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福建东南沿海地热田主要受断裂控制,温泉多为中低温水热系统,适用于直接供热。在该区典型地热田之一的贵安地热田进行了4种物探方法试验研究:大地电流和声频大地电磁测深、自然电场法、地面磁测、一米测温。由于温度并非是影响电阻率变化的唯一因素,因此仅仅根据电阻率值并不能区别高温带与低温带。研究表明:大地电流和声频大地电磁测深资料的定性和定量解释所获取的电阻率分布可确定断裂构造在地表以及向地下延伸分布特征;另外3种方法在某种程度上反映构造或温度变化,可以有效地圈定热田中心部位。例如,构造破碎带可以引起负磁异常;自然电位正异常与上涌泉相关;浅孔测温高值带与热田最高温泉相对应等。 相似文献
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S. J. Swithenby 《Cellular and molecular life sciences : CMLS》1988,44(8):673-678
Summary The ionic currents flowing in developing organisms produce weak magnetic fields that can be detected using SQUID magnetometers. The method is non-invasive and dc recording is possible. To date SQUID magnetometers have mainly been used in human studies. The features of the technique are described and the prospects of extending its use to developmental studies are discussed. Feasible instrumental specifications are indicated. A recent SQUID magnetometer investigation of ionic current flow in the developing chick in ovo is summarised as an illustration of the magnetometer method. The paper as a whole argues that magnetometry is a useful alternative or adjunct to electrode-based experiments on the electrophysiology of developing organisms. 相似文献
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