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검색결과 73건 처리시간 0.025초

비정제 유채유의 산패에 미치는 금속이온의 영향 (Effect of Metal ion on Rancidity of Crude Rapeseed Oil)

  • 김연순;김윤수;남형근;서광엽
    • 환경위생공학
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    • 제24권1호
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    • pp.33-39
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    • 2009
  • In order to investigate effect of metal ion and antioxidant on rancidity of crude rapeseed oil (CRO), $Fe^{2+}$, $Cu^{2+}$, $Co^{2+}$, $Ni^{2+}$, $Cr^{2+}$, $Sn^{2+}$, $Mn^{2+}$, $Zn^{2+}$, and antioxidants including BHA, Vitamin C, and Tocopherol were used. The specific gravity and refractive index of CRO were $0.92g/cm^3$ and 1.45, respectively. The chromaticities of light, red, and yellow in CRO were 88.6 and 98.7, respectively. Among various fatty acids, Oleic acid (C18:1) concentration was highest, 62.3% and Linoleic acid (C18:2) concentration was 19.16%. In the case of Linolenic acid (C18:3) and Palmitic acid (C16:0), they were 9.88 and 5.2%, respectively. The concentrations of unsaturated fatty acids and saturated fatty acid were 92.2 and 7.8%, respectively. The degree of expediting rancidity of CRO was an order of $Fe^{2+}$> $Cu^{2+}$> $Cr^{2+}$> $Zn^{2+}$> $Ni^{2+}$> $Al^{2+}$> $Mn^{2+}$> $Mn^{2+}$> $Sn^{2+}$> $Co^{2+}$> $Li^{2+}$. Especially, when $Cu^{2+}$ and $Fe^{2+}$ was used, the peroxide value concentration was about 4.0 fold higher than non addition of them. The inhibition effect of rancidity of CRO using antioxidant with $Cu^{2+}$ and $Fe^{2+}$ was an order of BHA> Vitamin C> Tocopherol.

저온균일침전법에 의해 제조된 $TiO_2$의 상변화 (Phase Transition of $TiO_2$ prepared by HPPLT)

  • 황두선;이남희;이강;김선재
    • 한국재료학회:학술대회논문집
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    • 한국재료학회 2003년도 춘계학술발표강연 및 논문개요집
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    • pp.208-208
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    • 2003
  • 저온균일침전법(HPPLT)으로 제조된 TiO$_2$나노분말은 10$0^{\circ}C$이하의 온도에서 rutile상을 얻을 수 있다. 또한, rutile에서 anatase로의 상변화는 합성시간, 가열속도, 반응온도 그리고 음이온 첨가에 의해 일어난다고 보고되어졌지만, 금속양이온들에 의한 상변화는 알려진 바가 없다. 따라서, 다양한 양이온을 첨가하여 저온균일침전법에서 TiO$_2$의 상변화가 어떻게 일어나는지를 조사하였다. 출발원료인 TIC1$_4$를 사용하여 가수분해하여 0.67M의 TiOCl$_2$을 얻었다. 얻어진 TiOCl$_2$ 수용액에 각각 0.01M의 금속염화물(ZrOCl$_2$, NiCl$_2$, CuCl$_2$, FeCl$_3$, AlCl$_3$ 그리고 NbCl$_{5}$)을 첨가한 후 반응기에 넣고 10$0^{\circ}C$에서 4시간동안 가열하였다 가열한 후 얻어진 침전물에 NaOH 수용액을 이용하여 PH 7-8로 중화한 후 증류수로 Cl$^{-}$이온이 제거될 때까지 충분히 세척하였다. 세척된 침전물을 105$^{\circ}C$에서 24h동안 건조하여 분말을 얻었고, rutile에서 anatase로의 상변화특성을 관찰하기 위하여 XRD, SEM, TEM, ICP 분석을 실시하였다.

