• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2004년도 총회 및 춘계학술발표회
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• pp.499-502
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• 2004

Groundwater chemistry in a coastal region having complex contaminant sources was investigated. Water analysis data for 197 groundwater samples collected from the uniformly distributed sixty-six wells were used. Chemical analysis rand results indicate that groundwaters show wide concentration ranges in major inorganic ions, reflecting complex hydrochemical processes of pollutants. Due to the complexity of groundwater chemistry, Results illustrate that thirty five percent of the wells do not fit for drinking based on nitrate and chloride concentration in the study area. the samples were classified into four groups based on Cl and NO$_3$ concentrations and the processes controlling water chemistry were evaluated based on the reaction stoichiometry. The results explained the importance of mineral weathering, anthropogenic activities (nitrification and oxidation of organic matters), and Cl-salt inputs (seawater, deicer, NaCl, etc.) on groundwater chemistry. It was revealed that mineral dissolution is the major process controlling the water chemistry of the low Cl and NO$_3$ group (Group 1). Groundwaters high in NO$_3$ (Groups 2 and 4) are acidic in nature, and their chemistry is largely influenced by nitrification, oxidation of organic matters and mineral dissolution. In the case of chloride rich waters (Group 3), groundwater chemistry is highly influenced by mineral weathering and seawater intrusion associated with cation-exchange reactions.

• Ocean and Polar Research
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• 제36권4호
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• pp.319-326
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• 2014

Mineral dust in the polar snow plays an important role both in the climate system of the Earth and in global biogeochemical cycles. Analysis of the concentration and the particle size distribution of mineral dust has been carried out in the snow from the Antarctic surface snow and the Greenland snowpit. Among the various particle size determination techniques, a Multisizer 3 Coulter Counter in a class 100 clean bench counted all particles between 1.1 and $30.0{\mu}m$ with a $50{\mu}m$ aperture tube. The aperture tube size, the concentration of electrolytes and the accuracy of the particle size distribution were determined in this study. The number concentrations from the Antarctic surface snow were 81,843 particles $mL^{-1}$, but those from the Greenland snowpit were 10,666 particles $mL^{-1}$. In the volume distribution, the distributions of mineral dust in both the Antarctic surface snow and the Greenland snowpit showed lognormal distribution in the size interval 1.1 to $6.0{\mu}m$ with the mode, 3.562 and $3.836{\mu}m$, respectively. The analysis technique using a coulter counter for mineral dust could be used for reconstructing paleoclimates from polar ice cores.

• 자원리싸이클링
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• 제20권6호
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• pp.28-36
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• 2011

황산용액 중에 존재하는 니켈을 회수하기 위해 이온교환수지법을 이용한 기초연구를 수행하였다. 제조된 모의 니켈(Ni)용액에 독일 Lanxess사(社)의 Lewatit Monoplus TP 220를 이용하여 회분식 실험을 하였다. 흡착반응에 영향을 미치는 온도, 교반속도, 반응시간, pH, 이온교환수지 양, 니켈이온농도 등에 대해 고찰하였다. 초기 pH(2.0~5.0)와 교반속도는 니켈의 흡착에 거의 영향을 미치지 않았으며, 평형에 도달하기 위하여 72시간의 시간이 필요했다. 평형실험결과 Freundlich 흡착등온식에 적합하였고, 흡착반응속도는 유사 2차 반응 모델(pseudo-second order)로 잘 모사되었다. 한편 니켈을 함유한 실제 도금세정폐액의 흡착 실험을 행하여 모의용액의 흡착거동과 비교하였고, 흡착된 니켈은 황산 농도가 높아짐에 따라 수지로부터 효과적으로 용리되었다.

• 대한금속재료학회지
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• 제47권6호
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• pp.349-355
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• 2009

In the solvent extraction of Ru(IV) with Alamine336, it was found that Ru took part in the reaction as $RuCl_{6}_^{2-}$ in the HCl concentration range of 1 to 5 M. Interaction parameter between hydrogen ion and $RuCl_{6}_^{2-}$ was estimated by applying Bromley equation to the extraction data. From the mixed solutions of Pd(II) and Ru(IV), the distribution coefficients of Pd were found to be higher than those of Ru in the experimental ranges. Separation factor between Pd and Ru rapidly increased with the decrease of Alamine336 concentration. About 60% of the Ru from the mixed solutions was extracted by TBP at 8.3 M HCl, while Pd was not extracted in the HCl concentration range of 1.6 to 8.3 M.

