• Title/Summary/Keyword: FeRB

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Significance of Dissimilatory Fe(III) Reduction in Organic Matter Oxidation and Bioremediation of Environmental Contaminants in Anoxic Marine Environments (혐기성 해양환경에서 철 환원세균에 의한 유기물 분해 및 생물정화)

  • Hyun Junc-Ho
    • The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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    • v.10 no.3
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    • pp.145-153
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    • 2005
  • I reviewed an ecological and environmental significance of microbial carbon respiration coupled to dis-similatory reduction of fe(III) to Fe(II) which is one of the major processes controlling mineralization of organic matter and behavior of metals and nutrients in various anaerobic environments. Relative significance of Fe(III) reduction in the mineralization of organic matter in diverse marine environments appeared to be extremely variable, ranging from negligible up to $100\%$. Cenerally, Fe(III) reduction dominated anaerobic car-bon mineralization when concentrations of reactive Fe(III) were higher, indicating that availability of reactive Fe(III) was a major factor determining the relative significance of Fe(III) reduction in anaerobic carbon mineralization. In anaerobic coastal sediments where $O_2$ supply is limited, tidal flushing, bioturbation and vegetation were most likely responsible for regulating the availability of Fe(III) for Fe(III) reducing bacteria (FeRB). Capabilities of FeRB in mineralization of organic matter and conversion of metals implied that FeRB may function as a useful eco-technological tool for the bioremediation of anoxic coastal environments contaminated by toxic organic and metal pollutants.

Element Dispersion by the Wallrock Alteration of Janggun Lead-Zinc-Silver Deposit (장군 연-아연-은 광상의 모암변질에 따른 원소분산)

  • Yoo, Bong Chul
    • Economic and Environmental Geology
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    • v.45 no.6
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    • pp.623-641
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    • 2012
  • The Janggun lead-zinc-silver deposit is hydrothermal-metasomatic deposit. We have sampled wallrock, hydrother-maly-altered rock and lead-zinc-silver ore vein to study the element dispersion during wallrock alteration. The hydrothermal alteration that is remarkably recognized at this deposit consists of rhodochrositization and dolomitization. Wallrock is dolomite and limestone that consisit of calcite, dolomite, quartz, phlogopite and biotite. Rhodochrosite zone occurs near lead-zinc-silver ore vein and include mainly rhodochrosite with amounts of calcite, dolomite, kutnahorite, arsenopyrite, pyrite, chalcopyrite, sphalerite, galena and stannite. Dolomite zone occurs far from lead-zinc-silver ore vein and is composed of mainly dolomite and minor calcite, rhodochrosite, pyrite, sphalerite, chalcopyrite, galena and stannite. The correlation coefficients among major, trace and rare earth elements during wallrock alteration show high positive correlations(dolomite and limestone = $Fe_2O_3(T)$/MnO, Ga/MnO and Rb/MnO), high negative correlations(dolomite = MgO/MnO, CaO/MnO, $CO_2$/MnO, Sr/MnO; limestone = CaO/MnO, Sr/MnO). Remarkable gain elements during wallrock alteration are $Fe_2O_3(T)$, MnO, As, Au, Cd, Cu, Ga, Pb, Rb, Sb, Sc, Sn and Zn. Remarkable loss elements are CaO, $CO_2$, MgO and Sr. Therefore, elements(CaO, $CO_2$, $Fe_2O_3(T)$, MgO, MnO, Ga, Pb, Rb, Sb, Sn, Sr and Zn) represent a potential tools for exploration in hydrothermal-metasomatic lead-zinc-silver deposits.

A Geochemical Study on Trace Elements in the Granitic Rocks in relation to Mineralization in the Limestone Area of the Taebaegsan Basin (화강암류중 미량원소와 태백산분지내 석회암지역 광화작용과의 지구화학적 관계)

