[국내논문]한국 토양에 대한 포화침출액법과 1:5 법에 의한 전기전도도 간의 희석배수와 CEC의 관계에 대한 고찰 Discussion on Dilution Factor for Electrical Conductivity Measured by Saturation-paste Extract and 1:5 Soil to Water Extract, and CEC of Korean Soils원문보기
포화침출액의 전기전도도, ECe와 토양과 증류수를 1:5로 하여 측정된 EC1:5간의 직선 관계식의 경사 또는 희석 배수 (DF)에 대해 서로 독립적으로 발표된 연구 결과를 분석한 결과, DF는 CEC와 고도의 유의성을 보이는 부상관 관계에 있었다. 이 관계로부터 한국 대표 토양에 대한표토의 CEC로부터 산출한 DF는 사토에서 12.29, 식토에서 6.44이었다. 이 연구에서 포화수분점에 대한 조사가 이루어지지 않았으나, 측정된 EC1:5로부터 ECe를 추정할 때 토양의 CEC를 고려해야 하며, 제시된 토성에 따른 DF값의 적용이 바람직할 것으로 판단되었다.
포화침출액의 전기전도도, ECe와 토양과 증류수를 1:5로 하여 측정된 EC1:5간의 직선 관계식의 경사 또는 희석 배수 (DF)에 대해 서로 독립적으로 발표된 연구 결과를 분석한 결과, DF는 CEC와 고도의 유의성을 보이는 부상관 관계에 있었다. 이 관계로부터 한국 대표 토양에 대한표토의 CEC로부터 산출한 DF는 사토에서 12.29, 식토에서 6.44이었다. 이 연구에서 포화수분점에 대한 조사가 이루어지지 않았으나, 측정된 EC1:5로부터 ECe를 추정할 때 토양의 CEC를 고려해야 하며, 제시된 토성에 따른 DF값의 적용이 바람직할 것으로 판단되었다.
Linear regression analyses between the electrical conductivity of the saturation-paste extract. ECe, and the electrical conductivity of the 1:5 soil extract, EC1:5, for different soils yielded different dilution factors, or slopes with significant $r^2$ values from 0.842 to 0.905. The dil...
Linear regression analyses between the electrical conductivity of the saturation-paste extract. ECe, and the electrical conductivity of the 1:5 soil extract, EC1:5, for different soils yielded different dilution factors, or slopes with significant $r^2$ values from 0.842 to 0.905. The dilution factor was inversely proportional to the cation exchange capacity of soil which reflected textural difference. The dilution factors recommended for different textural classes ranged from 6.44 for clay soil to 12.29 for sandy soil based on the CEC's of the textural classes among 350 surface soils recorded in the Taxonomical Classification of Korean Soils except volcanic ash derived soils. Though saturation percentage of the saturation-paste of the soils in this study, CEC should be taken into account for dilution factor between ECe and EC1:5, and the suggested dilution factors might be reasonable estimate for the soil textural classes.
Linear regression analyses between the electrical conductivity of the saturation-paste extract. ECe, and the electrical conductivity of the 1:5 soil extract, EC1:5, for different soils yielded different dilution factors, or slopes with significant $r^2$ values from 0.842 to 0.905. The dilution factor was inversely proportional to the cation exchange capacity of soil which reflected textural difference. The dilution factors recommended for different textural classes ranged from 6.44 for clay soil to 12.29 for sandy soil based on the CEC's of the textural classes among 350 surface soils recorded in the Taxonomical Classification of Korean Soils except volcanic ash derived soils. Though saturation percentage of the saturation-paste of the soils in this study, CEC should be taken into account for dilution factor between ECe and EC1:5, and the suggested dilution factors might be reasonable estimate for the soil textural classes.
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제안 방법
ment factors for most Korean soils. However, since no measure of the saturation percentage of the saturation paste or in-situ volumetric moisture content of the samples were made, this study lacks supporting to ejqplicitfy explain the effect of soil moisture content on dilution factor. Despite the aforementioned drawback, the results of this study would be of practical use in predicting the ECe from the ECj:5.
The result of this study shows that the dilution factor varies depending on soil texture, more specifically on the CEC of soils, thus providing chemical analysis or field extension personnel with the reasonable estimates of the dilution ment factors for most Korean soils. However, since no measure of the saturation percentage of the saturation paste or in-situ volumetric moisture content of the samples were made, this study lacks supporting to ejqplicitfy explain the effect of soil moisture content on dilution factor.
대상 데이터
soil texture groups. The data of the surface soils of three hundred fifty soil series in the Taxanomical Classification of the Korean Soils surveyed by NIAST(2000), excluding the volcanic ash soils, were analyzed. We obtained dilution factors or slopes with cation exchange capacities in various soil textures by applying the regression equation in Fig.
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