2010—2019年台州市市区降水化学组成特征及变化趋势

为了解台州市市区大气降水化学成分组成特征及变化规律,对2010—2019年台州市市区降水监测数据进行了统计分析。结果表明:2010—2019年降水样品pH为4.20～4.84夏高冬低,强酸性降水频率下降显著,电导率平均值为3.16 mS/cm。SO_4~(2-)和NO_3~-是降水中最主要的阴离子,NH_4~+和Ca~(2+)是降水中最主要的阳离子。Ca~(2+)浓度在2018年开始有所抬升,SO_4~(2-)和NO_3~-浓度整体呈波动下降趋势。SO_4~(2-)与NO_3~-浓度比均值为1.50,呈下降趋势,同大气中SO_2与NO_2的质量浓度比变化趋势基本一致。SO_4~(2-)和NO_3~-相关性显著,Cl~-、Na~+及Mg~(2+)三者之间具有较好相关性。降水与气态污染物相关性不大,对颗粒物有明显冲刷去除作用。SO_2和NO_x的排放量显著下降,酸雨污染呈现改善过程。     

《大气污染防治行动计划》对郑州市冬季PM2.5浓度及化学组成影响

基于《大气污染防治行动计划》实施前后,在污染严重的冬季（2013年和2018年12月同期）,采集郑州市监测站的PM_2.5样品,分析PM_2.5化学组成,通过对比分析PM_2.5中的EC、OC、水溶性离子和金属元素的浓度变化来评估PM_2.5浓度及化学组成的变化,同时选取不同阶段重污染过程,探究PM_2.5浓度及组成的变化. 结果表明：①郑州市冬季ρ（PM_2.5）平均值由2013年的（215.38 ±107.28） μg·m^-3 下降至2018年的（77.45 ±49.81） μg·m^-3,下降率高达64%. ②PM_2.5中EC、K⁺、SO₄^2-和Cl^-,分别下降了85%、80%、78%和72%;OC、NH₄⁺和NO₃^-下降幅度较小,分别为50%、41%和32%. ③与2013年冬季相比,2018年冬季OC/EC的值升高了2.6倍,二次有机碳在OC中占比升高至57%;同时,硫氧化率和氮氧化率的值分别升高了1.5倍和1.0倍,表明郑州市二次污染较为严重,二次转化程度升高. ④NO₃^-/SO₄^2-（质量比）由2013年的0.8 ±0.2升高至2018年2.5 ±1.0,表明郑州市移动源贡献上升并且超过固定源成为冬季大气污染的主要来源. ⑤不同阶段重污染过程对比结果显示,与2013年相比,2018年重污染过程中PM_2.5浓度下降显著,峰值浓度下降了61%,主要化学组成由OC、NO₃^-、SO₄^2-和NH₄⁺变为OC、NO₃^-和NH₄⁺. 研究结果表明郑州市一次排放源管控取得了显著的成效,但二次生成对PM_2.5贡献呈现升高趋势,因此未来需要关注二次生成的影响.     

四川及重庆蕨类植物区系组成、特有现象和珍稀种类

四川及重庆为我国蕨类植物最丰富的区域之一,总计有52科,141属,约880种。鳞毛蕨科、蹄盖蕨科和水龙骨科是最重要的3个科,其种数占本区种数的50.5%,金星蕨科、中国蕨科和铁角蕨科在本区也有较多的种类分布。在本区主要的属为耳蕨属、鳞毛蕨属和蹄盖蕨属,它们的种数都超过50种,合计占本区种数的22.8%,其次有铁角蕨属、瓦韦属和毛蕨属,其种数都逾25种,而有近85%的属不足10种。热带成分的属在本区占53.9%,但它们的区系存在度不大;东亚分布的属占16.3%,其区系存在度相对较大;温带分布的属占12.7%。本区无特有科;仅光叶蕨属1个特有属,还有6个中国特有属;有387种为中国特有种,约占本区种数的44%。特有种的32%为本区特有,其余以与中国西南片区（占22.5%）和整个南方片区（占26.1%）共有为主。本区被列入国家重点保护的珍稀濒危蕨类植物有10种,其中1级3种,2级7种。     

砷尾矿污染土壤的细菌群落结构多样性及其相关环境影响因子分析

以湖南石门雄黄尾矿污染土壤为对象,研究纵向不同深度、横向不同距离土样中的重金属污染程度以及细菌群落结构变化规律,查明砷污染土壤的核心微生物组成并将其与土壤理化指标进行共存网络图分析.结果表明:该尾矿区的土壤各项重金属指标严重超标,尤以铅(626.54 mg·kg?1,Ei=105.48)、砷(1804.75 mg·kg...     

