• Title/Summary/Keyword: $Na_2SeO_3$

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Potential Element Retention by Weathered Pulverised Fuel Ash : II. Column Leaching Experiments (풍화 석탄연소 고형폐기물(Pulverised Fuel Ash)의 중금속 제거가능성 : II. 주상용출실험)

  • Lee, Sanghoon
    • Economic and Environmental Geology
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    • v.28 no.3
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    • pp.259-269
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    • 1995
  • Column leaching tests were conducted using fresh and weathered pulverised fuel ash of some 17 and 40 years old from two major British power plants, with deionised water and simulated synthetic industrial leachate. The former was to see the leaching behaviour of weathered ash and the latter was to see if the formation of secondary products from water and PFA interaction and ameliorating effect in removing metals from industrial leachates. Fresh PFA liberates elevated concentrations of surface-enriched inorganics, including Ca, Na, K, B, $Cr_{total}$, Li Mo, Se and $SO^{2-}_4$. This might indicate their association with the surface of PFA particles. In the column leaching tests using weathered ash and deionised water, elements are not readily leached but are released more slowly, showing relatively constant concentrations. For the case of weathered ash, some readily soluble surface-enriched elements appears to have been liberated in their early stage of leaching and the liberation of glass associated elements are thought to be more important function in controlling the element concentration. The result from column leaching tests exceed for a number of elements when compared with various Water Standards and suggests the leachate from PFA disposal mound needs dilution to achieve target concentrations. PF A shows element retention effect for many elements, including B, Fe, Zn, Hg, Ni, Li and Mo, in the order of fresh Drax ash > weathered Drax ash > Weathered Meaford ash in retaining capacity. Geochemical modelling using a computer program WATEQ4F reveals some solubility controlling secondary solid products. These include $CaSO_4{\cdot}2H_2O$ for Ca, $Al(OH)_3$ for Al and $Fe(OH)_3$ for Fe.

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Reduction and Equilibrium of Vanadium-Diethylenetriamine Pentaacetates at Mercury Electrode in Aqueous Solution (수용액중의 수은전극에서 바나듐-디에틸렌트리아민 펜타아세트산염의 환원 및 평형연구)

  • Ki-Suk Jung;Se Chul Sohn;Young Kyung Ha;Tae Yoon Eom;Sock Sung Yun
    • Journal of the Korean Chemical Society
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    • v.33 no.1
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    • pp.55-64
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    • 1989
  • Reduction and equilibrium of vanadium-DTPA (DTPA = diethylenetriaminepentaacetic acid, $H_5A$) complexes at mercury electrodes are studied in 0.5M $NaClO_4$ aqueous solution at 3.2 < pH < 10.5 and 25$^{\circ}$C. At 3.2 < pH < 5.9, the reduction reaction is $V{\cdot}A^{2-}+H^-+e^-=V{\cdot}HA^{2-}$, while at 5.9 < pH < 10.5 it is $V{\cdot}A^{2-}+H^-+e^-=V{\cdot}A^{3-}$. The stability constants of $V{\cdot}HA^{2-}$ and $V{\cdot}A^{3-}$ are found to be $6.46{\times}10^{9}$ and $3.09{\times}10^{14}$, respectively. V(IV)-DTPA undergoes stepwise complexation as $VO^{2+}+H_2A^{3-}=VO{\cdot}HA^{2+}H^{+}$ and $VO{\cdot}HA^{2-}=VO{\cdot}A^{3+}+H$, where acidity constant of $VO{\cdot}HA^{2-}$- is pKa = 7.15. Stability constants of $VO{\cdot}HA^{2-}$ and $VO{\cdot}A^{3-}$ are found to be $1.41{\times}10^{14}$ and $3.80{\times}10^{17}$, respectively. It is detected that $VO^{2+}-DATA$ is reduced irreversibly to $VO^{2-}$ with the transfer coefficient of $\alpha$ = 0.43. At more cathodic overpotential, the reduction is stepwise as V(IV)${\to}$V(III)${\to}$V(II). The first one corresponds to $VO{\cdot}HA^{2-}+e^{-}{\to}VO{\cdot}HA{3+}$ at 3.2 < pH < 7.2 and $VO{\cdot}A^{3-}+e^{-}{\to}VO{\cdot}A^{4-}$ at 7.2 < pH < 10.5. The second is identical to that of V(III). Diffusion coefficients of $VO{\cdot}HA^{2-}$ and $VO{\cdot}A^{3-}$ are found to be $(9.0{\pm}0.3){\times}10^{-6}cm^2/s$ and $(5.9{\pm}0.4){\times}10^{-6}cm^2/ses$, respectively.

