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<title>Akram N. Alshawabkeh</title>
<copyright>Copyright (c) 2012  All rights reserved.</copyright>
<link>http://works.bepress.com/aalshawabkeh</link>
<description>Recent documents in Akram N. Alshawabkeh</description>
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<lastBuildDate>Thu, 22 Nov 2012 17:32:19 PST</lastBuildDate>
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<title>Cross-Well Radar I: Experimental Simulation of Cross-Well Tomography and Validation</title>
<link>http://works.bepress.com/aalshawabkeh/6</link>
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<pubDate>Wed, 25 Apr 2012 12:12:29 PDT</pubDate>
<description>
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	<p>This paper explains and evaluates the potential and limitations of conducting Cross-Well Radar (CWR) in sandy soils. Implementing the experiment and data collection in the absence of any scattering object, and in the presence of an acrylic plate (a representative of dielectric objects, such as DNAPL (dense non-aqueous phase liquid) pools, etc.), as a contrasting object in a water-saturated soil is also studied. To be able to image the signature of any object, more than one pair of receiving and transmitting antennas are required. The paper describes a method to achieve repeatable, reliable, and reproducible laboratory results for different transmitter-receiver combinations. Different practical methods were evaluated for collecting multiple-depth data. Similarity of the corresponding results and problems involved in each method are studied and presented. The data show that the frequency response of a saturated coarse-grained soil is smooth due to the continuous and dominant nature of water in saturated soils. The repeatability and potential symmetry of patterns across some borehole axes provide a valuable tool for validation of experimental results. The potential asymmetry across other borehole axes is used as a tool to evaluate the strength of the perturbation on  the electromagnetic field due to hidden objects and to evaluate the feasibility of detecting dielectric objects (such as DNAPL pools, etc.) using CWR. The experimental simulation designed for this paper models a real-life problem in a smaller scale, in a controlled laboratory environment, and within homogenous soils uniformly dry or fully water-saturated, with a uniform dielectric property contrast between the inclusion and background. The soil in the field will not be as homogenous and uniform. The scaling process takes into consideration that as the size is scaled down; the frequency needs to be scaled up. It is noteworthy that this scaling process needs to be extensively studied and validated for future extension of the models to real field applications. For example, to extend the outcome of this work to the real field, the geometry (antennas size, their separation and inclusion size) needs to be scaled up back to the field size, while soil grains will not scale up. Therefore, soil, water and air coupling effects and interactions observed at the laboratory scale do not scale up in the field, and may have different unforeseen effects that require extensive study.</p>

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<author>Arvin Farid et al.</author>


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<title>Experimental Validation of a Numerical Forward Model for Tunnel Detection Using Cross-Borehole Radar</title>
<link>http://works.bepress.com/aalshawabkeh/5</link>
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<pubDate>Wed, 25 Apr 2012 12:12:25 PDT</pubDate>
<description>
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	<p>The goal of this research is to develop an experimentally validated twodimensional (2D) finite difference frequency domain (FDFD) numerical forward model to study the potential of radar-based tunnel detection. Tunnel detection has become a subject of interest to the nation due to the use of tunnels by illegal immigrants, smugglers, prisoners, assailants, and terrorists. These concerns call for research to nondestructively detect, localize, and monitor tunnels. Nondestructive detection requires robust image reconstruction and inverse models, which in turn need robust forward models. Cross-Well Radar (CWR) modality is used for experimentation to avoid soil-air interface roughness. CWR is not a versatile field technology for political boundaries but is still applicable to monitoring the perimeter of buildings or secure sites. Multiple-depth wideband frequency-response measurements are experimentally collected in fully water-saturated sand, across PVC-cased ferrite-bead-jacketed borehole monopole antennae at a pilot scale facility (referred to as SoilBED). The experimental results are then compared with the 2D-FDFD model. The agreement between the results of the numerical and experimental simulations is then evaluated. Results of this work provide key diagnostic tools that can help to develop the algorithms needed for the detection of underground tunnels using radar-based methods.</p>

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<author>Arvin Farid et al.</author>


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<title>The progress of RapSoch (rapid soil characterization system)</title>
<link>http://works.bepress.com/aalshawabkeh/4</link>
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<pubDate>Wed, 25 Apr 2012 12:12:22 PDT</pubDate>
<description>
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	<p>The objective of the program is to design and build a system (Hardware and Software) to characterize physical soil properties including soil strength, moisture content, and classification to a depth of 36 inches. These measurements will be used for the following applications: 1) Selecting optimal locations for vehicle crossings over soil surfaced-terrain obstacles, 2) Prediction of soil deformation under vehicular traffic, 3) Site selection for contingency infrastructure facilities.</p>

