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Regional Basic Professional Training Course in Korea

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<strong>Regional</strong> <strong>Basic</strong> <strong>Professional</strong> <strong>Tra<strong>in</strong><strong>in</strong>g</strong> <strong>Course</strong> (BPTC) on Nuclear Safety<br />

• Decrease <strong>in</strong> feedwater temperature;<br />

• Increase <strong>in</strong> feedwater flow;<br />

• Increased ma<strong>in</strong> steam flow;<br />

• Inadvertent open<strong>in</strong>g of a steam generator relief or safety valve<br />

• Steam system pip<strong>in</strong>g failures <strong>in</strong>side and outside conta<strong>in</strong>ment.<br />

Among the events listed above, first four events are AOOs and the last, assum<strong>in</strong>g the<br />

double ended break of the steam l<strong>in</strong>e, is an accident. A typical event sequence of steam<br />

l<strong>in</strong>e breaks is as follows:<br />

A steam l<strong>in</strong>e break causes excess steam release from the secondary system, and<br />

results <strong>in</strong> overcool<strong>in</strong>g of the RCS. In the presence of strong negative MTC, typical<br />

of EOC condition, core power <strong>in</strong>creases to equalize the thermal load caused by the<br />

steam blowdown. To compensate for degraded marg<strong>in</strong>‐to‐DNB, the Reactor<br />

Protection System (RPS) generates a reactor trip, caus<strong>in</strong>g <strong>in</strong>sertion of the control<br />

rods to make core sub‐critical.<br />

Due to the cont<strong>in</strong>ued steam blow‐down through the break from one affected and<br />

other unaffected SGs, early <strong>in</strong> this phase the SG pressure falls below steam l<strong>in</strong>e<br />

isolation signal actuation pressure, and then the path for steam from unaffected SG<br />

to reach the break location is blocked.<br />

When RCS pressure decreases cont<strong>in</strong>uously and reach the setpo<strong>in</strong>t of the Safety<br />

Injection (SI) actuation signal, the boric acid is entered <strong>in</strong>to the RCS, decreas<strong>in</strong>g<br />

the core reactivity. The cool‐down and associated shr<strong>in</strong>kage of RCS fluid is<br />

<strong>in</strong>terrupted after the affected SG blowdown <strong>in</strong>to the conta<strong>in</strong>ment has been<br />

completed.<br />

The RCS energy balance is established where the heat sources (core decay heat,<br />

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