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CO2 Sequestration through Deep Saline Injection and ...

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sun <strong>and</strong> have the characteristic wavelengths less than 300 nm. Visible light spectra account for<br />

45 percent of the energy coming from the solar spectra <strong>and</strong> have the characteristic wavelengths<br />

from 300 to 700 nm. Infrared radiation is the heat component of the solar spectrum <strong>and</strong> accounts<br />

for 54 percent of the energy, with the characteristic wavelengths from 700 to 11,000 nm [39].<br />

3.3.2. Solar Irradiance<br />

The design of a solar collection <strong>and</strong> transmission system requires an estimation of how much<br />

energy is delivered by the sun to the location at which the system will be located. The rate at<br />

which solar energy reaches a unit area at the earth is called the solar irradiance <strong>and</strong> is typically<br />

measured in watts per square meter (W/m 2 ). This solar irradiance is not constant <strong>through</strong>out the<br />

day. To design a solar collection system a designer must know the average solar energy density.<br />

The typical units of measure are watt-hours per square meter (Wh/m 2 ). The power released from<br />

the sun reaches the outer layer of the earth’s atmosphere at 1367 W/m 2 (known as the<br />

extraterrestrial solar constant (SC)) where it then undergoes additional losses due to atmospheric<br />

particles such as water molecules, ozone, <strong>and</strong> dust. The actual amount of solar power received at<br />

the earth’s surface can vary greatly depending on the amount of matter encountered in the<br />

atmosphere, <strong>and</strong> can range from 90 percent, of the SC on a very clear day to around 30 percent<br />

on a very cloudy day [33]. Since the actual solar irradiation can vary so much over the course of<br />

the year it is best to view the solar irradiation as an average over the course of the year. Figure<br />

13 provides an average daily solar irradiation for the entire United States that can be used to<br />

estimate the solar irradiance at a particular location in the United States.<br />

The location of the PBR is intended to be in the southwest United States <strong>and</strong> will have an<br />

average solar irradiance of 7.0 – 8.0 kWh/m 2 /day. If the system were to be located in Alberta,<br />

Canada for example, then the average solar-irradiance would decrease to 3.0 – 4.0 kWh/m 2 /day<br />

[40]. In the later case, implementation of a solar collecting system does not make sense <strong>and</strong> was<br />

not considered. To design the solar collecting system for the PBR an average value of 8.0<br />

kWh/m 2 /day was assumed in the calculations of required collector surface area, see Appendix C<br />

for detailed procedure of calculating collector surface area.<br />

24

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