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Characteristics of South Korea's Geothermal Water in Relation to Its Geological and Geochemical Feature

  • Lee, Chung-Mo;Hamm, Se-Yeong;Lee, Cholwoo;Choi, Sung-Ja;Chung, Sang Yong
    • Journal of Soil and Groundwater Environment
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    • v.19 no.2
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    • pp.25-37
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    • 2014
  • The volcanic type of geothermal water is linked intimately to active or potentially active volcanoes and takes place near the plate boundaries. In contrast to the volcanic type, the geothermal water in Korea has a non-volcanic origin. Korea's geothermal water is classified into the residual magma (RM) type and deep groundwater (DG) type according to the criterion of $35^{\circ}C$. This study reviewed the relationship between the physical and chemical features of the 281 geothermal water sources in South Korea in terms of the specific capacity, water temperature, and chemical compositions of two different basements (igneous rock and metamorphic rock) as well as the geological structures. According to the spatial relationship between the geothermal holes and geological faults, the length of the major fault is considered a key parameter determining the movement to a deeper place and the temperature of geothermal water. A negligible relationship between the specific capacity (Q/s) and temperature was found for both the RM type and DG type with the greater specific capacities of the RM- and DG-igneous types than the RM- and DG-metamorphic types. No relationship was observed between Q/s and the chemical constituents ($K^+$, $Na^+$, $Ca^{2+}$, $Mg^{2+}$, $Zn^{2+}$, $Cl^-$, $SO_4{^{2-}}$, $HCO_3{^-}$, and $SiO_2$) in the DG-igneous and DG-metamorphic types. Furthermore, weak relationship between temperature and chemical constituents was found for both the RM type and DG type.

Fabrication and characteristics of micro-machined thermoelectric flow sensor (실리콘 미세 가공을 이용한 열전형 미소유량센서 제작 및 특성)

  • Lee, Young-Hwa;Roh, Sung-Cheoul;Na, Pil-Sun;Kim, Kook-Jin;Lee, Kwang-Chul;Choi, Yong-Moon;Park, Se-Il;Ihm, Young-Eon
    • Journal of Sensor Science and Technology
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    • v.14 no.1
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    • pp.22-27
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    • 2005
  • A thermoelectric flow sensor for small quantity of gas flow rate was fabricated using silicon wafer semiconductor process and bulk micromachining technology. Evanohm R alloy heater and chromel-constantan thermocouples were used as a generation heat unit and sensing parts, respectively. The heater and thermocouples are thermally isolated on the $Si_{3}N_{4}/SiO_{2}/Si_{3}N_{4}$ laminated membrane. The characteristics of this sensor were observed in the flow rate range from 0.2 slm to 1.0 slm and the heater power from 0.72 mW to 5.63 mW. The results showed that the sensitivities $(({\partial}({\Delta}V)/{\partial}(\dot{q}));{\;}{\Delta}V$ : voltage difference, $\dot{q}$ : flow rate) were increased in accordance with heater power rise and decreasing of flow rate.

