Burning Buried Sunshine (2003)
plus.maths.org
plus.maths.org
Wow, and this is a lower bound because it doesn't even consider manufacturing and distribution.
My cognitive dissonance at the gas station is approaching an all-time high.
Soybeans are a common way of capturing carbon from the atmosphere, using solar energy, to produce diesel.
I meant freshwater cycle time.
Yes there are certainly places that run out of water, I meant more places like Vancouver where the city just doesn’t build a bigger reservoir and instead bemoans an annual water shortage.
At the risk of a major digression, one sees this constantly in discussions of inequality where net personal wealth or market capitalisation (both stocks) are compared to income or GDP (both flows).
(And at the risk of digressing my own digression, economists aren't even settled on whether wealth is a stock or a flow. Adam Smith's definition is the latter.)
With water, there is is a throughput in a given region. That flow is not uniformly available, and varies with time (further complications). It serves processes and consumers (in both economic and ecological senses), and changes to those flows and availability do have major impacts (whether surpluses or shortages).
There are times when the critical need is getting rid of excess water (via dikes, pumps, and other control structures), others when the critical need is obtaining or preserving water (again: via pumps, reservoirs, cisterns, etc.). The total demand, flow, and impact are high enough that even modest deviations from normal experience or expectations are often devastating --- floods, droughts, and the like.
Transporting water more than a few km / miles is tremendously expensive and typically requires major public infrastructure. It's best moved under gravity flow alone.
If the litre of water you have used comes from an excess, there is no issue. If it won't be replaced for a year, it's the last litre available, and the nearest additional litre is 100km away ... you may be having a problem.
As far as I know it costs about the same as any other good to transport in small volumes and is incredibly cheap to transport in larger volumes, on par with oil.
I do tend to agree with you tho that if you want government to transport it, it gets ridiculous as one would expect from tasking government to do something nature does for free, and the private sector does extremely efficiently.
It's not the unit volume cost, it's the total cost.
The United States consumes about 20 million barrels of oil per day. That's about 840 million gallons.
Water consumption is 322 billion gallons/day, 380 times more. That's about a thousand gallons per person per day.
Note that this isn't individual direct consumption (drinking, cleaning, bathing), but the net total use. If you're looking at replacing all city consumption (residential, commercial, industrial) plus agrigulture, you'd be moving these volumes of water. Even at pennies per gallon, the costs add up.
Keep in mind that the watershed for major Western US cities already extends over hundreds to thousands of miles. A chief reason that the Western US looks far more like an island archipelligo than the richly-settled East is because of water scarcity and prior claims.
https://upload.wikimedia.org/wikipedia/en/4/48/Earthlights_d...
San Francisco (and much of the Penninsula) draws water from the Hetch Hetchy Reservoir, 180 miles east. Los Angeles draws much of its water from the California Aqueduct, streching over 500 miles north, and the Colorado River, whose watershed extends to the eastern front of the Rocky Mountains, 1,500 miles to the east. Both delivery systems operate virtually entirely under gravity flow.
The California aqueduct has exceptions --- there are pumping stations in the Delta which provide a few metres of lift, and the Edmunston Pumping Plant which lifts water over the Tehachapi mountains utilises 14 * 80,000 horsepower pumps (835 combined MW) to provide 600m (1,926 feet) of lift to 2 million gallons/minute (7.5 million litres/minute), 7,500 tonnes of water per minute --- roughly the capacity of the Oroville Dam spillway at peak capacity, for comparison. It has its own dedicated 1 GW capacity generating plant.
Note that when the Oroville reservoir is discharging water it is generating electricity. What you gain in shipping Oroville water you lose shipping Tehachapi water. The opportunity cost is not 835 MW, but 1,670 MW. At retail California rates, that's nearly $200,000 per hour of operation, $4.6 million per day, $1.7 billion/year, to move water 750 km across land and 600 m high ... and that's only considering the Edmunston plant itself (there are numerous other pump stations in the system as a whole).
The California Department of Water Resources annual budget is about a billon dollars (there's considerable variation).
So long as you want to use / access water where it's flowing already, costs are low. Major river systems (the Mississippi-Missouri-Ohio-Red river system in the US is among the largest in the world) provide just that.
But when you start wanting to move water laterally, or worse, through or over mountains, costs increase tremendously.
