Author
Listed:
- Edgard Gonzales
(Universidad Nacional de San Agustín de Arequipa, Arequipa 04001, Peru
International Institute for Research and Innovation in Sustainable Mining, Arequipa 04001, Peru)
- Javier Ticona
(Universidad Nacional de San Agustín de Arequipa, Arequipa 04001, Peru)
- Armando Minaya
(Universidad Nacional de San Agustín de Arequipa, Arequipa 04001, Peru)
- Richard Krahenbuhl
(Department of Geophysics, Colorado School of Mines, Golden, CO 80401, USA
Humanitarian Engineering & Science IGP, Colorado School of Mines, Golden, CO 80401, USA)
- Jeffrey Shragge
(Department of Geophysics, Colorado School of Mines, Golden, CO 80401, USA
Humanitarian Engineering & Science IGP, Colorado School of Mines, Golden, CO 80401, USA)
- Jared Low
(Department of Geophysics, Colorado School of Mines, Golden, CO 80401, USA)
- Hanna Flamme
(Department of Geophysics, Colorado School of Mines, Golden, CO 80401, USA)
Abstract
Cemented subsoils, commonly referred to as caliche, pose a regular challenge for agricultural development in arid and semi-arid regions like coastal southern Peru. These subsurface features restrict root penetration, limit water infiltration and hinder essential soil processes, ultimately reducing crop yields and agricultural productivity. Accurate and efficient mapping of caliche is important for optimizing land-use planning and implementing sustainable agricultural practices. This study presents the application of near-surface geophysical techniques for mapping caliche deposits in the context of agricultural development at the future Majes II site in the Arequipa region of southern Peru. Specifically, we employed high-frequency ground-penetrating radar (GPR) and frequency-domain electromagnetics (FDEM) at a testbed on the Majes II site to evaluate their ability to delineate the extent, thickness, and depth of caliche within the local geology. GPR offers high-resolution imaging, effectively capturing sharp contrasts between caliche and surrounding materials, providing detailed information on the thickness (approximately 0.4 m) and the depth (up to 1.5 m) of the caliche layers. FDEM provides valuable insights into the presence of caliche at a faster rate of data acquisition and processing, enabling rapid assessment of the extent of caliche deposits, although with the tradeoff of lower resolution and depth information. We demonstrate that these two geophysical methods can be used separately or in an integrated manner for collaborative interpretation at the Majes II site to inform land management decisions, including identifying areas with favorable conditions for crop production and implementing targeted interventions to mitigate the adverse effects of caliche on agricultural productivity.
Suggested Citation
Edgard Gonzales & Javier Ticona & Armando Minaya & Richard Krahenbuhl & Jeffrey Shragge & Jared Low & Hanna Flamme, 2024.
"Geophysical Mapping of Cemented Subsoils for Agricultural Development in Southern Peru,"
Sustainability, MDPI, vol. 16(16), pages 1-18, August.
Handle:
RePEc:gam:jsusta:v:16:y:2024:i:16:p:6801-:d:1452446
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