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Impact of water percolation on nutrient leaching from an irrigated paddy field in Japan
Author(s) -
Katoh M.,
Iwata A.,
Shaku I.,
Nakajima Y.,
Matsuya K.,
Kimura M.
Publication year - 2003
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.1475-2743.2003.tb00319.x
Subject(s) - leaching (pedology) , nutrient , agronomy , irrigation , environmental science , paddy field , drainage , soil water , human fertilization , zoology , chemistry , soil science , biology , ecology , organic chemistry
. We examined the effect on soil nutrient status and sustainability of water percolation through an irrigated paddy field in Japan, to the depth of drainage (40 cm). The difference between amounts of nutrients leached by percolation and those supplied by irrigation indicated that 25–130 kg ha −1 Ca, 8–24 kg ha −1 Mg, from −1 to 9 kg ha −1 K, and 8–17 kg ha −1 Fe, respectively, were lost each year from the 0–40 cm soil layer during rice cultivation, when the supply from fertilization and rainfall and the loss in grain harvest were not accounted for. When the supply of K from rainfall and the loss in grain harvest were taken into account, a total K loss of about 10 kg ha −1 was estimated. The electrical neutrality of inorganic ions in the percolating water was always maintained. From these results we estimate that the amounts of exchangeable Ca and Mg in the soil to a depth of 40 cm would decrease by 50% within 50–260 and 30–100 years, respectively, if similar management were continued without fertilization. The total amount of carbon dioxide (ΣCO 2 ) leached in percolating water during the period of rice cultivation was 120–325 kg C ha −1 , which corresponded to 0.47–0.94% of the soil organic carbon to 40 cm depth.