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- 저자 : 현해남(Hae-Nam-Hyun) (검색결과 118 건)
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제주도 대표 토양에서 Alachlor 와 Chlorothalonil 의 흡착과 이동 연구
현해남,오상실,유순호 ( Hae Nam Hyun,Sang Sil Oh,Sun Ho Yoo ) 한국환경농학회 1995 한국환경농학회지 Vol.14 No.2
This study was conducted to investigate the adsorption characteristics, distribution coefficients, and movement of alachlor(2-chloro-2`, 6`-dimethyl-N-(methoxymethyl) acetanilide) and chlorothalonil(tetrachloroisophthalonitrile) for the 3 soils sampled from major soil groups in Cheju Island. Namwon, Jeju, and Mureng soils used in this study were classified as black volcanic ash soil, dark brown volcanic ash soil and dark brown nonvolcanic soil, respectively. Organic carbon content and CEC of Namwon soil were very high and those of Mureung soil were very low. Linear and Freundlich adsorption isotherms were the best to fit the adsorption of alachlor and chlorothalonil in the soils. K value, Freundlich coefficient, of alachlor for Namwon soil was 21.38, being 5.4 and 97.2 times higher than that for Jeju and Mureung soils respectively. The values of chlorothalonil for the soils were similar to those of alachlor but were much higher than them. When Mureung, Jeju and Namwon soil columns were leached with a solution containing 10.25 ㎎/ℓ of alachlor and 1.50 ㎎/ℓ of chlorothalonil, alachlor was first detected at 0.265, 0,47, and 1.86 pore volume (PV) and chlorothalonil was 3.71, 4.7 and 17.5 PV, respectively. The pore volumes at C/C_o=1 of alachlor in the leachates from Mureung, Jeju and Namwon soil columns were 1.1, 3.7 and 6.6 PV and those at C/C_o=0.2 of chlorothalonil were 7.5, 8.5 and 27.5, respectively. This means that the deceasing order of the mobility of the chemicals in soils was Mureung soil>Jeju soil》Namwon soil. The pore volumes detecting C/C_o=0.5 of alachlor and C/C_o=0.05 of chlorothalonil in leachate were positively correlated with the distribution coefficients for the soils.
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현해남,오상실,구본준,강호준,Hyun, Hae-Nam,Oh, Sang-Sil,Koo, Bon-Jun,Kang, Ho-Jun 한국토양비료학회 2000 한국토양비료학회지 Vol.33 No.2
일반 밭, 논, 과수원 및 비닐하우스 토양 78점을 채취하여 3반복으로 농촌진흥청 표준분석법과 Soiltek$^{(R)}$ KA-P 분광광도계법으로 유기물, 치환성 K, Ca 및 Mg, CEC, 유효규산 및 질산염 함량을 측정하였다. Soiltek$^{(R)}$ KA-P 분광광도계로 측정한 유기물, 치환성 Ca, 및 Mg 용액의 발색 안정도는 1시간 동안 약 2%정도 낮아졌으며, 치환성 K, CEC및 질산염은 거의 변화가 없었다. Soiltek$^{(R)}$ KA-P 분광광도계로 측정한 분석 절대값은 농촌진흥청 표준분석법으로 측정한 값과 거의 1:1의 관계를 갖고 있었으며, 결정계수($R^2$)는 0.9501 이상이었다. 두 방법으로 측정한 유기물, 치환성 K, Ca 및 Mg, CEC, 유효규산 및 질산염의 표준편차는 각각 ${\pm}1.8gkg^{-1}$, ${\pm}0.05cmol^+kg^{-1}$, ${\pm}0.18cmol^+kg^{-1}$ 및 ${\pm}0.13cmol^+kg^{-1}$, ${\pm}1.0cmol^+kg^{-1}$, ${\pm}5.0mgkg^{-1}$ 및 ${\pm}10.0mgkg^{-1}$ 이하였다. 모든 성분에 대한 분석값은 95% 신뢰수준을 만족시켰으며, 변이계수는 7~17% 이하였다. 따라서, 기기조작의 간편성 저가 기기의 사용, 정확도, 정밀도 등을 고려한다면 Soiltek$^{(R)}$ KA-P 분광광도계에서 제시하는 방법으로 측정하는 것도 유용한 방법이라고 생각된다. To enable rapid and convenient soil test, new soil analytical methods, which require only one instrument, UV/Vis spectrophotometer, were developed and named "Soiltek KA-P spectrophotometric methods". The Soiltek$^{(R)}$ KA-P spectrophotometric method was compared with standard method of RDA in analytical capability for soil chemical properties. Using the 78 soils collected from upland, paddy, orchard, and vinyl house soils, soil organic matter, exchangeable K, Ca, and Mg. CEC, available $SiO_2$, and nitrate were analyzed by the two methods. The color stability(ratio of the absorbance at elapsed time t to the absorbance at time t=0) of organic matter. Ca, Mg, and available $SiO_2$ decreased to about 2% within one hour. However, that of exchangeable K, CEC, and nitrate remained constant. The results obtained with Soiltek$^{(R)}$ KA-P spectrophotometric method showed highly significant correlation with those measured by the standard method of RDA($R^2$ >0.9501), in which the slopes were near unity of $1.0{\pm}0.05$. The standard deviation values of organic matter, exchangeable K, Ca, and Mg, CEC, available $SiO_2$, and nitrate were apparently lower than ${\pm}1.8gkg^{-1}$, ${\pm}0.05cmol^+kg^{-1}$, ${\pm}0.18cmol^+kg^{-1}$, and ${\pm}0.13cmol^+kg^{-1}$, ${\pm}1.0cmol^+kg^{-1}$, ${\pm}5.0mgkg^{-1}$, and ${\pm}10.0mgkg^{-1}$, respectively. All the measurements showed coefficients of variation of less than 7~17% and were within the confidence level of 95%, which means both the methods are precise. Considering the relative simplicity, low cost, precision and accuracy, the proposed Soiltek$^{(R)}$ KA-P spectrophotometric methods could be recommended as an alternative to standard method.
