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991.
福建省沿海地区海盐和大气污染物反应的致酸作用 总被引:4,自引:0,他引:4
本文着重研究福建省沿海地区盐和大气污染物反应的致酸作用,从源排放估算、致酸前体物观测、大气气溶胶组成分析、降水离子特征分析四个层次进行讨论,结果表明HCl人为排放源仅占SO2,NOs的4%;大气中活性氯;HCl最大浓度为4.23μg/m^-3,Cl2最大浓度为3.97μg.m^-3,气溶胶中Cl^-/Na^+比和降水中Cl/Na^+比背离,降水中过量氯与H浓度呈现正相关,过量氯对H浓度最大贡献达3 相似文献
992.
The excess growth of cyanobacteria in semi enclosed water areas caused by eutrophication brings about coagulation inhibition in drinking water treatment processes. In this study, coagulation inhibitor proteins produced by Microcystis aeruginosa, a major cyanobacterium in algal bloom, were acquired by a phage display technique, an aluminum-immobilized affinity chromatography and a protein expression technique using Escherichia coli cells. Two cyanobacterial peptides with a high ratio of metallophilic amino acids were recovered, which were a part of homologues of a thiol oxidase enzyme Ero1p and a trans-acting repressor ArsR. It was also shown that the homologue of ArsR exhibited a stronger inhibitory effect on the coagulation of kaolin suspension with polyaluminum chloride than the control proteins. This is the first report to identify a cyanobacterial cell component to inhibit coagulation. The compositions of polar amino acids were critical to explain the strength of coagulation inhibition potential. Polar proteins from cyanobacteria could collectively consume coagulants or stabilize clay particles, which would be plausible explanations for causing coagulation inhibition. Meanwhile, results from the kaolin coagulation tests using the control proteins implied that the neutralization of positive charges of coagulant constituents by simple electrostatic interactions might not be the key mechanism on the protein-induced coagulation inhibition. 相似文献
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994.
以凹土(AG)和聚合氯化铝(PAC)为原料,制备了纳米复合材料AG-PAC复合物(AP),探讨AG与PAC复配比(以质量比计,下同)、AP投加量、反应时间和溶液pH等因素对AP处理低浓度含磷废水的影响.结果表明,在相同的反应条件下,AP对TP的去除效果比单用PAC和AG的去除效果均要好;AG与PAC的最佳复配比为10~... 相似文献
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998.
Po Neng Chiang Ming Kuang Wang Pan Ming Huang Jeng Jong Wang 《Journal of environmental radioactivity》2010,101(6):472-481
The dynamics of Cs and Sr sorption by soils, especially in the subtropics and tropics, as influenced by soil components are not fully understood. The rates and capacities of Cs and Sr sorption by selected subtropical and tropical soils in Taiwan were investigated to facilitate our understanding of the transformation and dynamics of Cs and Sr in soils developed under highly weathering intensity. The Langmuir isotherms and kinetic rates of Cs and Sr sorption on the Ap1 and Bt1 horizons of the Long-Tan (Lt) and the A and Bt1 horizons of the Kuan-Shan (Kt), Mao-Lin (Tml) and Chi-Lo (Cl) soils were selected for this study. Air-dried soil (<2 mm) samples were reacted with of 7.5 × 10−5 to 1.88 × 10−3 M of CsCl (pH 4.0) or 1.14 × 10−4 to 2.85 × 10−3 M of SrCl2 (pH 4.0) solutions at 25 °C. The sorption maximum capacity (qm) of Cs by the Ap1 and Bt1 horizons of the Lt soil (62.24 and 70.70 mmol Cs kg−1 soil) were significantly (p < 0.05) higher than those by the A and Bt1 horizons of the Kt and Cl soils (26.46 and 27.49 mmol Cs kg−1 soil in Kt soil and 34.83 and 29.96 mmol Cs kg−1 soil in Cl soil, respectively), however, the sorption maximum capacity values of the Lt and Tml soils did not show significant differences. The amounts of pyrophosphate extractable Fe (Fep) were correlated significantly with the Cs and Sr sorption capacities (for Cs sorption, r2 = 0.97, p < 1.0 × 10−4; for Sr sorption, r2 = 0.82, p < 2.0 × 10−3). The partition coefficient of radiocesium sorbed on soil showed the following order: Cl soil ? Kt soil > Tml soil > Lt soil. It was due to clay minerals. The second-order kinetic model was applied to the Cs and Sr sorption data. The rate constant of Cs or Sr sorption on the four soils was substantiality increased with increasing temperature. This is attributable to the availability of more energy for bond breaking and bond formation brought about by the higher temperatures. The rate constant of Cs sorption at 308 K was 1.39-2.09 times higher than that at 278 K in the four soils. The activation energy of Cs and Sr sorbed by the four soils ranged from 7.2 to 16.7 kJ mol−1 and from 15.2 to 22.4 kJ mol−1, respectively. Therefore, the limiting step of the Cs+ or Sr2+ sorption on the soils was diffusion-controlled processes. The reactive components, which are significantly correlated with the Langmuir sorption maxima of Cs and Sr by these soils, substantially influenced their kinetic rates of Cs and Sr sorption. The data indicate that among components of the subtropical and tropical soils studied, short-range ordered sesquioxides especially Al- and Fe-oxides complexed with organics play important roles in influencing their capacity and dynamics of Cs and Sr sorption. 相似文献
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