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various build<strong>in</strong>g materials at <strong>the</strong> <strong>University</strong> <strong>of</strong><br />

<strong>Plymouth</strong>, <strong>in</strong> <strong>the</strong>rmally controlled, labora<strong>to</strong>ry<br />

conditions (Goodhew and Griffiths, 2004,2005).<br />

Three unknowns exist <strong>in</strong> <strong>the</strong> established equation<br />

(4) that represents <strong>the</strong> heat<strong>in</strong>g curve <strong>of</strong> <strong>the</strong> probe<br />

dur<strong>in</strong>g a measurement cycle: <strong>the</strong>rmal conductivity<br />

(; ý); <strong>the</strong>rmal diffusivity (a); and a property with<br />

notation H, which has not been def<strong>in</strong>ed absolutely<br />

Figure 2: A Hukseflux<br />

but is usually taken <strong>to</strong> denote <strong>the</strong> reciprocal <strong>of</strong><br />

TP08 <strong>the</strong>rmal probe<br />

contact resistance between <strong>the</strong> probe and sample<br />

material, sometimes termed probe conductance. Fur<strong>the</strong>r explanation <strong>of</strong><br />

equation (4) is given <strong>in</strong> chapter 2, <strong>the</strong> literature review, <strong>in</strong>dexed <strong>the</strong>re <strong>in</strong> two<br />

forms as equations (7) and (14), and <strong>in</strong> a fur<strong>the</strong>r form <strong>in</strong> chapter 4, <strong>in</strong>dexed<br />

<strong>the</strong>re as equation (33).<br />

2A<br />

lný 4a. t<br />

7+ +r lný 4a. 1 a. MPC 4a. 1<br />

AT -- In<br />

22Y+I-2P 2<br />

Y+<br />

2A<br />

ýJ+Oýr<br />

4, TA rrH 2a. 1 r )r. r rrHa. t<br />

2<br />

Equation (4)<br />

Apart from <strong>the</strong>se three unknowns <strong>in</strong> equation (4), many o<strong>the</strong>r unknowns were<br />

foreseen <strong>in</strong> tak<strong>in</strong>g forward <strong>the</strong> previous labora<strong>to</strong>ry work, regard<strong>in</strong>g <strong>the</strong> practical<br />

application<br />

<strong>of</strong> <strong>the</strong> <strong>the</strong>rmal probe approach. These <strong>in</strong>cluded: <strong>the</strong> effect <strong>of</strong><br />

reduced contact between <strong>the</strong> probe and sample with <strong>the</strong> vary<strong>in</strong>g hole diameters<br />

envisaged when drill<strong>in</strong>g coarse materials; <strong>the</strong> effects <strong>of</strong> different fillers used <strong>to</strong><br />

improve contact; lack <strong>of</strong> or <strong>in</strong>complete fillers; and whe<strong>the</strong>r heat from <strong>the</strong> hole<br />

drill<strong>in</strong>g process or heat<strong>in</strong>g cycles would cause sufficient moisture migration,<br />

10

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