Na₂CO₃와 NaHCO₃로 활성화한 Na-벤토나이트의 팽창특성과 Cd와 Pb의 상대적 등온흡착곡선

정덕영,양재의,오택근,이교석,Chung, Doug-Young,Yang, Jae E.,Oh, Taek-G.,Lee, Kyo-S. Korean Society of Soil Science and Fertilizer 2007 한국토양비료학회지 Vol.40 No.1

본 실험은 서로 다른 온도조건하에서 두 가지 Na 화합물을 이용하여 Ca-벤토나이트를 Na-벤토나이트 전환하였다. 두 가지 Na 화합물은 양이온 원으로 Na를 가지고 있는 5가지 화합물 중에서 선택하였다. 전환된 Na-벤토나이트의 팽창능은 Na의 농도가 높아질수록 증가하였으며 반면 온도가 증가할수록 최대 Na 농도는 감소하는 경향을 보였다. Na_2CO_3 은 조사된 Na-화합물 중에서 최대 팽창능을 보여주었으며 팽창지수는 처리온도가 최대 100 에 도달할 때까지 최고로 증가하였다. 동일 Na 처리농도에서는 팽창지수는 체류시간이 증가하거나 온도가 높아질 때 다소 감소하였다. 전환된 Na-벤토나이트의 흡착은 조사된 Pb나 Cd의 평형농도가 증가함에 따라 증가하는 경향을 보였으며 Pb의 흡착량이 Cd보다 다소 높은 것으로 조사되었다. 그리고 전환된 Na-벤토나이트에 Pb와 Cd의 흡착은 5 % $Na_2CO_3$. ${\approx}$ 5% $NaHCO_3$ > 3 % $NaHCO_3$ > 3 % $Na_2CO_3$ > 1 % $NaHCO_3$ > 1 % $Na_2CO_3$ > 원형 Na-B > 원형 Ca-B. 그러나 이러한 결과는 CEC에 따른 흡착의 결과와는 다소 상반되는 결과를 보여주고 있다. In this experiment we transformed the Ca-bentonite into Na-bentonite with two inorganic Na-chemicals under different temperatures. These two Na-chemicals were selected among five different Na-chemicals which carries Na as cation. The swelling capacity of the Na chemical-treated bentonite was increased with increasing Na concentration, while the maximum concentration of Na solution decreased with increasing temperature. $Na_2CO_3$ was most effective in exchanging Ca ions and resulting in the highest swelling index among the Na-chemicals. The swelling index was significantly increased with increasing temperature to $100^{\circ}C$. But the equilibration time reversely affected the swelling index due to a rapid increase in evaporation of water. Within same amount of Na treatment SI slightly decreased not only with increasing contacting time but also with increasing temperature. The adsorption for the transformed Na-bentonite was increased with increasing equilibrium concentrations of Pb and Cd ions for all the activated Na-B and indigenous Ca-B and Na-B while the adsorbability of $Pb^{2+}$ onto each Na-B sample is more than that of $Cd^{2+}$. And the maximum adsorption capacity sequence of Na-B samples for Pb and Cd has been found to be 5 % $Na_2CO_3.$ - 5 % $NaHCO_3$ > 3 % $NaHCO_3$ > 3 % $Na_2CO_3$ > 1 % $NaHCO_3$ > 1 % $Na_2CO_3$ > indigenous Na-B > indigenous Ca-B, showing that there are contradictory results about the relationship of cation adsorption to CEC.

Competition of Sulfate for Sorption Sites of Cecil Bt Soil in Binary Anion System

정덕영,Chung, Doug Young Institute of Agricultural Science 1996 Korean Journal of Agricultural Science Vol.23 No.2

Observed results of the adsorption between two competing anions for the shared sorption sites represent that the adsorption phenomena may depends on the characteristics of anion and available sorption sites in a given conditions. In binary systems, adsorption of one species can significantly influence the fate of the other anion, resulting in control of the extent of solute-adsorbate distributions throughout soil profile. And the proton-donation mechanisms by organic anions having a carboxyl as a functional group can also influence the adsorption of inorganic anions onto the hydroxylated sites of Fe and Al oxides. However, study of competitive adsorption of specifically adsorbed anions illustrates some of difficulties which arise in interpretation of reactions at oxide/aqueous solution interfaces. At least two factors prevented a simple analysis of reactions. First, at any pH value the maximum amount of adsorbate taken up at the surface depends on the identity of the anion. Second, it was necessary to postulate the sorption sites where the anion can be adsorbed. Hence, anions having non-specific adsorption characteristics are less capable for sorption sites, compared to those of specific adsorption characteristics, even though competition complies both ordinary and electrostatic interactions for sorption sites. Therefore, competition among chemical species in soil matrix can be of major significance in determining the effective mobility of any reactive anions with sorption sites.

