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how can 30,000 kg of snow at 0 C have more heat energy than 1 mL of water at 100 C?
The discussion explores the concept of heat energy in relation to mass, specifically comparing the heat energy of a large mass of snow at 0°C to a small volume of water at 100°C. The focus includes theoretical considerations of heat content and temperature measurement.
Participants present differing views on the comparison of heat energy between the two samples, with some providing calculations to support their claims. There is no consensus reached on the implications of these comparisons.
The discussion includes assumptions about the specific heat capacities and the calculations depend on the definitions of heat content and temperature scales. There are unresolved aspects regarding the implications of these calculations in practical terms.
This discussion may be of interest to those studying thermodynamics, heat transfer, or related fields in physics and engineering.
