镝—钛铁试剂—CTMAB—聚丙烯酰胺荧光体系的研究

本文将聚丙烯酰胺(PAM)应用于多元络合物荧光分析中。探讨了醇等有机溶剂对镝(Dy)—钛铁试剂(Tiron)—溴化十六烷基三甲胺(TMAB)—PAM荧光体系的溶剂化效应,讨论了体系的荧光增强机理。结果表明,PAM的吸附作用以及醇等低介电常数的有机溶剂对络合物微区静电环境的影响使荧光反应的灵敏度大大提高。可望建立一些高灵敏度的荧光测定体系。用本法测定镝的最低检测限达1×10~(-9)M(1.6×10~(-4)μg/ml),对稀土样品中镝的测定结果令人满意。     

袋除尘技术中耐高温滤料的选用与发展趋势

通过对袋除尘技术的进步分析,主要介绍了袋式除尘器滤料选择时根据的性能参数及实际的工况条件。     

普通化学教学中的几个问题

提出了普通化学教学中的几个问题．即普通化学的教学对象、教学地位及教学内容等．作者就此阐述了个人的一些教学的做法及体会．     

采用8098单片机构成切削参数实时采集系统

介绍一一种用于切削参数实时采集的８０９８单片机系统。该系统可以实时采集６路切削参数信号，具有双极性的１１位Ａ／Ｄ转换功能。可作为刀具瞬时磨损率神经网络测量的端系统。     

钼精矿氧化焙烧脱硫的研究

在八层焙烧炉内采取同一焙烧制度,辽宁钼精矿脱硫合格率高于陕西钼精矿。本文从理论和实验两方面研究其原因,并对陕西矿的焙烧工艺采取降温措施防止过热而产生烧结,使其脱硫合格率达到与辽宁矿相同的标准。     

改性壳聚糖吸附剂对水中低浓度汞的吸附

制备了几种改性壳聚糖吸附剂,通过优化试验确定了制备改性壳聚糖吸附剂的乙酸/壳聚糖浓度配比及固化碱液条件,并比较了不同吸附剂对Hg2+的吸附性能.以分子印迹法结合交联胺化改性法制备的Hg2+分子印迹改性壳聚糖吸附剂小球(P-C-CTS-ex(Hg0.3))对Hg2+具有最高的吸附容量,在低浓度Hg2+(CHg2+<40mg/L)溶液中,此吸附剂对Hg2+的吸附容量可达9.017 mg/g,比未改性壳聚糖(CTS)的吸附量高出1倍以上.研究还揭示了交联前Hg2+对壳聚糖分子中的活性氨基的保护功能及除Hg2+后的分子印迹作用.循环再生实验表明,P-C-CTS-ex(Hg0.3)经过8个循环以后的吸附容量保持稳定,颜色与外观等基本不变,重复使用性能稳定;而未改性CTS吸附剂经过"吸附-脱附-再生"8个循环后,球体积明显变小,颜色逐渐变黄,吸附容量不稳定.这表明本研究制备的Hg2+分子印迹改性壳聚糖吸附剂的吸附容量和再生性能均明显优于普通壳聚糖吸附剂,具有应用于含Hg废水处理的潜力.     

Protection efficacy of national wetland reserves in China

Wetlands have the most abundant biodiversity,the highest carbon sequestration capacity,and the highest values for ecological services per unit area,of all the world’s ecosystems.Practice has shown that establishing reserves is the most effective way of protecting typical ecosystems and their biodiversity,and saving rare or endangered wildlife.The Chinese government’s policy is to protect wetland systems by establishing reserves that encompass a massive network of wetlands,including wetland nature re-serves,internationally important wetlands,and wetland parks.Many are already established.The effect of protecting wetland nature reserves at the national level has not yet been reported.We used the latest database evaluating the protection value of wet-land reserves,and remotely sensed wetland maps(1978-2008) ,developed by the same mapping specialists and based on the same classification system,and related environmental data,to evaluate the effects of protecting China’s national wetland reserves over the last 30 years.We conclude that(i) the total area of wetland in the national wetland reserves has decreased over the last 30 years to 8152.47 km2,and just 8% of China’s net decrease in wetlands;(ii) about 79% of the 91 national wetland reserves are in a poor condition.These are generally located around the Yangtze River,Eastern Coast,the Three Rivers Source,and Southwest China.Protection measures should be undertaken urgently in these areas.Only 15% of national wetland reserves are under sound protection,and these are generally located in the upper reaches of the Songhua River;(iii) although 88% of national wetland re-serves are primitive(relatively natural) ,implying that the site selection has been scientific,a high percentage of national wetland reserves show early warning signs of decline and require urgent attention;(iv) based on our evaluation of protection effects and pressures on ecology,we have made a priority list of national wetland reserves,and propose several protection strategies.     

十氢十硼酸双四乙基铵/纳米铝复合物的制备及其性能

为了改善硼氢燃料的能量输出特性,提高其作为推进剂及火炸药添加剂的燃烧效率,使用溶剂-非溶剂法制备了十氢十硼酸双四乙基铵/纳米铝含能复合物,并对其表面形貌、比表面积、热性能及气体分解产物进行了研究。结果表明,使用溶剂-非溶剂方法可制备具有良好分散性的十氢十硼酸双四乙基铵/纳米铝复合物,并能极大的减少纳米铝的团聚。复合物的比表面积为7. 06 m~2/g,远大于混合物的0. 20 m~2/g。BHN-10/纳米铝复合物在分解过程中可形成一种熔融分解型的中间产物,分解过程分为两个阶段,两阶段的分解温度分别为285. 1℃和304. 4℃,在形成BHN-10/纳米铝复合物后分解温度提前,第一分解放热峰提前到262. 0℃,第二分解放热峰提前到298. 8℃。分解气体产物主要为乙烯、乙烷、氨气和氢气等具有高热值的可燃性小分子气体。     

几个扩展基础上的载荷试验及其蠕变行为研究

应用一个新的模型分析了几个扩展基础载荷试验,着重揭示前人无法解释的土体的蠕变行为。发现:使用的模型能够表征扩展基础载荷试验下土体的蠕变行为,且经模型变换后的应变时间曲线在双对数轴上是一条直线,其斜率为模型的指数n值,且n的取值与模型的参考量无关;载荷试验下土体蠕变行为的原始数据受到木制反力梁的自重蠕变、卸载-再加载、不等的蠕变观察时间等三个因素的干扰,当剔除这些干扰后得到的n值荷载水平曲线,显示n值与应力水平无关,n可以被看作表征土体的蠕变特性的一个指标。     

Lithium isotope evidence for subduction-enriched mantle in the source of mid-ocean-ridge basalts

'Recycled' crustal materials, returned from the Earth's surface to the mantle by subduction, have long been invoked to explain compositional heterogeneity in the upper mantle. Yet increasingly, problems have been noted with this model. The debate can be definitively addressed using stable isotope ratios, which should only significantly vary in primitive, mantle-derived materials as a consequence of recycling. Here we present data showing a notable range in lithium isotope ratios in basalts from the East Pacific Rise, which correlate with traditional indices of mantle heterogeneity (for example, 143Nd/144Nd ratios). Such co-variations of stable and radiogenic isotopes in melts from a normal ridge segment provide critical evidence for the importance of recycled material in generating chemical heterogeneity in the upper mantle. Contrary to many models, however, the elevated lithium isotope ratios of the 'enriched' East Pacific Rise lavas imply that subducted ocean crust is not the agent of enrichment. Instead, we suggest that fluid-modified mantle, which is enriched during residency in a subduction zone, is mixed back into the upper mantle to cause compositional variability.