共查询到20条相似文献，搜索用时 55 毫秒
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高岭土/胡敏酸复合体对重金属离子吸附解吸实验研究 总被引：2，自引：0，他引：2
本文利用高岭土对胡敏酸吸附形成稳定的有机一无机络合物,研究了高岭土／胡敏酸复合体对Cu^2＋、Cd^2＋和Cr^2＋的吸附。结果表明,胡敏酸对高岭土改性后能提高上述三种重金属离子的吸附性能,高岭土／胡敏酸复合体对三种重金属离子的吸附量都随pH值的升高而增加,随离子强度的增加而减小。本文还研究了高岭土／胡敏酸复合体对上述三种重金属离子的吸附动力学,发现吸附过程可用Elovich方程和一级动力学方程进行较好的拟合。 相似文献
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运用十二烷基磺酸钠和聚羟基硅铝对蒙脱石进行改性后的柱撑蒙脱石,分别研究了溶液的pH值,初始浓度和反应时间对Cu2 ,Cr3 和Cd2 三种重金属离子的吸附性能、平衡模型和动力学过程。结果表明:十二烷基磺酸钠柱撑蒙脱石对三种重金属离子都具有很强的吸附能力,聚羟基硅铝柱撑粘土次之;柱撑后的蒙脱石对单组分的重金属离子的吸附平衡方程符合Langmuir模型;吸附行为的动力学符合假一级动力学方程。柱撑粘土吸附去除水中重金属离子的实验研究@刘云$华南理工大学环境科学与工程学院!广州,510640
@吴平霄$华南理工大学环境科学与工程学院!广州,5… 相似文献
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主要研究了蒙脱石吸附胡敏酸后形成的复合体对Cu2 、Cd2 、Cr3 3种重金属离子的吸附.实验结果表明:用胡敏酸对蒙脱石改性后能提高其对3种重金属离子的吸附性能,胡敏酸浓度越大,吸附性能提高程度越大,3种重金属离子的Langmuir吸附等温线线性相关都能达到0.99以上.蒙脱石/胡敏酸复合体对3种重金属离子的吸附量都随pH值的升高而增加,随离子强度的增加而减小.另外还对其吸附动力学进行了研究,发现可用Elovicb方程和双常数方程对吸附过程进行较好地拟合. 相似文献
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柱撑蛭石吸附去除废水中重金属离子的实验研究 总被引：2，自引：0，他引：2
分别利用有机柱化剂十二烷基磺酸钠(SDS)和无机柱化剂聚羟基铝(HA)对蛭石进行柱撑制得十二烷基磺酸钠柱撑蛭石(SDS-V erm icu lite)和聚羟基铝柱撑蛭石(HA-V erm icu lite),并通过XRD、红外光谱、ZETA电位等表征手段对柱撑蛭石进行表征,同时针对柱撑蛭石对Cu2 ,Cd2 ,C r3 3种重金属离子的吸附进行研究,结果表明:吸附去除率受反应时间、重金属离子的初始浓度、pH值等因素的影响,经柱撑后的蛭石对重金属离子吸附的吸附性能比蛭石原矿要强。柱撑蛭石吸附3种重金属离子的动力学吸附过程可用E lov icb方程和双常数方程进行较好的拟合。 相似文献
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柱撑蒙脱石吸附水中硫酸根离子的实验研究 总被引：18，自引：1，他引：18
在实验条件下，制备了两种柱撑蒙脱石，用X射线衍射分析和BET N2比表面积分析对其进行了表征，并对水中的硫酸根离子进行了吸附试验，通过正交实验研究了柱撑蒙脱石对水中硫酸根离子的吸附率、吸附容量及其与硫酸根离子初始浓度、PH值、吸附时间等因素间的关系，确定了它们吸附硫酸根离子的适宜条件，并与钠蒙脱石对水中硫酸根离子的吸附情况进行了对比。在此基础上初步探讨了吸附的机理，认为A13及Al2O3柱撑蒙脱石具有很强的吸附硫酸根离子的能力，在pH分别为4和5时硫酸根离子去除效果最好。 相似文献
6.
TDTMA+-柱撑蒙脱石吸附硝基苯的实验研究 总被引：3，自引：0，他引：3
以阳离子表面活性剂(十四烷基三甲基溴化铵,TDTMBA)为柱撑剂,在不同浓度条件下(0.2 CEC～2.5 CEC)制备了一系列柱撑蒙脱石,并通过XRD对有机蒙脱石进行表征,研究季铵盐离子在层间的排列结构.同时针对TDTMA -柱撑蒙脱石对硝基苯的吸附进行研究.实验结果表明,吸附去除率受硝基苯的初始浓度、反应时间等因素的影响,而与pH值没有太大的关系.经过柱撑改性后,粘土对硝基苯的吸附能力较原土有了明显的提高.随着层间柱撑浓度的增大,柱撑蒙脱石对硝基苯的吸附量也增大.另外钙基蒙脱石和平卧双层,倾斜单层以及倾斜双层的结构的TDTMA -柱撑蒙脱石对硝基苯的吸附等温线符Freundlich和Langmuir等温方程,假三层结构的TDTMA -柱撑蒙脱石对硝基苯的吸附等温线符合Linear等温方程,这表明前者是以表面吸附为主,后者是以分配作用为主. 相似文献
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锆基柱撑蒙脱石是近年来多孔材料研究的热点之一。由于大的比表面积、层间距以及孔容积，而具有良好的吸附与催化性能。近年来，锆基柱撑蒙脱石的研究进展主要集中在多种复合柱撑蒙脱石的制备，其应用多在有机物、重金属吸附和催化有机反应等方面，而对柱撑机理、层间结构的研究较少，有待深入。 相似文献
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Gilles Serge Odin 《Comptes Rendus Geoscience》2002,334(6):409-414
Lithostratigraphy, physicochemical stratigraphy, biostratigraphy, and geochronology of the 77–70 Ma old series bracketing the Campanian–Maastrichtian boundary have been investigated by 70 experts. For the first time, direct relationships between macro- and microfossils have been established, as well as direct and indirect relationships between chemo-physical and biostratigraphical tools. A combination of criteria for selecting the boundary level, duration estimates, uncertainties on durations and on the location of biohorizons have been considered; new chronostratigraphic units are proposed. The geological site at Tercis is accepted by the Commission on Stratigraphy as the international reference for the stratigraphy of the studied interval. To cite this article: G.S. Odin, C. R. Geoscience 334 (2002) 409–414. 相似文献
12.
