Wind power

Winds are generated by uneven heating of the earth’s atmosphere by the sun, which causes hotter, less dense air to rise and more dense, colder air to be pulled into replace it.  Of course, land masses, water evaporation over oceans, and the rotation of the earth amongst other things added to the complexity of weather systems.  However, essentially weather systems are driven by natural convection, a form of heat or energy transfer, as I hinted in my recent post entitled ‘On the beach’ [24th July, 2013].

If you are thinking of building a wind turbine to extract some of the energy present in the wind, then you would be well-advised to conduct some surveys of the site to assess the potential power output.  The power output of a wind turbine [P] can be defined as a half of the product of the air density [d] multiplied by the area swept by the blades [A] multiplied by the cube of the velocity [v].  So the wind velocity dominates this relationship [P = ½dAv3] and it is important that a site survey assesses the wind velocity.  But the wind velocity is constantly changing so how can this be done meaningfully?

Engineers might tackle this problem by measuring the wind speed for ten minute intervals, or some other relatively short time period, and calculating the average speed for the period.  This process would be repeated over a long period of time, perhaps weeks or months and the results plotted as frequency distribution, i.e. the results would be assigned to ‘bins’ labelled for instance 0.0 to 1.9 m/s, 2.0 to 3.9 m/s, 4.0 to 5.9 m/s etc and then the number of results in each bin plotted to create a bar chart.  The number of results in a bin divided by the total number of results provides the probability that a measurement taken at any random moment would yield a wind speed that would be assigned to that bin.  Consequently, the mathematical function used to describe such a bar chart is called a probability density function.  Now returning to the original relationship, P = ½dAv3 and using the probability density function instead of the wind velocity yields a power density function that can be used to predict the annual output of the turbine taking account of the constantly changing wind velocity.

If you struggled with my very short explanation of probability density functions, then you might try the Khan Academy video on the topic found on Youtube at http://www.youtube.com/watch?v=Fvi9A_tEmXQ

Engineers use probability density functions to process information about lots of random or stochastic events such as forces ocean waves interacting with ships and oil-rigs, flutter in aircraft wings, the forces experienced by a car as its wheels bounce along a road or the motion of an artificial heart valve.  These are all activities for which the underlying mechanics are understood but there is an element of randomness in their behaviour, with respect to time, that means we cannot predict precisely what will be happening at an instant in time; and yet engineers are expected to achieve reliable performance in designs which will encounter stochastic events.  Frequency distributions and probability density functions are one popular approach used by engineers.  Traditionally engineers have studied applied mathematics that was equated to mechanics in high school but increasing they need to understand statistics.

Water, water, everywhere

Wood engraving illustration of the Ancient Mariner by Gustave Dore

Wood engraving illustration of the Ancient Mariner by Gustave Dore

Water, water, every where,
And all the boards did shrink;
Water, water, every where,
Nor any drop to drink.

These lines are from the Rime of the Ancient Mariner by Samuel Taylor Coleridge published in 1798.  They were brought to my mind when I was looking at the data in the GIO report on ‘Water’ that I mentioned in my post entitled ‘Closed system: water’ [17th July, 2013].

The quantity of water used to produce some everyday familiar items is staggering, for instance 140 liters to make one cup of coffee [growing the beans, harvesting, transporting and processing them], or 1,300 litres for a kilogram of wheat resulting in 40 litres per slice of bread but that is tiny compared to 1800 litres for a 4oz beef burger.  You might be reading this in a part of the world that is constantly, or at least frequently, deluged with rain and so be thinking that none of this matters, except that much of what you consumes probably comes from a part of the world where water is less readily available and massive civil engineering projects are required to ensure an adequate supply, which have enormous ecological consequences.

And that pair of jeans you are probably wearing, well, they required 10,855 litres of water!

Click to access ibm_gio_water_report.pdf

On the beach

beachMaybe you are lying on the beach reading this, or if not dreaming about lying on the beach.  We enjoy lying on the beach, or next to a swimming pool, in part because it involves doing nothing and in part because of the heat transfer.  Heat transfer is transfer of energy from a high to a lower temperature zone.  It can occur in four ways: conduction, free convection, forced convection and radiation; and all of them occur on the beach on a hot day.

Conduction occurs as a flow of kinetic energy from one molecule to the next by direct contact.  When you are lying on the beach it occurs between you and the surface that you are lying on.  When you first lie down on hot sand, then the energy flows from the hot sand to your cooler body by conduction.

Free or natural convection is heat transfer carried by a rising current of fluid due to buoyancy effects created by the hotter fluid being less dense.  This tends to happen above your warm body after you have been lying in the sun for a while.  It also happens above the hot sand and you can sometimes see a heat haze caused by the rising hot air that has a lower density and thus different refractive index compared to the surrounding air.

Forced convection also involves heat transfer by a moving current of fluid but in this case the flow is caused by an external source.  So if there is breeze across the beach then you will be cooled by forced convection as you lie on the beach.

Radiation consists of electromagnetic waves in the infrared spectrum travelling away from a source in all directions.  This is the heat from the sun that makes it so pleasant to lie on the beach on a sunny day.

Ok, shut your eyes and go back to sleep.  The heat transfer lesson is over – though some of you might want to think about whether that breeze is really forced convection since it is probably caused by natural convection on a climatic scale.

Closed system: water

gio_waterSometime ago I wrote about the need to consider the planet as a closed system, i.e. a system to which no new mass is being added, other than the occasional meteor from space [see my posts ‘Closed systems in nature?’ and ‘Open-world mind-set’ on December 21st, 2012 and January 4th, 2013, respectively].  This closed system approach applies to water.  The total amount of water on the planet does not change and it has been moving around the hydrologic cycle for thousands of years.  Mankind interacts with this cycle changing the chemistry, usefulness and availability of water.  All of us contribute to these changes in a small way but 6.5 billion of us make a big impact.

Most of us are aware of pollution to rivers and groundwater caused by use of fertilizers and pesticides.  We are perhaps less aware that removing groundwater for irrigation, industrial processes and domestic consumption can reduce water pressure underground in coastal regions causing saltwater to percolate and mix with freshwater reserves.  Or that discharges from desalination plants increases the local salinity of seawater while carbon emissions in the atmosphere is sequestered by the oceans raising water acidity levels.  All of these effects can damage ecosystems.

80% of available freshwater resources in the world are used to grow food.  Yet, we also need it in huge quantities for industrial processes, for instance it requires 10 litres of water to make a sheet of paper and 200 litres to make one kilogram of plastic.  Just as in energy consumption, there are huge global variations in daily domestic consumption per capita from 778 litres in Canada, 139 litres in the UK and India to 95 litres in China.

So, in addition to thinking about energy consumption when designing products and services, engineers need to think about water requirements since although there is a renewable supply it is not  infinite or even constant.

The data above was taken from ‘Water: A Global Innovation Outlook Report’ available at http://www.ibm.com/ibm/gio/media/pdf/ibm_gio_water_report.pdf