生物堆修复多环芳烃类污染土壤研究进展及工业化应用初试

土壤的多环芳烃污染日益受到社会关注,经济有效的生物修复技术逐渐成为研究热点,生物堆即其中新兴的技术之一。本文先结合国内外运用生物堆技术修复多环芳烃污染土壤的案例,从生物堆技术简介、修复过程影响因子、修复过程机理简析等三个方面进行综合阐述。在此基础上于某工业污染场地现场建立处理能力为500m3的生物堆进行为期6个月的工业化应用初试。运行结束后,各采样点最终浓度均低于风险评估中所确定的修复目标值,土壤中2环至6环的PAHs降解率依次分别为78%,55%,45%,43%和22%。最后对该技术在"土十条"出台后的研究应用进行展望。     

张家口地区土壤硒形态分布及其植物有效性初步研究

分别采集了张家口克山病区非病村4个砂土样品和重病村6个草甸土、褐土样品．用连续提取程序分离出水溶态硒、离子交换态硒、有机态硒、酸溶态硒、硫化物态硒和残余态硒。水溶态硒容易被植物吸收。交换态硒也能被植物吸收，但受到吸附环境和pH值的影响。有机结合态硒只有在碱性条件下其中的富啡酸态硒才能被植物吸收。酸溶态硒是铁锰氧化物和碳酸盐类矿物醚性淋溶作用的结果，酸性条件下硒容易流失，碱性条件下硒被原矿物固定，因此都难被植物吸收利用。硫化物态硒和残余态硒是最难溶的，基本上不被植物吸收。张家口地区重病村土《铁锰氧化物和腐殖质含量高，呈中-微酸性，而非病村正好与之相反。因此，重病村土壤虽然水溶性硒+交换态盾+有机态硒高于非病村，但这三种硒形态所反映的土壤植物有效性反而低于非病村。这可能是病村粮食比非病村低硒的原因。     

我国农耕土壤Cd污染与植物修复现状

中国人均耕地面积不足,农耕土壤的Cd污染问题对土壤资源的可持续利用和农作物的安全构成了巨大的潜在威胁。通过简述中国农耕土壤Cd污染现状和造成农耕土壤Cd污染的原因,并结合中原地区农耕土壤Cd污染调查情况,概述了中国近5年农耕土壤和农作物受到Cd污染的程度。总结近年来国家在济源开展植物修复土壤Cd污染试点工程及湖南启动长株潭耕地重金属污染修复以及农作物种植结构调整试点工程的修复效果,并简述了目前中国土壤的治理措施。最后,通过试点工程期间遇到的问题探究中国农耕土壤Cd污染的修复之路,展望未来Cd污染土壤修复工作的重点和预防措施。     

关于环境影响评价几个问题的探讨

通过对传统发展模式下的环境影响评价的分析和探讨,指出其存在的主要缺失;提出可持续发展的环境影响评价需要强化的机制和面临的新课题,对环境影响评价为当前的环境保护服务提出几点可行的建议。     

Influences of influent carbon source on extracellular polymeric substances (EPS) and physicochemical properties of activated sludge

It is necessary to understand the bioflocculation, settling and dewatering characteristics in the activated sludge process in order to establish more efficient operational strategies. The influences of carbon source on the extracellular polymeric substances (EPS) and flocculation, settling and dewatering properties of the activated sludge were investigated. Laboratory-scale completely mixed activated sludge processes were used to grow the activated sludge with different carbon sources of starch, glucose and sodium acetate. The sludge fed with acetate had highest loosely bound EPS (LB-EPS) and that fed with starch lowest. The amount of tightly bound EPS (TB-EPS), protein content in LB-EPS, polysaccharide content and protein contents in TB-EPS, were independent of the influent carbon source. The polysaccharide content in LB-EPS of the activated sludge fed with sodium acetate was lower slightly than those of starch and glucose. The sludge also had a nearly consistent flocs size and the sludge volume index (SVI) value. ESS content of the sludge fed with sodium acetate was higher initially, although it was similar to those fed with glucose and starch finally. However, the specific resistance to filtration and normalized capillary suction time fluctuated first, but finally were stable at around 5.0 × 10⁸ m kg⁻¹ and 3.5 s L g⁻¹ SS, respectively. Only the protein content in LB-EPS weakly correlated with the flocs size and SVI of the activated sludge. But there was no correlation between any other EPS contents or components and the physicochemical properties of the activated sludge.     