Evaluation of Glucosinolate Content and Composition Contained in Korean Leaf Mustard (Brassica juncea var. integrifolia) Germplasm Using Liquid Chromatography Electrospray Ionization Mass Spectrometry(LC-ESI-MS/MS)

  • Kim, Jung-Bong;Kim, Heon-Woong;Ko, Ho-Cheol;Kim, So-Young;Kim, Se-Na;Jin, Yong-Xie;Kim, Jae-Hyun
    • Proceedings of the Plant Resources Society of Korea Conference
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    • 2010.05a
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    • pp.18-18
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    • 2010
  • Glucosinolates(GSLs) are major secondary products($\beta$-thioglucoside N-hydroxysulfates) containing sulfates that are found mainly in Cruciferae family such as cabbage, broccoli, radish, turnip, kale, mustard and rapeseed as the important crops in agronomic and economic aspects. Especially, isothiocyanates(ITCs) have been shown to inhibit carcinogenesis with regulation cancer cell development followed by regulating target enzymes, inducing cell cycle arrest and apoptosis against various human cancer cell lines. Total desulfo(DS)-GSLs of nine type in 210 Korean leaf mustard accessions were isolated and confirmed using electrospray ionization mass spectrometric(ESI-MS/MS) method and DS-GSLs powerful library maked from several reference data. The isolated individual DS-GSLs were identified by removed $\beta$-D-glucopyranose residue ($C_6H_{11}O_5$, MW 163) from MS/MS data. Among them sinigrin(41.7%), glucoiberverin(21.7%) and gluconasturtiin(12.6%) were major components, Especially, despite gluconapin was minor component, accession K046197-1 and K046197-2 showed higher content of 4.11 and 3.31 mg/g(DW), respectively. The total GSLs contents in 210 accessions were ranged from 5.3 to 23.2 mg/g(DW) with a mean value of 13.0 mg/g(DW). As a result of principal component analysis(PCA), the individual GSLs loading plots were composed of three groups and components belonged to each group showed correlationship in quantitative pattern.

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Effects of Dietary Organic Selenium and Vitamin E on Growth Performance, Selenium Retention and Quality of Meat in Broiler Chickens (유기태 셀레늄과 Vitamin E의 복합 급여가 육계의 생산성, 계육 품질 및 Selenium 축적에 미치는 영향)

  • Na, J.C.;Kim, J.H.;Yu, D.J.;Jang, B.G.;Kang, G.H.;Kim, S.H.;Suh, O.S.;Lee, W.J.;Lee, J.C.
    • Korean Journal of Poultry Science
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    • v.34 no.2
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    • pp.143-149
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    • 2007
  • The experiment was conducted to examine the effects of dietary organic selenium and vitamin E on weight gain, feed intake, feed conversion, and selenium retention in meat of broiler chickens. For each growth phase, the basal diet was supplemented with 0 (control), vitamin E 150 IU/kg and the combination of 1.2 ppm Se from selenium yeast (SY) and vitamin E 100, 150, 200 and 300 IU/kg. Weight gain was significantly higher in supplemental control and vitamin E 150 compared to the combination of 1.2 ppm SY and vitamin E 150 IU during day 1 to 21. Feed intake significantly(P<0.05) increased in supplemental vitamin E 150 compared to the combination of 1.2 ppm SY and vitamin E 150 and 200 IU during day 1 to 21. Feed intake was significantly(P<0.05) higher in control compared to that of combination of 1.2 ppm SY and vitamin E 200 IU during day 21 to 35. However feed conversion was not affected in supplemental vitamin E and SY during day 1 to 35. Selenium concentrations of breast muscle and liver tissue significantly increased (P<0.05) in supplemental combination of 1.2 ppm SY and vitamin E compared to the control and vitamin E 150 IU. TBARS of control and vitamin E 150 IU were significantly (P<0.05) higher in day 3 than day 1, but the combination of Se 1.2 ppm and vitamin E of TBARS had no difference during day 1 to 3. TBARS in day 3 was significantly (P<0.05) lower in supplemental combination of Se 1.2 ppm and vitamin E than control and vitamin E 150 IU.

