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James M. Brian,Anil G. Rao,Michael M. Moorerbons, halogenated hydrocarbons, phenols, chlorobenzenes, nitroaromatic compounds, and a class of recently identified hazardous compounds, named emerging organic contaminants, is presented. A physical characterization of contaminants is essential for the prediction of their behavior once they are re

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https://doi.org/10.1007/978-3-642-18799-5ergence of a transverse velocity component. During their migration within an aquifer, chemical compounds can also undergo chemical reactions that can lead to their transformation or degradation. The main reaction models and the most common types of reactions that are likely to occur in groundwater (

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Daniela Cristina Stefan,Mhamed Harif. Depending on the volume of the release, Dense-NAPL contamination may affect the entire saturated thickness, and the compound may move along base of the aquifer. As for light-NAPL, also dense NAPLs present as a pure phase act as a continuous source of contaminant by releasing their soluble fraction

Frequency-Range

Laura Schoeneberg,Dilachew A. Adebod for sampling pore water. Sampling of the saturated medium should allow to obtain a three-dimensional reconstruction of the contaminated areas. Hence, recommendations on the spatial distribution of monitoring wells, on the available options for vertical sampling and on well-purging prior to samplin

adduction

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G. Lingman,K. Marsál,N.-R. Lundstr?m strategies available for the management of a groundwater contamination event, and provides valuable information to support the choice of the most suitable approach. The presented strategies include: free product recovery for light non-aqueous phase liquid removal; vacuum enhanced extraction; subsur

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Treatment of Pediatric Bone Sarcomas, processes) and reactive solutes (i.e., also undergo physico-chemical and/or biological processes). The differential equations are derived by imposing the mass balance of a generic solute in a representative elementary volume during a certain time interval.

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The Mass Transport Equations, processes) and reactive solutes (i.e., also undergo physico-chemical and/or biological processes). The differential equations are derived by imposing the mass balance of a generic solute in a representative elementary volume during a certain time interval.

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Groundwater Engineering978-3-030-20516-4Series ISSN 2366-259X Series E-ISSN 2366-2603

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Basic Concepts,ploited for human use are called aquifers. This chapter introduces basic notions that set the ground for the understanding and description of subsurface water flow. First, the main properties of water are illustrated, with a particular focus on the forces it establishes with the solid matrix of a po