Abstract
Abstract. We present a new versatile datalogger that can be used for a wide range of possible applications in geosciences. It is adjustable in signal strength and sampling frequency, battery saving and can remotely be controlled over a Global System for Mobile Communication (GSM) connection so that it saves running costs, particularly in monitoring experiments. The internet connection allows for checking functionality, controlling schedules and optimizing pre-amplification. We mainly use it for large-scale electrical resistivity tomography (ERT), where it independently registers voltage time series on three channels, while a square-wave current is injected. For the analysis of this time series we present a new approach that is based on the lock-in (LI) method, mainly known from electronic circuits. The method searches the working point (phase) using three different functions based on a mask signal, and determines the amplitude using a direct current (DC) correlation function. We use synthetic data with different types of noise to compare the new method with existing approaches, i.e. selective stacking and a modified fast Fourier transformation (FFT)-based approach that assumes a 1∕f noise characteristics. All methods give comparable results, but the LI is better than the well-established stacking method. The FFT approach can be even better but only if the noise strictly follows the assumed characteristics. If overshoots are present in the data, which is typical in the field, FFT performs worse even with good data, which is why we conclude that the new LI approach is the most robust solution. This is also proved by a field data set from a long 2-D ERT profile.
Highlights
In geosciences there is a high demand of data from observations of different sorts
Three of the channels are used by three direct current (DC)-coupled high-impedance differential preamplifiers, with four programmable gain stages that are controlled by the microprocessor
It is vital for good electrical resistivity tomography (ERT) data to optimize the input gain, as ERT signals cover a wide range of magnitudes due to different geometries
Summary
In geosciences there is a high demand of data from observations of different sorts. understanding processes requires monitoring various variables with a high temporal resolution. In order to achieve deeper signal penetration, one can use dipole–dipole experiments, in which both current injection and voltage measurement are realized by dipoles that are small compared to the total layout (Alfano 1974). Most large-scale ERT surveys used either high-frequency single-channel seismic dataloggers (e.g. Reftek Texan-125) or three-channel magnetotelluric dataloggers (Roßberg, 2007; Golden et al, 2004) The latter provided only a maximum sampling frequency of 8 Hz leading to anthropogenic noise energy folding into the signal frequency band (typically slightly below 1 Hz) due to aliasing effects. Schünemann et al (2007) used an inverse method to determine the correlation coefficient between the current and voltage This approach is already related to the lock-in approach, which is used in some multi-electrode resistivity instruments (e.g. 4point light 10 W of LGM electronics, www.l-gm.de).
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More From: Geoscientific Instrumentation, Methods and Data Systems
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