|
Type
|
Journal Article
|
|
Author
|
Wayne R. Smith
|
|
Author
|
Shiladitya Paul
|
|
URL
|
Free Full Text Source: http://www.mdpi.com/2079-6412/5/4/816
|
|
Volume
|
5
|
|
Issue
|
4
|
|
Pages
|
816-829
|
|
Publication
|
Coatings
|
|
Date
|
2015-11-12
|
|
Abstract
|
The calcareous coating formed during cathodic
protection (CP) in seawater reduces current demand by hindering the transport
of species required to support the cathodic reactions and, thereby, improve
the economic performance of CP systems. However, it is unclear as to whether
the coating reduces or enhances hydrogen uptake. To determine this, two sets
of samples were polarized at −1.1 V (standard calomel electrode, SCE) in 3.5%
w/v NaCl and synthetic seawater (ASTM D1141) at 20 °C and the diffusible
hydrogen content measured over a period of 530 h.
Under such conditions reports suggest a deposit with two distinct layers, comprising an initial brucite layer followed by an aragonite layer. Contrary to other findings, a fine initial layer containing Ca and Mg followed by a brucite layer was deposited with a few specks of Ca-containing zones in synthetic seawater. The hydrogen uptake was found to occur within the initial 100 h of exposure in synthetic seawater whilst it continued without the benefit of a deposit coating, i.e., in 3.5 wt % NaCl solution. |
Thursday, January 21, 2016
Natural Deposit Coatings on Steel during Cathodic Protection and Hydrogen Ingress
Natural Deposit Coatings on Steel during Cathodic
Protection and Hydrogen Ingress
Subscribe to:
Post Comments (Atom)
No comments:
Post a Comment