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On the Formation of Nitrogen Oxides During the Combustion of ...

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3 Experiments on Droplet Array <strong>Combustion</strong><br />

vapor and acidic gases such as NO 2 . A constant flow rate <strong>of</strong> 3.0 l min −1 was ensured.<br />

Development <strong>of</strong> <strong>the</strong> analytical methods was done in <strong>the</strong> s<strong>of</strong>tware package<br />

QuantPad (version: 6.1), followed by implementation into <strong>the</strong> s<strong>of</strong>tware<br />

package OMNIC ® (version: 6.1a), both supplied by Thermo Nicolet [435, 436].<br />

<strong>On</strong>e spectral region was regularly selected for <strong>the</strong> determination <strong>of</strong> a particular<br />

component (species). This region had to include portions without significant<br />

absorption, as <strong>the</strong>y built <strong>the</strong> baseline to determine <strong>the</strong> absorbance<br />

A λ (cf. Eq. (3.6)). Fur<strong>the</strong>rmore, each spectral region needed to be subdivided<br />

into different subregions to allocate <strong>the</strong> component-specific bands employed<br />

for spectral analysis. Interference occurring on account <strong>of</strong> cross-sensitivity<br />

additionally increased <strong>the</strong> fragmentation within a spectral region. Crosssensitivity<br />

due to H 2 O and CO 2 renders measurement extremely difficult in<br />

<strong>the</strong> infrared spectrum. It is high for NO, in particular under ambient pressure.<br />

Even though tilted, shifted, and curved baselines are feasible and baseline correction<br />

may be applied by <strong>the</strong> user, it is a disadvantage to have wide-spread<br />

spectral regions and high absorbance A λ <strong>of</strong>, for instance, 0.8 to 1.0. The latter<br />

may occur due to strongly varying levels <strong>of</strong> concentration. If absorption and<br />

hence signal-to-noise ratio (SNR) get too large with an increase <strong>of</strong> concentration,<br />

switching to a different spectral region might deliver better results.<br />

Consequently, more than one spectral region might be required for a single<br />

component under certain circumstances [435–438].<br />

Since light gases, such as NO and CO, absorb rotational energy in addition to<br />

vibrational energy, a polynomial instead <strong>of</strong> a linear curve fit became necessary<br />

for <strong>the</strong> calibration <strong>of</strong> <strong>the</strong>se components. This involved a larger number <strong>of</strong><br />

span gases because <strong>the</strong> number <strong>of</strong> available data points must outnumber <strong>the</strong><br />

polynomial order.<br />

To cover all <strong>the</strong>se effects, both calibration standards (Tabs. 3.7 and 3.8) were<br />

employed in <strong>the</strong> present study on a “competitive” basis, as <strong>the</strong>y represent differing<br />

approaches. Never<strong>the</strong>less, <strong>the</strong>y showed consistent results that were in<br />

good agreement with <strong>the</strong>ory (see Chap. 5). In <strong>the</strong> end, <strong>the</strong> reliability <strong>of</strong> <strong>the</strong> results<br />

depends on <strong>the</strong> maintenance and calibration <strong>of</strong> <strong>the</strong> FT-IR spectrometer,<br />

which is time-consuming in comparison with o<strong>the</strong>r analytical methods, but<br />

<strong>the</strong> analysis time itself is short.<br />

98

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