大庆红岗生态工业园区创建的现有条件

生态工业园是根据循环经济理念和工业生态学原理而设计建立的一种新型工业组织形态,在园区内通过废物交换、循环利用、清洁生产等手段,实现资源利用的最大化和废物排放的最小化.文章通过对大庆市石油、石油化工产业链现状分析及产品代谢和废物代谢分析,说明大庆红岗具有创建生态工业园区的区位和资源优势,园区所在区域内现已经初步形成了石油开采、石油化工、轻烃加工和化工建材产业(品)代谢连及废油、废水回注等废物代谢链的生态工业雏形,为创建大庆红岗生态工业(石化)示范园区奠定了一定的基础.     

2500 m3多级内循环(MIC)厌氧反应器在柠檬酸废水处理工程中的应用

MIC反应器是在UASB反应器的基础上发展起来的第三代厌氧反应器,它具有效率高、能耗低、投资少、占地省等优点。作者所在单位自行研制、安装、调试的生产规模2500m3MIC反应器用于处理高浓度柠檬酸生产废水,经过两年多的启动和实际运行,在水力停留时间12.5h,COD有机负荷12kg·m-3·d-1时,COD去除率仍始终在90%左右。     

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。     

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.     

涕灭威在植物和土壤中的移动与分布

报道了涕灭威在花生、棉花、柑橘和土壤中的吸收、运转和分布。结果表明，涕灭威及其代谢物在柑橘叶子中的残留４０ｄ达到最高峰（３．４４９ｐｐｍ），可食部位的残留范围为０－０．０８９ｐｐｍ，低于美国ＥＰＡ规定的ＭＲＬ。涕灭威在土壤中降解较快，半衰期约１周。收获时土壤中的检出范围为０－０．１５７ｐｐｍ。涕灭威及其代谢物水溶性很强，且具有渗透和扩散性，因此使用不当可能造成地下水污染。     

高强铝合金超塑挤压成形

主要介绍了工业牌号高强铝合金在供应态或经简单预处理后在通用油压机上超塑成形的实例,并分析探讨了非理想组织材料超塑成形中微观组织的变化。     

高效液相色谱在环境监测中的应用

论述了高效液相色谱法适于环境样品中分子量大、挥发性低、热稳定性差的有机污染物的分析与分离。参阅了国内外文献，例举了用高效液相色谱法测定环境样品中多环芳烃、酚类、多氯联苯、酞酸酯类、联苯胺类、阴离子和非离子表面活性剂、有机农药等有机污染物的测定条件及分离结果。     

假单胞杆菌抗镉基因的克隆

以pBR322为载体,将抗镉的假单胞杆菌R4染色体的抗镉基因克隆至大肠杆菌HB101,从5000个重组体中筛选出一株抗镉基因克隆株,命名为大肠杆菌HB101(pBC311)。重组质粒pBC311经PstⅠ酶解和琼脂糖凝胶电泳证实抗镉基因位于3.6kb长的PstⅠ片段上。克隆菌株可在含100μg/ml CdCl_2的L-肉汤中生长,其生长停滞期比受体大肠杆菌HB101短得多,说明克隆菌株含有抗镉基因。