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国家自然科学基金(40303013)

作品数:7 被引量:74H指数:4
相关作者:汪福顺梁小兵刘丛强魏中青尹然更多>>
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贵州红枫湖沉积物中有机质的降解与微生物作用被引量:11
2005年
对红枫湖沉积物中有机碳, 孔隙水中的SO42-, 以及沉积物中的DNA和类脂化合物的分布进行了研究. 红枫湖沉积物有机碳的含量(23.3~76.8 mg·g-1)从上到下呈下降趋势, 0~8 cm含量最高. 沉积物孔隙水中SO42-含量为0.89~40.50 mg·L-1, 表层4 cm深度内迅速下降至12 mg·L-1, 4 cm后基本不变. 硫酸盐还原指数代表硫酸盐还原细菌对硫酸盐的还原强度, 表征SO42-作为一种电子受体在有机质降解过程中被利用的程度. 对硫酸盐还原指数SRI的计算表明有机质保留年限为14年, 与孔隙水中SO42-含量相对应. 沉积物中微生物的总DNA凝胶图像显示, DNA在0~9 cm含量相对较高, 9 cm后相对较低, 与有机碳的变化规律和SRI值一致, 表明微生物在湖泊沉积物有机质降解过程中发挥了重要作用; 缺氧条件下, SO42-是重要的电子受体被微生物利用; 沉积物中微生物的总DNA分析为分子生物地球化学研究能为湖泊营养元素循环及湖泊富营养盐化的研究提供重要手段.
魏中青刘丛强梁小兵汪福顺王少锋
关键词:有机碳SRI红枫湖沉积物
Degradation of organic matterin the sediments of Hongfeng Reservoir被引量:2
2005年
In this work, the distribution of organic carbon, DNA and lipids in the sediments of Hongfeng Reservoir were described in addition to SO42? profile in pore water. The con- tents of organic carbon in the sediments range from 23.3 to 76.8 mg·g?1, with the peak value appearing at the depth of 8 cm bellow the sediments water interface (SWI), and tend to decrease gradually with sedimentation depth. The concentra- tions of SO42? decreased from 40.50 mg·L?1 to 12.00 mg·L?1 at SWI in top 4 cm sediment, and was kept at 12.0 mg·L?1 bel- low that depth. Newly produced organic carbon can be con- served as long as 14 years in the sediments. The contents of DNA were relatively high in top 9 cm surface sediments, as revealed by agarose gel images, close to those of organic car- bon and sulphate reduction index (SRI). This study shows that bacteria played an important role in organic matter degradation; SO42? is the primary electron acceptor under anaerobic condition in this reservoir; DNA in the lake sedi- ments can provide important information for the study of cycling of nutrient elements in the lake.
WEI ZhongqingLIU CongqiangLIANG XiaobingWANG FushunWANG Shaofeng
关键词:湖泊有机物沉积物硫酸盐
滇池、红枫湖沉积物中总磷、分态磷及生物硅形态与分布特征被引量:26
2009年
通过对不同富营养化程度的湖泊(滇池及红枫湖)沉积柱剖面进行不同形态磷以及生物硅含量分析,对比了磷及生物硅的沉积分布特征,并探讨了其与湖泊富营养化演化的关系。结果表明:滇池沉积物中碎屑磷和有机磷在总磷中占50.5%~80.8%,是影响总磷趋势的主要原因;红枫湖中有机磷对总磷的贡献较大,占总磷的53%~60.9%;且两湖各形态磷均随深度的增加而减少;两湖总磷、有机磷、铝磷以及滇池沉积柱中的碎屑磷等的快速增长,表明其主要来源于人为污染;生物硅含量呈现从下层沉积物向上逐渐增加,在上层沉积物中逐渐减少的趋势;总磷、有机磷、铁结合态磷、铝结合态磷、弱结合态磷以及生物硅都能较好地反映富营养化污染的演变和现状。
吴峰炜汪福顺吴明红尹然
关键词:生物硅沉积物
Expression of c-fos and oxidative stress on brain of rats reared on food from mercury-selenium coexisting mining area被引量:2
2006年
Wanshan mercury mine is the largest mercury deposit in Guizhou Province of China, but there were few reports on mercury toxic" effect in the mining area. In order to study the neurotoxicity of food from Wanshan mercury mine area and probe into the effect of food from Wanshan mercury miner area on the changes of brain oxidative damage and expression of c-fos gene. The rats were exposed to mercury contaminated food for 20 d. The content of malondialdehyde (MDA), superoxide dismutase (SOD), GSH-peroxidase (GSH-px) and Glutathione (GSH) in rat brain was measured, and the effect of mercury contaminated rice on the expression of c-los mRNA in rat brain and the expression of c-FOS protein in cortex, hippocampus were observed using reverse transcription polymerase chain reaction (RT-PCR) and immunocytochemical methods. The results showed the levels of GSH, MDA, SOD and of GSH-dependent enzymes in the rat brain changed between exposure groups and control group; The mercury polluted rice induced significantly the expression of c-los mRNA; the c-FOS positive cells in hippocampus and cortex of exposure groups were significant different from control group (P〈0.01). It could be concluded that oxidative stress signals could contribute to the induction of immediate early genes (IEGs); free radicals and their by-products might not only cause oxidative damage, but also influenced gene expression; IEGs c-fos participated in the toxicity process of brain injury by mercury polluted food.