• Asian-Australasian Journal of Animal Sciences
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• 제16권4호
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• pp.519-528
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• 2003

A survey was conducted in certain parts of Haryana to record the prevalence of micro mineral deficiency in buffaloes. The prevalence of soil Cu, Co, Zn and Fe deficiency was 55.26%, 6.9%, 59.12% and 7.89% respectively. While that of fodder Cu, Co, Zn and Fe was 60.64%, 6.7%, 61.22% and 11.37% respectively. The overall prevalence of serum Cu, Co, Zn and Fe deficiency in Haryana was 59.2%, 19.1%, 59.2% and 19.9% respectively. The correlation co-efficient of Cu, Co, Zn and Fe in soil, fodder and serum was significant in most of the cases the values were above 0.8. Blood examination revealed significant decrease in haemoglobin and TEC level. However, no variation in level of TLC were observed in mineral deficient buffaloes. In micro mineral deficiency, thyroid hormone (T3 and T4) levels were decreased in buffaloes. Marginally lower concentration of vitamin A and E were observed in mineral deficient buffaloes in Haryana. The highest deficiency of micro minerals was 61.76% in copper at Ambala followed by 65.86% in zinc at Rhotak. For therapeutic studies a mineral mixture was prepared according to defiency obtained and fed to three groups of animals. Observation was recorded on 0, 15, 30, 45 and 60 days. Group A consist of normal healthy animals and group B mineral deficient animal untreated and group C mineral deficient animal, treated with prepared mineral mixture. 25 gram of mineral mixture was fed daily along with normal ration. There was increase in body weight, milk yield, haemoglobin concentration and total erythrocyte level in group C animals when compared to group B animals. The milk yield in group C animals increased to 6.970${\pm}$0.41 after 60th day of supplement in comparison to 0 day where it was 5.910${\pm}$0.37, similarly the body wt. of group C animals increased from 129.42${\pm}$01.13 (at 0 day) to 159.31${\pm}$03.61 at 60th day of treatment.

• 대한가정학회지
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• 제18권2호
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• pp.15-21
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• 1980

Three kinds of soybean curd were prepared with three coagulants such as calcium chloride, magnesium chloride and glucono delta lactone. The mineral contents of the three soybean curds were analyzed before soaking and after various lengths of soaking(1/2 hour, 1 hour, 2 hours, and 2 hours(water changed after 1/2 hour)). Results therefrom were as follows: 1. Before the three soybean cured were soaked, their moisture contents were 79-83g/%. The ash contents were 5.04g% in the soybean curd made with CaCl_{2}4.42g/% in the soybean curd prepared with MgCl_{2} and 3.86g/% in the soybean curd coagulated by glucono delta lactone. an analysis of calcium, magnesium and phosphorous contents showed that each element had a greater concentration in the soybean curds made with divalent mineral salts than in the soybean curd made with acid. 2. Changes taking place in the mineral contents of the soybean curds according to different soaking times were examined. The mineral contents tended to decease in process of soaking time. The soybean curds showed the highest rate of mineral dissolution after one hour of soaking, and then they tended to reabsorb minerals. When the soybean curds were soaked I freshly changed water for one hour and 30 minutes, their mineral contents indicated a greater diminishing trend but no significant difference was noticed among the different kinds of soybean curd. In case coagulant has been used excessively, it is necessary to soak the bean curds for about one hour to get the coagulant dissolved.

• 한국지구물리탐사학회:학술대회논문집
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• 한국지구물리탐사학회 2003년도 Proceedings of the international symposium on the fusion technology
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• pp.455-458
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• 2003

A combination of drilling, hydrogeochemical survey, geophysical survey and the numerical modelling for the flow and transport of groundwater was performed to evaluate the seawater intrusion in Baeksu-eup, Yeonggwang-gun, Korea. The survey area extends to over 24 $km^2$. Twelve wells were also drilled for the collection of geologic, geochemical, hydrologic, and geophysical logging data to delineate the degree and vertical extent of seawater intrusion. To evaluate and map the salinity in a coastal aquifer, geophysical data and hydrogeochemical results were used. Layer parameters derived from VES data, various in situ physical properties from geophysical well loggings, and the estimated equivalent NaCl concentration were used as the useful input parameters for the numerical simulation with density-dependent flow. Our multidisciplinary approach for evaluating the seawater intrusion can be considered as a valuable attempt to enhancing the utilization of various data and the reliability of numerical ground modelling.