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일라이트, 할로이사이트에 대한 중금속 원소의 흡착특성 (Adsorption Behaviors of Metal Elements onto Illite and Halloysite)

  • 추창오;김수진;정찬호;김천수
    • 한국광물학회지
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    • 제11권1호
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    • pp.20-31
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    • 1998
  • Adsorption of metal elements onto illite and halloysite was investigated at $25^{\circ}C$ using pollutant water collected from the gold-bearing metal mine. Incipient solution of pH 3.19 was reacted with clay minerals as a function of time: 10 minute, 30 minute, 1 hour, 12 hour, 24 hour, 1 day, 2 day, 1 week, and 2 week. Twenty-seven cations and six anions from solutions were analyzed by AAs (atomic absorption spectrometer), ICP(induced-coupled plasma), and IC (ion chromatography). Speciation and saturation index of solutions were calculated by WATEQ4F and MINTEQA2 codes, indicating that most of metal ions exist as free ions and that there is little difference in chemical species and relative abundances between initial solution and reacted solutions. The adsorption results showed that the adsorption extent of elements varies depending on mineral types and reaction time. As for illite, adsorption after 1 hour-reaction occurs in the order of As>Pb>Ge>Li>Co, Pb, Cr, Ba>Cs for trace elements and Fe>K>Na>Mn>Al>Ca>Si for major elements, respectively. As for halloysite, adsorption after 1 hour-reaction occurs in the order of Cu>Pb>Li>Ge>Cr>Zn>As>Ba>Ti>Cd>Co for trace elements and Fe>K>Mn>Ca>Al>Na>Si for major elements, respectively. After 2 week-reaction, the adsorption occurs in the order of Cu>As>Zn>Li>Ge>Co>Ti>Ba>Ni>Pb>Cr>Cd>Se for trace elements and Fe>K>Mn>Al, Mg>Ca>Na, Si for major elements, respectively. No significant adsorption as well as selectivity was found for anions. Although halloysite has a 1:1 layer structure, its capacity of adsorption is greater than that of illite with 2:1 structure, probably due to its peculiar mineralogical characteristics. According to FTIR (Fourier transform infrared spectroscopy) results, there was no shift in the OH-stretching bond for illite, but the ν1 bond at 3695 cm-1 for halloysite was found to be stronger. In the viewpoint of adsorption, illite is characterized by an inner-sphere complex, whereas halloysite by an outer-sphere complex, respectively. Initial ion activity and dissociation constant of metal elements are regarded as the main factors that control the adsorption behaviors in a natural system containing multicomponents at the acidic condition.

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문경지역 폐탄광지 주변 산림토양의 화학적 성질 및 중금속 함량 (Chemical Properties and Heavy Metal Content of Forest Soils around Abandoned Coal Mine Lands in the Mungyeong Area)

  • 민재기;박은희;문현식;김종갑
    • 한국농림기상학회지
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    • 제7권4호
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    • pp.265-273
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    • 2005
  • 본 연구에서는 폐탄광 주변 산림의 복원을 위한 기초자료를 제공하고자 경북 문경지역에 위치한 폐탄광 중 4개의 광산을 대상으로 산림토양의 화학적 특성과 중금속 오염현황을 i.자한 결과를 보고한다 폐탄광지 산림토양의 pH는 $5.30\~6.76$의 범위에 있었으며, 대조구 지역의 토양 pH는 5.23이었다. 폐탄광지역의 산림토양 중 유기물과 전질소 함량은 각각 $4.46\~7.19\%,\;0.07\~0.15\%$의 범위에 있는 것으로 조사되었다. 평균 유효인산 함량은 삼창탄광 6.54, 봉명탄광 6.52, 갑정탄광 3.94, 단봉탄광 5.45 그리고 대조구 5.25mg/kg으로 토양 pH와 정의 상관을 가지는 것으로 나타났다. 폐탄광지역의 치환성양이온 평균 함량은 Ca 196.1, Mg 88.7, K 88.2 그리고 Na $10.2cmol^+/kg$로 나타났으며, 그 범위는 Ca $132.1\~242.1,\;Mg 24.2\~138.6,\;K 64.9\~120.8$ 그리고 Na $8\~12.2cmol^+/kg$에 있는 것으로 조사되었다 대조구 지역의 Ca, Mg, K, Na의 평균 함량은 각각 192.8, 95.8, 104 and $21.2 cmol^+/kg$로 조사되었다. 폐탄광지 산림토양의 중금속(Al, As, Cd, Cr, Cu, Fe, Mn, Ni, Pb, Zn) 함량은 대조구 산림토양보다 높은 것으로 분석되었다. 특히, Al, Mn 그리고 Pb의 함량은 대조구에 비해 폐탄광지가 아주 높은 것으로 나타났다. 폐탄광지 산림토양의 Al함량은 $397\~917 ppm$으로 나타나 식물생육에 영향을 미칠 수 있을 것으로 추정된다 그러므로 과거 석탄채굴이 활발하게 이루어졌던 폐탄광지에 대해서는 환경문제를 최소화하기 위하여 산림토양을 대상으로 한 적절한 관리가 필요할 것으로 추정된다.

