• 자원환경지질
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• 제32권6호
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• pp.611-631
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• 1999

Enviromental geochemisty and heary metal contamination at the Kongjueil mine creek were underaken on the basis of physicohemical properties and mineralogy for various kinds of water (surface, mine and ground water),soil, precipitate and sediment collected of April and December in 1998. Hydrgeochemical composition of the water samples are characterized by relatively significant enricant of Ca+Na, alkiali ions $NO_3$ and Cl inground and surfore water, wheras the mine waters are relatively eneripheral water of the mining creek have the characteristics of the (Ca+Mg)-$(HCO_3+SO_4)$type. The pH of the mine water is high acidity (3.24)and high EC (613$\mu$S/cm)compared with those of surface and ground water. The range of $\delta$D and $\delta^{18}O$ values (relative to SMOW) in the waters are shpwn in -50.2 to -61.6% and -7.0 to -8.6$\textperthousand$(d value=5.8 to 8.7). Using computer program, saturation index of albite, calcite, dolomite in mine water are nearly saturated. The gibbiste, kaolinite and smectite are superaturated in the surface and ground water, respectively. Calculated water-mineral reaction and stabilities suggest that weathing of silicate minerals may be stable kaolinite owing to the continuous water-rock reaction. Geochemical modeling showed that mostly toxic heavy metals may exist larfely in the from of metal-sulfate $(MSO_4\;^2)$and free metal $(M^{2+})$ in nmine water. These metals in the ground and surface water could be formed of $CO_3$ and OH complex ions. The average enrichment indices of water samples are 2.72 of the groundwater, 2.26 of the surface water and 14.15 of the acid mine water, normalizing by surface water composition at the non-mining creek, repectively. Characteristics of some major, minor and rate earth elements (Al/Na, K/Na, V/Ni, Cr/V, Ni/Co, La/Ce, Th/Yb, $La_N/Yb_N$, Co/Th, La/Sc and Sc/Th) in soil and sediment are revealed a narrow range and homogeneous compositions may be explained by acidic to intermediate igneous rocks. And these suggested that sediment source of host granitic gneiss colud be due to rocks of high grade metamorphism originated by sedimentary rocks. Maximum concentrations of environmentally toxic elements in sediment and soil are Fe=53.80 wt.% As=660, Cd=4, Cr=175, Cu=158, Mn=1010, Pb=2933, Sb=4 and Zn=3740 ppm, and extremely high concentrations are found are found in the subsurface soil near the ore dump and precipitates. Normalizing by composition of host granitic gneiss, the average enerichment indices are 3.72 of the sediments, 3.48 of the soils, 10.40 of the precipitates of acid mine drainage and 6.25 of the soils near the main adit. The level of enerichment was very severe in mining drainage sediments, while it was not so great in the soils. mineral composition of soil and sediment near the mining area were partly variable being composed of quartz, mica, feldspar, chlorite, vermiculite, bethierin and clay minerals. reddish variable being composed of quartz, mica, feldspar, chlorite, vermiculite, bethierin and clay minerals. Reddish brown precipitation mineral in the acid mine drainage identifies by schwertmanite. From the separated mineralgy, soil and sediment are composed of some pyrite, arsenopyite, chalcopyrite, sphalerite, galena, malachite, goethite and various kinds of hydroxied minerals.

• 한국환경농학회지
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• 제23권2호
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• pp.92-98
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• 2004

