浅层地下水遥感找水模型研究

采用遥感-数据-模型相融合的方法,建立了浅层地下水推断模型。该模型克服了以往勘察方法费用高、效率低、周期长的不足,从未知出发,由面到点,层次分明,衔接有序。经实地考察验证,该模型精度较准,效率较高,具有实用性,不仅可以宏观、快速、高效地确定浅层地下水的分布和范围,而且可以降低费用,缩短周期,起到事半功倍的作用,为进一步找水工程的布置提供依据,确定找水方向,避免找水的盲目性。     

重庆市加油站周边浅层地下水中石油烃污染调查与特征分析

为了解加油站运营对周边浅层地下水环境质量的影响,随机选择了12个正常运营20年以上的加油站,在加油站上游和下游共布设了27口地下水监测井,对地下水中石油烃、苯系物、萘、1,2-二氯乙烷和甲基叔丁基醚开展了水质监测。结果表明,石油烃在地下水中的检出率较高,为96.3%,检出浓度为4.2~544.7μg/L,检出组分主要为柴油烃中的C26和C20,检出率分别达到了88.9%和77.8%;汽油烃的有效组分C6~C9未检出,作为汽油添加剂的1,2-二氯乙烷和甲基叔丁基醚在地下水中存在,检出率分别为96.3%和22.2%,检出浓度分别为1.7~30.9μg/L和3.8~30.9μg/L。其中,11.1%的监测井中甲基叔丁基醚浓度超过了EPA推荐的饮用水安全的浓度限值(20μg/L),3.7%的监测井中1,2-二氯乙烷浓度超过了《地表水环境质量标准》(GB 3838-2002)中"集中式生活饮用水地表水源地特定项目标准限值"规定的30μg/L。总体而言,石油烃、苯系物、1,2-二氯乙烷和甲基叔丁基醚的含量远低于油品渗(泄)漏导致的污染水平。     

晋南铬渣堆场主要植物重金属富集特征

为筛选适合山西当地气候与土壤条件的重金属耐性植物,于山西某铬渣堆场采集草本植物及表层土壤(0～20cm)样品,从中选取6种主要植物品种,测定植物地上部分、根部及土壤中4种重金属(Cu、Zn、Pb和Cr)含量,分析6种植物对重金属的富集特征。结果表明:铬渣堆场土壤Cr污染严重,平均质量浓度为2 207mg/kg,是山西省土壤背景值(58mg/kg)的38.1倍,是《土壤环境质量农用地土壤污染风险管控标准(试行)》(GB 15618—2018)规定风险筛选值(250mg/kg)的8.8倍。选取的6种植物中,狼尾草(Pennisetum alopecuroides (L.)Spreng.)、羊草(Leymus chinensis (Trin.)Tzvel.)和狗牙根(Cynodon dactylon (L.)Pers.)等植物体内Cr含量相对较高,表现出较强的Cr吸收能力。根据植物对重金属的吸收机制,羊草、狼尾草和狗牙根属于根部囤积性植物;狗尾草(Setaria viridis (L.)Beauv.)、虎尾草(Chloris virgate Sw.)和牛筋草(Eleusine indica ...     

黑麦草修复重金属污染土壤与废水及富集植物的微生物降解

为了研究黑麦草(Lolium perenne)修复复合重金属污染土壤与废水的综合利用效应,探索微生物对富集重金属黑麦草的降解效果,以复合重金属污染的土壤与废水为修复对象,利用黑麦草对土壤和废水进行修复,并考察了黑麦草的重金属含量、富集量、富集系数和转移系数。采用8种微生物对富集重金属黑麦草进行降解,考察黑麦草的失重率,黑麦草纤维素、半纤维素和木质素的变化情况以及重金属的浸出效果。结果表明:黑麦草对重金属污染的土壤与水体均具有较好的修复效果;在土壤修复阶段,黑麦草对U的富集系数最大,达到7.43;而对Cd的富集系数为2.61,对Pb和Sr的修复效果不明显;在废水修复阶段,黑麦草对U的富集量达到1 213.70 mg·kg-1DW,U、Cr、Sr、Co的富集系数和转移系数均大于1,其中U的富集系数达到11.24。另外,里氏木霉(Trichoderma ressei)和黄孢原毛平革菌(Phanerochaete chrysosporium)对富集黑麦草的总降解率达到60%以上;里氏木霉(Trichoderma ressei)、枯草芽孢杆菌(Bacillus subtilis)和地衣芽孢杆菌(Bacillus lincheniformis)对重金属的平均浸出率分别达到87.19%、90.58%和90.33%。在重金属污染的土壤和水体中,通过对黑麦草的循环使用,可以提高黑麦草的综合利用效率,有效减少富集生物质的产生;同时微生物对富集生物质有较好的降解能力。研究为重金属富集生物质微生物处置以及重金属回收技术奠定基础。     

