• 한국토양비료학회지
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• 제34권1호
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• pp.71-75
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• 2001

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.

• 한국환경농학회지
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• 제38권2호
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• pp.69-75
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• 2019

BACKGROUND: Measurement of electrical conductivity of saturated soil paste ($EC_e$) for assessment of soil salinity is time-consuming, and thus conversion of EC of 1:5 soil-water extract ($EC_{1:5}$) to $EC_e$ using a dilution factor may be of help to monitor salinity of huge number of soil samples. This study was conducted to evaluate the dilution factor for reclaimed tideland (RTL) soils of South Korea. METHODS AND RESULTS: Soil samples (n=40) were collected from four RTLs, and analyzed for $EC_{1:5}$, $EC_e$, and cation compositions of 1:5 soil-water extract. The dilution factor (8.70) was estimated by regression analysis between $EC_{1:5}$ and $EC_e$, and the obtained dilution factor was validated by applying to an independent data set (n=96) of $EC_{1:5}$ and $EC_e$. The $EC_e$ measured and predicted was strongly correlated ($r^2=0.74$, P<0.001), but $EC_e$ was overestimated by 16% particularly for the soils with high clay content and low sodium adsorption ratio (SAR). CONCLUSION: This study suggests that using the dilution factor to convert $EC_{1:5}$ to $EC_e$ is feasible method to monitor changes in the soil salinity of the study RTL. However, overestimation of $EC_e$ should be cautioned for the soils with high clay content and low SAR.

• 한국농공학회:학술대회논문집
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• 한국농공학회 2002년도 학술발표회 발표논문집
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• pp.405-408
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• 2002

The electrical conductivity, EC is a major indicator of soil salinity. Measuring EC of saturation-paste extract of soil, ECe, is the standard way to evaluate soil salinity. However much of the data on soil salinity have been obtained by measuring the EC of the 1:5 soil-to-water extract, EC(1:5) or salts contents(%) which multiplied by conversion factor. And, thus we attempted to collect and analysis 90 soil samples at 9 reclaimed tidelands in Korea and to derive a relationship between ECe and dilution factor at ECe and EC(1:5), $DF_{1:5}$ of 3 soil textural conditions and 6 salinity conditions. Regression equations between ECe and $DF_{1:5}$ were obtained $ECe=1.4701ln(DF_{1:5})+5.0974(r^2=0.97^{**})$ in case of more than 50% silt contents, $ECe=2.1399ln(DF_{1:5})+5.3462 (r^2=0.99^{***})$ in case of below 50% silt contents, and $ECe=1.5927ln(DF_{1:5})+5.2486 (r^2=0.98^{***})$ in all cases, and then we suggested the $DF_{1:5}\;and\;DF_%$ of 3 soil textural conditions and 6 salinity conditions.

• 한국토양비료학회지
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• 제36권4호
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• pp.193-199
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• 2003

토양전기전도도는 토양의 염분농도의 주요 지표인데 표준방법으로 토양포화침출액의 전기전도도를 측정하여 사용하고 있다. 그러나 많은 토양 염분농도 관련 자료들이 토양과 물의 1:5 희석법으로 측정하고 있으며 환산 계수를 곱하여 염분%로도 제시되고 있다. 따라서 포화침출액법과 1:5 희석법으로 측정하여 제시되어 있는 자료 및 염분%로 표시되어 있는 자료들을 상호비교하는 데 있어서 필요한 환산계수를 도출하였다. 우리나라 서남해안에 조성된 9개 간척지에서 토양시료 90점을 채취 분석하여 2가지 토성조건과 5수준의 염분농도 조건별로 환산계수를 산출하였다. 포화침출액법과 1:5 희석법간의 환산 회귀식은 미사 함량 50%이상인 토양의 경우 DF1:5=1.3624ln(ECe)+5.1386 ($r^2=0.37^{***}$) 이었고 미사 함량이 50%이하인 토양의 경우 DF1:5=1.9505ln(ECe)+5.3679 ($r^2=0.66^{***}$) 이었으며, 토성을 고려하지 않은 전체 토양의 경우에는 DF1:5=1.4001ln(ECe)+5.4865 ($r^2=0.51^{***}$) 이었다. 이들 관계식을 토대로 하여 EC1:5와 염분%로 제시된 자료들을 ECe로 환산할 수 있는 계수 DF1:5와 DF%를 산출하여 제시하였다.