본 연구에서는 생물흡착제인 미역을 사용하여 인공폐액내의 중금속의 흡착 특성을 조사하였으며, 다음과 같은 결론을 얻었다. 미역 폐기물을 이용하여 제조된 생물흡착제의 단일 중금속 흡착효율은 각 중금속 100 mg/L인 용액에 biosorbent 3g을 처리했을 때 Pb는 거의 100%였고, Cu와 Cd가 약 $85{\sim}86%$, Zn과 Cr은 약 $60{\sim}64%$, Co와 Ni은 약 57%, Mn은 약 48%였다. 복합중금속 흡착효율은 단일중금속 흡착효율에 비하여 Pb를 제외한 다른 중금속들은 크게 감소되었으나 biosorbent g당 전체 중금속 흡착량은 더 증가되었다. 온도, pH에 따른 중금속 흡착효율은 별 차이가 없었으며 전반적으로 pH는 pH $5{\sim}6$ 범위, 온도는 $20{\sim}30^{\circ}C$ 범위의 실온이 적당한 것으로 나타났다. 생물흡착제의 흡착평형은 모든 중금속이 1시간 이내에 이루어졌다. Freundlich과 Langmuir 등온흡착식을 구하여 실제폐수처리에 적용여부를 검토한 결과 Pb, Cu, Cr, Cd, Co 순으로 비교적 친화도가 큰 것으로 나타났고, Freundlich 등온 흡착식에 가장 잘 일치하였다. 모든 중금속의 Freundlich 지수 1/n값이 $0.1{\sim}0.5$ 범위에 포함되어 흡착이 용이하고, Pb, Cr, Cu, Cd 순으로 비교적 평형 흡착량이 큰 것으로 나타났으며, 이 결과는 Langmuir 흡착등온식의 결과와 거의 유사하였다. 따라서, 중금속 농도범위에 따른 한계범위를 설정하여 등온흡착식을 적용시키면 매우 높은 중금속 처리효율을 나타낼 것으로 판단된다. 생물흡착제가 중금속 흡착 후의 구조적인 특성을 조사하기 위하여 FT-IR분석 결과, 중금속 이온과 치환될 것으로 생각되는 functional group을 확인할 수 있었으며, 3,400/cm에서의 -OH group, 1,648/cm에서의 C=O bond,1,426/cm에서의 C-O bond그리고 850/cm에서의 S=O등이 전반적으로 중금속 흡착 후에 peak가 커지는 것이 관찰되었다. 생물흡착제의 재사용 가능성을 검토하기 위하여 최적의 중금속 탈착조건 검토하였는데, 탈착제 종류에 따른 중금속 탈착효율은 탈착제 종류와 중금속 종류에 따라 차이가 있었고, 전반적으로 NTA>$H_2SO_4$>HCl>EDTA 순으로 우수하였으며, 전체적으로 특정 중금속의 탈착효율이 떨어지지 않는 NTA가 탈착제로 가장 적합하였다. NTA농도에 따른 중금속 탈착효율은 NTA $0.1{\sim}0.3%$ 농도범위에서는 농도 증가에 따라 탈착 효율도 약간 증가되었으나 그 이상의 농도에서는 별 차이 없었다. 온도와 pH 변화에 따른 중금속 탈착효율은 Cr을 제외한 다른 중금속들은 크게 영향을 받지 않는 것으로 나타났으며 전반적으로 온도는 $30^{\circ}C$, pH는 2에서 높았다. 탈착제 접촉 반응시간에 따른 탈착효율은 10분 이내에 전체 탈착량의 80%이상이 탈착 되었으며 1시간 이후에는 거의 변화가 없었다.

• 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 $220{\pm}10^{\circ}C$.

• 자원환경지질
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• 제28권3호
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• pp.259-269
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• 1995

