Carbon dioxide (CO2) is commonly found dissolved in hydrothermal fluids and could be released from pore water when cores are recovered. CO2 is usually considered inert and is heavier than air (1.5 times), concentrating in low areas of quiet air.
Carbon dioxide gas is toxic in higher concentrations but much less so than H2S (see Table AT2). The threshold limit of CO2 is 5000 ppm. Short-term exposure to 50,000 ppm (5%) is reasonable. This gas is colorless and odorless and can be tolerated in relatively high concentration.
Air containing 5% CO2 will cause disorientation in a few minutes. Continued exposure to CO2 after being affected will cause convulsions, coma, and respiratory failure. If a massive flow of CO2 from the well bore should occur (highly unlikely), the principal danger would be from asphyxiation due to lack of air.
Using a BA will provide adequate oxygen until the emergency can be controlled.
Common
name |
Chemical
formula |
Specific gravity
(air = 1) |
Threshold* limit
(ppm) |
Hazardous†
limit (ppm/hr) |
Lethal‡ concentration
(ppm) |
Hydrogen cyanide | HCN | 0.94 | 10 | 150 | 300 |
Hydrogen sulfide | H2S | 1.18 | 10 | 250 | 600 |
Sulfur dioxide | SO2 | 2.21 | 2 | — | 1,000 |
Chlorine | Cl2 | 2.45 | 1 | 4 | 1,000 |
Carbon monoxide | CO | 0.97 | 50 | 400 | 1,000 |
Carbon dioxide | CO2 | 1.52 | 5,000 | 5% | 100,000 |
Methane | CH4 | 0.55 | 90,000 | >5% in air | — |
Notes: * = concentration at which it is believed that all workers may repeatedly be exposed, 8 hr/day, every day, without adverse effect. † = concentration that may cause death. ‡ = concentration that will cause death with short-term exposure.
Hydrocarbon compounds are known to be present in sediments and potentially in hydrothermal fluids. These hydrocarbons are primarily in the form of methane gas, but some heavier gases and even liquids are possible.
The toxicity of methane is very low (see Table AT2), but it is often a "carrier" of H2S. Because hydrocarbon gas is lighter than air, it does not tend to settle and is easily dispersed. The major threat from natural gas is its extreme flammability and explosivity. Hydrocarbon liquids may be carcinogenic, so common sense should be used in handling them if they are encountered.
The blowout control measures specified in this document can be use to control hydrocarbon gas as well as H2S.
The barite precipitated in seafloor rocks and sediments by hydrothermal activity has been found to contain measurable amounts of radioactive radium-226, which is chemically similar to barium. Small amounts of radon may also be present in the pore water.
The radium emits very small amounts of radon-222 gas through radioactive decay, which also is radioactive. The radiation is in the form of alpha particles, which have extremely limited ability to penetrate tissue. Thus, the principal danger comes from inhaling or ingesting the radioactive material. Furthermore, the levels of radioactivity are extremely low—on the nannocurie scale.
ODP has investigated the potential effect of that radiation on health and safety on board the ship. Nevertheless, cores will be monitored for radioactivity if radioactive material is present.
The following precautions are to be taken if radon is encountered:
Sulfur dioxide is produced during the burning of H2S. Sulfur dioxide is colorless, transparent, nonflammable, heavier than air, but will be picked up by a breeze and carried downwind at elevated temperatures, and extremely irritating to the eyes and mucous membranes of the upper respiratory tract.
Table AT3 indicates the toxic nature of the gas.
Concentration of SO2
|
Effect
|
|
(%)
|
(ppm)
|
|
0.0002 | 2 | Safe for 8 hr |
0.005 | 3–5 | Pungent odor; normally a person can detect SO2 in this range |
0.0012 | 12 | Throat irritation, coughing, chest constriction, eyes tear and burn |
0.015 | 150 | So irritating that it can only be endured for a few minutes |
0.05 | 500 | Causes a sense of suffocation, even with first breath. |