双电极法现场快速检测地下水和湖水中碳酸氢根和碳酸根

地下水和湖水中碳酸氢根( HCO-3)和碳酸根( CO2-3)含量是地球化学碳行为和碳循环的重要表征,但两种离子的浓度易受环境影响而改变,因此,地下水和湖水中HCO-3和CO2-3真实含量的测定一直是个难题。实验利用CO2的水解平衡,通过pH电极和二氧化碳电极联用,建立了HCO-3和CO2-3现场快速测定的新方法,解决了地下水和湖水中HCO-3和CO2-3真实含量的测定难题。研究结果表明,在pH=4.8±0.1的底液中, HCO-3和CO2-3的线性范围分别为0.027~570 mg/L和1.25×10-8~39.7 mg/L。共存的金属离子、强酸阴离子(K+、Na+、Mg2+、Cl-、SO2-4,100 mg/L)、弱酸阴离子和弱酸(HSO-3、NO-2、HOAc,50 mg/L)对测定干扰小于5%。实际水样加标实验回收率在95.2%~99.2%之间,相对标准偏差为2.6%~3.7%。与酸碱滴定法进行对比,本方法的准确性良好。但方法受温度影响,因此标准溶液与样品应在同一温度下测量。总体而言,双电极法灵敏、快速、经济且电极携带方便、操作简单、对环境要求不高,十分适合现场和室内一般自然水体的快速检测。本方法已成功应用于青海省地下水和青海湖湖水中HCO-3和CO2-3的现场测定。实验表明,海东地区地下水样品pH在6.4~7.4之间,HCO-3含量为234~4096 mg/L,CO2-3含量为0.16~1.89 mg/L；青海湖湖水样品pH≈8.7,HCO-3含量范围在1.36~1.86 g/L,CO2-3含量在32.3~43.9 mg/L,与文献结果吻合。     

云母石英片岩斜坡弯曲倾倒变形的理论分析

片岩斜坡中弯曲倾倒变形是通过密集的片理上逐层剪切位移实现的。文中给出了瞬时变形终止时σ1与片理面法线夹角γ的理论公式。瞬时变形结束后, 由于片理面上剪应力作用, 将继续发生剪切蠕变。本文给出了γ随着时间t变化的公式。最后本文讨论了地下水压力在倾倒变形中的作用, 并在理论公式中考虑了这一因素。     

杭州市郊来龙山滑坡的治理与监测

滑坡是一种重大的地质灾害,本文结合杭州市郊来龙山的滑坡工程,具体分析了滑坡的成因、稳定计算和最终采取的治理措施,通过监测的具体内容和结果进行分析,表明治理效果比较好,为以后该地区的滑坡治理与加固提供相关参照。     

Monitoring and Evolution of the Pollution by Volatile Organic Compounds (Vocs) in the Groundwaters of The Najerilla River Basin (Spain)

VOCs were detected and identified in the water of several wells in the area of Nájera (La Rioja). The past uncontrolled spills from an important painting and varnishing industry and from other smaller ones devoted to the manufacture of furniture and varnishing activities were the sources of the VOCs plume detected in this aquifer. This article shows the results obtained in the monitoring and assessment of the pollution at 18 sampling points for more than a year. It has allowed us to study the evolution of the different pollutants and the influence of a remediation process applied by the company in the main pollution source. The analytical method is based on headspace-solid-phase microextraction (SPME) using a 75-μm carboxen-polydimethylsiloxane fibre. Quantification was carried out by gas chromatography with flame ionization detection. This method has allowed us to determine the 13 VOCs identified in the polluted underground samples providing good sensitivity (LOD between 0.1 and 6.0 ng/mL) and reproducibility (r.s.d. less than 10%).     

