A process-based numerical approach to estimate forest groundwater consumption in flatland petrocalcic soils
Author(s) -
Claudio Ramón Mujica,
Germán Marcelo Milione,
Sergio A. Bea,
Javier Gyenge
Publication year - 2019
Publication title -
journal of hydroinformatics
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.654
H-Index - 50
eISSN - 1465-1734
pISSN - 1464-7141
DOI - 10.2166/hydro.2019.093
Subject(s) - groundwater , aquifer , environmental science , soil salinity , soil water , phreatic , transpiration , hydrology (agriculture) , soil horizon , soil science , geology , photosynthesis , geotechnical engineering , botany , biology
Grasslands are extensively distributed in flatland areas around the world, such as the Pampas in South America. It is one of the most economically productive landscapes and, as in other regions, they are being replaced by forests at increasing rates. Soil salinization emerges as a negative consequence associated with water deficit and forest groundwater consumption (∼250–500 mm/yr, in this region). An assessment of forest groundwater consumption is crucial for risk evaluation of soil salinization on flatland environments. For this aim, numerical modeling based on physical/biological processes and atmospheric boundary conditions was successfully applied in monitored grassland and afforested plots. Modeling results suggested a partial hydraulic disconnection between forest and phreatic aquifer due to the presence of petrocalcic horizons. Forest transpiration estimates were approximately 13% of total groundwater usage. Forest water consumption was then restricted to that soil portions above the petrocalcic horizons. Estimated forest transpiration rates (∼723 mm/yr) were similar to and even exceeded those reported in salinized sites with similar features. However, the risk of salinization of these soils was unlikely, because forest transpiration was restricted to the upper soil portions filled with fresh rainwater. The petrocalcic horizon retained water and prevented both deep drainage and, indirectly, soil salinization. doi: 10.2166/hydro.2019.093 s://iwaponline.com/jh/article-pdf/doi/10.2166/hydro.2019.093/607148/jh2019093.pdf C. R. Mujica (corresponding author) G. M. Milione S. A. Bea J. E. Gyenge Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET), Av. Rivadavia 1917, C1033AAJ Ciudad Autónoma de Buenos Aires, Argentina E-mail: cmujica@ihlla.org.ar C. R. Mujica G. M. Milione S. A. Bea Instituto de Hidrología de Llanuras ‘Eduardo J. Usunoff’, Av. República Italia 780, Azul, Buenos Aires 7300, Argentina J. E. Gyenge AER INTA, Tandil, EEA Balcarce INTA, Gral. Rodríguez 370, Tandil, Buenos Aires 7000, Argentina
Accelerating Research
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom
Address
John Eccles HouseRobert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom