2004～2009年我国典型陆地生态系统地下水硝态氮评价

利用中国生态系统研究网络（CERN）2004～2009年31个典型陆地生态系统38个浅层地下水井硝态氮（NO 3--N）的监测数据,评价我国典型陆地生态系统地下水NO 3--N污染状况.结果表明,农田（4.85 mg.L-1±0.42 mg.L-1）、绿洲农田（3.72mg.L-1±0.42 mg.L-1）、城市（3....     

A novel colorimetric method for field arsenic speciation analysis

Accurate on-site determination of arsenic (As) concentration as well as its speciation presents a great environmental challenge especially to developing countries. To meet the need of routine field monitoring, we developed a rapid colorimetric method with a wide dynamic detection range and high precision. The novel application of KMnO₄ and CH₄N₂S as effective As(Ⅲ) oxidant and As(V) reductant, respectively, in the formation of molybdenum blue complexes enabled the differentiation of As(Ⅲ) and As(V). The detection limit of the method was 8 μg/L with a linear range (R² = 0.998) of four orders of magnitude in total As concentrations. The As speciation in groundwater samples determined with the colorimetric method in the field were consistent with the results using the high performance liquid chromatography atomic fluorescence spectrometry, as evidenced by a linear correlation in paired analysis with a slope of 0.9990-0.9997 (p < 0.0001, n = 28). The recovery of 96%-116% for total As, 85%-122% for As(Ⅲ), and 88%-127% for As(V) were achieved for groundwater samples with a total As concentration range 100-800 μg/L. The colorimetric result showed that 3.61 g/L As(Ⅲ) existed as the only As species in a real industrial wastewater, which was in good agreement with the HPLC-AFS result of 3.56 g/L As(Ⅲ). No interference with the color development was observed in the presence of sulfate, phosphate, silicate, humic acid, and heavy metals from complex water matrix. This accurate, sensitive, and easy-to-use method is especially suitable for field As determination.     

PRB修复铬污染地下水反应介质研究进展

传统的抽出处理技术治理铬污染地下水时,耗时长、效率低、投资与成本高,限制了其广泛应用,近年来兴起的PRB技术很好地解决了这一问题。PRB技术的关键在于反应介质的研究,活性炭、沸石、铁屑等具有较好的除铬性能,但选择性差、易堵塞,混合反应介质可以克服其缺点。同时,对反应介质的研究大多处于实验室阶段,应加强其工程应用研究。     

我国不同区域地质环境城市地下水防污性能分布特征分析

以近几十年来积累的地下水化学和水文地质资料为基础,对我国城市地下水防污性能进行了综合评价,分析了我国不同区域地质环境城市地下水防污性能分布特征及其形成原因,并提出了针对不同地下水防污性能等级的防污建议。     

基于3MRA模型的填埋场安全填埋废物污染物阈值评估方法与应用研究

选取案例填埋场7种目标污染物为研究对象,运用3MRA模型模拟污染物在填埋场周围环境介质中的迁移转化.结果表明,7种目标污染物最低安全填埋阈值大小顺序为:污染物二价镍>苯>镉>铅>六价铬>砷>汞;污染物苯、砷、汞各自的人类和生态受体安全填埋阈值相同,镉和二价镍的人类受体安全填埋阈值高于生态受体,六价铬的生态受体安全填埋阈值高于人类受体,场区地下水的致癌风险和危害商分别为5.06×10-7和2.3×10-1.     

三江平原典型灌区井灌地下水中铁的随水迁移特征

以三江平原典型水稻灌区———黑龙江省农垦总局建三江分局为例,系统调查了该区地下水的铁含量特征,并具体分析了铁通过井灌从地下水进入晒水池、稻田,再通过排水进入多等级沟渠系统的季节迁移过程及铁在相应沉积物或土壤中的分布特征.结果表明,研究区地下水总铁质量浓度为(1.73±0.41)mg.L-1,最大值为11.4 mg.L-1,最小值0.01 mg.L-1,变异系数1.29%.根据2010年水稻种植面积和当地实行的每亩额定灌水量推算,从地下进入稻田和其它地表水体中的铁可达4 976.40 t.溶解性Fe2+、溶解性Fe3+、溶解性铁和总铁都具有明显的季节变化(6、7月较高),且沿水流方向以稻田积水中的含量较高.晒水池和稻田对地下水铁的富集效应明显,二者的总铁质量浓度分别达到地下水的6.17和21.65倍.晒水池沉积物的总铁含量显著高于稻田、农渠和干渠(浓江河).不同氧化铁形态中,仍以晒水池沉积物中各形态铁氧化物的含量较高,而稻田土壤、农渠和干渠沉积物之间没有显著性差异.三江平原典型灌区地下水中的铁通过井灌进入地表水体中,大部分被蓄积在晒水池和稻田中,仅有少部分随稻田退水进入沟渠网,并逐级沉淀在稻田和沟渠沉积物中.铁在随水迁移过程中除了总量变化外,还伴随着种类和形态的转化,这些变化直接受水稻灌溉管理方式的影响,具有明显的季节特征.长期井灌或将导致铁在稻田土壤和沟渠沉积物中的富集,具有潜在的污染风险.     

