金属氧化物对CO还原NO反应的催化作用

采用固定床流动反应器,研究ＣｕＯ、Ｃｒ２Ｏ３、ＭｎＯ２、Ｆｅ２Ｏ３、Ｎｉ２Ｏ３等单元金属氧化物及它们形成的复合氧化物对ＣＯ还原ＮＯ反应的催化活性。结果表明,在５００℃８００ｍｌ／ｍ＾３ＮＯ－０．２％ＣＯ－２．０％ＣＯ２－Ｎ２气氛中ＣＯ还原ＮＯ的能力很小,稳定还原率仅为１．５０％。     

钢铁企业循环冷却水处理技术的研究

钢铁企业循环冷却水在炼铁、炼钢、连铸、轧钢等主体生产中起着至关重要的作用.通过对循环冷却水处理技术的现状分析,研究了化学药剂处理、静电水处理、磁化处理、膜处理及臭氧处理等技术,进一步研究了循环冷却水处理技术的发展趋势.     

黄土丘陵区不同水体中氢氧同位素特征及相互关系

为了研究典型黄土丘陵区不同水体氢氧同位素特征及水体间补给转化关系,合理利用干旱半干旱区水资源,通过野外采集2019年6月至11月延安市安塞墩山周围降水、河水、地下水和土壤水样品,运用同位素示踪技术,结合混合模型探索研究区不同水体氢氧同位素特征及水循环转化关系.结果表明:河水、地下水较土壤水富集氢氧同位素;各水体D和18...     

湖南长沙地区大气降水中稳定同位素特征变化

根据2010年1月~2011年2月长沙地区日降水中δD、δ18O资料,分析了该地区天气尺度下降水中δD、δ18O变化特征。结果表明:在天气尺度下长沙地区大气降水中δ18O与降水量、水汽压、温度及相对湿度之间存在显著的负相关关系,表明该地区降水中δ18O的变化具有显著的降水量效应、湿度效应及反温度效应。长沙地区的大气降水线为:δD=8.38δ18O+173〖WTBZ〗,该方程与GNIP（Globe Network of Isotopes in Precipitation）提供的长沙在月尺度下所得到的大气水线方程的斜率和截距相近,但斜率和截距都比GMWL(Globe Meteoric Water Line)偏大,说明该地区具有湿润多雨的气候特点。研究结果对揭示东亚季风区稳定同位素变化特征以及古气候的解释具有重要意义     

纳米SiO2在含阴离子表面活性剂低浊水处理中的应用

在含有阴离子表面活性剂-十二烷基硫酸钠(SDS)的6 NTU高岭土悬浊液中,改变SDS的浓度,投加纳米SiO2与聚合铝PAC进行动态混凝实验与静沉实验,借助图像分析技术与分形理论,探讨了纳米SiO2与PAC处理含SDS低浊水的作用机理、絮凝效果与形态学特征.结果表明:①纳米SiO2与SDS使高岭土粒子表面负电性增强.纳米SiO2的絮凝机理以吸附架桥为主.②纳米SiO2对SDS的去除效果优于PAC.SDS浓度越高,去除效果越显著.但纳米SiO2对无机高岭土粒子的处理能力不如PAC,PAC絮凝后的上清液浊度低.当SDS浓度增至10 mg/L时,纳米SiO2对SDS的去除率高,而PAC对SDS的絮凝能力弱,PAC对无机颗粒的去除效果也下降.③助凝剂纳米SiO2较强的吸附活性能加快PAC絮体成长为结构密实的RLCA构型,分维值高,絮凝效果好.     

Variations of sulfur isotope ratios in a single lichen thallus: A potential historical archive for sulfur pollution

Utilizing the analytical capability to measure S isotope ratios of small quantities of S in biological material without any chemical pretreatment, the variation of δ³⁴S within a lichen thallus was investigated using old and young segments of fruticose lichen thalli (Alectoria sarmentosa) from an oil refinery area in Come-By-Chance and two coastal areas, Newfoundland, Canada. Old segments of lichen samples from the oil refinery area showed significantly higher δ³⁴S values (1.0-2.5‰) than their corresponding young segments. Lichen samples from two coastal areas showed no noticeable differences in δ³⁴S values between old and young segments. These results demonstrate that lichen thalli record temporal changes in the isotopic composition of atmospheric S and hence constitute a historical archive of atmospheric S pollution.     

