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  • Wiley  (2)
  • Bogena, Heye R.  (2)
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  • Wiley  (2)
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  • 1
    In: WIREs Water, Wiley, Vol. 2, No. 6 ( 2015-11), p. 635-647
    Abstract: Soil moisture is an important state variable in the terrestrial system because it controls the exchange of water and energy between the land surface and the atmosphere. In this study, we review recent advances in noninvasive techniques that allow continuous noninvasive and contactless measurements of soil moisture dynamics at the field to basin scale. In particular, we report on (1) cosmic‐ray neutron probes, (2) Global Navigation Satellite System reflectometry, (3) ground‐based microwave radiometry, (4) gamma‐ray monitoring, (5) terrestrial gravimetry, and (6) low‐frequency electromagnetic surface waves. Each method is described in terms of its basic principle, measurement scales, calibration issues, measurement accuracy, and applications. We hope that this review will further stimulate the community to invest in the continued development of novel soil moisture sensing methods that address the need for large‐scale soil water content measurements with sufficiently high temporal resolution. WIREs Water 2015, 2:635–647. doi: 10.1002/wat2.1097 This article is categorized under: Science of Water 〉 Hydrological Processes Science of Water 〉 Water and Environmental Change
    Type of Medium: Online Resource
    ISSN: 2049-1948 , 2049-1948
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2015
    detail.hit.zdb_id: 2751191-1
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  • 2
    Online Resource
    Online Resource
    Wiley ; 2018
    In:  Vadose Zone Journal Vol. 17, No. 1 ( 2018-01), p. 1-13
    In: Vadose Zone Journal, Wiley, Vol. 17, No. 1 ( 2018-01), p. 1-13
    Abstract: Dynamics of redox potential were induced by water‐table changes in a lysimeter. The redox potential measurements well reflected the different GHG emission sources. Redox potential monitoring is a viable tool for better understanding of GHG emissions. Soil greenhouse gas (GHG) emissions contribute to global warming. To support mitigation measures against global warming, it is important to understand the controlling processes of GHG emissions. Previous studies focusing mainly on paddy rice fields or wetlands showed a strong relationship between soil redox potential and GHG emission (e.g., N 2 O). However, the interpretation of redox potentials for the understanding of the controlling factors of GHG emission is limited due to the low number of continuous redox measurements in most ecosystems. Recent sensor developments open the possibility for the long‐term monitoring of field‐scale soil redox potential changes. We performed laboratory lysimeter experiments to investigate how changes in the redox potential, induced by changes in the water level, affect GHG emissions from agricultural soil. Under our experimental conditions, we found that N 2 O emissions followed closely the changes in redox potential. The dynamics of redox potential were induced by changing the water‐table depth in a laboratory lysimeter. Before fertilization during saturated conditions, we found a clear negative correlation between redox potentials and N 2 O emission rates. After switching from saturated to unsaturated conditions, N 2 O emission quickly decreased, indicating denitrification as the main source of N 2 O. In contrast, the emissions of CO 2 increased with increasing soil redox potentials. After fertilization, N 2 O emission peaked at high redox potential, suggesting nitrification as the main production pathway, which was confirmed by isotope analysis of N 2 O. We propose that redox potential measurements are a viable method for better understanding of the controlling factors of GHG emissions, for the differentiation between different source processes, and for the improvement of process‐based GHG models.
    Type of Medium: Online Resource
    ISSN: 1539-1663 , 1539-1663
    Language: English
    Publisher: Wiley
    Publication Date: 2018
    detail.hit.zdb_id: 2088189-7
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