不同环境下微动开关腐蚀形貌及接触电阻变化对比分析研究

目的对比分析不同试验环境下微动开关的腐蚀行为,研究其腐蚀机理。方法针对干湿交替酸性盐雾试验环境、盐雾/SO2复合试验环境及热带海洋大气环境下微动开关接触电阻的变化趋势,以及对不同试验环境后微动开关内部被腐蚀的细小结构件进行微观形貌观察和能谱分析。通过对比分析不同试验环境下微动开关的腐蚀机理及其对电性能参数的影响。结果含硫环境对微动开关内部银质触点的影响最严重。结论腐蚀产物硫化银的导电性极差,这会导致微动开关接触电阻升高。     

Spatiotemporal dynamics of cell abundance, colony size and intracellular toxin concentrations of pelagic and benthic Microcystis in Lake Caohai, China

Lake Caohai has experienced extensive Microcystis blooms in recent years,and to improve its water quality,the local government carried out a series of water control measures.To better understand the dynamics of both pelagic and benthic Microcystis and their characteristics in Lake Caohai,we conducted a 1-year investigation from December 2015to December 2016 to gain a seasonal outlook on the distribution and dynamics of cell abundance,colony size and intracellular microcystins(MCs)of Microcystis.The results indicated that the Microcystis bloom occupied primarily the northeastern region and then moved gradually from lakeshore to lake center.The perennial southwesterly winds and the water inflow from northeast to southwest in Lake Caohai determined the spatiotemporal distribution of pelagic Microcystis.Benthic Microcystis was mainly distributed in the northeastern region in summer,occupied the lake center in autumn and then occupied the southeastern region in winter,determined by the sedimentation of pelagic Microcystis and the death of benthic Microcystis.Small colonies(20-60μm)overwintered more easily in both water column and sediment.The concentrations of intracellular toxin of benthic Microcystis were observed to be significantly higher than those of pelagic Microcystis.This might be because Microcystis synthesized large amount of MCs to acclimate to an unfavorable benthic environment.This knowledge on the dynamics of Microcystis expands our understanding of mechanisms underpinning the formation of Microcystis blooms.     

Comprehensive analysis of nitrogen distributions and ammonia nitrogen release fluxes in the sediments of Baiyangdian Lake, China

The condition of Baiyangdian Lake(BYDL) will improve as the Xiongan New Area evolves and fulfills its role of easing overcrowding and supporting economic growth. Water and sediment samples from BYDL were analyzed to provide information on nitrogen(N) contamination in BYDL. The mean ammonium N(NH_4~+-N), nitrate N, and total N concentrations in the water samples were 0.36, 0.12, and 2.22 mg/L, respectively, and the ranges were 0.003–8.38, 0.06–0.30,and 1.25–10.34 mg/L, respectively. The N concentrations in water gradually increased from the north to the south of BYDL. Sediment at 90% of the sampling sites was in or above the moderately contaminated class(1000–2000 mg/kg) defined in US Environmental Protection Agency total N pollution standards. Positive NH_4~+-N fluxes were found for 28 of the 34 sediment core samples, so the potential for NH_4~+-N being released from sediment was relatively high. The NH_4~+-N fluxes were 5.35–48.76 mg/m~2/day, and the mean and maximum fluxes were 8.71 and 48.76 mg/m~2/day, respectively. Benthic organisms will be affected more by NH_4~+-N and NH_3·H_2O in the surface sediment pore water(mean concentrations 4.93 and 0.13 mg/L, respectively) than by the other forms of N.     

Chromosome doubling of Sedum alfredii Hance: A novel approach for improving phytoremediation efficiency

Sedum alfredii Hance is a cadmium(Cd)/zinc(Zn) hyperaccumulator native to China.However, its relatively low biomass restricted the large-scale application for heavy metal contamination remediation. The chromosome set doubling of S. alfredii in vitro was achieved by 0.1%–0.2%(W/V) colchicine treatment. The plant DNA ploidy was analyzed by flow cytometry and chromosome set doubling plants(CSD) were identified based on the obvious different sharp peak. A tissue culture experiment with different Cd treated levels and a field trial with natural polluted mined soil were conducted to study the effects of chromosome doubling on plant biomass and Cd accumulation in shoots. The results suggested that S.alfredii is a mixoploid. Compared with the wild type plants(WT), CSD exhibited typical"gigas" characteristics in morphology including stem thickness, root hair production,number of leaves and size of stoma guard cell. Fresh weight and dry weight of CSD were increased to 1.62–2.03-fold and 2.26–3.25-fold of WT. And Cd content of CSD showed a17.49%–42.82% increase and 59% increase under tissue culture and field condition,accordingly. In addition, the TF and in BCF of CSD were 2.37-and 1.59-fold of WT,respectively. These results proved that it is feasible to promote phytoextraction efficiency of S. alfredii in Cd contaminated soils through chromosomal engineering, which provides a novel approach for hyperaccumulator application in phytoremediation.     

