Arid
DOI10.1029/2001WR000813
Chemical diffusion between a fracture and the surrounding matrix: Measurement by computed tomography and modeling
Polak, A; Grader, AS; Wallach, R; Nativ, R
通讯作者Polak, A
来源期刊WATER RESOURCES RESEARCH
ISSN0043-1397
出版年2003
卷号39期号:4
英文摘要

[ 1] A medical-based X-ray CT scanner was used to monitor the diffusion of NaI into the matrix of a 20-cm-long, 5-cm diameter fractured chalk core. The core was retrieved from a core hole at a depth of 18.3 m and was artificially fractured along its axis using a Brazilian-like test. The NaI solution flowed continuously along the vertically oriented fracture and the transient lateral concentration distribution within the matrix at different cross sections along the core was monitored by two-dimensional 2-mm-thick slices through the sample and an in-plan pixel resolution of about 0.25 mm. The lateral concentration distribution within the matrix was characterized by a sharp decrease at a thin matrix layer adjacent to the fracture/matrix interface followed by diffusion-type concentration distribution elsewhere. This concentration variation suggests that a thin transition layer exists along the fracture/matrix interface where the diffusion coefficient is higher than that of the bulk matrix. The higher diffusion coefficient of the transition layer is possibly related to minifissures that develop when fractures are formed. After 6 days of tracer injection into the fracture inlet, distilled water was injected for 11 days, forming a reverse concentration gradient and back diffusion. A mathematical model that assumes diffusion within the matrix and a linear concentration variation through the transition layer from its value in the fracture to its time-dependent value at the transition layer/matrix interface was developed. Very good agreement was obtained between the predicted and measured concentrations during both the diffusion and back diffusion phases. Application of the model to a field site in the Negev desert, Israel, suggested that the rock matrix that had been subjected to 20 year of contaminant diffusion would require more than 200 years before it would stop releasing contaminants into the intersecting fractures ( a parabolic process). According to these calculations, remediation efforts based on clean water injection into the fractures are not feasible.


英文关键词diffusion fractured rock chalk contaminant transport computerized tomography
类型Article
语种英语
国家Israel ; USA
收录类别SCI-E
WOS记录号WOS:000182847300001
WOS关键词POROUS-MEDIA ; CONTAMINANT TRANSPORT ; SOLUTE TRANSPORT ; PROCESS ZONE ; CHALK ; POROSITY ; GRANITE ; FLOW ; RETARDATION ; DISPERSION
WOS类目Environmental Sciences ; Limnology ; Water Resources
WOS研究方向Environmental Sciences & Ecology ; Marine & Freshwater Biology ; Water Resources
来源机构Hebrew University of Jerusalem
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/145979
作者单位(1)Hebrew Univ Jerusalem, Fac Agr Food & Environm Qual Sci, Seagram Ctr Soil & Water Sci, IL-76100 Rehovot, Israel;(2)Penn State Univ, Energy & Geoenvironm Engn Dept, Petr & Nat Gas Engn Program, University Pk, PA 16802 USA
推荐引用方式
GB/T 7714
Polak, A,Grader, AS,Wallach, R,et al. Chemical diffusion between a fracture and the surrounding matrix: Measurement by computed tomography and modeling[J]. Hebrew University of Jerusalem,2003,39(4).
APA Polak, A,Grader, AS,Wallach, R,&Nativ, R.(2003).Chemical diffusion between a fracture and the surrounding matrix: Measurement by computed tomography and modeling.WATER RESOURCES RESEARCH,39(4).
MLA Polak, A,et al."Chemical diffusion between a fracture and the surrounding matrix: Measurement by computed tomography and modeling".WATER RESOURCES RESEARCH 39.4(2003).
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