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논문 / 제주도 흑색 화산회토의 살균제 chlorothalonil 흡착
현해남(Hae Nam Hyun) 한국수처리학회 1995 한국수처리학회지 Vol.3 No.1
This study was conducted to investigate the adsorption characteristics of chlorothalonil(tetrachloroisophthalonitrile) for black volcanic ash soil and dark brown nonvolcanic soil in Cheju Island. Linear and Freundlich adsorption isotherms were best to fit the adsorption of chlorothalonil for Namwon and Mureung soils sampled from black volcanic ash soil and dark brown nonvolcanic soils, respectively. K values, Freundlich coefficient, of chlorothalonil for Namwon soil was 239.88, being 13.1 times higher than that for Mureung soil. Adsorption isotherm for Namwon soil was L-shaped isotherm which the solid has a high affinity for the solute but that for Mureung soil was not. Black volcanic ash soils have higher pH(NaF), organic carbon content, and cation exchange capacity compared to dark brown nonvolcanic soils. Average distribution coefficient of chlorothalonil for black volcanic ash soils was 98.7, being 4.3 times higher than that for dark brown nonvolcanic soils.
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아연광산 주변 논토양에서 토양(土壤) 화학성(化學性)이 중금속의 형태(形態) 및 그 분포(分布)에 미치는 영향
현해남,유순호,Hyun, Hae-Nam,Yoo, Sun-Ho 한국토양비료학회 1991 한국토양비료학회지 Vol.24 No.3
본 연구는 아연광산(亞鉛鑛山) 주변의 논토양에 존재하는 Cd, Pb, Cu 및 Zn의 형태별 함량을 조사하여 중금속간의 분포(分布) 특성(特性)을 검토하였으며, 토양 화학적 성질이 이들의 형태별 함량 분포에 미치는 영향을 밝히기 위하여 수행되었다. 그 결과를 요약하면 다음과 같다. 1. 공시토양에 존재하는 Cd, Pb, Cu 및 Zn은 주로 해화물-잔류태(殘留態)로 존재하였으며, Cd와 Pb의 산화물(酸化物)-탄산염태(炭酸鹽態)와 Cu의 유기복합태(有機複合態)의 함량도 높은 편이었다. Pb와 Cu의 치환태는 소량 존재하였으며, 수용태는 Zn만 검출되었다. 2. 치환태의 분포비가 높은 토양일수록 산화물-탄산염태 및 황화물-잔류태의 분포비가 낮았다. 3. 토심이 깊어질수록 치환태 Cd 및 Zn의 분포비(分布比)는 낮아지고 항화물-잔류태의 분포비가 높아졌으며, Pb는 산화물-탄산염태의 분포비가 낮아지고 황화물-잔류태의 분포비가 높아졌다. 4. Cu는 유기물이 많은 토양일수록 Cu의 유기복합태 함량이 많았으며, Cd, Pb 및 Zn의 유기복합태는 유기물함량과 관계가 없었다. 치환태 Cd, Pb 및 Zn의 분포비는 pH가 높은 토양일수록 낮았으나, 이들의 산화물-탄산염태과 황화물-잔류태의 분포비의 합은 높았다. Pb의 산화물-탄산염태 및 황화물-잔류태의 분포비는 공시토양의 pH 전범위에서 Cd 및 Zn에 비하여 높았다. A study was conducted to determine the influence of soil chemical properties on the distribution and forms of cadmium (Cd), lead (Pb), copper(Cu) and Zinc(Zn) in paddy soils near zinc mines. A sequential extraction procedure was used to fractionate the heavy metals in soils into the designated from of water soluble, exchangeable, organically bound, oxide/carbonate, and sulfide/residual. The predominant form of Cd, Pb, Cu and Zn in the soils was found to be sulfide/residual form. Oxide/carbonate Cd and Pb and organically bound Cu were high, while exchangeable Pb and Cu were very low. Water soluble Cd, Pb and Cu were not detected in the soils. The percentages of the heavy metals content in exchangeable fractions were inversely correlated with those in sulfide/residual fractions in the soils. Exchangeable Cd and Zn and the oxide/carbonate Pb were shifting to the sulfide/residual form with soil depth and the chemical forms of Cu were not changed. Organically bound Cu was positively correlated with soil organic matter content but Cd, Pb and Zn were not. The percentages of Cd, Pb and Zn content in exchangeable forms decreased with soil pH, while those in oxide/carbonate and sulfide/residual forms increased with soil pH. The amounts of oxide/carbonate and sulfide/residual forms of pb were higher than those of Cd and Zn at same soil pH.
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