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31.
Shixiang Li Xulan Zhang Er Bei Huihui Yue Pengfei Lin Jun Wang Xiaojian Zhang Chao Chen 《环境科学学报(英文版)》2017,29(8):331-339
N-nitrosodimethylamine(NDMA) precursors consist of a positively charged dimethylamine group and a non-polar moiety, which inspired us to develop a targeted cation exchange technology to remove NDMA precursors. In this study, we tested the removal of two representative NDMA precursors, dimethylamine(DMA) and ranitidine(RNTD), by strong acidic cation exchange resin. The results showed that pH greatly affected the exchange efficiency, with high removal(DMA 78% and RNTD 94%) observed at pH pk_a-1 when the molar ratio of exchange capacity to precursor was 4. The exchange order was obtained as follows: Ca~(2+) Mg~(2+) RNTD~+ K~+ DMA~+ NH_4~+ Na~+. The partition coefficient of DMA~+to Na~+was 1.41 ± 0.26, while that of RNTD~+to Na~+was 12.1 ± 1.9. The pseudo second-order equation fitted the cation exchange kinetics well. Bivalent inorganic cations such as Ca~(2+)were found to have a notable effect on NA precursor removal in softening column test. Besides DMA and RNTD, cation exchange process also worked well for removing other 7 model NDMA precursors. Overall, NDMA precursor removal can be an added benefit of making use of cation exchange water softening processes. 相似文献
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33.
Yilei Yu Xianfang Song Yinghua Zhang Fandong Zheng Ji Liang Dongmei Han Ying M Hongmei Bu 《环境科学学报(英文版)》2013,25(9):1754-1763
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. 相似文献
34.
新型磁性聚谷氨酸吸附剂对水中Pb2+的吸附去除 总被引:2,自引:1,他引:1
德岛大学安澤幹人首次利用γ-PGA在Fe3O4磁性纳米颗粒上进行涂层,制得了γ-聚谷氨酸-Fe3O4磁性纳米颗粒(PG-M).本实验利用透射电镜以及扫描电镜对PG-M吸附剂的形貌进行了分析,发现PG-M与未涂层的Fe3 O4具有相似的形状以及大小,均为不规则的层状结构,且晶粒直径在120~320 nm之间;实验中针对性地对水溶液中Pb2+进行了吸附探讨.在振荡实验中,通过主要参数的变化(pH值、吸附时间、竞争离子浓度、腐殖酸浓度),得到如下结果:吸附最佳pH值为7.0;吸附量随着吸附时间的延长而增长,吸附平衡时间为45 min;Na+对PG-M去除Pb2+没有很强的干扰性,而Ca2+则显示出一定的干扰作用;腐殖酸对吸附效果的影响是复杂的,表现为先增强吸附效果,随后降低吸附效果;最佳条件时Pb2+的最大吸附量为93.3 mg/g.PG-M对Pb2+的吸附均能较好地符合Freundlich和Langmuir等温吸附模型,其中Langmuir方程能更好地描述PG-M的吸附特征,说明PG-M在水溶液中对金属离子的吸附为单分子层吸附.PG-M吸附符合准二级动力学模型(r2〉0.99).不同浓度的HCl和HNO3溶液的再生实验发现,0.1 mol/L的HCl溶液作为吸附再生液,可取得较好的再生效果.表明PG-M是可再生的,具有较好的经济性和可持续性. 相似文献
35.
针对石化工业废水开展沸石强化脱氮处理试验研究,通过比较沸石浓度25mg/L与空白,以及沸石浓度25 mg/L与50mg/L两阶段脱氮效果,探讨沸石促进脱氮功能的机理,结果表明,曝气池中投加沸石可明显提高氨氮和总氮的去除率,硝化细菌总数和硝化功能也得到增强。与空白对照组相比, 沸石浓度25mg/L的试验组运行稳定后,氨氮去除率提高约10%~13%,总氮去除率约提高13%,出水中NO3--N含量约提高100%,氨氮与总氮之比下降6%,内源硝化耗氧呼吸速率可提高138%,硝化细菌总数是空白对照组2.2folds。沸石浓度提高到50mg/L后,试验组的脱氮效果略有增加,但效果不明显。通过对试验结果的关联分析,认为沸石提高系统脱氮能力的原因一方面是因为沸石对NH4+及硝态氮的交换吸附,另一方面NH4+离子富集于沸石表面及内部、沸石颗粒独特的好氧-缺氧微环境,以及沸石离解出CO32- 或HCO3-增加碱度等条件,促进了硝化细菌和反硝化细菌的生长,从而提高了系统脱氮能力。 相似文献
36.
