• 제목/요약/키워드: Oxygen depletion zone

검색결과 9건 처리시간 0.023초

충주호의 환경특성에 관한연구 (The Study on Envionmental Characteristics of Chungju Reservoir)

  • 사성오;정영도;김학성
    • 환경위생공학
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    • 제13권3호
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    • pp.1-8
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    • 1998
  • Chungju reservoir is a multipurpose dam lake located at the upstream of Nm Han river and known as having the biggest watershed and the second water volume in korea. Conclusions are made as follows. 1. Environmental characteristics of the reservoir appear to be as follows. Chungju reservoir has long hydaulic retention time, 60-160 days. Water column has oxygen depletion zone in hypolimnion. Chungju reservoir is found to be in the midst of eutrophication. Chlorophyll-a and other physical parameters are found to be significantly dependent. 2. Nitrogen to phosphorus ratio was 50-350 for the water samples taken from the reservoir in 1996. It is very important clue for water quality management in relation to phytoplankton growing kinetics. Variations in chlorophyll-a contents appear to be related closely to total phosphorus concentration.

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시화방조제의 건설은 저서동물군집의 시${\cdot}$공간 분포에 어떠한 영향을 미쳤는가? (How are the Spatio-Temporal Distribution Patterns of Benthic Macrofaunal Communities Affected by the Construction of Shihwa Dike in the West Coast of Korea?)

  • 홍재상;정래홍;서인수;윤건탁;최병미;유재원
    • 한국수산과학회지
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    • 제30권5호
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    • pp.882-895
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    • 1997
  • 본 연구는 시화방조제 건설로 인하여 외해수와의 순환이 차단된 후 유기물오염과 담수화가 진행된 시화호 내에서 방조제 완공 전과 후의 저서동물 군집을 비교함으로써 시화호 내에서 저서동물군집이 어떤 천이과정을 거쳤는지, 그리고 군집의 천이를 일으킨 주된 요인은 무었인지, 또한 방조제 건설 전의 시화지구 해역 저서동물 군집과 건설 후 방조제 외곽해역의 저서동물 군집을 비교함으로써 방조제 건설이 주변 해역에 미친 영향을 파악하는데 그 목적이 있다. 방조제 완공 후 시화호 내에서의 저서동물 군집의 천이는 두 방향으로 진행되었다. 첫번째는 유기물 유입의 증가에 따른 저층수의 무산소 및 빈산소 환경의 형성으로 인해 저서동물이 완전히 사라진 중오염역 (Grossly Polluted Zone)의 출현이다. 두번째는 저서동물 군집이 계속 유지되고 있는 방조제 근처의 낮은 수심에서의 기회종으로 구성된 오염역 (Polluted Zone)으로의 저서동물 군집의 천이이다. 이런 군집의 천이는 방조제의 배수갑문을 통한 빈번한 해수 유입으로 인하여 저층수의 염분도와 용존산소량의 변화에 크게 영향을 받는 것으로 나타났다. 또한 시화방조제 건설은 주변 외곽지역의 저서동물 군집에도 영향을 미쳐 건설 전보다 후에 평균 출현종수는 2.6배, 밀도는 7배나 증가하는 전형적인 부영양화의 특징적 현상을 보임으로서 방조제 외곽해역의 저서동물 군집 또한 불안정한 상태로 변하고 있음을 알 수 있다.

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PWR 1차측 환경에서 Alloy 600 응력부식균열 선단 부근에서의 산화 거동 (Oxidation Behavior around the Stress Corrosion Crack Tips of Alloy 600 under PWR Primary Water Environment)

  • 임연수;김홍표;황성식
    • Corrosion Science and Technology
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    • 제11권4호
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    • pp.141-150
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    • 2012
  • Stress corrosion cracks in Alloy 600 compact tension specimens tested at $325^{\circ}C$ in a simulated primary water environment of pressurized water reactor were analyzed by analytical transmission electron microscopy and secondary ion mass spectroscopy (SIMS). From a fine-probe chemical analysis, oxygen was found on the grain boundary just ahead of the crack tip, and chromium oxides were precipitated on the crack tip and the grain boundary attacked by the oxygen diffusion, leaving a Cr/Fe depletion (or Ni enrichment) zone. The oxide layer inside the crack was revealed to consist of a double (inner and outer) layer. Chromium oxides existed in the inner layer, with NiO and (Ni,Cr) spinels in the outer layer. From the nano-SIMS analysis, oxygen was detected at the locations of intergranular chromium carbides ahead of the crack tip, which means that oxygen diffused into the grain boundary and oxidized the surfaces of the chromium carbides. The intergranular chromium carbide blunted the crack tip, thereby suppressing the crack propagation.

