• Title/Summary/Keyword: Jangsu Area

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The Research for Relationships between Concentration of Indoor Radon and Distribution of Soil Geological Map using GIS : Based on the Hwacheon and Jangsu Areas (지리정보시스템(GIS)을 이용한 토양지질도 분포와 실내라돈 상관성 연구 : 화천 및 장수의 사례를 근거로)

  • Kwon, Myunghee;Lee, Jaewon;Kim, Seongmi;Lee, Jungsub;Jung, Joonsig;Yoo, Juhee;Lee, Kyusun;Song, Suckhwan
    • Journal of Korean Society of Occupational and Environmental Hygiene
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    • v.27 no.4
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    • pp.333-351
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    • 2017
  • Objectives: This study examines the relationships between indoor radon concentrations and distribution from soil geological mapping in the Hwacheon and Jangsu areas. Methods: GIS and a pivot table were used for inquiries about indoor radon contents, soil characteristics, and geological differences. Results: The Hwacheon area was characterized by the presence of normal and reverse faults as a passage of runoff for radon, sufficient occurrences of minerals containing uranium within granite as a radon source, a high concentration of radon within the granite area and clear differences of radon concentrations between granitic and metamorphic areas. The Jangsu area was characterized by the presence of normal faults, wide distributions of alluvium, and ambiguities on radon concentrations indoors among areas of geological differences. Considering the granite area and alluvium surrounded with granite areas, the characteristics of radon concentrations within soils and indoors in the Jangsu area are similar to those of the Hwacheon area. High concentrations are found with entisol and inceptisol in the Hawcheon area, but with entisol, inceptisol, and ultisol in the Jangsu area. High radon concentrations are found in sandy loam and/or loam. High concentrations are found in recently constructed or brick buildings, but low concentrations in traditional or prefabricated houses showing a high possibility of outward flow. Conclusions: The overall results suggest that radon concentrations in the Hwacheon and Jangsu area are dominantly influenced by geological characteristics with additional artificial influences.

Quality Characteristics of Baechu Kimchi at Jangsu Area as Compared with Commercial Kimchi (장수지역 배추김치와 시판 배추김치의 품질 평가)

  • Lee, Young-Sook;Cha, Jin-A;Rho, Jeong-Ok
    • Journal of the East Asian Society of Dietary Life
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    • v.23 no.4
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    • pp.413-422
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    • 2013
  • This study investigates the kimchi from Jangsu area (JSK) and its comparison with commercial kimchi (CMK). We conducted a sensory evaluation for the pH, titratable acidity, salinity, hunter's color values and mechanical characteristics of kimchi. The pH of JSK is significantly higher than CMK throughout the fermentation (p<0.001). At 15 days, JSK reached the stage of optimal maturity for pH 4.23~4.55 and CMK showed pH 3.96~4.00 as conditions after the optimal maturity (p<0.001). From the results of acidity analyses, CMK also showed higher acidity values than JSK (p<0.001), indicating that the rate of fermentation progress was faster in CMK. Salinity of JSK was a litter higher than CMK1 and CMK2 (p<0.001) and JSK indicated significantly higher L, a, b values during fermentation (p<0.001). Moreover, the textural values were significantly higher in JSK2 and JSK3 retaining hardness of the tissues. In the sensory assessment, the color, flavor, crispness, taste, and overall preferences were higher in JSK3 at 15 days and 30 days than CMK. Therefore, it seems necessary for recipe developments of kimchi with local characteristics in order to industrialize kimchi by using alpine crops at Jangsu area.