  • Lee, Jae Yeong
    • Economic and Environmental Geology
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    • v.20 no.3
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    • pp.179-196
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    • 1987
  • Various skarn ore deposits of Pb-Zn, Fe-Cu, W-Mo and others are widely distributed in the study area which consists mainly of Cambro Ordovician calcareous rocks. The ore deposits are all in close association with specific types of granitic rocks of mid-late Cretaceous age according to the kinds of ores: Fe-Cu deposit with granodiorite-quartz monzodiorite, Pb-Zn deposit with granite-granodiorite, W-Mo deposit with granite, and Mn deposit with quartz porphyry. The granitic rock of Fe-Cu deposit has lower content in K and higher in Ca than those of Pb-Zn deposits. On the contrary, the granitic rock of W-Mo deposit has much higher content in K and lower in Ca in comparison to those of Pb-Zn deposits. However, the granitic rock of Mn deposit shows similar variation to those of Pb-Zn deposits. Lithophile trace elements of Sr and Rb tend to vary in close relation with major elements of K and Ca, respectively. In good contrast, chalcophile elements of Cu, Pb, Zn, Wand Mo are enriched in the granitic rocks of their ore deposits, and other trace elements of Ni and Co show a trend to vary in relation with Mg, Fe and Cu, which have the same replacement index (0.14) as Ni and Co. Average K/Rb and Ca/Sr ratios of the granitic rocks range nearly within 300~150 and 150~40, respectively, and the distribution pattern of the ratios is different according to the kind of ore deposits: Fe-Cu deposit is plotted toward K-Rb poor region whereas Pb-Zn and W-Mo deposits toward K-Rb rich region. In contrast, Fe-Cu and Fe deposits are plotted toward Ca-Sr rich region whereas Pb-Zn deposit toward Ca-Sr poor region. The variation trend of chemical elements of the mid-late Cretaceous granitic rocks in the study area is similar to that of the Cretaceous granitic rocks in the Gyeongsang Basin. Therefore, this geochemical result may be applicable to determining what kinds of ore deposits a Cretaceous granitic rock is favourable for, and whether it is productive or non-productive for systematic geochemical exploration works.

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Precipitation of cations by alginate, polyguluronate and polymannuronate

  • Jeong, Dae-Yeong;Seo, Hyeong-Pil;Lee, Dong-Su;Byeon, Jae-Hyeong;Lee, Jin-U
    • 한국생물공학회:학술대회논문집
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    • 2000.11a
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    • pp.495-499
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    • 2000
  • The relative affinity of seaweed alginate, polyguluronate and polymannuronate for cations was investigated. The cations used in this study were $Ca^{2+}$, $Cd^{2+}$, $Co^{2+}$, $Cu^{2+}$, $Fe^{3+}$, $Hg^{2+}$, $Mg^{2+}$, $Mn^{2+}$, $Pb^{2+}$, $Rb^{1+}$, $Sr^{2+}$ and $Zn^{2+}$. The ability of cations to precipitated polymers was determined as the relative affinity of seaweed alginate, polyguluronate and polymannuronate for cations. The relative affinity of polymers for cations in order are as follow: Seaweed alginate: $Fe^{3+}$,$Cu^{2+}$,$Cd^{2+}>Pb^{2+}>Co^{2+}$,$Zn^{2+}>Ca^{2+}>Sr^{2+}$,$Rb^{1+}>Mn^{2+}>Mg^{2+}$,$Hg^{2+}$ Ployguluronate:$Fe^{3+}$,$Cu^{2+}$,$Cd^{2+}>Ca^{2+}$,$Co^{2+}$,$Pb^{2+}>Sr^{2+}$,$Rb^{1+}$,$Zn^{2+}>Hg^{2+}$,$Mn^{2+}>Mg^{2+}$ Polymannuronate:$Fe^{3+}$,$Cd^{2+}$,$Cu^{2+}>Ca^{2+}$,$Pb^{2+}>Zn^{2+}$,$Rb^{1+}$$Sr^{2+}$,$Hg^{2+}>Co^{2+}>Mn^{2+}>Mg^{2+}$

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Rb-Sr Isotopic Ages of Biotite in the Weathering Profile of Granodiorite, Yecheon (예천지역 화강섬록암 풍화대내 흑운모의 Rb-Sr 동위원소연대 변화)

  • Jeong Gi Young;Cheong Chang-Sik;Lee Bong Ho
    • Journal of the Mineralogical Society of Korea
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    • v.18 no.1
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    • pp.53-59
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    • 2005
  • Rb-Sr isotopic ages of oxidized biotite in the weathering profile of granodiorite, Yecheon area, were measured by thermal ionization mass spectrometry, and compared with their K-Ar ages. A decrease of Rb-Sr isotopic age is well correlated with iron oxidation, and consistent with K-Ar age. Octahedral and interlayer cations including Rb and Sr were partly released from the oxidizing biotite by excess positive charge from iron oxidation. Divalent /sup 87/Sr decayed from monovalent /sup 87/Rb was more easily released from biotite, resulting in the reduction of Rb-Sr isotopic age. Weathered biotite is not suitable for the age dating of parent rocks, but behaviour of radiogenic isotopes provides useful information on the geochemical and structural changes of biotite during weathering.