밀양 납석광상의 모암변질작용과 생성환경 (Wall Rock Alteration and Genetic Environment of the Milyang Pyrophyllite Deposit)

  • 이강원;문희수;송윤구;김인준
    • 자원환경지질
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    • 제26권3호
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    • pp.289-309
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    • 1993
  • Milyang pyrophyllite deposit which was formed by hydrothermal alteration occurs in Late Cretaceous andesitic tuff in the Milyang area, Gyeongsangnamdo. The wall rock alteration and genesis of the Milyang pyrophyllite deposit were studied. The ore minerals are composed dominantly of pyrophyllite accompanied by small amounts of quartz, kaolinite, pyrite, dumortierite and diaspore. The alteration halo of this deposit can be divided into three zones on the basis of mineral assemblage; pyrophyllite, sericite and chlorite zone. The common mineral assemblages of each alteration zone are as follows: (1) pyrophyllite zone; pyrophyllite-quartz-kaolinite-pyrite-dumortierite-diaspore, (2) sericite zone; sericite-quartz-pyrite-kaolinite, and (3) chlorite zone; chlorite-plagioclase-quartz. Major element chemistry shows that characteristic depletion in MgO, CaO, and $Na_2O$ and relative increase in FeO from less altered chlorite zone to extensively altered pyrophyllite zone corresponding to variation in mineral assemblages. The paragenesis of ore minerals, oxygen isotope data, chlorite and illite geothermometry suggest that ore deposit was formed at about $250{\sim}330^{\circ}C$. Both hydrogen and silica activities are high in pyrophyllite zone. Potassium activity increases in sericite zone while hydrogen activity becomes low in chlorite zone. The pyrophyllite zone was formed relatively higher temperature than those of sericite and chlorite zones. The ore fluid was considered to be magmatic water in origin derived from the residual granitic magma which interacted with meteoric water.

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하계정체기에 있어서 수개호소의 생태학적 비교연구 (Ecological Comparison of Several Lakes in Summer Stagnation Period)

  • 엄규백
    • Journal of Plant Biology
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    • 제16권3_4호
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    • pp.17-34
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    • 1973
  • The physico-chemical factors, the distribution of chlorophyll and the primary production of the lakes Hwajinpo, Yongrangho, Chunchonho, Uiamho, Soyangho and Changjamot have been studied in order to make ecological comparison among these lakes during summer stagnation period of August to September of 1973. On the basis of the characteristics of these lakes, the lake types have been discussed. Thermocline is observed at 3-4m zone in the lake Changjamot and 4-5m zone in the lake Yongrangho. In the case of lake Hwajinpo and impoundments, the distinct thermal stratification is not observed at the summer stagnation period. As to vertical distribution of dissolved oxygen, a positive heterograde curve is obtained in the lakes Hwajinpo and Yongrangho. In the lake Changjamot the typical clinograde curve and the oxygen depletion in hypolimnion are observed. In the case of impoundments, however, the orthograde curve is observed in the lakes Chunchonho and Uiamho. While in the lake Soyangho, any stratification of the disssolved oxygen is not found. In the brackish lakes, such as lakes Hwajinpo and Yongragho, the salinity of hypolimnion is found to be much higher than that of epilimnion. In the lake Hwajinpo, the salinity of hypolimnion is exhibited 32.7$\textperthousand$, which is nearly the same as sea water. The distribution of nitrogenous compounds and phosphates is found to be high in the lake Changjmot. The silicate is also found in high concentration in the lake Chunchonho, and the distribution of nutrients in the brackish lakes is generally low. As to the vertical distribution of chlorophyll level, the lake Changjamot shows a stratum type and the brackish lakes L-type stratification. In the impoundments, lakes Chunchonho and Uiamho appear to be homogeneous type. Seasonal variation of chlorophyll level in the lake Changjamot is examined from January to September 1973. The vertical distribution of chlorophyll during the period of circulation from January to April is homogeneous type and is stratum type thereafter. The maximum chlorophyll level is 277.4mg/$m^2$ on June 23 and the pattern of seasonal variation of chlorophyll level is comparable to the type of eutrophy. The horizontal distribution of chlorophyll level is studied in the brackish lakes, Hwajinpo and Yongrangho. The pattern of distribution is found to be an irregular type. On the basis of measurements of primary production by means of the carbon-14 method and the distribution of chlorophyll level, it is concluded that the interior part of the lake Hwajinpo and Changjamot are eutrophic and the exterior part of the lake Hwajinpo, lake Yongrangho and the impoundments, lake Uiambo and Soyangho are mesotrophic.

