The following problem arises when experiments are done solids at high pressures. if the pressure is increased by an amount delta p, this being done under circumstances where the sample is thermally insulated and at a sufficiently slow rate that the process can be regarded as quasi-static, what is the resulting change of temperature delta t of the sample? if delta p is fairly small, derive an expression for delta t in terms of delta p, the absolute temperature t of the sample, its specific heat at constant pressure c_p (in ergs g^-1 deg^-1), its density rho (in g/cm^2), and its volume coefficient of thermal expansion alpha (in deg^-1).

explanation: magnetic pole, region at each end of a magnet where the external magnetic field is strongest. the south-seeking pole, or any pole similar to it, is called a south magnetic pole. unlike poles of different magnets attract each other; like poles repel each other.

here are some information of the future of geothermal energy:

-the future of geothermal energy can pretty much be summed up with a single word: more

-scientists plan in going deeper than 120 meters

-we are hoping that one day, we will get all of our energy from renewable energy sources such as geothermal energy

hope this !

explanation:

considering the bohr theory, the type of connection that requires the transfer the answer conuldn't be right