PubMed · 3272646
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P O Granberg. 1988. Cold injuries.. https://pubmed.ncbi.nlm.nih.gov/3272646/
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Methyl chloride (CH3Cl), the most abundant halocarbon in the atmosphere, has received much attention as a natural source of chlorine atoms in the stratosphere. The annual global flux of CH3Cl has been estimated to be around 3.5 Tg on the grounds that this must balance the loss through reaction with OH radicals (which gives a lifetime for atmospheric CH3Cl of 1.5 yr). The most likely main source of methyl chloride has been thought to be oceanic emission, with biomass burning the second largest source. But recent seawater measurements indicate that oceanic fluxes cannot account for more than 12% of the estimated global flux of CH3Cl, raising the question of where the remainder comes from. Here we report evidence of significant CH3Cl emission from warm coastal land, particularly from tropical islands. This conclusion is based on a global monitoring study and spot measurements, which show enhancement of atmospheric CH3Cl in the tropics, a close correlation between CH3Cl concentrations and those of biogenic compounds emitted by terrestrial plants, and OH-linked seasonality of CH3Cl concentrations in middle and high latitudes. A strong, equatorially located source of this nature would explain why the distribution of CH3Cl is uniform between the Northern and Southern hemispheres, despite their differences in ocean and land area.
Discharges of 99Tc and 129I from the reprocessing plant at Sellafield have increased significantly since the mid-1990s, against the overall trend of most other radionuclides. The 'pulsed' release of 99Tc has provided an opportunity to study transport pathways and transit times in UK waters, the North Sea and beyond. Transit times estimated from the 99Tc data are signifcantly shorter than rates reported previously using other radiotracers. The possible reasons for this are discussed. A comparison is made between the response of seawater concentrations and those in the brown seaweed Fucus vesiculosus to variations in the release rates. Current discharges of plutonium are very low compared with the 1970s and 1980s. However, the seabed sediments of the Irish Sea represent a substantial source and remobilisation into the water column results in the continuing export of plutonium from the Irish Sea and its transport to Arctic waters.