CHENG Jin-pingHU Wei-xuanLIU Xiao-jieZHENG MinSHI WeiWANG Wen-hua
关键词:C-FOS
A decade of variation of COD in the Changjiang River (Yangtze River) and its variation trend analysis被引量:1
2007年
The average annual value of COD (chemical oxygen demand) fluxes of the Changjiang River (Yangtze River) and its main tributaries in the past decade (i.e., 1991–2000), has been evaluated. Based on the data from the Datong Hydrological Station (DHS), it was found that the Dongting Lake drainage basin contributed the greatest water discharge (35.8%) and COD flux (48.3%) among the main tributary drainage basins, followed by the Poyang Lake drainage basin with the contributions of 15.4% and 19.3%,respectively. By the end of the year of 2000, COD flux in the Changjiang River rose by almost 45% relative to that in the year of 1991, reaching about 1941000 ton/a at DHS. Statistical analysis revealed that industrial wastewater discharge, as well as COD in it, was found decreasing in the same period, due to the gradual reinforcement of environmental management. Moreover, correlation analysis indicated that non-point pollution from agriculture and increasing discharge of domestic sewages caused by rapid growth of population along the Changjiang River drainage valley should be responsible for the high COD. Furthermore, with the current trend of population growth and agricultural development in this basin, water quality of the Changjiang River, in terms of COD level, is going to deteriorate in the near future. Thus, the rational applications of fertilizers and pesticides in agriculture and the proper treatment of domestic sewages before they are discharged would be the most concerned controlling parameters.
WANG FushunWANG YuchunZHANG Jing
关键词:长江水质量种群
铁锰在贵州阿哈湖沉积物中的分离被引量:17
2005年
贵州阿哈湖 1982年扩容后 ,长期受到煤矿废水的污染 ,大量铁、锰元素随废水带入湖中 .研究发现 :主要来自酸性矿山废水的还原态溶解铁、锰离子在入湖向下游迁移过程中发生了显著地分离 .受岩溶地区湖泊较强的酸中和能力及近年人为石灰投放的影响 ,湖泊未被酸化 ,Fe2 + ,Mn2 + 在入湖运移过程中由于氧化速率的差异 ,在不同的湖区发生沉积 ,形成了铁、锰在水平迁移上的明显分离 ;锰在深湖区上层沉积物中富集现象明显 ,并在沉积深度上与铁形成垂向上的显著分离 .经过陆源校正 ,证实铁、锰在阿哈湖的显著分离的开始是对该湖扩容事件的响应 .扩容后下游沉积物中铁含量逐渐减少 ,孔隙水中溶解铁分布特征也指示铁还原作用主要发生在沉积物下层 ,表明铁在沉积后再迁移能力较弱 .锰还原过程则发生在上层沉积物中 ,再迁移能力很强 .本研究还提出了来自煤矿废水的Fe2 + 、Mn2 + 在入湖水平运移过程中 ,铁、锰逐步分离、富集以及在沉积深度上的分离模式 .
汪福顺刘丛强梁小兵魏中青李军
关键词:沉积物矿山废水
湖泊沉积物中微量金属二次迁移过程中微生物作用的实验研究被引量:19
2006年
蓄积在湖泊沉积物中污染物质某些情况下可以成为威胁上覆水体水质安全的二次污染源.根据贵州省阿哈湖季节性缺氧的特性,通过控制氧化还原状况,设计了对该湖沉积物-水柱的原样/抑菌条件的培养实验.实验发现,微生物活动对界面附近氧化还原反应具有控制作用;改变水体的含氧状况可以显著影响上覆水体水质,包括表观性状和水体中污染物含量.聚类分析结果表明,早期成岩过程中Mn,Ga,SO4 2-,Cu,Cr,Pb和Co,Ni,Fe,Sc,V,Rb两大类分别具有相似的地球化学行为.根据实验结果,计算了厌氧培养过程中,微量元素的最大释放量,发现铁、锰在厌氧过程中可以大量向水体释放.
汪福顺刘丛强梁小兵魏中青李军徐海
关键词:湖泊沉积物微量元素
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