Fenton试剂处理青霉素废水实验研究

以青霉素废水为研究对象 ,初步探讨了 Fenton试剂处理有毒有机废水时各影响因素的作用机制 ,通过实验确定了 Fenton试剂氧化降解青霉素废水的适宜操作条件为 :CODCr为 30 0 0 mg/L左右的青霉素废水 ,p H为 6.0、H2 O2 (30 % )投加量为 0 .6% (体积分数 )、Fe SO4 · 7H2 O投加量为 0 .2 % (质量分数 )、反应时间为 lh,此条件下废水 CODcr的去除率可达 70 % ,而且该方法设备简单 ,易于下一步实现工业放大 ,是一种有较好开发前景的处理青霉素废水工艺。     

含氮杂环化合物吲哚的缺氧降解性能研究

以好氧、厌氧作为对比，研究了含氮杂环化合物——吲哚的缺氧生物降解性能。主要研究在缺氧状态下吲哚的生物降解性能、适宜N／C比、氮源的变化情况以及吲哚的缺氧降解途径。结果表明，缺氧反硝化状态下吲哚具有较好的生物降解性能。     

The effect of metapleural gland secretion on the growth of a mutualistic bacterium on the cuticle of leaf-cutting ants

In Acromyrmex octospinosus leaf-cutting ants the metapleural glands produce an array of antibiotic compounds that serve as a general defence against unwanted microbes on the cuticle. Leaf-cutting ants also grow mutualistic Pseudonocardiaceae bacteria on their cuticle that produce antibiotics controlling a microfungal parasite of their fungus gardens. Interaction between this bacterium and gland secretion therefore seems unavoidable. We document the typical development of bacterial growth on the cuticle of young major workers, show that growth starts a few days after eclosion, and that the maximal cover is reached after 2–3 weeks and gradually declines when workers mature. Experimental closure of the metapleural glands had no effect on the initial exponential growth phase of the bacterium, but significantly reduced the cover during the decline phase. The age-dependent abundance of the bacterium and its partial dependence on metapleural gland secretion support the hypothesis that the abundance of this mutualist is actively regulated.     

未熟-低熟烃源岩的有机岩石学特征

采用全岩光片镜鉴和显微荧光分析方法 ,对我国不同地区 5 0 0余块未熟 低熟烃源岩样品进行了系统的有机岩石学研究。未熟 低熟烃源岩显微组分组成具有显著的非均质性 ,不同地区显示出陆源组分与水生生源组分不同的“配比”关系 ,反映出其有机质组成的复杂性 ,并确认藻类体、孢子体、树脂体、木栓质体、壳屑体和矿物沥青基质等组分是其最常见的生烃组分。基于对镜质组反射率Ro和孢子体荧光变化等演化指标特征的分析 ,认为未熟 低熟烃源岩有机质早期热演化具有明显的阶段性 ,一般都表现为“二段式”变化 ,其变化界限大致以Ro等于 0 .5 0 %～ 0 .5 5 %为界。     

Pulse cleaning flow models and numerical computation of candle ceramic filters

ＩｎｔｒｏｄｕｃｔｉｏｎＣｌｅａｎｉｎｇｔｈｅｆｉｎｅｐａｒｔｉｃｌｅｓｉｎｈｉｇｈｔｅｍｐｅｒａｔｕｒｅ (450℃ -950℃ )ａｎｄｈｉｇｈｐｒｅｓｓｕｒｅｃｏｎｄｉｔｉｏｎｃａｎｅｎｈａｎｃｅｔｈｅｔｈｅｒｍａｌｅｆｆｉｃｉｅｎｃｙｏｆｃｌｅａｎｃｏａｌｔｅｃｈｎｏｌｏｇｉｅｓｓｕｃｈａｓＩＧＣＣｏｒＰＦＢＣ .Ｒｉｇｉｄｃｅｒａｍｉｃｆｉｌｔｅｒｓｏｆａｖａｒｉｅｔｙｏｆｓｔｒｕｃｔｕｒｅｓａｒｅｕｎｄｅｒｄｅｖｅｌｏｐｍｅｎｔｉｎｐｒｏｇｒａｍｓａｒｏｕｎｄｔｈｅｗｏｒｌｄ ,ｗｈｉｃｈｃａｎｆｉ…     

纺织工业空调废水处理回用的试验研究

纺织工业空调排水占整个纺织生产过程排水量的９０％。通过多种方法试验比较，发现用锅炉炉渣过滤处理，出水水质可达到印染用水水质要求。     

宁夏灌溉回归水开发再利用的评价

宁夏灌溉回归水指灌溉农业土壤深层渗滤水、农田尾水、渠道渗漏水、退水及少量的工业废水和城镇生活污水,年排量３０～３５亿ｍ^３。对灌溉回归水２０种物质含量的评价表明,它属无毒有害型淡水。采取与渠水（来自黄河水）掺灌或轮灌对作物生长无不良影响,也不会引起土壤盐碱化,可大胆开发利用。     

三槽式切换氧化沟运行工况数学模式及应用

三槽式切换氧化沟运行工况呈周期性的变化。根据理论分析，建立了各槽活性污泥浓度变化及相互关系的数学模式，并进行了验证。同时就数字模式在周期程序设置及排泥方式选择时的应用做了说明。     

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.