营养盐水平对念珠藻胞外有机物产生的影响

以我国湖泊典型固氮蓝藻发状念珠藻(Nostoc flagelliforme)为研究对象,考察了氮、磷营养盐对发状念珠藻生长特性及其胞外有机物产生的影响.采用藻细胞浓度计数法表征发状念珠藻生长特性;分别采用溶解性有机碳(DOC)、三维荧光光谱(EEM)和紫外-可见光谱法,从总量和主要物质方面分析了发状念珠藻胞外有机物的产生规律.结果表明,在不同氮、磷营养水平下,发状念珠藻的4个关键生长时期基本相同,氮是控制发状念珠藻生长的关键营养控制要素;氮营养元素浓度的增高,有利于发状念珠藻产生胞外有机物,其产生量逐渐增大,而磷营养元素浓度的增高对胞外有机物产生量贡献较小,氮营养盐是发状念珠藻产生胞外有机物的关键限制因子;通过EEM谱图分析,发状念珠藻胞外有机物主要以类氨基酸类物质和类富里酸物质为主.以磷为控制营养盐时,类富里酸是主要的胞外有机物之一,以氮为控制营养盐时,类富里酸产生量极低;作为主要的胞外有机物,蛋白质和碳水化合物的产生规律显著不同,其中蛋白质含量显著高于碳水化合物含量.     

Evaluation of the aggressive potential of marine chloride and sulfate salts on mortars applied as renders in the Metropolitan Region of Salvador--Bahia, Brazil

In recent years, growing interest has focused on determining the performance of materials and evaluating the service life of structures exposed to various environmental forces. In this context, the determination of the aggressive potential of marine salts on mortars used as external renders is critical. The present study aimed to evaluate the spatial distribution of marine salts relative to distance from the sea. This was done by monitoring the deposition rate of chlorides and sulfates in wet candle sensors, located at nine stations scattered around the Metropolitan Region of Salvador, state of Bahia, Brazil. The study also determined the effectiveness of water-soluble salts at penetrating three different types of mortars of varying cement content via deposition and diffusion. The methodology employed enabled an evaluation of the efficiency of the monitoring sensors' measurement of the aggressiveness potential of local marine aerosol, and determination of the comparative performance of the three mortars tested, from the standpoint of resistance to salt penetration. The type and amount of salts captured both in solution and in powder samples extracted from the mortars were determined by ion chromatography. The analysis of the various types of mortars tested indicated which types are more resistant to the aggressive potential of the region's marine aerosol and the distance from the shore where local buildings are liable to be most strongly affected.     

MBR在橡胶废水处理中的应用

橡胶废水具有含盐量高、色度高、有机污染成分含量高且难于生化降解等特点。膜生物反应器(MBR)技术的核心是生化处理加微滤膜过滤,通过将MBR技术应用于橡胶废水处理的实践表明,该技术对COD、氨氮、磷酸盐的平均去除率都达到了85%以上,再辅之以药剂处理后,降低了色度和难降解有机物含量,出水水质完全符合排放标准的要求,是一种解决橡胶污水处理难题的有效途径。     

水热炭化餐厨垃圾制备纳米铁/炭复合材料

以餐厨垃圾中有机组分作为碳源,通过添加铁盐水热炭化制备铁/炭纳米复合材料。考察了不同铁盐(Fe-SO4,FeCl3,Fe(NO3)3)对餐厨垃圾水热炭化物的形貌,以及氮、磷元素的迁移转化的影响;并研究了负载铁的物理、化学性质。实验结果表明,铁盐在水热炭化过程中促进了餐厨垃圾转化生成多种纳米结构。铁的价态是影响复合物形貌的主要影响因素:三价铁离子对大分子有机物的水解和炭化过程有催化作用,从而促进壳核式结构的纳米线及微米球复合物的生成;而亚铁离子则导致可溶性有机物炭化形成空心纳米球结构。负载铁的化学形态主要受阴离子的影响:硝酸铁体系中铁主要以氢氧化物形式沉积、其他阴离子体系则以磷酸盐为主要形态负载。     

成都市城区大气细颗粒物水溶性离子污染特征

为了解成都市城区大气细颗粒物水溶性离子污染特征,在成都市城区四季采集PM2.5有效样品共计102个,测得颗粒物质量浓度以及水溶性离子质量浓度(NH4+、Ca2+、Na+、Mg2+、K+、F-、NO3-、SO42-、Cl-),并分析其浓度变化特征,重点关注二次无机离子的污染特征及形成影响.结果表明,成都市城区水溶性离子与...     