某矿区土壤和地下水重金属污染调查与评价

为了解湘南某矿区土壤和地下水重金属污染状况,对该矿区东河流域附近重金属污染源进行了调查,同时,对地下水和土壤样品进行了采样分析,结果表明：（1）该矿区东河流域附近的主要污染源有18个,其中有色金属选厂、尾矿库、采矿场和冶炼厂是排放重金属较多的污染源;（2）20个采样点中土壤重金属Pb、Cd、Zn、As和Hg大部分超过国家土壤环境质量标准（GB15618-1995）,综合污染指数P综〉1,该矿区主要的重金属污染元素为Cd、As和Hg,且土壤中Cd、Zn和As的含量两两之间存在着极显著的正线性相关关系;（3）重金属元素在土壤中的纵向迁移不明显,该矿区附近20个采样点的地下水并未受到污染,综合污染指数P综〈1。20个采样点地下水Pb、Cd、Zn、As、Hg浓度均能达到地下水质量标准（GB／T14848．9）中的Ⅲ类标准。     

杭州市大气降尘重金属污染特征及来源研究

于2006年6月至2009年6月期间,在杭州市主城区7个采样点对大气降尘进行采集,并对10种重金属元素含量进行了分析。结果表明:重金属元素Cu、Cd、Mn、Ni、Pb、Zn、Co、Al、Fe、Mo质量浓度分别为223.6、15.6、741.1、27.8、363.7、1 820.4、7.0、8 982.4、21 149.0、13.4mg/kg;各功能区差异较大,半山(工业区)Fe、Mn、Pb、Zn浓度较高,江城立交(交通枢纽)Cu、Cd浓度较高。富集因子评价结果表明,Cd、Mo、Pb、Zn、Cu富集程度较高,受到不同程度人为污染。主因子分析结果显示,Mn、Fe可能来自钢铁冶炼及机械制造;Cu、Cd可能来自交通源;Zn、Mo可能来自相关的冶炼加工及合金工业;Ni、Co可能由煤和石油等化石燃料燃烧排放;Pb来自工业排放;Al主要来自地壳。     

堆肥污泥重金属在黄土中的淋滤特征

堆肥污泥中所含重金属是污泥堆肥土地利用最大的障碍,实验选用北方贫瘠的黄土作为供试样品,通过室内土柱淋滤实验,对堆肥污泥重金属在黄土中的淋滤特征进行了研究。结果显示,在0～40 cm的浅层淋滤层,各种重金属在黄土中的纵向迁移能力为:Pb>Zn>Ni>Cu,而在50～55 cm的深层淋滤层,Cd在黄土中的迁移能力相对其他4种重金属是比较强的;各种重金属在50～60 cm深层淋滤层中会出现二次富集,出现明显富集层。研究揭示了堆肥污泥重金属在黄土中的迁移特征,为有效控制和消除堆肥污泥土地利用中重金属的污染研究提供了理论依据。     

Hydraulic constraints on the performance of a groundwater denitrification wall for nitrate removal from shallow groundwater

Denitrification walls are a practical approach for decreasing non-point source pollution of surface waters. They are constructed by digging a trench perpendicular to groundwater flow and mixing the aquifer material with organic matter, such as sawdust, which acts as a carbon source to stimulate denitrification. For efficient functioning, walls need to be permeable to groundwater flow. We examined the functioning of a denitrification wall constructed in an aquifer consisting of coarse sands. Wells were monitored for changes in nitrate concentration as groundwater passed through the wall and soil samples were taken to measure microbial parameters inside the wall. Nitrate concentrations upstream of the wall ranged from 21 to 39 g N m(-3), in the wall from 0 to 2 g N m(-3) and downstream from 19 to 44 g N m(-3). An initial groundwater flow investigation using a salt tracer dilution technique showed that the flow through the wall was less than 4% of the flow occurring in the aquifer. Natural gradient tracer tests using bromide and Rhodamine-WT confirmed groundwater bypass under the wall. Hydraulic conductivity of 0.48 m day(-1) was measured inside the wall, whereas the surrounding aquifer had a hydraulic conductivity of 65.4 m day(-1). This indicated that during construction of the wall, hydraulic conductivity of the aquifer had been greatly reduced, so that most of the groundwater flowed under rather than through the wall. Denitrification rates measured in the center of the wall ranged from 0.020 to 0.13 g N m(-3) day(-1), which did not account for the rates of nitrate removal (0.16-0.29 g N m(-3) day(-1)) calculated from monitoring of groundwater nitrate concentrations. This suggested that the rate of denitrification was greater at the upstream face of the wall than in its center where it was limited by low nitrate concentrations. While denitrification walls can be an inexpensive tool for removing nitrate from groundwater, they may not be suitable in aquifers with coarse textured subsoils where simple inexpensive construction techniques result in major decreases in hydraulic conductivity.     

三氯甲烷在浅层地下水中的赋存特征及迁移淋溶性研究

伴随着世界各地工业进程的不断加速,地下水有机污染呈现愈加严重的态势.对滹沱河冲积平原390组浅层地下水样品进行测试、分析和研究.结果表明:(1)研究区浅层地下水三氯甲烷检出率高达15.64％;(2)三氯甲烷集中检出区域均位于工业集散地及排污河流沿线;(3)三氯甲烷的检出点分布同研究区包气带岩性特征有较好的一致性;(4)...     

