Abstract
Soils are the biggest terrestrial carbon store. The contribution of plant roots to soil and atmospheric carbon is significant and difficult to survey accurately. Worldwide interest in reducing greenhouse gases has led to research activities for quantifying the root biomass and evaluating their critical role in space and time. Geophysical methods image the medium under study in 2D and 3D, and monitor changes and processes in 4D. They offer good parametrical and spatiotemporal resolution combined with a minimum-invasive character. The high-resolution techniques of electric resistivity imaging (ERI) and ground penetrating radar (GPR) have extended newly their applications into the less known in vivo investigation of biogeophysical targets of living plants and trees. This includes mapping roots and trunk structures, diagnosing wood decay, analysing fluid content and physiological processes of water redistribution, sap uptake, etc. (e.g., Hagrey and Michaelsen, Eur J Environ Eng Geophys 7:75–93, 2002; Hagrey and Michaelsen, Geophysics 64:746–753, 1999; Hagrey et al., Geophys J Int 138:643–654, 1999; Hagrey et al. Proceedings, Meeting of Engineering Geology, Kiel, Germany, 2003; Hanafy and Hagrey, Geophysics 71:k9–k18, 2006; Hubbard et al., The Leading Edge 21:552–559, 2002). Applications of ERI and GPR techniques to image roots and root-zones are based on the electrical and electromagnetic contrast of these targets relative to surrounding soils (e.g., Hruška et al. Tree Physiol 19:125–130, 1999; Butnor et al., Tree Physiol 21:1269–1278, 2001; Butnor et al., Am J Soil Sci Soc 67:1607–1615, 2003; Hagrey et al. Geophys J Int 138:643–654, 2004, Hagrey 2007; Werban et al. J Plant Nutr Soil Sci 171:927–935, 2007; Amato et al. Tree Physiol 28:1441–1448, 2008; Amato et al. Eur J Agron 31:213–222, 2009; Petersen and Hagrey, The Leading Edge 28(10):1220–1224, 2009; Doolittle and Butnor, Soils, peatlands and biomonitoring. In: Jol HM (Ed) Ground penetrating radar: theory and applications. Elsevier, Amsterdam, 177–192, 2009; Hagrey and Petersen, Geophysics 76(2), G25–G35, 2011). In this chapter, we present principles of ERI and GPR techniques for root studies.
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Hagrey, S.A.a. (2012). Geophysical Imaging Techniques. In: Mancuso, S. (eds) Measuring Roots. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-22067-8_10
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