GB1587951A - Particle coating analysis and mineral prospecting - Google Patents

Description

(54) PARTICLE COATING ANALYSIS AND MINERAL PROSPECTING (71) I, DENNIS JOHN CARSON MACOURT, an Australian citizen, of 73 Dickson Avenue, Artarmon 2064, New South Wales, Australia, do hereby declare the invention for which I pray that a patent may be granted to me, and the method by which it is to be performed, to be particularly described in and by the following statement: The present invention relates to a method of prospecting for minerals by analysis or to coatings on particles. The invention has particular relevance to the aerial prospecting for both uranium and related minerals as well as for hydrocarbon deposits which have, as a common feature, the presence of (i) radon (Atomic No. 88 and Atomic Weight 222, a "daughter" product of the radioactive decay of uranium accumulated within the mineral deposit), and (ii) halogen (in particular iodine).

The anomalous occurrence of radon gas around deposits of oil and natural gas, as well as around deposits of uranium and associated minerals, is well known and has been used by numerous prospectors in the search for such deposits. Previous techniques which have been used to detect anomalous radon gas involve drilling shallow holes in the ground from which a sample of air and gas is pumped over a period of time. Radon may be detected by passing the sample through a suitable gamma ray detector which counts the emission of gamma rays by radon as it decays to Bismuth (Bi214), and helium.

Because the "half life" of radon is only approximately 3.7 days, there occurs a sharply anomalous concentration of radon over a deposit of thewabove-mentioned type (the radon rapidly breaks down with time).

Accordingly. in the prior art technique mentioned above, the analysis of the gas sample has to be performed continuously as the hold is pumped out. This process is laborious and costly in that it requires considerable on-site equipment and the time taken to cover a reasonable area of ground makes it uneconomic in regional prospecting.

There are several other prior art methods for measuring radon gas concentrations in shallow holes, the most recent of which is known by the trade designation "Trak Etch". This method involves leaving suitable polymeric or photgraphic materials in such holes, or secured to the bottom of an inverted plastic cup located in such a hole, for several days - during which time a, P and y rays emanating from the decaying radon, issuing from the ground, produce small apertures in the polymeric material, or cause patterns to be produced in the photographic material (emulsion) according to the rate of release (and hence decay) of the radon gas. The apertures in the polymeric material may be etched with suitable chemicals to increase the size of the apertures to the point where they are visible under a microscope; similarly the photographic material may be developed so as to render the patterns visible. In either case the frequency of the patterns may be ascertained in order to determine the concentration of radon gas released.

Measurement-wise, instruments have been developed to count, automatically, the holes in the polymer or photographic film.

The just-mentioned prior art methods require labour intensive, and time consuming, analysis after collection of the exposed material - and are therefore expensive. In consequence such methods are restricted in current use to those areas which are known to be highly prospective and which only require detailed examination over a limited area. Additionally, they (the prior art methods) are also restricted to individual sampling points rather than continuous mobile analysis - which may give rise to errors in that cracks in the earth's surface (such as faults) may be near some holes and not others. and the leakage of radon up these cracks may be detected by the "near" holes (and make interpretation difficult and erroneous). Workers in this field have found that even relatively closely spaced holes do not necessarily give similar readings.

It is among the objects of the invention to provide a novel process whereby the above disadvantages are substantially avoided. The invention is predicated upon my discovery that certain materials, which one would not expect to find in the atmosphere, are in fact present and can be efficiently detected therein - and thereby used to locate deposits of uranium and associated minerals, oil and natural gas. Specifically, I am utilising the quite unexpected presence in the atmosphere of radon (normally not known to rise above the surface of the earth because of its high molecular weight) and halogen, in particular iodine (not expected to be atmospherically located because of its propensity to sublimate and adsorb) for the above purpose.

According to one aspect of the present invention there is provided a method of prospecting for minerals by collecting particles from positions adjacent a locality to be prospected. and spectroscopically determining whether radon and/or a halogen is contained in coatings on the particles, such spectroscopic determination including the steps of entraining particles in a flow of inert gas, heating the inert gas so as to neutralise the charge attaching the coatings to the particles and separating the coatings from the particles, conducting the gas and coatings, but not the particles into a plasma vessel. plasmatizing the gas and coatings therein and spectroscopically analysing the light emitted.

Where the determination is in respect of a halogen, the halogen will preferably be iodine.

