VivB said:
But the suprising bit was that bomb testing and nuclear energy production supposedly contributed "too little to meter" , or less than one %. I don't know if I believe it one bit, but that's what I wrote on my exam paper, and I didn't fail!
Atmospheric-borne radon seems to be at quite a high level. It is commonly suggested that the 'source' is contaminated rock and soil. However, why is it that just the first few inches of soil is supposed to carry the radon gas-emitting particles? The depth of penetration of rainwater could provide an alternative explanation here.
In studying the radon results from Agen Allwedd and Eglwys Faen, as published in the latest issue of 'Descent' (No. 203) for August/September 2008, what is striking is the difference in levels between the two caves. The plausible-sounding explanation given is: "The theory runs that relatively small caves with many entrances probably have low radon concentrations: radon is heavier than air and can collect in low-flow areas, while the ingress of fresh air will dilute it . . . Eglwys Faen is a relatively small, dry and ungated cave with several large entrances which should allow unrestricted airflow through much of the outer regions, particularly as there are several circular connections."
However, when you understand the make-up of the Llangattock cave system(s) you start to see the flaws in the 'big cave'/'little cave' hypothesis. The entrances to Eglwys Faen are not that large, it is the size of the Main Chamber in close proximity to the surface which gives rise to this misconception. The strong draughts in the system are mirrored by almost equally strong draughts in the Agen Allwedd/Ogof Gam Entrance Series (two separate entrances). So, therefore, according to this hypothesis one would expect readings taken in the nearer sections of the Agen Allwedd Entrance Series, at a similar point in time, to match those of Eglwys Faen, but they do not: the readings are appreciably higher in Agen Allwedd - in the Entrance Series they are, in fact, almost double those of the Main Chamber in Eglwys Faen.
A solution for the Agen Allwedd results appears to be at hand: "The high concentrations recorded in the cave suggest that during the duration of the experiment the airflow was predominantly outwards, bringing air laden with radon towards the entrance." However, the 25 readings carried out for this report are implied to have been taken in both caves simultaneously, between 19 September and 27 October 2007. The draught in Eglwys Faen is not driven by the few relatively small surface entrances being located in close proximity to each other, but by their connection with a large deep-mountain cave system - the Mynydd Llangattwg Cave System - currently inaccessible to cavers and located somewhere beyond the present various end boulder chokes of the cave. So, if a strong outwards cave draught were to be responsible for the high levels of radon detected in the Agen Allwedd Entrance Series, bringing the gas from deeper within the system, then exactly the same effect should also be experienced in Eglwys Faen (eg. in The Warren east passages where the draught has not yet diverged to depart from one of the cave's various entrances), but it is not - the levels throughout the cave are lower than those found in Agen Allwedd. Yet the Llangattock cave draughts act in unison, from one separately-named cave system to another, according to temperature and barometric variations between the surface and underground.
So, the next culprit could be determined to be the limestone strata, except both Agen Allwedd and Eglwys Faen are situated in the same bed of Blaen Onneu Oolite . . .
The only difference of any significance between the two caves is the presence or otherwise of running water. In Agen Allwedd you immediately enter a sizeable stream passage where the water has only had a minimal passage through the overlying strata before entering the cave. Direct rainfall from air to ground to cave has taken place. The small surface stream which enters Eglwys Faen can be seen trickling down the mountainside and falling as a waterfall before it enters the Eastern Series. Tumbling water is one way to cause unwanted gasses and particles to be expelled - look at water treatment plants. There are other very small streams inside Eglwys Faen, but they carry nothing like the quantity of water which is found flowing in the Main Stream Passage of Agen Allwedd - in proximity to which a good number of the radon measurements have been taken and the largest readings obtained. Streams also run from the Ace of Spades Inlet, past the edge of the Music Hall and along the inner end of Trident Passage. Another stream runs beneath the floor of the mouth of Southern Stream Passage - originating from Northern Stream Passage. All carry appreciably more water than that found flowing in Eglwys Faen.
So, for future tests, it would be interesting to see a greater mix of sites ranging between not only the current active stream passages but also inside the old high-level fossil chambers and tunnels, such as in Erse Passage and Midnight Passage.
Having argued the contention that rainwater is bringing a significant quantity of radon into caves, I will accept that high levels of radon in the atmosphere could result from more than a single source. It is certainly naturally present in (man-made) uranium mines. Accepted 'wisdom' appears to discount nuclear experimentation as providing "too little to meter" (but I do not think power stations should be included here, given these perform properly according to design and that waste matter from the reactors is contained and disposed of in a controlled fashion). In addition radon is not listed as emanating from cosmic radiation, but one article I have read suggests that radon is also present on Mars! Does ozone depletion have an effect here? Since there appears to be so much radon around in the atmosphere a re-evaluation of all its potential sources would be useful.
Radon gas appears to be a problem in certain buildings and soils in specific areas. Whilst the means by which people are subjected to its effects are not fully quantified or comprehended, it is impossible to determine what additional effect radon exposure obtained in caves may have over and above already-exisiting exposures to the gas. If things are as dismal as you appear to have been taught, in terms of the effect of radon on the metabolism, then we'll have to stop using whole swathes of the countryside and seal off or demolish many buildings.
I think the human metabolism is more robust than realised and can repair itself. However, those starting caving now need to know more about the risk they may be taking on through entering caves at specific times of the year and under certain conditions. Therefore, I stand by my call for 'radon tables' to be developed through thorough measurement of the variation in radon levels within caves in the various limestones of the UK. Rainfall, barometric and air temperature readings ought to be taken at the same time, to enable a correlation to be made between the quantities of radon gas present and the prevailing water and air flow conditions underground. The exposure to radon for those carrying out the experimentation should be spread as widely and sparingly as possible, using as many different cavers as can be found willing to participate. These will be cavers who are keen to learn more about the mechanism behind the presence of radon gas in caves, rather than bury their heads in the sand.
As I ended my original piece on this subject, my advice for those who have been caving some time, should anyone feel that their own personal exposure to radon gas in caves (over time) might have affected them in one way or another, is to do something else for a while, not in caves. If, on the other hand, you're enjoying your caving and mix going underground with climbing and other outdoor activities, then I don't think you're putting yourself any more at risk than everyone else trying to enjoy life in the world which we have inherited from our predecessors . . .