Research and application of method of oxygen isotope of inorganic phosphate in Beijing agricultural soils

Phosphorus (P) in agricultural ecosystems is an essential and limited element for plants and microorganisms. However, environmental problems caused by P accumulation as well as by P loss have become more and more serious. Oxygen isotopes of phosphate can trace the sources, migration, and transformation of P in agricultural soils. In order to use the isotopes of phosphate oxygen, appropriate extraction and purification methods for inorganic phosphate from soils are necessary. Here, we combined two different methods to analyze the oxygen isotopic composition of inorganic phosphate (δ¹⁸O_P) from chemical fertilizers and different fractions (Milli-Q water, 0.5 mol L^?1 NaHCO₃ (pH = 8.5), 0.1 mol L^?1 NaOH and 1 mol L^?1 HCl) of agricultural soils from the Beijing area. The δ¹⁸O_P results of the water extracts and NaHCO₃ extracts in most samples were close to the calculated equilibrium value. These phenomena can be explained by rapid P cycling in soils and the influence of chemical fertilizers. The δ¹⁸O_P value of the water extracts and NaHCO₃ extracts in some soil samples below the equilibrium value may be caused by the hydrolysis of organic P fractions mediated by extracellular enzymes. The δ¹⁸O_P values of the NaOH extracts were above the calculated equilibrium value reflecting the balance state between microbial uptake of phosphate and the release of intracellular phosphate back to the soil. The HCl extracts with the lowest δ¹⁸O_P values and highest phosphate concentrations indicated that the HCl fraction was affected by microbial activity. Hence, these δ¹⁸O_p values likely reflected the oxygen isotopic values of the parent materials. The results suggested that phosphate oxygen isotope analyses could be an effective tool in order to trace phosphate sources, transformation processes, and its utilization by microorganisms in agricultural soils.     

Linking landscape development intensity within watersheds to methyl-mercury accumulation in river sediments

An indicator of the disturbance of natural systems, the landscape development intensity (LDI) index, was used to assess the potential for land-use within watersheds to influence the production/accumulation of methyl-mercury (MeHg) in river sediments. Sediment samples were collected from locations impacted by well-identified land-use types within the Mobile-Alabama River Basin in Southeastern USA. The samples were analyzed for total-Hg (THg) and MeHg concentrations and the obtained values correlated to the calculated LDI indexes of the sampled watersheds to assess the impact of prevalent land use/land cover on MeHg accumulation in sediments. The results show that unlike THg, levels of MeHg found in sediments are impacted by the LDI indexes. Overall, certain combinations of land-use types within a given watershed appear to be more conducive to MeHg accumulation than others, therefore, pointing to the possibility of targeting land-use practices as potential means for reducing MeHg accumulation in sediments, and ultimately, fish contamination.     

湖泊底泥磷释放及磷形态变化

为研究底泥中内源性磷释放对城市景观水体富营养化的影响,以西安市曲江南湖为对象,采用底泥磷形态标准测试方法(SMT)分析了磷的赋存形态,通过模拟实验探究了在不同环境条件(温度、pH和溶解氧)下磷形态变化的特征。结果表明:温度升高促进内源磷的释放,在夏季加剧水体富营养化程度;碱性条件有利于磷的释放,增大补给水源可减少底泥释磷量;厌氧环境下底泥释磷量是好氧时的3.96倍;Al-P 和Ca-P较稳定,在酸性条件下会加速其溶解;NH4+-P、 Fe-P 和OrgP受溶解氧、pH和温度影响较大,其吸附与释放能力有明显的差异。     

酸碱改性对活性焦烧结烟气脱硫性能的影响

选取一定目数范围的活性焦,用3种酸(HCl、H2SO4和HNO3)、3种碱(KOH、NaOH和NH3·H2O)和酸碱两步(HNO3和KOH)对其进行改性处理,对比这几种方法改性的活性焦对烧结烟气的脱硫性能,实验结果表明,20~40目范围的活性焦脱硫性能最好;HCl改性活性焦的脱硫性能基本无变化,HNO3改性后有促进作用但作用不大,H2SO4改性反而降低了活性焦的脱硫活性;KOH和NaOH溶液改性活性焦对其脱硫性能有很大的提升作用,其中KOH改性效果更好,NH3·H2O改性基本无影响;先KOH后HNO3两步改性的活性焦效果最佳,并且能维持一定时间100%的脱硫效率。     

