CAJ | 학술논문

对北京平原区北西向和北东向两条氡浓度剖面进行了测量，发现北部地区氡背景值要大于南部，东向西方向氡浓度变化起伏频繁。分析其原因主要是受到土壤母质、地层以及断裂的影响，发现断裂是影响北京平原区氡浓度高值的主要因素。
대북경평원구북서향화북동향량조동농도부면진행료측량，발현북부지구동배경치요대우남부，동향서방향동농도변화기복빈번。분석기원인주요시수도토양모질、지층이급단렬적영향，발현단렬시영향북경평원구동농도고치적주요인소。
In order to understand the distribution characteristics of soil radon and its influence factors, the investigation of radon characteristics on the two NW-direction and NE-direction profiles are finished in Beijing plain area. The result indicates that the background radon concentration in the north of the area is much higher than that in the south, and the radon concentration varies obviously from east to west. The soil’s parent material, stratum and fault are the major influence factors that cause the above characteristics. Further more, the fault is the major factor on impacting the radon concentration in Beijing plain area.