Reaction mode between Si and Fe and evaluation of optimal species in poly-silicic-ferric coagulant

A kind of Fe-polysilicate polymer, poly-silicic-ferric （PSF） coagulant was prepared by co-polymerization （hydroxylation of mixture of Fe^3＋ and fresh polysilicic acid （PS））, in which PSF0.5, PSF1 or PSF3 denotes Si/Fe molar ratio of 0.5, 1 or 3, respectively. The effects of Si/Fe ratio and reaction time （co-polymerization time or aging time） on the reaction mode between Si and Fe were studies, and the optimal species of PSF was evaluated by pH change during the preparation of PSF and coagulation tests. The results showed that the characteristics of PSF are largely affected by both reaction time and Si/Fe ratio. PSF is found to be a essential complex of Si, Fe, and many other ions. The reaction mode between Si and Fe differs with various Si/Fe ratios. The pH of PSF0.5, PSF1 or PSF3 tended to be stable when reaction time is 10, 25 or 55 rain, respectively, which is almost consistent with the time reaching the relative stable morphology that is just the optimal species of higher coagulation efficiency. The optimal reaction time reaching optimal species can be evaluated by measuring the pH change during the polymerization process.     

湘东北地区大气降水和地下水的氢氧稳定同位素研究

深入认识湘东北地区的水文循环过程,对规范该区水资源的有效利用和减缓该区生态环境问题具有重要意义。在2021年10月—2023年2月,对该区金井镇的大气降水和不同深度（~4.7 m和~61 m）井水每月开展样品采集和测试。该区大气降水稳定同位素值（δ¹⁸O、δD）呈现夏半年偏负、冬半年偏正,且氘盈余、水汽通量和HYSPLIT模型分析结果显示,在夏季,影响该区降水气团主要来自暖湿的海洋洋面,冬季主要来自稳定的南支西风和局地水汽输送。浅井水和深井水的δ¹⁸O和δD与该区大气降水δ¹⁸O和δD的均值接近,变幅较小且呈现夏季偏正冬季偏负的特征,说明地下水受到大气降水的补给,但可能滞后于大气降水的变化。然而,不同深度地下水对大气降水的响应机制和滞后时间,还需进一步研究。     

Using biochemical and isotopic tracers to characterise organic matter sources and their incorporation into estuarine food webs (Rufiji delta,Tanzania)

Fatty acid biomarkers and stable isotope signatures were used to identify the sources of particulate and sedimentary organic matter and its input into the food web through the dominant consumer within the mangrove-dominated Rufiji estuary, Tanzania. Specific fatty acids were used to identify the preferred basal sources of dominant fauna (i.e. filter feeder bivalves, snails, crabs, shrimps, and three fish species), and their presence in the water and sediment samples in the estuary. Both fatty acid and stable isotope results revealed that food web in the Rufiji estuary depended on a variety of carbon sources (mangroves, allochthonous terrestrial inputs, macroalgae, and phytoplankton), contributing to a different degree into the diets of primary consumers and members of near-shore fish, but none of them were obligatory for the survival of these species. The δ¹⁵N values of major primary producers and consumers/predators revealed a trend for δ¹⁵N enrichment with increasing trophic level. The ratio of docosahexaenoic acid to eicosapentaenoic acid (DHA:EPA) decreased from pelagic to benthic feeding fish. This indicated that fish with different feeding modes derived their fatty acids from different primary sources of nutrition, and suggested that the DHA:EPA ratio may be a useful indicator of feeding mode.     

伊乐藻和氮循环菌技术对太湖氮素吸收和反硝化的影响

从太湖梅梁湾采集无扰动泥芯样,分别添加固定化氮循环细菌、水生植物伊乐藻建立室内微宇宙,模拟生态修复,探讨不同修复处理下,硝氮的去除机制.采用15N标记结合同位素配对技术测定了各生态模拟柱中的反硝化速率和植物吸收速率.结果表明,不同处理的实验柱反硝化速率差异明显,同时添加了水生植物和固定化氮循环细菌的实验柱反硝化速率最高,为99.35μmol·(m2·h)-1,植物氮吸收速率为36.55μg·(m2·h)-1.沉水植物伊乐藻在自身吸收氮素的同时也提高了耦合硝化反硝化的作用.与植物吸收相比,反硝化过程是主要的氮去除途径.沉水植物与固定化氮循环菌组合生态修复技术促进了湖泊水体氮素的脱除,起到了净化作用.