杭州萧山区饮用水源地铁污染评价及控制对策研究

以杭州市萧山区2008—2014年饮用水源地铁含量监测数据为分析对象,研究饮用水源地的铁含量时空分布并评价铁污染状况,结果表明,铁含量单次测值历年超标,超标倍数0.01~8.80,超标率16.7%~86.1%,7年间超标率呈现阶段性的螺旋式上升,铁污染日趋严重,到2014年有所减轻。通过对饮用水源地周边环境和污染源调查,结合文献资料,分析铁污染成因,提出防治对策:制定地表水体中铁的分类标准,完善废水的铁排放标准;建立跨行政区域的水环境管理机制,全面实施河长制;加强水土保持和酸雨控制,进行河流综合整治;加强饮用水源管理,扩建备用水源和另找水源。     

二溴羟基苯基荧光酮-OP胶束荧光熄灭法测定地面水中的微量铁(Ⅲ)

本文基于Ｆｅ（Ⅲ）二溴羟基苯基荧光酮（ＤＢＨ—ＰＦ）ＯＰ体系的荧光熄灭效应,提出一种测定微量铁（Ⅲ）的新荧光方法,在ｐＨ３８４８的缓冲介质范围内和ＯＰ存在下,Ｆｅ（Ⅲ）与ＤＢＨＰＦ形成１∶３的络合物,络合物的最大激发波长和发射波长分别是３６５ｎｍ和５６０ｎｍ。铁（Ⅲ）量在０１６～１８０μｇ／Ｌ范围内与△Ｆ成线性关系,检测限为０１６μｇ／Ｌ,方法用于地面水中微量铁的测定,结果满意。     

农村饮用井水铁锰含量升高调查与探讨

饮用水质量与人体健康密切相关.水中所含的铁、锰是人体必需的微量元素,但其含量过多或过少都会对人类的机体代谢产生不利影响.随着经济社会的高速发展,环境污染日益严重,水体污染事件不断出现.从区域地质环境、周边生产状况等方面分析了该地区地下水污染成因,并对饮用井水中铁、锰元素含量过高提出了简易的处理方法.     

桑色素-吐温-20胶束增溶分光光度法测定微量铁

本文对铁（Ⅲ）与桑色素（Ｍｏｒｉｎ）的显色反应进行了研究。在非离子表面活性剂吐温－２０存在下，于ｐＨ４．１的邻苯二甲酸氢钾缓冲溶液中，铁（Ⅲ）与桑色素形成稳定的黄色配合物，其组成比为Ｆｅ（Ⅲ）∶Ｍｏｒｉｎ＝１∶３，最大吸收波长为４１８ｎｍ，表观摩尔吸光系数为６．６９×１０４Ｌ／ｍｏｌ·ｃｍ，铁（Ⅲ）浓度在０～１６μｇ／２５ｍｌ范围内符合比耳定律。方法简便、快速，选择性好。应用于环境水样和植物中微量铁的测定，结果满意。     

邻菲啰啉直接光度法测定水中总铁

为了准确快速测定印染企业生产用水中的铁,探讨了Fe3＋在水浴和室温25℃时的还原反应试验,发现在这2个条件下Fe3＋均能被盐酸烃胺快速还原为Fe3＋,进而提出了测定水中总铁的新方法——邻菲哕啉直接光度法。并对该方法的检出限、显色络合物的稳定性、干扰及消除、盐酸用量、校准曲线、精密度和准确度进行了试验。检出限为0．03mg／L,显色络合物显色15min可稳定6个月,精密度RSD〈4．32％,加标回收率为95．3％～103％。通过地下水、地表水、工业废水和铁标准样品的比对实验表明,邻菲哕啉直接光度法与邻菲啰啉光度法（标准法）的测定结果无显著差异。     