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시화호와 시화호 주변 해역 식물플랑크톤의 대증식과 일차 생산력에 관한 연구 (The Study on the Phytoplankton Bloom and Primary Productivity in Lake Shihwa and Adajcent Coastal Areas)

  • 최중기;이은희;노재훈;허성회
    • 한국해양학회지:바다
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    • 제2권2호
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    • pp.78-86
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    • 1997
  • 시화 방조제 건설 후 급속도로 오염되고 있는 시화호 내의 식물플랑크톤 대증식 현상을 파악하기 위하여 1995년 10월부터 1996년 8월까지 시화호 내외에서 환경요인들과 식물플랑크톤 chlorophyll-a, 현존량, 우점종, 일차생산력 등을 4계절 조사하였다. 시화호는 부영양화된 기수호의 성격을 띄고 있으며 저층에는 밀도가 높은 잔류해수가 남아있다. 시화호의 표층에서 육상으로부터 유입된 오염된 하천수의 영향으로 chlorophyll-a 농도가 평균 168.0 ${\mu}g\;l^{-1}$에 이르는 식물플랑크톤 대증식 현상이 연중 지속적으로 일어났다. 식물플랑크톤의 대증식은 추계와 동계에는 돌말류 Cyclotella atomus 에 의해 주로 일어났고, 춘계와 하계에는 와편모류 Prorocentrum minimum 등과 황갈조류 등에 의해 일어났다. 시화호 바깥해역에서도 시화호수의 방류로 통계에서 하계에 걸쳐 돌말류 Thalassiosira nordenskioeldii, Skeletonema costatum, Chaetoceros sp. 등에 의해 대증식이 계속 일어났다. 시화호의 식물플랑크톤에 의한 일차생산력은 연평균 3,972 mgC $m^{-2}\;day^{-1}$로 높게 일어났다. 그러나 일차생산력의 대부분은 표층에서의 높은 광흡수로 수심 3 m 내로 국한되고, 추계와 동계에는 규산염이 제한요인으로 작용하여 더 이상 높게 나타나지 못하였다. 저층에서는 광제한 등으로 광합성 작용이 거의 없었고, 표층에서 떨어진 유기물이 분해되어 산소가 고갈되는 양상을 보였다.

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Field Studios of In-situ Aerobic Cometabolism of Chlorinated Aliphatic Hydrocarbons

