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    <title>DSpace Collection: Physics Publications</title>
    <link>http://hdl.handle.net/2440/12354</link>
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  <item rdf:about="http://hdl.handle.net/2440/53803">
    <title>Comparison of band-limited RMS of error channel and calibrated strain in LIGO S5 data</title>
    <link>http://hdl.handle.net/2440/53803</link>
    <description>Title: Comparison of band-limited RMS of error channel and calibrated strain in LIGO S5 data
&lt;br/&gt;
&lt;br/&gt;Author: Brooks, Aidan Francis; Hosken, David John; Mudge, Damien Troy; Munch, Jesper; Veitch, Peter John
&lt;br/&gt;
&lt;br/&gt;Abstract: Many LIGO data analysis pipelines use either the DARM ERR or AS Q channels as the data source and use a response function R(f) generated from time-dependent calibration measurements to convert to strain in the frequency domain. As calibration varies on a timescale of tens of seconds, the response function must be updated frequently. An alternative is to use time-domain calibrated strain h(t). During the recent year-long LIGO science run (S5), preliminary strain data was published alongside raw interferometer output, typically within half an hour of the raw data being produced. As strain data is now available in highly-reduced form within the LIGO data archive, it represents a convenient alternative for LIGO search pipelines. This paper examines a measure of quality for calibrated strain data by calculating the band-limited RMS (BLRMS) difference between h(t) and strain he(t) as calculated directly from DARM ERR in the frequency domain.</description>
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  <item rdf:about="http://hdl.handle.net/2440/53473">
    <title>Very high energy gamma-ray observations of the Galactic Plane with the CANGAROO-III telescopes</title>
    <link>http://hdl.handle.net/2440/53473</link>
    <description>Title: Very high energy gamma-ray observations of the Galactic Plane with the CANGAROO-III telescopes
&lt;br/&gt;
&lt;br/&gt;Author: Clay, Roger William; Stamatescu, Victor; Swaby, David Leslie John; Thornton, Gregory John
&lt;br/&gt;
&lt;br/&gt;Abstract: In 2004, we searched for very high energy (VHE) gamma-ray emission from the Galactic Plane using the CANGAROO-III stereoscopic observation system. Two different longitude regions (ℓ = −19°.5 and ℓ = +13°.0) on the Galactic Plane were observed during July and August 2004. We analyzed events that triggered three telescopes aiming to measure the diffuse emission component. No significant signal associated with the Galactic Plane was found from either of the regions. Assuming that the gamma-ray spectrum is described by a single power-law for energies ranging between a few GeV and TeV, lower limits of the power-law spectral indices were found to be 2.2 for both of the regions with a 99.9% confidence level. This result is consistent with the other VHE measurements and constrains a hypothesis in which a very hard (2.0) cosmic ray electron spectrum was introduced to explain the EGRET GeV anomaly.</description>
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  <item rdf:about="http://hdl.handle.net/2440/53472">
    <title>2.5-D/3-D resistivity modelling in anisotropic media using Gaussian quadrature grids</title>
    <link>http://hdl.handle.net/2440/53472</link>
    <description>Title: 2.5-D/3-D resistivity modelling in anisotropic media using Gaussian quadrature grids
&lt;br/&gt;
&lt;br/&gt;Author: Zhou, Bing; Greenhalgh, Mark Stewart; Greenhalgh, Stewart A.
&lt;br/&gt;
&lt;br/&gt;Abstract: We present a new numerical scheme for 2.5-D/3-D direct current resistivity modelling in heterogeneous, anisotropic media. This method, named the 'Gaussian quadrature grid' (GQG) method, cooperatively combines the solution of the Variational Principle of the partial differential equation, Gaussian quadrature abscissae and local cardinal functions so that it has the main advantages of the spectral element method. The formulation shows that the GQG method is a modification of the spectral element method but does not employ the constant elements or require the mesh generator to match the Earth's surface. This makes it much easier to deal with geological models having a 2-D/3-D complex topography than using traditional numerical methods. The GQG technique can achieve a similar convergence rate to the spectral element method. We show it transforms the 2.5-D/3-D resistivity modelling problem into a sparse and symmetric linear equation system that can be solved by an iterative or matrix inversion method.

Comparison with analytic solutions for homogeneous isotropic and anisotropic models shows that the error depends on the Gaussian quadrature order (abscissa number) and the subdomain size. The higher the order or the smaller the subdomain size that is employed, the more accurate are the results obtained. Several other synthetic examples, both homogeneous and inhomogeneous, incorporating sloping, undulating and severe topography, are presented and found to yield results comparable to finite element solutions involving a dense mesh.</description>
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  <item rdf:about="http://hdl.handle.net/2440/53415">
    <title>Luminescence dating: an Australian perspective</title>
    <link>http://hdl.handle.net/2440/53415</link>
    <description>Title: Luminescence dating: an Australian perspective
&lt;br/&gt;
&lt;br/&gt;Author: Prescott, John Russell; Robertson, Gillian Barnard
&lt;br/&gt;
&lt;br/&gt;Abstract: Applications of luminescence dating to Quaternary earth science are reviewed, the examples being from Australia. The methods of thermoluminescence (TL) and optical dating using optically stimulated luminescence (OSL) are briefly described, together with their limitations. Prominent results are: (i) the distribution of ages of Australian desert dunes shows peak activity at about the time of the last glacial maximum; (ii) the lake-full episodes of Lake Eyre are traced back to 140 ka; (iii) the ages of relict beach dunes in South Australia, when compared with independent geological ages based on δ18O records, show that luminescence dating can be used for ages to 500 ka and older; and (iv) the development of interior river systems has been traced. Among less common applications are: (i) the dating of Australia's youngest volcanoes at 5-4 ka (in these cases the luminescence signal was reset by heat); (ii) the determination of age vs depth of a deep-sea core; and (iv) the age of earthquakes (from the age of the infilling of fault scarps). The emphasis is on recent work and is illustrative rather than exhaustive, the object being to show the scope of luminescence dating. There are suggestions where further research might be directed.</description>
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