In 1909 [[Theodor Wulf]] developed an [[electrometer]], a device to measure the rate of ion production inside a hermetically sealed container. Wulf used it to find higher levels of radiation at the top of the [[Eiffel Tower]] than at its base. However, his paper was not widely accepted. In 1911, [[Domenico Pacini]] wanted to determine if ionizing radiation came from the Earth or from other sources. He measured simultaneous variations of the rate of ionization over a lake, over the sea, and at a depth of 3 meters from the surface. His measurements suggested that there was a source other than just the Earth.<ref> | In 1909 [[Theodor Wulf]] developed an [[electrometer]], a device to measure the rate of ion production inside a hermetically sealed container. Wulf used it to find higher levels of radiation at the top of the [[Eiffel Tower]] than at its base. However, his paper was not widely accepted. In 1911, [[Domenico Pacini]] wanted to determine if ionizing radiation came from the Earth or from other sources. He measured simultaneous variations of the rate of ionization over a lake, over the sea, and at a depth of 3 meters from the surface. His measurements suggested that there was a source other than just the Earth.<ref> |