强化除磷型A/O-MBR工艺运行稳定性

采用缺氧/好氧膜生物反应器(A/O-MBR)处理合成的生活污水,考察了投加不同浓度的聚合氯化铝(PAC)对该工艺在除磷效能及运行稳定性方面的影响。结果表明,投加PAC可以有效降低出水TP的浓度;在投加量为150 mg/L时,TP的去除率达到最优,为90.1%,出水浓度维持0.48 mg/L左右,达到《城镇污水处理厂污染物排放标准》(GB18918-2002)的一级A标准。投加一定量的PAC可以有效提高微生物的活性;此外,可以降低污泥絮体的Zeta电位,增大污泥絮体的粒径,降低胞外聚合物(EPS)中多糖的浓度,进而有效延缓膜污染的速率。     

预处理-水解酸化-厌氧-好氧工艺对玉米淀粉废水有机污染物的降解

采用气相色谱/质谱(GC/MS)、三维荧光光谱(EEM)等检测手段分析预处理/水解酸化/厌氧/好氧组合工艺对玉米淀粉废水有机污染物的降解情况。结果表明,竖流沉淀预处理阶段对TOC平均去除率36.7%,废水中主要为芳烃、烷烯烃以及杂环类物质,EEM产生的5个荧光峰均为芳香蛋白类有机物;水解酸化阶段大部分杂环以及芳烃类有机物水解成有机酸和醇类物质,TOC平均去除率22.7%;厌氧阶段TOC平均去除率最高,达到97.8%,废水中以芳烃和烷烯烃为主,荧光峰减少至2个且强度减弱;好氧阶段TOC平均去除率为61.3%,有机物主要为难降解的长链烷烃物质,芳香蛋白类有机物荧光峰全部消失,新生成了与微生物代谢相关的腐殖酸类物质。     

基于磷脂脂肪酸法分析A+OSA污泥减量工艺微生物群落结构

以传统缺氧-好氧(AO) 工艺为参照,采用磷脂脂肪酸(PLFA)分析技术研究了缺氧-好氧-沉淀-厌氧(A+OSA)污泥减量工艺微生物生物量变化及群落结构分布特征。结果表明,参照工艺及减量工艺PLFAs组成以饱和脂肪酸、支链脂肪酸和单不饱和脂肪酸为主,并含有少量环丙烷脂肪酸和羟基脂肪酸。减量工艺污泥减量主要是源于贮泥池中污泥衰减,好氧菌和革兰氏阴性菌(G-菌)为与污泥衰减相关的微生物类群。真菌含量变化表明,减量工艺有抑制真菌生长的作用。减量工艺由于贮泥池的插入造成其微生物群落结构与参照工艺有显著不同,减量工艺缺氧池与好氧池微生物群落结构相似度提高。     

温度对热水解预处理高含固污泥特性的影响

以含固率为10%的污泥为对象,研究不同温度和时间条件下热水解过程中有机物转化规律对污泥特性的影响。结果表明:随着热水解时间的延长和温度的升高,污泥中挥发性悬浮固体(VSS)的水解率逐渐升高。在热水解时间为20 min时,温度由150℃升高到180℃,VSS水解率由22.9%增至38.4%,污泥中VSS由46.28 g/L降低到40.63 g/L。水解液组分分析表明,溶解性化学需氧量(SCOD)主要组成为蛋白质(50%)、碳水化合物(15%~20%)、可挥发性脂肪酸(15%~20%)。水解液中氮主要以有机氮的形式存在。在热水解条件达到165℃、50 min时,氨氮浓度为1.16 g/L,之后,随着温度的升高和时间的延长,氨氮浓度基本不变。     

The regulatory role of endogenous iron on greenhouse gas emissions under intensive nitrogen fertilization in subtropical soils of China

Environmental Science and Pollution Research - Anaerobic batch experiments were conducted to study the regulatory role of endogenous iron in greenhouse gas emissions under intensive nitrogen...     

电化学氧化法处理垃圾渗滤液纳滤浓缩液

实验利用电化学氧化法处理垃圾渗滤液纳滤浓缩液,以提高废水的可生化性。研究考察了水力停留时间、进水流量、循环流量、电流强度和原水氯离子浓度对有机物去除的影响。研究结果表明,电化学氧化法的最佳运行条件如下:水力停留时间为 3 h,进水流量为1 m3/h,循环流量为15 m3/h,电流强度为420 A。在上述条件下,原水COD浓度从3 100 mg/L降到1 311.3 mg/L,去除率达到57.7%,BOD/COD值由0.03提升至0.31。氯离子对电解有促进作用,但原水氯离子浓度超过5 000 mg/L,不需要外加工业盐。