석탄연소 폐기물 (Pulverised Fuel Ash: PFA)을 17년, 40년 매립 풍화받은 것 그리고 현재 발생하는 신선한 시료등으로 구분 영국내 2개 화력발전소로부터 각각 채취하여 주상용출시험 (Column leaching test)을 실시하였다. 용매는 증류수와 인공합성 침출수의 2가지를 이용하였다. 전자의 경우 풍화 시료의 용출행태를 주로 알아보고자 하였으며 후자의 경우 PFA시료와 용매간의 반응중에 발생하는 2차 물질형성이 폐수처리중 중금속제거에 활용가능성이 있는가를 알아보자고 함이었다. 신선한 시료로부터 매우 높은 함량의 원소방출이 관찰된다. 이는 Ca, Na, K, B, Cr, Li, Mo, Se, 그리고 $SO^{2-}_4$등을 포함한다. 이는 원소들의 분포위치에 관한 정보를 제공하며 이들원소의 입자 표면 수반을 시사한다. 풍화 받은 시료로부터 채취된 용액시료에서는 신선한 시료와는 달리 원소들의 급격한 초기방출은 관찰되지 않으며 비교적 일정함량을 보이며 매우 완만한 농도감소 현상을 보인다. 이는 17년과 40년이라는 매립기간중 표면의 용융성원소들의 방출을 의미하며 입자를 주로 구성하는 유리질물질에 수반되는 부분이 이들 시료에서의 원소방출에 중요한 역할을 하는 것으로 생각된다. 증류수를 이용한 실험결과를 여러가지 침출수배출기준, 음용수기준치 등과 비교시 PFA는 이들 기준에 초과하는 농도를 나타내는바 침출수배출시에는 희석 등의 처리가 필요할 것으로 생각되며 매립시 침출수가 지하수로 유입되지 않도록 하여야할 것으로 보인다. 인공 침출수가 PFA기둥을 통과하며 많은 중금속 - B, Fe, Zn, Hg, Ni, Li, Mo -등이 침출수로부터 제거되며 이 제거정도는 신선한 Drax > 풍화 Drax > 풍화 Meaford 시료의 순이다. 물분석시료를 지구화학 모델링 프로그램인 WATEQ4F를 이용하여 PFA 침출수내의 농도조정물질의 존재여부를 알아본 결과 Ca의 경우 $CaSO_4{\cdot}2H_2O$, Al의 경우 $Al(OH)_3$, Fe는 $Fe(OH)_3$ 등이 PFA침출수내에 각 해당원소의 농도를 제한하는 2차물질로 판단되었다.

• Natural Product Sciences
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• 제26권3호
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• pp.207-213
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• 2020

Characterization and in vitro inhibition studies of protease inhibitor from the mushroom Pleurotus floridanus (PfTI) towards the pest Papilio demoleus is studied. The addition of 1 mM Mn²⁺, Na²⁺, Ba²⁺ and Ni ²⁺ enhanced the PfTI activity. The ICP-atomic emission spectrum showed the presence of Ca²⁺, Mg²⁺ and Zn²⁺ in the PfTI. Surfactants SDS and CTAB at a concentration of 1% reduced the PfTI activity whereas, the nonionic detergents Triton X and Tween 80 increased the activity. The inhibitory activity gradually decreased with increase in concentration of DMSO and H₂O₂. The activity was increased by dithiothreitol up to a concentration of 80 μM and inactivated at 140 μM. The activity of PMSF modified PfTI was drastically reduced to 0.234 U/mL at 4 mM concentration and similar results were obtained for modification of cysteine by N-Ethylmaleimide at slightly higher concentrations. The complex of trypsin and PfTI showed complete loss in fluorescence intensity at 343 nm compared with control. In vitro inhibition studies of PfTI with midgut proteases isolated from citrus pest P. demoleus with protease activity of 1.236 U was decreased to 0.613 U by 50 μL (0.1 mg/mL) of the inhibitor. Inhibitor was stable up to 0.04 M concentration of HCl.

• 한국물환경학회지
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• 제37권4호
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• pp.306-314
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• 2021

The application of organic fertilizer could be accompanied by potential hazards to soil and humans due to trace metals. Livestock manure compost·liquefied fertilizer is a well-established approach for the stabilization of nutrients and the reduction of pathogens and odors in manures, which can be evaluated as compost·liquefied. In this study, the livestock manure compost·liquefied fertilizers produced at 333 liquid manure public resource centers and liquid fertilizer distribution centers were collected from May to December 2019. The nutrient content (nitrogen, phosphorus, and potassium), physicochemical properties, and heavy metal content were investigated. The livestock manure compost·liquefied fertilizer was measured using a mechanical maturity measurement device. The organic matter, arsenic, cadmium, mercury, lead, chromium, copper, nickel, zinc, E. coli (O157:H7), Salmonella, etc. of the livestock manure compost·liquefied fertilizers were analyzed. The average heavy metal content in the livestock manure compost·liquefied fertilizer was as follows: Cr 2.9 mg/kg (0.2~8.7 mg/kg), Cu 20.4 mg/kg (1.6~74.1 mg/kg), Ni 1.3 mg/kg (0.4~4.2 mg/kg), and Zn 79.8 mg/kg (3.0~340.7 mg/kg). Although large-scale organic fertilizer plants and resources recycling centers produce good organic (liquid) fertilizers with proper components, it is necessary to standardize livestock manure compost·liquefied fertilizer in order to facilitate efforts to turn livestock manure into useful resources.

