压电复合阻尼减振材料和压电复合吸声降噪材料中压电陶瓷应用形态研究

我们曾经将压电陶瓷粉体复合到传统的吸声降噪材料与阻尼减振材料中 ,制作出了性能更好的新型吸声降噪材料和新型阻尼减振材料 ;而且还发现废品压电陶瓷的粉体与正品压电陶瓷的粉体具有相同的功效[1～4 ] ,分析了它们同样发挥压电效应的原因。     

污泥焚烧中二氧化硫检测新方法及污泥处理探讨

对新乡市9个污水处理场污泥预处理后,用测硫仪分析污泥含硫量,并用经验公式根据年污水处理量,估算焚烧污泥方法年二氧化硫排放总量。结果显示：用测硫仪测定污泥含硫量,核算二氧化硫排放量,与现有方法相比,操作简便易行,结果不受采样条件、时间、环境、布点等因素影响,重现性好、完整、精密。同时发现部分污泥含硫量超过规定用煤中含硫量,建议用焚烧方法处置污泥,净化尾气。     

徐州市环境监测网络建设现状及发展探讨

从环境质量监测、污染源监测、应急监测、生态监测和监测信息等方面对徐州市环境监测网络建设的现状进行分析及未来徐州市环境监测网络的发展探讨.     

不同沉水植物净水能力与植株体细菌群落组成相关性

选取苦草(Vallisneria natans)、密刺苦草(Vallisneria denseserrulata)、黑藻(Hydrilla verticillata)、伊乐藻(Elodea canadensis)、金鱼藻(Ceratophyllum demersum)、竹叶眼子菜(Potamogeton malaianus)、篦齿眼子菜(Potamogeton pectinatus)和微齿眼子菜(Potamogeton maackianus)这8种亚热带地区常见的沉水植物为研究对象,在室内静水条件下对其氮、磷吸收和水质净化能力进行对比试验,并结合16S rRNA基因测序对沉水植物关联细菌群落组成进行测定,研究沉水植物对水体的净化能力与植株体菌群之间的相关性.结果表明,8种沉水植物对水体中的氮磷的去除主要通过植物增效作用,植物吸收富集作用去除率较低.其中密刺苦草对水体中TN、TP的去除率最高,达到了91. 58%和96. 81%.伊乐藻、金鱼藻对水中氮磷自身吸收能力高于其他组,密刺苦草和苦草的植物增效的净化能力最强.经分析,8种沉水植物对水体中氮磷的净化能力较强可能是因为植物关联的细菌大多具有降解作用.根瘤菌目(Rhizobiales)、伯克霍尔德氏菌目(Burkholderiales)、黄杆菌目(Flavobacteriales)、产碱杆菌科(Alcaligenaceae)、贪铜菌属(Cupriavidus)和芽孢杆菌属(Bacillales)的细菌可能是引起密刺苦草增效的净化能力较强的优势菌群,异常球菌纲(Deinococci)、丛毛单胞菌科(Comamonadaceae)、腐螺旋菌科(Saprospiraceae)和生丝微菌属(Hyphomicrobium)的细菌可能是引起苦草增效的净化能力较强的优势菌群.     

泰安市冬季一次严重空气污染过程分析

为揭示泰安市空气污染形成原因,选取泰安市2016年12月一次严重空气污染过程,利用泰安市2016年12月地面和探空资料及NCEP/NCAR（美国国家环境预报中心/美国国家大气研究中心）提供的FNL资料,对泰安市严重污染期间大气环流形势、边界层条件、污染源及传输路径进行分析.结果表明:在泰安市霾污染期间,500 hPa大气环流形势呈"两槽一脊"的特征,850 hPa泰安市处于南支槽前,受西南暖湿气流影响,为ρ（PM_2.5）的升高提供了有利条件;泰安市近地面处于高压控制下的弱风区（平均风速约为1.2 m/s）且边界层有逆温层存在,阻碍了PM_2.5的垂直输送,造成近地面ρ（PM_2.5）急剧升高.此外,泰安市及周边地区污染严重,聚类分析结果表明此次过程本地输送占比约为34%,其余均为外来传输,即污染物主要通过外来源传输,本地污染源贡献比率较小.污染物的高、低空传输路径不一致,低空污染物主要从安徽省水平输送至泰安市,高空污染物则先由河北省、河南省向南传输至安徽省、湖北省等地,再随南风气流向北输送至泰安市.研究显示,外来污染源传输作用配合本地静稳天气形势是造成此次泰安市空气污染的主要原因.      

滇池水生植物分布对沉积物间隙水中不同形态氮的影响

为揭示水生植物分布对滇池沉积物间隙水中各形态氮质量浓度的影响,于2015年6月在滇池分别采集有植物区域和无植物区域的沉积物柱状样,检测间隙水及上覆水中DTN(溶解性总氮)、NH₄+-N、NO₃--N和DON(溶解性有机氮)的质量浓度,分析其垂向变化特征以及水生植物对间隙水中各形态氮的释放控制效果. 结果表明:①水生植物改变了柱状沉积物间隙水中不同形态氮的分布规律,并且这种改变随湖区不同而表现不尽一致;②水生植物显著降低了沉积物间隙水中DON的贡献率,有植物分布区域ρ(DON)对ρ(DTN)的平均贡献率为41.05%,无植物区域可达58.48%;③水生植物显著抑制了沉积物中无机氮的释放,促进了DON的转化,同一采样点有植物区域NH₄+-N和NO₃--N的沉积物-水界面扩散通量分别比无植物区域平均降低了87.52%和91.99%;④水生植物生长显著削减了沉积物间隙水中氮的质量浓度,其中ρ(DON)的削减率达到了53.27%~80.42%. 研究显示,水生植物根系作为微生物和多种活性酶的主要载体,为沉积物有机氮的矿化降解起到了促进作用.      

