• Title/Summary/Keyword: 미량 원소

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보잘 것 없는 계분으로 큰 수확

  • 대한양계협회
    • KOREAN POULTRY JOURNAL
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    • v.24 no.12 s.278
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    • pp.91-95
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    • 1992
  • 한때 악취나고 파리가 들끓는 오염물로 여겨지던 계분이 이제는 적량의 화학미량원소가 첨가되어 귀중한 유기질 비료가 되었다. 이와같은 변신을 21년에 걸쳐서 이룩하게 된 것은 시드니 라우스-힐에 사는 N.제닝스씨의 끈기와 능력의 결실이다. 오늘날 노-옴이라고 불리는 제닝스씨는 키가 크고, 머리가 희끗희끗한, 기계공학도에서 시작한 양계가로서 건조계분 생산의 선구자로 국제적으로 인정받고 있으며 세계 최대의 유기질 비료생산 체제를 콘트롤 하고 있다.

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Geochemistry and Sm-Nd isotope systematics of Precambrian granitic gneiss and amphibolite core at the Muju area, middle Yeongnam Massif (영남육괴 중부 무주 지역에 위치하는 선캠브리아기 화강편마암 및 앰피볼라이트 시추코아의 Sm-Nd 연대 및 지구화학적 특징)

  • Lee Seung-Gu;Kim Yongje;Kim Kun-Han
    • The Journal of the Petrological Society of Korea
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    • v.14 no.3 s.41
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    • pp.127-140
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    • 2005
  • The Samyuri area of Jeoksang-myeon, Muju-gun at the Middle Yeongnam Massif consists of granitic gneiss, porphyroblastic gneiss and leucocratic gneiss, which correspond to Precambrian Wonnam Series. Here we discuss a geochemical implication of the data based on major element composition, trace element, rare earth element (REE), Sm-Nd and Rb-Sr isotope systematics of the boring cores in the granite gneiss area. The boring cores are granitic gneiss (including biotite gneiss) and amphibolite. The major and trace element compositions of granitic gneiss and amphibolite suggest that the protolith belongs to TTG (Tonalite-Trondhjemite-Granodiorite) and tholeiitic series, respectively. Chondrte-normalized REE patterns vary in LREE, HREE and Eu anomalies. The granitic gneiss and amphibolite have Sm-Nd whole rock age of $2,026{\pm}230(2{\sigma})$ Ma with an initial Nd isotopic ratio of $0.50979{\pm}0.00028(2{\sigma})$ (initial ${\epsilon}_{Nd}=-4.4$), which suggests that the source material was derived from old crustal material. Particularly, this initial ${\epsilon}$ Nd value belongs to the range of the geochemical evolution of Archean basement in North-China Craton, and also corresponds to the initial Nd isotope evolution line by Lee et al. (2005). In addition, chondrite-normalized REE pattern and initial Nd value of amphibolite are very similar to those of juvenile magma in crustal formation process.

A Provenance Study of Iron Archaeological Sites in the Gyeongsang Province: Petrographic and Geochemical Approaches (경상지역 제철유적의 산지추정 연구: 암석기재학 및 지화학적 접근)

  • Jaeguk Jo;Seojin Kim;Jiseon Han;Su Kyoung Kim;Dongbok Shin;Byeongmoon Kwak;Juhyun Hong;Byeongyong Yu;Jinah Lim
    • Economic and Environmental Geology
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    • v.56 no.4
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    • pp.475-499
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    • 2023
  • To infer the provenance of raw iron materials utilized in iron production at the archaeological sites in Gyeongsang province, petrographic and geochemical analyses were conducted for smelting samples and major iron ores sourced from ore deposits. The smelting samples excavated from various iron archaeological sites were classified into different types according to their refining processes, such as iron bloom, iron bloom slag, pig iron, pig iron slag, forging iron flake, smithery iron, iron flake, and arrowhead. These samples exhibited discernable differences in their mineralogical components and texture. The enrichments of major elements such as aluminum and calcium in silicate minerals of the residual slags and the high contents of trace elements such as nickel and copper in some iron-making relics reflect the characteristics of raw iron ores, and thus can be regarded as potential indicators for inferring the provenance of source materials. In particular, the compositional ranges of Pb-Sr isotope ratios for the iron smelting samples were classified into three categories: 1) those exhibiting similar ratios to those of the raw iron ores, 2) those enriched in strontium isotope ratio, and 3) those enriched in both lead and strontium isotope ratios. The observed distinct Pb-Sr isotope characteristics in the iron smelting samples suggest the potential contribution of specific additives being introduced during the high-temperature refining process. These results provide a new perspective on the interpretation of the provenance study of the iron archaeological samples in Gyeongsang province, particularly in terms of the potential contribution of additives on the refining process.