• 한국식품과학회지
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• 제46권1호
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• pp.108-114
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• 2014

오이와 고추의 안전성에 영향을 미치는 위해요소 분석의 기초자료로 활용하기 위해 오이와 고추 재배지에서 총 72점의 시료를 채취하여 미생물학적(위생지표세균, 병원성미생물, 곰팡이) 위해요소와 화학적(중금속, 잔류농약) 위해요소를 조사하였다. 미생물학적 위해요소 중 위생지표세균과 곰팡이는 오이 재배지에서 ND-7.2와 ND-4.8 log CFU/g (g, mL, hand, or $100cm^2$) 범위로 검출되었고, 고추 재배지에서는 ND-6.8와 0.4-5.3 log CFU/g (g, mL, hand, or $100cm^2$) 범위로 검출되었다. 특히 대장균군은 고추재배지의 토양에서 최대 5.6 log CFU/g까지 검출되었다. 병원성 미생물은 S. aureus는 오이 농장의 장갑에서만 1.4 log CFU/$100cm^2$으로 검출되었고, B. cereus는 대부분의 시료에서 ND-4.8 log CFU/g (g, mL, hand, or $100cm^2$) 범위로 검출되었다. L. monocytogenes, E. coli O157:H7 및 Salmonella spp.는 검출되지 않았다. 화학적 위해요소에 해당하는 중금속은 Zn, Cu, Ni, Pb 및 Hg이 국내 허용기준치 이하로 검출되었고, 잔류농약의 경우 오이에서는 모든 성분이 불검출 되었으나 고추에서 hexaconazole 성분이 0.016 mg/kg (기준치: 0.3 mg/kg)으로 검출되었다.

• 한국수산과학회지
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• 제39권2호
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• pp.106-117
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• 2006

We measured the concentrations of organic matter and metallic elements (Al, Fe, Cr, Mn, Ni, Cu, Zn, As, Cd, Pb and Hg) in the surface sediments of Masan Harbor (in the southern sea, Korea) to evaluate the geochemical characters of sediment and the pollutions by organic matter and metallic elements. The mean grain size of the surface sediments in the study area ranged from $5.6{\phi}$ to $7.8{\phi}$, indicating silt sediment. The water content of the surface sediments exceeded 60% except at some stations. The contents of ignition loss (IL), total organic carbon (TOC) and total nitrogen (TN) ranged from 7.2-14.3%, 1.2-3.2%, and 0.10-0.28%, respectively. Based on the C/N ratios, the organic matter in the surface sediments of Masan Harbor may originate from terrigenous sources including fluvial inputs (mainly sewage in urban areas). The chemical oxygen demand (COD) and acid volatile sulfide (AVS) ranged from $11.3-29.9\;mgO_2/g\;dry$ and 0.20-4.47 mgS/g dry, respectively, and low concentrations were observed near a shipping route. In addition, the concentrations of metallic elements showed large spatial variations in Masan Harbor and the distributions of metallic elements were also comparable to those of organic matter. This implies that the distributions of organic matter and metallic elements in the surface sediments of Masan Harbor are mainly controlled by biogenic matter and artificial action (mainly dredging). In addition, we calculated the enrichment facto. (EF) and geoaccumulation index (Igeo) in order to evaluate pollution by metallic elements. The enrichment of metallic elements relative to Al was three to eighteen times higher at the study sites, compared to levels in the Earth's crust except for Fe, Ni and Mn. In addition, the Igeo class indicated that the surface sediments in the study area were moderately to strongly polluted in terms of metallic elements.