R. AndrewsAuthor VitaeJ.M. PearceAuthor Vitae 《Journal of Cleaner Production》2011,19(13):1446-1454
As the economic costs of energy and the negative externalities associated with the combustion of fossil fuels threaten the economic viability of greenhouses in northern climates there is a renewed interest in the use of waste heat. This paper presents a technical and economic methodology to determine the viability of establishing waste heat greenhouses using the waste heat from industrial processes in northern climates. A case study is presented of an exchange between a tomato greenhouse and a flat glass manufacturing plant, which found the waste heat system is significantly more economic to operate than a purely natural gas system. 相似文献
37.
春、夏季长江口及其邻近海域溶解N2O的分布和海-气交换通量 总被引:1,自引:1,他引:0
分别于2012年3月和7月对长江口及其邻近海域进行了调查,对水体中溶解氧化亚氮(N2O)的分布及海-气交换通量进行了研究.结果表明,春季长江口及其邻近海域表层海水中溶解N2O浓度范围为9.34~49.08 nmol·L-1,平均值为(13.27±6.40)nmol·L-1.夏季表层溶解N2O浓度范围为7.27~27.81 nmol·L-1、平均值为(10.62±5.03)nmol·L-1.两航次表、底层海水中溶解N2O浓度相差不大.长江口溶解N2O浓度由近岸向外海逐渐降低,受陆源输入影响显著.溶解N2O浓度高值出现在长江口最大浑浊带附近,这主要是由于水体中较高的硝化速率造成的.温度是影响N2O分布的另一个重要因素,对溶解N2O浓度有双重作用.春季和夏季表层海水中N2O饱和度范围分别为86.9%~351.3%和111.7%~396.0%,平均值分别为(111.5±41.4)%和(155.9±68.4)%,大部分站位处于过饱和状态.利用LM86、W92和RC01公式分别计算了长江口及其邻近海域N2O的海-气交换通量,春季分别为(3.2±10.9)、(5.5±19.3)和(12.2±52.3)μmol·(m2·d)-1,夏季分别为(7.3±12.4)、(12.7±20.4)和(20.4±35.9)μmol·(m2·d)-1,初步估算出长江口及其邻近海域的年平均释放量分别为0.6×10-2Tg·a-1(LM86)、1.1×10-2Tg·a-1(W92)、2.0×10-2Tg·a-1(RC01).长江口及其邻近海域虽然只占全球海洋总面积的0.02%,但其释放的N2O占全球海洋释放量的0.06%,表明长江口及其邻近海域是产生和释放N2O的活跃区域. 相似文献
38.
软弱结构面塑性程度高、强度低,在地下水长期作用下,很易导致岩体产生变形、形成集中渗漏通道及渗透破坏.软弱结构面的渗透稳定性,一直是水利水电工程的重要工程地质及水文地质问题之一,目前对其渗透破坏机理的认识还存在不少尚未解决的问题.针对已有对基岩软弱结构形成集中渗漏通道研究的不足,本文在软弱结构面内讨论渗透变形问题,主要探... 相似文献
39.
Paoletti E Contran N Manning WJ Castagna A Ranieri A Tagliaferro F 《Environmental pollution (Barking, Essex : 1987)》2008,155(3):464-472
Treatments with ethylenediurea (EDU) protect plants from ozone foliar injury, but the processes underlying this protection are poorly understood. Adult ash trees (Fraxinus excelsior), with or without foliar ozone symptoms in previous years, were treated with EDU at 450ppm by gravitational trunk infusion in May-September 2005 (32.5ppmh AOT40). At 30-day intervals, shoot growth, gas exchange, chlorophyll a fluorescence, and water potential were determined. In September, several biochemical parameters were measured. The protective influence of EDU was supported by enhancement in the number of leaflets. EDU did not contribute its nitrogen to leaf tissue as a fertiliser, as determined from lack of difference in foliar N between treatments. Both biochemical (increase in ascorbate-peroxidase and ascorbic acid, and decrease in apoplastic hydrogen peroxide) and biophysical (decrease in stomatal conductance) processes regulated EDU action. As total ascorbic acid increased only in the asymptomatic trees, its role in alleviating O(3) effects on leaf growth and visible injury is controversial. 相似文献
40.