Optimization of Hybrid Process of(Chemical Coagulation, Fenton Oxidation and Ceramic Membrane Filtration) for the Treatment of Reactive Dye Solutions (반응성 염료폐수 처리를 위한 화학응집, 펜톤산화, 세라믹 분리막 복합공정의 최적화)

  • Yang, Jeong-Mok;Park, Chul-Hwan;Lee, Byung-Hwan;Kim, Tak-Hyun;Lee, Jin-Won;Kim, Sang-Yong
    • Journal of Korean Society of Environmental Engineers
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    • v.28 no.3
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    • pp.257-264
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    • 2006
  • This study investigated the effects of hybrid process(chemical coagulation, Fenton oxidation and ceramic UF(ultrafiltration)) on COD and color removals of commercial reactive dyestuffs. In the case of chemical coagulation, the optimal concentrations of $Fe^{3+}$ coagulant for COD and color removals of RB49(reactive blue 49) and RY84(reactive yellow 84) were determined according to the different coagulant dose at the optimal pH. They were 2.78 mM(pH 7) in RB49 and 1.85 mM(pH 6) in RY84, respectively. In the case of Fenton oxidation, the optimal concentrations of $Fe^{3+}\;and\;H_2O_2$ were obtained. Optimal $[Fe^{2+}]:[H_2O_2]$ molar ratio of COD and color removals of RB49 and RY84 were 4.41:5.73 mM and 1.15:0.81 mM, respectively. In the case of ceramic UF, the flux and rejection of supernatant after Fenton oxidation were investigated. After ceramic UF for 9 hr, the average flux of RB49 and RY84 solutions were $53.4L/m^2hr\;and\;67.4L/m^2hr$ at 1 bar, respectively. In addition, the permeate flux increased and the average flux recovery were 98.5-99.9%(RB49) and 91.0-97.3%(RY84) according to adopting off-line cleaning(5% $H_2SO_4$). Finally, COD and color removals were 91.6-95.7% and 99.8% by hybrid process, respectively.

The Geochemistry of Yuksipryeong Two-Mica Leucogranite, Yeongnam Massif, Korea (영남육괴내 육십령 복운모화강암에 대한 지화학적 연구)

