한국토양비료학회지 (Korean Journal of Soil Science and Fertilizer)
- 제34권6호
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- Pages.373-379
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- 2001
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- 0367-6315(pISSN)
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- 2288-2162(eISSN)
잔적 암쇄토의 화학조성과 풍화도
The Weathering and Chemical Composition of Young Residual Entisols in Korea
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Zhang, Yong-Seon
(National Institute of Agricultural Science and Technology, RDA) ;
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Jung, Pil-Kyun
(National Institute of Agricultural Science and Technology, RDA) ;
- Kim, Sun-Kwan (National Institute of Agricultural Science and Technology, RDA) ;
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Jo, In-Sang
(National Institute of Agricultural Science and Technology, RDA)
- 발행 : 2001.12.30
초록
우리 나라 산지토양의 주요 모암에서 발달된 잔적층 암쇄를 대상으로 토양의 단면 특성, 이화학적 특성 X-선 형광분석 (XRF)을 통하여 모재에 따른 토양의 화학조성 변화와 주요한 구성원소의 풍화량을 토양층위 및 모암별로 비교하였다. 모암에 관계없이 토양의 C층에 비하여 A층에서 점토함량, 양이온 치환용량 (CEC), 유기물 함량은 높았으며, 용적밀도 (
The weathering rates and change of chemical composition of 6 residual Entisols derived from granite, granite-gneiss, limestone, sandstone, shale, amd basalt in Korea were studied. The chemical composition of each profile with parent rocks were determined using XRF with the physico-chemical properties and the morphology of soils. In the A horizons of all the soils except Euiseong series, the content of clay, organic matter and cation exchange capacity(CEC) showed higher than those of C horizon, but bulk density and pH showed lower than C horizon. Clay content in the soil from sandstone was decrease with soil depth, which may caused by the elluriation. In total element analysis.