Chlorella 대량 배양을 위한 농업용 비료에 trace element의 첨가 효과

  • 배진희;이계안;허성범
    • Proceedings of the Korean Aquaculture Society Conference
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    • 2003.10a
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    • pp.88-89
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    • 2003
  • Rotifer의 먹이 생물로 이용되는 Chlorella의 대량 배양에는 농업용 비료가 널리 이용되고 있다. 그러나 농업용 비료만을 사용할 경우 f/2배지에 비해 성장이 낮은 단점이 있다. 따라서 본 연구는 농업용 비료 배지에 여러 가지 미량 성분을 첨가하여 그 성장 변화를 측정하고, 고밀도 대량 배양에 필요한 미량 원소 성분을 파악하고자 하였다. 먼저 Chlorella의 대량 배양에 이용되는 농업용 비료 배지(복합, 요소비료)에 실내 배양에 주로 이용되는 f/2배지의 trace element 성분 중 코발트(Co), 구리(Cu), 아연(Zn) 및 몰리브덴(Mo)를 f/2배지의 함량을 기준으로 각각 0.5, 1.0, 1.5 및 2.0배로 첨가하여 $25^{\circ}C$, 5,000 lux 연속조명, 15$\textperthousand$에서 배양한 결과 각 미량 원소의 첨가 함량이 높을수록 Chlorella의 성장은 높게 나타났다. 전체 실험구 중에서 아연 2.0배, 구리 2.0배를 첨가한 비료 배지에서 S.G.R.이 각각 0.3598, 0.3599의 성장을 나타내었으며, 아연과 구리 성분을 첨가한 Chlorella에서 높은 성장률을 보였다. 위의 실험에서 첨가효과가 좋은 Cu와 Zn 2.0배와 철(Fe)과 망간(Mn)을 같은 비율(0.5~2.0배)로, 다시 배양한 결과, Cu 2.0배와 Zn 2.0배는 S.G.R.이 각각 0.6283과 0.6231로 가장 높았으며, Fe 2.0배, Mn 2.0배와 1.5배에서 S.G.R이 각각 0.6210, 0.6200, 0.6183의 높은 성장률을 나타내었다. 위의 실험에서 농업용 비료에 첨가된 모든 trace element 중에서 가장 좋은 성장을 나타낸 구리(Cu) 성분의 정확한 공급 농도를 파악하기 위하여 농업용 비료에 2, 3, 4 및 5배를 첨가하여 $25^{\circ}C$, 5,000 lux, 15$\textperthousand$에서 배양한 결과, S.G.R.이 CU 함량을 3배로 첨가하였을 경우 2716$\times$$10^4$cells/$m\ell$로 가장 높은 세포 밀도를 나타내었다. 또한 5종의 trace element (Fe, Mn, Zn, Cu, Co)를 혼합하여 비료 배지(1.25배)에 첨가하여 미량 원소간의 상호 작용에 대해서 알아 본 결과, Fe와 Mn 두가지 성분만을 농업용 비료 배지에 혼합하였을 경우 세포수가 2720$\times$$10^4$cells/$m\ell$로서 높은 성장을 나타내었다. 다음으로 Fe, Mn, Zn 및 Cu 4종을 모두 혼합하여 첨가한 실험구가 2608$\times$$10^4$ cells/$m\ell$ 높은 세포 밀도를 나타내었다. 이러한 결과로서 옥외에서 농업용 비료배지에 구리(Cu, f/2배지 기준 3.0배)성분을 첨가함으로써 Chlorella의 성장을 효율적으로 향상시킬 수 있을 것으로 판단된다.

