• Korean Journal of Environmental Agriculture
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• v.22 no.1
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• pp.7-15
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• 2003

The characteristic of the quality of stream water and the riparian vegetation during rice cultivation in the rural area of the eastern Jeonnam province was surveyed from April to November, 2000. The water quality of the streams during rice cultivation was variable. The pH of these water bodies ranged from $6.5{\sim}8.3$. Electro conductivity (EC) at each water body ranged from $162{\sim}4,910\;{\mu}S/cm$ for Beogyo-cheoa $114.7{\sim}286.6\;{\mu}g/cm$ for Boseong-cheon, $74.8{\sim}147\;{\mu}S/cm$ for Songgwang-cheon, and $61.6{\sim}82.1\;{\mu}S/cm$ for Isa-cheon. Total nitrogen and other parameters (K, Ca, Mg, Na, $Cl^-$, SS) were higher at May (Boseong-cheon) through June (Songgwang-cheon, Isa-cheon) during the transplanting season than these same parameters at August October and November. Thirty weed species of sixteen families were found in the survey areas of Songgwang-cheon, Boseong-cheon Isa-cheon and Beolgyo-cheon. Nine annual weeds, four biennial weeds, and seventeen perennial weeds were found, several different life forms were identified. Of those species three were submerged, two were free floating, five were emerged, and twenty were water-side weeds.

• Korean Journal of Environmental Biology
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• v.26 no.4
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• pp.392-401
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• 2008

The vertical changes (upper layer: 0$\sim$0.5 m, middle layer: 4$\sim$5 m and lower layer: 8$\sim$10 m) of the limnological variables, zooplankton dynamics and community filtration rate on the phytoplankton were evaluated monthly intervals from November 2004 to June 2007 at the artificiallake (Okjeong Lake). During the study, the annual mean of water temperatures were 15.2$\pm$7.8$^{\circ}C$ (upper layer), 14.5$\pm$7.4$^{\circ}C$ (middle layer) and 13.0$\pm$6.2$^{\circ}C$ (lower layer), respectively (n=30). The vertical variations of most limnological parameters (DO, pH, conductivity and turbidity) were fairly similar, except for chl.-${\alpha}$ concentration. Annual mean of chl.-${\alpha}$ concentration was highest at the upper layer (21.4 ${\mu}g$ L$^{-1}$), while annual means of concentrations were low at the middle layer and lower layer (4.3 ${\mu}g$ L$^{-1}$ and 3.5 ${\mu}g$ L$^{-1}$, respectively). Annual mean of Secchi depth was 261 cm (n=30). A total 45 species of zooplankton were identified (28 rotifers, 12 cladocerans and 5 copepods) during the study. The mean abundance of rotifers was highest (124$\pm$232 ind. L$^{-1}$, n =90) and that of cladocerans and copepods were relatively low (22$\pm$56 ind. L$^{-1}$ and 13$\pm$30 ind. L$^{-1}$) in the whole layer. Total zooplankton abundance increased from late spring to summer, and then declined and remained low throughout the winter. The annual mean of total zooplankton filtration rate for phytoplankton at the lower layer was much higher than that of both layers (upper layer: 44.4$\pm$107.8, middle layer: 95.1$\pm$436.4 and lower layer: 158.2$\pm$436.4 mL L$^{-1}$ day$^{-1}$). Among the major zooplankton community, relative community filtration rate (RCFR, %) of copepods for phytoplankton (50.2$\sim$54.8%) was much higher than that of cladocerans (27.7$\sim$36.3%) and rotifers (8$\sim$17.6%). The seasonal variation of RCFRs of major zooplankton community was observed. The RCFRs of rotifers were high in winter (44.6%, n=9), while the RCFRs of cladocerans were high in summer (58.0%, n=7). In spring and fall, the RCFRs of copepods were high in the whole layer (spring: 67.4%, n=9; fall: 74.4%, n=5).