Overview of Rosetta for Estimation of Soil Hydraulic Parameters using Support Vector Machines

정덕영,Chung, Doug-Young Korean Society of Soil Science and Fertilizer 2009 한국토양비료학회지 Vol.42 No.S2

심층토 내에서의 흐름과 이동과정을 포함하는 연구와 관리 측면에서 수학모델에 대한 관심도가 점점 증가하고 있다. 로제타는 토성이나 용적밀도 자료와 같은 대체 토양자료로부터 불포화수리특성에 대한 자료를 추정하는 프로그램이다. 이와 같은 형태의 모델은 애초 기본 토양자료를 수리특성자료로 전환하기 시작한 이래 대체 측정수단으로서 PTF라 불리워졌다. 이러한 기능은 유사-실험모델을 사용하여 예측한 자료를 근간으로 하여 직간접적으로 토양수분을 추정할 수 있다. Mathematical models have become increasingly popular in both research and management problems involving flow and transport processes in the subsurface. Rosetta is a program to estimate unsaturated hydraulic properties from surrogate soil data such as soil texture data and bulk density. Models of this type are called pedotransfer functions (PTFs) as an alternative measurements since they translate basic soil data into hydraulic properties. These functions may be either measured directly or estimated indirectly through prediction from more easily measured data based using quasi-empirical models.

Effects of the Fractionated Raw Cow Manure on Mobility of NO₃^--N in A Double-Layered Soil Column with Constant Water Head

정덕영,이규승,백명진,Chung, Doug-Young,Lee, K.S.,Baek, M.J. 한국토양비료학회 2001 한국토양비료학회지 Vol.34 No.1

본 연구는 다층구조 토양의 토양표면에서 수두를 5cm로 유지하면서 미세입자로 분쇄된 건조 생우분(FRCM)의 혼합 비율에 따른 $NO_3{^-}$-N의 이동특성을 조사한 것이다. 토양의 상층부는 월곡통 토양을 그리고 하층부는 청원통 토양을 용적밀도 $1.25g\;cm^{-1}$으로 조절하여 사용하였으며 FRCM은 0%부터 10.4 %까지 6단계로 나누어 상층부에 균일하게 혼합한 후 약 65일간 지속적으로 관개를 실시하면서 토주의 하부에서 용탈돼 나오는 용출수를 조사하였다. 조사 결과 포화 수리전도도는 유기물함량이 0% 에서 10.4%로 증가함에 따라 $1.7{\times}10^{-3}cm/min$에서 $8{\times}10^{-4}cm/min$으로 감소하는 경향을 보여주었으며 안정된 상태의 수리전도도를 얻기까지 약 7일에서 64일정도 소요됨을 알 수 있었다. 그리고 토양내와 유기물로부터 전환된 $NO_3{^-}$-N와 $NH_4{^+}$-N의 용탈 특성은 혼합된 유기물 함량이 10.4%에서 0%로 감소함에 따라 최고 $14.8mmolc\;kg^{-1}$ to $0.58mmolc\;kg^{-1}$의 변이를 보여주고 있으며 용탈된 $NO_3{^-}$-N의 함량은 $NH_4{^+}$-N와 비교시 약 4배 정도임을 알수 있었다. 따라서 $NO_3{^-}$-N의 전환율은 담수상태에서도 활발히 진행됨을 알 수 있었고 토양내에서 질소의 공급은 토양내 수리전도도와 결부하여 조사할 수 있을 것으로 추정한다. Influence of various rates of fractionated raw cow manure on hydraulic conductivity of the soil was observed. The fractionated raw cow manure(hereafter as FRCM) incorporated into soil. The hydraulic conductivity was measured for the double-layered soil while maintaining the water head by 5 cm over the soil surface. The influence on the mobility of $NO_3{^-}$-N transformed from the FRCM was analyzed. The upper layers (Wolgok series) were made with FRCM ranging from 0% to 10.4 % on weight basis for air-dried soil while the organic matter in the bottom layers (Chungwon series) was removed by combustion. The initial bulk densities for both layers were adjusted to $1.25g\;cm^{-3}$. In this experiment the $K_{sat}$ for the upper layer gradually decreased from $4.71{\times}10^{-3}cm\;min^{-1}$ to $1.2{\times}10^{-3}cm\;min^{-1}$ with increasing the rate of the FRCM from 0 % to 10.4%, while the Ksat of the bottom layer was maintained as $3.7cm\;min^{-1}$. For the double-layered soil columns, the $K_{sat}$ decreased with increasing rate of FRCM at the upper layer from $1.7{\times}10^{-3}cm\;min^{-1}$ to $8{\times}10^{-4}cm\;min^{-1}$ as the rate of organic matter increased from 0 % to 10.4 %, while it took almost 7 days to 64 days to obtain the steady state $K_{sat}$ The elution patterns of $NO_3{^-}$-N and $NH_4{^+}$-N showed that the amounts of both $NO_3{^-}$-N and $NH_4{^+}$-N rapidly approached to the maximum ranging from $14.8mmol_c\;kg^{-1}$ to $0.58mmol_c\;kg^{-1}$ as the rate of FRCM decreased from 10.7 % to 0 % which is equivalent to indigenous amount of $NO_3{^-}$-N and $NH_4{^+}$-N. And the amounts of $NO_3{^-}$-N were approximately three or four time than those of $NH_4{^+}$-N, indicating that the transformation rate of $NO_3{^-}$-N was improved by the higher FRCM rate. Thus, the ability of a soil to supply N can be predicted from its mineralization parameters and leaching potentials influenced by water flow regime in soil.