• 한국토양비료학회지
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• 제45권3호
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• pp.393-398
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• 2012

지형 특성에 따른 논토양 화학성변화를 조사하기 위해 전북지역 논 300개 지점에서 토양 물리화학성 및 중금속함량을 조사하였다. 논토양 분포 지형은 곡간 및 선상지 43.0%, 하해혼성평탄지 39.3%, 하성평탄지 15.0%, 홍적대지 2.7% 순이었다. 토양성분별 적정비율은 pH 65.3%, CEC 48.3%, 유효인산 22.3%이었고, 부족비율은 유기물 63.3%, 치환성 $K^+$ 61.3%, $Ca^{2+}$ 51.0%, $Mg^{2+}$ 59.3%, 유효규산 75.7%이었다. 곡간 및 선상지의 논토양 유형은 미숙답과 사질답이 각각 34.4과 33.6%이었고, 하성평탄지는 사질답 57.8%, 하해혼성평탄지는 보통답 47.4%, 홍적대지는 미숙답이 75.7%이었다. 곡간 및 선상지형의 토성은 양토가 53.5%를 차지하고, 하성평 탄지는 사양토 37.8%, 하해혼성평탄지에서는 미사질양토가 55.1%를 차지하고 있었다. 지형에 따라 pH와 유기물함량은 차이가 없었고, 유효인산은 홍적대지에서 224 mg $kg^{-1}$로 적정범위를 초과하였고, 치환성양이온은 곡간 및 선상지에서 $Ca^{2+}$을 제외하고 모두 적정범위에 분포하였다. 유효규산은 112~127 mg $kg^{-1}$ 수준으로 모든 지형에서 적정수준에 미치 지 못하였다. 토양 pH는 유효규산, 치환성 $Ca^{2+}$, $Mg^{2+}$, $Na^+$, CEC, 치환성 $K^+$ 순으로 정의 상관관계, 토양유기물 함량은 CEC, 유효인산, 치환성 $Ca^{2+}$, 유효규산과 정의 상관관계를 보 였다. 논토양의 Cd, Cr, Cu, Ni, Pb, Zn은 토양오염우려기준의 약 10%, As는 약 20~30%수준으로 분포하고 있어 전북지역 논토양은 안전한 것으로 조사되었다.

• 자원환경지질
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• 제32권4호
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• pp.385-398
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• 1999

The Narim gold mine is located approimately 200km southeast of Seoul within the Muju mineralized district of the Sobaegsan gneiss complex, Korea. Environmental geochemistry were undertaken for various kinds of water (surface, ground and mine water) collected of April, September and November in 1998 from the narim mine creek. Hydrogeochemical compositions of water samples are characterized by the relatively significant enrichment of Na+K, alkali ions, $HCO_{3}$, $NO_{3}$, Cl and F in groundwater, wheras the mine and surface waters are relatively enriched in Ca+Mg, hea표 metals and $SO_{4}$. Therefore, the groundwaters belong to the (Na+Ca)-( $HCO_{3}+SO_{4}$) type, respectively. The pH and EC values of the non-mining creek surfers are relatively lower compared with those of the surface water of the mine and ore dump area. The d values ($\delta$D-8$\delta^{18}$O) of all kinds of water from the Narim mine creek are 5.8 to 13.1 The range of $\delta$D and $\delta^{18}$O values (relative to SMOW) are shown in distinct two groups as follows: for the April waters of -64.8 to -67.8$\textperthousand$ and -9.6 to -10.0$\textperthousand$(d value=10.1 to 13.1), and for the November waters of -65.9 to -70.2$\textperthousand$ and -9.3 to -9.6$\textperthousand$ (d value=5.8 to 7.9), respectively. This range variation indicates that two group water were composed of distinct waters with seasonal difference. Geochemical modeling showed that mostly toxic metals (As, Fe, Mn, Ni, Pb, Zn) may exist largery in the from of metal $(M2^+)$ and metal-sulfate $(MSO_4\;^{2-$\mid$),\; and \;SO_4^{2-$\mid$}$ concentration influenced the speciation of heavy metals in the meteoric water. These metals in the groundwater could be formed of $CO_3 \;and \;(OH)_3$ complex ions. Using computer program, saturation index of albite, calcite, dolomite in meteoric water show undersaturated and progreddively evolved toward the saturation state, however, ground and mine water are nearly saturated. The gibbsited water-mineral reaction and stabilities suggest that the weathering of silicate minerals may be stable kaolinite, illite and Nasmectite. The clay minerals will be transformed to more stable kaolinite owing to the contiunous reaction.