湖泊沉积物中硫的地球化学循环机制研究

湖泊沉积物中的硫是控制氧化还原体系的重要元素之一。湖泊硫酸盐还原作用主要发生在沉积物表层几厘米范围内,界面硫酸盐还原具有双重环境效应。硫酸盐还原主要形成黄铁矿和有机硫,黄铁矿的生成要受到沉积物中硫酸盐、有机质以及铁氧化物活性的控制。单硫化物不稳定,并且会影响沉积物中重金属的迁移。     

Eco-environmental changes and causative analysis in the source regions of the Yangtze and Yellow Rivers, China

In the most recent four decades the eco-environment in the source regions of the Yangtze and Yellow Rivers has been continuously getting worse, this is mainly manifested in the serious vegetation degradation, rapidly developing desertification, lake shrinkage and salinization, wetland degradation and biodiversity reduction. This paper attempts to give a quantitative analysis to such eco-environmental changes and explore their causes. The main factors responsible for such changes are climate change and the alterations of glacial snow accumulation and the freeze-thaw processes of the frozen soil, as well as overgrazing and rodent damage. The eco-environmental changes in the source regions not only influence the social-economic development of these regions but also have affected, or are affecting, the whole river basins' social-economic development.     

CHANNEL INSTABILITY IN THE LOESS AREA OF THE MIDWESTERN UNITED STATES1

ABSTRACT: The bess area of the midwestern United States contains thousands of miles of unstable stream channels that are undergoing system‐wide channel‐adjustment processes as a result of (1) modifications to drainage basins dating back to the turn of the 20th century, including land clearing and poor soil‐conservation practices, which caused the filling of stream channels, and consequently (2) direct, human modifications to stream channels such as dredging and straightening to improve drainage conditions and reduce the frequency of out‐of‐bank flows. Today, many of these channels are still highly unstable and threaten bridges, other structures, and land adjacent to the channels. The most severe, widespread instabilities are in western Iowa where a thick cap of bess and the lack of sand‐and gravel‐sized bed sediments in many channels hinders downstream aggradation, bed‐level recovery and the consequent reduction of bank heights, and renewed bank stability. In contrast, streams draining west‐central Illinois, east‐central Iowa, and other areas, where the bess cap is relatively thin and there are ample supplies of sand‐and gravel‐sized material, are closer to recovery. Throughout the region, however, channel widening by mass‐wasting processes is the dominant adjustment process.     

TiO2光催化降解低浓度溴氰菊酯

用高压汞灯为光源,以二氧化钛光催化降解有机溴杀虫剂－溴氰菊酯,研究了ＴｉＯ２用量、ＰＨ值、等对降解的影响及采用太阳光做光源处理溴氰菊酯的可行性。说明以高压汞灯及太阳光作光源,ＴｉＯ２催化降解敌杀死是有效的。     

电催化降解废水中阴离子表面活性剂的研究

本文以十二烷基苯磺酸钠和十二烷基磺酸钠为研究对象,在最佳的物理化学条件下,利用紫外光谱、红外光谱和气相色谱-质谱联用等仪器分析和化学分析的方法研究了电催化降解新技术去除废水中阴离子表面活性剂的机理.实验结果表明.在羟基自由基(@OH)的氧化分解作用下,十二烷基苯磺酸钠和十二烷基碘酸钠先降解为丁烷,最终均矿化为CO2、H2O和SO42-.     

白腐真菌对染料脱色及降解过程机理和影响因素

许多白腐真菌对染料具有广谱的脱色和降解能力 ,其脱色及降解作用可能主要是由于其在次生代谢阶段产生的木质素过氧化酶LiPs和锰过氧化酶MnPs所致。培养条件对白腐真菌脱色及降解活性有较大的影响 ,在培养基中加入藜芦醇和二价锰等能够显著提高木质素过氧化酶的产生 ;富氮培养基会抑制LiPs的生成 ;硫脲、叠氮化物、氰化物等均能明显地抑制白腐真菌的脱色及降解活性 ;缓冲液的选择对维持稳定的 pH值和菌丝的形态有一定作用 ,从而影响其脱色效果 ;富氧环境是一切白腐真菌对染料进行脱色和降解的必要条件 ;适度的搅拌混合有利于反应时的物质之间传递 ;一般地 ,在培养时间达到 3天以后白腐真菌才能达到较高的脱色与降解活性。染料分子大小和结构及其基团的位置对脱色及降解效果有明显影响。使用特殊填料极大地提高处理系统中的生物量以克服真菌生长速度相对较慢、提高处理能力是该技术今后的研究重点。     

锌粉降解地下水中的农药阿特拉津

研究了Zn⁰催化还原模拟地下水中阿特拉津.结果表明,Zn⁰比Fe⁰具有更高的反应活性,反应5d对阿特拉津的降解率为100%,在Zn⁰还原脱氯的过程中,溶液的pH值逐渐增加,反应过程中通过添加磷酸缓冲溶液调节pH值,24h降解率达到100%.阿特拉津降解产物的GC/MS鉴定表明,阿特拉津还原脱氯的产物为2-乙胺基-4-乙丙胺基-1,3,5-三嗪(DCA).     

降解菌CDS-1产呋喃丹水解酶的条件及酶学特征

Sphingomonas sp.CDS-1是一株呋喃丹高效降解菌.为了给利用该菌产生的酶去除环境中的呋喃丹残留提供一些理论依据,对CDS-1产生的呋喃丹水解酶粗酶进行了研究.结果表明,在LB培养基中,CDS-1产生呋喃丹水解酶的最适条件为pH6～8、30℃、培养30h;该酶在20～30℃、pH>6.0的条件下比较稳定;在pH6.5和30℃时显示最大的呋喃丹水解酶活性;大多数金属离子浓度在0.2mmol/L时对其酶活有促进作用;酶定域实验结果显示该酶为胞内酶.     

电化学法生成Fenton试剂及其在工业染料废水降解脱色中的应用

以多孔石墨电极为阴极 ,电解时在阴极通以氧气或空气 ,电解生成的过氧化氢与阳极溶解的Fe2 +进行随后化学反应 ,现场生成羟基自由基 (Fenton试剂 ) ,进而对有机染整工业废水进行降解脱色反应。以可见光吸收谱图表征了工业染料废水经电解槽处理后吸光度的变化 ,以重铬酸钾法测试染料处理后的COD。实验结果表明 ,COD的去除率大于 80 % ,染料的脱色率达 1 0 0 % ,若将电解电流密度控制在 1 0mA/cm2 以下 ,槽电压可控制在 5V以内。实验结果表明 ,向阴极多孔石墨电极中通入空气与通入氧气的效果一致。     

Soil Fertility Quality and Agricultural Sustainable Development in the Black Soil Region of Northeast China

The black soil in northeast China is considered one of the most fertile soils in China. Consequently, the black soil region has become one of the most important regions for cereal grain production in China. Agriculture has developed rapidly since the early part of the nineteenth century. To date, approximately 70 percent of total land in the area is cultivated. Even though the agricultural production in this region is increasing continuously, some soil fertility quality problems have become serious. This is hampering agricultural development and sustainability in the region. A brief history of population growth and agricultural development in the region is presented. Major soil quality problems, particularly soil degradation and soil erosion, are analyzed. Based on studies, suggestions for improving soil quality and for promoting sustainable agricultural development in the region are presented. These suggestions include improving agricultural landscape patterns, developing conservation cultivation, promoting combinations of crop production with combinations of forestry and animal husbandry, and implementing integrated management for soil and water conservation.