A GIS-based Analysis for Suitable Site of Chisandra chinensis Cultivation - Focused on Jangsu County forest - (GIS 기반 오미자 재배적지 분석 - 장수군 산림을 대상으로-)

  • Kim, Hyun;Kim, Hyun-Jun;Choi, Soo-Min;Lee, Sang-Hyun
    • Journal of agriculture & life science
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    • v.45 no.1
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    • pp.41-47
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    • 2011
  • This study that is to increase forest income with Omija (Chisandra chinensis) was conducted to analyse the status of production of Omija and the suitable site of cultivation in Jangsu-gun forest using GIS Omija production was increased by 297.2% with 3,786,237 kg in 2009, compared with in 2007. Of this figure, the most amount of Omija production was producted with 2,013,379 kg (53.2%) in Gyeongsangbuk-do Production of Jeollabuk-do was the third most amount in the whole country with 407,210 kg (10.8%). Of this figure, the most amount of Omija production was producted with 131,000 kg (32.2%) in Jangsu-gun. On the other hand, the cultivated area of Omija in Jangsu-gun was 159.0ha in 2008, and of this fugure, Jangsu-eup had 48.8 ha (30.7%) which was the most amount of the clutivated area of Omija. The suitable site of cultivation for Omija in Jangsu-gun analysed by using GIS was 1,199 ha, moreover, the suitable site of cultivation for Omija by eup and myeon was 304 ha (25.4%) in Cheoncheon-myeon, 272 ha (22.7%) in Jangsu-eup, 172 ha (14.3%) in Gyenam-myeon, 158ha (13.2%) in Beonam-myeon, 135 ha (11.3%) in Janggye-myeon, 129 ha (10.8%) in Gyebuk-myeon, and 29 ha (2.4%) in Sanseo-myeon, respectively. It was thought that investment should be made efficiently and effectively by considering the result of this study to increase forest income with Omija in Jangsu-gun.

Geochemistry of the Gneisses in the Jangsu Area, Jeonbuk, Korea (전북 장수지역에 분포하는 편마암류의 지구화학적 연구)

  • Son, Jeong-Mo;Shin, In-Hyun;Ahn, Kun-Sang
    • Journal of Integrative Natural Science
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    • v.4 no.1
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    • pp.58-71
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    • 2011
  • The precambrian gneisses are widely distributed in the Jangsu area. This study focuses on the metamorphic mineral assemblages and metamorphic P-T conditions of the gneiss. We have analyzed garnet, biotite and plagioclase among the gneiss through the EPMA analysis, and calculated the metamorphic temperature and pressure accordingly. The metamorphic temperature was estimated by the average of values from the garnet and biotite formulas, and the metamorphic pressure by value of the Hoisch(1990) geopressured on garnet-biotite-plagioclase. The mineral sample we examined shows garnet-biotite-plagioclase-quartz composite and garnet-plagioclase-orthoclase-quartz composite. Garnet shows almandine-pyrope solid solution in general, while porphyroblastic gneiss shows almandine-grossluar solid solution. The fact that the abundances, observed by garnet profile, are almost identical in both the central region and the outer egion indicates that the crystal was developed uniformly. There is almost negligible variance in biotite on metamorphic grade, and andesine is observed in plagioclase. The metamorphic temperature and pressure from EPMA analysis and its indications are as follows: the middle-temperature, high-pressure metamorphism ($500-650^{\circ}C$, 6.9-10 kbar) ensued in the beginning, and then was followed by the high-temperature, middle-pressure($600-740^{\circ}C$, 2.7-5.9 kbar) to ($500-540^{\circ}C$, 3.1 kbar) retrograde metamorphism.

Impacts of Temperature Rising on Changing of Cultivation Area of Apple in Korea (한국에서 기온상승이 사과 재배지역의 변화에 미치는 영향)

  • Kim, Sun-Young;Heo, In-Hye;Lee, Seung-Ho
    • Journal of the Korean association of regional geographers
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    • v.16 no.3
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    • pp.201-215
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    • 2010
  • This paper aimed to analyze the impact of temperature rising on the change of cultivation area and yields of apple. This study used apple data from statistical year book and climate data from Daegu, Uiseong, and Jangsu weather station. It was investigated whether temperature rising have had significant impact on apple. In the 1970s, the apple grew mostly in the southern part of Gyeongsangbuk-do between regions in and around Daegu and Gyeongsan. Recently, the cultivation area and yields of apple were concentrated on northern part of Gyeongsangbuk-do between regions in and around Uiseong and Mungyeong. The mean temperature from April to October is good in Uiseong and Jangsu. But the mean temperature from April to October is higher than optimal condition in Daegu. It means that temperature rising have a bad influence in apple cultivation. The daily temperature range is decreasing in Daegu and Jangsu, but it is increasing in Uiseong.