• Proceedings of the Korean Aquaculture Society Conference
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• 2003.10a
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• pp.143-144
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• 2003

봄철 해역에 따른 부착미세조류의 영양성분 변화를 알아보기 위하여 본 실험을 수행하였다. 실험은 울진, 부안, 완도, 부산 지역에서 봄철인 2~4월 동안 실시되었으며 실험간의 오차를 줄이기 위해 실험 시작일의 차이는 최대 10일 이내로 하였다. 배양을 위한 실험해역의 기초 조사로 배양지역 연안해수의 수온, 염분, pH, 총질소, 총인, Chlorophyll-a의 측정을 하였고 각 지역의 부착미세조류를 수확하여 영양분석을 하였다. 실험에 사용된 파판은 전복 종묘생산에 이용되는 규조배양용 파판과 틀을 이용하였고 실험기간은 총 8주 동안 실시하였다. 2주마다 파판을 수거한 뒤 부착된 미세조류를 부드러운 솔로 분리하여 원심 분리한 후 지방산과 아미노산의 측정을 하였다. 또 각 시료의 일정량을 Sedwick-rafter counting chamber를 이용하여 검경ㆍ계수한 후 이를 단위면적당 개체수(cells/$\textrm{cm}^2$)로 환산하여 biomass를 구하였다. 봄철 지역간의 수온의 범위는 13.9~16.6$^{\circ}C$를 보였으며 울진이 가장 높고 부안지역이 가장 낮았다. 염분은 부안지역의 염분이 평균 2$\textperthousand$ 이상 낮았으며 그 외의 지역은 큰 차이가 없었다. pH는 7.77~8.21의 범위를 보이고 있었으며 질산염 농토는 부산이 0.265mg/$\ell$로 최대값을 보였고 울진이 0.032mg/$\ell$로 제일 낮았다. 인산염 농도는 완도지역이 0.018mg/$\ell$로 최대치를 보였고 부안은 검출되지 않았다. Chlorophyll-a의 농도는 울진지역이 0.66mg/$\ell$으로 제일 낮았으며 부산이 2.69mg/$\ell$, 부안지역이 2.27mg/$\ell$ 로 높은 값을 보였다. 봄철 지역에 따른 부착미세조류의 아미노산 분석결과는 울진이 실험지역 중 제일 높은 총 아미노산과 필수아미노산의 함량을 나타냈으며 각 지역별로 울진은 4주에 20.3%, 부안은 8주째 8.1%, 완도는 8주째 4.7%, 부산은 6주째 10.4%로 서로다른 시기에 높은 아미노산의 함량을 나타냈다. 실험지역 부착미세조류의 지방산 결과를 보면 전 실험기간동안 지방산 중 대부분은 $C_{18}$이하의 포화 또는 불포화 지방산이 주를 이루고 있었으며 palmitic acid( $C_{16:0}$)와 palmitoleic acid( $C_{16:0}$)의 양이 전체 지방산 함량중 37.47~75.94%로 대부분을 차지하고 있었다. 그리고 n-3HUFA(high unsaturated fat쇼 acids)인 EPA는 부안지역이 2주째 20.85%로 전체 지역중 함량이 제일 높았고, 울진은 실험기간중 6주가 14.76%로 제일 높은 함량을 보였다. 완도는 6주에만 10.97%의 함량을 보였으며 부산지역의 시료에서는 EPA의 검출이 없었다. 봄철 각지역에 설치된 파판에서의 부착미세조류 출현량을 보면 2주째의 부착미세조류량은 부안이 8.3$\times$$10^3$ cells/$\textrm{cm}^2$로 가장 높았고 부산이 0.6$\times$$10^3$ cells/$\textrm{cm}^2$로 가장 낮았다. 울진의 경우 0.7$\times$$10^3$ cells/$\textrm{cm}^2$로 부산과 비슷하게 낮은 출현량을 보였고 완도는 2.4$\times$$10^3$ cells/$\textrm{cm}^2$였다. 4주째의 출현량은 울진지역이 471.1$\times$$10^3$ cells/$\textrm{cm}^2$로 가장 높았으며 부안, 완도, 부산 순으로 출현량이 낮았고 특히 부산은 1.2$\times$$10^3$ cells/$\textrm{cm}^2$로 가장 낮았다. 6주째의 출현량은 울진 지역이 368.6$\times$$10^3$ cells/$\textrm{cm}^2$로 가장 높았으며 부안 89.8$\times$$10^3$ cells/$\textrm{cm}^2$, 완도 25.1$\times$$10^3$ cells/$\textrm{cm}^2$, 부산 5.9$\times$$10^3$ cells/$\textrm{cm}^2$ 순이었다. 8주째의 경우에도 울진, 부안, 완도, 부산이 각각 255.8$\times$$10^3$ cells/$\textrm{cm}^2$, 157.8$\times$$10^3$ cells/$\textrm{cm}^2$, 44.3$\times$$10^3$ cells/$\textrm{cm}^2$, 1.1$\times$$10^3$ cells/$\textrm{cm}^2$로 4주, 6주의 경우와 같은 경향을 보였다.보였다.

