Studies on the Alleviation of Heavy Metal (Cadmium) Damage through Soil Improvement (Extraction of Cadmium and the Damage through Exchangeable Cd⁺⁺ by the Application of Soil Amendments)

중금속(重金屬)(Cd)의 피해경감(被害輕減)을 위(爲)한 토양개량(土壤改良)에 관(關)한 연구(硏究) I. Cd침출(浸出)과 개량제(改良劑) 시용(施用)으로 인(因)한 치환성(置換性) Cd의 감소(減少)

Effects of lime and ameliolating materials on decreasing available soil cadmium were studied, applying the amendments to Cd pre-and post-treated soils. Soil sttreated with Cd were placed in pots and kept under field moisture condition, summer through winter in 1981. The results of soil analysis made 40 to 60 days after the Cd treatment are as follows ; 1. Greater amount of Cd was extracted by 0.1N-HCl or 2% Citric acid than N-AcNH4 solution. More Cd was dissoluted by 0.1-HCl than 2% Citric acid. No Cd was extracted by pure water. Showing a wide variance in the amount of extractable Cd among treatments (amendments), the $N-AcNH_4$ solution seemed to be the most effective extracting solution of available soil cadmium. 2. Calcium hydroxide was the most effective materials in reducing $N-AcNH_4$ extractable Cd, followed by calcium carbonate and calcium silicate. 3. Superphosphate is also effective in reducing exchangeable cadmium. The reduction seemed to be attributed to the precipitation of cadmium phosphate. 4. The exchangeable cadmium by $N-AcNH_4$ was large in the soil pH range of 6.0 and 6.5, and it decreased as the soil pH became far apart from these values. The decrese of exchangeable Cd at low pH seemed to be related to the increase of $Mn^{+{+}}$ and that at the high pH to the precipitation as Cd-hydroxide.

카드뮴의 해독(害毒)을 경감(輕減)하는데 필요(必要)한 기초지식(基礎知識)을 얻기 위(爲)하여 카드뮴이 처리(處理)된 토양(土壤)에 석회물질(石灰物質)과 개량제(改良劑)를 사용(使用)한 것과 이미 석회(石灰)가 사용(使用)된 토양(土壤)에 Cd를 처리(處理)한 것을 분(盆)에 담아서 1981년(年) 여름 또는 가을에 자연토양수분조건하(自然土壤水分條件下)에 묻고 처리후(處理后) 40일(日)~70일(日)사이에 토양시료(土壤試料)를 채취분석(採取分析)한 결과(結果)는 다음과 같다. 1. 카드뮴은 토양(土壤)을 0.1N-HCl나 2%구연산으로 침출(浸出)했을 때에 많고, $N-AcNH_4$로 침출(浸出)했을때 적었으며 물로 침출(浸出)했을 때는 나오지 않았다. 침출(浸出)된 카드뮴의 처리간(處理間) 차이(差異)는 $N-NH_4A$ 침출(浸出)에서 가장 뚜렷하여 이것을 유효카드뮴으로 할 수 있을 것 같다. 2) 치환성(置換性)카드뮴을 줄이는데 가장 유효한 것은 수산화(水酸化)카드뮴이며 탄산(炭酸)카드뮴, 규산(珪酸)카드뮴의 순서(順序)로 효과가 적어졌다. 3. 과석(過石)도 치환성(置換性)카드뮴을 줄였는데 인산(燐酸)카드뮴을 침전(沈澱)시키기 때문으로 판단(判斷)되었다. 4. 치환성(置換性)카드뮴은 토양(土壤)의 pH 6.0~6.5에서 많고 그 이하(以下)나 이상(以上)에서 적었다. pH 5.0이하(以下)에서는 $Mn^{+{+}}$으로 인(因)한 $Cd^{+{+}}$의 침전(沈澱)때문이고, pH 6.0이상(以上)에서는 수산화(水酸化)카드뮴의 침전(沈澱)때문으로 판단(判斷)되었다.