• 자원환경지질
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• 제42권5호
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• pp.487-494
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• 2009

본 연구에서는 무산소 환경에서 As(III)로 대체된 자철석으로의 침전 가능성을 확인하기 위하여 Fe(II)와 As(V)의 반응을 통한 As(V)의 As(III)로의 환원 여부를 조사하였다. Fe(II)와 As(V)가 용액상으로 존재하는 균질조건에서의 환원반응 실험은 pH에 따른 영향을 알아보기 위해 수행되었고, 주어진 pH 조건(3.0~7.3)에서 용해된 Fe(II)에 의한 As(V)의 As(III)로의 환원반응은 일어나지 않았다. 균질조건에서의 환원반응 실험결과와 유사하게 침철석을 이용한 불균질조건에서의 환원반응 실험에서도 침철석에 흡착된 Fe(II)에 의한 As(V)의 환원반응은 일어나지 않았다. 또한 Fe(II)의 산화에 미치는 As(V)의 영향에 대한 회분식 실험결과, As(V)가 Fe(II)의 산화반응을 저해하는 영향을 주었고 균질한 조건에서보다 불균질한 조건에서 As(V)의 영향이 명확하게 나타난 것으로 사료된다. 이런 결과들은 무산소 및 지하 환경에서 Fe(II)와 공존할 때, As(V)는 안정한 상태로 존재함을 시사한다.

• 자원환경지질
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• 제55권1호
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• pp.45-51
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• 2022

독도에서의 "인간의 거주 혹은 독자적인 경제활동을 영위할 수 있는가의 여부"는 국제법 상으로 독도의 지위를 결정하는 중요한 요소로 작용한다. 이러한 관점에서 독도의 활용가능한 물(water resource)에 대하여, 독도에서 유일하게 지하수 유출이 발생하고 있는 서도의 물골을 대상으로 조사한 수문학적 결과를 보고한다. 이 조사에서 평가한 물골의 지하수 유출량은 최소 1.1 m³/d로 나타났으며, 이는 기존의 연구들에서 제시한 결과와 통계적으로 유사하다. 물의 산소-수소 안정동위원소비를 통한 기원 분석에서 지하유출수의 기원은 강수로 판단되며, 일강수량을 기준으로 할 때, 강수의 약 36% 정도는 화산암 내의 절리를 통해 빠르게 지하수로 유출된다. 지하유출수의 수질은 생활용수와 음용수로 사용하기에는 높은 염도와 질산염 농도를 보이며, 이들은 해무와 파도 등에 의한 염분과 괭이 갈매기 등 조류 배설물로부터 기인된 것으로 판단된다.

• 한국물환경학회지
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• 제28권4호
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• pp.561-573
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• 2012

The object of this study was to analyze long-term water quality gradients during 1992-2008 at six sites of Geumho River and near-by two sites of Nakdong River and their influences on fish trophic guilds and tolerance guilds along with ecological health. Water quality including biological oxygen demand (BOD), chemical oxygen demand (COD), conductivity, total phosphorus (TP), total nitrogen (TN), and total suspended solids (TSS) varied largely depending on the sampling locations and seasons. Values of ambient BOD, COD, TP, and TN were greater in the downstream than in the upstream reach, and seasonal and interannual variabilities were also higher in the downstreams. This phenomenon was evident due to a dilution by the Asian monsoon rainfall during the monsoon. These outcomes indicate that point sources near the downstream are important for the chemical conditions, but also seasonal stream runoff was considered as an important factor regulating the chemical conditions. Conductivity decreased rapidly during the summer due to ionic dilution, and nutrients (N, P), BOD, COD had an inverse function of seasonal precipitation. Based on the water quality, we selected two sites (control site = $C_s$ vs. impacted site = $I_s$) for impact analysis of water chemistry on fish community and trophic/tolerant guilds. Fish guild analysis showed that species diversity was higher in the headwater stream ($C_s$) than the impacted downstream ($I_s$), and that the proportion of tolerant and omnivore species were greater in the impacted site of downstream. Comparisons of water quality between Geumho River and Nakdong River indicated that Geumho River was considered as a point source which degradated water quality to the Nakdong River. Overall, chemical water quality and fish guild analysis suggest that even if current chemical quality got better after 1996 due to continuous constructions of wastewater disposal plants near the downstreams, fish compositions of tolerant and omnivores were still dominated the community. Thus, biological restoration based on ecological health is required for the ecosystem conservation.

