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991.
湖泊沉积物中硫的地球化学循环机制研究 总被引:2,自引:0,他引:2
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。 相似文献
992.
Eco-environmental changes and causative analysis in the source regions of the Yangtze and Yellow Rivers, China 总被引:4,自引:0,他引:4
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. 相似文献
993.
Andrew Simon Massimo Rinaldi 《Journal of the American Water Resources Association》2000,36(1):133-150
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. 相似文献
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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。 相似文献
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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. 相似文献
999.
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 总被引:2,自引:0,他引:2
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。 相似文献
1000.
Soil Fertility Quality and Agricultural Sustainable Development in the Black Soil Region of Northeast China 总被引:2,自引:0,他引:2
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. 相似文献