Chloride Released from Three Permeable Pavement Surfaces after Winter Salt Application

Few studies exist on how chloride from chloride‐based deicers is transported in infiltration‐based stormwater control measures. In 2009, the U.S. Environmental Protection Agency (USEPA) constructed a 0.4 ha parking lot in Edison, New Jersey, that was surfaced with permeable interlocking concrete pavers (PICP), pervious concrete (PC), and porous asphalt (PA). Each surface type has four equally sized, lined sections that direct all infiltrate to separate 5.7 m³ collection tanks. The USEPA acute criterion for aquatic life (860 mg/l) was exceeded in events immediately following a snow event. Concentrations of the infiltrate exceeded the detection limit (5 mg/l) year round but did not exceed the USEPA chronic toxicity (230 mg/l) after April. The chloride concentration decreased with cumulative rainfall since previous snow event, and a power regression described this relationship. In the power regression, the coefficient (b) described the initial concentration following a snow event, and the exponent (m) described the rate in which chloride was flushed through the system with infiltrating water. PC had the largest coefficient (5,664) and largest absolute exponent (?0.92), followed closely by PICP (b = 4,943 and m = ?0.87), and distantly by PA (b = 2,907 and m = ?0.67). The differences in release rate were proportional to the measured surface infiltration rates of 4,000; 2,400; and 200 cm/h for PC, PICP, and PA, respectively. These results will assist those who manage or regulate stormwater where receiving waters are chloride impaired.     

钢筋混凝土结构盐冻破坏分析及寿命预测

为评估北方季冻区除冰盐对钢筋混凝土结构耐久性的影响,开展了混凝土试件的盐冻试验,根据试验测得的混凝土相对动弹性模量与质量损失率,分析了钢筋混凝土结构在冻融环境下的损伤情况,得到了盐冻环境下钢筋混凝土盐冻损伤度随冻融循环周期变化的关系式。同时将钢筋混凝土盐冻损伤度引入到氯离子扩散模型(DuraCete模型)中,修正了公式中氯离子扩散系数,使得该公式更适用于冻融环境,最终得到了钢筋混凝土结构的寿命预测公式。修正后的钢筋混凝土结构的寿命预测公式既考虑了冻融和氯离子侵蚀双重作用,又不需要对氯离子扩散系数进行经验取值,使得本预测模型更方便、实用。     

AFTER THE 1993 FLOOD: A WATER AND SURFICIAL BED SEDIMENT QUALITY SCENARIO ON THE ILLINOIS AND UPPER MISSISSIPPI RWERS1

ABSTRACT: Effects of the 1993 flood on river water and sediment quality were investigated using historical data and data collected from the Illinois River and Upper Mississippi River in a post‐flood period. Overall the post‐flood results showed systematic reductions and individual changes in the water and sediment constituents. The reductions in sediment metals and nutrients were most obvious at the Keokuk and Lock and Dam 26 stations. By analyzing and comparing the physical changes to the changes in water and sediment constituents at each station, it was found that physical processes such as sediment entrainment and, more importantly, the removal of fine sediment to be the main causes for the reduced concentrations in sediment constituents. On the other hand, sediment redistribution and associated secondary contamination could have caused the emergence of several water and sediment constituents that were undetected before the flood.     

黄河三角洲人工草场群落土壤盐分动态集成预报模型及其应用

提出了以ＧＭ（１,１）模型拟合发展的趋势、傅里叶变换撮周期分量ＡＲ（ｐ）模型模拟随机过程的集成预报模型,并用于黄河三角洲人工草场群落土壤盐分的定量研究中,经理论和应用检验证明：该模型能以较高的精度模拟或预报土壤盐分在较长时期内的动态变化过程,方法简单,计算工作量小,并优于传统的单一预报模型。     

柴达木盆地盐类资源成矿构造环境及成矿预测

运用区域地质资料和地球重力测量资料的分析成果,对柴达木盆地新生代地层沉积建造的空间位置和基本构造形式进行了讨论;用实验对比和地质概化的方法,建立了新生代盆地的构造边界和构造系统;用地球动力成矿和层位耦合成矿的规律说明,新生代盆地内部存在共轭成矿作用,并可用来预测成盐成矿地段和筛选寻矿找矿靶区,为中国大陆盆地的盐类矿产资源的开发和研究提供依据。根据柴达木盆地基底构造的分析,在第四纪成矿作用的基础上,在新生代地层深部寻找新的盐类矿床是大有前景的。依据成矿环境条件,圈定出5个盐类矿床的成矿构造带,是今后找矿勘探的靶区及成矿远景地带。