• 한국양식학회지
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• 제15권1호
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• pp.49-60
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• 2002

Research on practices for improving water quality in channel catfish Ictalurus punctatus ponds was conducted at the Auburn University Fisheries Research Station, Auburn, Alabama, in 1998 and 1999. The objective of this two-year study was to determine better management practices to enhance water quality and improve production efficiency. In the first year, oxidation of bottom soil by drying, tilling, and applying sodium nitrate was performed (dry-till and dry-till with sodium nitrate treatments). The second year, based on the results obtained during the first year, precipitation of phosphorus (P) from water by applying gypsum was compared to the dry-till treatment (dry-till and dry-till with gypsum treatments). Control ponds were not subjected to bottom drying, tilling, sodium nitrate, or gypsum treatment. Channel catfish fingerings were stocked at 15,000/ha. In the first year, water in ponds from dry-till and dry-till with sodium nitrate treatments had lower concentrations (P < 0.01) of soluble reactive P, nitrate ($NO_{3} ^{-}) and nitrite ($NO_{2} ^{-}) nitrogen (N), total ammonia ($NH_3$) nitrogen, total suspended solids and turbidity, and higher values of pH, Secchi disk visibility, total alkalinity, total hardness, and calcium ($Ca^{2+}) hardness than water in control ponds. Ponds of the dry-till treatment also had lower concentrations (P < 0.01) of total P and total N than control ponds. Total fish production and survival rate did not differ among the treatments (P > 0.05). The findings suggested that drying and tiling pond bosoms between crops could achieve water quality improvement. Applying sodium nitrate to dry, tilled pond bosoms did not provide water quality improvement. In the second year, the treatment with the best results from the first year, dry-till, was compared with a dry-till with gypsum treatment. Enough gypsum was applied to give a total hardness of about 200 mg/L, and gypsum was reapplied as needed to maintain the hardness. Compared to the control, dry-till and dry-till with gypsum treatments had lower concentrations (P < 0.01) of total and soluble reactive P, total N, and total $NH_3$-N, and higher concentrations (P < 0.01) of dissolved oxygen. Ponds of the duty-till with gypsum treatment also had lower concentrations (P < 0.01) of chlorophyll $\alpha$, chemical oxygen demand, and total alkalinity than the control. Total fish production and survival rate did not differ (P > 0.05) among the treatments. These findings suggest that drying and tilling pond bosoms between crops and treating low hardness waters with gypsum could achieve water Quality improvement.

• 한국수산과학회지
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• 제12권1호
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• pp.27-33
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• 1979

1978년 진해만에서 있었던 적조현상과 양식 굴의 대량폐사에 관한 조사결과를 요약하면 아래와 같다. 1. 진해만에서 1978넌 9월중 양식 굴의 대량폐사가 있었다. 폐사량은 $96\%$인 5,687M/T으로 피해액은 22억 7천 5백만원이었다. 2. 상기의 대량폐사는 지속된 고온, 대규모의 적조와 그로 인한 저층수의 빈산소 내지 무산소화로 인한 질식이 주 원인의 일보였다고 추측된다. 3. 적조의 원인종은 와편모조의 일종인 Ceratium fusus로서 각장 $340{\mu}m$, 각폭 $20{\mu}m$ 정도의 대형 식물플랑크톤이었다. 클로로필-a량은 최고 $50mg/m^3$ 이었다.4. 춘기의 가뭄과 6월의 다우로 성층이 형성된데다 지속된 고온과 장일조 그리고 해상의 평온함이 대규모의 적조를 유발시킨 원인의 일부라 생각된다.

• 자원환경지질
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• 제21권1호
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• pp.45-56
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• 1988