  • Koh, Jeong-Seon;Yun, Sung-Hyo
    • The Journal of the Petrological Society of Korea
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    • v.12 no.3
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    • pp.119-134
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    • 2003
  • Yuksipryeong two-mica granite presents strongly peraluminous characteristics in both mineralogy and geochemistry. It has high aluminum saturation index with 1.15∼l.20 and high corundum with 2.20∼2.98 wt% CIPW norm. As the color index is <16% and FeO$\^$T/+ MgO + TiO$_2$is average 1.9 wt%, it corresponds to leucogranite. Yuksipryeong two-mica leucogranite shows negative linear trend for TiO$_2$, Al$_2$O$_3$, FeO, Fe$_2$O$_3$, MgO, CaO, K$_2$O, P$_2$O$\_$5/, Rb, Ba, and Sr as SiO$_2$increases, and the positive relation of Zr and Th, which result from feldspar, biotite, apatite and zircon fractionation. Pegmatitic dike has higher SiO$_2$and P$_2$O$\_$5/, but lower another major elements. Yuksipryeong two-mica leucogranite has lower Rb, but higher Ba and Sr than Manaslu, Hercynian two-mica leucogranites, and S-type granites in Lachlan Fold Belt. Pegmatitic dike has higher Rb and Nb but lower Ba, Sr, Zr, Th, and Pb contents than Yuksipryeong two-mica leucogranite, resulting in removing or mobilizing for some trace elements from the granitic melt. Yuksipryeong two-mica leucogranite has total REEs with 95.7∼l23.3 ppm, and chondrite-normalized REE pattern is very steep ((La/Yb)$\_$N/ = 6.9∼24.8), light REEs (LREEs)-enriched End heavy REEs (HREEs)- depleted pattern with low to moderate Eu anomalies (Eu/Eu*= 0.7∼0.9). While pegmatitic dike has low total REEs with 7.0 ppm, and chondrite-normalized REE pattern is flat-pattern ((La/Yb)$\_$N/ = 2.1) with strong negative Eu anomalies (Eu/Eu*= 0.2). The melt compositions having formed two-mica leucogranites depend on not only the source rock but also the amounts of the residual remaining after melting of source rocks. The CaO/Na$_2$O and Rb/Sr-Rb/Ba ratios depend mainly on the composition of source rocks in the strongly peraluminous granite, that is, plagioclase/clay ratio of the source rocks. Yuksipryeong two-mica leucogranite has higher CaO/Na$_2$O and lower Rb/Sr-Rb/Ba ratios than Manaslu and Hercynian two-mica leucogranites (Millevaches and Gueret) derived from clay-rich, plagioclase-poor (polite), which suggest that the probable source rocks for Yuksipryeong two-mica leucogranite is clay-poor, plagioclase-rich quartzofeldspathic rocks. As the concentrations of Al$_2$O$_3$remain nearly constant but those of TiO$_2$increases as increasing temperature in the strong peraluminous melt, the Al$_2$O$_3$/TiO$_2$ratio may reflect relative temperature at which the melts have formed. Comparing the polite-derived Manaslu and Hercynian two- mica leucogranites, Manaslu two-mica leucogranite has higher Al$_2$O$_3$/TiO$_2$ratio than latter, and its melt have formed at relatively lower temperature ($\leq$ 875$^{\circ}C$) than Hercynian two-mica leucogranites. Likewise, comparing the quartzofeldspathic rock-derived granites, Yuksipryeong two-mica granite has higher Al$_2$O$_3$/TiO$_2$, ratio than S-type granites in Lachlan Fold Belt (>875$^{\circ}C$). The melt formed Yuksipryeong two-mica leucogranite are considered to have been formed at temperature at below the maximum 875$^{\circ}C$C$.

Biosorption of Metal Ions by Seaweed Alginate, Polyguluronate, and Polymannuronate (알긴산, 폴리글루론산 및 폴리만뉴론산에 의한 금속이온의 흡착)

  • Jung, Dae-Young;Son, Chang-Woo;Kim, Sung-Koo;Kim, Yi-Joon;Chung, Chung-Han;Lee, Jin-Woo
    • Journal of Life Science
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    • v.19 no.5
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    • pp.553-560
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    • 2009
  • Based on $P_{1/2}$ values, relative affinities of alginate, polyguluronate, and polymannuronate for metal ions are, in order, as follows; 1) seaweed alginate: $Cu^{2+}$ > $Cd^{2+}$ > $Pb^{2+}$ > $Fe^{3+}$ >> $Zn^{2+}$ > $Sr^{2+}$ > $Ca^{2+}$ > $Co^{2+}$ >> $Cr^{6+}$ > $Mn^{2+}$ >> $Hg^{2+}$, $Mg^{2+}$, $Rb^+$, 2) polyguluronate: $Cd^{2+}$ > $Cu^{2+}$ > $Pb^{2+}$ > $Fe^{3+}$ >> $Ca^{2+}$ > $Sr^{2+}$, $Zn^{2+}$, $Co^{2+}$ >> $Mn^{2+}$ > $Cr^{6+}$ >> $Hg^{2+}$, $Mg^{2+}$, $Rb^+$, and 3) polymannuronate: $Cd^{2+}$, $Cu^{2+}$ > $Fe^{3+}$ > $Pb^{2+}$ > $Ca^{2+}$ > $Zn^{2+}$ > $Sr^{2+}$ > $Co^{2+}$ > $Cr^{6+}$ >> $Mn^{2+}$ >> $Hg^{2+}$, $Mg^{2+}$, $Rb^+$. Amounts of the metal ions, $Cd^{2+}$, $Cu^{2+}$, $Fe^{3+}$, $Pb^{2+}$, and $Zn^{2+}$, bound to 1 g of seaweed alginate, were measured as $363.5{\pm}45.0$, $226.3{\pm}9.2$, $1,299.4{\pm}$81.3, 500.7${\pm}$27.7, and 165.9${\pm}$11.4 mg, respectively. Amounts of the metal ions, $Cd^{2+}$, $Cu^{2+}$, $Fe^{3+}$, $Pb^{2+}$, and $Zn^{2+}$, bound to 1g of polyguluronate, were 354.5${\pm}$26.5, 177.6${\pm}$8.7, 1,288.6${\pm}$60.1, 424.0${\pm}$7.4, and 140.2${\pm}$28.5 mg, respectively, whereas those bound to 1 g of polymannuronate were 329.0${\pm}$10.3, 206.9${\pm}$1.9, 1,635.6${\pm}$11.1, 419.8${\pm}$12.6, and 251.0${\pm}$49.1 mg, respectively. Due to its higher solubility than alginate and higher affinity for metal ions than polyguluronate, polymannuronate can be used for bioremediation or biosorption of toxic and/or noble metal ions.

