不同草皮构建的湖泊缓冲带对污染物的净化效果研究

选择宜兴地区常见的3种草皮百慕大(Cynodon dactylon)、白花三叶草(Trifolium repens)、高羊茅(Festuca arundinacea),利用自行设计的实验装置模拟构建草皮缓冲带,并模拟宜兴地区降雨时产生的汇流过程和雨量进行太湖缓冲带对陆域面源污染物的净化效果研究.结果表明,草皮缓冲带能有效地截留径流中的SS,3种草皮缓冲带的径流对SS的去除率为百慕大缓冲带＞三叶草缓冲带＞高羊茅缓冲带＞空白对照(不种植草皮的空白土壤),且沿程去除效果增强;草皮缓冲带的渗流对TN、NH3-N、TP净化效果均显著(p＜0.05)高于径流;3种草皮缓冲带在试验槽前0.9m处的污染物去除效果最为明显,湖泊缓冲带的宽度与其污染物截留效果呈正比;总体来说,草皮生物量与其构建的湖泊缓冲带的污染物去除率呈正相关,三叶草和百慕大有较大的地上生物量,其构建的缓冲带表现出较高的污染物去除率,而高羊茅的地上生物量相对较小,其构建的缓冲带污染物去除率也相对较低.     

聚合氯化铝铁絮凝剂的性能研究

煤矸石是采煤过程之废料。本文利用煤矸石制备出了聚合氯化铝铁（ＰＡＦＣ）：一种新型无机高分子絮凝剂，探讨了Ｆｅ＾３＋的稳定性与溶液离子强度之间的关系，发现溶液的离子强度越大，则产生Ｆｅ（ＯＨ）３沉淀时的ＰＨ越高。研究了ＰＡＦＣ水解产物的ζ电位及絮凝效果随ＰＨ的变化情况，比较了ＰＡＦＣ、ＰＡＣ和ＰＦＳ的除浊性能，ＰＡＦＣ在ＰＨ为７．０－８．２范围内除浊效果最佳，ＰＡＦＣ的除浊效果优于ＰＡＣ。     

酸性降水中甲醛的测定方法及其稳定性研究

本文研究了测定酸雨中游离甲醛和络合甲醛总量的方法，在液相中ＨＣＨＯ与Ｓ（Ⅳ）络合生成ＨＭＳＡ，通过加入Ｉ２丙酮溶液使甲醛游离出，再使用ＮａＳｈ试剂（乙酰丙酮和铵）在６０℃水浴中显色３０ｍｉｎ后在４１５ｎｍ光度测定，甲醛总量的检出率≥９７％。１９９２年夏季用该方法测定北京市雨水，其络合甲醛和游离甲醛各占５０％左右。测定甲醛总量时，雨样的最佳保护剂是ＮａＨＳＯ３。测定游离甲醛时，雨样的最佳保护剂是Ｈｇ     

砾间接触氧化法对白鹤溪低污染水体的净化效果

为研究生物膜技术在低污染水体净化中的应用前景,以洱海入湖河流——白鹤溪为研究对象,采用分段进水和分区曝气方式强化砾间接触氧化工艺的脱氮性能,探讨HRT(水力停留时间)、O/A(曝气区和非曝气区容积比)对低污染水体中COD_Mn、NH₄+-N、TN去除的影响. 结果显示:①HRT对有机物去除效果影响较大,在HRT为0.8、1.5、2.5、3.5 h下,COD_Mn去除率平均值分别为14.7%、28.6%、42.7%、48.8%;而当HRT为2.5 h时为较佳运行工况,COD_Mn、NH₄+-N、TN去除率平均值分别为42.7%、83.6%、31.6%. ②O/A对NH₄+-N的去除影响不大,在O/A为1∶1、1∶2、1∶3下,NH₄+-N去除率平均值分别为86.7%、83.1%、80.5%;而当O/A为1∶3时具有较佳的脱氮除碳效果,COD_Mn、NH₄+-N、TN去除率平均值分别为42.2%、80.5%、40.2%. ③在HRT为2.5 h、O/A为1∶3下稳定运行15 d后,对生物膜样品的微生物群落结构分析表明,在装置后段有脱氮微生物的富集,其优势菌为Pseudomonas、Pantoe、Synechococcus、Chloroflexi bacterium. 研究表明,砾间接触氧化工艺对低污染水具有较好的脱氮除碳效果.      

不同粒径方解石在不同pH值时对磷的等温吸附特征与吸附效果

以天然方解石为材料,研究了不同pH值与不同粒径方解石对磷吸附效果的影响.实验设置了不同质量浓度磷系列溶液,加人1g不同粒径,即小于100目、100～180目、180～325目和325目的方解石,在PH值分别为9.00±0.02、7.00±0.02和6.00±0.02时.研究方解石对磷的吸附效果,并用Langmuir模型和Freundlich模型对等温吸附线进行了拟合.结果表明,方解石对磷的吸附等温线能较好地用Freundlich方程来拟合.方解石的粒径越小,对磷的吸附能力越强,在本实验选取的粒径范围内,325目方解石对磷酸盐的吸附效果最好;但180～325目方解石对磷的吸附能力与325目方解石的差别不大,实际应用中,选用180～325目方解石即可取得对磷的较好的吸附效果.pH值是影响方解石吸附磷的重要因素,pH为6时,由于方解石微溶产生的Ca2 与水体中PO3-4结合形成Ca-P化合物,使其吸附磷效果较好;pH≥7时,通过方解石吸附作用、与碳酸钙共沉作用及以方解石作为结晶核的钙磷化合物结晶作用去除磷;pH为9时方解石对PO3-4吸附效果好于pH值为7时.     