Elemental Composition of the Soils using LIBS Laser Induced Breakdown Spectroscopy

  • Muhammad Aslam Khoso;Seher Saleem;Altaf H. Nizamani;Hussain Saleem;Abdul Majid Soomro;Waseem Ahmed Bhutto;Saifullah Jamali;Nek Muhammad Shaikh
    • International Journal of Computer Science & Network Security
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    • 제24권6호
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    • pp.200-206
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    • 2024
  • Laser induced breakdown spectroscopy (LIBS) technique has been used for the elemental composition of the soils. In this technique, a high energy laser pulse is focused on a sample to produce plasma. From the spectroscopic analysis of such plasma plume, we have determined the different elements present in the soil. This technique is effective and rapid for the qualitative and quantitative analysis of all type of samples. In this work a Q-switched Nd: YAG laser operating with its fundamental mode (1064 nm laser wavelength), 5 nanosecond pulse width, and 10 Hz repetition rate was focused on soil samples using 10 cm quartz lens. The emission spectra of soil consist of Iron (Fe), Calcium (Ca), Titanium (Ti), Silicon (Si), Aluminum (Al), Magnesium (Mg), Manganese (Mn), Potassium (K), Nickel (Ni), Chromium (Cr), Copper (Cu), Mercury (Hg), Barium (Ba), Vanadium (V), Lead (Pb), Nitrogen (N), Scandium (Sc), Hydrogen (H), Strontium (Sr), and Lithium (Li) with different finger-prints of the transition lines. The maximum intensity of the transition lines was observed close to the surface of the sample and it was decreased along the axial direction of the plasma expansion due to the thermalization and the recombination process. We have also determined the plasma parameters such as electron temperature and the electron number density of the plasma using Boltzmann's plot method as well as the Stark broadening of the transition lines respectively. The electron temperature is estimated at 14611 °K, whereas the electron number density i.e. 4.1 × 1016 cm-3 lies close to the surface.

중국 Xiquegou 연-아연 광상의 돌로마이트와 녹니석 산상과 화학조성 (Occurrence and Chemical Composition of Dolomite and Chlorite from Xiquegou Pb-Zn Deposit, China)

