Detection of subsurface resistivity contrasts with application to location of fluids
View Patent ↗The invention relates to a method of mapping subsurface resistivity contrasts by making multichannel transient electromagnetic (MTEM) measurements on or near the earth's surface using at least one source, receiving means for measuring the system response and at least one receiver for measuring the resultant earth response. All signals from the or each source-receiver pair are processed to recover the corresponding electromagnetic impulse response of the earth and such impulse responses, or any transformation of such impulse responses, are displayed to create a subsurface representation of resistivity contrasts. The invention enables subsurface fluid deposits to be located and identified and the movement of such fluids to be monitored.
1. A method of mapping subsurface resistivity contrasts or representations of resistivity contrasts comprising making multichannel transient electromagnetic (MTEM) measurements using at least one source, at least one measuring device for determining the system response and at least one receiver for measuring the resultant earth response, so that system response signals may be determined each time the earth response signals are measured by the at least one receiver, processing the earth response signal from the or each source-receiver pair and the or each corresponding system response signal to recover the or each corresponding electromagnetic impulse response of the earth, and displaying such impulse responses, or any transformation of such impulse responses, to create a subsurface representation of resistivity contrasts.
2. A method according to claim 1 , wherein the impulse response of the earth is obtained from the equation
a k ( x s ,x r ,t )= s k ( x s ,x r ,t )* g ( x s ,x r ,t )+ n k ( x r ,t )
where k indicates the kth measurement in a suite of measurements for a given source-receiver pair, a k (x s ,x r ,t) is the measured transient response for a given source-receiver pair of said MTEM measurements, * denotes convolution, s k (x s ,x r ,t) is the system response, g(x s ,x r ,t) is the impulse response of the earth for a given source-receiver pair, and n k (x r ,t) is uncorrelated electromagnetic noise at the receiver.
3. A method according to claim 2 , wherein said source comprises a current dipole and said receiving means measures the system response for the electric field and comprises two closely spaced apart, for example of the order of centimeters, electrodes positioned close to, for example of the order of centimeters from, the source.
4. A method according to claim 2 , wherein said source comprises a current dipole and said receiving means measures the system response for the magnetic field and comprises a horizontal loop positioned close to, for example of the order of a few centimeters from, the source.
5. A method according to claim 2 , wherein said source comprises at least one current loop and said receiving means comprises measuring means, for example a current meter, for measuring the current in the at least one current loop.
6. A method according to claim 2 , wherein the recording system used to measure the system response has the same characteristics as the system used to record the measurement a k (x s ,x r ,t).
7. A method according to claim 2 , wherein the recording system used to measure the system response has different characteristics from the recording system used to record the measurement a k (x s ,x r ,t) and wherein these differences are eliminated using the transfer function between the two recording systems.
8. A method according to claim 2 , wherein an estimate of the earth impulse response with noise is obtained by deconvolution of the said equation.
9. A method according to claim 8 , wherein said estimate of the earth impulse response is improved by stacking the estimated impulse responses.
10. A method according to claim 2 , wherein the measured system response and corresponding measured transient are synchronised.
11. A method according to claim 2 , wherein any different time origin between the measured system response and corresponding measured transient is measured and compensated for.
12. A method according to claim 1 , wherein the MTEM measurements are made on the earth's surface.
13. A method according to claim 1 , wherein the MTEM measurements are made at or near a sea floor of the earth's surface.
14. Apparatus for mapping subsurface resistivity contrasts comprising means for making multichannel transient electromagnetic (MTEM) measurements comprising at least one source, receiving means for measuring system response and at least one receiver for measuring the resultant earth response, processing means for processing all signals from the or each source-receiver pair to recover the corresponding electromagnetic impulse response of the earth, and display means for displaying such impulse responses, or any transformation of such impulse responses, to create a subsurface representation of resistivity contrasts.
15. A method according to claim 1 in which the system response is approximated by a step function and therefore the earth impulse response function is determined approximately from the measured earth response signal by differentiation.