Systems and methods for soil moisture estimation

• US 7,804,309 B2
• Filed: 12/07/2007
• Issued: 09/28/2010
• Est. Priority Date: 12/07/2006
• Status: Expired due to Fees

• Current Assignee: Vaisala Oyj
• Original Assignee: Vaisala Oyj
• Inventors: Cummins, Kenneth L.
• Primary Examiner(s): Nguyen; Vincent Q
• Application Number:
  US11/953,005
• Publication Number:
  US 20080143350A1
• Time in Patent Office: 1,026 Days
• Field of Search: 324/694, 324/72, 324/637, 324/640, 324/643, 324/329, 324/330, 324332-335
• US Class Current: 324/694
• CPC Class Codes: G01N 33/246 for water content
• CPC Class Codes: G01V 3/12 operating with electromagnetic waves operating with millimetre waves G01V8/005

Abstract

Embodiments of the present invention provide estimates of soil moisture by measuring the change in electrical conductivity near the surface of the earth using surface-propagated electromagnetic fields. A method is provided for estimating near-surface soil moisture, including measuring signals from an electromagnetic ground wave propagating between one or more receiving element locations, determining a transfer characteristic proportional to an average electrical conductivity between pairs of locations; and determining estimated soil moisture in one or more regions derived from analyzing the determined electrical conductivity between pairs of locations and a predetermined regional relationship between electrical conductivity and soil moisture.

Claims

1. A method for estimating near-surface soil moisture, the method comprising:

measuring signals from a vertically polarized electromagnetic wave propagating as a ground wave between two or more receiving element locations, the two or more receiving element locations separated from each other by at least one kilometer;

determining a transfer characteristic proportional to an average electrical conductivity between pairs of locations; and

determining estimated soil moisture in one or more regions derived from analyzing the determined electrical conductivity between pairs of locations and a predetermined regional relationship between electrical conductivity and soil moisture.

2. The method as disclosed in claim 1, wherein measuring signals from an electromagnetic wave further comprises measuring signals produced by a vertically-polarized radiation-field component of the electromagnetic wave.

3. The method as disclosed in claim 1, wherein the electromagnetic wave is produced by cloud-to-ground lightning.

4. The method as disclosed in claim 3, wherein the transfer characteristic is derived from waveform parameters in the time domain.

5. The method as disclosed in claim 4, wherein a plurality of time-domain parameters is determined from rising edge characteristics of the signals.

6. The method as disclosed in claim 5, wherein the time-domain parameters are the at least one of a peak amplitude, a time delay, and a rise time of the signal.

7. The method as disclosed in claim 3, wherein the transfer characteristic is derived from waveform parameters in the frequency domain.

8. The method as disclosed in claim 1, wherein the electromagnetic wave is produced by a narrow-band transmitter.

9. The method as disclosed in claim 8, wherein the transfer characteristic is derived from waveform parameters in the time domain.

10. The method as disclosed in claim 9, wherein the waveform parameters include at least one of a peak amplitude and a phase delay.

11. The method as disclosed in claim 8, wherein the transfer characteristic is derived from waveform parameters in the frequency domain.

12. A method for estimating near-surface soil moisture, the method comprising:

measuring signals from a vertically polarized electromagnetic wave propagating as a ground wave produced by one or more man-made narrowband transmitters in the frequency range of 30 kHz 5 MHz at two or more receiving element locations, the two or more receiving element locations separated from each other by at least one kilometer;

determining a transfer characteristic proportional to an average electrical conductivity between pairs of locations; and

determining estimated soil moisture in one or more regions derived from the determined electrical conductivity between pairs of locations and knowledge of the regional relationship between electrical conductivity and soil moisture.

13. The method as disclosed in claim 12, wherein the transfer characteristic is derived from waveform parameters in the time domain.

14. The method as disclosed in claim 13, wherein the waveform parameters include at least one of a peak amplitude and a phase delay.

15. The method as disclosed in claim 12, wherein the transfer characteristic is derived from waveform parameters in the frequency domain.

16. A method for estimating near-surface soil moisture, the method comprising:

measuring signals from an electromagnetic wave propagating as a vertically polarized ground wave produced by one or more return strokes of cloud-to-ground lightning from at least one receiving element location;

determining a transfer characteristic proportional to an average electrical conductivity between the locations of the lightning and one or more receiving elements;

determining estimated soil moisture in one or more regions derived from;

the determined electrical conductivity between a lightning strike location and at least one receiving element location; and

knowledge of the regional relationship between electrical conductivity and soil moisture.

17. The method as disclosed in claim 16, wherein the transfer characteristic is derived from waveform parameters in the time domain.

18. The method as disclosed in claim 16, wherein a plurality of time-domain parameters is determined from rising edge characteristics of the signals.

