Groundbed Design
For underground structures requiring cathodic protection, the location and nature of the site where the anode is placed needs careful consideration. A low soil resistivity, which would otherwise be classified as a highly corrosive soil, is not the only factor which determines the location of the anode. Other factors to be considered include the presence of foreign metallic structures, accessibility and availability of a power source. The location which is specifically prepared to house a single or a combination of anodes is called a groundbed.
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Impressed anode groundbeds: Once a location is selected and the soil resistivity is determined, the engineer needs to design the type of groundbed and choose anode material and combination. Types of groundbeds are classified as: shallow vertical, shallow horizontal or deep well. Anode materials used for underground impressed current systems are generally graphite or high silicon cast iron. In the groundbed, it is preferred for the anode to be surrounded by a carbonaceous backfill. The backfill particles help to reduce anode resistance to earth, extend anode life by allowing anodic reactions to occur on their surface and provide a porous structure so the gases produced can escape.
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Sacrificial Anode Groundbeds: In certain situations, for example in reducing stray current effects, a sacrificial system may be specified to protect underground structures. The backfill used with these anodes is different from that described for impressed anodes. A typical backfill contains a mixture of clay and gypsum. The function of this chemical backfill to provide conditions favorable to anode dissolution. It also helps to reduce the groundbed resistance. Groundbed resistances can be calculated using the same procedure adopted for impressed current anodes. Individual galvanic anodes in a horizontal groundbed are generally not used. For this type of groundbed a continuous galvanic anode strip is found to be practical. | |||||||
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Remote and Close Groundbeds: Since a groundbed is a source of current, there is a field (potential) gradient associated with it. When the voltage gradient in the soil near the structure is far from the voltage gradient of the groundbed, the groundbed is referred to as remote. However when the voltage gradient in the soil near the structure overlaps with that of the groundbed, the groundbed is referred to as close. This is because the groundbed is near enough to interfere significantly with the field gradient around the structure. |
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