Comparison between Lucigenin- and Luminol-dependent Chemiluminescence Responses of Rockfish (Sebastes schlegeli) Head Kidney Phagocytes

  • Jung Jae Hyuck;Kwon Se Ryun;Lee Eun Hye;Kim Sung Mi;Jeong Hyun Do;Chung Joon Ki;Kim Ki Hong
    • Fisheries and Aquatic Sciences
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    • v.6 no.4
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    • pp.209-212
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    • 2003
  • Lucigenin (Lg)- and luminol (Lm)-dependent chemiluminescence (CL) was used to compare the respiratory burst of rockfish (Sebastes schlegeli) phagocytes after stimulation with phorbol myristate acetate (PMA). To establish which reactive oxygen species (ROS) contributes to the observed CL, the modulators of ROS metabolism, such as superoxide dismutase (SOD), catalase, and sodium azide $(NaN_3)$ were used. Although LgCL responses were inhibited significantly by the addition of either SOD or catalase, in comparison to the control, significantly lower LgCL responses were recorded by SOD than catalase. LmCL also showed significantly decreased responses by the addition of SOD and catalase. However, there were no statistical differences in CL responses between SOD and catalase additions. More profound and significant decrease of LmCL responses were recorded by simultaneous addition of SOD and catalase. Sodium azide markedly enhanced LgCL responses, while it significantly inhibited LmCL responses. These results indicate that LgCL and LmCL can be used to measure extracellular $O_2$ production and myeloperoxidase (MPO)-mediated ROS production in fish phagocytes, respectively. Furthermore, LmCL can be used for analyzing intracellular ROS production by simultaneous addition of both SOD and catalase.

Flora changes on Pasture in forest composition and analysis of Useful Plant Resources (임간초지 조성에 관한 식물상 변화와 자원식물의 유용도 분석)

  • Han, Gyu-Il;Kim, Se-Chang;Son, Yong-Hwan;Park, Seong-Ho;Seo, Han-Na;Park, Wan-Geun
    • Proceedings of the Plant Resources Society of Korea Conference
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    • 2019.04a
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    • pp.60-60
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    • 2019
  • 지속가능한 개발이 주목받고 남북 평화의 시대를 맞이하여 임업분야와 농업 축산분야가 결합된 혼농임업(Agroforestry)이 주목받고 있다. 혼농임업(Agroforestry)은 식량, 과실, 풀사료, 땔감, 목재 등을 생산하고 토양보전을 실천하여 지속농업을 가능케 하는 복합영농의 한 형태이며, 북한 산지의 경우 황폐화된 산지가 많아 경제성과 산림녹화를 동시에 해결할 수 있어 많은 관심을 받고 있다. 본 연구는 강원도 하늘목장을 시범목장으로 선정하여 조사를 실시하였고, 연구조사지의 총 면적은 2.4ha로 백두대간과 오대산국립공원이 인접한 지역으로 다양한 식물상을 파악할 수 있는 지역이다. 그러므로 외래종침입에 따른 생태적 교란을 방지하기 위하여 완충지대를 설정하고 식물상 조사를 실시하였다. 그리고 조사지내의 대표 수종으로 선정된 모수만 남기고 벌채를 실시하여 변화양상을 모니터링 하였다. 2014년~2017년 총 3개년 계절별 조사를 통해 임간초지의 식물상 정보를 파악하였고 임간초지의 관속식물상을 조사한 결과 92과 250속 323종 4아종 43변종 6품종으로 총 376분류군이 조사되었다. 자원식물의 유용도 분석한 결과 식용자원(E)이 160분류군으로 가장 많은 비율을 차지하고 있었으며, 약용(M) 141분류군, 관상용(O) 45분류군으로 나타났으며, 용도미상(U) 식물도 73분류군이 분포하고 있는 것으로 나타났다. 또한 연구 대상지역의 특성을 고려하여 조성된 초지 내에서 조사료로 사용할 수 있는 식물 종을 파악하였다. 나아가 미비한 임간초지 식생의 DB를 구축하고, 지속가능한 녹색성장을 모색하여야 할 것이다.