19. The method as disclosed in claim 18, wherein the time-domain parameters include at least one of a peak amplitude, a time delay, and a rise time of the signals.

20. The method as disclosed in claim 16, wherein the transfer characteristic is derived from waveform parameters in the frequency domain.

21. A method for estimating near-surface soil moisture, the method comprising:

synthesizing a broadband signal for propagation as a ground wave;

transmitting the synthesized signal from a transmitting element location as a vertically polarized electromagnetic wave coupled to a ground propagation medium at known times;

measuring one or more received signals at one or more receiving element locations separated from each other by at least one kilometer;

determining a transfer characteristic proportional to an average electrical conductivity between pairs of locations; and

determining estimated soil moisture in one or more regions derived from the determined electrical conductivity between the transmitting element location and at least one receiving element location and knowledge of the regional relationship between electrical conductivity and soil moisture.

22. The method as disclosed in claim 21, wherein the transfer characteristic is derived from waveform parameters in the time domain.

23. The method as disclosed in claim 22, wherein the waveform parameters include at least one of a peak amplitude and a phase delay for at least one frequency.

24. The method as disclosed in claim 21, wherein the transfer characteristic is derived from waveform parameters in the frequency domain.

25. The method as disclosed in claim 21, further comprising generating a set of vectors representing a broadband test signal.

26. The method as disclosed in claim 21, wherein the time of transmission of the synthesized signal is not precisely known and two or more receiving elements are employed.

27. The method as disclosed in claim 21, wherein the broadband signal comprises a pseudorandom noise signal.

28. The method as disclosed in claim 21, wherein the broadband signal comprises a broadband Gaussian noise signal.

29. The method as disclosed in claim 25, further comprising controlling broadcast of the broadband signal by specifying at least one of an initial broadcast time, and ending broadcast time, a broadcast repeat interval, and a number of broadcast repetitions.

30. A soil moisture monitoring system comprising:

a data collection and management component coupled to;

one or more RF receiving elements respectively located at one or more receiving element locations, the receiving element locations separated from each other by at least one kilometer; and

an input archive;

a central processing component coupled to;

the data collection and management component;

a product generator for delivering processed information products; and

an output archive; and

a memory coupled to the processing component and storing instructions that, when executed, cause the processing component to;

obtain signals measured from a vertically polarized electromagnetic wave propagating as a ground wave between a transmitter and at least one receiving element location;

determine a transfer characteristic proportional to an average electrical conductivity between the transmitter and at least one receiving element; and

determine estimated soil moisture in one or more regions derived from analyzing the determined electrical conductivity between pairs of locations and a predetermined regional relationship between electrical conductivity and soil moisture.

31. The soil moisture monitoring system as disclosed in claim 30 wherein the data collection and management component is further coupled to:

an RF transmission source comprising the transmitter; and

an input generator, coupled to the RF transmission source and the data collection and management component, the input generator configured to create data for presentation to inputs of the RF transmission source.

32. The soil moisture monitoring system as disclosed in claim 31, wherein the transmission source further comprises one or more transmitting elements that transmit signals at one or more frequencies that can propagate as a ground wave.

33. The method as disclosed in claim 32, wherein the transfer characteristic is derived from waveform parameters in the time domain.

34. The method as disclosed in claim 33, wherein the waveform parameters include at least one of a peak amplitude and a phase delay.

35. The method as disclosed in claim 32, wherein the transfer characteristic is derived from waveform parameters in the frequency domain.

36. The soil moisture monitoring system as disclosed in claim 30, further comprising a transmission source including RF energy produced by one or more return strokes of cloud-to-ground lightning.

37. The method as disclosed in claim 36, wherein the transfer characteristic is derived from waveform parameters in the time domain.

38. The method as disclosed in claim 37, wherein a plurality of time-domain parameters is determined from rising edge characteristics of the signals.

39. The method as disclosed in claim 38, wherein the time-domain parameters include at least one of a peak amplitude, a time delay, and a rise time of the signals.

40. The method as disclosed in claim 36, wherein the transfer characteristic is derived from waveform parameters in the frequency domain.

41. The soil moisture monitoring system as disclosed in claim 30, wherein the electromagnetic wave includes RF sources selected from the group consisting of AM, LORAN, ATC directional beacons, man-made sources of broadband electromagnetic energy, and combinations thereof

42. The method as disclosed in claim 41, wherein the transfer characteristic is derived from waveform parameters in the time domain.

43. The method as disclosed in claim 42, wherein the waveform parameters include at least one of a peak amplitude and a phase delay.

44. The method as disclosed in claim 41, wherein the transfer characteristic is derived from waveform parameters in the frequency domain.