Oxygen not included iron volcano
Automated volcano system! oxygen not included
This tutorial will go into some of the more obscure aspects of metal volcanoes. The primary aim is to remove useful cool metal, but I try to think of other ways to bring the heat to good use. On a side note, the wiki’s average output does not seem to correspond to actual game numbers.
This is fantastic! I’m using it on a ridiculously good gold volcano (seed 963372579) that’s supposedly 87 percent better than normal. Thanks to this excellent build, I’ve amassed well over 100 trillion dollars in gold with little effort.
– By vacuuming out the volcano, the molten metal liquid is kept contained, allowing it to build up and eventually overflow into the cooling tile area. I had enough natgas in the region for the liquid to solidify into gold bars just underneath the volcano. To get them into the tamer, some manual handling of hot items was needed.
– Flatulent Idiots Must Perish! Instead of training him as an astronaut, I’ve put him in a capsule. I eventually found out why natgas were “spawning” in all of my vacuum/liquid lock regions. I believe this is the worst dupe trait in the game!
Oxygen not included – automated renewable volcano power
Over-pressurization can prevent emission during an eruption. In a Gas, such as Steam, or when its first two layers are completely immersed in a Liquid, such as its own output, the maximum pressure it can release is 150 kg. The tile of interest from which the emission emanates is the exact center tile of the 3 by 3 volcano, which is moved to the left on the 4 tile neutronium base.
At sufficient temperatures, metal volcanoes expel their metals in molten form. While all metal volcanoes have the same eruption times and ejection rates, the metals have different ejection temperatures, freezing points, and basic heat capacities, so a one-size-fits-all approach is unlikely to be wasteful for most volcanoes.
Any geyser, vent, or volcano, in this case, goes through three stages. The active phase, which involves the ejection phase and the idle phase, and the inactive phase. And it’s critical to see it that way, since simply measuring the volcano’s average production over its lifetime will cause equipment to overheat.
The easiest volcano tamer ever! steam turbine cooling
You can see the production of your volcano if you test it. Then, over the course of a complete dormancy period, measure the average mass per second (kg/s) produced. – Look up iron’s heat power. -Multiply the mass per second by the heat power. The effect is the amount of energy required to reduce the iron by one degree. -Multiply by the number of degrees you want to cool, and you’ll get the total amount of energy required. – Your response would be in kDTU/s if you used kg/s for the mass. I believe the aetn has a cooling capacity of just over 80kDTU/s.
Iron, gold and copper volcanoes : tutorial nuggets : oxygen
Molten rock (magma) that has been ejected from the interior of a terrestrial planet (such as Earth) or a moon is referred to as lava. Magma is formed by the planet’s or moon’s internal heat, and it erupts as lava at volcanoes or through cracks in the crust at temperatures varying from 800 to 1,200 °C (1,470 to 2,190 °F). Lava is the term used to describe the volcanic rock that forms after cooling.
A lava flow is a lava outpouring caused by an effusive eruption. Rather than lava flows, explosive eruptions contain tephra, a mixture of volcanic ash and other fragments. Despite the fact that lava is 100,000 times more viscous than water, it will flow for long distances before cooling and solidifying since lava exposed to air forms a solid crust quickly. This helps to hold the remaining molten lava hot and inviscid by insulating it.  The word lava is of Italian origin, and it is most likely derived from the Latin word labes, which means “fall” or “slide.” [two]  It was apparently in a short account published by Francesco Serao on the eruption of Vesuvius in 1737 that the word was first used in connection with extruded magma (molten rock underneath the Earth’s surface).  Serao likened the flood of water and mud down the volcano’s flanks following heavy rain to “a flow of fiery lava.”