Sequential Fractionation of Heavy metals from Mine Tailings and Two Series of Agricultural Soils

정덕영,이도경,Chung, Doug-Young,Lee, Do-Kyoung 한국토양비료학회 1999 한국토양비료학회지 Vol.32 No.4

본 연구는 폐 금속광산으로부터 발생한 중금속이 주변 환경으로 오염 확산되는 특성과 이를 중금속으로 오염된 토양의 효과적인 복원 방안을 모색하기 위하여 토양내 중금속의 거동 특성을 바탕으로 한 반응 특성을 조사하였다. 토양내 중금속의 이동성과 생물에 의한 흡수에 영향을 미치는 화학적 존재 형태를 중금속이 다량 함유되어 있는 충남 청양의 구봉 폐 금광의 광미와 인위적으로 중금속을 오염시킨 농경지 토양에서 중금속의 토양과의 화학적 결합 형태를 연속 축출법에 의해 분리하였으며, 그 순서에 따라 토양 내에서 다음과 같이 용해도와 이동성이 감소한다: Soluble fraction> exchangeable>carbonate>Fe-Mn oxide>organic>residual fraction. 광미중에 결합 부위에 가장 높은 친화력을 보인 Pb는 대부분 Fe-Mn Oxide와 Carbonate fraction에 존재하였고 이 두 Fraction에 각각 48.3%와 26.8% 나타났다. Cu와 Cd는 각각 organic과 carbonate fraction이 71.8% 42.9%로 가장 높게 나타났다. 이들 fraction은 비교적 이동성이 강한 fraction으로 중금 속의 오염 조사시 반드시 평가되어야 하며, 복원방안 결정시 반드시 고려되어야 할 것이다. 중금속을 인위적으로 흡착시킨 토양에 있어서 중금속은 대부분 Exchangeable, carbonate 그리고 Fe-Mn oxide fraction 흡착되어 있는 것으로 나타났다. 예산통에 있어서 흡착된 Pb는 이들 fraction에 91%가 존재하였고, Cu는 Fe-Mn Fraction에 30.4% 그리고 Cd는 exchangeable fraction에 67.9% 가 존재하였다. 월곡통에 있어서는 흡착된 Cd는 Exchangeable fraction에 93.2%가 존재하였고, Pb와 Cu는 대부분 exchangeable, carbonate와 Fe-Mn Oxide에 흡착되어 있었다. 따라서 토양내 이들 중금속이 가해질 경우 대부분 독성이 강한 오염원으로서 잠재적인 이동성과 생물학적 흡수가능성을 갖는 것으로 나타났다. In order to investigate the contamination characteristics of the heavy metals in the mine tailings of abandoned gold mine and its surrounding agricultural soils, a sequential extraction procedure of increasing reactivity in the dissolution processes of the heavy metals(Cd, Cu, and Pb) which were associated with solid and/or solution phase in soils was attempted to partition into six particulate fractions : exchangeable, bound to carbonate, bound to Fe-Mn oxides, bound to organic matter, residual, and soluble. Among indigenous heavy metals in the mine tailings, Pb was the most abundant and Cu and Cd were followed by. Fractionation result of Pb obtained from the triplicate samples of the mine tailings were in the order of Fe-Mn oxide> Carbonate> Residual> Organic> Exchangeable> Soluble, while Wolgok series were Exchangeable > Fe-Mn oxide > Carbonate> Organic> Residual> Soluable. However the other heavy metals studied were not followed this trend. The fractionation results of mine tailing and agricultural soils demonstrated that different geochemical fractions were operationally defined by an extraction sequence that generally followed the order of decreasing solubility. Therefore potential mobility and bioavailability of heavy metals as toxic pollution sources can be evaluated when studying the pollution levels of heavy metals in soils.

