Kong Xiang-Sheng, Qi Shi-Hua, Huang Bao-Jian, Zhang Yuan, Li Jie
Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin 541004, China.
Huan Jing Ke Xue. 2012 Mar;33(3):746-53.
In order to understand atmospheric deposition of polycyclic aromatic hydrocarbons impact on ecological environment of Dashiwei Karst Tiankeng Group in Leye County, Guangxi (National Geological Park), the dry and wet deposition samples around Dashiwei Tiankeng were collected by season for a year, and were analyzed utilizing GC-MS for 16 EPA PAHs. The results showed that PAH depositional fluxes ranged from 132.36-1 655.27 ng x (m2 x d)(-1), with an average value of 855.00 ng x (m2 x d)(-1). Weight of PAHs which deposited into Dashiwei Tiankeng was 51.98 g x a(-1), and the dominant PAH compounds are benzo[b] fluoranthene, chrysene, benzo[a] pryene, benzo[k]fluoranthene, anthracene, phenanthrene and naphthalene. Spatial distribution of PAHs around Dashiwei Tiankeng was: the east valley entrance > the south valley entrance > the north valley entrance > the west peak; seasonal variability of PAH depositional fluxes was: spring > summer > autumn > winter. Deposition fluxes of PAHs were 4.6 times higher in spring and summer than those in autumn and winter. The dominant PAH compounds were 4-6 rings PAHs in spring and summer, but the dominant PAH compounds were 2-3 rings PAHs in autumn and winter. PAH depositional fluxes in this study area were closely related with precipitation, wind direction, temperature, wind speed and location of pollution sources. PAHs increased in spring and summer in Dashiwei Karst Tiankeng Group, this could be transported by atmospheric movement from higher air temperature and lower elevation areas where industry developed in Guangxi.
为了解广西乐业县大石围喀斯特天坑群(国家地质公园)大气中多环芳烃沉降对生态环境的影响,对大石围天坑周边的干湿沉降样品进行了为期一年的季节性采集,并利用气相色谱 - 质谱联用仪对16种美国环保署优先控制的多环芳烃进行了分析。结果表明,多环芳烃的沉降通量范围为132.36 - 1655.27 ng x (m2 x d)(-1),平均值为855.00 ng x (m2 x d)(-1)。沉降到大石围天坑的多环芳烃总量为51.98 g x a(-1),主要的多环芳烃化合物为苯并[b]荧蒽、 Chrysene、苯并[a]芘、苯并[k]荧蒽、蒽、菲和萘。大石围天坑周边多环芳烃的空间分布为:东谷口 > 南谷口 > 北谷口 > 西峰;多环芳烃沉降通量的季节变化为:春季 > 夏季 > 秋季 > 冬季。春夏季多环芳烃的沉降通量比秋冬季高4.6倍。春夏季主要的多环芳烃化合物为4 - 6环多环芳烃,而秋冬季主要的多环芳烃化合物为2 - 3环多环芳烃。本研究区域内多环芳烃的沉降通量与降水、风向、温度、风速及污染源位置密切相关。大石围喀斯特天坑群春夏季多环芳烃含量增加,这可能是由大气运动从广西工业发达的气温较高、海拔较低地区传输而来的。