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Phosphorus interception in floodwater of paddy field during the rice-growing season in TaiHu Lake Basin

机译:太湖流域水稻生长期稻田洪水中的磷截留

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摘要

A field experiment located in TaiHu Lake Basin in China was conducted, by application of superphosphate or a mixture of superphosphate with manure, to elucidate the interception of P export during a typical rice growing season through 'zero-drainage water management' combined with sound irrigation, rainfall forecasting and field drying. P concentrations in floodwater rapidly declined before the first event of field drying, and subsequently tended to return to the background levels. Before the first field drying TPP was the predominant P form in floodwater on fields with no P input, DRP on plots that received superphosphate only, and DOP on plots treated with the mixture of superphosphate and manure. Thereafter TPP became the major form. No P export was found from the paddy fields, but a retention of 0.65 kg ha~(-1), mainly due to soil P sorption. The results recommend the zero-drainage water management for full-scale areas for minimizing P export.
机译:通过使用过磷酸钙或过磷酸钙与肥料的混合物,在中国太湖流域进行了田间试验,以通过“零排水管理”结合合理灌​​溉来阐明典型水稻生长季节对磷出口的拦截。 ,降雨预报和田间干燥。在第一次田间干燥之前,洪水中的磷浓度迅速下降,随后趋于回到本底水平。在第一次田间干燥之前,TPP是无磷田地中洪水中的主要P形式,在仅接受过磷酸钙的田地上是DRP,在用过磷酸钙和肥料的混合物处理过的田地上是DOP。此后,TPP成为主要形式。稻田中没有磷的输出,但保留量为0.65 kg ha〜(-1),这主要是由于土壤对磷的吸收。结果建议对零排放进行全面管理,以最大程度地减少磷的出口。

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