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典型金矿区入湾河流重金属的时空分布特征及风险评价 期刊论文
环境化学, 2021, 卷号: 40, 期号: 4, 页码: 1167-1178
作者:  蔡永兵;  孙延康;  孟凡德;  索改弟;  李飞跃;  范行军;  张华
浏览  |  Adobe PDF(949Kb)  |  收藏  |  浏览/下载：371/200  |  提交时间：2021/12/01
矿区  界河  沉积物  重金属  时空分布  风险评价  
片段/虚拟分子印迹聚合物的应用新进展 期刊论文
色谱, 2021, 卷号: 39, 期号: 2, 页码: 134-141
作者:  王艺晓;  李金花;  王莉燕;  齐骥;  陈令新
浏览  |  Adobe PDF(1018Kb)  |  收藏  |  浏览/下载：411/169  |  提交时间：2021/12/01
分子印迹聚合物  片段印迹  虚拟模板印迹  制备  应用  综述  
环境中微塑料研究进展与展望 期刊论文
科学通报, 2021, 卷号: 66, 期号: 13, 页码: 1547-1562
作者:  骆永明;  施华宏;  涂晨;  周倩;  季荣;  潘响亮;  徐向荣;  吴辰熙;  安立会;  孙晓霞;  何德富;  李艳芳;  马旖旎;  李连祯
浏览  |  Adobe PDF(1556Kb)  |  收藏  |  浏览/下载：2779/990  |  提交时间：2021/12/01
微塑料  环境介质  环境行为  生态风险  
福建闽江口潮间带大型底栖动物次级生产力时空特征 期刊论文
海洋通报, 2020, 卷号: 39, 期号: 3, 页码: 342-350
作者:  周细平;  吴培芳;  李贞;  吴茜;  陈逸欣;  刘康格;  刘东艳;  王玉珏;  王跃启
浏览  |  Adobe PDF(594Kb)  |  收藏  |  浏览/下载：369/184  |  提交时间：2021/12/01
闽江口  大型底栖动物  次级生产力  P/B值  时空变化  
分子印迹聚合物在抗生素残留测定中的应用 期刊论文
色谱, 2020, 卷号: 38, 期号: 3, 页码: 265-277
作者:  王莉燕;  王加男;  李金花;  陈令新
浏览  |  Adobe PDF(3660Kb)  |  收藏  |  浏览/下载：289/123  |  提交时间：2021/12/01
固相萃取  样品前处理  印迹策略  分子印迹聚合物  抗生素  综述  
山东黄河三角洲国家级自然保护区鸟类多样性 期刊论文
山东林业科技, 2018, 卷号: 48, 期号: 04, 页码: 44-46+62
作者:  连海燕;  吴立新;  曹爱兰;  张孝帅
Adobe PDF(924Kb)  |  收藏  |  浏览/下载：277/84  |  提交时间：2020/07/08
自然保护区  鸟类多样性  居留型  区系  
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：526/230  |  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.