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References:
US petroleum use: https://www.eia.gov/todayinenergy/detail.php?id=44556
US water use: https://www.usgs.gov/mission-areas/water-resources/science/w...
Edmunston Plant: https://en.wikipedia.org/wiki/Edmonston_Pumping_Plant
Oroville Dam: https://en.wikipedia.org/wiki/Oroville_Dam_crisis
California Aqueduct: https://en.wikipedia.org/wiki/California_Aqueduct
CA DWR budget: https://lao.ca.gov/Publications/Report/4103
https://www-legacy.dge.carnegiescience.edu/DGE/Dukes/Dukes_C...
I'd stumbled across this through my own research, trying to find literature with a detailed description of fossil-fuel formation. I've since found it referenced by numerous other works --- yes, one of my forms of entertainment is looking for familiar citations amongst footnotes. Smil's Energy and Civilization being one work citing Dukes.
It's not just the material conversion that's staggering, there's the time of accumulation. For petroleum, humans burn in one year a quantity which took five million years to accumulate.
The correct number would be closer to 3.54 tonnes of plant material. The other 18.91 tonnes aren't spent. They are instead fully recycled and re-enter in the system (or go away out of the oil processing chain).
A better intuition is this: plants, etc. used energy to create two products, oxygen (which went into the atmosphere) and hydrocarbons (buried in the ground). When we recombine them and add heat, we reconfigure some bonds and release energy in the oxygen bond. The hydrocarbons act as a “sponge” for the oxygen atoms, and the denser the sponge the more energy we can release.
If it was the oxygen buried underground we would probably call it “fuel”!
I read a proposal to send an aircraft to Titan and bring along oxygen as the energy source to burn with the methane in the atmosphere. (It works… sort of. In a methane and oxygen stoichiometric reaction, the oxygen is 4/5ths the mass so it’s not nearly as good of a deal as it is on Earth.)
It truly doesn't matter which one you consider it to be, given that both are technically incorrect.
> The energy is in them being split apart.
This is a common misconception (likely) perpetuated by highschool chemistry textbooks. The energy is actually release by the combination of oxygen with hydrogen and carbon. Let me explain.
It takes energy to break chemical bonds. Some bonds take more energy to break, others take less. When a bond is created, an amount of energey (roughly) equal to the energy require to create the bond is released.
Here I will demonstrate the combustion of a simple hydrocarbon:
CH4 + 2 O2 -> CO2 + 2 H2O
When this reaction takes place, there is not energy "stored" in either the Carbon-Hydrogen bonds or the Oxygen-Oxygen bonds that is "given off". Rather, energy is actually required to break the bonds. It goes something like this:
CH4 + 2 O2 + (a little bit of energy) -> CO2 + 2 H2O + (a lot of energy).
Making hydrocarbons (or hydrogen from water) is an energy intensive process because breaking the bonds in CO2 and H2O requires a lot of energy.
The products on the right side sit at a lower energy level (they hold together “tighter”) overall. On the left, O2 needs less energy to break up while CH4 needs more, so in that sense the energy “comes” from O2 being easier to break apart. Conceptually I imagine these as a bunch of magnets with the two “magnets” in O2 held at a larger gap (so easier to take apart). With a jolt, things reconfigure and snap into a tighter pattern, and there’s an overall energy release.
The paper on which this article is based directly addresses that:
Marine sediments produced the majority (about 86%) of the world’s petroleum, while deltaic and lacustrine sediments yielded smaller amounts (about 11% and 3%, respectively) (Demaison, 1993). The organic matter in carbon-rich marine sediments is primarily composed of the remains of phytoplankton. The percentage of annually fixed organic carbon that accumulates in sediment (the PF) is difficult to estimate because it can vary over several orders of magnitude, depending on the length of time that organic matter experiences oxic conditions, and on other factors (Bralower and Thierstein, 1987; Bordenave, 1993; Canfield, 1994; Gélinas et al., 2001). Two types of marine settings are thought to have been the major environments for the formation of petroleum source rocks: silled basins with oxygen-deficient waters, and highly productive upwelling zones (which generated 78% and 8% of world petroleum stocks, respectively; Demaison, 1993).
https://www-legacy.dge.carnegiescience.edu/DGE/Dukes/Dukes_C...
Surely plants are majority water by mass? A quick google claims 89-90% water[1]
1: https://www.toppr.com/ask/question/the-percentage-of-water-i...