石墨炉原子吸收光谱法测定氟化物中的铁

用石墨炉原子吸收光谱法测定氟化物中的铁，以Ｎｉ（ＮＯ３）２作基本改进剂测定，结果表明Ｎｉ（ＮＯ３）２对于氟化物中铁有强抗干扰、强增感效应。     

邻菲啰啉分光光度法测定海水中总铁

采用邻菲哕啉分光光度法测定海水中的总铁,方法在0mg／L～3．00mg／L范围内线性良好,检出限为0．03mg／L,相对标准偏差为3．0％,不同样品的加标回收率为95．2％～108％。     

邻菲哕啉分光光度法测定海水中总铁

采用邻菲哕啉分光光度法测定海水中的总铁,方法在0mg／L～3．00mg／L范围内线性良好,检出限为0．03mg／L,相对标准偏差为3．0％,不同样品的加标回收率为95．2％～108％。     

邻菲哕啉直接光度法测定水中总铁

为了准确快速测定印染企业生产用水中的铁,探讨了Fe3+在水浴和室温25℃时的还原反应试验,发现在这2个条件下Fle3+均能被盐酸烃胺快速还原为Fe2+,进而提出了测定水中总铁的新方法--邻菲哕啉直接光度法.并对该方法的检出限、显色络合物的稳定性、干扰及消除、盐酸用量、校准曲线、精密度和准确度进行了试验.检出限为0.03 mg/L,显色络合物显色15 min可稳定6个月,精密度.RSD＜4.32%,加标回收率为95.3%～103%.通过地下水、地表水、工业废水和铁标准样品的比对实验表明,邻菲哕啉直接光度法与邻菲哕啉光度法(标准法)的测定结果无显著差异.     

α,α''''--连吡啶固相萃取光度法测定饮用水中的铁

研究了α,a'-连吡啶与铁的显色反应,在pH为4.5的盐酸-六次甲基四氨缓冲介质中,α,a'-连吡啶与铁反应生成3:1稳定络合物,该络合物可被C18固相萃取小柱萃取,小柱上富集的络合物用乙醇洗脱后用光度法测定,体系λmax=520nm,ε=8.60×103L·mol-1·cm-1.铁含量在0-5 mg/L内符合比耳定律,方法用于饮用水中铁含量的测定,结果令人满意.     

农业生态与土壤环境中铁元素的关系

论述了铁元素的地球化学特征及其分布 ,与铁元素有关的主要作物分类、作物与铁元素的关系以及影响铁元素有效态的因素 ,铁肥的种类和施用方法与效果     

Chromium speciation in groundwater of a tannery polluted area of Chennai City, India

Chromium speciation in groundwater of a tannery polluted area was investigated for the distribution of chromium species and the influence of redox couples such as Fe(III)/Fe(II) and Mn(IV)/Mn(II). Speciation analysis was carried out by ammonium pyrolidinedithiocarbamate (APDC)–methylisobutylketone (MIBK) procedure. The groundwater samples were analyzed for Cr(III), Cr(VI), and Cr(III)-organic complexes. The APDC could not extract the Cr(III)-organic complexes, but HNO₃ digestion of the groundwater samples released the Cr(III)-organic complexes. The groundwater of the area is relatively oxidizing with redox potential (E _h) and dissolved oxygen (DO) ranged between 65 and 299 mV and 0.25 and 4.65 mg L^???1, respectively. The Fe(II) reduction of Cr(VI) was observed in some wells, but several wells that had Fe(II)/Cr(VI) concentrations more than the stoichiometric ratio (3:1) of the reduction reaction also had appreciable concentration of Cr(VI). This could partly be due to the oxidation of Fe(II) to Fe(III) by DO. It appears that the occurrence of Mn more than the Fe(II) concentration was also responsible for the presence of Cr(VI). Other reasons could be the Fe(II) complexation by organic ligands and the loss of reducing capacity of Fe(II) due to aquifer materials, but could not be established in this study.     