As used above. and hereafter. the term "coating", or "radon coating", or "halogen coating", will be used to cover a wide variety of possible combinations including individual. or numbers, or radon or halogen atoms or molecules (or condensation neuclei) adhering to, or being adsorbed. on the surfacc(s) of a particle - and, in addition, actual coatings of radon or halogen atoms or molecules (or condensation ncuclei) in which the particle itsclf is partially or substantially completely covcred or enveloped with a thin layer of radon or halogen atoms or molecules (or condensation ncuclei).

The invention will now be described with sequential reference to (i) preferred subgeneric details. and (ii) a specific operation as illustrated by reference to accompanying drawings. As a general prclude thereto. it is emphasised that such cnsuing description is not to be limitatively construed.

1. Radon Detection Dealing firstly (and sub-generically) with the instant method as applied to the detection of radon, it is initially pointed out that such method enables the continuous detection of radon to be achieved from an aircraft operating at low altitude and speed.

This therefore makes the present invention highly suitable for regional prospecting over large areas for anomalous concentrations of radon emanating from surface, subsurface, or deeply buried deposits of uranium - as well as deposits of oil or natural gas at varying depths. The detection of such anomalous emanations and, with a suitable means of navigation, the accurate determination of their locations within a region, represents a major step in the search for these deposits (and will accurately indicate an area in which further detailed geophysical and geochemical work could be carried out on the ground). In addition, under suitable conditions, the determination of such anomalies may lead to the direct discovery of commercially viable deposits of such minerals or hydrocarbon accumulations.

Proceeding with this form of the present invention, atoms or molecules, or condensation nuclei. of radon gas, which are highly charged, adsorb on the surface of larger particles such as dust at the surface of the earth where the radon gas emanates. The dust particles are elevated into the atmosphere by the action of either wind and/or sun alone or in combination. Such elevated particles could be collected and concentrated by a number of well known methods of subsequent analysis. However unless the analysis is carried out very shortly after the particles are collected, the natural decay of the radon adsorbed on the collected particles will cause the apparent magnitude of the anomaly to be severely reduced once the particle is removed from the area in which the radon gas is being given off. Most importantly, undue delay in analysing the coating may preclude radon being detected at all.

Furthermore, unless the analytical technique used is specific for radon, confusion could result in the interpretation of the results. For example. the Bismuth isotope, having an atomic weight of 214, is a decay product of radon gas which has a half-life of several years. This decay product appears ubiquitously throughout the atmosphere.

Therefore if an inadequate technique is used, this can give misleading anomalous radioactivity which may not be due to radon at all.

In the preferred practice of the present invention. only the larger particles, that is those having a dimension greater than 15 to 20 microns. which are located in currents of rising air close to the surface of the ground.

are collected by low flying aircraft. These particles are transferred to a chemically inert carrier gas such as helium or argon or a mixture thereof (but which need not be a noble gas) in a manner similar to that used in a conventional mass spectrometer. This manner of transfer involves the projection of the particles, which are heavy relative to the air in which they are carried and collected, into a stream of inert gas which transports them to the desired region i.e. an area in which the radon coating is removed from the surface of the particle. In one form of the invention this transference is effected as illustrated hereafter (in the description with reference to the accompanying drawings). Alternatively, it may be effected by a virtual impaction technique wherein it is the stream of inert gas which, at a predetermined point, is reversed in direction of flow thereby acquiring the particles and transporting them to the said region. The size of the particle acquired by the inert carrier gas stream can be accurately controlled by varying the velocity of the counter-flowing agent and also the distance through which the particles are projected before flow reversal occurs.

The radon coating is released from the particles by neutralizing the electrical charge attaching the atoms or molecules (or condensation neuclei) to the particles and thereby volatilising the coating. This is carried out by heating the particles in a suitable oven i.e. the particles are subjected to pyrolisation, the dust particles in the oven being trapped on a porous sintered filter in which the pore size is finer than the size of the collected particles.

In this way the particles are retained by the filter and only the gaseous products of pyrolisation are carried forward in the inert gas stream beyond the filter. The temperature of the oven is as low as possible (a temperature of the order of 1500C - or less - is invariably adequate) to release the atom(s) or molecule(s) or radon in the coating, by the process of thermophoresis, since at the same time a number of other molecules of varying volatility will also be released. Such molecules may include hydrocarbons and possibly mercury, which volatilsed molecules pass on with the stream of gas and radon.

These steps are elaborated in the ensuing illustrated description.

