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Zeolite and fungi’s flocculability of simulated wastewater containing heavy metal ions or phosphorus 被引量:10
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作者 CAO Wenchuan HAO Jianchao +2 位作者 LIAN Bin LIU Congqiang WU Fengchang 《Chinese Journal Of Geochemistry》 EI CAS 2010年第2期137-142,共6页
This paper focuses on the flocculability of simulated wastewater containing heavy metal ions (Fe3+, Cd2+) or phosphorus by zeolite, microbial flocculants (MBF) produced by Aspergillus niger and the composite flocculan... This paper focuses on the flocculability of simulated wastewater containing heavy metal ions (Fe3+, Cd2+) or phosphorus by zeolite, microbial flocculants (MBF) produced by Aspergillus niger and the composite flocculant composed of zeolite and MBF. The main results are presented as follows: zeolite was a good flocculant when the contamination of the three simulated wastewaters was low, but the treated water is of turbidness and the particles in it are hard to precipitate. The MBF have a good flocculability toward Fe3+ wastewater, as well as particulate matter. Significant changes in flocculability occurred after adding the composite flocculant in different simulated wastewa-ters, the best or least effect respective for Fe3+ and Cd2+ wastewater. The research we have done shows that the method by which the composite flocculant is used to treat the wastewater containing heavy metal ions or phosphorus provides important reference value for practical application. 展开更多
关键词 含重金属离子废水 模拟废水 水絮凝 沸石 复合絮凝剂 真菌 微生物絮凝剂
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Adsorption behaviors of Cd^(2+) on Fe_2O_3/MnO_2 and the effects of coexisting ions under alkaline conditions 被引量:7
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作者 WANG Zuwei ZENG Xiangfeng YU Xiaoman ZHANG Hui LI Zhaojiang JIN Di 《Chinese Journal Of Geochemistry》 EI CAS 2010年第2期197-203,共7页
This study describes the adsorption features of cadmium on Fe2O3 and MnO2 in alkaline saline conditions. The adsorption reached equilibrium in 6 hours under alkaline conditions. The absorption of cadmium on Fe2O3 and ... This study describes the adsorption features of cadmium on Fe2O3 and MnO2 in alkaline saline conditions. The adsorption reached equilibrium in 6 hours under alkaline conditions. The absorption of cadmium on Fe2O3 and MnO2 was consistent with Freundlich absorption isotherms, and the corresponding adsorption capacities were 16.3 and 16.7 mg·g-1, respectively. Moreover, the adsorption quantity of cadmium on Fe2O3 and MnO2 rose with increas-ing pH from acidic to neutral, and reached the maximum at pH= 9. The coexisting chlorides reduced the adsorption capacity of Fe2O3 and MnO2. The influence intensities of different cations follow the order of CaCl2>>KCl>NaCl. However, the influence of sodium salts on the capacities of Fe2O3 and MnO2 to adsorb cadmium appeared more complicated: the relatively low concentrations of sodium salts could reduce the adsorption capacity; with increasing concentrations of sodium salts, e.g. NaCl and NaNO3. the adsorption capacity decreased continually. Moreover, due to the competition adsorption and precipitation effects, the adsorption capabilities of Na2CO3, NaH2PO4 and Na2HSO4 could also be reduced and cadmium concentrations in the solution were reduced as well. 展开更多
关键词 吸附行为 碱性条件 共存离子 镉吸收 FE2O3 吸附能力 二氧化锰 MNO2
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The altitude effect of ^(18)δO in precipitation and river water in the Southern Himalayas 被引量:12
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作者 WEN Rong TIAN LiDe +2 位作者 WENG YongBiao LIU ZhongFang ZHAO ZhongPing 《Chinese Science Bulletin》 SCIE EI CAS 2012年第14期1693-1698,共6页
The lapse rate of water isotopes is used in the study of the hydrologic cycle as well as in the estimation of uplift of the Tibetan Plateau.The greater elevation contrast in the Southern Himalayas allows for a detaile... The lapse rate of water isotopes is used in the study of the hydrologic cycle as well as in the estimation of uplift of the Tibetan Plateau.The greater elevation contrast in the Southern Himalayas allows for a detailed discussion about this lapse rate.We analyze variations of 18δO in precipitation and river water between 1320 m and 6700 m elevations in the Southern Himalayas,and calculate the specific lapse rate of water 18δO.The results show that the multi-year average lapse rate in precipitation over this region is 0.15‰/100 m.The one-year average lapse rate is 0.17‰/100 m from three sites along the Southern Himalayas.The two results agree,but are much lower than the global average of 0.28‰/100 m.This work also shows that there is a difference in precipitation 18δO lapse rate between the monsoon and non-monsoon seasons.The calculated precipitation lapse rate is much lower than that in surface water. 展开更多
关键词 喜马拉雅山脉 降水率 河水 高程效应 青藏高原隆升 递减率 水文循环 同位素
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