Garbesi K, Robinson A L, Sextro R G, Nazaroff W W
Department of Environmental Studies, San José State University, San José, CA 94709, USA.
Health Phys. 1999 Aug;77(2):183-91. doi: 10.1097/00004032-199908000-00008.
Soil permeability to air can increase substantially with measurement length scale. We tested the hypothesis that the scale effect could resolve large model underpredictions of radon and soil-gas entry into two experimental basement structures located in natural sandy-loam soil at a field site in Ben Lomond, CA. Previously, the model input for permeability at the site had been assessed based on 0.5-m scale measurements. After determining the soil-structure interaction scale (system scale) to be approximately 3 m, the model input was changed to reflect 3-m scale permeability measurements. This adjustment reduced unacceptably large model underpredictions, of a factor of 3 to 5, to a range near that of acceptable experimental error, 20 to 40%. The permeability scale effect may explain large and persistent model underestimates of radon entry into real houses. The results argue strongly for determining permeability at a length scale consistent with that of the system under study.
土壤对空气的渗透率会随着测量长度尺度的增加而大幅提高。我们检验了这样一个假设:尺度效应能够解决大型模型对氡和土壤气体进入位于加利福尼亚州本洛蒙德一个野外场地天然砂壤土中的两个实验性地下室结构的预测严重偏低的问题。此前,该场地渗透率的模型输入是基于0.5米尺度的测量来评估的。在确定土壤 - 结构相互作用尺度(系统尺度)约为3米后,模型输入被更改以反映3米尺度的渗透率测量结果。这种调整将不可接受的大幅模型预测偏低(低3至5倍)降低到了接近可接受实验误差范围(20%至40%)。渗透率尺度效应可能解释了模型对实际房屋中氡进入量长期存在的大幅低估。结果有力地表明,应在与所研究系统一致的长度尺度上确定渗透率。