  • 유봉철
    • 광물과 암석
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    • 제35권2호
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    • pp.125-140
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    • 2022
  • Xiquegou 연-아연 광상은 중국 동북지역에선 가장 규모가 큰 연-아연 광화대 중의 하나인 Qingchengzi orefield에 위치한다. 이 광상의 주변지질은 시생대의 그래뉼라이트(granulite)와 이를 관입한 고원생대의 미그마타이트질 화강암과 고-중원생대의 소딕(sodic) 화강암을 부정합으로 피복한 고원생대의 Liaohe 층군 및 이들을 관입한 중생대의 섬록암과 몬조나이틱 화강암으로 구성된다. 이 광상은 고원생대의 Liaohe 층군내 Dashiqiao 층의 unit 3(돌로마이트질 대리암과 편암)내에 발달된 단층대를 따라 산출되는 맥상 광체로 트라이아스기의 마그마-열수형 광상에 해당된다. Xiquegou 연-아연 광상에서 석영, 인회석, 방해석, 황철석, 유비철석, 자류철석, 백철석, 섬아연석, 황동석, 황석석, 방연석, 사면동석, 에렉트럼, 휘은석, 자연은 및 농홍은석 등이 산출되며 모암변질로는 규화작용, 황철석화작용, 돌로마이트화작용, 녹니석화작용 및 견운모화작용 등이 관찰된다. 이 광상의 산출 광물조합 및 정출순서를 기초로, 돌로마이트는 1)모암인 돌로마이트(D0) 및 2)연-아연 광화작용에 따른 모암변질 산물인 돌로마이트(D1)로 두 유형이 확인된다. 이들 돌로마이트의 화학조성은 각각 Ca1.03-1.01Mg0.95-0.83 Fe0.12-0.02Mn0.02-0.00(CO3)2(D0) 및 Ca1.16-1.00Mg0.79-0.44Fe0.53-0.13Mn0.03-0.00As0.01-0.00(CO3)2(D1)로써 이론적인 돌로마이트의 화학조성보다 미량원소들의 함량이 높다. 특히, FeO, PbO, Sb2O5 및 As2O5 원소들은 모암변질 산물인 돌로마이트(D1)에서 높은 함량을 갖는다. 또한 이 광상의 모암에서 산출되는 돌로마이트(D0)는 Ferroan 돌로마이트에 해당되며 모암변질 산물인 돌로마이트(D1)는 철백운석 및 Ferroan 돌로마이트에 해당된다. 모암변질 산물인 녹니석의 화학조성은 (Mg1.65-1.08Fe2.94-2.50Mn0.01-0.00Zn0.01-0.00Ni0.01-0.00Cr0.02-0.00V0.01-0.00Hf0.01-0.00Pb0.01-0.00Cu0.01-0.00As0.03-0.00Ca0.02-0.01Al1.68-1.61)5.77-5.73(Si2.84-2.76Al1.24-1.16)4.00O10(OH)8로써 이론적인 녹니석과 유사하며 Fe-rich 녹니석에 해당된다. 또한 이 녹니석의 화학조성 변화는 주로 팔면체적 Fe2+ <-> Mg2+ (Mn2+) 치환과 일부 팬자이틱 또는 Tschermark 치환(Al3+,VI+Al3+,IV <-> (Fe2+ 또는 Mg2+)VI+(Si4+)IV)메카니즘에 의해 일어났음을 알 수 있다.

LA-ICP-MS를 이용한 한국 자동차 유리의 미량원소 분석 (Trace element analysis of korean car windshield using LA-ICP-MS)

  • 민지숙;최만식;허상철;김재균
    • 분석과학
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    • 제22권3호
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    • pp.235-246
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    • 2009
  • 제조 공장의 구분이 가능한지 검토하기 위하여 LA-ICP-MS를 이용한 한국 자동차 전면 유리의 미량원소 분석을 실시하였다. 먼저 Si를 내부 표준물질로 하여 표준품 NIST 610, 612, 614과 616을 분석하여 검량선을 작성하였다. 시료와 표준품은 24원소에 대해 정량을 실시하였고 LOQ는 0.11 mg/kg(Ti)-4.91 mg/kg(Ca) 였다. 2개 공장의 11개 시료에 대하여 각각 5개씩의 위치에 따른 부시료를 분석하였다. 검출한계이하의 원소들(Cu, Cr, Cd와 Ni), 표준품에 존재하지 않는 원소들(Ti, Pr, Mg, Nb, Nd)과 균질성에 문제가 있는 원소들(Pb와 Sn)은 분석 대상 원소에서 제외하였다. 제조공장과 제조년도와 관련하여 삼각 다이어그램을 그려 본 결과 구별의 가능성을 볼 수 있었으며 Mn, Ce와 Rb를 토대로 한 정준 판별 분석식에 의해 제조공장의 구별이 가능하였다.

