Magnetic Resonance in the Subsurface – 5th International ... - LIAG
Magnetic Resonance in the Subsurface – 5th International ... - LIAG
Magnetic Resonance in the Subsurface – 5th International ... - LIAG
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One-Dimensional Theoretical Research on MRS Excited by F<strong>in</strong>ite Current Wire<br />
One-Dimensional Theoretical Research on MRS Excited by F<strong>in</strong>ite Current<br />
Wire<br />
Yuanjie Li, Zhenyu Li, Jianwei Pan, Jiagang Zhang, Hao Liu, Kai Wang<br />
Institute of Geophysics and Geomatics, Ch<strong>in</strong>a University of Geosciences, Wuhan, PRC<br />
liyuanjie305@163.com<br />
<strong>Magnetic</strong> <strong>Resonance</strong> Sound<strong>in</strong>g, abbreviated as<br />
MRS, is a novel geophysical technic specially<br />
designed for direct water exploration by us<strong>in</strong>g<br />
NMR phenomena. At present, <strong>in</strong> <strong>the</strong> fields a<br />
large loop normally acts as both transmitter<br />
and receiver, and <strong>in</strong> this model <strong>in</strong>formation of<br />
aquifers <strong>in</strong> varied depth from <strong>the</strong> shallow to <strong>the</strong><br />
deep will be obta<strong>in</strong>ed through amplify<strong>in</strong>g<br />
stimulat<strong>in</strong>g pulse. However, this traditional<br />
work mode has shortcom<strong>in</strong>gs of <strong>in</strong>tense labour<br />
of <strong>the</strong> operator, great <strong>in</strong>fluence from landform,<br />
only one-dimensional <strong>in</strong>formation of aquifers<br />
be<strong>in</strong>g achieved, and f<strong>in</strong>ite maximum depth of<br />
<strong>in</strong>vestigation which is a problem to be solved<br />
urgently. These drawbacks may be related to<br />
field source that is <strong>the</strong> magnetic field of <strong>the</strong><br />
loop, so, we propose a pioneer<strong>in</strong>g and bold<br />
assumption that <strong>the</strong> stimulat<strong>in</strong>g loop is<br />
superseded by f<strong>in</strong>ite current wire as <strong>the</strong> field<br />
source. In <strong>the</strong>ory, <strong>the</strong> new mode possesses few<br />
advantages of flexible lay-pattern, free from<br />
tomography limitation, affluent <strong>in</strong>formation<br />
about underground aquifer, potential research<br />
<strong>in</strong> detect<strong>in</strong>g depth. Therefore, we will do<br />
research about MRS methods excited by f<strong>in</strong>ite<br />
current wire, and determ<strong>in</strong>e its feasibility.<br />
The distribut<strong>in</strong>g of magnetic field stimulated<br />
by f<strong>in</strong>ite current l<strong>in</strong>e is numerical simulated <strong>in</strong><br />
<strong>the</strong> homogeneous half-space, while its<br />
characteristics will be quantitatively analysed.<br />
And <strong>the</strong>n various aquifers models <strong>in</strong> <strong>the</strong> mode<br />
of MRS method excited by wire source will be<br />
built to acquire NMR signals, characteristics of<br />
which will be compared with those <strong>in</strong> <strong>the</strong><br />
traditional mode. By do<strong>in</strong>g so ,it is can be<br />
concluded that it is feasible to employ l<strong>in</strong>e<br />
source excit<strong>in</strong>g MRS technique , and also <strong>the</strong><br />
superiority of this new method over<br />
conventional mode can be demonstrated. To<br />
perfect one-dimensional <strong>the</strong>oretical system of<br />
MRS method stimulated by l<strong>in</strong>e source,<br />
appropriate <strong>in</strong>version about new method will<br />
be carried out.<br />
References<br />
Anderson, W.L.. (1979): Numerical <strong>in</strong>tegration of<br />
related Hankel transforms of order 0 and 1 by<br />
adaptive digital filter<strong>in</strong>g. Geophysics, 44(10):<br />
1287-1305.<br />
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magnetic resonance as a geophysical tool for<br />
hydrogeologists. Journal of Applied Geophysics,<br />
50(1-2): 21-46.<br />
Braun, M., U. Yaramanci. (2011): Evaluation of <strong>the</strong><br />
Influence of 2-D Electrical Resistivity on<br />
<strong>Magnetic</strong> <strong>Resonance</strong> Sound<strong>in</strong>g. Journal of<br />
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<strong>Magnetic</strong> <strong>Resonance</strong> <strong>in</strong> <strong>the</strong> <strong>Subsurface</strong> <strong>–</strong> 5 th <strong>International</strong> Workshop on <strong>Magnetic</strong> <strong>Resonance</strong><br />
Hannover, Germany, 25 <strong>–</strong> 27 September 2012<br />
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