The explosion of non-nano iron dust suspension in the 20-l spherical bomb

The understanding of dust explosion is still incomplete because of the lack of reliable data and accurate models accounting for all the physic-chemical aspects. Besides, most of the experimental data available in the current literature has been accumulated on the 20-l spherical bomb tests, which gives coarse results for the pressure history that cannot be easily converted into fundamental combustion parameters. Nevertheless, the large amount of experimental data available in the spherical bomb is attractive. In this work, the explosion of non-nano iron dust in the standard spherical vessel is analyzed, aiming at evaluating the burning velocity from the theoretical point of view and the simple experiments performed by the standard explosion tests. The choice of iron is of relevance because its adiabatic flame temperature is below the boiling temperature of both the reactants and oxidized gaseous, liquid, or solid (intermediate and final) products and for the negligible particle porosity, which instead is typical of organic dust. Therefore, a non-nano iron dust explosion can be reconducted to a reduced mechanism since heterogeneous (surface) combustion may be determinant, and the diffusion mechanism for oxygen is the only relevant. The laminar burning velocity is strongly dependant on the particle diameter, whereas little effects are due to the dust concentration. The reported final value was found in agreement with typical limiting laminar burning velocity, adopted for the estimation of flammability limits.     

中国钢铁工业职业卫生40年回顾和今后展望

通过对中国钢铁工业职业卫生四十年的回顾,笔者认为:钢铁工业卫生管理体制已基本形成,但管理水平急需提高;主要的传统职业危害有所抑制,而今后任务仍十分艰巨;随着钢铁工业生产技术的发展广大职工又面临新的职业危害的挑战。本文最后对90年代钢铁工业职业卫生的形势进行了展望,提出了新的对策。在执行「八五」职业卫生规划的基础上,还需加强职业互生服务机构,扩大服务覆盖面,提高专业素质、开展普及教育、加强专业队伍的自身建设,这些任务是实现十年战略目标的重要保证。     

四川盆地海相三叠系硫同位素组成及其地质意义

系统整理研究了四川盆地海相三叠系硬石膏和卤水的硫同位素组成、演化特点及其地质意义。这对促进四川和全球海相三叠系硫酸盐硫同位素的研究有重要参考价值。     

Diagenesis of Upper Carboniferous rocks in the Ouachita foreland shelf in mid-continent USA: an overview of widespread effects of a Variscan-equivalent orogeny

Diagenesis of Upper Carboniferous foreland shelf rocks in southeastern Kansas took place at temperatures as high as 100–150° C at a depth of less than 2 km. High temperatures are the result of the long distance (hundreds of kilometers) advection of groundwater related to collisional orogeny in the Ouachita tectonic belt to the south. Orogenic activity in the Ouachita area was broadly Late Carboniferous, equivalent to the Variscan activity of Europe. Mississippi Valley-type Pb-Zn deposits and oil and gas fields in the US midcontinent and elsewhere are commonly attributed to regional groundwater flow resulting from such collisional events. This paper describes the diagenesis and thermal effects in sandstone and limestone of Upper Carboniferous siliciclastic and limestone-shale cyclothems, the purported confining layer of a supposed regional aquifer. Diagenesis took place in early, intermediate, and late stages. Many intermediate and late stage events in the sandstones have equivalents in the limestones, suggesting that the causes were regional. The sandstone paragenesis includes siderite cement (early stage), quartz overgrowths (intermediate stage), dissolution of feldspar and carbonates, followed by minor Fe calcite, pore-filling kaolinite and sub-poikilotopic Ca ankerite (late stage). The limestone paragenesis includes calcite cement (early stage); megaquartz, chalcedony, and Fe calcite spar (intermediate stage); and dissolution, Ca-Fe dolomite and kaolinite (late stage). The R _m value of vitrinite shows a regional average of 0.6–0.7%; Rock-Eval T _maX suggests a comparable degree of organic maturity. The T _h of aqueous fluid inclusions in late stage Ca-Fe-Mg carbonates ranges from 90 to 160° and T _mice indicates very saline water (>200000 ppm NaCl equivalent); ¹⁸O suggests that the water is of basinal origin. Local warm spots have higher R _m, T _max, and T _h. The results constrain numerical models of regional fluid migration, which is widely viewed as an artesian flow from recharge areas in the Ouachita belt across the foreland basin onto the foreland shelf area. Such models must account for heating effects that extend at least 500 km from the orogenic front and affect both supposed aquifer beds and the overlying supposed confining layer. Warm spots indicate either more rapid or more prolonged flow locally. T _h and T _mice data show the highest temperatures coincided with high salinity fluids.     

威远震旦系天然气与油气生运聚

根据威远震旦系气藏天然气组成、同位素特征、储层包裹体的对比研究 ,我们认为该气藏的天然气主要来源于下寒武统筇竹寺组泥岩 ,其天然气主要是干酪根裂解气 ,次为油的裂解气。威远震旦系气藏是喜山期形成的 ,威远的天然气无论是干酪根裂解气还是油裂解气都由北面古构造聚集的干酪根裂解气和油裂解气转移而来 ,威远构造之所以能形成工业聚集的重要原因就是威远构造的形成与北面古构造的消失的良好匹配关系     

Analysis of chemical composition of precipitation in a typical background site

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