• Mass Spectrometry Letters
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• 제5권1호
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• pp.12-15
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• 2014

Thermal ionization mass spectrometry (TIMS) was used to determine the concentration and isotope ratio of uranium contained in samples of soil and groundwater collected from Korea. Quantification of uranium in ground water samples was performed by isotope dilution mass spectrometry. A series of chemical treatment processes, including chemical separation using extraction chromatography, was applied to the soil samples to extract the uranium. No treatments other than filtration were applied to the groundwater samples. Isotopic analyses by TIMS showed that the isotope ratios of uranium in both the soil and water samples were indistinguishable from those of naturally abundant uranium. The concentration of uranium in the groundwater samples was within the U.S. acceptable standards for drinking water. These results demonstrate the utility of TIMS for monitoring uranium in environmental samples with high analytical reliability.

• 한국환경농학회지
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• 제34권1호
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• pp.1-5
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• 2015

BACKGROUND: The stabilities of the two alkaloidal insecticides of S. flavescens including matrine and oxymatrine are important factor to establish expiry date and usage manual for crop protection. However, the environmental stability of the compounds had not been studied with the extract and its commercial biopesticide. METHODS AND RESULTS: The environmental stabilities of the two alkaloids were performed with extract of S. flavescens, and its two commercial biopesticides both in controlled aquatic and soil conditions. The half-lives of the total matrines for the extract and its two commercial biopesticides were estimated over 200 days both under aerobic and anaerobic water condition. Under dry soil condition, the initial decay rates of the matrines were calculated 0.0804-0.1275 ($t_{1/2}$ 5.4-8.6 days), and the half-lives under wet soil condition were calculated 33.0-231 days. Total soil bacteria on the wet soil ranged 6.0-8.0 log CFU/g-soil during the experiments period. CONCLUSION: The aquatic mixture of the extract showed excellent stability both with the extract and its biopesticides, however, the stability of soil mixture were shorter than the aquatic mixture, suggesting that soil metal consider as a catalyst for the degradation of the two alkaloids.

• 생약학회지
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• 제9권3호
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• pp.149-156
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• 1978

The result of the study about the cultivation, the constituents, the sweetenity, and the development of preparations of Stevia and Hydrangea are as follows: 1. Hydrangea thrived at $200{\sim}1,400m$ above the sea-level, and the good ones were brought up at $600{\sim}1,200m$. 2. The good ones which belonged to the genera of Hydrangea were produced in the damp, dark and cold place. 3. The growth and cultivated yield of Stevia was not significantly influenced by the acidity of the soil. 4. The best season was May and June for propagation of Stevia by cutting method. 5. The growth rate of Stevia and Hydrangea was really good in the sandy fertile soil, but in the mucotic soil it was not suitable. 6. The extraction and separation of phyllodulcin by solvent had many difficulties, because it was very soluble in water, ethanol, ether, petroleum ether, acetone and benzene, etc. 7. The solubility of stevioside on the solvent was as follows: It was very soluble in water and methanol, slightly soluble in ethanol and acetone, and insoluble in ether, petroleum ether and chloroform. 8. The alkaloid reaction by Mayer reagent in Hydrangea extract was positive. 9. The ashification rate of Stevia was 8.66% to 8.72% and that of Hydrangea 17.02% to 17.04%. 10. The tannin of Stevia leaf was 7.80% to 7.88% and its of Hydrangea decreased 9.46% to 6.08% by fermentation. 11. The percent rates in minimum concentration-occurring sweetness in sugar, glycyrrhiza methanol extract, Hydrangea water extract, Stevia leaf water extract, decoction of Stevia's leaf, decoction of Stevia's stem were as follows: 1.2, 0.1, 0.1, 0.2, 0.4, 0.01, 0.1, 0.6. and sweetenity ratios of those were 1, 12, 12, 6, 3, 64, 12, 2, 12. It was very meaningful to develop preparations of stevia as stevioside, micronized powder, water extract, methanol extract and compound teas and in Hydrangea, water extract, methanol extract, single tea, and compound teas were less meaningful. 13. The genera of Hydrangea which is natural species in Korea was positive in phyllodulcin-identification test, but it was not available to make the sweet tea because of having a little content.