海洋平台桩腿周围局部冲刷及其对基础承载力的影响∗

在海洋平台桩靴基础安装施工过程中,容易发生穿透现象而导致破坏。业界建议可通过在桩靴周边加设向上的袖结构来抑制贯入时周围土体的回流,从而缓解穿透破坏。但这种袖结构的存在会导致局部冲刷,形成的冲刷坑会减小桩靴有效埋深,进而影响其使用期的承载力。通过一系列水槽试验,探讨了不同形式桩腿的面积比、开孔率、来流角度等因素对于冲刷坑形状的影响,进而开展了考虑冲刷坑影响的桩靴基础承载力数值计算,并与忽略最大冲刷深度以上土体的传统模型、假设冲刷坑为倒圆台状的简化模型计算结果进行了对比。主要研究结果如下：（1）加设圆形袖结构的桩腿引起的冲刷深度要比方形袖结构桩腿小,建议工程中采用面积比较小的圆形袖结构来缓解穿透破坏;（2）桩腿的面积比、开孔率、来流角度等因素对冲刷坑形状都存在影响。最大冲刷深度随着开孔率的增大而减小,当开孔率较大时,冲刷现象近似于群桩冲刷,出现随着冲刷角度的增大冲刷深度先增大后减小的现象;（3）当考虑冲刷坑对于桩靴承载力的影响时,简化模型能够合理反映冲刷坑对于桩靴基础承载力的影响。     

对硝基苯酚在阴-阳离子有机膨润土/水间的界面行为研究

用阴、阳离子表面活性剂改性制得一系列阴-阳离子有机膨润土,表征了有机膨润土的结构特征,研究了对硝基苯酚在阴-阳离子有机膨润土/水间的界面行为,并探讨了其吸附机理.结果表明:阴-阳离子有机膨润土的层间距和有机碳含量与改性时阴、阳离子表面活性剂的组成和配比有关;阴-阳离子表面活性剂在有机膨润土中形成了增溶(分配)作用较强的有机相,在一定配比下对水中有机污染物产生协同效应.     

载钯树脂对偶氮类染料的吸附降解及其产物对发光菌的毒性暴露试验

合成了表面负载金属钯的聚丙烯醛异烟酰腙树脂后,通过Q67发光菌的毒性暴露实验研究了该树脂材料对直接大红、直接天蓝和桃红等3种水溶性偶氮染料的催化降解效果及其在降解过程中对发光菌的生物毒性变化情况,并对降解结果进行了气相色谱-质谱(GC-MS)分析.实验结果表明:载钯树脂对直接大红、直接天蓝和桃红等偶氮染料具有良好的吸附...     

基于MIKESHE模型的潮河流域土地利用与降水变化对水文的影响评价

运用多测站校正检验机制率定方法,应用MIKESHE模型量化评价土地利用与降水变化对流域水文的影响。结果表明,尽管MIKESHE模型在流域上游大阁站的模拟性能稍逊于下会站和戴营站,3个测站校正和验证阶段的Nash-sutchliffe系数值分别为0.56和0.49、0.65和0.69、0.57和0.68,但模型对于各测站平均径流的模拟效果较好,说明该模型在潮河流域等华北土石山区具有一定的适用性和应用潜力。与基准期(1963—1979年)相比,1980—1989年潮河流域年径流量减少约22 mm,土地利用与降水变化对流域水文变化的贡献相当,两者分别占总径流变化的59%和41%;1990—1999年年径流量较基准期基本没有变化,这主要是由于降水变化与土地利用变化对流域水文的影响作用相反;2000—2008年,流域年径流量较基准期减少35 mm,降水变化对径流减少的影响作用占80%,土地利用变化则占20%。     

Application of wind-profiling radar data to the analysis of dust weather in the Taklimakan Desert

The Urumqi Institute of Desert Meteorology of the China Meteorological Administration carried out an atmospheric scientific experiment to detect dust weather using a wind-profiling radar in the hinterland of the Taklimakan Desert in April 2010. Based on the wind-profiling data obtained from this experiment, this paper seeks to (a) analyze the characteristics of the horizontal wind field and vertical velocity of a breaking dust weather in a desert hinterland; (b) calculate and give the radar echo intensity and vertical distribution of a dust storm, blowing sand, and floating dust weather; and (c) discuss the atmosphere dust counts/concentration derived from the wind-profiling radar data. Studies show that: (a) A wind-profiling radar is an upper-air atmospheric remote sensing system that effectively detects and monitors dust. It captures the beginning and ending of a dust weather process as well as monitors the sand and dust being transported in the air in terms of height, thickness, and vertical intensity. (b) The echo intensity of a blowing sand and dust storm weather episode in Taklimakan is about ?1~10 dBZ while that of floating dust ?1~?15 dBZ, indicating that the dust echo intensity is significantly weaker than that of precipitation but stronger than that of clear air. (c) The vertical shear of horizontal wind and the maintenance of low-level east wind are usually dynamic factors causing a dust weather process in Taklimakan. The moment that the low-level horizontal wind field finds a shear over time, it often coincides with the onset of a sand blowing and dust storm weather process. (d) When a blowing sand or dust storm weather event occurs, the atmospheric vertical velocity tends to be of upward motion. This vertical upward movement of the atmosphere supported with a fast horizontal wind and a dry underlying surface carries dust particles from the ground up to the air to form blown sand or a dust storm.