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양인(陽人) 해역병(解?病)과 영양결핍성(營養缺乏性) 질환(疾患)의 상관성(相關性) 연구(硏究) -관우태양인해역병여영양결핍성질병적상관성연구-

  • Lee, Pil-U;Yun, Chang-Yeol
    • Journal of Korean Medical classics
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    • v.18 no.4 s.31
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    • pp.134-144
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    • 2005
  • 통과대해역병재${\ulcorner}$동의수세보원(東醫壽世保元)${\lrcorner}$중적상관내용여현대의학적비교연구(中的相關內容與現代醫學的比較硏究), 가류추출여하결론(可類推出如下結論): ${\ulcorner}$내경(內經)${\lrcorner}$중출현적해역병, 재척부혹맥적진단법급자침적류오인식상(在尺部或脈的診斷法及刺針的謬誤認識上), 언급도해역병. 저시인위파열(這是因爲把熱), 혈소(血少), 비토허(脾土虛), 상화작위료기근원적연고(相火作爲了其根源的緣故). 해역병적증상시‘한불한(寒不寒), 열불열(熱不熱), 약불약(弱不弱), 장불장(壯不壯)’급(及)‘소삭, 행산, 불능거(不能去)’ 재(在)${\ulcorner}$동의수세보원(東醫壽世保元)${\lrcorner}$중칭위‘기병가유(其病可愈)’, 이종현대의학적각도진행연구결과(而從現代醫學的角度進行硏究結果), 인위유류사여말초신경적병증(認爲有類似與末稍神經的病證). 종현대의학적원인래간(從現代醫學的原因來看), 유어단백질(由於蛋白質)-능량적영양결핍화유생소급미량원소적부족(能量的營養缺乏和維生素及微量原素的不足), 출현말초신경병증(出現末稍神經病證). 재(在)${\ulcorner}$동의수세보원(東醫壽世保元)${\lrcorner}$적약물중(的藥物中), 야유능량화유생소급미량원소등성분(也有能量和維生素及微量原素等成分), 소이인위대태양인적처방(所以認爲對太陽人的處方), 종영양학각도진행분석연구시유가치적(從營養學角度進行分析硏究是有價値的).

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Ion Exchange Separation and Spectrofluorometric Determination of Lanthanides in Nuclear Grade Material (이온 질환수지 및 형광분석법에 의한 핵급물질 중희토류원소의 분리정량)

  • Ki-Soo Cho;In-Suck Suh
    • Nuclear Engineering and Technology
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    • v.15 no.2
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    • pp.142-148
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    • 1983
  • Distribution coefficients between cation exchange resin (Dowex 50W$\times$8) and $\alpha$-hydroxyisobutric acid ($\alpha$-HIBA) are measured in order to separate traces of Sm, Eu, Gd and Dy from nuclear material. Individual separations are performed by pH gradient technique with 0.40M $\alpha$-HIBA from 3.40 to 3.60 in cation exchange resin after a group separation. Each of separated elements is determined with a fluorometric method except Gd by colorimetry. The results are applied to analyze Sm, Eu, Gd and Dy in magnesium diuranate (yellow cake).

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Petrology of the Basalts in the Seongsan-Ilchulbong area, Jeju Island (제주도 성산일출봉 일대 현무암에 대한 암석학적 연구)

