石英表面配合物与溶解动力学模型

阐述了石英表面配合物和溶解动力学机理之间的关系，指出了石英的反应性主要受负电性表面物种的控制，从而导致电解质、离子强度、pH等因素对石英溶解的催化效应．溶解达率的提高与反应活化能的降低成活化熵的增大有关。最后，介绍了在过渡态理论和表面反应模型基础上建立的石英溶解速率方程。     

试剂管法快速测定环境水质中的洗涤剂

本文采用维多利亚蓝简易试剂管法，直接在水相中显色快速测定环境水质中的洗涤剂．此法操作简便、结果准确可靠．ｔ检验结果，Ｐ＞０．０５，简易法与标准方法之间无显著性差异，适合于现场及野外条件下使用．     

UASB-BIOFOR滤池组合工艺处理柠檬酸废水的中试研究

采用UASB-BIOFOR滤池组合工艺处理柠檬酸废水,对其中的操作步骤及注意事项进行了详细介绍.实验结果表明,该组合工艺对柠檬酸废水处理效果良好,系统出水能够达到GB 8978-1996《污水综合排放标准》中的一级标准.     

Cells of the connective tissue differentiate and migrate into pollen sacs

In angiosperms, archesporial cells in the anther primordium undergo meiosis to form haploid pollen, the sole occupants of anther sacs. Anther sacs are held together by a matrix of parenchyma cells, the connective tissue. Cells of the connective tissue are not known to differentiate. We report the differentiation of parenchyma cells in the connective tissue of two Gordonia species into pollen-like structures (described as pseudopollen), which migrate into the anther sacs before dehiscence. Pollen and pseudopollen were distinguishable by morphology and staining. Pollen were tricolpate to spherical while pseudopollen were less rigid and transparent with a ribbed surface. Both types were different in size, shape, staining and surface architecture. The ratio of the number of pseudopollen to pollen was 1:3. During ontogeny in the connective tissue, neither cell division nor tetrad formation was observed and hence pseudopollen were presumed to be diploid. Only normal pollen germinated on a germination medium. Fixed preparations in time seemed to indicate that pseudopollen migrate from the connective tissue into the anther sac.     

滇南湖群环境综合治理总体规划研究

本规划采用决策支持系统 (DSS)对湖泊的水量平衡和水质现状以及采用不同措施对水质的影响进行评估 ,并通过多标准分析 (MAC)对每项措施进行优先排序 ,使规划更具科学性和可操作性。     

BOD测定中微生物传感器法与稀释接种法的比较

用微生物传感器快速法和稀释接种法对地表水和污水处理厂出水中的生化需氧量(BOD)进行了测定,用数理统计的方法对两种方法测定的结果进行了比较。     

低浓度渣油-水系乳化液的抑尘性能现场试验研究

本文介绍了作者用渣油－水系乳化液做路面抑尘剂在某矿露天坑３种不同类型路面进行的大规模工业性试验。现场测定结果表明：这种路面抑尘剂可以获得比较理想的防尘效果，长期使用该乳化液可取得显著的综合经济效益。     

南京东郊石炭纪威宁期的风暴沉积

南京东郊石炭纪威宁期碳酸盐岩地层中普遍见有风暴沉积,以有突变的底界和底面构造、贝壳层、粒序层以及在风暴低能快速堆积条件下所形成的遮蔽构造等为基本鉴别要素,这些要素的不同组合构成的剖面结构可划分为五种类型,据此笔者提出本区风暴沉积的综合剖面结构。     

湖北黄梅乱泥滩花岗岩体的同位素年龄及成因初析

黄梅乱泥滩花岗岩侵入年龄为124.1Ma,完全冷却暴露地表年龄为80Ma,据岩石化学、稀土元素地球化学、~(87)Sr/~(86)Sr初始比值、∈Nd值、δ~(18)0值等综合分析,均显示该岩体具有“S”型花岗岩类的特征,其原始物质来自地壳。岩浆侵位深度为4.8km,结晶温度为798℃,氧逸度fO_2=1×10~(-11)a,压力P=6.57×10~8Pa岩体侵位时处于张性构造环境的陆内碰撞带。