厦门市森林生态系统固碳服务评估

生态系统固碳服务是生态系统服务评估的重要指标之一,也是区域碳循环研究的重要组成部分,可以为减缓气候变化的区域碳管理提供决策依据.以厦门市森林生态系统为研究对象,选取VPM（Vegetation Photosynthesis Model）和ReRSM（Remote Sensing Model for Ecosystem Respiration）评估其2015年的固碳服务,并阐明其固碳服务的时空变异.结果表明:2015年厦门市森林生态系统固碳量（以C计）为31.36×104 t/a,平均固碳量为644.86 g/（m2·a）,其时间动态总体呈单峰曲线分布,但受台风影响该曲线波动较大.厦门市森林生态系统固碳量空间格局总体表现为西北边缘地区较高、其他地区相对较低,与DEM的空间分布较为相似,且绝大部分区域为碳汇区.厦门市分区统计显示,同安区森林生态系统面积和固碳量均最大,分别占厦门市总量的52.58%和57.10%,其与翔安区、集美区的固碳量之和占厦门市总量的88.27%,是厦门市森林生态系统固碳的主体;湖里区固碳量最少,平均固碳量仅为14.25 g/（m2·a）,几乎为碳中性.研究显示,厦门市森林生态系统具有较好的固碳能力.      

厦门市陆地生态系统空气负离子服务能力评估

为探讨厦门市陆地生态系统负离子的服务能力及其影响因素,以生态系统产生的有益于人类身心健康的空气负离子个数为表征指标,改进了空气负离子服务评估方法,基于空气负离子监测数据计算了厦门市空气负离子服务功能量,并分析了厦门市空气负离子的时空变化规律及其影响因子.结果表明:厦门市2015年空气负离子服务功能量为1.37×1025个,单位面积负离子服务功能量为0.8×1016个/m2.从行政分区来看,同安区空气负离子服务功能量最大,约占厦门市总量的56.5%;从生态系统类型上看,森林生态系统空气负离子服务功能量最大,约占厦门市总量的86.6%.厦门市空气负离子日浓度存在明显的"波峰"与"波谷",波峰主要分布01:00-07:00之间,波谷主要分布在12:00左右;厦门市空气负离子浓度存在明显的季节性变化特征,夏季生态系统空气负离子平均浓度为2 437个/cm3,约为春季的2倍;不同生态系统空气负离子浓度存在明显差异,如森林远大于草地、耕地等生态系统;对于大多数生态系统类型而言,空气负离子浓度主要受到温度和湿度的影响,表现为随着温度的升高而降低、随着湿度的升高而增加.研究显示,厦门市森林生态系统的空气负离子服务能力最强,乔木绿地空气负离子服务能力大于灌木、草本绿地,城市森林、乔木绿地面积越大,为人类提供的空气负离子服务越大.      

