几年来已经用电阻—电容网络来模拟含水层,大多数的报导工作是论述了周期以微秒计的快时间模拟。然而另一可取的慢时间模拟因为电的实验过程有几秒钟,能使设备和实验技术简单,却有很多优点。本文集中在慢时间模拟的实用方面,给出各部件的细节,叙述模拟井和注水的方法并比较了测量的仪器。还用一个简化了的例题来说明其做法。 Resistivity-capacitance networks have been used to model aquifers for several years, and most of the coverage is about fast-time cycles in microseconds. However, another desirable slow-time simulation has several advantages because the electrical experiment has a few seconds to make the device and the experimental technique simple. This article focuses on the practical aspects of slow time simulation, gives details of each component, describes methods for simulating wells and waterflooding, and compares measured instruments. A simplified example is also used to illustrate its approach.