As, and 0.5 ppm Sb was passed through the columns at flow rates of 64 (the OC column) and 62 (the FeOC column) ml d^− 1, which are equivalent to 0.79 (the OC column) and 0.78 (the FeOC column) pore volumes (PVs) per week or 0.046 m d^− 1 for both columns. The OC column showed an initial sulfate reduction rate of 0.4 µmol g (OC)^− 1 d^− 1 and exhausted its capacity to promote sulfate reduction after 30 PVs, or 9 months of flow. The FeOC column sustained a relatively constant sulfate reduction rate of 0.9 µmol g (OC)^− 1 d^− 1 for at least 65 PVs (17 months). In the FeOC column, the δ³⁴S values increase with the decreasing sulfate concentration. The δ³⁴S fractionation follows a Rayleigh fractionation model with an enrichment factor of 21.6‰. The performance decline of the OC column was caused by the depletion of substrate or electron donor. The cathodic production of H₂ by anaerobic corrosion of Fe probably sustained a higher level of SRB activity in the FeOC column. These results suggest that zero-valent iron can be used to provide an electron donor in sulfate reducing PRBs. A sharp increase in the δ¹³C value of the dissolved inorganic carbon and a decrease in the concentration of HCO₃⁻ indicate that hydrogenotrophic methanogenesis is occurring in the first 15 cm of the FeOC column.     

Bio-Hydrogen Synthesis from Wastewater by Anaerobic Fermentation Using Microflora

Biological hydrogen production was investigated using biomass in palm oil mill effluent (POME) and artificial wastewater containing 10g glucose under anaerobic fermentation in a batch process. Activated POME sludge and different types of composts were collected as sources of inocula for the study. The anaerobic microflora was found to yield significant amounts of hydrogen. The experimental results show that the gas composition contained hydrogen (66–68%) and carbon dioxide (32–34%). Through out the study, methane gas was not observed in the evolved gas. The hydrogen production was accompanied with the formation of acetate and butyrate. Furthermore, the cumulative hydrogen data were fitted to a simple model developed from Gompertz Equation, where the lag phase time, hydrogen production potential and hydrogen production rate at various conditions were quantitatively estimated.     

Persistence of fensulfothion in a sandy‐loam soil and uptake by rutabagas,carrots and radishes using microplots

Abstract

Field microplots were treated with 141 and 282 ppm fensulfothion and 37.1 and 74.2 ppm fensulfothion sulfone. These concentrations are equivalent to field treatment rates of 8.48 and 16.96 kg Al/ha, fensulfothion, and 2.23 and 4.47 kg Al/ha, fensulfothion sulfone, respectively, for banded application (10 cm wide, rows 80 cm apart). The half‐lives in a sandy loam soil were 30–39 and 14–23 days, respectively. Fensulfothion sulfone and sulfide were the main derivatives found in fensulfothion treated soil.

The maximum levels of these derivatives were 21.22 and 22.95 ppm, respectively for the 8.48 kg/ha treatment and 33.90 and 42.45 ppm, respectively, for the higher treatment, which occurred between 30–60 days.

Carrots appeared to take up more fensulfothion from soil than rutabagas or radishes. The residue levels at harvest decreased in the order carrot peel > pulp > rutabagas root > peel > pulp. Residue levels of fensulfothion and sulfone in radishes were similar to those found in rutabagas. The ratio sulfoxide/sulfone in rutabagas ranged from 0.4–1.5 and in carrots from 1.7–7.6. This phenomenon is thought to be due to oxidative enzyme systems present in rutabagas. Dimethyl phosphorothioic acid, but not dimethyl phosphoric acid was detected (max. 1.33 ppm) in some rutabagas samples but not in carrots.     

制冷剂二氟甲烷热解生成氟化氢的实验研究

空调制冷剂二氟甲烷(R32)是R22的替代制冷剂之一,其分子中含有氟元素,受热可产生剧毒物质氟化氢(HF),一旦泄漏分解,将会对人员造成极大危害.首次通过实验研究了R32泄漏后的受热分解情况,利用激光气体分析仪,测量了不同工况下HF的实时浓度,分析了R32受热分解的影响因素.结果表明R32泄漏后,在受热状态下很容易产生HF,HF浓度随着泄漏量和受热状态的变化而异,浓度可达1000ppm以上；研究结果可为含氟制冷剂的应用提供技术支持.     

常温下铁的硫化产物自燃性

含硫油品储运过程中H2S腐蚀产物是常温下硫铁化合物的主要来源,以H2S与铁粉反应制备的硫铁化合物来模拟设备内H2S的腐蚀产物,利用自然氧化的方法测定了硫化反应产物的一次氧化升温和二次氧化升温,考察了铁粉含水量对硫化反应及硫化反应产物自燃性的影响,采用XRD和SEM手段对硫化反应产物进行了表征。结果表明:H2S与铁粉的硫化反应产物为FeS,呈微小颗粒状,覆盖在铁粉表面;硫化反应产物具有自燃性,一次氧化升温最高达到87℃;未被完全氧化的硫化反应产物密封放置一段时间后自燃性明显增加,其二次氧化升温速率最高超过39℃/min;铁粉中含有适量的水可以增加硫化反应速率,提高硫化反应产物的自燃性。