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Petrochemistry and Geologic Structure of Icheon Granitic Gneiss around Samcheog Area, Korea (삼척지역 이천화강편마암의 암석화학과 지질구조)

  • Cheong Won-Seok;Cheong Sang-Won;Na Ki-Chang
    • The Journal of the Petrological Society of Korea
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    • v.15 no.1 s.43
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    • pp.25-38
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    • 2006
  • Metamophic rocks of Samcheog area, northeastern Yeongnam massif, was studied petrochemically. This area includes Precambrian Hosanri Formation (schists and gneisses) and granitoid (Icheon granitic gneiss, leucocratic granite and Hongjesa granite), Cambrian sedimentary rocks, and Cretaceous sedimentary and acidic volcanic rocks. Hosanri formation is composed of quartz+plagioclase+K-feldspar+biotite+muscovite+granet${\pm}$cordierite${\pm}$sillimanite. Mineral assemblage of biotite granitic gneiss, which is massive granodioritic rock with weak foliation, is similar to Hosanri formation. According to mineral assemblages, metamorphic rocks of studied area can be divided into two metamorphic zones (garnet and sillimanite zones). From Icheonri area, major, trace and rare earth element data of biotite granitic gneiss and luecocratic granite suggest that source rock is politic rocks of Hosanri formation and source magma was formed by anatexis and experienced fractionation of plagioclase. Trace element diagram show collisional environment such as syn-collisional, volcanic arc granite. Orientation of faults in study area have three maximum concentrations, $N54^{\circ}\;W/77^{\circ}\;SW,\;N49^{\circ}\;W/81^{\circ}\;NE\;and\;N10^{\circ}\;W/38^{\circ}\;NE$. Structure analysis suggests that faults in study area ware formed by uplift and compression. Faulting age is guessed after Tertiary because some shear joints is developed in dikes to intrusive Cretaceous acidic volcanic rock. Hosanri formation and Icheon granitic gneiss had experienced similar deformation history because they have maximum concentration to foliations, $N89^{\circ}\;E/55^{\circ}\;SE\;and\;N80^{\circ}\;E/45^{\circ}\;SE$, respectively.

Geochemical Studies on Au-Ag Hydrothermal Vein Deposits, Republic of Korea : Goryeong-Waegwan Mineralized Area (한반도(韓半島) 금(金)-은(銀) 열수(熱水) 광상(鑛床)의 지화학적(地化學的) 연구(硏究) : 고령(高靈)-왜관지역(倭館地域) 광화대(鑛化帶))

  • So, Chil-Sup;Choi, Sang-Hoon;Chi, Se-Jung;Choi, Seon-Gyu;Shelton, Kevin L.
    • Economic and Environmental Geology
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    • v.22 no.3
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    • pp.221-235
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    • 1989
  • Gold-silver mineralization of the Goryeong-Waegwan area was deposited in three stages of quartz and calcite veins which fill fissures in Cretaceous sedimentary rocks of the Sindong Group. Radiometric dating indicates that mineralization is Late Cretaceous age(98 Ma) likely associated genetically with intrusion of a small biotite granite stock. Fluid inclusion and stable isotope data indicate that Au-Ag ore was deposited at temperatures between $280^{\circ}C$ and $230^{\circ}C$ from fluids with salinities between 1.7 and 8.7 equiv.wt.% NaCl. Evidence of boiling indicates pressures of <100 bars, corresponding to depths of 425 and 1,150m, respectively, assuming lithostatic and hydrostatic loads. Within ore stage I there is an apparent decrease in ${\delta}^{34}S$ values of $H_2S$ with paragenetic time, from +1.4 to -2.5 per mil. This pattern was likely achieved through progressive increases in pH and activity of oxygen accompanying boiling. Measured and calculated hydrogen and oxygen isotope values of ore-forming fluids(${\delta}D$ = -90 to -100 per mil; ${\delta}^{18}O$ = +3.9 to -11.4 per mil) indicate meteoric water dominance, approaching unex-changed meteoric water values. Au-Ag deposition is thought to be the result of cooling and dilution of a boiling fluid through mixing with less evolved meteoric waters.

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