• Food Science and Preservation
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• v.16 no.6
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• pp.946-952
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• 2009

We investigated the physicochemical properties and antioxidant activities of green tea with respect to extraction conditions. The values of pH, and the L, a, and b Hunter parameters of green tea beverage 1 (GTB 1), green tea beverage 2 (GTB 2), and commercial green tea beverage (CGTB) were 6.22, 96.91, -1.06, and 7.77 5.40, 96.39, -1.73, and 13.68 and 6.20, 95.40, -4.75, and 25.51, respectively. The total free amino acid content of GTB 1 and 2, and CGTB, were 253.21, 262.65, and 58.36 mg/100 mL, and the major free amino acids were aminoadipic acid (102.56, 136.29, and 27.02 mg/100 mL), arginine (23.32, 30.75, and 7.31 mg/100 mL), and serine (18.22, 17.96, and 5.94 mg/100 mL). The levels of total phenolics and caffeine were higher in GTB 2 (852.58 and $225.51\;{\mu}g/mL$) than in GTB 1 (500.65 and $317.34\;{\mu}g/mL$) or CGTB (387.14 and $164.53\;{\mu}g/mL$). The catechin content of GTBs 1 and 2, and CGTB, were 294.8, 415.7, and $130.99\;{\mu}g/mL$, respectively. The major catechins of GTB 1 and 2, and CGTB were epigallocatechin, catechin, and epigallocatechin gallate, in that order, and the epigallocatechin contents were 186.50 in GTB 1, 268.10 in GTB 2, and $82.26\;{\mu}g/mL$ in CGTB. GTB 1 and 2 and CGTB showed substantial dose-dependent antioxidative activities. The DPPH radical-scavenging activities of GTB 1 and 2, and CGTB, were 85.48, 87.09, and 87.03%, respectively at a concentration of $125\;{\mu}g/mL$. The ferric reducing/antioxidant activities (FRAPs) of GTB 1 and 2 and CGTB were 2.66, 2.70 and 2.67 absorbance at a concentration of $1,000\;{\mu}g/mL$. Sensory evaluation tests revealed no significant differences among the three green tea beverages.

• Journal of Animal Science and Technology
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• v.49 no.5
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• pp.611-620
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• 2007

The current study was designed to define whether a blend of prunus mume extract(25%) containing lactic acid(75%) and grape seed extract(10ppm) could affect in vitro antimicrobial activity and growth performance, intestinal microflora, plasma biochemical profiles and digestive enzymes activities in broiler chickens. In paper disc agar diffusion test, we clearly observed antimicrobial activity against E. coli in response to prunus mume extract or a blend of prunus mume extract. For in vivo test, a total of ninety six 3-d-old male broiler chicks were assigned to basal diet(CON), basal diet supplemented with antibiotics (ANTI) and 0.5% a blend of prunus mume extract(PRNUS) until 35 days of age. Throughout the entire experimental period(3-35 days), there were no differences in BW and FCR between the birds fed the basal diet with antibiotics and the diet supplemented with a blend of prunus mume. However, ANTI group showed a significant increase in BW and total gain compared to CON group. The weights of digestive organs such as the pancreas and mucosal tissues were not affected by dietary treatments. There was no difference in plasma levels of glucose, cholesterol, AST and ALT activity. However, triglyceride in plasma increased(P<0.05) in the birds fed the diet supplemented with 0.5% a blend of prunus mume extract compared to those fed antibiotics supplemented diet. The activities of pancreatic trypsin and amylase, and intestinal hydrolase including disaccharidase were not affected by dietary treatment. The colony forming units(CFU) of lactobacillus in the lower ileal-cecum of the birds fed the diet supplemented with a blend of prunus mume extract was significantly(P<0.05) higher than that of birds fed antibiotic supplemented diet without affecting the CFU of E. coli. In conclusion, the birds fed the diet supplemented a blend of prunus mume as an alternative to antibiotics showed a similar growth performance and an significant increase in lactobacillus population compared with the birds fed basal and antibiotics supplemented diets.