  • Semprini, Lewts
    • 한국지하수토양환경학회:학술대회논문집
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    • 한국지하수토양환경학회 2004년도 총회 및 춘계학술발표회
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    • pp.3-4
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    • 2004
  • Results will be presented from two field studies that evaluated the in-situ treatment of chlorinated aliphatic hydrocarbons (CAHs) using aerobic cometabolism. In the first study, a cometabolic air sparging (CAS) demonstration was conducted at McClellan Air Force Base (AFB), California, to treat chlorinated aliphatic hydrocarbons (CAHs) in groundwater using propane as the cometabolic substrate. A propane-biostimulated zone was sparged with a propane/air mixture and a control zone was sparged with air alone. Propane-utilizers were effectively stimulated in the saturated zone with repeated intermediate sparging of propane and air. Propane delivery, however, was not uniform, with propane mainly observed in down-gradient observation wells. Trichloroethene (TCE), cis-1, 2-dichloroethene (c-DCE), and dissolved oxygen (DO) concentration levels decreased in proportion with propane usage, with c-DCE decreasing more rapidly than TCE. The more rapid removal of c-DCE indicated biotransformation and not just physical removal by stripping. Propane utilization rates and rates of CAH removal slowed after three to four months of repeated propane additions, which coincided with tile depletion of nitrogen (as nitrate). Ammonia was then added to the propane/air mixture as a nitrogen source. After a six-month period between propane additions, rapid propane-utilization was observed. Nitrate was present due to groundwater flow into the treatment zone and/or by the oxidation of tile previously injected ammonia. In the propane-stimulated zone, c-DCE concentrations decreased below tile detection limit (1 $\mu$g/L), and TCE concentrations ranged from less than 5 $\mu$g/L to 30 $\mu$g/L, representing removals of 90 to 97%. In the air sparged control zone, TCE was removed at only two monitoring locations nearest the sparge-well, to concentrations of 15 $\mu$g/L and 60 $\mu$g/L. The responses indicate that stripping as well as biological treatment were responsible for the removal of contaminants in the biostimulated zone, with biostimulation enhancing removals to lower contaminant levels. As part of that study bacterial population shifts that occurred in the groundwater during CAS and air sparging control were evaluated by length heterogeneity polymerase chain reaction (LH-PCR) fragment analysis. The results showed that an organism(5) that had a fragment size of 385 base pairs (385 bp) was positively correlated with propane removal rates. The 385 bp fragment consisted of up to 83% of the total fragments in the analysis when propane removal rates peaked. A 16S rRNA clone library made from the bacteria sampled in propane sparged groundwater included clones of a TM7 division bacterium that had a 385bp LH-PCR fragment; no other bacterial species with this fragment size were detected. Both propane removal rates and the 385bp LH-PCR fragment decreased as nitrate levels in the groundwater decreased. In the second study the potential for bioaugmentation of a butane culture was evaluated in a series of field tests conducted at the Moffett Field Air Station in California. A butane-utilizing mixed culture that was effective in transforming 1, 1-dichloroethene (1, 1-DCE), 1, 1, 1-trichloroethane (1, 1, 1-TCA), and 1, 1-dichloroethane (1, 1-DCA) was added to the saturated zone at the test site. This mixture of contaminants was evaluated since they are often present as together as the result of 1, 1, 1-TCA contamination and the abiotic and biotic transformation of 1, 1, 1-TCA to 1, 1-DCE and 1, 1-DCA. Model simulations were performed prior to the initiation of the field study. The simulations were performed with a transport code that included processes for in-situ cometabolism, including microbial growth and decay, substrate and oxygen utilization, and the cometabolism of dual contaminants (1, 1-DCE and 1, 1, 1-TCA). Based on the results of detailed kinetic studies with the culture, cometabolic transformation kinetics were incorporated that butane mixed-inhibition on 1, 1-DCE and 1, 1, 1-TCA transformation, and competitive inhibition of 1, 1-DCE and 1, 1, 1-TCA on butane utilization. A transformation capacity term was also included in the model formation that results in cell loss due to contaminant transformation. Parameters for the model simulations were determined independently in kinetic studies with the butane-utilizing culture and through batch microcosm tests with groundwater and aquifer solids from the field test zone with the butane-utilizing culture added. In microcosm tests, the model simulated well the repetitive utilization of butane and cometabolism of 1.1, 1-TCA and 1, 1-DCE, as well as the transformation of 1, 1-DCE as it was repeatedly transformed at increased aqueous concentrations. Model simulations were then performed under the transport conditions of the field test to explore the effects of the bioaugmentation dose and the response of the system to tile biostimulation with alternating pulses of dissolved butane and oxygen in the presence of 1, 1-DCE (50 $\mu$g/L) and 1, 1, 1-TCA (250 $\mu$g/L). A uniform aquifer bioaugmentation dose of 0.5 mg/L of cells resulted in complete utilization of the butane 2-meters downgradient of the injection well within 200-hrs of bioaugmentation and butane addition. 1, 1-DCE was much more rapidly transformed than 1, 1, 1-TCA, and efficient 1, 1, 1-TCA removal occurred only after 1, 1-DCE and butane were decreased in concentration. The simulations demonstrated the strong inhibition of both 1, 1-DCE and butane on 1, 1, 1-TCA transformation, and the more rapid 1, 1-DCE transformation kinetics. Results of tile field demonstration indicated that bioaugmentation was successfully implemented; however it was difficult to maintain effective treatment for long periods of time (50 days or more). The demonstration showed that the bioaugmented experimental leg effectively transformed 1, 1-DCE and 1, 1-DCA, and was somewhat effective in transforming 1, 1, 1-TCA. The indigenous experimental leg treated in the same way as the bioaugmented leg was much less effective in treating the contaminant mixture. The best operating performance was achieved in the bioaugmented leg with about over 90%, 80%, 60 % removal for 1, 1-DCE, 1, 1-DCA, and 1, 1, 1-TCA, respectively. Molecular methods were used to track and enumerate the bioaugmented culture in the test zone. Real Time PCR analysis was used to on enumerate the bioaugmented culture. The results show higher numbers of the bioaugmented microorganisms were present in the treatment zone groundwater when the contaminants were being effective transformed. A decrease in these numbers was associated with a reduction in treatment performance. The results of the field tests indicated that although bioaugmentation can be successfully implemented, competition for the growth substrate (butane) by the indigenous microorganisms likely lead to the decrease in long-term performance.

