石油污染土壤及地下水的生物修复进展[综述]

所谓石油污染土壤的生物修复［２］（Ｂｉｏｒｅｍｅｄｉａｔｉｏｎ）,是指利用微生物及其他生物,将存在于土壤、地下水和海洋中的有毒有害的石油污染物现场降解成二氧化碳和水或转化成为无害物质的工程技术系统．它是传统的生物处理方法的延伸,其创新之处在于它治理的对象是较大面积的污染．由于现场环境的复杂性,因而产生了许多不同于治理点污染的概念和技术措施．与物理、化学土壤修复技术相比,生物修复技术具有多种优点［１,２］．ＫｕｒｏｄａＤａｎｎａＲ［３］曾以美国应用实例对生物修复技的特点进行过详细的归纳与总结：既可…     

硫化亚铁活化过一硫酸盐降解含表面活性剂水溶液中三氯乙烯的效果与机制

采用硫化亚铁(FeS)活化过一硫酸盐(PMS)降解含表面活性剂吐温-80(TW-80)水溶液中的三氯乙烯(TCE),考察了PMS和FeS投加量、TW-80浓度、溶液初始pH、无机阴离子(Cl^–和HCO₃^–)对TCE降解的影响,确定了PMS/FeS体系中的主导自由基及TCE降解机理,验证了PMS/FeS体系处理实际地下水中含TW-80的TCE效果。结果表明：增加PMS或FeS投加量有利于TCE的降解,但当其投加剂量分别超过0.8 mmol·L^–1和0.6 g·L^–1时,TCE降解反而受到抑制,且TCE的降解率随TW-80浓度的增加而下降;PMS/FeS体系对pH有较宽的适用范围,在pH=11时受到抑制,Cl^–和HCO₃^–对TCE降解有抑制作用;通过自由基淬灭实验和电子顺磁共振实验确定了SO₄^–·、HO·和O₂^–·是PMS/FeS体系中的主导自由基;相比于其他氯代烃,该体系对四氯乙烯和四氯化碳也有较好的降解效果;实际地下水的处理结果证实PMS/FeS体系在实际应用中具有潜力和优势。     

Uranium quantification in groundwater and health risk from its ingestion in Haryana,India

Uranium is a naturally occurring radioactive element which may cause toxicological or radiological hazards to the public if present in drinking water. This study reports the quantification of uranium in groundwater of major towns of the district Fatehabad, Haryana, India. Uranium concentrations ranged between 0.3 and 48 μg L^?1. In 22% of the groundwater samples, uranium concentrations were higher than the World Health Organization maximum permissible limit of 30 µg L^?1. The radiological dose for males was found to be in the range of 4.8?×?10^?4–7.1?×?10^?2 mSv y^?1 and for females 3.5?×?10^?4–5.2?×?10^?2 mSv y^?1. The results showed that due to the ingestion of groundwater in the study area, radiological cancer risk is in the range of 9.1?×?10^?7–1.3?×?10^?4, lower than the risk limit. Uranium ingestion from groundwater varied from 0.02 to 3.5 µg kg^?1 day^?1, which is within acceptable limit.     

Ground water pollution by pesticides at the watershed‐soil catena scale: Lindane at the lower Colorado river basin (Argentina)

The movement of Lindane from application points at the surface soil towards the underground water and further transport within this compartment at the watershed‐soil catena scale, was inspected by measurements of the pesticide concentration in soil water at a controlled experiment where it was applied at a usual label dose. The concentrations of Lindane in soil water and the upper phreatic level were also measured at successive dates in samples obtained from a net of phreatimeter probes distributed over the area (1,500 km²) of the lower Colorado River basin (Bs. Aires, Argentina). The location of cultivated‐irrigated areas within the watershed was inferred from NDVI (Normalized Difference Vegetation Index)‐1 km‐10 day AVHRR images obtained at successive dates during the irrigation season. Feasible paths of underground gravitational water flows were computed by means of a GIS‐simulation model on the basis of local terrain slopes and aspects. The pattern of Lindane distribution over the basin was explained on the basis of the distribution of diffuse sources, the patterns of percolation and groundwater flows and the thermodynamic characteristics of the pesticide.     

环鄱阳湖浅层地下水水化学特征的时空变化

系统采集了鄱阳湖周边地下水,分析测定各单元的水化学参数.结果表明,环鄱阳湖浅层地下水整体偏酸性,呈低矿化度,局部地区出现微咸水.环鄱阳湖浅层地下水丰、枯水期的优势阴离子为HCO3-,阳离子为Ca2+和Mg2+.运用SPSS软件做离子相关性分析,各离子间均呈正相关性,说明可能有相同的来源.地下水的水化学类型整体表现为HCO3-Ca-Mg型,丰水期相对于枯水期出现较多的NO3-型和SO24-型水体,局部区域优势阴离子改变,出现了NO3-型、Cl-型地下水,可能受到农业化肥和工业废水排放的影响.整体上地下水的水化学类型受当地岩石类型的影响比较大,个别地区受人为的活动干扰较为强烈.     

氯唑磷在土壤中的降解性能与移动性研究

在实验室与野外田间状态下，研究了氯唑磷农药在砂土，砂壤土及粘壤土中的降解特性，降解速率依次为：砂壤土〉粘壤土〉矿土；其降解半衰期分别为４７．２、５９．８和６７．３ｄ。     

蔬菜常用农药在地下水中残留风险评估

为明确蔬菜常用农药在地下水中的环境风险,运用China-Pearl和SCI-GROW模型开展地下水环境暴露评估,并根据我国成人和儿童暴露参数推导25种农药预测无效应浓度(PNEC)。研究发现,25种农药PECgw为0~18.340μg·L-1,成年人PNECgw为0.003~19.654 mg·L-1,儿童PNECgw为0.001~23.253 mg·L-1。成年人和儿童的RQgw值均小于1,表明25种农药按照登记用量使用,我国成人和各年龄阶段儿童直接饮用施用农药区域地下水的环境风险可接受。     

内蒙古乌海热电厂水源地地下水资源量评价

在分析勘察区水文地质条件的基础上,用水量均衡法计算了该区地下水的补给量和排泄量,结果为负均衡。水源地开采后水源主要来源于黄河激发补给量,抽水试验和数值模拟表明黄河激发补给量为3.45×10⁴m³/d。根据水位预测,水源地开采20年后和不利水文、气象条件下连续开采2年,水位下降值均不及含水层厚度的1/10,说明水源地开采量3×10⁴m³/d是有保证的,可以满足电厂供水要求。     

贵州遵义高坪水源地岩溶地下水重金属污染健康风险初步评价

健康风险评价是定量描述污染物对人体健康产生危害的重要方法. 对贵州省遵义市高坪水源地岩溶地下水21个采样点中Cd,Cr,Pb和Cu的含量进行了调查研究,并应用目前美国环境保护局(USEPA)推荐的健康风险评价模型,对该地岩溶地下水中重金属所引起的健康风险做出初步评价. 结果表明:研究区内丰水期健康危害的个人致癌风险最大值为3.52×10-5 a-1,没有超过国际辐射防护委员会(ICRP)推荐的通过饮水途径最大可接受风险水平(5.00×10-5 a-1);枯水期各采样点的个人致癌风险值为10-8～10-7 a-1,远低于ICRP推荐的最大可接受水平. 丰水期的健康风险明显大于枯水期,重金属Cr是产生风险的主要污染物.