Key Methodologies to Effective Site-specific Accessment in Contaminated Soils : A Review

정덕영,Chung, Doug-Young 한국토양비료학회 1999 한국토양비료학회지 Vol.32 No.4

오염토양을 효과적으로 진단하고 경제적인 복원을 위해서는 오염토양의 오염원인, 오염정도, 주변 환경이나 인축에 대한 피해발생 유무, 오염물의 이동경로 등을 올바르게 평가하는 것이 대단히 중요하다. 이를 위해서는 오염토양과 토양내 가스, 주변 지하수 및 지표수, 침전물 등의 효율적 시료채취와 정확한 분석이 필수적이라 할 수 있다. 오염지역 토양의 오염도평가를 표준화하고 처리효율성을 높이기 위해서는 전문처리요원이 토양의 오염도와 위험성을 정확하게 판단 할 수 있도록 단순하면서도 경제적인 연속시험법을 필요로 한다. 이것은 오염토양의 조사와 복원시간 및 전치적일 기술의 진보를 가져오는데 상당한 시간절약을 꾀할 수 있다. 특히 효과적인 현장평가를 위해서는 오염특성을 포함한 많은 관련 요인들에 대한 표준화된 기준하에서 오염의 형태와 정도를 결정하는 것이 중요하다. 현장평가를 위한 일반적인 절차는 작업계획과 토양조사수준에 따라 Phase I, II, III의 단계적 방법으로 구성되어 있다. Phase I은 토양의 과거용도 및 오염물의 유입경로를 기초로 하여 현장의 환경여건을 파악하는 단계이다. Phase I에서 잠재적 오염물질에 의해 오염된 것이 확인되면 Phase II에서는 오염물의 존재여부와 존재정도를 파악하는 단계로 시료의 채취 및 분석과정이 여기에 포함된다. Phase III는 Phase I과 II의 결과를 바탕으로 오염토양을 복원하는 단계이다. 여기서 평가기준이 지역 특이적인 것인지 적당한 것인지를 결정하는 중요한 요인은 (1) 시료채취의 공간분포도와 지역의 크기, (2) 취해진 시료의 수, (3) 시료채취 방법, 그리고 (4) 자료를 분석요령 등이다. 선택된 분석방법이 추천할만한 것일지라도 정량방법의 선택여부는 현장조사방법에 대한 훈련이나 조사경험을 가진 사용자에 의해 결정되는 것이 바람직할 것이다. For sites to be investigated, the results of such an investigation can be used in determining foals for cleanup, quantifying risks, determining acceptable and unacceptable risk, and developing cleanup plans t hat do not cause unnecessary delays in the redevelopment and reuse of the property. To do this, it is essential that an appropriately detailed study of the site be performed to identify the cause, nature, and extent of contamination and the possible threats to the environment or to any people living or working nearby through the analysis of samples of soil and soil gas, groundwater, surface water, and sediment. The migration pathways of contaminants also are examined during this phase. Key aspects of cost-effective site assessment to help standardize and accelerate the evaluation of contaminated soils at sites are to provide a simple step-by-step methodology for environmental science/engineering professionals to calculate risk-based, site-specific soil levels for contaminants in soil. Its use may significantly reduce the time it takes to complete soil investigations and cleanup actions at some sites, as well as improve the consistency of these actions across the nation. To achieve the effective site assessment, it requires the criteria for choosing the type of standard and setting the magnitude of the standard come from different sources, depending on many factors including the nature of the contamination. A general scheme for site-specific assessment consists of sequential Phase I, II, and III, which is defined by workplan and soil screening levels. Phase I are conducted to identify and confirm a site's recognized environmental conditions resulting from past actions. If a Phase 1 identifies potential hazardous substances, a Phase II is usually conducted to confirm the absence, or presence and extent, of contamination. Phase II involve the collection and analysis of samples. And Phase III is to remediate the contaminated soils determined by Phase I and Phase II. However, important factors in determining whether a assessment standard is site-specific and suitable are (1) the spatial extent of the sampling and the size of the sample area; (2) the number of samples taken: (3) the strategy of taking samples: and (4) the way the data are analyzed. Although selected methods are recommended, application of quantitative methods is directed by users having prior training or experience for the dynamic site investigation process.