  • Koh, Jeong-Seon;Yun, Sung-Hyo;Jeong, Eun-Ju
    • Journal of the Korean earth science society
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    • v.28 no.3
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    • pp.324-342
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    • 2007
  • This study reports petrography and geochemical characteristics of the basalt lava flows in Seongsan-Ilchulbong area, the easternpart of Jeju island, Korea, to understand the evolutionary processes of magma. Basalt lavas are classified into the Pyoseon-ri basalt and the Seongsan-ri basalt. The Pyoseon-ri basalt is dark-gray colored with many vescicles, and mainly consists of olivine, feldspar and rarely of clinopyroxene as phenocrysts. The Seongsan-ri basalt is largely aphanitic basalt and bright-gray colored, divided into two lava-flow units: lower lava flow (B1) and upper lava flow (B2) by the intercalated yellowish lapillistone and paleosol. The lavas plotted into sub-alkaline tholeiitic basalt and alkaline basalt series. The tholeiitic basalts have characteristically higher $SiO_2,\;FeO^T$, and CaO contents, but lower $TiO_2,\;K_2O,\;P_2O_5$ and other incompatible elements compared to the alkali basalts. The tholeiitic basalts have higher $SiO_2$ to the same MgO contents than the alkalic basalts. The contents of Ni, Cr, and MgO show a strong positive correlation, which indicates that low-MgO phases like plagioclase and titanomagnetite were important during the differentiation of magma. The contents of incompatible elements against that of Th show a strong positive correlation. The chondrite-nomalized REE patterns of tholeiitic and alkalic basalts are subparallel each other. LREEs contents of the former are lower than, but HREEs contents are similar to the latter. They both are similar to their K/Ba ratios. The primitive-mantle normalized spider diagram demonstrates that the contents of Ba and Th of all basaltic magma are enriched, and yet Cr, Ni are depleted. The tholeiitic and alkalic basalts may be originated from a different degree of the partial melting of the same mantle material source, and one shows a higher degree of the partial melting than the other.

Effect on the Measurement of Trace Element by Pressure Bomb and Conventional Teflon Vial Methods in the Digestion Technique (압력용기 산분해법과 테플론 바이알에서의 산분해법이 미량원소의 함량측정에 미치는 영향)

  • Lee, Seung-Gu;Kim, Taehoon;Tanaka, Tsuyoshi;Lee, Seung Ryeol;Lee, Jong Ik
    • The Journal of the Petrological Society of Korea
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    • v.25 no.2
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    • pp.107-119
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    • 2016
  • Trace element abundances in the igneous rocks are important data for petrogenetic interpretation. Their concentrations are generally measured using ICP-MS from the dissolved solution. The acid digestion of rock powder can be performed by conventional teflon vial or pressure bomb. In this paper, we investigated a problem that happened during acid digestion experiment using conventional teflon vial or pressure bomb of BCR2 and GSP2 USGS rock standard materials. The results show that the measured concentrations of the elements like Cr, Ni, Zn, Ta, W in the BCR2 are different from the recommended values of USGS whereas those of the elements like Rb, Sr, Zr, Hf, Ta, W in the GSP2 are different from those values. Our experiment shows that defect of specific elements like Cr, Ni may happen during the sample digestion. Our results also indicate that the Cr, Ni, W, Zr, Hf, Ta concentration obtained based on an acid digestion of geological samples need to be careful in their geochemical interpretation.

Comparative Assessment of INAA and ICP-MS for the Determination of Trace Elements in Airborne Particulate Matter (대기입자 중 미량원소의 정량을 위한 기기 중성자방사화분석과 유도결합플라즈마 질량분석법의 비교 평가)

  • Lim, Jong-Myoung;Lee, Jin-Hong;Chung, Yong-Sam
    • Journal of Korean Society of Environmental Engineers
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    • v.28 no.10
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    • pp.1038-1045
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    • 2006
  • A series of experiments was conducted to test the compatibilities of two different techniques to determine elemental concentrations by INAA and ICP-MS based on both the NIST SRM 2783(air particulate on filter media) and the field samples for PM10. For NIST SRM the results of INAA were more accurate and precise for all target elements than those of ICP-MS. The comparative data set for PM10 samples collected in an industrial complex area showed that mean of concentration ratio, derived for the two different methods such as C(INNA/ICP-MS), were distinguished from each other: (1) Ba, Cu, K Mg, Na, and Sb: $0.9{\sim}1.1$; (2) Al, Co, Fe, and Mn: $0.8{\sim}1.2$; and (3) Se, Ti, and Zn: >1.3. When the results obtained from both methods were evaluated in terms of regression analysis, paired t-test, and Wilcoxon signed-rank test, the results of many elements determined from PM10 samples(such as Al, Ba, Co, Cu, Fe, K, Mn, Nd, and Sb) exhibited a fairly good agreement between the two methods, despite a wide range of variation.