镧改性沸石活性覆盖控制重污染河道底泥溶解性磷酸盐和铵释放研究

通过实验考察了镧改性沸石对水中磷酸盐和铵的吸附性能,并探讨了低溶解氧情况下镧改性沸石覆盖控制底泥溶解性磷酸盐和铵态氮释放的效率.镧改性沸石对水中磷酸盐和铵的吸附动力学过程满足准二级动力学模型.镧改性沸石对水中磷酸盐的吸附平衡数据可以采用Langmuir等温吸附方程加以描述,对水中铵的吸附平衡数据可以采用Langmuir、Freundlich和Dubinin-Radushkevich(D-R)等温吸附方程加以描述.当pH 7时,镧改性沸石吸附水中磷酸盐的机制包括配位体交换、路易斯酸碱反应和静电吸引,吸附水中铵的机制是阳离子交换.镧改性沸石覆盖不仅可以有效地控制溶解性磷酸盐从底泥向上覆水的释放,而且可以明显降低铵态氮从底泥向上覆水迁移的速率.镧改性沸石覆盖量越多,控制底泥铵态氮释放的效果越好.镧改性沸石覆盖层吸附从底泥中释放出来的溶解性磷酸盐后主要以较为稳定的形态存在,低溶解氧情况下不容易重新释放出来.上述结果表明,镧改性沸石适合作为一种覆盖材料用于控制低溶解氧情况下溶解性磷酸盐和铵态氮从底泥向上覆水的释放.     

20 a来中国占补耕地光温生产潜力时空特征

研究占补耕地光温生产潜力的时空特征对指导耕地资源开发与粮食生产具有重要意义。论文基于1980年代末-2010年的多期土地利用和多年平均光温生产潜力,以占用耕地与增补耕地单位面积光温生产潜力为依据,分析20 a来中国占补耕地光温生产潜力时空特征,并进一步探讨其对光温生产潜力总量的影响。结果表明:①1980年代末-2010年,全国耕地存在明显的占优补劣情况;②从各分区看,东北平原主产区、北方干旱半干旱主产区、青藏高原区、华南主产区、云贵高原区占用耕地单位面积光温生产潜力持续高于增补耕地,长江中下游主产区占用耕地单位面积光温生产潜力持续低于增补耕地,四川盆地及周边地区、黄土高原区、海南由占优补劣变为占劣补优,黄淮海平原区由占劣补优变为占优补劣;③占优补劣对全国光温生产潜力总量变化有显著影响;④东北平原主产区等我国耕地开垦的主要区域受占优补劣的影响较大,华南主产区等耕地损失区受占优补劣的影响相对较小,占劣补优对缩小耕地占用对光温生产潜力总量影响的作用并不大。     

水解酸化工艺的研究现状与发展趋势

水解酸化工艺对各类有机物的去除率较高,可处理高浓度、难降解废水,运行费用低,在处理纺织印染、化工、造纸废水等领域发挥了重要作用。目前研究主要集中在处理复杂污染物、工艺参数优化、机理及动力学。其发展趋势大致有:与其他工艺结合,深入研究降解机理、探索微生物菌群等。     

悬浮膜(CFM)分离技术在油田废水处理中的应用

应用微电解等技术对油田废水进行预处理,然后用悬浮膜进行分离,使其中的油、微生物和固体物与水相分离,使其达到回注用水要求。重点对CFM分离设备的结构及原理加以介绍,以期推进过滤技术的进步,提高油田废水的处理水平。     

Influences of perfluorooctanoic acid on the aggregation of multi-walled carbon nanotubes

The aggregation of multi-walled carbon nanotubes (MWCNTs) in the aqueous phase not only inhibits their extensive utilization in various aspects but also dominates their environmental fate and transport.The role of surfactants at low concentration in the aggregation of MWCNTs has been studied,however the effect of perfluorinated surfactants at low concentration is uncertain.To understand this interfacial phenomenon,the influences of perfluorooctanoic acid (PFOA),and sodium dodecyl sulfate (SDS) as a control,on MWCNT aggregation in the aqueous phase were examined by the UV absorbency method.Influences of pH and cationic species on the critical coagulation concentration (CCC) value were evaluated.The CCC values were dependent on the concentration of PFOA,however a pronounced effect of SDS concentration on the CCC values was not observed.The CCC values of the MWCNTs were 51.6 mmol/L in NaCl and 0.28 mmol/L in CaCl 2 solutions,which suggested pronounced differences in the effects of Na+ and Ca2+ ions on the aggregation of the MWCNTs.The presence of both PFOA and SDS significantly decreased the CCC values of the MWCNTs in NaCl solution.The aggregation of the MWCNTs took place under acidic conditions and was not notably altered under neutral and alkaline conditions due to the electrostatic repulsion of deprotonated functional groups on the surface of the MWCNTs.     