Mechanisms of Adsorption with Respect to Sulfate Mobility in Multispecies Systems of Soils

정덕영,Chung, Doug Young Institute of Agricultural Science 2000 Korean Journal of Agricultural Science Vol.27 No.2

The mobility of sulfate in soils defends on several factors including redox potential, soil mineralogy, pH, and the presence of other anions that compete for sorption sites with sulfate. The proposed model of adsorption mechanism for sulfate postulated that reaction is between anions in solution and charged surfaces of soil particles. With appropriate choice of parameters obtained from the adsorption-desorption experiments, the equation of transport model adapt an empirical approach, capable of handling most general equilibrium adsorption isotherms, suitable for multispecies systems. 토양내에서 황산이온의 이동성은 산화환원전위, 토양광물 특성, pH, 그리고 환산이온과 토양입자 표면에 흡착에 관여하는 타 음이온들에 의해 영향을 받는다고 알려져 있 다. 제시된 황산이온의 흡착 기작은 토양입자 표면과 수용성상태의 음이온간의 상관 관계를 나타낸 것이다. 그러므로 흡 탈착연구로 부터 얻어진 적정한 계수를 적용함으로서 다중 이온이 존재하는 토양내에서의 일반적 등온흡착 곡선을 적용할 수 있는 이 동모형은 실험적 접근 방법을 수용하게 된다.

Competition of Sulfate for Sorption Sites of Cecil Bt Soil in Binary Anion System

Doug Young Chung(정덕영) 충남대학교 농업과학연구소 1996 농업과학연구 Vol.23 No.2

Prediction of Nitrogen Loading from Forest Stands in 430Eutrophication of Lake

Doug-Young Chung(정덕영),Young-Han Lee(이영한),Jin-Ho Lee(이진호),Mi-suk Park(박미숙) 한국토양비료학회 2010 한국토양비료학회지 Vol.43 No.4

The continuous release of nutrient sources into natural water resource can be a continuing problem in eutrophication, as well as severe reductions in water quality. However, any desirable measure is not developed yet even though so many researches and efforts have been done to solve this problem. Forest as one of troublesome nonpoint sources may contributes most to nutrient loading, but the loading of N and P from forest in order to grasp the eutrophication potential of nonpoint sources has not been evaluated. The nutrient sources from the organic litter accumulated on the surface of forest soils can be a critical factor in continuity of eutrophication of a lake. The decomposition rate of litter can be estimated to predict release of N and P from the forest stand. The loss rate of nitrogen is complicated but depends in part upon the physical matrix of the element. Therefore, long-term nutrient budget and flux estimates at stand would be useful tools in calculating potential nutrient fluxes into the watercourses in a sustainable way. The present investigation can give insight to the actual situation of the eutrophication potentials of forest as the practical nonpoint sources.

Sequential Fractionation of Heavy Metals from Mine Tailings and Two Series of Agricultural Soils

Doug-Young Chung(정덕영),Do-Kyoung Lee(이도경) 한국토양비료학회 1999 한국토양비료학회지 Vol.32 No.4