• 한국토양비료학회지
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• 제46권5호
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• pp.351-358
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• 2013

A suitable supply of mineral elements into shoot via a root system from growth media makes plants favorable growth and yield. The shortage or surplus of minerals directly affects overall physiological reactions to plants and, especially, strongly influences carbohydrate metabolism as a primary response. We have studied mineral uptake and synthesis and translocation of soluble carbohydrates in N, P or K-deficient tomato plants, and examined the interaction between soluble carbohydrates and mineral elements. Four-weeks-old tomato plants were grown in a hydroponic growth container adjusted with suboptimal N ($0.5mmol\;L^{-1}\;Ca(NO_3)2{\cdot}4H_2O$ and $0.5mmol\;L^{-1}\;KNO_3$), P ($0.05mmol\;L^{-1}\;KH_2PO_4$), and K ($0.5mmol\;L^{-1}\;KNO_3$) for 30 days. The deficiency of specific mineral element led to a significant decrease in its concentration and affected the concentration of other elements with increasing treatment period. The appearance of the reduction, however, differed slightly between elements. The ratios of N uptake of each treatment to that in NPK sufficient tomato shoots were 4 (N deficient), 50 (P deficient), and 50% (K deficient). The P uptake ratios were 21 (N deficient), 19 (P deficient), and 28% (K deficient) and K uptake ratios were 11 (N deficient), 46 (P deficient), and 7% (K deficient). The deficiency of mineral elements also influenced on carbohydrate metabolism; soluble sugar and starch was substantially enhanced, especially in N or K deficiency. In conclusion, mineral deficiency leads to an adverse carbohydrate metabolism such as immoderate accumulation and restricted translocation as well as reduced mineral uptake and thus results in the reduced plant growth.

• 한국환경과학회지
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• 제16권1호
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• pp.21-26
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• 2007

The concentrations of fourteen mineral and trace elements (Al, Ca, Fe, K, Mg, Se, Ba, Co, Cu, V, Pb, Hg, Cd and As) were determined in Ganoderma Lucidum and their infusions consumed for medical purposes collected from Vietnam, China and some places in Korea. Concentrated acid digestion procedure was applied under optimized conditions for dissolution of these medicinal fungi. Element concentrations in these fungi and their in-fusions were then determined by ICP-AES. The mineral and trace element content of these samples and their in-fusions showed a wide variability However, distribution of some elements in the infusions is not high.

• 한국수소및신에너지학회논문집
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• 제20권5호
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• pp.447-454
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• 2009

Electrolyzed reduced water was known as an alkaline solvent than piped water, natural water and mineral water etc. By means of reduction property, electrolyzed reduced water could dissolve a solute than other kinds of water without chemicals. In this study, serpentine dissolution in electrolyzed reduced water was investigated as a novel pre-treatment of serpentine which was a minerals for carbon dioxide sequestration. The elements (Ca, Si, Mg etc.) of serpentine were dissolved rapidly at early in the dissolvation then after some minutes the solubilities of serpentine elements showed stable state without abrupt changes. In spite of serpentine elements dissolution, chemical bondings and crystallographic structure of serpentine were not changed. It was explained that the dissolution mechanism of serpentine occurred from surface in electrolyzed reduced water and bulk structure sustained without collapse.

• International Journal of Industrial Entomology and Biomaterials
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• 제43권2호
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• pp.52-58
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• 2021

The article presents the results of the content of the chemical and biochemical composition of the pupa of the wild silkworm Saturnia pyri belonging to the family Saturniidae, species of Lepidoptera. The nutritional value of silkworm Saturnia pyri pupae was evaluated, which contained 51% dry matter, 52.50% crude protein, 27.89% fat, 10.50% chitin fibers, 2.5% ash and 27 macro- and microelements and 25 mg alpha tocopherols in 100 g oil. The X-ray fluorescence method was used to determine the content of mineral elements in the pupa of the silkworm Saturnia pyri. It was revealed that the pupa of this type of silkworm contains 25 elements, of which the relative amount of K, Mg, Na, Ca, Al is much higher than other elements.

