Joules/minute to Terawatt

When the experiment naturally operates on a minute timescale. A bomb calorimeter measuring heat of combustion might collect data over 5–10 minutes, making J/min the natural rate unit. Reporting 350 J/min is more meaningful in context than 5.83 W, because the researcher thinks in minutes. It's the same reason we say "km per hour" for driving rather than "meters per second" — matching the unit to the human timescale of the observation.

Divide by 60. Since 1 W = 1 J/s and there are 60 seconds per minute, 60 J/min = 1 W. So 6,000 J/min = 100 W. For a quick mental approximation, drop two zeros and add two-thirds: 6,000 → 60 + 40 = 100 W. Going the other direction, multiply watts by 60: a 100 W bulb = 6,000 J/min. It's one of the easier unit conversions because 60 is such a clean number.

Cellular respiration rates in isolated mitochondria, enzyme reaction kinetics (heat of reaction per minute), metabolic rates of small organisms in respirometry chambers, and wound healing energy expenditure. A mouse in a calorimetry chamber might produce 200–400 J/min of heat. Plant leaf photosynthesis absorbs roughly 5–20 J/min of light energy per leaf. The minute timescale matches typical biological measurement intervals.

A standard candle releases about 5,000 J/min (roughly 80 W) of total thermal power, of which only about 600 J/min (10 W) is visible light — the rest is infrared radiation and hot convection gases. The candle burns paraffin at about 0.1 g/min, and each gram of paraffin contains roughly 46,000 J. That's why a single candle can meaningfully warm a small enclosed space.

Rarely, but it shows up in slow curing processes (epoxy heat generation during setting), low-temperature drying rates, and pharmaceutical dissolution testing where drug release rates are tracked per minute. Some food science labs measure heat of mixing or fermentation rates in J/min. In most industrial contexts, watts or kW are preferred — but when a process engineer times everything in minutes, J/min avoids constant ÷60 conversions in their spreadsheets.

The Sun delivers about 173,000 TW to Earth's surface. Human civilisation uses roughly 18 TW total. So we'd only need to capture 0.01% of incoming solar energy to power everything — an area of solar panels roughly 400 km × 400 km, about the size of Montana. The challenge isn't total energy availability; it's cost, storage, transmission, and the fact that sunlight is spread thin and intermittent.

Imagine 18 trillion light bulbs burning continuously, or 9 billion people each running a 2 kW heater non-stop. That 18 TW figure includes everything — electricity, transport fuel, industrial heat, cooking, heating. About 40% comes from oil, 27% from coal, 24% from gas, and the rest from nuclear and renewables. The US alone accounts for about 3 TW despite having only 4% of world population.

Replacing all 18 TW of human energy with clean sources would require roughly 60–75 TW of installed solar capacity (accounting for ~25% average capacity factor). That's about 40 times current installed solar. At 2023 installation rates of ~0.4 TW/year, it would take 150 years — but installation rates are doubling every 2–3 years. If that exponential trend holds, we could theoretically reach 60 TW of solar within 15–20 years.

Earth radiates about 47 TW of geothermal heat from its interior, driven by radioactive decay and residual primordial heat. That's 2.5× human energy consumption, but it's spread across the entire surface at extremely low density (~0.09 W/m²). Iceland, sitting atop a mantle plume, exploits geothermal for 90% of its heating. Globally, geothermal electricity capacity is only about 16 GW — a tiny fraction of what's theoretically available.

No — the terawatt scale is a very recent phenomenon. In 1800, global human power consumption was about 0.5 TW (mostly biomass burning). By 1900 it reached 1 TW with coal industrialisation. We crossed 10 TW around 1985. The jump from 1 to 18 TW in just 120 years tracks almost perfectly with global population growth times rising per-capita energy use. Pre-industrial humans used about 0.1 kW each; Americans now average 10 kW per person.