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A Study of Chromium Adsorption on Natural Goethite Biomineralized with Iron Bacteria 被引量:3
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作者 SUN Zhenya ZHU Chunshui +3 位作者 HUANG Jiangbo GONG Wenqi CHEN Hesheng MU Shanbin 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2006年第4期597-603,共7页
Goethite, especially biogenic goethite, has high specific surface area and great capacity for the adsorption of many contaminants including metal ions and organic chelates. Chromium is a redox actively toxic metal ion... Goethite, especially biogenic goethite, has high specific surface area and great capacity for the adsorption of many contaminants including metal ions and organic chelates. Chromium is a redox actively toxic metal ion that exists as either Cr^Ⅲ or Cr^Ⅵ in nature, and as such it is essential to understand its behavior of adsorption on natural goethite mineralized by iron bacteria, as Gallionella and Leptothrix in water body. The adsorption of Cr^3+ and Cr^Ⅵ on naturally biomineralized goethite is studied in this paper. The results show that both Langmuir and Freundlich adsorption isothermal models are able to accurately describe the adsorption of these two ions. Investigation of SEM/EDS, TEM/EDS indicates that the two ions do not adsorb homogeneously on goethite owing to the different microstructures of goethite, and that the microspherical goethite has a greater adsorption capacity for chromium ions than the helical one. XPS data show that redox reaction of chromium on the surface of biomineralized goethite takes place in the adsorption of both Cr^3+ and Cr^Ⅵ. The CrvI adsorbed on biogoethite is much easier to transform into CrIII than the oxidization of Cr^Ⅲ on the bio-goethite. 展开更多
关键词 biomineralized goethite adsorption chromium iron bacteria
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铬取代针铁矿异化铁还原过程及铬的环境行为研究 被引量:5
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作者 王春 童辉 +2 位作者 华健 陈曼佳 刘承帅 《生态环境学报》 CSCD 北大核心 2020年第9期1883-1889,共7页
铬(Cr)是环境中常见的重金属污染物,在土壤中常与铁氧化物结合在一起,其环境行为受到土壤铁循环过程的影响;尤其是在铁还原菌作用下,该类铁氧化物容易发生还原溶解,增强了Cr的移动性。以土壤中常见的Cr(Ⅲ)取代针铁矿(CrGoe)为研究对象... 铬(Cr)是环境中常见的重金属污染物,在土壤中常与铁氧化物结合在一起,其环境行为受到土壤铁循环过程的影响;尤其是在铁还原菌作用下,该类铁氧化物容易发生还原溶解,增强了Cr的移动性。以土壤中常见的Cr(Ⅲ)取代针铁矿(CrGoe)为研究对象,利用微生物生长Logistic方程拟合、相关分析等统计方法以及X射线衍射(XRD)表征手段,研究异化铁还原菌Shewanella oneidensis MR-1对不同铬取代量针铁矿的Fe(Ⅲ)还原、重金属释放固定以及矿物物相变化。不同反应体系中Fe(Ⅱ)的生成表明,Shewanella oneidensis MR-1具备还原Cr取代针铁矿的能力;与纯针铁矿相比较,铬的取代抑制了针铁矿的铁还原过程,且铁还原效果随Cr取代率的增加而降低,其大小顺序为针铁矿>1.5%Cr-Goe>3.4%Cr-Goe>9.03%CrGoe>10.3%Cr-Goe。铁还原速率k值与针铁矿中Cr(Ⅲ)的取代量呈指数关系(R2=0.999 5,P<0.001);当针铁矿中Cr(Ⅲ)的摩尔取代量大于9.03%时,Cr-Goe的铁还原速率呈最低值,约为0.26 d-1。在异化铁还原的同时,包裹于铁矿中的Cr被释放到环境中,且随矿物二次成矿,部分Cr(Ⅲ)再一次被包裹到矿物晶格中。XRD表征显示,矿物在异化铁还原过程中,矿物相仍为针铁矿。该研究结果可为土壤铁还原过程中重金属的环境行为提供理论依据。 展开更多
关键词 异化铁还原 针铁矿 希瓦氏菌
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