纳滤去除地表水中微污染物生产饮用水

为了研究纳滤去除某市河水中微污染物生产饮用水的可行性,并筛选生产饮用水的最佳纳滤膜,采用四种纳滤膜DESAL 51 HL、DESAL 5 DL、UTC-20和UTC-60处理河水,研究其去除COD、UV254吸收值以及硝酸盐等微污染物效率,考察纳滤过程中水通量变化.试验结果表明,四种膜对COD和具254nm吸收值的有机物去除率在50%～95%之间,UTC-20去除有机物效率最高.DESAL 51 HL、DESAL 5 DL和UTC 60对无机物截留率在22%～65%之间,而UTC-20达到93%.UTC-20对不同原水中硝酸盐的去除率均大于70%.在短时间纳滤实验中,存在着不可逆的水通量减少,有轻度膜污染发生.结论UTC-20适用于处理有机污染和硝酸盐复合污染的地表水源生产饮用水.     

Aspects of Romanian Early-Middle Jurassic palaeobotany and palynology. Part VII. Successions and floras

The Jurassic floras of Romania occur in the Carpathian Mountains and in Dobrogea (Eastern Romania). In the South Carpathians, diverse and well preserved floras have been recorded since the middle of the 19th Century in the Resita, Sirinia, Presacina, CernaJiu, Holbav and Cristian Basins. The ages of these floras range between Hettangian and Sinemurian, with representatives belonging to Bryophytes, Pteridophytes and Gymnosperms. Excellent preservation and diversity were recorded in Anina, in the central area of the Resita Basin, a possible fossile-Lagerst?tte locality. The 3D collecting opportunities due to underground coal mining permitted detailed phytostratigraphical studies. These studies showed a floral change at the Hettangian-Sinemurian boundary, related to climate change. The Jurassic coal basins of the South Carpathians show both intramontainous and paralic features. The Resita Basin is a typical intramountainous depression basin, while the other basins are influenced by the marine realm. From a paleogeographical point of view, the Romanian Early and Middle Jurassic floras occurred on the northern frame of the Tethys realm, floristic features indicating the Eurosinian Province. One of the closest floras in terms of floristic similarities is the Iranian Early Jurassic flora. In the Apuseni Mountains, the HettangianSinemurian flora is less well-preserved and diverse than those of the South Carpathians. The Middle Jurassic flora of Romania is confined to Dobrogea (Eastern Romania), where a bennettite-dominated assemblage with low diversity and preservation was recorded.     

关于R.G.Douglas的一个问题

本注记给出一个定义在某个Banach空间上的1-1,非紧算子,它的值域不含无限维闭线性子空间。这与Douglas所提的问题有关。     

关于R.G.Douglas的一个问题

本注记给出一个定义在某个Banach空间上的1-1,非紧算子,它的值域不含无限维闭线性子空间。这与Douglas所提的问题有关。     

137Cs tracing of lacustrine sediments in the Dalian Lake, Qinghai Province, China

Based upon the analysis of Cs and grain-size parameters, the total amounts of ¹³⁷Cs deposition by wind and water in the Dalian Lake of Gonghe Basin, Qinghai Province are defined. The vertical profile of ¹³⁷Cs in the lacustrine sediments exhibits three ¹³⁷Cs activity maxima and one minimum. The major maximum corresponds to the global ¹³⁷Cs fallout in 1963; the two secondary maxima correspond to the leakage of the Chernobyl reactor in 1986 and complete desiccation of the lake in 1994, respectively. The minimum corresponds to aeolian deposition caused by extensive reclamation in the late 1980s and early 1990s. The 137Cs data set was used to evaluate average sedimentation rate of the Dalian Lake since 1963. The deposition was stable in 1963-1986 and 1994-1998, and it was rapid during 1986-1994. This preliminary study reveals that l37Cs has the same potential to trace environmental changes introduce by human interference in arid/semiarid regions as in humid regions.