透冠水对稻田生态系统养分再循环的作用初报

A PRELIMINARY STUDY ON HE CONTRIBUTION OF THROUGHFALL TO NUTRIENT RECYCLING IN RICE FIELD ECOSYSTEMS

  • 摘要: 本文初步研究了杂交水稻(汕优6号)生育后期(拔节孕穗期至成熟期)透冠水的化学组成及其在稻田生态系统养分再循环中的作用。结果表明,自然降水穿过水稻冠层之后其化学组成发生明显变化,氮、磷、钾、钙、镁和硅等元素的浓度都有所增加。乳熟期出现氮、钾、钙、镁和硅浓度的“峰值”。计算养分通过透冠水的再循环量氮达15.91kg/ha,磷、钾、钙、镁和硅分别为1.11、3.78、1.13、1.70和8.52kg/ha。养分(特别是氮素)通过透冠水返回土壤很可能是稻田生态系统养分再循环的重要机制。

     

    Abstract: A prelimipary study Was made on the chemical composition of throughfall and its contribution to the nutrient recycling in rice field ecosystem at the late growth stages ( from booting to ripening stage )of hy-brid rice ( Xianyou no. 6 ) . The results showed that the chemical composition of precipitation remarkably changed when it passed through the rice canopy, the concentrationsm of N, P, K, Ca, Mg and Si Were increased.Peak concentrations of these elements occured in milky stage of rice growth.The amount of N, P, K, Ca, Mg and Si recycled by throughfall were 15.91, 1.11, 3-70, 1.13, 1.70 and 8.25 kg/ha respectively.It appeared that the nutrients (especially N)returned to soil by throughfall may be an important mechanism of nutrient recycling in rice field ecosystems.

     

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