• 생물환경조절학회지
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• 제16권4호
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• pp.352-357
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• 2007

본 연구는 착색단고추의 겨울철 시설재배시 탄산가스 시비의 이용효율을 높이기 위한 시비 농도 및 시간을 구명하기 위해 수행하였다. 탄산가스의 공급 설정농도 수준은 400ppm과 700ppm이였으며, 시비 시간은 09:00-12:00(3h)과 09:00-15:00(6h)로 농도와 시간을 조합한 4 수준과 무처리구를 합하여 5 처리를 하였고, 정식 후 55일간 처리하였다. 그 결과 전반적으로 탄산가스 농도가 높고, 시비시간이 길어질수록 전반적인 생육이 증가하였다. 그러나 겨울철에는 광도가 제한 요소로 작용하기 때문에 탄산가스의 높은 농도보다는 시비 시간이 길어질수록 생육이 더 증가하였다. 그러므로 광이 적은 겨울철에는 높은 농도의 이산화탄소를 짧은 시간 시비하는 것보다 낮은 농도로 긴 시간 시비하는 것이 효율적인 것으로 판단된다.

• 한국작물학회:학술대회논문집
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• 한국작물학회 2005년도 춘계학술발표회 요지
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• pp.150-151
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• 2005

• 한국작물학회:학술대회논문집
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• 한국작물학회 2006년도 한국약용작물학회 공동춘계학술발표회
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• pp.284-285
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• 2006

• 한국미생물학회:학술대회논문집
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• 한국미생물학회 2004년도 International Meeting of the Microbiological Society of Korea
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• pp.21-23
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• 2004

• 자원환경지질
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• 제31권4호
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• pp.297-310
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• 1998

Geochemical characteristics of environmental toxic elements at the Narim mine area were investigated on the basis of major, minor, rare earth element geochemistry and mineralogy. Ratios of $Al_2O_3/Na_2O$ and $K_2O/Na_2O$ in soils and sediments range from 11.57 to 22.21 and from 1.86 to 3.93, and are partly negative and positive correlation against $SiO_2/Al_2O_3$ (3.41 to 4.78), respectively. These suggested that sediment source of host granitic gneiss could be due to rocks of high grade metamorphism originated by sedimentary rocks. Characteristics of some trace and rare earth elements of V/Ni (0.33 to 1.95), Ni/Co (2.00 to 6.50), Zr/Hf (11.27 to 53.10), La/Ce (0.44 to 0.55), Th/Yb (4.07 to 7.14), La/Th (2.35 to 3.93), $La_N/Yb_N$ (6.58 to 13.67), Co/Th (0.63 to 2.68), La/Sc (3.29 to 5.94) and Sc/Th (0.49 to 1.00) are revealed a narrow range and homogeneous compositions may be explained by simple source lithology. Major elements in all samples are enriched $Al_2O_3$, MgO, $TiO_2$ and LOI, especially $Fe_2O_3$ (mean=7.36 wt.%) in sediments than the composition of host granitic gneiss. The average enrichment indices of major and rare earth elements from the mining drainage are 2.05 and 2.91 of the sediments and are 2.02 and 2.60 of the soils, normalizing by composition of host granitic gneiss, respectively. Average composition (ppm) of minor and/or environmental toxic elements in sediments and soils are Ag=14 and 1, As=199 and 14, Cd=22 and 1, Cu=215 and 42, Pb=1770 and 65, Sb=18 and 3, Zn=3333 and 170, respectively, and extremely high concentrations are found in the subsurface sediments near the ore dump. Environmental toxic elements were strongly enriched in all samples, especially As, Cd, Cu, Pb, Sb and Zn. The level of enrichment was very severe in mining drainage sediments, while it was not so great in the soils. Based on the EPA value, enrichment index of toxic elements is 8.63 of mining drainage sediments and 0.54 of soils on the mining drainage. Mineral composition of soils and sediments near the mining area were partly variable being composed of quartz, mica, feldspar, amphibole, chlorite and clay minerals. From the gravity separated mineralogy, soils and sediments are composed of some pyrite, arsenopyrite, chalcopyrite, sphalerite, galena, goethite and various hydroxide minerals.

