滇池湖滨区新农村建设中的污染防治工程技术方案研究

对滇池湖滨区农村环境现状及主要环境问题进行了详细分析，就工程总体思路、设计原则及主要考核指标体系等进行了探讨，提出沿湖农村非点源污染防治工程技术方案，即通过以沼气池为纽带的农村能源结构改造、村级污水处置处理和配套沟渠系统建设、村内垃圾处理处置以及普及卫生旱厕、村庄道路修缮及绿化等工程和管理措施，从源头上控制污染物产生量，减少入湖污染负荷，有效地解决滇池环湖新农村建设中的环境保护问题。     

间歇式加煤锅炉SO2的定电位电解法测试技术探讨

针对间歇式加煤锅炉SO2的排放特性和平均排放浓度测试，结合两种常用的智能烟气分析仪，列举定电位电解法在实际测试中的应用情况以及不同测试分析仪器的功能性特点，指出当前在实际测试过程中存在的人为随意性和易出现的测试误差，提出消除和减少误差的相应对策。     

调引太湖水改善苏州市水动力条件研究

基于苏州地区独特的地理位置,简述引水改善该地区水环境的必要性,拟定了3种调水方案,利用感湖河网数学模型,对3种方案调水后主要河道的水动力条件进行预测,分析了各河道调水后的水动力变化趋势,提出了利用太湖水自流引水改善苏州市水环境的最佳方案.     

人工生物浮岛载体的研究进展

为改善浮岛性能,减少有机高分子材料所造成的"白色污染",有必要研制开发新型浮岛载体-轻质高效微生物载体.从国内外浮岛的研究现状看,目前在工程实例中广泛采用的是有机高分子材料载体,无机材料的浮岛尚处于实验研究阶段.在对几种典型无机材料-轻质滤料的物理特性、成分、化学稳定性、价格、来源等方面进行综合分析后可知,用无机材料制作有机浮岛载体的替代品是可行的,具有广阔的发展前景,但还需进一步的研究和探索.     

云南蒙自县新建小区室内空气污染调查及防治措施探讨

对蒙自县新建小区11户33个点室内环境空气中的游离甲醛、氨、苯进行了监测，游离甲醛和苯均超过标准。对有害物质的来源、危害及防治进行了讨论。     

柴油机排放碳颗粒物的催化燃烧

在热天平装置上考察了柴油机和碳颗粒物燃烧催化剂的活性，讨论了样品制备因素对样品失重的影响，这些因素包括碳颗粒物组成、催化剂栽体、催化剂与碳颗粒物质量比，着重筛选了催化剂的组份，得到了组份催化剂ＣｕＣｌ２－ＫＣｏ－ＮＨ４ＶＯ３其５５０℃焙烧后能使样品的Ｔｍ和Ｔｆ值都降低１８０℃以上，并对催化剂的热稳定性进行了研究。     

浅谈不锈钢拉深件成形时的表面保护方式

拉深是利用拉深模具把平板材料变成开口空心零件的冲压过程，是典型的变形工序。通过对不锈钢拉深件成形过程中的滑移状态及应力、应变分析，揭示了不锈钢拉深件成形时的表面划痕出现的根源，进而提出了表面保护的基本方式。     

沼泽红假单胞菌H3对酸性红B2GL染料的厌氧脱色和降解作用

从印染厂污泥中分离到一株沼泽红假单胞菌（ＲｈｏｄｏｐｓｅｕｄｏｍｏｎａｓｐａｌｕｓｔｒｉｓＨ３），在光照厌氧条件下该菌生长细胞可将１００ｍｇ／Ｌ酸性红Ｂ２ＧＬ染料去除到３０ｍｇ／Ｌ．完整细胞脱色的最适条件为ｐＨ７０，温度３０℃，细胞浓度２０—２５ｍｇ／ｍＬ（湿重）．低浓度的阳离子对脱色影响不大．在通Ａｒ气使严格厌氧和加有还原性辅酶Ｉ的条件下无细胞提取液的脱色活性最高，比活率为１５４×１０－２ｍｇ／（ｍｇ·ｈ）．根据降解产物的分析，推断了该菌对酸性红染料的降解代谢途径．     

