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海水中活性铁检测的研究进展 期刊论文
海岸科学, 2022, 卷号: 9, 期号: 1, 页码: 24-31
作者:  王晨晨;  韩海涛;  潘大为
Adobe PDF(1488Kb)  |  收藏  |  浏览/下载：335/1  |  提交时间：2022/07/26
活性铁  海水  形态分析  电化学方法  
塑料污染生物降解及其评价分析方法研究进展 期刊论文
海岸科学, 2021, 卷号: 8, 期号: 2, 页码: 1-8
作者:  杜泓钰;  王巧宁;  王虹丹;  王运庆;  陈令新
Adobe PDF(540Kb)  |  收藏  |  浏览/下载：416/93  |  提交时间：2021/11/30
微纳塑料  生物降解  分析方法  
近20年来我国沉积物环境与污染控制研究进展与展望 期刊论文
地球科学进展, 2021, 卷号: 36, 期号: 4, 页码: 346-374
作者:  范成新;  刘敏;  王圣瑞;  方红卫;  夏星辉;  曹文志;  丁士明;  侯立军;  王沛芳;  陈敬安;  游静;  王菊英;  盛彦清;  朱伟
浏览  |  Adobe PDF(6042Kb)  |  收藏  |  浏览/下载：717/339  |  提交时间：2021/12/01
沉积物  环境效应  生态风险  质量基准  污染控制与修复  处理利用  中国  
黄海近岸溶解活性态铁定点连续分析研究 期刊论文
海洋环境科学, 2021, 卷号: 40, 期号: 4, 页码: 492-496
作者:  丁小艳;  陶文艳;  韩海涛;  潘飞;  潘大为
浏览  |  Adobe PDF(2105Kb)  |  收藏  |  浏览/下载：348/151  |  提交时间：2021/12/01
溶解活性态铁  黄海  潮汐  连续监测  
不同前处理方法对沉积物中镉赋存形态分析的影响 期刊论文
环境工程, 2018, 卷号: 36, 期号: 12, 页码: 93-97+129
作者:  王婧;  孙瑞川;  杨剑;  宋江敏;  盛彦清
收藏  |  浏览/下载：227/0  |  提交时间：2020/07/07
沉积物  镉形态分析  Tessier连续提取法  前处理  sediment  speciation analysis of cadimum  tessier sequential extraction method  pretreatment  
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
浏览  |  Adobe PDF(1528Kb)  |  收藏  |  浏览/下载：528/230  |  提交时间：2020/07/08
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.  
海岸带表层沉积物中磷的地球化学特征 期刊论文
中国环境科学, 2014, 卷号: 34, 期号: 1, 页码: 246-252
曲瑛璇; 盛彦清; 丁超锋; 孙启耀
浏览  |  Adobe PDF(296Kb)  |  收藏  |  浏览/下载：818/269  |  提交时间：2014/07/07
沉积物  磷形态  莱州湾  分布特征  磷的连续提取法