A novel wet-scrubbing process using Fe(VI) for simultaneous removal of SO2 and NO

The objective of this work was to develop a novel wet-scrubbing process using Fe(VI) for the simultaneous removal of gaseous NO and SO(2). The oxidation of SO(2) and NO with Fe(VI) was studied in aqueous solution at alkaline pH (9.0-11.0). A stoichiometric molar ratio for NO and SO(2) oxidation with Fe(VI) was determined to be nearly 3.0. Sulfate and nitrate was identified as final products by ion chromatography from the reaction at pH 9.0-11.0. The feasibility of simultaneous removal of multiple gas pollutants with the continuous feeding of ferrate in lab-scale was investigated from the view of industrial application. It was found that the removal efficiency of NO and SO(2) was enhanced with the increase of Fe(VI) concentration, more than 90% NO removal efficiency and 100% SO(2) removal efficiency were achieved by wet-scrubbing process using Fe(VI) at room temperature and ambient atmosphere. The results demonstrate that Fe(VI) could be an effective wet-scrubbing agent for the simultaneous removal of NO and SO(2).     

Iron and sulfur geochemistry in semi-arid mangrove soils (Ceará, Brazil) in relation to seasonal changes and shrimp farming effluents

Iron and sulfur are key elements in the biogeochemistry of estuarine soils, in which Fe and sulfate reduction (SR) pathways are important for organic matter decomposition. In the semi-arid coast of NE Brazil, mangroves are characterized by large seasonal variations in weather and the presence of numerous shrimp farms. The objective was to determine the impacts of shrimp farm effluents on iron and sulfur geochemistry in mangrove soils under the semi-arid climate of NE Brazil. A seasonal study was made of two mangrove forest soils (SF, a mangrove forest that directly receives wastewater from shrimp ponds and CS, a control site). Pyrite Fe, oxyhydroxides Fe, acid volatile sulfide, degree of pyritization (DOP), pH, Eh, total organic carbon (TOC) and total S were determined. There was a clear decrease in pyritic Fe and DOP in the SF soils, which may be related to the anaerobic oxidation of pyrite coupled with nitrate reduction, or to the dominance of denitrification over SR. Lower TOC contents in the SF site suggest that below ground decomposition increased in response to eutrophication. The seasonal variations led to important changes in the semi-arid mangrove soils. During the dry period, both soils experienced oxidizing conditions with remarkable loss of reduced and oxidized forms of Fe, which may have important environmental implications as Fe is biolimiting for marine primary production. The data show that both factors (seasonal weather variations and shrimp effluents) play important roles in the geochemical processes that occur in these soils and, thus, may affect their functioning and maintenance.     

Assessment of daily intake of trace elements by Kakrapar adult population through ingestion pathway

Concentration of trace elements such as Fe, Cu, Ni, and Zn were measured in cereals, pulses, vegetables, fish, meat, milk, egg, and water samples collected around Kakrapar, Gujarat, India. A wide variation of the trace element concentration was observed among all the dietary matrices. The concentration of Fe is comparatively more in all the dietary matrices. The concentrations of these elements are translated into intake rates through ingestion pathways. Daily intake (milligrams/day) of Fe, Cu, Ni, and Zn by adult population of Kakrapar, Gujarat were 16.5 ± 6.2, 3.3 ± 1.2, 1.8 ± 1.0, and 3.6 ± 1.3, respectively. Dietary sources of Fe, Cu, and Ni by Kakrapar adult population are comparable with RDA. In case of Zn, the daily dietary intake is comparatively lower than that of RDA.     

Using multivariate statistical methods to assess the groundwater quality in an arsenic-contaminated area of Southwestern Taiwan