Determination of benzotrifluoride derivative compounds in groundwater

Two simple analytical methods for the simultaneous determination and quantification of benzotrifluoride and eight chlorinated, amino and nitro benzotrifluoride derivatives in groundwater are proposed. Benzotrifluoride, 4-chlorobenzotrifluoride, 2,4-dichlorobenzotrifluoride and 3,4-dichlorobenzotrifluoride, were extracted by Purge-and-Trap on the basis of their volatile properties, while 3-aminobenzotrifluoride, 4-nitrobenzotrifluoride, 3-amino-4-chlorobenzotrifluoride, 3-nitro-4-chlorobenzotrifluoride and 4-chloro-3,5-dinitrobenzotrifluoride extractions were done with an automated SPE system. The analytical separations and detections were performed with two different GC systems, both equipped with single quadrupole mass spectrometer as detector. The LOD ranges for the two methods were 0.002–0.005 μg L⁻¹ and 0.01–0.07 μg L⁻¹, respectively. Both extraction methods were developed using spiked Milli-Q water and were then demonstrated with groundwater samples collected during autumn 2008. The areas of groundwater collection were polluted due to an episode of improper industrial soil disposal and consequent leakage of aliphatic and aromatic, fluorinated chemicals into the groundwater. This work eventually revealed the presence of several benzotrifluoride compounds most of them, like dichloro- and amino-derivatives, never been reported as environmental contaminants.     

Trace-level analysis of organic contaminants in drinking waters and groundwaters

We expect drinking water and groundwater samples to be contaminated very little, so they are subject to trace-level analysis. Due to the very low levels of contamination, this sort of analysis requires not only powerful analytical technologies to reach limits around the ng/L level, but also quality-control parameters (e.g., blank and spike samples) to monitor potential contamination or losses during sample treatment. Based on a literature review and laboratory experience, we discuss the problems linked to the difficulties of calculating limits of detection, distinguishing instrumental from methodological limits and preventing false-positive results in cases of sample contamination, or false-negative results in cases of compound losses. When possible, we suggest solutions to compensate for, or to prevent, these problems.     

Quantitative determination of toluene,ethylbenzene, and xylene degradation products in contaminated groundwater by solid-phase extraction and in-vial derivatization

Benzylsuccinic acid (BSA) and methylbenzylsuccinic acids (mBSAs) are unambiguous indicators of anaerobic toluene and ethylbenzene/xylene degradation, and so the determination of these compounds in landfill leachates and contaminated groundwater is highly relevant. Samples were diluted to <0.8?mS?cm^?1 in order to reduce their ionic strength, and subsequently extracted through strong anion exchange disks, followed by simultaneous in-vial elution and methylation. A detection limit of 0.1?µg?L^?1 was obtained for 100?mL samples. Using this method, 19.3?µg?L^?1 of BSA was measured in a landfill leachate, and low µg?L^?1 levels of all of the mBSAs were measured in gasoline-contaminated groundwater. The results were compared with the findings of BSAs at 16 other contaminated sites, and BSAs as indicators of biodegradation were evaluated. The estimation of biodegradation rates based on parent hydrocarbons and BSA concentrations or ratios is questionable. However, the degradation products serve as good qualitative in situ indicators for anaerobic biodegradation in contaminated groundwater.     

Isotopes in groundwater as indicators of climate changes

Isotopes of the water molecule (δ¹⁸O and δ²H) are a well-used tool for investigating groundwater origin and history (i.e. tracing the recharge conditions over time, processes occurring during infiltration of rainwater towards aquifers and those involved in the water-rock interaction, and mixing of different waters).This review covers several large European aquifers (Portugal, France, UK, Switzerland, Germany, Hungary, and Poland), which were investigated in terms of their recharge conditions, and the story of the groundwater at a large scale, involving recent, Holocene and Pleistocene components and their eventual mixing.     

河道施工降水引起的邻近建筑物沉降分析

通过对地基进行沉降计算, 对基础沉降进行实际观测, 将计算数值与观测数值进行对比分析. 结果表明: 施工降水是导致邻近建筑物沉降、开裂的原因; 邻近建筑物地基沉降的规律是离 施工降水现场由近至远逐渐减小; 采用设止水帷幕和回灌井联合控制地下水位下降是一种有 效的措施.     

Temporal 18O and deuterium variations in hydrologic components of a small watershed during a typhoon event

The differences between δ¹⁸O and δ²H in throughfall and open rainfall were studied for a selected typhoon event in a watershed within the Taihu Lake drainage basin, eastern China. In this event, the isotopic composition of precipitation exhibited a strong temporal variation. Comparison results show that an isotopic composition difference existed not only between gross rainfall and average incremental rainfall, but also between different calculation methods used to derive average. The differences between incremental precipitation and throughfall isotopic composition were observed in this study. Considering the temporal variation in rainfall and throughfall during this typhoon event, the incremental value can have an effect on hydrograph separation more accurately in evaluating the importance of ‘new’ water. In addition, isotopic fluctuations of surface water and groundwater differed from those of rainfall and throughfall throughout the event.