Volcano Probe Essay Example | Topics and Well Written Essays - 1000 words

Volcano Probe - attempt ExamplePressure and temperature changes in a volcano leads to its construction and its overall behaviour in deference to the period of formation to the eruption period. It is tweet and temperature that explains how a volcano is formed and how it erupts on to the earth step up in the long run (Beatty, 1998, p. 67).In general volcanoes normally occur in areas where tectonic familys influence or converge or where the earth perkiness stretch or thin as in the case of African Rift Valley. Similarly, volcanoes can arise as a result of mantle plumes or hotspots which may occur far from the platonic plates boundaries. Where volcanoes occur due to divergence of platonic plates, new ocean crust is formed by hot molten lock or the magma which slowly cool and solidify. In essence, the crust is very thin at these ridges as a result of tectonic plates pull. Pressure resulting from the crust thinning gives rise to adiabatic expansion with a new oceanic crust formin g as a result of partial melting of the mantle. In regard to converging platonic plates, the collision of a Continental plate and an oceanic plate results into a subduction zone which by extension results into the submersion of the oceanic plate under the continental plate. The subducting layer releases water which lowers the temperature of the mantle wedge above the result of which is magma creation.On the separate hand, hotspots which are commonly located above mantle plumes where there is convection of the mantle of the earth results into a tug of hot material that rises up to the earth crust. Plume temperature causes the crust to melt forming pipes useful in give vent magma (Beatty, 1998, p. 98). Following the above discussion, radiation diagraming a volcano probe would require one to properly take the factors and forces behind volcano formation. In essence, one would be required to put into consideration the thermal forces touch on and it is at this point that knowledge o f thermal physics becomes essential. In this case, one would be required to design a temperature and pressure measuring system that is compatible with changes in the two parameters and which can withstand massive changes for that matter. As such, one would be required to consider the materials with which the pressure and temperature measuring system is built from as some materials may not be able to withstand huge changes in these two parameters. For example, metals are known to melt under different temperatures with some melting at lower temperatures than the others. Still, some of these metals when open to high pressures react or behave differently from the others (A.I.P. 2000, p. 56). Any component designed to study the behavior of a volcano will have to put into consideration all the thermal physics aspects of pressure and temperature among other things. Such things include the permissible pressure range of the pressure sensing element and the temperature range of the tempera ture sensor to be used in the measuring instrument. Equally important is the pressure and temperature range of the outer structure inhibiting the sensors. Moreover, the data collected by these sensors will need to be transmitted to a receiver by dint of a transmitter.