Effect of Flooding and Organic Matter to the Release of Iron, Manganese, and Silica in Soils

침수처리(湛水處理) 및 유기물(有機物) 첨가(添加)가 답토양(畓土壤)의 Fe, Mn 및 SiO2의 용출량(溶出量)에 미치는 영향(影響)에 관(關)한 연구(硏究)

  • Park, Y.S. (Institute of Plant Environment, Office of Rural Development) ;
  • Oh, W.K. (Institute of Plant Environment, Office of Rural Development) ;
  • Park, N.J. (United Nations Special Fund Korean Soil Fertility Project)
  • 박영선 (농촌진흥청 식물환경연구소) ;
  • 오왕근 (농촌진흥청 식물환경연구소) ;
  • 박내정 (한국토양비옥도사업기구)
  • Published : 1968.12.31

Abstract

A low yielding paddy soil was water logged at $30{\pm}2^{\circ}C$ with soluble starch as a easily decomposable organic matter for 3 weeks in the laboratory. The relation of pH and Eh changes and soluble iron, manganese and silica was investigated. The experimental results obtained were summarized as follows; 1. When organic matter was applied, reduction of the soil was severer, that is, Eh value was lower by 200 mv. for a week in the beginning of submergence. 2. pH of the untreated soil was dropped a little just after submergence, and then gradually increased to 60. When treated, pH was increased due to abrupt drop of Eh in the beginning but decreased to 4.5 after a week, and became constant at this pH value. 3. Slight increase in soluble iron, manganese and silica was observed in the untreated soil whereas soluble iron, manganese and silica in the treated soil were increased about 20, 10, and 3 times, respectively. 4. When soluble starch was treated, pH and soluble silica or manganese was highly correlated[($H^+$) and Mn ${\gamma}=0.734^{**}$, ($H^+$) and $SiO_2$ ${\gamma}=0.923^{**}$] and below pH 5.0, release of these element was rapidly increased.

수량(收量)이 낮은 답토양(畓土壤)에 역분해성(易分解性) 유기물(有機物)로서 Soluble Starch를 첨가(添加)하여 $30{\pm}2^{\circ}C$에서 21 일간(日間) 담수(湛水) Incubation 하면서 토양(土壤)의 pH, Eh 변화(變化), 수용성(水溶性) Fe, Mn 및 $SiO_2$의 용출량(溶出量)을 조사(調査) 연구(硏究)한 결과(結果)를 요약(要約)하면 다음과 같다. 1. 유기물(有機物)을 첨가(添加)할 경우(境遇)에는 유기물(有機物)을 처리(處理)하지 않았을때 보다 초기(初期) 1주일간(週日間) Eh는 200mv 더 낮아 환원(還元)이 심(甚)하였다. 2. pH는 무처리(無處理)에서는 담수초기(湛水初期) 약간 하강(下降)하는 경향(傾向)이다가 계속(繼續) 상승(上昇)하여 pH 6.0 정도(程度)를 유지하였으나 유기물처리시(有機物處理時)에는 초기(初期)에는 급격(急激)한 환원(還元)에 의(依)해 pH가 상승(上昇)하였다가 7 일후(日後)에는 떨어져서 계속(繼續) pH 4.5 정도(程度)를 유지(維持)하였다. 3. 유기물(有機物)을 처리(處理)하지 않았을때는 수용성(水溶性) Fe, Mn 및 $SiO_2$는 담수환원(湛水還元)에 의(依)하여 약간 증가(增加)를 보이고 있으나 유기물처리시(有機物處理時)에는 수용성(水溶性) Fe는 약(約) 20배(倍), Mn 약(約) 10배(倍) $SiO_2$는 3배정도(倍程度)로 증가(增加)하였다. 4. 유기물(有機物) 처리시(處理時)에 수용성(水溶性) Mn 및 $SiO_2$의 용출량(溶出量)은 pH와 유의적(有意的)인 상관관계(相關關係)([$H^+$] & Mn ${\gamma}=0.734^{**}$, [$H^+$] & $SiO_2$ ${\gamma}=0.750^{**}$)가 있었으며 pH5.0 이하(以下)에서 용출량(溶出量)이 급증(急增)하였다.

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