Breccias of the Adnet Formation: indicators of a Mid-Liassic tectonic event in the Northern Calcareous Alps (Salzburg/Austria)

Stratigraphy, lithology and depositional structures of Liassic red limestone-breccias of the Adnet Formation, including the 'Adnet Scheck', were studied at several outcrops of the Northern Calcareous Alps (NCA) south-east of Salzburg. A four-fold lithostratigraphic division is proposed for the Adnet Formation of the Osterhorn Mountains: the hemipelagic Schmiedwirt (Sinemurian) and Kehlbach (Carixian) members are separated from the pelagic Saubach Member (Toarcian) by a layer of amalgamated breccias (Scheck Member, probably Domerian to early Toarcian). Several other breccia beds occur locally from the base of the Kehlbach Member up to the lower Saubach Member. Although the sediments overlying the Scheck Member breccias are of coeval age, the ages of the underlying strata are very different. This can be explained by submarine Liassic erosion during a period of resedimentation from the middle Carixian until the early Toarcian. At least 10–15?m of partly lithified sediments were eroded by gravity flows. The entire Kehlbach Member and up to two-thirds of the Schmiedwirt Member were removed at Adnet. The breccias originated from submarine debris flows. Repeated flows over a long period and the depositional setting exclude a triggering by sea-level fluctuations. Most probably they arose from tectonically triggered slumps and slides of superficial sediments. The 'Scheck' was initiated on the steep upper slope of the drowned Triassic Adnet reef and flowed to the north-east.The Pliensbachian to early Toarcian period of tectonic activity indicated by the breccias was the most important during the Liassic in the Osterhorn Mountains and other parts of the NCA. From the large-scale regional distribution of the breccias and in accord with published data, a roughly north-east trending strike-slip fault zone is proposed, crossing the NCA south of the Osterhorn block, with a peaking activity during the Pliensbachian to early Toarcian as the cause of the tectonic movements.     

Latest precambrian (Cadomian) zircon ages, Nd isotopic systematics and P-T evolution of granitoid orthogneisses of the Erzgebirge, Saxony and Czech Republic

Single zircons from two orthogneiss complexes, the Grey Gneiss and Red Gneiss, the lowermost tectonic units in the Erzgebirge, were dated. The grey Freiberg Gneiss is of igneous origin and has a ²⁰⁷Pb/²⁰⁶Pb emplacement age of 550±7 Ma. A quartz monzonite from Lauenstein contains idiomorphic zircons with a mean ²⁰⁷Pb/²⁰⁶Pb age of 555±7 Ma as well as xenocrysts ranging in age between 850 and 1910 Ma. Red gneisses from the central Erzgebirge contain complex zircon populations, including numerous xenocrysts up to 2464 Ma in age. The youngest, idiomorphic, zircons in all samples yielded uniform ²⁰⁷Pb/²⁰⁶Pb ages between 550±9 and 554±10 Ma. Nd isotopic data support the interpretation of crustal anatexis for the origin of both units. _Nd(t) values for the grey gneisses are –7.5 and –6.0 respectively, (mean crustal residence ages of 1.7–1.8 Ga). The red gneisses have a wider range in _Nd(t) values from –7.7 to –2.8 (T _DM ages of 1.4–1.8 Ga). The zircon ages document a distinct late Proterozoic phase of granitoid magmatism, similar in age to granitoids in the Lusatian block farther north-east. However, Palaeozoic deformation as well as medium pressure metamorphism ( 8 kbar/600–650° C) are identical in both gneiss units and distinguish these rocks from the Lusatian granitoids. The grey and red gneisses were overthrust by units with abundant high-pressure relicts and a contrasting P-T evolution. Zircon xenocryst and Nd model ages in the range 1000–1700 Ma are similar to those in granitoid rocks of Lusatia and the West-Sudetes, and document a pre-Cadomian basement in parts of east-central Europe that, chronologically, has similarities with the Sveconorwegian domain in the Baltic Shield.