Calculation of Thickness and Composition Profiles of Sputtered TbFe Thin Films (TbFe 스퍼터박막의 두께 및 조성분포 계산)

  • 박종철;김순광
    • Electrical & Electronic Materials
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    • v.3 no.2
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    • pp.131-137
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    • 1990
  • 스퍼터링시 타겟에서 튀어나오는 원자의 방출각도분포를 새로운 함수로 표현하고 이를 이용하여 박막의 두께와 조성분초를 예측하는 방법을 구하였다. 2원계 RbFe박막의 복합타겟 마그네트론 스퍼터에 의해 제작된 박막의 조성 및 두께해석에 본 모델을 적용한 결과, 스퍼터시 Tb는 overcosine, Fe는 undercosine 방출분포를 갖는다는 것이 밝혀졌으며 이를 이용하여 실용디스크의 대면적균일화 방안의 도출기반을 마련하게 되었다.

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Sulfur Dioxide, Mineral Contents and Physicochemical Properties Generated during Manufacture of Bamboo Salt (죽염 제조공정에 따른 이산화황, 미네랄 함량 및 이화학적 특성)

  • Kim, Hag-Lyeol;Lee, Seong-Jae;Lee, Jung-Hee;Kim, In-Cheol
    • Journal of the Korean Society of Food Science and Nutrition
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    • v.43 no.8
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    • pp.1248-1256
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    • 2014
  • The purpose of this study was to investigate the mechanisms of behind $SO_2$ formation and elevated cause of reducing power in purple bamboo salt (PBS) along with an analysis of physicochemical properties, content of sulfur compounds, oxidation reduction potential (ORP), mineral contents of salt type (MSS, mudflat solar salt; BS, bamboo salt), and addition of raw bamboo (RB). $SO_2$ content of 630 ppm was detected in PBS. $SO_2$ was not detected in MSS, BS, or RB, whereas $SO_2$ (782 ppm) from $K_2SO_4$ was detected after heating a NaCl, KCl, $MgCl_2$, $MgSO_4$, MgO, $CaCl_2$, $K_2SO_4$, and $FeSO_4$ with RB. $SO_2$ content of BS increased with baking time, and it originated from BSRB1 (13.88 ppm) to BSRB4 (109.13 ppm). $SO_3{^{2-}}$ originated only from MSSRB4 and BSRB2~BSRB4. Sulfate ion content decreased along with increasing $SO_2$ and sulfite ion contents. ORP increased with baking time of MSS and BS, and it was present at higher levels in BSRB4 (-211.40 mV) of BS than MSS. Insoluble content was higher in BS than MSS. Further, Ca, K, and Mg ion contents decreased in MSS and increased in BS with baking time. BSRB4 had 1.4 fold higher levels of Ca, 1.5 fold higher levels of Mg, and 1.8 fold higher levels of K than BS. Li, Al, Mn, Fe, and Sr in MSS as well as Al, Fe, and Ni in BS increased with baking time. Anions (Cl, $NO_3$, and Br) and heavy metals (Pb, Cd, Hg, and As) between MSS and BS were not significantly different. These results suggest that the reducing power of BS was due to $SO_2$ and sulfite ion. To increase the amounts of these compounds and reducing power, higher melting temperature and longer baking time are necessary along with BS, which is created by the addition of RB to roasted salt.