Inter-regional correlation of transgressions and regressions in the Cretaceous period 总被引：1，自引：0，他引：1
T. Matsumoto 《Cretaceous Research》1980,1(4):359-373
Well investigated platforms have been selected in each continent, and the history of Cretaceous transgressions and regressions there is concisely reviewed from the available evidence. The factual records have been summarized into a diagram and the timing of the events correlated between distant as well as adjoining areas.On a global scale, major transgressions were stepwise enlarged in space and time from the Neocomian, via Aptian-Albian, to the Late Cretaceous, and the post-Cretaceous regression was very remarkable. Minor cycles of transgression-regression were not always synchronous between different areas. Some of them were, however, nearly synchronous between the areas facing the same ocean.Tectono-eustasy may have been the main cause of the phenomena of transgression-regression, but certain kinds of other tectonic movements which affected even the so-called stable platforms were also responsible for the phenomena. The combined effects of various causes may have been unusual in the Cretaceous, since it was a period of global tectonic activity. The slowing down of this activity followed by readjustments may have been the cause of the global regression at the end of the Cretaceous. 相似文献
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The Afyon stratovolcano exhibits lamprophyric rocks, emplaced as hydrovolcanic products, aphanitic lava flows and dyke intrusions, during the final stages of volcanic activity. Most of the Afyon volcanics belong to the silica-saturated alkaline suite, as potassic trachyandesites and trachytes, while the products of the latest activity are lamproitic lamprophyres (jumillite, orendite, verite, fitztroyite) and alkaline lamprophyres (campto-sannaite, sannaite, hyalo-monchiquite, analcime–monchiquite). Afyon lamprophyres exhibit LILE and Zr enrichments, related to mantle metasomatism. 相似文献
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正20140751 Guo Xincheng(Geological Party,BGMRED of Xinjiang,Changji 831100,China);Zheng Yuzhuang Determination and Geological Significance of the Mesoarchean Craton in Western Kunlun Mountains,Xinjiang,China(Geological Review,ISSN0371-5736,CN11-1952/P,59(3),2013,p.401-412,8 相似文献
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正20141058 Chen Ling(Key Laboratory of Mathematical Geology of Sichuan Province,Chengdu University of Technology,Chengdu610059,China);Guo Ke Study of Geochemical Ore-Forming Anomaly Identification Based on the Theory of Blind Source Separation(Geosci- 相似文献
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正20141334 Chen Kun(Institute of Geophysics,China Earthquake Administration,Beijing100081,China);Yu Yanxiang Shakemap of Peak Ground Acceleration with Bias Correction for the Lushan,Sichuan Earthquake on April20,2013(Seismology and Geology,ISSN0253-4967,CN11-2192/P,35(3),2013,p.627-633,2 illus.,1 table,9 refs.)Key words:great earthquakes,Sichuan Province 相似文献
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正20141624 Cai Xiongfei(Key Laboratory of Geobiology and Environmental Geology,Ministry of Education,China University of Geosciences,Wuhan 430074,China);Yang Jie A Restudy of the Upper Sinian Zhengmuguan and Tuerkeng Formations in the Helan Mountains(Journal of Stratigraphy,ISSN0253-4959CN32-1187/P,37(3),2013,p.377-386,5 illus.,2 tables,10 refs.) 相似文献
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正20142263Lü Shaojun(Geological Survey of Jiangxi Province,Nanchang 330030,China)Early-Middle Permian Biostratigraphical Characteristics in Qiangduo Area,Tibet(Resources SurveyEnvironment,ISSN1671-4814,CN32-1640/N,34(4),2013,p.221-227,2illus.,2tables,22refs.)Key words:biostratigraphy,Lower Permian,Middle Permian,Tibet 相似文献
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正20142560Hu Hongxia(Regional Geological and Mineral Resources Survey of Jilin Province,Changchun 130022,China);Dai Lixia Application of GIS Map Projection Transformation in Geological Work(Jilin Geology,ISSN1001-2427,CN22-1099/P,32(4),2013,p.160-163,4illus.,2refs.) 相似文献
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正20140692 Duo Tianhui(No.402 Geological Team,Exploration of Geology and Mineral Resources of Sichuan Authority,Chengdu611730,China);Wang Yongli Computer Simulation of Neptunium Existing Forms in the Groundwater(Computing Techniques for Geophysical and Geochemical Exploration,ISSN1001-1749,CN51-1242/P,35(3), 相似文献