Response of Total Nitrogen and Phosphorus Concentrations of Paddy Flooding Water to Fertilization under Rain-shielding Conditions

비가림 조건에서 시비에 대한 논담수 중 총질소 및 총인 농도 반응

  • 정재운 (전남대학교 대학원 지역.방이오시스템공학과) ;
  • 최우정 (전남대학교 농업과학기술연구소 생물산업공학과) ;
  • 윤광식 (전남대학교 농업과학기술연구소 생물산업공학과) ;
  • 김한용 (전남대학교 농업과학기술연구소 생물산업공학과) ;
  • 곽진협 (전남대학교 대학원 지역.바이오시스템공학과) ;
  • 임상선 (전남대학교 생물산업공학과) ;
  • 장남익 (국립환경과학원 영산강물환경연구소) ;
  • 허유정 (국립환경과학원 영산강물환경연구소)
  • Published : 2007.06.30

Abstract

Temporal changes in total nitrogen (T-N) and phosphorus (T-P) concentrations in paddy floodwater in response to fertilization under rain-shielding pot and small-scaled field conditions were investigated. On the basis of the changing patterns, suggestions for the use of fertilization factors, such as days after fertilization, in developing models for the estimation of T-N and T-P loads from paddy fields were made. Total N concentration was susceptible to fertilization, showing a peak concentration right after fertilization followed by a decreasing pattern with the elapse of days after fertilization. The decreasing pattern of T-N concentration followed the first- order kinetics, indicating that the models are likely to be an exponential equation using days after fertilization as an independent variable. Comparison between the pot and field experiments conducted with soils different in soil fertility revealed that indigenous soil N concentration significantly affected T-N concentration, and this suggests that soil N status can be used as the second variable for the models. Meanwhile, temporal changes in T-P concentration did not respond to P fertilization as sensitively as T-N. In combination with other published results, our study suggests that rainfall intensity and other factors associated with farming activities that are likely to cause disturbance of soil particles containing P may be used as possible variables for the models.

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