Korean Journal of Soil Science and Fertilizer (한국토양비료학회지)
- Volume 27 Issue 2
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- Pages.72-77
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- 1994
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- 0367-6315(pISSN)
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- 2288-2162(eISSN)
Influence of Fly Ash Application on Content of Heavy Metal in the Soil II. Content Change by the Successive Application
석탄회(石炭灰) 시용(施用)이 토양중(土壤中) 중금속(重金屬) 함량(含量)에 미치는 영향(影響) II. 운용(連用)에 따른 함량변화(含量變化)
- Kim, Bok-Young (Agricultural Science Institute, RDA) ;
- Lim, Sun-Uk (College of Agriculture and Life Science, Seoul National University) ;
- Park, Jong-Hyun (Research Center, Korea Electric Power Corporation)
- Published : 1994.06.30
Abstract
This study was conducted to investigate the influence of treatment of fly ash on heavy metal contents of the arable soil. Rice was cultivated on the two types of paddy field clay loam and sandy loam with 0, 12ton/10a of anthracite fly ash and bituminous coal fly ash application. And soybean was cultivated at the same type of upland fields with those ashes of 0, 9ton/10a, yearly for three years. At the harvest time, the heavy metal contents in the different layer were investigated. The results were summarized as follows : 1. The contents of some heavy metal were increased in the surface soils but didn't show the tendency in the deeper layer or soil texture. 2. In the paddy fields, the contents of Cd, Cu, Zn, Cr were increased. Meanwhile and the upland fields, the contents of Cd and Cr were increased with the successive application of Anthracite fly ash, but the others didn't show those tendency. 3. The contents of Cd, Cu and Zn in the paddy field, were increased but the upland field, the contents of Cd, Cr and Ni were increased by the successive application of bituminous coal fly ash.
무연탄회(無煙炭灰)와 유연탄회(有煙炭灰)를 논토양(土壤)의 식양토(植壤土)와 사양토(砂壤土)에 각 12톤/10a씩 3('91~'93)연간(年間) 연용(連用)하고, 밭 토양(土壤)도 식양토(植壤土)와 사양토(砂壤土)에 각 9톤/10a씩 3년('91~'93)간 연용하면서 벼와 콩을 각각 재배(栽培)한 후에 토양(土壤)을 I, II, III층으로 구분 채취(採取)하여 중금속(重金屬)인 Cd, Cu, Pb, Zn, Ni, Cr, Fe, Mn함량(含量)을 조사(調査)한 결과(結果)는 다음과 같다 1. 토양(土壤) 깊이별(別) 중금속(重金屬) 함량(含量)은 표층(表層)이 가장 높고 토심이 깊어질수록 낮았으며 석탄회(石炭灰) 시용량(施用量) 증가(增加)에 따라서 논 밭 모두 표층(表層)에서만 일부 성분이 증가(增加) 경향이 있고 심층(深層)은 일정한 경향이 없었으며, 토성(土性)에 따라서도 일정한 경향이 없었다. 2. 무연탄회(無煙炭灰)는 논토양(土壤)에서는 Cd, Cu, Zn, Cr함량(含量)이, 밭토양(土壤)에서는 Cd, Cr함량(含量)이 증가(增加)되었고 그 함량(含量)은 우리나라 평균치(平均値) 또는 평균치(平均値)+표준편차(標準偏差) 범위(範圍)이었다. 3. 유연탄회(有煙炭灰)는 논토양(土壤)에서는 Cd, Zn, Cr함량(含量)이 밭토양(土壤)에서는 Cd, Zn, Cr, Ni함량(含量)이 증가(增加)되는 경향이었고. 그 함량(含量)은 우리나라 평균치(平均値) 또는 평균치(平均値)+표준편차(漂準偏差) 범위(範圍)이었다.