Control concept and countermeasures for shallow lakes’ eutrophication in China

Research on lake eutrophication in China began in the early 1970s, and many lakes in China are now known to be in meso-eutrophic status. Lake eutrophication has been showing a rapidly increasing trend since 2000. Investigations show that the main reasons for lake eutrophication include a fragile lake background environment, excessive nutrient loading into lakes, excessive human activities, ecological degeneration, weak environmental protection awareness, and lax lake management. Major mechanisms resulting from lake eutrophication include nutrient recycling imbalance, major changes in water chemistry (pH, oxygen, and carbon), lake ecosystem imbalance, and algal prevalence in lakes. Some concepts for controlling eutrophication should be persistently proposed, including lake catchment control, combination of pollutant source control with ecological restoration, protection of three important aspects (terrestrial ecology, lake coast zone, and submerged plant), and combination of lake management with regulation. Measures to control lake eutrophication should include pollution source control (i.e., optimize industrial structural adjustments in the lake catchment, reduce nitrogen and phosphorus emission amounts, and control endogenous pollution) and lake ecological restoration (i.e. establish a zone-lake buffer region and lakeside zone, protect regional vegetation, utilize hydrophytes in renovation technology); countermeasures for lake management should include implementing water quality management, identifying environmental and lake water goals, legislating and formulating laws and regulations to protect lakes, strengthening publicity and the education of people, increasing public awareness through participation in systems and mechanic innovations, establishing lake region management institutions, and ensuring implementation of governance and management measures.     

土壤气相抽提法去除红壤中挥发性有机污染物的影响因素研究

土壤气相抽提技术(SVE)是一种安全、经济、高效的土壤治理技术,广泛应用于不饱和土壤中挥发性有机污染物的去除.本实验以我国南方典型土壤红壤(粘性较大的土壤)为实验土样,选用最常见的挥发性有机物苯作为污染物,采用一维土柱通风模拟SVE过程,研究了通风流量、土壤含水率以及间歇操作对苯污染红壤去污过程的影响.结果表明,在各土柱垂向气相中苯浓度变化趋势一致,通风初期浓度迅速降低后进入长时间的拖尾阶段,拖尾阶段初期进行间歇操作可降低能耗达到较经济的治理效果.通风流量与土壤含水率是影响净化时间和修复效果的重要因素,两者均存在最佳值.当通风流量为600 mL/min,含水率为17.2%时本实验净化时间降低为36 h,去除率为99.9%,达到了最佳的治理效果.     

崖角藤的化学成分

从天南星科崖角藤茎95%乙醇提取物中分离得到10个化合物,通过波谱数据鉴定为羽扇豆醇乙酸酯(1)、羽扇豆醇(2)、β-谷甾醇(3)、桦木醇(4)、桦木酸(5)、硬脂酸(6)、ficubee A(7)、ficubee B(8)、artelastin(9)和β-胡萝卜苷(10).     

4-[1-Ethyl-1-methylhexy]-phenol induces apoptosis and interrupts Ca2+ homeostasis via ROS pathway in Sertoli TM4 cells

Environmental Science and Pollution Research - Biological effect of an individual nonylphenol (NP) isomer extremely relies upon the side chain structure. This research was designed to evaluate the...     

Analysis of the phenolic compounds in root exudates produced by a subalpine coniferous species as responses to experimental warming and nitrogen fertilisation

In terrestrial ecosystems, plant root exudates clearly play a crucial role in the belowground ecosystem. However, there have been few reports on root exudates from field-grown plants or mature trees in situ, especially when exposed to experimental warming. In this study, we adopted and modified a culture-based cuvette system developed especially for root exudation collection in the field to collect soluble root exudates of a subalpine coniferous species, Abies faxoniana, under experimental warming and nitrogen fertilisation treatments. We then analysed the chemical composition and relative abundance of root exudates using gas chromatography-mass spectrometry (GC-MS). The major chemical constituents of root exudates were phenols and their derivatives of all the different treatments, such as 2,6-di-tert-butyl-4-methylphenol. Experimental warming had significant effects on the relative contents of major compounds and an increase effect on the total phenolic acid compounds. By contrast, there were small significant effects of N fertilisation on root exudation and no significant effects of the warming×N fertilisation interaction. Meanwhile, warming also markedly increased soil polyphenol oxidase activity and it may be soil ecological adjustment response to changes of root exudation under global climate warming.