Alternatively, the radon coating et al may also be volatilised by the employment of a primary plasma in which the particulate material is retained, and the adsorbed material being volatilised is separated therefrom and passed on to a next stage - where analysis of the volatilised material is carried out.

From the foregoing, it will be observed that a plasma need not be employed to obtain the release or volatilisation of the radon coating (although if it is desired to also analyse the particulate coatings for other adsorbed molecules of low volatility, it may be advantageous to do so). Volatilisation of the adsorbed material may also be accomplished by using a laser if desired.

In the next stage, the released gases and volatilised materials are then transported immediately to a plasma (or secondary plasma) which is viewed by a conventional spectrometer or other suitable instrument which permits the emission or absorption of radon to be observed and measured. The plasma may be either a direct current discharge or an alternating current discharge and in the latter case, low frequencies, radio frequencies, and microwave frequencies may be used as desired.

When the analysis of the light emitted from the above-mentioned plasma is carried out, in accordance with this embodiment, using the methods of atomic emission spectroscopy, the strongest emission line for radon is at 434.96 nanometers (nm) whilst the next strongest line is at 745.00 nm.

The first of these emission lines is adjacent to the emissions of a well-developed C-H band structure, which emission ends at approximately 433.5 nm at the longer end, and could cause interference. This is particularly relevant if the instant method is used for prospecting for oil or natural gas where hydrocarbons could be adsorbed on the surface of atmospheric particles - and which, in turn, would give significant emission in the well known C-H and C-N bands, the latter of which occurs at approximately 388 nm.

The resolution of the strongest emission line at 434.96 nm will depend on the quality of the particular spectrometer used, but there are several techniques well known to those skilled in the art, for achieving the desired resolution and separation from the above-mentioned C-H band. Additionally the emission line at 745.00 nm or another radon emission line nearby at 705.54 nm, are both relatively free from interference from other continuums and these lines can be used either separately or as a measure of differentiating the radon emission at 434.96 nm from the above-mentioned C-H band emission.

2. Halogen Detection This form of the present invention is described with particular reference to the detection of iodine (especially) and bromine - which (just as in the case of radon) I have found to be both associated with deposits of oil and natural gas et al, and surprisingly present in the atmosphere. Here (referring to iodine) the atoms or molecules (or condensation nuclei) of iodine gas adsorb on the surface of particles such as dust at the surface of the earth where the iodine gas emanates and (as above) these dust particles are elevated into the atmosphere. Thereafter, entrapment of the particles (in the flow of chemically inert carrier gas), heating (whereby the iodine coating is released), and spectroscopic analysis (whereby errors - that could flow from the natural sublimation of the iodine adsorbed on the entrapped particles - are forestalled) are generally carried out as hereinabove described. In this form of the invention - when the analysis of the light emitted from the plasma is carried out by atomic emission spectrosco y - the most suitable emission line for iodine is at 608.2 naometers (nm) whilst other suitable lines are at 546.4 nm and 533.8 nm. For bromine, the most suitable emission line is at 478.5 nanometers.

In the detection of iodine by emission spectroscopy, the wave lengths of light produced by electrode decay should not interfere with the iodine spectral lines. It has been found that this is best achieved by the use of electrodes of solid platinum or platinum/ indium .

3. An Illustrated Embodiment Hereunder, the detection of radon gas is described with reference to the annexed illustrative drawings. In again emphasising that such description is by way of example only, it is-also recorded that a schematic type of illustration- is employed because the individual integers of the illustrated apparatus are themselves conventional in structure.

In the drawings: Figure 1 schematically depicts an apparatus whereby the instant method may be carried out; Figure 2 is a representation of a prospecting aircraft equipped with such an apparatus.

The illustrated apparatus consists of a cyc ldne concentrator 1 into the mouth 2 of which the air outside the aircraft is forced by reason of its velocity. The particulate matter in the air is concentrated on the conical walls of the cyclone and falls toward a base outlet 4. The remaining air is vented through an outlet 3. A pump 5 draws air off the bottom of cyclone 4 along a tube 6 to a virtual impactor 7, in which a sudden reversal of the direction of flow (of the air) causes the concentrated particles to be projected into and along a pipe 8, which is juxtaposed, and in close proximity to, a similarly-diametered pipe 9 in chamber 10. The reduction of air volume entering impactor 7, compared to that entering the mouth 2 of the cyclone concentrator. may be as much as 1000 times.

