In the 1950s, the behavior of volcanoes could be simulated with analog circuits.
I haven't been able to find a diagram of these circuits, however I'm curious as to what the electrical components might have represented:
The "mantel" (the region 3 layers below the crust) is actually a "plastic solid" which suddenly melts (and creates magma/lava) when the pressure is removed by geologic processes such as plate tectonics. However as the magma/lava rises in the column (forming the volcanic vent), the pressure on the mantel increases. Eventually, the pressure increases to a threshold at which the melting stops and this would represent a dormant volcano.
To electrically simulate the process, I suppose the mantle could be the DC source connected to the diodes. When DC is applied to the string, the diodes initially conduct (-IE- the mantle melts) until the capacitor charges enough to created a back EMF (the increase in pressure in the magma/lava column) and the conduction (melting) eventually stops.
I suppose an eruption could also be simulated by discharging the capacitor so the diodes conduct all the time which is analogous to continuous melting and lava flowing to the surface.
I haven't been able to find a diagram of these circuits, however I'm curious as to what the electrical components might have represented:
- Variable DC Voltage = Pressure at the magma reservoir
- Resistance = Viscosity and opposition to magma/lava flow to the earth's surface.
- Capacitance = Pressure of magma/lava column at the earth's surface.
- Diode Threshold Conduction = magma/lava melting threshold for a given pressure below the earth's surface.
The "mantel" (the region 3 layers below the crust) is actually a "plastic solid" which suddenly melts (and creates magma/lava) when the pressure is removed by geologic processes such as plate tectonics. However as the magma/lava rises in the column (forming the volcanic vent), the pressure on the mantel increases. Eventually, the pressure increases to a threshold at which the melting stops and this would represent a dormant volcano.
To electrically simulate the process, I suppose the mantle could be the DC source connected to the diodes. When DC is applied to the string, the diodes initially conduct (-IE- the mantle melts) until the capacitor charges enough to created a back EMF (the increase in pressure in the magma/lava column) and the conduction (melting) eventually stops.
I suppose an eruption could also be simulated by discharging the capacitor so the diodes conduct all the time which is analogous to continuous melting and lava flowing to the surface.
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