• 자원리싸이클링
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• 제17권6호
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• pp.24-33
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• 2008

전해생성염소를 산화제로 사용하여 폐인쇄회로기판으로부터 구리의 침출에 대한 연구를 수행하였다. 구리침출반응과 관련된 실험인자들의 영향을 정량적으로 파악하기 위하여 실험계획법을 적용하였다. 실험결과의 분산분석으로부터 전류밀도, 침출온도, 염산농도 그리고 침출온도와 염산농도의 교호작용 등이 구리침출에 유효한 인자로 나타났다. 이들 중 구리침출에 가장 큰 영향을 미치는 인자는 침출실험 결과해석의 95.7%출 차지하는 전류밀도로 분석되었다. 실험결과의 중회귀분석을 이용하여 침출실험 결과의 99%를 설명할 수 있는 침출 모델식을 얻었다. 또한 모델식을 통한 구리 등침출선의 예측으로부터 침출온도가 높아질수록 구리침출량의 증가에 대한 염산농도의 영향이 커지는 것을 알 수 있었다.

• 한국작물학회지
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• 제23권1호
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• pp.14-20
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• 1978

배양액중 무기영양, 인산농도가 수도, 대맥의 철흡수에 미치는 영향을 검토하기 위하여 수도는 영남조생, 대맥은 밀양 006를 공시하였다. 실험1은 각종무기영양(N, $P_2O_5$, K, Ca, Mg)이 결핍된 배양액에서, 시험 II는 철, 인산농도가 철은 0,50,100,200,300ppm, 인산은 0,50,100ppm의 배양액에 35일묘를 이용하여 15일간 처리하였던 바 그 결과를 요약하면 다음과 같다. 1. 수도, 대맥의 철전이율은 무기영양중 가이, 인산결핍에서 높은 경향이었고, 대맥은 수도보다 높았다. 2. 수도, 대맥의 무기영양함량은 (p, K, Mg, Mn) 철저농도보다 철고농도에서 생육한 것이 감소되었다. 3. 수도, 대맥의 철함량은 배양액중 철농도가 높을수록 많았으며 특히 수도근에서 많은 경향이었다. 그러나 배양액중 인산농도가 증가될수록 철함량은 감소되었다. 4. 철과잉증은 배양액중 인산이 공존하지 않을 경우 수도는 100 ppm, 대맥은 50 ppm 철농도에서 나타났으며, 공존할 경우 수도는 300ppm, 대맥은 100ppm 철농도에 서 나타났다. 5. 수도는 배양액중 철농도와 철전이율과는 정의 유의 상관관계가 인정되었으며, 대맥은 부의 회귀곡선이었다. 6. 이상의 결과로 철은 수도보다 대맥의 생육에 크게 영향을 미치고 있었다.

• Asian-Australasian Journal of Animal Sciences
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• 제12권8호
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• pp.1277-1284
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• 1999

Eight feeds and their residues left after washing with tap water (water residue) or incubation in the rumen (rumen residues) were treated with hydrochloric acid, neutral detergent solution without EDTA (NDS) or both, and the release or sorption of minerals (Ca, Mg, P, Na, K, Cu and Zn) assessed. Six of the feeds were from Sri Lanka (Panicum maximum ecotype Guinea A, Glyricidia maculate, Artocarpus heterophyllus (jak leaves), untreated and urea-treated rice straw, and rice bran) and two from the Netherlands (maize silage and wheat straw). The initial concentration of mineral elements, the concentration of neutral detergent fibre (NDF) and the type of feed significantly influenced (p<0.01). The proportion of the mineral elements released or sorbed. In general, feeds with high NDF content (straws and guinea grass) sorbed Ca from tap water, or released less in the rumen, and within these feeds the extent of sorption varied with source of fibre. Acid or NDS treatment removed little of the sorbed Ca, but they removed much of the Mg from both water and rumen residues. Fibres of wheat straw and jak leaves showed an affinity for Mg in the rumen. All feeds and their water and rumen residues sorbed P and Na from NDS, and the extent of sorption varied with the initial concentrations of these elements and with the type of fibre. Acid treatment removed part of the sorbed Na, but not the P. The solubility of K was not affected by the content of NDF, the type of fibre or the initial concentration of K. All feeds and their residues, except for the rumen residues of rice bran sorbed Cu from tap water and in the rumen. The recovery of Cu in rumen residues declined from 353% to 147% after NDS treatment, and with some feeds (glyricidia and jak leaves) the recovery was below 100%. Acid treatment removed part of the Zn sorbed by the water and rumen residues, but the capacity of residues to retain Zn varied with the type of feed.