• Applied Microscopy
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• v.39 no.4
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• pp.333-340
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• 2009

In the present study, ultrastructural features of the mesophyll tissue have been investigated in Crassulacean acid metabolism (CAM)-performing succulent Orostachys. A large central vacuole and numerous small vacuoles in the peripheral cytoplasm were characterized at the subcellular level in both developing and mature mesophyll cells. The most notable feature was the invagination of vacuolar membranes into the secondary vacuoles or multivesicular bodies. In many cases, tens of single, membrane-bound secondary vacuoles of various sizes were found to be formed within the central vacuole. multivesicular bodies containing numerous small vesicles were also distributed in the cytoplasm but were better developed within the central vacuole. Occasionally, electron-dense prevacuolar compartments, directly attached to structures appearing to be small vacuoles, were also detected in the cytoplasm. One or more huge central vacuoles were frequently observed in cells undergoing differentiation and maturation. Consistent with the known occurrence of morphologically distinct vacuoles within different tissues, two types of vacuoles, one representing lytic vacuoles and the other, most likely protein storage vacuoles, were noted frequently within Orostachys mesophyll. The two types coexisted in mature vegetative cells but did not merge during the study. Nevertheless, the coexistence of two distinct vacuole types in maturing cells implies the presence of more than one mechanism for vacuolar solute sorting in these species. The vacuolar membrane is known to be unique among the intracellular compartments for having different channels and/or pumps to maintain its function. In CAM plants, the vacuole is a very important organelle that regulates malic acid diurnal fluctuation to a large extent. The membrane invagination seen in Orostachys mesophyll likely plays a significant role in survival under the physiological drought conditions in which these Orostachys occur; by increasing to such a large vacuolar volume, the mesophyll cells are able to retain enormous amounts of acid when needed. Furthermore, the mesophyll cells are able to attain their large sizes with less energy expenditure in order to regulate the large degree of diurnal fluctuation of organic acid that occurs within the vacuoles of Orostachys.

• Korean Journal of Soil Science and Fertilizer
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• v.45 no.3
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• pp.444-450
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• 2012

The physical and chemical properties of soil in the Mangyeong and Dongjin river basin had been investigated in order to establish the most optimum soil improvement plan on the reclaimed land. The total soil area by reclamation in Saemangeum basin is 113,971 ha. The classification by the distribution of soil series and soil texture is as following. 13 soil series including Chonnam, Buyong and Chonbuk series are period-unknown areas. Regarding the soil texture, they are fine silty ~ clayey very fine. From 1920s to 1960s, Mangyeong, Gwanghwal and Chonbuk series had coarse silty textured soil. After the 1970s, Mangyeong, Gwanghwal, Munpo, Yeompo, Poseung, Gapo and Hasa series have more sandy soil ~ moderately coarse loamy textured soil. Regarding the chemical properties, the concentrations of EC, Exch. $K^+$, $Mg^{2+}$, $Na^+$ and pH are high regardless of the time of reclamation. On the other hand, organic matter (OM) of top soil were 3.3~16.1 g $kg^{-1}$. The organic matter contents were very low though the soil had been farmed for a long time. Furthermore, the deep soil had almost no organic matter with 5.6~1.1 g $kg^{-1}$. The reason is believed that there had not been any movement of OM and clay because pressure or induced pans had been formed by large agricultural machineries and poor vertical drain. Regarding the forming of illuvial horizon (B layer) which tells the development extent of soil, only in the Hwapo reclaimed area where rice had been cultivated for past 90 years, Fe and Mn from top soil are deposited at underground 20~30 cm with 7~8 cm thickness by the movement of clay. It is believed that it had been possible because the earthiness is silty clay loam soil with relatively high content of clay. The soils are soil with concern of damage from sea water, soil on flimsy ground and sandy soil. Therefore, soil improvement for stable crop production can be expected; if the water table would be lowered by subsurface drainage, the water permeability would be enhanced by gypsum and organic matter, and the sandy soil would be replaced by red soil with high content of clay.

• The Korean Journal of Pesticide Science
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• v.16 no.1
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• pp.1-10
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• 2012

