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渤海和北黄海有色溶解有机物(CDOM)的分布特征和季节变化 期刊论文
环境科学, 2018, 卷号: 40, 期号: 03, 页码: 1198-1207
作者:  刘兆冰;  梁文健;  秦礼萍;  唐建辉
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有色溶解有机物(CDOM)  紫外-可见光吸收光谱  三维荧光光谱(EEM)  平行因子分析  分布特征  季节变化  渤海和北黄海  
黄河三角洲湿地非生长季土壤CO_2浓度及地表CO_2通量的动态变化 期刊论文
生态学杂志, 2018, 卷号: 37, 期号: 09, 页码: 2698-2706
作者:  王先鹤;  王秀君;  韩广轩;  王钧漪;  宋维民;  尤再进
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土壤CO2浓度  地表CO2通量  非生长季  土壤呼吸模型  黄河三角洲湿地  soil CO2 concentration  CO2 efflux  non-growing season  soil respiration model  Yellow Ｒiver Delta wetland  
基于AIS和多尺度空间模型的船舶活动时空特征及潜在压力 期刊论文
大连海事大学学报, 2018, 卷号: 44, 期号: 03, 页码: 115-121+128
作者:  刘柏静;  贾静;  吴晓青;  杜培培
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莱州湾  海上船舶活动  时空特征  生态环境  潜在压力  船舶自动识别系统(AIS)  多尺度空间模型  
渤海三湾表层水域细菌群落结构多样性及其环境因子分析 期刊论文
微生物学通报, 2018, 卷号: 45, 期号: 09, 页码: 1956-1971
作者:  王彩霞;  王毅波;  刘鹏远;  吴霖;  孙延瑜;  胡晓珂
Adobe PDF(4487Kb)  |  收藏  |  浏览/下载：305/70  |  提交时间：2020/07/08
渤海  高通量测序  微生物多样性  细菌  
铜藻的分类地位、生物地理分布以及2016年底黄海漂浮铜藻源头的初步分析 期刊论文
海洋与湖沼, 2018, 卷号: 49, 期号: 01, 页码: 214-223
作者:  黄冰心;  丁兰平;  秦松;  付晚涛;  陆勤勤;  刘正一;  庞云龙;  李晓丽;  孙忠民
Adobe PDF(1253Kb)  |  收藏  |  浏览/下载：469/158  |  提交时间：2020/07/08
铜藻  区系  黄海  成熟型  种群  
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.  
Annual pattern of zooplankton communities and their environmental response in a subtropical maritime channel system in the northern Bay of Bengal, Bangladesh 期刊论文
ACTA OCEANOLOGICA SINICA, 2018, 卷号: 37, 期号: 8, 页码: 65-73
作者:  Abdullah Al Mamun;  Alam Md Didarul;  Akhtar Aysha;  Xu Henglong;  Islam Md Shafiqul;  Mustafa Kamal Abu Hena;  Uddin M Muslem;  Alam Md Wahidul
Adobe PDF(11061Kb)  |  收藏  |  浏览/下载：254/32  |  提交时间：2021/06/15
EAST-COAST  WATER-QUALITY  INDIA  ABUNDANCE  ESTUARY  CREEK  MESOZOOPLANKTON  COPEPODS  BIOMASS  SEA  zooplankton  trophic levels  subtropical channel  community structure  multivariate approach