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氮输入对滨海盐沼湿地碳循环关键过程的影响及机制 期刊论文
植物生态学报, 2021, 卷号: 45, 期号: 4, 页码: 321-333
作者:  韩广轩;  李隽永;  屈文笛
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氮输入  碳循环  碳分配  碳汇  滨海盐沼湿地  潮汐作用  
孔石莼净化高盐废水海藻叶表微生态分析 期刊论文
盐湖研究, 2021, 卷号: 29, 期号: 1, 页码: 99
作者:  卢文娟;  吕剑;  武君;  张宇轩;  崔德杰
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孔石莼  高盐废水  微生态  
Influence of Sea Surface Temperature on Outbreak of Ulva prolifera in the Southern Yellow Sea,China 期刊论文
中国地理科学:英文版, 2020, 卷号: 30, 期号: ., 页码: 631-642
作者:  ZHANG Guangzong;  WU Mengquan;  ZHANG Anding;  XING Qianguo;  ZHOU Min;  ZHAO Deheng;  SONGXiaodong;  YU Zhilu
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Sea  Surface  Temperature(SST)  Photosynthetically  Active  Radiation(PAR)  Ulva  prolifera  MODIS(Moderate  Resolution  Imaging  Spectroradiometer)  the  southern  Yellow  Sea  
非损伤微测Zn~(2+)选择性微电极的研发及应用 期刊论文
土壤, 2020, 卷号: 52, 期号: 02, 页码: 333-339
作者:  张云超;  李连祯;  徐世艾;  于顺洋;  李瑞杰;  骆永明
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Zn2+  非损伤微测技术  离子选择性微电极  伴矿景天  
非损伤微测Zn~(2+)选择性微电极的研发及应用 期刊论文
土壤, 2020, 卷号: 52, 期号: 2, 页码: 333-339
作者:  张云超;  李连祯;  徐世艾;  于顺洋;  李瑞杰;  骆永明
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非损伤微测技术  离子选择性微电极  伴矿景天  
烟台近海浮游动物优势种空间生态位研究 期刊论文
生态学报, 2020, 卷号: 40, 期号: 16, 页码: 5822-5833
作者:  侯朝伟;  孙西艳;  刘永亮;  张晨;  张文静;  赵建民;  董志军
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dominant zooplankton species  spatial niches  niche breadth  niche overlap  redundancy analysis (RDA)  浮游动物优势种  空间生态位  生态位宽度  生态位重叠  冗余分析(RDA)  
基于CTAC改性活性炭的信封式膜包用于水溶液中六价铬去除 期刊论文
环境化学, 2020, 卷号: 39, 期号: 9, 页码: 2593-2601
作者:  赵曼淑;  刘涛;  鹿文慧;  张晓龙;  李金花;  陈令新
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CTAC modified activated carbon  envelope-type membrane-package  Cr(Ⅵ)  removal  adsorption  CTAC改性活性炭  信封式膜包  六价铬  去除  吸附  
大叶藻(Zostera marina)海草床沉积物细菌和古菌丰度及组成的垂直剖面特征 期刊论文
微生物学通报, 2020, 卷号: 47.0, 期号: 006, 页码: 1662-1674
作者:  郑鹏飞;  张晓黎;  龚骏
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海草床  垂直剖面  微生物群落结构  丰度  多样性  
基于CTAC改性活性炭的信封式膜包用于水溶液中六价铬去除 期刊论文
环境化学, 2020, 卷号: 39, 期号: 9, 页码: 2593-2601
作者:  赵曼淑;  刘涛;  鹿文慧;  张晓龙;  李金花;  陈令新
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CTAC改性活性炭  信封式膜包  六价铬  去除  吸附  
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.