Chemically inert carrier gas (specifically helium) is introduced into chamber 10 at constant pressure by means of a valve 11, the suction of the pump 5 causing some of the gas to counter flow along the pipe 8 (thereby preventing the entry of air when the pressure of the valve 11 is suitably correlated to the vacuum of the pump 5). A further pump, 12.

draws an aliquot of the inert carrier gas through pipe 9 - and thence through the remainder of the apparatus (see below). the flow thercthrough being accurately control led by a valve ,:,6ted over 16.

Particles projected over the gap between the pipes 8 and 9 are entrapped in the carrier gas in the pipe 9, and carried to a sintered porous filter 13 which is contained in a thermostatically controlled oven 14 (at a temperature of, for example, 100-200"C). Sizewise, the particles entering pipe 9 can be adjusted by means of the pressure in chamber 10 - which will increase or decrease the counter flow in the pipe 8 (a larger flow will prevent the smaller particles being projected far enough to reach the pipe 9). The size of the smallest particle reaching the sintered filter should be greater than the pass size of the filter. In itself, the filter is removable (form the oven) for cleaning and empty,- ing - and can be sealingly reassembled with equal facility.

The radon gas released from the surface of the particles by thermophoresis, in the oven 14, passes to a two electrode plasma 15 (RF or microwave plasmas would, of course, be equally suitable). This plasma is viewed by a conventional spectrometer or monochrometer 17 of which the output is processed and recorded by electronic means 18 coupled to a navigating system 19. In this way, the output of the spectrometer (or monochrometer) can be correlated with the position of the aircraft over the ground.

The apparatus preferably operates at or slightly below atmospheric pressure; for example in the range of 0.5 to 1.0 atmospheres. However, it may operate at much lower pressures (e.g. 0.1 or even 0.01 atmospheres) provided sufficient chemically inert carrier gas is present to transfer the particles into the porous sintered filter.

In the method as just illustrated, the chemically inert carrier gas is specified as helium.

However, in lieu thereof, there may be employed any other such gas, noble or otherwise, as exemplified by argon, and mixtures (the latter possibility in turn being exemplified by an argon/helium mixture). The electrodes (of the electrode plasma) are constructed from materials that are free of those elements that are being viewed by the spectrometer; specifically, in the embodiment illustrated, the electrodes are of platinum. In referring to the spectrometer, the opportunity is taken to underscore the fact that the invention is not limited in respect of the type of spectrometer (or method of spectroscopic analysis) employed. Also, whilst discussing alternatives, it will be appreciated that, in lieu of the aircraft (schematically illustrated in Figure 2), the apparatus of Figure 1 could be mounted in a prospecting road vehicle.

WHAT I CLAIM IS: 1. A method of prospecting for minerals by collecting particles from positions adjacent a locality to be prospected, and spectroscopically determining whether radon and/or a halogen is contained in coatings on the particles, such spectroscopic determination including the steps of entraining particles in a flow of inert gas, heating the inert gas

**WARNING** end of DESC field may overlap start of CLMS **.

Claims (11)