Groundwater is a major water resource in Southwestern Taiwan; hence, long-term monitoring of water quality is essential. The study aims to assess the hydrochemical characteristics of water in the arsenic-contaminated aquifers of Choushui River alluvial fan and Chianan Plain, Taiwan using multivariate statistical methods, namely, factor analysis (FA), cluster analysis (CA), and discriminant analysis (DA). Factor analysis is applied to reveal the processes controlling the hydrochemistry of groundwater. Cluster analysis is applied to spatially categorize the collected water samples based on the water quality. Discriminant analysis is then applied to elucidate key parameters associated with the occurrence of elevated As concentration (>10 μg L(-1)) in groundwater. Major water types are characterized as Na-Ca-Cl and Na-Mg-Cl in the Choushui River alluvial fan and Chianan Plain, respectively. Inorganic species of arsenic (As), particularly As(III), prevail in these two groundwater catchments, and their levels are higher in the Chianan Plain than in the Choushui River alluvial fan. Through FA, three factors, namely, the degree of salination, As reduction, and iron (Fe) reduction, are determined and denoted irrespective of some differences between the factorial compositions. Spatial distribution patterns of factors As reduction and Fe reduction imply that the redox zonation is delineated by As- and Fe-dominance zones separately. The results of CA demonstrate that three main groups can be properly explained by the factors extracted via FA. Three- (Fe(2+), Fe(3+), and NH (4) (+) ) and four-parameters (Fe(2+), Fe(3+), NH (4) (+) , and Ca(2+)) derived from discriminant analysis for Choushui River alluvial fan and Chianan Plain are elucidated as key parameters affecting the distribution of As-contained groundwater. The analytical results indicate that the reductive dissolution of Fe minerals is prerequisite for the mobilization of As, whereas the shift of redox condition from Fe- to As-reducing leads to the accumulation of dissolved As in this area.     

Nitrate and ammonium ions removal from groundwater by a hybrid system of zero-valent iron combined with adsorbents

Nitrate (NO(3)(-)) is a commonly found contaminant in groundwater and surface water. It has created a major water quality problem worldwide. The laboratory batch experiments were conducted to investigate the feasibility of HCl-treated zero-valent iron (Fe(0)) combined with different adsorbents as hybrid systems for simultaneous removal of nitrate (NO(3)(-)) and ammonium (NH(4)(+)) ions from aqueous solution. The maximum NO(3)(-) removal in combined Fe(0)-granular activated carbon (GAC), Fe(0)-filtralite and Fe(0)-sepiolite systems was 86, 96 and 99%, respectively, at 45 °C for 24 h reaction time. The NO(3)(-) removal rate increased with the increase in initial NO(3)(-) concentration. The NO(3)(-) removal efficiency by hybrid systems was in the order of sepiolite > filtralite > GAC. The NH(4)(+) produced during the denitrification process by Fe(0) was successfully removed by the adsorbents, with the removal efficiency in the order of GAC > sepiolite > filtralite. Results of the present study suggest that the use of a hybrid system could be a promising technology for achieving simultaneous removal of NO(3)(-) and NH(4)(+) ions from aqueous solution.     

化学发光法测定环境水体中的亚硝酸盐氮

利用鲁米诺-铁氰化钾-尿酸化学发光体系,在酸性介质中,NO-2将亚铁氰化钾氧化为铁氰化钾,建立了一种间接测定痕量亚硝酸盐的新方法。     

Heavy Metals Monitoring using Bivalves from Mediterranean Sea and Red Sea

The concentrations of heavy metals (Cd, Co, Cu, Fe, Mn, Ni, Pd and Zn) were measured in the Bivalves (Modiolus auriculatus and Donax trunculus) collected from the Egyptian coasts of Mediterranean Sea and Brachiodonates sp. from the Egyptian coasts of Red Sea. The average concentrations of the heavy metals analyzed exhibited the following decreasing order: Fe > Zn > Cu > Mn > Ni > Co > Pb > Cd for both Mediterranean Sea and Red Sea. The analyses of Cd, Co, Ni, Pb, and Zn showed higher average concentrations for samples collected from Red Sea than that collected from Mediterranean Sea, while Fe, Cu and Mn showed the reverse results. Fe was used as a normalizing agent for all studied metals and exhibited presence of two locations from each of Mediterranean Sea and Red Sea have anthropogenic inputs of heavy metals. These results suggest that the coastal area in both Mediterranean Sea and Red Sea of Egypt might be considered relatively unpolluted with heavy metal.