Many hydrothermal skarn-type iron ore deposits inchiding Mulgeum, Yangseong, Maeri and Kimhae mines are distributed in the south-eastern Gyeongnam Province, Korea. The deposits are magnetite veins which occurred in propylitized andesitic rock near the contact with late Cretaceous Masanite. Symmetrical zoned skarns are commonly developed around the magnetite veins. The order of the skarn zones from the vein is garnet-quartz skarn, epidote skarn, and epidote-orthoclase skarn. The garnets include isotropic or anisotropic andradite($Ad_{100{\sim}70}$), and the epidotes are composed of pistacite($Ps_{21-31}$). Fe contents of the epidotes generally increase toward the magnetite veins. Epidotes and garnets often show compositional variations from grain to grain, that is, their Fe and Al contents vary inversely. This suggests that the variations depend mainly upon $fo_2$ during the skarnization. Oxygen and carbon isotope analyses of minerals from andesitic rock, micrographic granite, major skarn zones and post-mineralization zones were conducted to provide the information on the formation temperature, the origin and the evolution of the hydrothermal solution forming the iron ore deposits. Becoming more distant from the ore vein, temperatures of skarn zones represent the decreasing tendency, but most ${\delta}O^{18}$ and ${\delta}O^{18}_{H_2O}$ values of skarn minerals represent no variation trend, and also the values are relatively low. Judging from all the isotopic data from the ore deposits, the major source of hydrothemal solution altering the skarn zones and precipitating the ore bodies was magmatic water derived from the more deeply seated micrographic granite. This high temperature hydrothermal solution rising through the fissures of propylitized andesitic rock was mixed with some meteoric water, and the extensive isotopic exchange occurred with the propylitized andesitic rock. During this process, the temperature and ${\delta}O^{18}_{H_2O}$ value of hydrothermal solution were lowered gradually. At the stage of iron ore precipitation, because after all the alteration was already finished, the oxygen isotopic exchange with the wall rock was nearly not taken. The relatively high ${\delta}O^{18}$ and ${\delta}O^{18}_{H_2O}$, and relatively low ${\delta}C^{13}$ values of calcites of post mineralization stage, are the results of leaching of the high ${\delta}O^{18}$ chert xenolith in the andesitic rock and low ${\delta}C^{13}$ andesitic rock.

• 자원환경지질
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• 제39권2호
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• pp.151-162
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• 2006

경상남도 창원시 대산면에 위치하는 강변여과수 개발을 위한 충적층 지하수의 수질특성과 변화양상을 조사하였다. 지하수의 총용존고형물(TDS)은 3월에 비해 3월에 상당히 낮은 값을 보이며, 관측정에서 나타난 계절에 따른 용존산소 농도 변화 역시 강우의 함양으로 인한 지하수의 희석현상이 원인으로 판단된다. 충적층 지하수의 철(Fe)과 망간 (Mn)에 의한 오염현상은 지하수의 심도에 따른 용존산소의 감소에 따른 환원환경의 발생에 기인하며, 철은 비정질의 산화침전물이, 망간은 $MnCO_3$와 같은 탄산염 광물들이 주요 반응물질로 나타났다. 질산성질소$(NO_3-N)$에 의한 오염현상은 지하수 채취 심도에서의 산화환원 환경과 탈질반응이 중요한 역할을 한다. 질산성질소의 불규칙한 분포는 질산성질소가 관측지점 주변의 충적층의 농업시설에서 유입된 것을 지시한다. 연구부지의 관측정들 중 DS-2, D-2, DS-3, SJ-1 및 SJ-3은 주 대수층인 모래/자갈층을 관통하지 못해서, 취수정의 수질변화를 감시하는 모니터링 기능이 제한될 수 밖에 없었다. 나아가, 강변여과수 시설부지에서는, 적어도 여과부지로 사용되는 충적층에 대해서는 농업활동의 제한 등 적절한 오염방지대책이 시행되어야 한다.

• 한국수소및신에너지학회논문집
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• 제13권2호
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• pp.143-150
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• 2002

The thermal behavior of $(Co_{0.5}\;Mn_{0.5})Fe_2O_4$ prepared by a co-precipitation wasinvestigated for Hz generation by the thermochemical cycle. The reduction reaction of $(Co_{0.5}\;Mn_{0.5})Fe_2O_4$ started from $480^{\circ}C$, and the weight loss was 1.6 wt% up to $1100^{\circ}C$. At this reaction, $(Co_{0.5}\;Mn_{0.5})Fe_2O_4$ was reduced by release of oxygen bonded with the $Fe^{3+}$ ion in the B site of ($CO_{0.5}$ $(Co_{0.5}\;Mn_{0.5})Fe_2O_4$. In the $H_2O$ decomposition reaction, $H_2$ was generated by oxidationof reduced $(Co_{0.5}\;Mn_{0.5})Fe_2O_4$. The crystal structure of $(Co_{0.5}\;Mn_{0.5})Fe_2O_4$ for reduction reaction maintained spinel structure and the lattice constant of $(Co_{0.5}\;Mn_{0.5})Fe_2O_4$ ($8.41\AA$) was enlarged to $8.45\AA$. But the lattice constant of $(Co_{0.5}\;Mn_{0.5})Fe_2O_4$ after $H_2O$ decomposition reaction did not change to $8.45\AA$. Then, $(Co_{0.5}\;Mn_{0.5})Fe_2O_4$ is excellent material in the thermochemical cyclic reaction due to release oxygen at low temperature for the reduction reaction and produce $H_2$ maintaining crystal structure for redox reaction.

