不同水肥耦合下双季稻氮磷吸收、利用与流失差异

为优化双季稻水肥管理措施,在福建省东部双季稻区设置田间径流小区试验,研究了T₀(对照,未施肥+常规灌溉)、T₁[习惯施肥(273 kg N·hm^-2, 59 kg P·hm^-2, 112 kg K·hm^-2)+常规灌溉]、T₂[优化施肥(240 kg N·hm^-2, 52 kg P·hm^-2, 198 kg K·hm^-2)+常规灌溉]和T₃(优化施肥+节水灌溉)4种水肥耦合处理下双季稻产量、养分吸收利用及田面水氮、磷流失变化。结果表明: 与T₀相比,T₁、T₂和T₃处理早稻稻谷产量显著提高了0.7、1.0和1.1倍,晚稻稻谷产量显著提高了0.9、1.1和1.0倍;T₁、T₂和T₃处理早、晚稻植株地上部分,尤其稻谷氮、磷吸收量增加显著,早稻稻谷氮吸收量分别增加1.1、1.2和1.2倍,磷吸收量增加0.9、1.4和1.6倍,晚稻稻谷氮吸收量增加0.8、1.0和1.0倍,磷吸收量增加0.7、0.9和0.9倍。T₃比T₁处理早稻氮、磷肥农学利用率分别显著增加71.1%和69.2%,晚稻分别显著增加26.4%和25.0%,但田面水可溶性总氮流失量减少了16.0%,并以硝态氮流失为主;T₂与T₃处理早晚稻氮、磷肥农学利用率差异均不显著。本试验中的优化水肥管理措施(T₃)既能促进水稻氮、磷吸收利用,提高双季稻产量,又能降低早稻田面水氮素尤其是硝态氮的流失。本研究可为福建省东部双季稻区水肥利用管理和氮、磷面源污染防治提供理论支持。

Differences in uptake,utilization and loss of nitrogen and phosphorus in a Chinese double rice cropping system under different irrigation and fertilization managements

In order to optimize water and fertilizer use in the double-cropping rice in eastern Fujian Province, a field runoff plot experiment was conducted to investigate rice yield, nutrient uptake, and runoff losses of N (nitrogen) and P (phosphorus) in the T₀(no chemical fertilization with traditional flooding irrigation), T₁(common chemical fertilizer of 273 kg N·hm^-2, 59 kg P·hm^-2, and 112 kg K·hm^-2 combined with traditional flooding irrigation), T₂(chemical fertilizer of 240 kg N·hm^-2, 52 kg P·hm^-2, and 198 kg K·hm^-2 combined with traditional flooding irrigation) and T₃(chemical fertilizer combined with shallow intermittent irrigation) treatments. Results showed that early rice grain yield in the T₁, T₂ and T₃ treatments significantly increased by 0.7, 1.0, 1.1 times, late rice grain yield significantly increased by 0.9, 1.1, 1.0 times compared to that in the T₀ treatment, respectively. The T₁, T₂ and T₃ treatments significantly increased the uptake of N and P in aboveground parts of the plants, especially in grains. The T₁, T₂ and T₃ treatments significantly increased N uptake by 1.1, 1.2, 1.2 times, increased P uptake by 0.9, 1.4, 1.6 times in early-season grains, and significantly increased N uptake by 0.8, 1.0, 1.0 times, increased P uptake by 0.7, 0.9, 0.9 times in late-season grains, compared to T₀, respectively. Furthermore, T₃ increased agronomic N use efficiency (AEN) and agronomic P use efficiency (AEP) by 71.1% and 69.2% in early rice plants, increased AEN and AEP by 26.4% and 25.0% in late rice plants, whereas T₃ decreased total dissolved N (DN) by 16.0% in comparison with T₁. Dissolved inorganic N loss in surface runoff occurred mainly in the form of NO₃^--N (nitrate N) under different water and fertilizer regimes. However, there were no significant differences in AEN and AEP between T₂ and T₃ treatments. These findings suggested that optimal applications of water and fertilizers (T₃) might increase N and P uptake in rice plants, maintain yield, and reduce N loss, especially in the form of NO₃^--N in surface water from early rice field. In general, this study could provide theoretical support for the optimization of irrigation and fertilization and for the control of N and P non-point source pollution from the double cropping rice paddy fields in eastern Fujian Province.