用氯和氢氧同位素揭示洋戴河平原地下水的形成演化规律

通过分析地表水和地下水中氯离子浓度和δD、δ¹⁸O值的空间分布特征,揭示了秦皇岛洋戴河平原地下水的形成演化规律.结果发现,洋戴河平原地表河水来源于中上游水库水和大气降水的混合,且河水沿程受到δD、δ¹⁸O值、氯离子浓度更低的支流或灌渠水补给,从而使δD、δ¹⁸O值、氯离子浓度呈现沿程逐渐降低的现象.山前丘陵区地下水主要接受大气降水的直接补给,洪积扇及山麓地带地下水受到了一定的蒸发作用影响,除了接受丘陵区地下水的侧向补给外,洋河附近地下水还受到洋河水库水的混合.研究区西部咸水带的地下水由上游地下水和大泥河地热咸水混合而成,地热咸水的混合比率约为13%,而东部咸水带的地下水由上游地下水、本地污水和地热咸水混合而成,地热咸水的混合比率不超过9%.在海水入侵区,地下水主要由本区地下淡水和海水(海水混合比率不超过10%)混合而成,并且受到了不同程度的地表水或农田灌溉水的补给,其中,浦河一带是地表水或灌溉水补给较为明显的地段.     

Identification of key factors governing chemistry in groundwater near the water course recharged by reclaimed water at Miyun County, Northern China

Reclaimed water was successfully used to recover the dry Chaobai River in Northern China, but groundwater may be polluted. To ensure groundwater protection, it is therefore critical to identify the governing factors of groundwater chemistry. Samples of reclaimed water, river and groundwater were collected monthly at Chaobai River from January to September in 2010. Fifteen water parameters were analyzed. Two kinds of reclaimed water were different in type (Na-Ca-Mg-Cl-HCO3 or Na-Ca-Cl-HCO3 ) and concentration of nitrogen. The ionic concentration and type in river were similar to reclaimed water. Some shallow wells near the river bed had the same type (Na-Ca-Mg-Cl-HCO3 ) and high concentration as reclaimed water, but others were consistent with the deep wells (Ca-Mg-HCO3 ). Using cluster analysis, the 9 months were divided into two periods (dry and wet seasons), and all samples were grouped into several spatial clusters, indicating different controlling mechanisms. Principal component analysis and conventional ionic plots showed that calcium, magnesium and bicarbonate were controlled by water-rock interaction in all deep and some shallow wells. This included the dissolution of calcite and carbonate weathering. Sodium, potassium, chloride and sulfate in river and some shallow wells recharged by river were governed by evaporation crystallization and mixing of reclaimed water. But groundwater chemistry was not controlled by precipitation. During the infiltration of reclaimed water, cation exchange took place between (sodium, potassium) and (calcium, magnesium). Nitrification and denitrification both happened in most shallow groundwater, but only denitrification in deep groundwater.     

水体中总氮检测的方法研究

使用碱性过硫酸钾氧化紫外分光光度法(GB 11894—1989)测定水中的总氮时,在严格按该方法分析步骤操作的情况下,依然会出现空白值偏高、检测结果不准确等问题。本文对水中总氮检测过程中的影响因素进行了总结、分析,对需要重点注意的环节进行了探讨,找出了问题的原因并提出了解决方法。     

壳聚糖三元接枝共聚物的合成及其阻垢性能

以壳聚糖(CTS)、衣康酸(IA)和马来酸酐(MA)为原料,以醋酸为溶剂、(NH_4)_2S_2O_8为引发剂,合成了CTS-IA-MA三元接枝共聚物。聚合反应的最佳条件为:反应温度90℃,n(CTS):n(IA):n(MA)=1:1.5:1.0,引发剂质量分数0.35%,反应时间5 h。通过傅立叶变换红外光谱(FTIR)表征,所得产物为CTS-IA-MA接枝共聚物。三元接枝共聚物质量浓度为50 mg/L、水样pH为中性或弱酸性时三元接枝共聚物对CaCO_3的阻垢效果较好。     

Hydrogeochemical Indicators of Groundwater Flow Systems in the Yangwu River Alluvial Fan,Xinzhou Basin,Shanxi, China