• 한국광물학회지
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• 제24권1호
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• pp.55-62
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• 2011

• 한국광물학회지
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• 제10권1호
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• pp.60-73
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• 1997

The talc of the Daeheung, Pyeongan, and Cheongdang (Shinyang) talc deposits in the Yesan-Gongju-Cheongyang area is a hydrothermal alteration product of serpentinite originated from ultramafic rocks. The mineral assemblages in alteration zones are: serpentine, serpentine-talc, talc, talc-chlorite, talc-phlogopite-chlorite, and talc-tremolite-chlorite. Chemical distributions in both the Al2O3-FeO-MgO system and the immobile elements suggest that the serpentine-talc and talc rocks are the reaction product of ultramafic rocks and silicic hydrothermal solution without addition of other granitic components, whereas chlorite-, phlogopite-, and tremolite-bearing rocks are the metasomatic alteration product of serpentinite by hydrothermal solution affected by granitic gneiss. Discontinuities in the immobile element ratios of mineral assemblages are due to changes in their mineralogy. The relative contents of Al2O3, TiO2, Zr in the talc-phlogopite-chlorite and talc-tremolite-chlorite rocks increase irregularly with increasing phlogopite, tremolite, and/or chlorite contents in contrast to other ore types. But the relative contents of Cr, Ni, and Co are uniform in all the mineral assemblages. Chemistry of each mineral assemblage formed by steatitization of serpentinite suggests that Cr, Co, Ni, MgO, and Fe2O3 are relatively immobile during the alteration, whereas SiO2, Al2O3, CaO, and K2O are highly increased. The contents of chlorite, phlogopite, and tremolite in each mineral assemblage might be controlled by addition of Al2O3, K2O, and CaO, respectively. The high contents of other elements than immobile elements in the altered rocks as compared with unaltered rocks indicate that a large amount of elements were introduced from hydrothermal solution up to about 8∼41% in total mass showing maximum value in the talc-phlogopite-chlorite rock.

• Mycobiology
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• 제37권2호
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• pp.109-113
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• 2009

The mineral contents of the cultivation substrates, fruiting bodies of the mushrooms, and the postharvest cultivation substrates were determined in cultivated edible mushrooms Pleurotus eryngii, Flammulina velutipes, and Hypsizigus marmoreus. The major mineral elements both in the cultivation substrates and in the fruiting bodies were K, Mg, Ca, and Na. Potassium was particularly abundant ranging 10${\sim}$13 g/kg in the cultivation substrates and 26${\sim}$30 g/kg in the fruiting bodies. On the contrary, the calcium content in the fruiting bodies was very low despite high concentrations in the cultivation substrates, indicating Ca in the cultivation substrates is in a less bio-available form or the mushrooms do not have efficient Ca uptake channels. Among the minor mineral elements determined in this experiment, Cu, Zn, and Ni showed high percentage of transfer from the cultivation substrates to the fruiting bodies. It is noteworthy that the mineral contents in the postharvest cultivation substrates were not changed significantly which implies that the spent cultivation substrates are nutritionally intact in terms of mineral contents and thus can be recycled as mineral sources and animal feeds.

• Asian-Australasian Journal of Animal Sciences
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• 제5권1호
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• pp.63-67
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• 1992