나림 금광상의 열수변질대에서 산출되는 녹색크롬-견운모의 광물학적 및 지구화학적 특징 (Mineralogy and Geochemistry of Green-colored Cr-bearing Sericite from Hydrothermal Alteration Zone of the Narim Gold Deposit, Korea)

  • 이현구;이찬희
    • 자원환경지질
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    • 제30권4호
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    • pp.279-289
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    • 1997
  • Dark to pale green-colored, Cr-bearing sericites from hydrothermal alteration zone of the Narim gold deposit were investigated mineralogically and geochemically. The alteration zone is composed mineralogically of quartz, carbonate minerals and green sericite with minor amounts of chlorite, barite and sulfide minerals (pyrite, sphalerite, galena). The zone is enriched in As (967 to 1520 ppm), Cu (31 to 289 ppm), Ni (1027 to 1205 ppm), Pb (0.20 to 1.24 wt.%) and Zn (1.03 to 1.07 wt. %) compared with fresh rocks such as granitic gneiss, porphyritic biotite granite and basic dyke. The Cr, probably the chromophore element, is highly enriched in the alteration zone (1140 to 1500 ppm), host granitic gneiss (1200 ppm) and porphyritic biotite granite (1200 ppm). Occurrence and grain size of sericite are diverse, but most of the Cr-bearing sericites (150 to $200{\mu}m$ long and 20 to $30{\mu}m$ wide) occur along the boundaries between ore veins and host rocks (especially basic dyke and granitic gneiss). X-ray diffraction data of the sericite show its monoclinic form with unit-cell parameters of $a=5.202{\AA}$, $b=8.994{\AA}$, $c=20.103{\AA}$, ${\beta}=95.746^{\circ}$ and $V=935.83{\AA}^3$, which are similar with the normal 2M1-type muscovite. Representative chemical formula of the sericite is ($K_{1.54}Ca_{0.03}Na_{0.01}$)($Al_{3.42}Mg_{0.38}Cr_{0.14}Fe_{0.06}V_{0.02}$)($Si_{6.69}Al_{1.31}$)$O_{20}(OH)_4$. The Cr content increases with decrease of the octahedral Al content, and ranges from 0.36 to 2.58 wt.%. DTA and TG curves of the sericite show endothermic peaks at $342^{\circ}$ to $510^{\circ}$, $716^{\circ}$ to $853^{\circ}$ and $1021^{\circ}C$, which are due to the expulsion of hydroxyl group. The total weight loss by heating is measured to be about 8.8 wt. %, especially at $730^{\circ}C$. Infrared absorption experiments of the sericite show broad absorption band due to the O-H bond stretching vibration near the $3625cm^{-1}$, coupled with the 825 and $750cm^{-1}$ doublet. The vibration bands related with the H-O-Al and Si-O-Al bonds occur at $1030cm^{-1}$ and 500 to $700cm^{-1}$, respectively. Based on paragonite content of the sericite, the formation temperature of the Narim gold deposit is calculated to be $220{\pm}10^{\circ}C$.

