人工示踪剂在通风洞穴中的扩散

IF 1.3 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY International Journal of Speleology Pub Date : 2024-04-01 DOI:10.5038/1827-806x.53.1.2497
Claudio Pastore, Eric Weber, Frédéric Doumenc, P. Jeannin, Marc Lütscher
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引用次数: 0

摘要

人工二氧化碳被用作岩溶通风管道的示踪剂,用于推断气流和研究示踪剂的扩散。在岩溶浸润带,洞穴通风是热量、气体和气溶胶的一种有效传输方式,因此推动了气载粒子的空间分布。模拟这种空气传播需要导管系统的几何和物理参数,包括横截面积、气流和平均风速,以及描述溶质扩散的纵向扩散系数。我们在一个矿井(人工导管)和两个通风洞穴(天然导管)中进行了四次测量试验。在本文中,我们证明了使用二氧化碳作为示踪剂可以获得可靠的气流速率和岩溶通风导管的几何信息。我们沿两个洞穴和一个矿井测量了气流,并与用热线风速计进行的精确测量进行了比较。二氧化碳测试估计的横截面积与现场测量的横截面积进行了比较。此外,突破曲线(BTC)分析表明,由于分散奇点的存在,气溶胶可能会沉积在调查的天然导管中,从而导致尾流加剧。在 Milandre 和 Longeaigue 洞穴观察到的长尾现象可能是由于横截面的变化造成的。在这些地点测试的一维平流-弥散模型无法适应天然导管中的 BTC 尾流。在 Baulmes 人工导管中,没有观测到长尾流,使用 Chatwin 方法估算了分散系数,并与泰勒理论的预测进行了比较。尽管 Baulmes 煤矿的几何形状很规则,但泰勒相关理论明显低估了根据现场数据推断出的扩散系数,这表明需要对矿井中的湍流扩散开展更多的理论研究。本文对通风岩溶通道沿线的空气运动和物质弥散有了初步了解,为建立适当的气溶胶弥散模型做好了准备。
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Dispersion of artificial tracers in ventilated caves
Artificial CO2 was used as a tracer along ventilated karst conduits to infer airflow and investigate tracer dispersion. In the karst vadose zone, cave ventilation is an efficient mode of transport for heat, gases and aerosols and thus drives the spatial distribution of airborne particles. Modelling this airborne transport requires geometrical and physical parameters of the conduit system, including the cross-sectional areas, the airflow and average air speed, as well as the longitudinal dispersion coefficient which describes the spreading of a solute. Four gauging tests were carried out in one mine (artificial conduit) and two ventilated caves (natural conduits). In this paper, we demonstrate that it is possible to gain reliable airflow rates and geometric information of ventilated karst conduits using CO2 as a tracer. Airflow was gauged along two caves and one mine and compared with punctual measurements made with a hot-wire anemometer. Cross-sectional areas estimated with CO2 tests were compared with those measured in situ. Moreover, breakthrough curve (BTC) analysis displayed an accentuated tailing along the investigated natural conduits due to the presence of dispersive singularities which possibly enable aerosol deposition. The long tailing observed in Milandre and Longeaigue Caves is probably due to cross-section variations. A 1-D advection-dispersion model tested for these sites was unable to fit BTC tailing in natural conduits. In Baulmes artificial conduit, where long tailing is not observed, the dispersion coefficient has been estimated using Chatwin’s method, and compared with the prediction of Taylor’s theory. Despite the regular geometry of Baulmes Mine, Taylor’s correlation significantly underestimates the dispersion coefficient deduced from field data, showing the need for more theoretical work on turbulent dispersion in mines. This paper gives a first insight into air motion and matter dispersion along ventilated karst conduits, preparing for proper aerosol dispersion modelling.
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来源期刊
International Journal of Speleology
International Journal of Speleology 地学-地球科学综合
CiteScore
3.10
自引率
23.10%
发文量
12
审稿时长
>12 weeks
期刊介绍: The International Journal of Speleology has the aim to get cave and karst science known to an increasing number of scientists and scholars. The journal therefore offers the opportunity to all scientists working in and on karst to publish their original research articles or their review papers in an open access, high quality peer reviewed scientific journal at no cost. The journal offers the authors online first, open access, a free PDF of their article, and a wide range of abstracting and indexing services.
期刊最新文献
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