[Ammonia volatilization from rice field under different water conditions in lower Liaohe River Plain].
Zhenhua Chen, Lijun Chen, Wu Zhi, Yulan Zhang, Yinghua Juan
Abstract
Zhenhua Chen, Lijun Chen, Wu Zhi, Yulan Zhang, Yinghua Juan
Abstract
With ventilating chamber, this paper measured the ammonia volatilization from a meadow brown soil rice field after N fertilization under different water conditions in lower Liaohe River Plain. The results showed that there was an obvious ammonia volatilization after N fertilization. The total ammonia volatilization during rice growth period was 11.64-34.01 kg N x hm(-2), accounting for 4.66%-11.66% of applied N. The volatilization loss of applied N at different growth stages followed the order of tillering stage > booting stage > before transplanting, and the peak was appeared at 2-4 days after N fertilization. Field water condition had a strong effect on ammonia volatilization. Under waterlogging, both the amount of total ammonia volatilization and the percentage of lost fertilizer N were higher, and the ammonia volatilization rate increased with increasing N application rate, being significantly different among different N levels (P < 0.05). Under un-waterlogging, the ammonia volatilization was relatively low. N application rate and the ammonium concentration and pH in surface water were the main factors affecting ammonia volatilization, while P application rate had little effect when the N application rate was 180 kg N x hm(-2).
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With ventilating chamber, this paper measured the ammonia volatilization from a meadow brown soil rice field after N fertilization under different water conditions in lower Liaohe River Plain. The results showed that there was an obvious ammonia volatilization after N fertilization. The total ammonia volatilization during rice growth period was 11.64-34.01 kg N x hm(-2), accounting for 4.66%-11.66% of applied N. The volatilization loss of applied N at different growth stages followed the order of tillering stage > booting stage > before transplanting, and the peak was appeared at 2-4 days after N fertilization. Field water condition had a strong effect on ammonia volatilization. Under waterlogging, both the amount of total ammonia volatilization and the percentage of lost fertilizer N were higher, and the ammonia volatilization rate increased with increasing N application rate, being significantly different among different N levels (P < 0.05). Under un-waterlogging, the ammonia volatilization was relatively low. N application rate and the ammonium concentration and pH in surface water were the main factors affecting ammonia volatilization, while P application rate had little effect when the N application rate was 180 kg N x hm(-2).
Key concepts: Ammonia volatilization from urea, Volatilisation, Ammonia, Fertilizer, Chemistry, Waterlogging (archaeology), Human fertilization, Nitrogen