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</description>

<author>E. Corey et al.</author>


<category>Soil biodiversity--Measurement</category>

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<title>Cross-Well Radar II: Comparison and Experimental Validation of Modeling Channel Transfer Function</title>
<link>http://works.bepress.com/aalshawabkeh/3</link>
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<pubDate>Wed, 25 Apr 2012 12:12:18 PDT</pubDate>
<description>
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	<p>Close agreement between theory and experiment is critical for adequate understanding and implementation of the Cross-Well Radar (CWR, otherwise known as Cross-Borehole Ground Penetrating Radar) technique, mentioned in a previous paper by the authors. Comparison of experimental results to simulation using a half-space dyadic Green’s function in the frequency domain requires development of transfer functions to transform the experimental data into a compatible form. A Channel Transfer Function (CTF) was developed to avoid having to model the transmitting and receiving characteristics of the antennas. The CTF considers electromagnetic (EM) wave propagation through the intervening media only (soil in this case), and hence corresponds to the simulation results that assume ideal sources and receivers. The CTF is based on assuming the transmitting antenna, soil, and receiving antenna as a cascade of three two-port microwave junctions between the input and output ports of the Vector Network Analyzer (VNA) used in the experimental measurements. Experimentally determined CTF results are then compared with computational model simulations for cases of relatively dry and saturated sandy soil backgrounds. The results demonstrate a reasonable agreement, supporting both the model and CTF formulation.</p>

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<author>Arvin Farid et al.</author>


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<title>Electromagnetic Waves in Contaminated Soils</title>
<link>http://works.bepress.com/aalshawabkeh/2</link>
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<pubDate>Wed, 25 Apr 2012 12:12:15 PDT</pubDate>
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	<p>Soil is a complex, potentially heterogeneous, lossy, and dispersive medium. Modeling the propagation and scattering of electromagnetic (EM) waves in soil is, hence, more challenging than in air or in other less complex media. This chapter will explain fundamentals of the numerical modeling of EM wave propagation and scattering in soil through solving Maxwell’s equations using a finite difference time domain (FDTD) method. The chapter will explain how: (i) the lossy and dispersive soil medium (in both dry and fully water-saturated conditions), (ii) a fourth phase (anomaly), (iii) two different types of transmitting antennae (a monopole and a dipole), and (iv) required absorbing boundary conditions can numerically be modeled. This is described through two examples that simulate the detection of DNAPL (dense nonaqueous-phase liquid) contamination in soil using Cross-well radar (CWR). CWR —otherwise known as cross-borehole GPR (ground penetrating radar)—modality was selected to eliminate the need for simulation of the roughness of the soil-air interface. The two examples demonstrate the scattering effect of a dielectric anomaly (representing a DNAPL pool) on the EM wave propagation through soil. The objective behind selecting these two examples is twofold: (i) explanation of the details and challenges of numerical modeling of EM wave propagation and scattering through soil for an actual problem (in this case, DNAPL detection), and (ii) demonstration of the feasibility of using EM waves for this actual detection problem.</p>

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<author>Arvin Farid et al.</author>


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<title>Tunnel detection using cross borehole radar</title>
<link>http://works.bepress.com/aalshawabkeh/1</link>
<guid isPermaLink="true">http://works.bepress.com/aalshawabkeh/1</guid>
<pubDate>Wed, 25 Apr 2012 12:12:11 PDT</pubDate>
<description>
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	<p>Shallow tunnels present both military and homeland security threats. Smugglers with intentions of avoiding border security have turned tunnels into transit routes for trafficking weapons, people, drugs and other illegal materials. Shallow tunnels are also used by prisoners to escape prisons. While drug and human trafficking have long been border concerns, the threat of international terrorism has transformed the effort to detect tunnels into a national security priority. Imminent threats include assailants entering military fortifications by burrowing under buildings, detonation of high grade explosives from foundations of high security facilities, and high level prisoners escaping detention centers through tunnels. Real-time monitoring of the ground surrounding prisons across the country is a desired solution to this problem.</p>

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</description>

<author>Clay Kurison et al.</author>


<category>Tunnel Detection</category>

<category>Radar</category>

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