快速城镇化三角洲地区高碘地下水赋存特征及驱动因素:以珠江三角洲为例

沿海城镇化地区地下水中碘来源复杂,高碘地下水对生活饮用水安全存在潜在威胁.以城镇化快速发展的珠江三角洲为研究区,运用数理统计和主成分分析等方法探讨了珠江三角洲不同含水层和不同城镇化水平地区浅层地下水中碘的赋存特征及驱动因素.结果表明,研究区浅层地下水ρ(I-)介于未检出～2.34 mg·L-1,主要以I-的形式存在.研...     

广州大学城珠江水域多环芳烃的污染特征

利用GC-MS对广州大学城珠江水域的地表水及表层沉积物中多环芳烃(PAHs)的含量进行了分析。结果表明,广州大学城珠江水域及表层沉积物中均可检出PAHs,水体优控PAHs总量在1061.7~6577.8ng/L之间,沉积物中优控PAHs总量分布在896.1~7248ng/g之间。广州大学城珠江水域的PAHs属混合来源,主要有石油类产品的输入(漏油泄油)和化石燃料的燃烧(大气沉降)。     

珠三角区域空气质量预报方法及预报效果评估

介绍了珠三角区域空气质量预报的"六步法"流程,并对2015年空气质量等级和首要污染物预报准确率进行评估研究。结果表明,2015年珠三角区域空气质量以优良为主,24 h等级预报准确率1月最高2月最低,平均准确率为87.6%;出现的首要污染物种类包括PM2.5,PM10,O3-8 h和NO2,预报准确率9月最高3月最低,平均准确率为72.7%。     

粤港珠江三角洲区域空气质量分级技术及信息发布方法研究

根据珠江三角洲空气污染特征.将,SO2、NO2、PM10、O3四项参数作为评价指标,对建立区域空气质量指数(Regional Air Quality Index,RAQI)~型及区域空气质量分级方法,以及开展区域空气质量信息发布的空间表征技术进行了研究,以便直观有效地反映珠江三角洲区域空气质量状况.     

广佛珠江河网区石油类污染数值模拟研究

基于EFDC模型，构建了广佛珠江感潮河网区三维水动力模型；同时，通过耦合石油类污染物水力输运与悬沙吸附一沉降过程，构建石油类水质数学模型，从而更全面客观地模拟水体石油类污染物的迁移转化过程。通过2001年1月实例模拟及验证，表明模型能较好地模拟再现珠江水体石油类浓度变化过程，为日后珠江水环境质量监控与水质改善、城市河涌整治成果评价及预测等提供技术支持。     

Natural radioactivity levels in topsoil from the Pearl River Delta Zone, Guangdong, China

Concentrations of the natural radionuclides ²³⁸U, ²²⁶Ra, ²³²Th and ⁴⁰K have been measured by γ-ray spectrometry in 796 topsoil samples from the Pearl River Delta Zone (PRDZ) of Guangdong, China. The mean concentrations for ²³⁸U, ²²⁶Ra, ²³²Th and ⁴⁰K were found to be 140 ± 37 Bq kg⁻¹, 134 ± 41 Bq kg⁻¹, 187 ± 80 Bq kg⁻¹ and 680 ± 203 Bq kg⁻¹ dry mass, respectively. These values were all higher than the mean values in soil for China and the world. Outdoor air-absorbed dose rates, calculated from activity concentrations of ²²⁶Ra, ²³²Th and ⁴⁰K, ranged from 86 to 237 nGy h⁻¹, with a mean value of 165 ± 46 nGy h⁻¹. The corresponding annual outdoor effective dose rate per person was estimated to be between 0.11 and 0.29 mSv y⁻¹, with a mean value of 0.20 ± 0.06 mSv y⁻¹, which was also higher than the world mean value of 0.07 mSv y⁻¹. The radium equivalent activity (Ra_eq) and the external hazard index (I_r) resulted from the natural radionuclides in soil, were also calculated and found to vary from 230 to 676 Bq kg⁻¹ and from 0.6 to 1.8, respectively. The Ra_eq and the I_r in all the investigated regions were up to 75% higher than the set limits of 370 Bq kg⁻¹ and 1.0, respectively.