Adsorption of 2-mercaptobenzothiazole from aqueous solution by organo-bentonite

The adsorption behavior of 2-mercaptobenzothiazole onto organo-bentonite was investigated.Natural bentonite from Gaozhou in Guangdong Province,China was collected.Organo-bentonite was prepared by intercalation of cetyltrimethyl ammonium bromide into the natural bentonite.The physicochemical properties of the prepared organo-bentonite were characterized by X-ray diffraction,N2 adsorption-desorption isotherm and Fourier transform infrared spectroscopy.The results showed that montmorillonite is the main component of the natural bentonite.The basal spacing of the natural bentonite is 1.47 nm,which increased to 1.98 nm on intercalation with cetyltrimethyl ammonium bromide.Moreover,both the surface area and pore volume increased with intercalation.Clear CH2 stretching(3000-2800 cm-1) and scissoring(1480-1450 cm-1) modes of the intercalated surfactants were observed for organobentonite.Compared with the pseudo first-order kinetic model,the pseudo second-order kinetic model is more suitable to describe the adsorption kinetics of 2-mercaptobenzothiazole onto organo-bentonite.The adsorption capacity of 2-mercaptobenzothiazole onto organo-bentonite increased with increasing initial concentration of 2-mercaptobenzothiazole,but decreased with increasing adsorbent dosage.The adsorption isotherm of 2-mercaptobenzothiazole onto organo-bentonite fits well with the Langmuir model.The maximum adsorption capacity of organo-bentonite for 2-mercaptobenzothiazole was 33.61 mg/g,indicating that organo-bentonite is a promising adsorbent for 2-mercaptobenzothiazole.     

Identification of key factors governing chemistry in groundwater near the water course recharged by reclaimed water at Miyun County, Northern China

Reclaimed water was successfully used to recover the dry Chaobai River in Northern China, but groundwater may be polluted. To ensure groundwater protection, it is therefore critical to identify the governing factors of groundwater chemistry. Samples of reclaimed water, river and groundwater were collected monthly at Chaobai River from January to September in 2010. Fifteen water parameters were analyzed. Two kinds of reclaimed water were different in type (Na-Ca-Mg-Cl-HCO3 or Na-Ca-Cl-HCO3 ) and concentration of nitrogen. The ionic concentration and type in river were similar to reclaimed water. Some shallow wells near the river bed had the same type (Na-Ca-Mg-Cl-HCO3 ) and high concentration as reclaimed water, but others were consistent with the deep wells (Ca-Mg-HCO3 ). Using cluster analysis, the 9 months were divided into two periods (dry and wet seasons), and all samples were grouped into several spatial clusters, indicating different controlling mechanisms. Principal component analysis and conventional ionic plots showed that calcium, magnesium and bicarbonate were controlled by water-rock interaction in all deep and some shallow wells. This included the dissolution of calcite and carbonate weathering. Sodium, potassium, chloride and sulfate in river and some shallow wells recharged by river were governed by evaporation crystallization and mixing of reclaimed water. But groundwater chemistry was not controlled by precipitation. During the infiltration of reclaimed water, cation exchange took place between (sodium, potassium) and (calcium, magnesium). Nitrification and denitrification both happened in most shallow groundwater, but only denitrification in deep groundwater.     

不同类型湖泊沉积物中氮释放规律研究

通过对武汉市东湖子湖郭郑湖、庙湖以及南湖这3个不同类型的湖泊进行释氮模拟实验,结果表明:(1)在厌氧条件下,不同污染程度的湖泊中沉积物释氮作用均比较明显。为了抑制沉积物向上覆水释氮,控制湖泊富营养化,保持湖泊较高的溶解氧水平是必要的。(2)在厌氧条件下,高温对不同类型湖泊总氮和氨氮的释放均能起到促进作用。(3)沉积物与上覆水间污染物的浓度梯度越大,总氮和氨氮的释放速率与释氮量也越大,此时温度的影响不明显。(4)通过比较3类湖泊沉积物上覆水中总氮和氨氮两者的释放浓度可知,氨氮的释放贡献十分显著,因此控制氨氮的释放量对于控制湖泊氮释放量具有显著效果。     

水中氨氮测定不确定度的评定

采用蒸馏-中和滴定法测定水中氨氮,建立数学模型,找出影响不确定度的来源并进行各分量不确定度的评价,如实反映测量的置信度和准确度.     

基于LandsatTM数据的济宁市水体识别方法研究

文章基于济宁市2009年LANDSAT TM影像,根据影像各波段间的相关性和地物在各影像上的灰度差异,分别采用单波段阈值法、多波段谱间关系法、改进的水体指数法(MNDWI)及HIS空间水体提取模型法对济宁市水体信息进行识别提取。在此基础上,结合归一化指数法和HIS空间水体提取模型,提出了一种综合性的水体信息提取方法,并对各方法提取结果进行了精度评价。结果表明,已有方法对济宁市水体识别存在一定的缺陷,而综合法集成了归一化指数法和HIS空间水体模型的优点,很好地弥补了已有方法的不足,对济宁市水体信息进行了较好的提取,尤其是细小水体,同时也很好地消除了建筑物、阴影、水生植被等的影响,提高了济宁市水体信息识别的精度,为更好地定量评价济宁市地表水体时空演变规律等提供帮助。