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Intrusive Phases and Igneous Pricesses in the Yeongju Batholith (영주저반의 관입상과 화성과정)

  • 황상구
    • Economic and Environmental Geology
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    • v.32 no.6
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    • pp.669-688
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    • 1999
  • The Yeongju granitoid batholith is a plutonic complex of huge area (1180km2) intruding the metamorphic rocks of the Yeongnam massif. The batholith, which is divided into fivelithofacies, consists of three separate plutons. The oldest Buseok pluton comprises four lithofacies: hornblende biotite tonalite, porphyrotoc biotite granodiorite, equigranular biotite grandiorite and biotite granite. The middle Chunyang pluton has been called as Chunyang granite that ranges in compostion from granodiorite to granite. The youngest Jangsu pluton is intrusions that has lithofacies of two mica granite. The contact between Buseok pluton and the rest two plutons shows obvious intrusive relations, but relation between the Chunyang and the Jangsu pluton is far away, so gives no indication of relative ages. Changes in nextures and micristructures, as well as in the mineral contents, take place between rock types og the plutons. only the Buseok pluton shows faliations of two type: magmatic foliation and regional mylonal foliation. K-Ar age deteminations fall into 171.7$\pm$3.2~162.3$\pm$3.1 Ma in the Buseok pluton, 153.9$\pm$2.9 Ma in the Chunyang pluton and 145.3$\pm$2.7 Ma in the jangsu Pluton. The batholith presents three separate intrusive phases which range in composition from tonalite to granite to granite. Each intrusive phase apperars to have been intruded in a pulse from an underlying, differentiating magma. The petrochemical data showthat three plutons are within the diagnostic range for continental arc orogenic tectonic setting, whereas Jangsu pluton approaches postorogenic setting. The data suggest that three plutons are calc-aclkalline series, and that temporal compositional variations change progerssively from tonalite through grandiorite to granite between the intrusive phases. so we consider that the magmas for all the phases were probably derived from a differentiation by fractional crystallization of a parental magma. The tonalite magma of the Buseok phase was tapped was tapped from a chamber deep in the crust, and then would have to rise at a rapid rate to its final level of emplacement. The tonalite magma in the chamber was gradually enolved through granodiorite magma into granite magma by fractional crystallization. The magmas of the younger phases were respectively tapped with temporal interval from a evolved magma of the chamber that rose into a shallower lever in the crust, and rose to their present level of emplacement.

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Characteristics of Habitat-using of Siberian Roe Deer in Seoraksan(Mt.) National Park (설악산국립공원 지역의 노루 서식지 이용 특성에 관한 연구)

  • Park, Yong-Su;Lee, Woo-Shin
    • Journal of the Korean Society of Environmental Restoration Technology
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    • v.17 no.1
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    • pp.91-109
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    • 2014
  • This study was conducted to obtain the basic research about Siberian roe deer (Capreolus pygargus), and to establish a conservation area into Seoraksan(Mt.) National Park, South Korea. We recorded Siberian roe deer field signs (bedding sites, feeding areas, feces and tracks etc), and habitat variables such as nearest distance to the watercourse, trails, slope, aspect, forest type and land cover etc. from Jan. 2006 to Dec. 2007 in Seoraksan(Mt.) National Park. According to the research of habitat characteristics of Siberian roe deer inhabited in Seoraksan(Mt.) National Park preferred mixed forest consisted of aged forest and middle-aged forest on the gentle slope which was close to hydrosphere in the middle elevation area of altitude of 400~600m above sea level in Seoraksan(Mt.) National Park. The results indicated that Siberian roe deer appeared to prefer south slope or north slope during the snow season and west or east slope during the non-snow season. The area of most suitable habitat for Siberian roe deer in Seoraksan(Mt.) National Park was $128.5km^2$ (32% of the total area) followed by $244.3km^2$ buffer area (62.2% of the total area), and $22.9km^2$ unsuitable habitat area (5.8% of the total area), which means environmentally unsuitable habitat for Siberian roe deer was rare in Seoraksan(Mt.) National Park. Thus, the area classified as major area in Seoraksan(Mt.) National Park appeared to be most important for the protection of Siberian roe deer.