山东单县浅层高氟高碘地下水的水化学特征及成因分析

氟和碘作为人体必需的微量元素,过少或过多摄入都会影响人身健康,相较于缺氟、缺碘,高氟高碘地下水对人体的危害更加难以控制。该研究选择单县作为典型的水源型高氟高碘地区,通过对浅层高氟高碘地下水进行采样测试,采用箱线图、Piper图及双变量相关性分析等多元统计技术剖析了该区域浅层地下水的水环境特征;采用R型因子分析揭示了水化学成分之间的相互关系,探讨了该区浅层高氟高碘地下水的成因。结果表明:①单县浅层地下水中的氟化物和碘化物的质量浓度均值分别为1.2 mg/L和391 μg/L。②随着氟化物浓度的增加,水化学类型偏向于向HCO₃-Na型和HCO₃-Na·Mg型集中,而随着碘化物浓度的增加,水化学类型则倾向于以HCO₃-Na·Mg为主。③该区域强烈的蒸发浓缩作用是控制单县浅层地下水化学成分的最重要因子;萤石平衡控制作用是控制单县浅层地下水高氟背景的因子;水-有机沉积物相互作用是控制单县浅层地下水高碘背景的因子。     

Seasonal and Flood‐Induced Variations in Groundwater–Surface Water Exchange in a Northern Coldwater Fishery

Groundwater upwelling is important to coldwater fisheries survival. This study used stable isotopes to identify upwelling zones within a watershed, then combined isotope analyses with reach‐scale monitoring to measure surface water–groundwater exchange over time. Research focused on Amity Creek, Minnesota, a basin that exemplifies conditions limiting coldwater species survival along Lake Superior's North Shore where shallow bedrock limits groundwater capacity, lowering baseflows and increasing temperatures. Groundwater‐fed reaches were identified through synoptic isotope sampling, with results highlighting the importance of isolated shallow surficial aquifers (glacially derived sands and gravels) for providing cold baseflow waters. In an alluvial reach, monitoring well results show groundwater was stored in two reservoirs: one that reacts quickly to changes in stream levels, and one that remained isotopically isolated under most flow conditions, but which helps sustain summer baseflows for weeks to months. A 500‐year flood demonstrated the capacity of high‐flow events to alter surface water–groundwater connectivity. The previously isolated reservoir was exchanged or mixed during the flood pulse, while incision lowered the water table for years. The results here provide insight for streams that lack substantial groundwater inputs yet maintain coldwater species at risk in a warming climate and an approach for managers seeking to protect cold baseflow sources.     

Streamflow Depletion Modeling: Methods for an Adaptable and Conjunctive Water Management Decision Support Tool

Groundwater pumping depletes streamflow, which can have significant ecological impacts depending on the magnitude of depletion relative to environmental flow needs. Streamflow depletion estimates from groundwater pumping have been quantified using both analytical and numerical methods, but are not routinely compared to environmental flow needs or used in practical water management tools. Decision support tools that incorporate groundwater dynamics are becoming increasingly necessary for water managers as groundwater regulations become more important in environmental policy, particularly concerning the preservation of environmental flow needs. We develop and apply methods for a web‐based decision support tool for conjunctive groundwater and surface water management, demonstrated using a case study watershed in British Columbia, Canada. Open‐source data are analyzed with a combination of spatial algorithms and previously developed analytical models, such that the tool can be applied to other regions. Streamflow depletion estimates are calculated in four regions in the largely undeveloped Bulkley Valley, British Columbia. Our transparent methodology has geographic and data input flexibility which is a significant improvement on currently existing water management tool methods.     

苏州地区地下水资源城市应急利用适宜性研究

随着太湖水体富营养化程度的不断加剧,建立安全、稳定、可靠的应急备用水源日益重要。利用2005~2009年苏州地区地下水水质连续监测和补充监测资料,对第Ⅱ承压含水层进行了应急利用(生活饮用和工业利用)的水质适宜性和安全性评价分析。研究结果表明:第Ⅱ承含水层主要水化学类型为Na-HCO3、Ca-HCO3和Na-CaHCO3型,水质总体稳定,年际差异很小;地下水水质指数(WQI)均值较低(位于49.98~68.75之间),地下水没有受到有机物污染,可作为应急利用水源;WQI的水质指标贡献率表明,As、Fe、pH和Mn指标的贡献率最大,局部区域As、Fe、Mn及氨氮和亚硝酸盐含量较高,应急利用时应进行处理。朗格里尔饱和指数(LSI)和拉森比(LnR)评价结果表明,该水源易结垢,具有轻微腐蚀倾向,作为工业备用水源时应进行适当的处理。为苏州地区地下水应急水源建设和安全利用提供了科学依据和参考。