• Natanael@slrpnk.net
    link
    fedilink
    arrow-up
    5
    ·
    edit-2
    1 year ago

    Heat capacity of lava per degree Celsius per unit of mass

    Multiplied by temperature differential vs ambient, multiplied by mass = total extra heat energy

    Then you calculate the sum of heat capacity multiplied by mass for lava and for water, and calculate from that how many degrees above ambient the two masses will land at when combined as the extra energy above is divided over both (assuming water starts at ambient temp)

    It won’t be exact because heat capacity varies in materials as temperature changes, both steam and solidification of lava (state change) will contribute significantly, but it’s a decent first estimate

    • Eheran@lemmy.world
      link
      fedilink
      arrow-up
      1
      ·
      1 year ago

      Okay. Then they add more and it will boil quickly. I guess the question boiles (huehue) down to how much water you can turn into stream per amount of lava or the inverse, how much lava you can cool down per amount of water.

      The phase change from liquid water to stream will, by the way, not just contribute significantly but be by far the majority of energy needed. Simply heating water up, ignoring the phase change and changes of the heat capacity, with the same energy as it takes to go from liquid to gas (2257 kJ/kg) would result in a temperature rise of… dT = 2257 kJ/kg / 4.2 kJ/(kg*K) = 537 K

      • Natanael@slrpnk.net
        link
        fedilink
        arrow-up
        1
        ·
        1 year ago

        Assuming enough water that most of it doesn’t boil, then my math would still check out, but yeah, any substantial amount of boiling forces you do do the math in multiple steps to handle that