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矿区河流沉积物中砷和镉浸提及浸提液的处理 期刊论文
环境科学与技术, 2018, 卷号: 41, 期号: 11, 页码: 72-80
作者:  王婧;  孙瑞川;  盛彦清;  赵国强;  杨剑
收藏  |  浏览/下载：202/0  |  提交时间：2020/07/07
沉积物  重金属  界河  化学浸提  化学沉淀法  
风化煤改变黄河三角洲盐渍化土壤溶液组分的过程 期刊论文
土壤学报, 2018, 卷号: 55, 期号: 06, 页码: 1367-1376
作者:  王洁;  校亮;  毕冬雪;  韦婧;  袁国栋
浏览  |  Adobe PDF(1485Kb)  |  收藏  |  浏览/下载：491/187  |  提交时间：2020/07/08
盐渍土改良  风化煤  钠吸附比  氯硫比  减钠脱盐  
雨生红球藻低覆盖度基因组草图分析 期刊论文
中国生物工程杂志, 2018, 卷号: 38, 期号: 07, 页码: 21-28
作者:  陈军;  郑华军;  刘亚铭;  赵国屏;  秦松
Adobe PDF(509Kb)  |  收藏  |  浏览/下载：247/77  |  提交时间：2020/07/08
雨生红球藻  基因组测序  基因预测  功能注释  
基于高通量测序技术研究土壤细菌对盐生植被演替的响应 期刊论文
土壤通报, 2018, 卷号: 49, 期号: 03, 页码: 602-608
作者:  苗菁;  宗万松;  吕敏;  丁晶;  王晓凤;  郭笃发
Adobe PDF(1170Kb)  |  收藏  |  浏览/下载：405/191  |  提交时间：2020/07/08
黄河三角洲  细菌群落结构  高通量测序  盐生植被演替  
腐殖质纳米颗粒对镉污染土壤的修复 期刊论文
环境工程学报, 2018, 卷号: 12, 期号: 05, 页码: 1295-1302
作者:  毕冬雪;  邓亚娟;  孟凡德;  韦婧;  王海龙;  袁国栋
浏览  |  Adobe PDF(411Kb)  |  收藏  |  浏览/下载：466/211  |  提交时间：2020/07/08
镉  腐殖质  土壤修复  重金属钝化剂  重金属淋洗剂  
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：537/231  |  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.