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Submicron 부유분진의 화학적 조성 및 분포에 관한 연구 (Studies on the Chemical Compositions and Distributions of Ambient Sumicron Aerosols)

  • 황인조;김동술
    • 한국대기환경학회지
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    • 제14권1호
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    • pp.11-23
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    • 1998
  • The purpose of this study was to survey chemical distribution of inorganic elements and ions in the submicron particles, to characterize qualitatively emitting sources by factor analysis, and finally to reveal existing patterns in terms of chemical compounds by a stepwise multiple regression analysis. Total of 141 samples were collected by a cascade impactor from 1989 to1996. Fifteen chemical species (Al, Ba, Cd, K, Pb, Cu, Fe, Ni, $Cl^-, NO_3^-, SO_4^{2-}, K^+, Mg^{2+}, Ca^{2+}, and Na^+$) were characterized by AAS and IC. The study showed that average seasonal levels of submicron particulate matters $(d_p<0.43 \mum)$ were 18.7 $\mug/m^3$ in spring, 15.5 $\mug/m^3$ in summer, 15.7 $\mug/m^3$ in fall, and 24.5 $\mug/m^3$ in winter, respectively. All of the anion concentrations in the particle were highest in the winter season. By applying a factor analysis, 5 source patterns were qualitatively obtained, such as sulfate related source, nitrate related source, oil burning source, calcium related source, and coal combustion source. Finally, when applying a stepwise multiple regression analysis, the results clearly showed that $Na^+ and Ca^{2+}, K^+ and Ca^{2+}, NO_3^-$ and relative humidity, $Cl^-$ and ambient temperature, $Ca^{2+} and Cl^-, Mg^{2+} and SO_4^{2-}, Na^+ and NO_3^-, and Ca^{2+} and NO_3^-$, respectively, are negatively contributed to each other. As a result of those statistical analysis, we could suggest that some chemical compounds in the submicron particles such as$NaNO_3, MgSO_4, Ca(NO_3)_2, and CaCl_2$ may not exist on the filter as final composing products; however, other compounds may possibly exist in the form of $Mg(NO_3)_2, CaSO_4, Na_2SO_4, K_2SO_4, MgCl_2, NaCl, and KCl$. Thus, it must be necessary to identify differences between the results of above statistical analysis and of the real world by laboratory experiments.

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Mineralogy and Geochemistry of Shale Deposits in the Lower Anambra Basin, Nigeria: Implication for Provenance, Tectonic Setting and Depositional Environment

  • Olugbenga Okunlola;Agonsi Udodirim Lydia;Aliyu Ohiani Umaru;Raymond Webrah Kazapoe;Olusegun G. Olisa
    • 자원환경지질
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    • 제56권6호
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    • pp.799-816
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    • 2023
  • Mineralogical and geochemical studies of shales within the Lower Anambra Basin was conducted to unravel the depositional environment, provenance, maturity, paleo-weathering conditions, and tectonic settings. Mineralogical studies conducted using X-ray diffraction analysis revealed that the samples were composed of kaolinite, montmorillonite, chlorite, and illite. KaolinIite is the dominant mineral, constituting approximately 41.5% of the bulk composition, whereas the non-clay minerals are quartz, ilmenite, and sillimanite. Geochemical analysis showed a predominance of SiO2, Al2O3, and Fe2O3 contents of the shale samples with mean values of 52.29%, 14.09%, and 6.15% for Imo Shale (IS); 52.31%, 16.70%, and 7.39% for Mamu Shale (MS); 43.21%, 21.33%, and 10.36% for Enugu Shale (ES); 53.35%, 15.64%, and 7.17% for Nkporo Shale (NS); and 51.24%, 17.25%, and 7.78% for Agwu Shale (AS). However, the shales were depleted in Na2O, MgO, K2O, MnO, TiO2, CaO, and P2O5. The trace element ratios of Ni/Co and Cu/Zn of the shale suggest an oxic depositional environment. The average SiO2 vs. Al2O3 ratio of the shales indicated textural maturity. Compared to the PAAS standard, the shales plot below the PAAS value of 0.85, suggesting a high degree of maturity and intensive chemical weathering, further confirmed on a CIA vs. PIA plot. On log (K2O/Na2O) against SiO2 and tectonic setting discriminant function diagrams, the shales plot mostly in the field of passive continental margin tectonic setting. The discriminant function diagrams as well as Al2O3/TiO2 ratio of the shales showed that they were derived from a mixed source (mafic and intermediate igneous rocks).