This paper reports the effects of rare earth nitrate (REN) on the growth of internal organs and mineral elements in serums of broiler chickens. The REN used is mixture of light RE containing mainly La, Ce, Pr and Nd 4 elements. 40 eight-week old AA broiler chickens were divided randomly into four groups that their treatments were respectively 0, 20, 200 and 2000 mg REN/kg feed and the duration of the experiment was 60 days. Responses were measured in terms of internal organic weight and tissue, contents of mineral elements in serums. There were no significant differences between the organ ratios and tissue changes of the 20, 200 mg REN/kg groups and the control group. The organs included the heart, liver, kidneys, lungs, testicles, thyroids, adrenal glands, pancreas, tonsies of caecum, stomachus glandularis, duodenum, ileum and bursa of Fabricius. The liver and thyroid indices of 2000 mg REN/kg group were significantly higher than those of the control group (p < 0.01, p < 0.05) and the adrenal gland index lower (p < 0.05). The pathlolgic changes in the heart, kidney and thyroid were more serious than that of the control group. No significant differences occurred between the contents of K, Na, Mg elements in the serum of all groups, with the exception of the content of Ca, which was higher in the 2000 mg/kg group (p < 0.05). The contents of all trace elements including Mn, Zn and Cu, but except Fe, in the serums of all the treated groups were significantly higher than those of the control group (p < 0.01).

• 한국진공학회:학술대회논문집
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• 한국진공학회 2004년도 제27회 학술발표회 초록집
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• pp.190-190
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• 2004

• 광물과 암석
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• 제37권3호
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• pp.139-153
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• 2024

최근들어, 자원 선진국들은 광물자원에 대한 자원민족주의 심화와 함께 광물자원 고갈이 심해짐에 따라 광물자원 탐사에 한층 더 심혈을 기울이고 있다. 그래서 광물자원 탐사에 이용되는 방법 중의 하나는 광물의 화학조성을 통해 탐사하는 방법이다. 황철석은 광화작용 전반에 걸쳐 산출되고 광종에 관계없이 산출되는 광물로써 그 광물내 미량원소들의 종류 및 함량변화가 광상 탐사에 주요 지화학적 지시자들로써 많이 활용되고 있다. 저자는 이 논문에서 장군 연-아연 광상의 모암, 모암변질대 및 연-아연 광체에서 산출되는 황철석의 산상과 화학조성 변화 등을 연구함으로써 연-아연 광체 탐사 시 활용할 수 있는 지시원소들에 대해 보고하고자 한다. 이 광상은 모암인 고생대의 장군석회암층에 연-아연 열수용액과의 반응에 의해 형성된 열수교대형 광상이다. 이 열수교대형 광상의 연-아연 광화작용과 관련된 모암변질작용은 주로 능망간석화작용과 일부 돌로마이트화작용, 황철석화작용, 견운모화작용 및 녹니석화작용 등이 관찰된다. 모암, 모암변질대 및 연-아연 광체에서 산출되는 황철석은 조직, 산상 및 선후관계 등을 근거로 3가지 유형(Py I형, Py II형 및 Py III형)으로 분류되며 광화작용이 진행됨에 따라 Py I형에서 Py II형을 걸쳐 Py III형으로 산출된다. 각 유형별 황철석내 미량원소의 함량 변화가 큰 원소는 Mn, As, Ag, Sb 및 Pb 원소들이며 함량 변화가 작은 원소는 Zn, Cu, Cd, Se, Te, Co, Ni, Au, In 및 Sn 원소들이다. 각 유형별 황철석내 미량원소들은 각각 Fe²⁺↔Co²⁺ 치환(Py I형), 3Fe²⁺↔Ag¹⁺ +(Mn²⁺+Ni²⁺+As²⁺)+(As³⁺+Sb³⁺) 치환(Py II 형)과 3Fe²⁺↔Ag¹⁺+(Mn²⁺+As²⁺+Pb²⁺)+(Mn³⁺+As³⁺+Sb³⁺), S^1-↔(As^1-+Sb^1-) 치환(Py III형)이 관찰되는데 이는 연-아연 광화작용 말기로 감에 따라 상대적으로 Mn, As, Sb, Ag 및 Pb 원소들이 부화되었음을 의미한다. 따라서 상기 연구 결과를 토대로, 황철석은 연-아연 광체 탐사에 유용한 광물이며 또한 Mn, As, Sb, Ag 및 Pb 원소들은 유사한 지질조건을 갖는 연-아연 광체 탐사 시 부화정도에 따라서 연-아연 광체 탐사 지시원소로서 활용할 수 있을 것이다.