Based on analysis of groundwater hydrochemical and isotopic indicators, this article aims to identify the groundwater flow systems in the Yangwu River alluvial fan, in the Xinzhou Basin, China. Groundwater δ²H and δ¹⁸O values indicate that the origin of groundwater is mainly from precipitation, with local evaporative influence. d-excess values lower than 10% in most groundwaters suggest a cold climate during recharge in the area. Major ion chemistry, including rCa/rMg and rNa/rCl ratios, show that groundwater salinization is probably dominated by water–rock interaction (e.g., silicate mineral weathering, dissolution of calcite and dolomite and cation exchange) in the Yangwu River alluvial fan, and locally by intensive evapotranspiration in the Hutuo River valley. Cl and Sr concentrations follow an increasing trend in shallow groundwater affected by evaporation, and a decreasing trend in deep groundwater. ⁸⁷Sr/⁸⁶Sr ratios reflect the variety of lithologies encountered during throughflow. The groundwater flow systems (GFS) of the Yangwu River alluvial fan include local and intermediate flow systems. Hydrogeochemical modeling results, simulated using PHREEQC, reveal water–rock interaction processes along different flow paths. This modeling method is more effective for characterizing flow paths in the intermediate system than in the local system. Artificial exploitation on groundwater in the alluvial fan enhances mixing between different groundwater flow systems.     

Impact of human activities on coastal groundwater pollution in the Yang-Dai River plain,northern China

Environmental Science and Pollution Research - Overexploitation of groundwater has resulted in seawater intrusion in many semiarid and arid coastal areas. This study illustrates the origin of...     

北京北部水系沉积物中重金属的研究

主要研究了北京市北部水系沉积物中重金属(As、Hg、Cd、Cr、Cu、Mn、Ni、Pb、Ti和Zn)含量和来源.在潮白河及密云水库流域采集了17个沉积物样品,温榆河流域采集了5个样品,重金属含量As和Hg采用原子荧光光谱法测定,Cd、Cr、Cu、Mn、Ni、Pb、Ti和Zn含量用电感耦合等离子发射光谱法测定.研究结果表明,沉积物中重金属元素没有出现明显的富集状况,只有Hg、Cd、Cr和Zn在一些采样点有较高的富集.相关性分析表明Hg、Cd、Zn和Cu互相之间呈显著正相关(r0.06;p0.01),而Hg与Cr、Mn、Ni、Pb和Ti没有明显的相关性.通过主成分分析研究重金属的来源,发现前3个主成分贡献率分别为38%、23%和17%.因此,Hg、Cd、Zn和Cu作为第一主成分被认为与人类活动的工矿业开采有关,第二主成分As和Mn与人类活动的农业生产和生活污水排放有关,第三主成分Cr、Ni和Ti与岩石风化和土壤侵蚀有关.     

Numerical modeling of changes in groundwater storage and nitrate load in the unconfined aquifer near a river receiving reclaimed water

Environmental Science and Pollution Research - Reclaimed water (RW) has been widely used as an alternative water resource to recharge rivers in mega-city Beijing. At the same time, the RW also...     

氮、硫掺杂TiO2-壳聚糖微球的制备及其可见光催化性能

采用溶胶-凝胶法制备N、S掺杂TiO2光催化剂,将其与壳聚糖(CS)溶液共混交联,制取N、S掺杂的TiO2-CS(NSTC)微球光催化剂.通过扫描电子显微镜、X射线衍射技术对NSTC微球的形态和晶型结构进行了表征.研究表明,在焙烧温度为450℃、n(N):n(S):n(Ti)=3:3:1的条件下,制备的NSTC微球的可见光催化降解性能最佳.用在最佳条件下制得的NSTC微球在可见光下催化处理pH为3、质量浓度为20 mg/L的甲基橙溶液,反应240 min,甲基橙降解率可达94.1%.NSTC微球重复进行6次可见光催化降解实验,甲基橙降解率仍可达90.0%.     

Assessment and sources of heavy metals in surface sediments of Miyun Reservoir, Beijing

Heavy metals concentrations in surface sediments from Miyun Reservoir were determined to evaluate the pollution and identify the sources. The average content of metals in sediments from Miyun Reservoir followed the order Al>Fe>Ti>Mn>V>Zn>Cr>Ni>Cu>Pb>As>Cd>Hg, and the most mean values were lower than the globe average shale. Heavy metals concentrations at the inflow area of Baihe were higher than those at the inflow area of Chaohe. Heavy metals pollution assessment was carried out by factor enrichment (EF), geoaccumulation index (I _geo), and potential ecological risk (RI). The EF values for all heavy metals except Hg, Cd, and Cr at several sites were lower than 3, suggesting low anthropogenic impact on the metals level. The I _geo values of Pb indicated that half of the sites were unpolluted to moderately polluted and mainly located in the Baihe area of the reservoir. The RI showed that heavy metals of Miyun Reservoir were low potential risk, however, Hg approached or belonged to moderate ecological risk at sites of M5, M7, and M13. Correlation analysis and principal component suggested that Ni, Cu, V, Zn, Mn, Cr, Ti, and Pb were derived from soil erosion in upper reaches of the reservoir, while Fe, Cd, Hg, As, and partial Pb originated from anthropogenic sources, particularly industrial mining and gold tailings.