비소광산(砒素鑛山) 및 제련소(製鍊所) 인근답(隣近畓)에서 수확기(收穫期)에 토양(土壤)과 정조(正租)를 동시(同時)에 채취(採取)하여 토양중(土壤中) 비소(砒素)를 수용태(水容態)As, Al태(態)As, Fe태(態) As, Ca태(態)As, 잔여태(殘餘態)As로 분별분석(分別分析)하고 이들 형태별(形態別) As와 토양특성(土壤特性) 및 1N HCl가용성(可溶性) As함량(含量)과의 관계(關係)와 비소형태별(砒素形態別) 함량(含量) 및 1N HCl가용성함량(可溶性含量)과 현미중(玄米中) As함량(含量)과의 관계(關係)를 조사(調査)한 결과(結果)는 다음과 같다. 1. 형태별(形態別) As분포비(分布比)는 토양특성(土壤特性)에 따라 차이(次異)가 심(甚)하였으며, 무기태(無機態) As의 분포(分布)는 광산(鑛山) 및 제련소(製鍊所) 두지역 모두 Fe태(態)As>Al태(態)As>Ca태(態)As>수용성(水溶性)As의 순(順)이었고 잔여태(殘餘態)As(유기태(有機態)As+부용태(不溶態)As)는 광산지역(鑛山地域)이 제련소지역(製鍊所地域)보다 월등히 높았다. 2. pH가 높은 토양(土壤)일수록 두지역(地域) 모두 Al태(態)As 및 Fe태(態)As는 감소(減少)하나 Ca태(態)As 및 잔여태(殘餘態)As는 증가(增加)하는 경향(傾向)이며, 유기물(有機物) 함량(含量)과 이들 지역(地域)의 형태별(形態別) As분포(分布)와의 관계는 뚜렷한 경향(傾向)이 없었고 C.E.C가 높은 토양(土壤)일수록 Al태(態)As는 감소(減少)하나 그외(外) 형태(形態)의 As는 증가(增加)하는 경향(增加)임. 3. 토양중(土壤中) 활성(活性) 알루미늄 및 철함량(鐵含量)과 치환성(置換性) 칼슘함량(含量)은 토양중(土壤中) Al-As, Fe-As, 및 Ca-As분포비(分布比)와 각각정(各各正)의 상관(相關)을 나타내었으며 이들간의 상관(相關)은 광산지역(鑛山地域)이 제련소지역(製鍊所地域)보다 높았다. 4. 수용성(水溶性) 비소(砒素)를 제외(除外)한 토양중(土壤中) 비소형간(砒素形間)에는 서로 높은 정(正)의 상관(相關)이 있었고 비소형태(砒素形態)와 1N-HCl 침출법간(浸出法間)에도 같은 경향(傾向)이었다. 5. 현미중(玄米中) 비소함량(砒素含量)은 Al태(態)As함량(含量)과 가장 높은 상관(相關)을 나타내었으며 Fe태(態)As 및 Ca태(態)As와 Total As 및 1N HCl 가용성(可溶性) As함량(含量)과도 유의성(有意性) 있는 정(正)의 상관(相關)을 나타내었다.
This study was carried out to investigate the distribution of arsenic (As) fractions in paddy soils in relation to some soil characteristics and to find out the relationship between As fractions in soil and As content in brown rice. Soils and rice samples were collected from paddy field adjacent to arsenic mining and refinery sites. Sequential extraction procedures were used to fractionate As in soils into the designated forms of water soluble-As, Al-As, Fe-As, Ca-As, and residual-As. The results obtained were as follows: 1. The percent distribution of As fractions in soil showed a wide difference depending on some soil properties. The relative abundance of the extractable inorganic As fractions was in the order of Fe-As>Al-As>Ca-As>Water soluble-As regardless of mining and refinery sites. Residual-As fraction was more abundant in mining site than in refinery site. 2. With increasing soil pH, the percent distribution of Fe-As and Al-As fractions were decreased, but that of Ca-As and Residual-As fractions increased. The percent distribution of Al-As fraction in soil was negatively correlated with soil CEC, but others showed positive relationships. 3. Active Al and Fe content, and exchangeable Ca content in soil were positively correlated with the percent distribution of Al-As, Fe-As, and Ca-As fractions in soil respectively, and higher correlation between them was shown in mining site than in refinery site. 4. Soil As fractions, except for water soluble-As, showed significant correlation with among each others and also with 1N HCl extration method using as the common soil As extractant in Korea. 5. Arsenic content in brown rice had highly significant correlation with Al-As fraction in soil and it also showed significant correlation with Fe-As and Ca-As fractions, Total-As, and 1N-HCl extractable As.