• 한국토양비료학회지
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• 제33권6호
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• pp.398-404
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• 2000

본 시험은 높은 비율의 물로 회석된 토양용액의 EC(electrical conductivity)와 saturation parte EC($EC_e$) 간의 상관관계를 검토하고자 실시하였다. 시험토양은 24개 절화장미 재배지에서 수집하였고, 토성은 대부분 양토와 미사질양토 이었으며, 얻어진 시험 결과는 다음과 같다. 토양용액의 총이온 함량과 EC 간에는 고도의 정의 상관관계가 인정되고, 물추출 비율이 증가할수록 토양용액중 이온의 총략은 증가하였으나, 1:1, 1:2, 1:5 비율로 EC를 측정한 다음 각각 1, 2, 5를 곱한 EC 값은 $EC_e$에 비해 현저히 낮은 결과를 보였다. 이는 보다 높은 비율의 물로 추출한 용액의 EC와 $EC_e$간에 큰 오차가 있음을 의미한다. 포화 이상의 물추출조건 하에서 발생하는 이러한 오차를 감소시키기 위하여 회석된 용액의 EC값에 새로온 Diluted factor(DF)와 비선형 등식을 적용하여 $EC_e$를 추정한 결과, 두 방법 모두 측정된 ECe와 추정된$EC_e$간 1차 식의 기울기가 1에 근접하여 새로 적용된 방식들이 기존의 측정방식에 비해 정확성을 높여줄 수 있는 것으로 나타났다. 반면에 DF값은 토성에 크게 의존적이며, 비선형 등식을 이용한 측정방식은 토양의 saturation percentage에 따라 추정된 $EC_e$가 변동되므로 폭넓은 토성에 대한 추가적인 연구가 필요할 것으로 판단된다.

• 한국농공학회지
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• 제30권4호
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• pp.127-133
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• 1988

This study was performed to obtain the basic data analyzing salt movement and desalinization effects, and two different desalinization experiments through leaching and rinsing were carried out, using samples of silt loam soil and silty clay loam soil collected in reclaimed tidelands. The relationships between the electrical conductivity of saturation extract and the electrical conductivity at various dilutions, and the correlations between electrical conductivity, total salt concentration, exchangeable sodium percentage and pH during the desalinization of reclaimed tidelands, were analyzed by the statistical method. The results obtained from this study were summarized as follows: 1.The sample soils used in this study were saline-sodic soils in accordance with the USDA classi- fication system of salt affected soils. 2.The electrical conductivity of saturation extract could be estimated conveniently, using the electrical conductivity of extract from various different soil-water suspensions. 3.The total salt concentration could be expressed in the electrical conductivity, but there was a little difference by soil textures. 4.The regression analysis showed that the relationship between the electrical conductivity of saturation extract and the exchangeable sodium percentage during the desalinization of reclaimed lands could be described by a linear regression equation. 5.The value of pH showed a tendency to increase according as the exchangeable sodium percentage decreased during the desalinization of reclaimed tidelands.

• 한국농공학회지
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• 제36권1호
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• pp.141-152
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• 1994

Our experiment investigated the degree of soil contaimination caused by oil leakage. Each soil sample was taken by boring 5, 8m below the test areas, located 5 to 30m from storage tanks at oil stations. According to the results from a series of laboratory tests(both soxhiet extract test and gas chromatograph test), Traces of a light oil were found in all samples except in Dj8, rocky soil and gasoline and petroleum were not detected. We concluded that soil contamination was caused by the corrosion of storage tanks or alternatively by oil overflow caused during the flooding of underground water seeping into the tank during heavy rain fall or the spillage caused by carelessness during lubrication. Old stations without a concrete box enclosing their metal tanks run a greater risk of oil leakage. To research the effect of oil leakage on plant growth and underground water, We examined the results of research conducted overseas. According to these results, when oil leakage occurs, plant growth is repressed and agricultural crops experience low productivity levels. Also, the contamination of underground water can be serious when oil spreads to the aquifer layer. As a result of these problems, to prevent oil leakage and minimize its contaminating effects at oil stations, it is necessary to improve facilities of storage tanks and have the monitoring system of oil leakage.