DEEP WATER CATHODIC PROTECTION: Laboratory Simulation Experiments

摘要

Experiments were performed where steel specimens were cathodically polarized in natural sea water by galvanic coupling through an external resistor to an aluminum anode. Temperature was either ambient or 5 deg C; and pressure was atmospheric or 8.96 +- 0.14 MPa (1,300 +- 20 psi), which is equivalent to a water depth of 899 m (2,950 feet). For some experiments, dissolved oxygen concentration was controlled at 5.5 +- 0.2 mg/l and pH was 7.8. These corresponded to values that were measured at the above depth for a specific Gulf of Mexico site. The apparent steady-state potential (phi_c) and current density (i_c) for the different experiments were compared with previously reported ambient temperature and pressure data. Calcareous deposits that formed on specimens from each of the test categories were viewed and analyzed. The long-term phi_c-i_c trend for the different tests was the same at the two pressures and for 5.5 compared to 9 mg/l O_2. Also, i_c was independent of phi_c over the potential range investigated (approximately --0.80 to -1.10 V_(SCE)) despite differences in the calcareous deposit structure and composition. The results are discussed in terms of, first, design criteria for deep water cathodic protection and, second, experimental testing to develop such criteria.