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양양 남대천 하구역의 여름철 대형저서동물 군집의 생태학적 특성 (An Ecological Feature of Benthic Macrofauna during Summer 1997 in Namdaechon Estuary, Yangyang, Korea)

  • 홍재상;서인수;이창근;윤상필;정래홍
    • 한국수산과학회지
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    • 제33권3호
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    • pp.230-237
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    • 2000
  • 본 연구는 양양 남대천 하구역 대형저서동물의 생태학적 연구를 위하여 1997년 9월 23일 개량된 van Veen 그랩을 이용하여 총 11개 정점을 대상으로 현장조사를 실시하였다. 조사 지역에서 총 11종, 정점당 평균 345 개체/$m^2$ 및 67.148 g WWt/$m^2$이 채집되었다. 종 수, 개체수 및 생물량에 있어서 환형동물, 절지동물과 연체동물이 $95{\%}$ 이상의 점유율을 나타냈다. 양양 남대천 하구역은 대형저서동물의 다양성 측면에서 매우 빈약한 생물상 (生物相)을 보였으며, 개체수면에서는 다모류의 Heteromastus filiformis, Hediste japonica, Eteone longa, 빈모류의 Oilgochaeta Sp., 연체동물의 Corbicula japonica, 그리고 절지동물의 Cyathura higoensis 등이 우점종으로 나타났다. 한편, 본 조사지역은 소상하는 연어 채포를 위해 쌓아놓은 둑 근처의 수심 7m 정도되는 지역이 여름철 성층 (成層, stratifiestion) 형성으로 인한 저층수의 환경 악화로 대형저서동물이 출현하지 않는 무생물구역 (無生物區域, azoic zone)으로 나타났으며, 주변의 정점에서도 일부 기회종 (opportunistic species)들이 높은 밀도를 나타내는 오염역 (汚染域, Polluted Zone)이 출현하고 있어 물리적 환경 변화에 따라 국지적으로 이러한 중오염역 (重汚染域, Very Polluted Zone)이 확산되는 방향으로의 대형저서동물의 생태적인 천이가 일어날 수 있을 것으로 생각된다.

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연안통합관리의 과학적 및 지역적 접근 (A Regional Approach for Integrated Coastal Management with Scientific and Local Knowledge)

  • 이찬원
    • 한국해양환경ㆍ에너지학회지
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    • 제6권1호
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    • pp.21-29
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    • 2003
  • 수산, 항만, 관광 등 남해 연안 바다의 이용은 지역경제의 중요한 부분을 차지하고 있다. 기존의 연안관리와 연안 환경 문제에 관한 일시적인 처방은 더 이상 유동성 적조, 산소결핍, 잘피 서식의 감소 등 연안 문제 해결의 방안이 되지 못하고 있다. 1999년 연안관리법이 통과된 후 2001년부터 현재까지 연안지역관리계획이 수립되고 있다. 연안지역관리계획에는 연안 생태도시 구축, 연안오염물질 감소, 제도적 장치 개발, 모니터링 계획, 예산확보 등이 포함되어 있다. 연안역 통합관리의 성공적인 출발은 중앙정부와 지자체의 협조뿐만 아니라 지역의 NGO와의 조화로운 모색이 필요하다. 연안관리의 해역분류 중 특별관리해역으로 지정된 마산만 지역에는 마산만 살리기 시민연합이 조성되어 과학적인 정보의 제공과 지역 특수성에 부합될 수 있는 여러 가지 활동이 진행됨으로써 성공적인 연안통합관리의 실행이 가능해지고 있다.

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