Study on White Precipitate in Most of Waters after Thawing

물이 해동한 다음 발생하는 휜 침전물의 정성분석 및 이온의 변화

  • 윤수철 ((주)동원 F&B 식품연구소) ;
  • 박해룡 ((주)동원 F&B 식품연구소) ;
  • 윤형식 ((주)동원 F&B 식품연구소) ;
  • 김창수 (국립환경연구원 수질연구부)
  • Published : 2002.03.01

Abstract

The objectives of this study were to investigate the change of silicon, cations and anions dissolved in water before and after thawing, and analyzed what the white-colored precipitate (WP) farmed after thawing was composed of. The silicon concentration that has been changed might have been compared with the weight of WP under water-free state. The major component of WP has been approved to be a silicon, while calsium was only a little contained. As the weight of WP has been nearly equal to the reduced silicon concentration, the weight of its could be changeable calculated by silica (SiO$_2$) molecular weight. Therefore, WP could have been presumed to be a silica. The more silicon concentration was increased, the more weight of silicon was increased. Except for the sample "C", the amounts of cations and anions could be found to be unchangeable nearly. As a result of that, WP has been apparent to be silica itself while most of ions (excluded with Si) of any others were not changed.

Keywords

References

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