The hydrogen gas that makes up the atmosphere slowly transitions to liquid as pressures increase. Below the liquid hydrogen rest the heavier liquid helium. Deep in the depths of the body of Saturn the hydrogen, now under tremendous pressure, is transformed to liquid metallic hydrogen. It is believed that at the center of Saturn exists a rocky core about ten times the mass of the Earth. Saturn is approximately 75% hydrogen and 25% helium with traces of other substances like methane and water ice.
Atmosphere: Jupiter is a gaseous planet; it does not have a solid surface like the Earth does (but probably has a solid, rocky core 10 to 15 times the mass of the Earth). When we look at Jupiter, we are seeing icy clouds of gases moving at high speeds in the atmosphere. Jupiter's atmosphere is composed of about 90% hydrogen and 10 % helium. There are only minute traces (0.07%) of methane (CH3), water, ammonia, and rock dust. Mantle: Pressurized hydrogen in the mantle may generate electric currents which generate Jupiter's powerful magnetic field. The outer mantle is liquid hydrogen; the inner mantle is liquid metallic hydrogen. The layers of extraordinarily-compressed hydrogen are in a state so extreme that it has never been produced on Earth. The pressure is so great that the hydrogen molecules inside Jupiter conduct heat and electricity very well, in a metal-like fashion (they do not do this under Earth-like condition). Inside Jupiter, electrons from hydrogen molecules move freely from molecule to molecule (like the electrons of a metal); this is what allows the electrical and heat conductivity. Core: At the center of the planet is a molten rock core which is many times bigger and more massive than the entire Earth. It is 20,000 °C, about three times hotter than the Earth's core. Internal Heat: Jupiter is a heat source; it radiates 1.6 times a much energy as it receives from the Sun. This energy is produced by Jupiter's shrinking due to gravity, and this produces heat. Also, it is still cooling down, losing its initial energy (the energy it received as the Solar System formed).
Methane poses a potentially exciting problem. The gas cannot exist indefinitely in a planet's atmosphere because sunlight breaks it down. That means any atmospheric methane must have a source of replenishment.The most common source of methane is living organisms, which produce it as a byproduct of their metabolism. Cattle, for example, digest the plant material they eat and excrete - through their burps and other means - methane. In fact, cattle excretions account for nearly one-fifth of the methane in Earth's atmosphere - the second-biggest greenhouse gas.