CCS scenarios optimization by spatial multi-criteria analysis: Application to multiple source sink matching in Hebei province

A method, based on spatial analysis of the different criteria to be taken into consideration for building scenarios of CO₂ capture and storage (CCS), has been developed and applied to real case studies in the Hebei province. Totally 88 point sources (42 from power sector, 9 from iron and steel, 18 from cement, 16 from ammonia, and 3 from oil refinery) are estimated and their total emission amounts to 231.7 MtCO₂/year with power, iron and steel, cement, ammonia and oil refinery sharing 59.13%, 25.03%, 11.44%, 3.5%, and 0.91%, respectively. Storage opportunities can be found in Hebei province, characterised by a strong tectonic subsidence during the Tertiary, with several kilometres of accumulated clastic sediments. Carbon storage potential for 25 hydrocarbon fields selected from the Huabei complex is estimated as 215 MtCO₂ with optimistic assumption that all recovered hydrocarbon could be replaced by an equivalent volume of CO₂ at reservoir conditions. Storage potential for aquifers in the Miocene Guantao formation is estimated as 747 MtCO₂ if closed aquifer assumed or 371 MtCO₂ if open aquifer and single highly permeable horizon assumed. Due to poor knowledge on deep hydrogeology and to pressure increase in aquifer, injecting very high rates requested by the major CO₂ sources (>10 MtCO₂/year) is the main challenge, therefore piezometry and discharge must be carefully controlled. A source sink matching model using ArcGIS software is designed to find the least-cost pathway and to estimate transport route and cost accounting for the additional costs of pipeline construction due to landform and land use. Source sink matching results show that only 15–25% of the emissions estimated for the 88 sources can be sequestrated into the hydrocarbon fields and the aquifers if assuming sinks should be able to accommodate at least 15 years of the emissions of a given source.     

Suggested protocol for collecting, handling and preparing peat cores and peat samples for physical, chemical, mineralogical and isotopic analyses

For detailed reconstructions of atmospheric metal deposition using peat cores from bogs, a comprehensive protocol for working with peat cores is proposed. The first step is to locate and determine suitable sampling sites in accordance with the principal goal of the study, the period of time of interest and the precision required. Using the state of the art procedures and field equipment, peat cores are collected in such a way as to provide high quality records for paleoenvironmental study. Pertinent field observations gathered during the fieldwork are recorded in a field report. Cores are kept frozen at -18 degree C until they can be prepared in the laboratory. Frozen peat cores are precisely cut into 1 cm slices using a stainless steel band saw with stainless steel blades. The outside edges of each slice are removed using a titanium knife to avoid any possible contamination which might have occurred during the sampling and handling stage. Each slice is split, with one-half kept frozen for future studies (archived), and the other half further subdivided for physical, chemical, and mineralogical analyses. Physical parameters such as ash and water contents, the bulk density and the degree of decomposition of the peat are determined using established methods. A subsample is dried overnight at 105 degree C in a drying oven and milled in a centrifugal mill with titanium sieve. Prior to any expensive and time consuming chemical procedures and analyses, the resulting powdered samples, after manual homogenisation, are measured for more than twenty-two major and trace elements using non-destructive X-Ray fluorescence (XRF) methods. This approach provides lots of valuable geochemical data which documents the natural geochemical processes which occur in the peat profiles and their possible effect on the trace metal profiles. The development, evaluation and use of peat cores from bogs as archives of high-resolution records of atmospheric deposition of mineral dust and trace elements have led to the development of many analytical procedures which now permit the measurement of a wide range of elements in peat samples such as lead and lead isotope ratios, mercury, arsenic, antimony, silver, molybdenum, thorium, uranium, rare earth elements. Radiometric methods (the carbon bomb pulse of (14)C, (210)Pb and conventional (14)C dating) are combined to allow reliable age-depth models to be reconstructed for each peat profile.     

Small-scale spatial and temporal interactions among benthic crustaceans and one fish species in the Bay of Biscay

In the summer of 2004, a video survey was carried out in the northern part of the central mud bank (Grande Vasière) of the Bay of Biscay to study the small scale relationship between the dominant crustacean megafauna Nephrops norvegicus, Munida rugosa and Goneplax rhomboides and juvenile hake (Merluccius merluccius). Using a towed body, high-resolution videos were recorded in six sampling sites. Statistical modelling using generalised additive models (GAM) revealed variations in activity patterns for two species. More N. norvegicus were observed outside their burrows at dawn and somewhat at dusk (no observations during night) while G. rhomboides was less observed in the morning. In addition, reduced spatial overlap between G. rhomboides and N. norvegicus suggested reduced competition for food but also space as both are burrowing species. The observed temporal and spatial activity patterns may contribute to regulating assemblage structure as competing species may be actively foraging at different times and locations thus reducing direct competition.