• 청정기술
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• 제21권4호
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• pp.248-256
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• 2015

MnO₂를 KMnO₄와 MnCl₂･4H₂O을 이용해 자연침전을 유도한 후, 수열방법으로 120-200 ℃, 0.5-5시간 범위에서 제조하여 300 ℃에서 열처리 후 CO 산화반응을 수행하였다. 촉매활성 원인의 규명과 물리화학적 특성을 분석하기 위해 X 선 회절 분석, 질소 흡착, 주사전자현미경, 수소 또는 일산화탄소 승온환원 분석(H₂- 또는 CO-TPR)을 실시하였다. 합성조건에 따라 순수한 α-MnO₂ 혹은 α/β-혼합상을 가진 MnO₂가 각각 합성되었다. 촉매활성과 안정성은 순수한 α-MnO₂ 상에서 α/β-혼합상을 가진 MnO₂보다 우수하게 관찰되었다. 특히, 150 ℃에서 1시간 수열 합성된 촉매는 가장 큰 비표면적인 214 m² g^-1을 가졌으며 H₂, CO-TPR 분석에서 가장 우수한 환원성과 격자산소 종의 활성을 보였으며 일산화탄소의 승온 및 등온 산화반응에서 가장 우수한 촉매활성을 나타내었다. 이것은 촉매의 물리화학적 특성에 기인한 것으로 촉매의 결정구조, 비표면적, 환원성 및 격자산소 종의 활성은 촉매활성과 깊은 상관관계가 존재함을 확인하였다.

• 한국안전학회지
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• 제24권6호
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• pp.63-71
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• 2009

In order to improve flame retardancy, the halogen free organic melamine phosphate(M-P) flame retardant was synthesized from melamine and phosphoric acid by the reaction of precipitation. The ignition test was carried out preparing hybrid flame retardant compound($H_bFRC$) consisting of organic M-P and inorganic Mg$(OH)_2$ as a flame retardant in the polyolefin resins. The flame retardancy and mechanical properties of flame retardant aluminum composite panel($H_bFRC$-ACP) were performed to investigate the possibility of the composite material, which was contained M-P, as a inner core for $H_bFRC$-ACP. For this study, the results of ignition test indicate that a char formation and drip suppressing effect, and combustion time reduced as the content of M-P increased. The limited oxygen index(LOI) values were measured 17.4vol% and 31.5vol% for LDPE only and $H_bFRC$-3(M-P content: 15wt%), respectively. And it was verified that the $H_bFRC$-3 was needed more oxygen quantity with the increase of M-P content when it combustion. Also, the results from thermogravimetric analysis were observed endothermic peak at $350^{\circ}C$ and $550^{\circ}C$, it was confirmed predominant thermal stability though the wide temperature range by the mixture of M-P and Mg$(OH)_2$. The LDPE-ACP (using only LDPE as a inner core), $35.13kW/m^2$ of heat release rate(HRR) and 13.43MJ/m2 of total heat release(THR) were measured while the $H_bFRC$-ACP, $10.44kW/m^2$ of HRR and 1.84MJ/m2 of THR were measured by results of cone calorimeter test. In case of $H_bFRC$-ACP, the average gas emission amount of CO and $CO_2$ could be decreased down to 25% and 20%, respectively, in comparison with LDPE-ACP. The mechanical properties such as tensile strength, bending strength and adhesion strength of $H_bFRC$-ACP were revealed slightly high values $54N/mm^2$, $152N/mm^2$ and 120N/25mm, respectively, compared with LDPE-ACP. It was confirmed that flame retardancy was improved with the synergy effect because of char formation by M-P and hydrolysis by Mg$(OH)_2$. The result of this study suggest that $H_bFRC$ can be applied for an adequate halogen free flame retardant composite material as a inner core for ACP.