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Simulating the impact of irrigation management on the water and salt balance in drained marsh soils (Marismas, Spain)
Author(s) -
Andreu L.,
Jarvis N.J.,
Moreno F.,
Vachaud G.
Publication year - 1996
Publication title -
soil use and management
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.709
H-Index - 81
eISSN - 1475-2743
pISSN - 0266-0032
DOI - 10.1111/j.1475-2743.1996.tb00530.x
Subject(s) - irrigation , environmental science , leaching (pedology) , soil water , mediterranean climate , soil salinity , water balance , hydrology (agriculture) , salinity , water table , soil salinity control , growing season , leaching model , agronomy , soil science , groundwater , geology , geography , archaeology , oceanography , geotechnical engineering , biology
. Using the simulation model MACRO, this paper investigates the likely consequences of reduced irrigation inputs on the water and salt balance and crop growth in a drained, saline clay in a Mediterranean climate (Marismas, SW Spain). The model was first successfully validated against field measurements of the soil water and chloride balance, water table depths and drain outflows in the 1989 growing season. Three‐year simulations were then performed assuming two different irrigation applications (60 and 75% reductions from the 1989 amount) and two different frequencies (12 or 6 irrigations per growing season). The model predictions suggested that reduced irrigation may lead to up to a 15%) increase in the chloride content of the soil profile after 3 years. Also, despite overall reductions in water discharge, slight increases in chloride leaching via field drains ( c. 4 to 8%) were predicted. The model demonstrated that encroachment of salt into the soil profile may he exacerbated by the non‐equilibrium nature of water flow and solute transport (‘by‐passing flow’) in structured clays. With reduced water supply for irrigation, more frequent applications may give marginally better crop yields for the same quantity of irrigation but at the expense of slightly increasing salt concentration in the root zone.