骨炭粉对Cd污染农田的修复效果与稳定性评价

为了探明骨炭粉对Cd污染土壤的修复效果及稳定性,以潮土与红壤Cd污染农田土壤为对象,基于土壤Cd有效态、作物降Cd率（DR,%）及降Cd失活率（IR,%）等指标,研究田间条件下施用3种浓度（0.25%、0.50%及1.0%）骨炭粉对Cd污染土壤的修复效果及120,360d后修复效果的稳定性.结果表明：骨炭粉处理均能有效促进潮土与红壤中作物生长,增加作物产量.施用骨炭粉能不同程度提高土壤中pH值、阳离子交换量（CEC）、全磷及有效磷含量;其中,0.5%和1.0%骨炭粉处理均显著（P<0.05）提高土壤pH值、土壤全磷及有效磷含量.与对照相比,不同骨炭粉处理120d后潮土和红壤中有效态Cd含量分别降低32.1%~48.4%、32.8%~56.2%,360d后土壤中有效态Cd仍然显著低于对照,降幅为26.9%~37.8%、25.8%~39.5%.对修复后三季作物Cd吸收测定结果表明,与对照相比,不同浓度（0.25%~1.0%）骨炭粉处理的第一季作物降Cd率（DR_-Cd）分别达36.0%~60.4%、33.9%~58.2%,作物降Cd率随骨炭粉施用量增加而增加.基于降Cd失活率（IR_-Cd）对骨炭粉修复效果的稳定性测定结果表明,潮土与红壤施用骨炭粉360d后,第三季作物降Cd失活率IR_-Cd为21.2%~34.7%和6.2%~21.6%,表明在酸性红壤中修复效果的稳定性大于潮土.综上骨炭粉对Cd污染土壤的修复效果及其稳定性结果表明,骨炭粉在Cd污染农田土壤修复中具有较大应用价值.     

全氟辛烷磺酰胺在小麦和蚯蚓中的富集与转化

研究了不同培养介质和培养方式下全氟辛烷磺酰胺（PFOSA）在小麦、蚯蚓体内的生物富集和转化.结果表明：小麦根系可以从培养介质中吸收PFOSA并向上转运至茎叶.土壤中PFOSA生物有效性受总有机碳（TOC）的影响显著,高TOC含量土壤中PFOSA的生物有效性降低,导致其在小麦和蚯蚓中的生物富集因子分别由（61.24±8.42）和（21347.91±208.86）降至（5.61±0.23）和（1404.92±108.21）.PFOSA在小麦的根和茎叶以及蚯蚓中都可以转化为PFOS,但在蚯蚓中的转化率（（3.87±1.71）%）显著低于小麦（（26.39±3.02）%）.小麦根中PFOS的支链异构体（br-PFOS）比例在低、高TOC含量时分别为（14.8±2.0）%、（66.1±26.2）%,低于茎叶（分别为（63.0±21.3）%、（85.2±2.4）%））,可能是由于根部转化生成的br-PFOS更容易向茎叶转运.小麦特别是小麦茎叶中的br-PFOS比例（（85.2±2.4）%）显著高于蚯蚓（（16.5±4.0）%）.小麦的存在可以提高土壤中PFOSA的生物有效性,从而促进蚯蚓对PFOSA的富集,但对其转化影响不大.本文为小麦和蚯蚓中PFOSA的富集和转化提供了证据,有助于探索环境中PFOS的间接来源.     

泵群无线监测系统在石化装置中的应用

介绍了机泵无线监测系统的系统架构、监测方案,并结合具体诊断案例详细说明了其在某千万吨级炼化企业的应用情况。结果表明,该系统能准确评估机泵运行状态,并及时发布报警提示和维护建议,使用该系统事后维修占比由41%降到了15%,预知性维修由不足10%上升到近50%。     

Anaerobic oxidation of arsenite by bioreduced nontronite

The redox state of arsenic controls its toxicity and mobility in the subsurface environment. Understanding the redox reactions of arsenic is particularly important for addressing its environmental behavior. Clay minerals are commonly found in soils and sediments, which are an important host for arsenic. However, limited information is known about the redox reactions between arsenic and structural Fe in clay minerals. In this study, the redox reactions between As(III)/As(V) and structural Fe in nontronite NAu-2 were investigated in anaerobic batch experiments. No oxidation of As(III) was observed by the native Fe(III)-NAu-2. Interestingly, anaerobic oxidation of As(III) to As(V) occurred after Fe(III)-NAu-2 was bioreduced. Furthermore, anaerobic oxidization of As(III) by bioreduced NAu-2 was significantly promoted by increasing Fe(III)-NAu-2 reduction extent and initial As(III) concentrations. Bioreduction of Fe(III)-NAu-2 generated reactive Fe(III)-O-Fe(II) moieties at clay mineral edge sites. Anaerobic oxidation of As(III) was attributed to the strong oxidation activity of the structural Fe(III) within the Fe(III)-O-Fe(II) moieties. Our results provide a potential explanation for the presence of As(V) in the anaerobic subsurface environment. Our findings also highlight that clay minerals can play an important role in controlling the redox state of arsenic in the natural environment.