• 자원환경지질
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• 제30권6호
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• pp.553-566
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• 1997

Origin, behavior and enrichment of environmental toxic elements from the Deokpyeong area were investigated on the basis of major, trace and rare earth element geochemistry. Coaly metapelites of the Deokpyeong area are subdivided into grey phyllite, dark grey phyllite, coaly slate and black slate, which are interbedded along the Ogcheon Supergroup. The coaly slate had been mined for coal, but mining is closed. The coaly and black slates are lower contents of $SiO_2$ and $Al_2O_3$, and higher contents of LOI, CaO, $Na_2O$ and BaO as compared with the phyllitic rocks. Rare earth elements are highly enriched in the coaly and black slate. Average compositions (ppm) of minor and/or environmental toxic elements in the coaly and black slate are revealed as As=127, Ba=30,163, Cd=18, Cr=740, Cu=84, Mo=378, Pb=43, Sb=12, Se=44, U=144, V=8,147 and Zn=292, which are extremely high concentrations than those in the NASC compositions. Major elements (average enrichment index; 5.34) in the coaly metapelites are mostly depleted, excepting $P_2O_5$ and BaO, normalized by NASC. Rare earth elements (average enrichment index; 1.48) are enriched in the coaly slate. On the basis of NASC, minor and/or environmental toxic elements in the coaly metapelites were strongly enriched of all the elements with the exception of Co, Cs, Ni and Sr. Average enrichment index of trace elements in coaly metapelite is 31.51 (coaly slate; 51.94 and black slate; 15.46). Especially, enrichment index of potentially toxic elements (As, Ba, Cr, Cu, Mo, Ni, Sb, Se, U, V and Zn) of the rock is 46.10 (grey phyllite; 7.15, dark grey phyllite; 4.77, coaly slate; 88.96 and black slate; 22.11). These coal formations were deposited in basin of boundary between terrestrial and marine environments deduced to carbon, sulfur (C/S=2.2 to 275.7), trace and rare earth elements characteristics. Irregular behavior and dispersion between major, minor and rare earth elements of those metapelites indicates a variable source materials, incomplete mixing of differential source and/or reequilibrium of diagenesis and metamorphism.

• 한국지하수토양환경학회지:지하수토양환경
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• 제12권6호
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• pp.107-117
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• 2007

남해-화개지역 하상퇴적토 환경유해원소들의 분산특성 및 환경유해성을 알아보고, 지구화학적 재해에 대해 예견하고자 한다. 하상퇴적토는 오염의 우려가 없고, 집수분지를 대표할 수 있는 시료를 채취하였다. XRD, XRF, ICP-AES, NAA를 이용하여 주성분원소 및 환경유해원소를 분석하였다. 산분해법은 1차로 $HClO_4$와 HF를 혼합하여 $200^{\circ}C$에서 분해시킨 후,2차로 $HClO_4$, HF, HCl를 혼합한 후 $200^{\circ}C$에서 분해시켜 이를 1% $HNO_3$ 용액으로 만들었다. 남해지역 환경유해원소의 함량은 Cu $5.66{\sim}168\;ppm$, Pb $18.0{\sim}40.7\;ppm$, Cr $21.6{\sim}147\;ppm$, Co $4.86{\sim}25.3\;ppm$ 범위이고, 화개지역에서는 Cu $16.4{\sim}41.2\;ppm$, Pb $26.5{\sim}37.5\;ppm$, Cr $79.6{\sim}153\;ppm$, Co $15.7{\sim}29.5\;ppm$ 범위를 보였다. 상관 분석에서는 하상퇴적토의 $SiO_2$ 함량이 높아질수록 구리(Cu)와 코발트(Co)의 함량이 감소하는 특징을 보였다. 연구지역의 E.I.는 비부화 되어 있으며, 평균값은 남해지역 0.35와 화개지역 0.56이였다. 조사대상 하상퇴적토들은 납 > 크롬 > 코발트 > 구리 순으로 부화되어 있으며, E.F.의 평균값은 $0.46{\sim}2.84$이다. E.F값은 구리와 코발트에서 거의 비슷한 부화특성을 보이나, 크롬에서는 남해지역보다 화개지역에서 보다 큰 부화특성을 보인다. 납은 연구지역 모두에서 상당히 부화되어 있었지만, 토양 및 퇴적물의 환경오염 허용 한계치(tolerable level)을 이용하여 살펴본 결과에서는 환경유해원소의 오염에 특별히 노출되지 않는 것으로 판단된다.