A Survey on the Soil Environments of Alpine Vegetable Housing in Honam Area (호남지역(湖南地域) 고냉채소단지(高冷菜蔬團地)의 토양환경연구(土壤環境硏究))

  • Yoo, Chul-Hyun;Cho, Guk-Hyun;Choi, Jeong-Weon;Park, Keon-Ho
    • Korean Journal of Soil Science and Fertilizer
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    • v.21 no.3
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    • pp.246-253
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    • 1988
  • This survey was carried out to obtain the basic information for the stable high yield of income-crops. Cropping systems, soil morphological and chemical properties were investigated. The obtained results were summarized as follows: 1. In Jinan and Jangsu, cultivated area of radish was 76.5% and.65.4%, respecitively, but in Unbong Chinese Cabbage, 71.1%, by second Crop. 2. In topographycal distribution, the mountain foot slope area in Jinan, Jangsu and Unbong was 69, 77 and 85%, respectively. In the distribution of elevation, semi-Alpine region in Jinan and Unbong was 85 and 69%, respectively, but Alpine region in Jangsu was 62%, of cultivated area. 3. Ploughing depth was 0 to 10 cm in Jinan and Jangsu, and 11 to 15cm, in Unbong. Gravel content class was 4th class in Jinan and 3rd class in Jangsu and Unbong. 4. For the distribution of soil types, normal upland came to 69.2% in Unbong, sandy and skeletal upland, 46.1 % and normal and sandy upland, 39 and 38%, respectively, in Jangsu. 5. The uplands soil classified as the 5th class, with improper for adequate cropping were. 6. For the chemical properties according to topography available phosphate $(-0.344^*)$, Ca $(-0.398^*)$, K $(-0.485^{**})$ and CEC $(-0.325^{**})$ showed the negative significancy with the elevation. 7. Among the variations of chemical properties by continuous cropping, the soil pH $(-0.491^{**})$ and the content of organic matter $(-0.434^{**})$, Ca $(-0.705^{**})$, CEC $(-0.512^{**})$, total nitrogen $(-0.559^{**})$ showed the high negative correlations, while the contents of available phosphate $(0.671^{**})$ and K $(0.543^{**})$ showed the high positive correlations, with the number of years of continuous cropping.

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Dominant Species and Factors Related with Plant Coverage in the Cutting Slopes of Forest Road -In Jeollabuk-do Region­- (임도 절토비탈면의 우점식물과 식물피복에 미치는 인자들의 영향 -­전라북도를 대상으로­-)

  • Park, Moon-Su
    • Journal of the Korean Society of Environmental Restoration Technology
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    • v.5 no.1
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    • pp.19-27
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    • 2002
  • To investigate the dominant species and factors related with plant coverage by road structures and forest environment factors, forest roads elapsed from one year to twelve year after construction had been selected in six county(Gochang-gun, Muju-gun, Imsil-gun, Jangsu-gun, Jeongup-shi and Jinan-gun), and 20m segments were continuously set up in each road. The results obtained from this study are summarized as follows: The species diversity of Gochang, Muju, Imsil, Jangsu, Jeongup and Jinan were 1.304, 1.267, 1.308, 1.193, 1.289 and 1.018, respectively. In process of years, plant coverage was increased gradually and average of plant coverage was 15.3% in forest roads which elapsed three year, and was 86.5% in forest roads which elapsed nine year after construction. The dominant species in the cutting slope of surveyed area were covered with Arundinella hirta, Pinus rigida, Miscanthus sinensis var. purpurascens, Artemisia princeps var. orientalis, Pinus densiflora, Oplismenus undulatifolius, Rubus coreanus, Lysimachia clethroides, Lespedeza bicolor, and Alnus hirsuta of the 152 species. The high correlated factors between plant coverage and variables in cutting slopes appeared elapsed year, soil hardness, mean annual precipitation, vertical grade, inslope and arid humidity in surveyed area.