Acta Geodaetica et Cartographica Sinica ›› 2019, Vol. 48 ›› Issue (8): 1059-1066.doi: 10.11947/j.AGCS.2019.20180038

• Photogrammetry and Remote Sensing • Previous Articles     Next Articles

Theoretical analysis of soil freeze/thaw process on DDM waveform and multipath in order for GNSS-R/IR applications

WU Xuerui1,2,3, XIA Junming4,5, BAI Weihua4,5,6, ZHANG Xinggang7   

  1. 1. Shanghai Astronomical Observatory, Chinese Academy of Sciences, Shanghai 200030, China;
    2. Key Laboratory of Space Navigation and Position Technology, Shanghai 200030, China;
    3. Key Laboratory of Planetary Sciences, Chinese Academy of Sciences, Shanghai 200030, China;
    4. National Space Science Center, Chinese Academy of Sciences, Beijing 100190, China;
    5. Beijing Key Laboratory of Space Environment Exploration, Beijing 100190, China;
    6. School of Astronomy and Space Science, University of Chinese Academy of Sciences, Beijing 100190, China;
    7. National Time Service Center, Chinese Academy of Sciences, Xi'an 710600, China
  • Received:2018-01-22 Revised:2018-10-10 Online:2019-08-20 Published:2019-08-27
  • Supported by:
    The National Natural Science Foundation of China (No. 41501384);The National Key Research and Development Program of China (Nos. 2017YB0502800;2017YFB0502802);The Academician Workstation Foundation In Chifeng (No. cfxyys201710)

Abstract: In order to extend the applications GNSS-R/IR(GNSS-reflectometry/interferometric reflectometry) remote sensing technique to soil freeze/thaw process detection, soil(frozen/thawn) mixing permittivity models are employed to calculate the soil permittivity. Bistatic full-polarization coherent scattering model and random roughness surface scattering model are used to calculate the coherent and non-coherent scattering, which result in the variations of GPS multipath observables and DDM(delay Doppler map) waveforms, respectively. When the soil freeze/thaw process occurs, theoretical simulations indicate that soil freeze/thaw process induce the abrupt permittivity changes and affect the obvious variations of GNSS-R/IR signals. In this way, theoretical fundamentals for soil freeze/thaw process detections are presented.

Key words: GNSS-R/IR, soil freeze/thaw process, delay Doppler map, multipath, bistatic scattering full polarization

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