• 원예과학기술지
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• 제30권3호
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• pp.270-277
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• 2012

Greenhouse industry has been growing in many countries due to both the advantage of stable year-round crop production and increased demand for fresh vegetables. In greenhouse cultivation, $CO_2$ concentration plays an essential role in the photosynthesis process of crops. Continuous and accurate monitoring of $CO_2$ level in the greenhouse would improve profitability and reduce environmental impact, through optimum control of greenhouse $CO_2$ enrichment and efficient crop production, as compared with the conventional management practices without monitoring and control of $CO_2$ level. In this study, a mathematical model was developed to estimate the $CO_2$ emission from soil as affected by environmental factors in greenhouses. Among various model types evaluated, a linear regression model provided the best coefficient of determination. Selected predictor variables were solar radiation and relative humidity and exponential transformation of both. As a response variable in the model, the difference between $CO_2$ concentrations at the soil surface and 5-cm depth showed are latively strong relationship with the predictor variables. Segmented regression analysis showed that better models were obtained when the entire daily dataset was divided into segments of shorter time ranges, and best models were obtained for segmented data where more variability in solar radiation and humidity were present (i.e., after sun-rise, before sun-set) than other segments. To consider time delay in the response of $CO_2$ concentration, concept of time lag was implemented in the regression analysis. As a result, there was an improvement in the performance of the models as the coefficients of determination were 0.93 and 0.87 with segmented time frames for sun-rise and sun-set periods, respectively. Validation tests of the models to predict $CO_2$ emission from soil showed that the developed empirical model would be applicable to real-time monitoring and diagnosis of significant factors for $CO_2$ enrichment in a soil-based greenhouse.

• 한국식품위생안전성학회지
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• 제33권1호
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• pp.65-70
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• 2018

L. monocytogenes는 Listeriosis를 일으키는 중요한 식중독 균으로 현재 국내 식품공전에서는 증균배양을 기초로 검출하며, 규격은 불검출로 관리하고 있다. 그러나 Listeria종 간의 혼합오염시 증균 과정에서 경쟁생육이 존재하여 L. monocytogenes 위음성의 가능성이 있다고 보고되고 있다. 국내 식품공전은 L. monocytogenes 증균을 위한 1차 배지로 규정되어 있으나 LEB 배지에서의 Listeria 종 간의 생육 연구는 보고된 바 없다. 본 연구는 식품에서 주로 검출되는 Listeria 속 4종(L. monocytogenes, L. innocua, L. ivanovii, L. seeligeri)을 LEB배지에 혼합배양하며 증균과정에서 생육의 차이가 존재하는 것을 확인하였다. 특히, L. innocua에 의해 L. monocytogenes의 생육이 저해되며, L monocytogenes가 L. innocua보다 초기균수가 2.0 log CFU/mL 이상 오염이 되어있어야지만 L. innocua보다 생육이 잘 되는 것을 확인하였다. Listeria 종 간의 혼합오염이 있을 경우 현재 검출법으로는 L. monocytogenes의 검출이 어려울 수 있다고 판단된다. 따라서 L. monocytogenes 검출율을 높이는 새로운 증균배지 개발의 필요성을 확인하였다. 향후 본 연구는 L. monocytogenes 검출률을 높여 국내 식품의 식품 안전에 기여 할 수 있으며 국내 식품 관리 규격 개정 시 기초가 되는 참고 자료로 활용 할 수 있을 것으로 생각된다.

• ALGAE
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• 제35권4호
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• pp.375-388
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• 2020

Ocean acidification and warming, identified as environmental concerns likely to be affected by climate change, are crucial determinants of algal growth. The ichthyotoxic raphidophytes Chattonella species are responsible for huge economic losses and environmental impact worldwide. In this study, we investigated the impact of CO2 on the thermal performance curves (TPCs) of Chattonella marina and Chattonella ovata grown under temperatures ranging from 13 to 34℃ under ambient pCO2 (350 μatm) and elevated pCO2 (950 μatm). TPCs were comparable between the species or even between pCO2 levels. With the exception of the critical thermal minimum (CTmin) for C. ovata, CTmin for C. marina and the thermal optimum (Topt) and critical thermal maximum (CTmax) for both species did not change with elevation of pCO2 levels. While CO2 enrichment increased the maximum photosynthetic rates (Pmax) up to 125% at the Totp of 30℃, specific growth rates were not significantly different under elevated pCO2 for the two species. Overall, C. ovata is likely to benefit from climate change, potentially widening its range of thermal tolerance limit in highly acidic waters and contributing to prolonged phenology of future phytoplankton assemblages in coastal waters.