Fungicidal activities against phytopathogenic fungi of diarylthiazole compound of 4-[5-(2-cyclopropylaminopyrimidin-4-yl)-4-(4-fluorophenyl)thiazol-5-yl]-1-methylpiperidine (I) have been determined to be excellent and compound I was used as the leading compounds in this study. Furthermore, the compound was synthesized by reacting them with five functional groups, 4-fluoro-3-methylphenyl, 4-fluoro-3-chlorophenyl, 4-chloro-2-fluorophenyl, 4-bromo-3-methylphenyl and 2,4-dichlorophenyl groups instead of 4-fluorophenyl group. Also, 2-amino-, 2-(N-ethoxycarbonyl)piperidin-4-yl-, and 2-piperidin-4-yl-thiazole were introduced as the leads instead of 2-N-methylpiperidine-4-yl-thiazol of compound I. VIII-1~VIII-5 and XIII-1~XV-5 compounds were newly synthesized and their structures were confirmed by $^1H$-NMR-spectrum. The fungicidal activities of all the synthesized compounds against Phytophthora capsici were examined using the whole plant method. Among the VIII-1~VIII-5 and XIII-1~XV-5 chemicals, XIV-3 showed the most potent antifungal activity in vivo. While the $EC_{50}$ and $EC_{90}$ values of the commercial fungicide dimethomorph and I were $4.26{\pm}0.02$, $14.72{\pm}0.05$ and $1.01{\pm}0.11$, $6.31{\pm}0.09mM$, those of 4-[5-(2-cyclopropylaminopyrimidin-4-yl)-4-(4-chloro-2-fluorophenyl)thiazol-5-yl]-1-methylpiperidine (XIV-3) was $0.98{\pm}0.21$ and $5.85{\pm}0.05mM$. Therefore, XIV-3 can be considered as a viable candidate for the control of plant diseases caused by P. capsici, and further studies will be conducted on the mode of action XIV-3.

• Korean Journal of Soil Science and Fertilizer
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• v.24 no.2
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• pp.86-94
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• 1991

Volcanic ash soils were classified as Andepts, a suborder of the Inceptisols in Soil Taxonomy. Increased knowledge on the volcanic ash soils necessitated and facilitated considerable improvement in this system. As a result, the new Order of Andisols was incorporated in the 1990 edition of the Keys to Soil Taxonomy. The central concept of an Andisol is that of a soil developing in volcanic ejecta, and/or in volcaniclastic materials, whose colloidal fractions are dominated by short-range-order minerals or Al-humus complexes. Andic propertis of volcanic ash soil in Cheju Island were investigated. For this study, soils of toposequence distributed along the southern slope of Mt. Halla, and the major soil groups such as dark brown soils, very dark brown soils, black soils, and brown forest soils were collected and analyzed for Al, Fe and Si extracted with solutions of pyrophosphate, dithionite-citrate. and oxalate respectively. Weolpyeong and Yongheung soils developed on the lower elevations contain only small amounts of allophane and Al-and Fe-humus complexes. For other soils, allophane content decrease with elevation and increaes with soil depth,whereas Al-humus complexes increase with elevation and decrease with soil depth. Substantial amount of allophane and ferrihydrite are found in all horizons of Ora and Ara soils developed on 150-300m elevations and of Noro and Jeogag soils developed on cinder cones. In the A horizons of Pyeongdae, Tosan and Heugag soils developed on the higher elevations, Al-humus complexes are dominant form of Al reflecting low pH and high organic matter content. However, lower horizons are dominated by allophane.

• Journal of Korean Society of Environmental Engineers
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• v.22 no.2
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• pp.279-289
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• 2000

The objective of this study was to investigate the effect of coagulants and solid-liquid separation methods on algal removal in water treatment processes. Thus characterization of raw water quality in terms of turbidity. UV-254, $KMnO_4$ consumption, chlorophyll-a and correlation analysis of these parameters were conducted. In addition, the effect of commercial Al-based coagulants(Alum. PAC and PACS) on algal removal was studied by turbidity and organic removal, algal species removal, characteristic of pH drop and alkalinity consumption using laboratory jar tests. Organic components including UV-254, $KMnO_4$ consumption, chlorophyll-a in case of algal bloom were highly correlated with turbidity and the correlation coefficients of UV-254, $KMnO_4$ consumption, chlorophyll-a with turbidity were 0.775, 0674 and 0.623, respectively. In coagulation and sedimentation, the Al-based coagulants showed similar efficiency of organic and turbidity removal in low organic($KMnO_4$ consumption below 15mg/l) and low turbidity(below 30NTU). However, PAC and PACS showed better algal removal than alum in high organic concentration($KMnO_4$ consumption above 20mg/l) and high turbidity(above 100NTU) raw water conditions generated by high algal growth, which is considered to be due to the floc settleability. In comparison of sedimentation and flotation after chemical coagulation and flocculation, the removal efficiency of organic and turbidity were higher in case of alum dose with flotation than with sedimentation, while those were better in case or PAC and PACS with sedimentation than with flotation. Thus, Alum with flotation and PAC and PACS with sedimentation is recommended for efficient algal removal. The dominant phytoplankton in raw water were Microcystic and pediastrum simplex and the removal efficiency of algae with sedimentation using alum. PAC and PACS were 27%, 45% and 22% respectively, while those with DAF showed 100% removal of phytoplankton and zooplankton.