**WARNING** start of CLMS field may overlap end of DESC **. out as hereinabove described. In this form of the invention - when the analysis of the light emitted from the plasma is carried out by atomic emission spectrosco y - the most suitable emission line for iodine is at 608.2 naometers (nm) whilst other suitable lines are at 546.4 nm and 533.8 nm. For bromine, the most suitable emission line is at 478.5 nanometers. In the detection of iodine by emission spectroscopy, the wave lengths of light produced by electrode decay should not interfere with the iodine spectral lines. It has been found that this is best achieved by the use of electrodes of solid platinum or platinum/ indium . 3. An Illustrated Embodiment Hereunder, the detection of radon gas is described with reference to the annexed illustrative drawings. In again emphasising that such description is by way of example only, it is-also recorded that a schematic type of illustration- is employed because the individual integers of the illustrated apparatus are themselves conventional in structure. In the drawings: Figure 1 schematically depicts an apparatus whereby the instant method may be carried out; Figure 2 is a representation of a prospecting aircraft equipped with such an apparatus. The illustrated apparatus consists of a cyc ldne concentrator 1 into the mouth 2 of which the air outside the aircraft is forced by reason of its velocity. The particulate matter in the air is concentrated on the conical walls of the cyclone and falls toward a base outlet 4. The remaining air is vented through an outlet 3. A pump 5 draws air off the bottom of cyclone 4 along a tube 6 to a virtual impactor 7, in which a sudden reversal of the direction of flow (of the air) causes the concentrated particles to be projected into and along a pipe 8, which is juxtaposed, and in close proximity to, a similarly-diametered pipe 9 in chamber 10. The reduction of air volume entering impactor 7, compared to that entering the mouth 2 of the cyclone concentrator. may be as much as 1000 times. Chemically inert carrier gas (specifically helium) is introduced into chamber 10 at constant pressure by means of a valve 11, the suction of the pump 5 causing some of the gas to counter flow along the pipe 8 (thereby preventing the entry of air when the pressure of the valve 11 is suitably correlated to the vacuum of the pump 5). A further pump, 12. draws an aliquot of the inert carrier gas through pipe 9 - and thence through the remainder of the apparatus (see below). the flow thercthrough being accurately control led by a valve ,:,6ted over 16. Particles projected over the gap between the pipes 8 and 9 are entrapped in the carrier gas in the pipe 9, and carried to a sintered porous filter 13 which is contained in a thermostatically controlled oven 14 (at a temperature of, for example, 100-200"C). Sizewise, the particles entering pipe 9 can be adjusted by means of the pressure in chamber 10 - which will increase or decrease the counter flow in the pipe 8 (a larger flow will prevent the smaller particles being projected far enough to reach the pipe 9). The size of the smallest particle reaching the sintered filter should be greater than the pass size of the filter. In itself, the filter is removable (form the oven) for cleaning and empty,- ing - and can be sealingly reassembled with equal facility. The radon gas released from the surface of the particles by thermophoresis, in the oven 14, passes to a two electrode plasma 15 (RF or microwave plasmas would, of course, be equally suitable). This plasma is viewed by a conventional spectrometer or monochrometer 17 of which the output is processed and recorded by electronic means 18 coupled to a navigating system 19. In this way, the output of the spectrometer (or monochrometer) can be correlated with the position of the aircraft over the ground. The apparatus preferably operates at or slightly below atmospheric pressure; for example in the range of 0.5 to 1.0 atmospheres. However, it may operate at much lower pressures (e.g. 0.1 or even 0.01 atmospheres) provided sufficient chemically inert carrier gas is present to transfer the particles into the porous sintered filter. In the method as just illustrated, the chemically inert carrier gas is specified as helium. However, in lieu thereof, there may be employed any other such gas, noble or otherwise, as exemplified by argon, and mixtures (the latter possibility in turn being exemplified by an argon/helium mixture). The electrodes (of the electrode plasma) are constructed from materials that are free of those elements that are being viewed by the spectrometer; specifically, in the embodiment illustrated, the electrodes are of platinum. In referring to the spectrometer, the opportunity is taken to underscore the fact that the invention is not limited in respect of the type of spectrometer (or method of spectroscopic analysis) employed. Also, whilst discussing alternatives, it will be appreciated that, in lieu of the aircraft (schematically illustrated in Figure 2), the apparatus of Figure 1 could be mounted in a prospecting road vehicle. WHAT I CLAIM IS:

1. A method of prospecting for minerals by collecting particles from positions adjacent a locality to be prospected, and spectroscopically determining whether radon and/or a halogen is contained in coatings on the particles, such spectroscopic determination including the steps of entraining particles in a flow of inert gas, heating the inert gas

so as to neutralise the charge attaching the coatings to the particles, and separating the coatings from the particles, conducting the gas and coatings, but not the particles into a plasma vessel, plasmatizing the gas and coatings therein and spectroscopically analysing the light emitted.

2. A method according to claim 1, wherein when the determination is in respect of a halogen, the halogen is iodine.

3. A method according to claim 1 or 2, wherein the step of heating the inert gas and entrained particles involves plasmatizing the inert gas in a first plasma vessel.

4. A method according to claim 1 or 2, wherein the step of heating involves heating up to 200"C.

5. A method according to claim 1, 2 or 4, wherein particles are filtered from the gas after the heating step.

6. A method according to any preceding claim performed in an aeroplane.

7. A method according to any preceding claim, wherein the inert gas is a noble gas.

8. A method according to any preceding claim, wherein the particles are concentrated before being entrained in the inert gas.

9. A method according to any preceding claim, wherein only particles in excess of lS microns size are entrained in the inert gas.

10. A method according to any preceding claim, wherein the particles are entrained in the inert gas by projecting the particles into a counter-flowing steam of said gas which steam has a reversal of the direction of flow.

11. Methods of prospecting for minerals according to claim 1. substantially as hereinbefore described with reference to the accompanying drawings.