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土壤中二苯砷酸的吸附解吸、结合形态与代谢转化研究进展 期刊论文
生态环境学报, 2019, 卷号: 28, 期号: 12, 页码: 2447-2453
作者:  涂晨;  路露露;  朱濛;  韦婧;  刘颖;  骆永明
浏览  |  Adobe PDF(1362Kb)  |  收藏  |  浏览/下载：810/319  |  提交时间：2020/07/08
二苯砷酸  吸附解吸  结合形态  代谢转化  铁还原  硫酸盐还原  Diphenylarsenic Acid  Adsorption-desorption  Binding Species  Metabolic Transformation  Iron Reduction  Sulfate Reduction  
土壤—水环境中二苯砷酸污染及其修复研究进展 期刊论文
土壤学报, 2018, 卷号: 56, 期号: 2, 页码: 276-285
作者:  朱濛;  骆永明;  杨如意;  周守标
收藏  |  浏览/下载：230/0  |  提交时间：2020/07/07
二苯砷酸  土壤—水环境污染  提取检测  吸附/解吸  迁移转化  物化/生物修复  Diphenylarsinic acid (DPAA)  Soil-water environmental pollution  Extraction and determination  Adsorption/desorption  Translocation and transformation  Physico-chemico/bio-remediation  
铁还原细菌Shewanella oneidensis MR-4诱导水合氧化铁形成蓝铁矿的过程 期刊论文
微生物学报, 2018, 卷号: 58, 期号: 04, 页码: 573-583
作者:  王芙仙;  郑世玲;  邱浩;  曹长乾;  唐旭;  郝立凯;  刘芳华;  李金华
浏览  |  Adobe PDF(5426Kb)  |  收藏  |  浏览/下载：622/268  |  提交时间：2020/07/08
铁还原细菌  生物诱导矿化  磁铁矿  蓝铁矿  电子显微学  激光拉曼  X射线衍射  
烟台夹河口外柱状沉积物还原性无机硫、活性铁的变化特征及其相互关系 期刊论文
海洋科学, 2018, 卷号: 42, 期号: 8, 页码: 90-97
作者:  姜明;  赵国强;  李兆冉;  盛彦清
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还原性无机硫  活性铁  深层柱状沉积物  硫化度  矿化度  Reduced inorganic sulfur  Reactive iron  Deep core sediments  Degree of pyritization  Degree of sulfidity  The distribution characteristics and coupling mechanism of reduced inorganic sulfur (RIS)and reactive iron in marine core sediments are closely related to the evolution of environment quality.In this study,an improved cold diffusion method and hydrochloric acid extraction method were applied to the acid-volatile sulfur (AVS),pyrite sulfur (CRS),elemental sulfur (ES),and reactive iron [Fe (Ⅱ)and Fe (III)] analyses.The distribution characteristics and coupling mechanism of S and Fe were investigated based on a core sediment 4 meters deep collected in the northern sea area of the mouth of Jiahe River,Yantai.The results showed that the RIS in sediments was dominated by CRS,followed by AVS and ES.The content of AVS presented a narrow range with depth,whereas the CRS and ES were higher at the top and bottom layers than the middle layer  reactive iron was dominated by Fe (II),which increased with depth,while Fe (Ⅲ)gradually decreased with depth.Most of the Fe (III)was reduced to the disssolved Fe(II),which was combined with the soluble H_2S of the sulfate-reducing bacteria to produce CRS and ES in the deep layer,resulting in their accumulation at the bottom of core sediments.Furthermore,this study showed that reactive iron was not a limiting factor for the accumulation of RIS with lower degree of pyritization and degree of sulfidity.  
厌氧微生物降解多环芳烃研究进展 期刊论文
微生物学报, 2012, 卷号: 52, 期号: 8, 页码: 931-939
孙明明; 滕应; 骆永明
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厌氧降解  多环芳烃  微生物  降解机制  
油田硫酸盐还原菌酸化腐蚀机制及防治研究进展 期刊论文
生态学报  , 2010, 卷号: 31, 期号: 2  , 页码: 575-582
庄文; 初立业; 邵宏波 
浏览  |  Adobe PDF(269Kb)  |  收藏  |  浏览/下载：1735/647  |  提交时间：2011/07/21
硫酸盐还原菌  油田  腐蚀  生物竞争排斥  分子生物学