Temporal variability of groundwater chemistry in shallow and deep aquifers of Araihazar, Bangladesh

Samples were collected every 2-4 weeks from a set of 37 monitoring wells over a period of 2-3 years in Araihazar, Bangladesh, to evaluate the temporal variability of groundwater composition for As and other constituents. The monitoring wells are grouped in 6 nests and span the 5-91 m depth range. Concentrations of As, Ca, Fe, K, Mg, Mn, Na, P, and S were measured by high-resolution ICPMS with a precision of 5% or better; concentrations of Cl were measured by ion chromatography. In shallow wells <30 m deep, As and P concentrations generally varied by <30%, whereas concentrations of the major ions (Na, K, Mg, Ca and Cl) and the redox-sensitive elements (Fe, Mn, and S) varied over time by up to +/-90%. In wells tapping the deeper aquifers >30 m often below clay layers concentrations of groundwater As were much lower and varied by <10%. The concentrations of major cations also varied by <10% in these deep aquifers. In contrast, the concentration of redox-sensitive constituents Fe, S, and Mn in deep aquifers varied by up to 97% over time. Thus, strong decoupling between variations in As and Fe concentrations is evident in groundwaters from shallow and deep aquifers. Comparison of the time series data with groundwater ages determined by (3)H/(3)He and (14)C dating shows that large seasonal or inter-annual variations in major cation and chloride concentrations are restricted to shallow aquifers and groundwater recharged <5 years ago. There is no corresponding change in As concentrations despite having significant variations of redox sensitive constituents in these very young waters. This is attributed to chemical buffering due to rapid equilibrium between solute and solid As. At two sites where the As content of groundwater in existing shallow wells averages 102 microg/L (range: <5 to 648 microg/L; n=118) and 272 microg/L (range: 10 to 485 microg/L; n=65), respectively, a systematic long-term decline in As concentrations lends support to the notion that flushing may slowly deplete an aquifer of As. Shallow aquifer water with >5 years (3)H/(3)He age show a constant As:P molar ratio of 9.6 over time, suggesting common mechanisms of mobilization.     

A method for the in-situ determination of dissolved methane in groundwater in shallow aquifers

Dissolved methane in groundwater has potential for use as a tracer of waste contamination in aquifers, and is itself a contaminant of concern because of potential explosion hazards following pumping of groundwater to the surface. A technique is described and evaluated for in-situ determination of the variation in concentration of dissolved methane with depth in shallow aquifers. The technique uses diffusion cells (small diameter teflon tubes) buried in boreholes and connected to the surface by small diameter nylon access tubes. A stream of gas is passed through the cells until a steady flux of methane is obtained. The steady state flux can then be related to concentration or partial pressure of methane in groundwater in contact with the cell, from prior laboratory calibration. Some temperature compensation is required.Two strings of cells with nylon access tubes for gas purging have been emplaced in permeable grout within boreholes drilled in sand a aquifer. The depth-related concentrations of dissolved methane found using these cells compare reasonably well with less precise data obtained by sampling of conventional boreholes situated adjacent to each string of cells.     

Colloid characterization and in situ release in shallow groundwater under different hydrogeology conditions

Environmental Science and Pollution Research - Changes to groundwater hydrodynamics and chemistry can lead to colloid release that can have a major impact on the groundwater environment. To analyze...     

Influence of soil inorganic amendments on heavy metal accumulation by leafy vegetables

Environmental Science and Pollution Research - The present study aims to assess the effect of four inorganic soil amendments, such as lime (CaCO3), red mud consisting of 75% hematite (Fe2O3),...     

2009—2014年河北平原浅层地下水硝态氮特征及其来源

依据2009—2014年河北平原浅层地下水硝态氮(NO-3-N)监测数据,分析河北平原浅层地下水NO-3-N污染状况,并利用氮氧双同位素的方法对地下水中硝态氮的来源进行了示踪。结果表明,2009—2014年河北平原浅层地下水硝态氮平均含量变化范围在0.00~121.50 mg/L之间,总平均值为(18.72±1.55)mg/L,超过美国饮用水标准(10 mg/L)的0.872倍;三个子平原区的SO2-4/Cl-差异较大而NO-3/Cl-值相差不大,说明地下水中的氯化物、硝态氮以及硫酸盐有着不同的来源。东部滨海平原区NO-3-N含量最大,为31.55 mg/L,已超出美国饮用水标准2.155倍;其次为山前平原区,为16.45 mg/L,超出美国饮用水标准0.645倍;中部平原区的含量最低,仅为4.19 mg/L,未超标。根据同位素的数值进行分析,揭示了东部滨海平原区以及中部平原区的硝态氮来源主要为化粪池废弃物,山前平原区的硝态氮主要来自化肥中的NH+4。