Pre-polarization fields for earth's field NMR: Fast discharge for use with short T 1 and large coils
The sensitivity of earth's field NMR is greatly increased by the use of a pre-polarizing field B . When used with short T samples, the field must be decreased rapidly to avoid loss of the pre-polarized magnetization by relaxation. Such a rapid decrease in the field requires rapid discharge (∼10...
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Veröffentlicht in: | Journal of magnetic resonance (1997) 2017-08, Vol.281, p.241 |
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creator | Conradi, Mark S Altobelli, Stephen A Sowko, Nicholas J Conradi, Susan H Fukushima, Eiichi |
description | The sensitivity of earth's field NMR is greatly increased by the use of a pre-polarizing field B
. When used with short T
samples, the field must be decreased rapidly to avoid loss of the pre-polarized magnetization by relaxation. Such a rapid decrease in the field requires rapid discharge (∼10ms) of a large stored magnetic field energy (∼700J). In addition, in order that the full pre-polarized magnetization be available for the subsequent pulse sequence, the field discharge should be adiabatic. This requirement is difficult to fulfill in cases where B
is not everywhere parallel to the earth's field, such as with a large surface coil. Circuitry for rapid and controlled discharge is presented. Simulations and experiments confirm the importance of both of these conditions. |
doi_str_mv | 10.1016/j.jmr.2017.06.001 |
format | Article |
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. When used with short T
samples, the field must be decreased rapidly to avoid loss of the pre-polarized magnetization by relaxation. Such a rapid decrease in the field requires rapid discharge (∼10ms) of a large stored magnetic field energy (∼700J). In addition, in order that the full pre-polarized magnetization be available for the subsequent pulse sequence, the field discharge should be adiabatic. This requirement is difficult to fulfill in cases where B
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. When used with short T
samples, the field must be decreased rapidly to avoid loss of the pre-polarized magnetization by relaxation. Such a rapid decrease in the field requires rapid discharge (∼10ms) of a large stored magnetic field energy (∼700J). In addition, in order that the full pre-polarized magnetization be available for the subsequent pulse sequence, the field discharge should be adiabatic. This requirement is difficult to fulfill in cases where B
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. When used with short T
samples, the field must be decreased rapidly to avoid loss of the pre-polarized magnetization by relaxation. Such a rapid decrease in the field requires rapid discharge (∼10ms) of a large stored magnetic field energy (∼700J). In addition, in order that the full pre-polarized magnetization be available for the subsequent pulse sequence, the field discharge should be adiabatic. This requirement is difficult to fulfill in cases where B
is not everywhere parallel to the earth's field, such as with a large surface coil. Circuitry for rapid and controlled discharge is presented. Simulations and experiments confirm the importance of both of these conditions.</abstract><cop>United States</cop><pmid>28646695</pmid><doi>10.1016/j.jmr.2017.06.001</doi></addata></record> |
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title | Pre-polarization fields for earth's field NMR: Fast discharge for use with short T 1 and large coils |
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