mproving Gas Permeability Measurements for Environmental Monitoring and Management

T. P
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Abstract

Intrinsic permeability is a crucial parameter to interpret soil gas data recorded from monitoring stations in different environmental settings. It is also fundamental for environmental management and pollution reme diation. An improved version of a permeameter (PRM3) recently developed for environmental applications is presented and calibrated against a reference instrument (RADON - JOK produced by RADON v.o.s.). The innovations of this prototype are: i) the absence of the flow meter, and ii) a membrane pump in place of a rotary vane device. Proper calculation of the permeability from Darcy’s law is provided, as well as a modified formula for permeability determination in volcanic areas. Actually, soil gas viscosity and permeability are affected by changing gas temperature and composition. The effects of these two parameters on soil gas viscosity and permeability are also displayed. The second part of the paper shows the employ of permeability measurements in environment al monitoring. The aim of these field - works was the study of lateral and vertical variability of soil permeability at a very small scale (step of 0.25 m) and the effect of intrinsic permeability on gas transport through the soil and on gas concentration al ong depth profiles . We chose 2 different test sites: Valle della Caffarella (Roma, Italy) and Solfatara Volcano (Pozzuoli, Italy) areas. A specific protocol, designed to check any interference among permeability measurements carried out at very close dista nces demonstrated that no disturbance is occurring. Intrinsic permeability profiles resulted to be good proxy indicators for the degassing style of the two areas. In both cases, it gave important hints to interpret environmental data and help in the manage ment of the sites.
在环境监测和管理中改进气体渗透性测量方法
固有渗透率是解释不同环境条件下监测站记录的土壤气体数据的关键参数。它也是环境管理和污染治理的基础。介绍了最近为环境应用开发的一种改进型渗透仪(PRM3),并根据RADON v.o.s公司生产的RADON - JOK标准仪器进行了校准。这个原型的创新之处在于:i)没有流量计,ii)用膜泵代替旋转叶片装置。提出了用达西定律计算渗透率的方法,并提出了一种修正的火山岩地区渗透率计算公式。实际上,土壤气体的粘度和渗透性受气体温度和成分变化的影响。分析了这两个参数对土壤气体粘度和渗透率的影响。第二部分介绍了渗透率测量在环境监测中的应用。这些野外工作的目的是在非常小的尺度上(步距0.25 m)研究土壤渗透性的横向和垂直变化,以及固有渗透性对土壤中气体输送和长深度剖面的气体浓度的影响。我们选择了2个不同的测试地点:Valle della Caffarella(意大利罗马)和Solfatara Volcano(意大利波佐利)地区。设计用于检查在非常近距离进行的渗透率测量之间是否存在干扰的特定方案表明,没有发生干扰。本征渗透率曲线是两个地区脱气类型的良好代理指标。在这两种情况下,它为解释环境数据和帮助管理场地提供了重要的提示。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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