초록
원자력시설(原子力施設)에서 방출(放出)될 수 있는 장반감기핵종중(長半減期核種中)의 하나인 $Cs^{137}$을 5개 답토양(畓土壤)에 처리(處理)하여 토양중(土壤中)에서의 흡(吸) 탈착상태(脫着狀態)를 조사하여 다음과 같은 결과를 얻었다. 1. $Cs^{137}$은 토양(土壤)에 다량(多量) 흡착(吸着)되며 치환성형태(置換性形態)의 탈착량(脫着量)은 K첨가에 따라서는 감소(減少)하였고, $Cs^{137}$ 처리량(處理量)의 증가에 따라서는 비례적으로 증가하였으며 치환성형태의 탈착량(脫着量)은 수용성(水溶性)에 비하여 매우 높았다. 2. 토양(土壤)에 첨가된 $Cs^{137}$의 존재형태(存在形態)는 토양(土壤)에 따라서 차이(差異)가 있으나 평균적으로 수용성(水溶性)이 5.9%, 치환성(置換性)이 17.1%, 비치환성(非置換性)이 77.0%로 나타났다. 3. 토양(土壤)에 흡착(吸着)된 $Cs^{137}$의 수용성(水溶性) 및 치환성탈착량(置換性脫着量)은 토양(土壤)pH와 치환성 염기함량의 증가에 따라 감소(減少)하였고, 유기물과 점토함량(粘土含量)의 증가에 따라서는 증가하였다. 4. 토양(土壤)에 흡착(吸着)된 $Cs^{137}$은 Illite와 Vermiculite가 많은 토양(土壤)에서 비치환성형태(非置換性形態)로의 흡착(吸着)이 많았다.
This experiment was conducted to examined the effects of the physico-chemical and mineral-logical properties of paddy soil on the desorption of $Cs^{137}$ from radionuclide, $Cs^{137}$ absorbed soils. 1. Adsorption of $Cs^{137}$ by paddy soil was very much and exchangeable fraction of $Cs^{137}$ extracted by ammonium acetate was very high compared to the water soluble fraction. Exchangeable fraction of $Cs^{137}$ in paddy soil decreased with the increase of potassium application and increased proportionally with the increase of $Cs^{137}$ treatment. 2. The distribution of several forms of $Cs^{137}$ in soils depend on the soil type. Average-distribution rates of water soluble, exchangeable and non-exchangeable fractions of $Cs^{137}$ in soils were 5.9%, 17.1% and 77.0%, respectively. 3. The desorption of $Cs^{137}$ from adsorbed soils decreased with increase of pH and exchangeable cations of the soils, but it increased as organic matter and clay content increase in soil. 4. Non-exchangeable adsorption of $Cs^{137}$ was high in the soils of which both Illite and Vermiculite were dominant.