• 자원환경지질
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• 제25권3호
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• pp.337-349
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• 1992

The Tertiary basins in Korea have widely been studied by numerous researchers producing individual results in sedimentology, paleontology, stratigraphy, volcanic petrology and structural geology, but interdisciplinary studies, inter-basin analysis and basin-forming process have not been carried out yet. Major work of this study is to elucidate evidences obtained from different parts of a basin as well as different Tertiary basins (Pohang, Changgi, Eoil, Haseo and Ulsan basins) in order to build up the correlation between the basins, and an overall picture of the basin architecture and evolution in Korea. According to the paleontologic evidences the geologic age of the Pohang marine basin is dated to be late Lower Miocence to Middle Miocene, whereas other non-marine basins are older as being either Early Miocene or Oligocene(Lee, 1975, 1978: Bong, 1984: Chun, 1982: Choi et al., 1984: Yun et al., 1990: Yoon, 1982). However, detailed ages of the Tertiary sediments, and their correlations in a basin and between basins are still controversial, since the basins are separated from each other, sedimentary sequence is disturbed and intruded by voncanic rocks, and non-marine sediments are not fossiliferous to be correlated. Therefore, in this work radiometric, magnetostratigraphic, and biostratigraphic data was integrated for the refinement of chronostratigraphy and synopsis of stratigraphy of Tertiary basins of Korea. A total of 21 samples including 10 basaltic, 2 porphyritic, and 9 andesitic rocks from 4 basins were collected for the K-Ar dating of whole rock method. The obtained age can be grouped as follows: $14.8{\pm}0.4{\sim}15.2{\pm}0.4Ma$, $19.9{\pm}0.5{\sim}22.1{\pm}0.7Ma$, $18.0{\pm}1.1{\sim}20.4+0.5Ma$, and $14.6{\pm}0.7{\sim}21.1{\pm}0.5Ma$. Stratigraphically they mostly fall into the range of Lower Miocene to Mid Miocene. The oldest volcanic rock recorded is a basalt (911213-6) with the age of $22.05{\pm}0.67Ma$ near Sangjeong-ri in the Changgi (or Janggi) basin and presumed to be formed in the Early Miocene, when Changgi Conglomerate began to deposit. The youngest one (911214-9) is a basalt of $14.64{\pm}0.66Ma$ in the Haseo basin. This means the intrusive and extrusive rocks are not a product of sudden voncanic activity of short duration as previously accepted but of successive processes lasting relatively long period of 8 or 9 Ma. The radiometric age of the volcanic rocks is not randomly distributed but varies systematically with basins and localities. It becomes generlly younger to the south, namely from the Changgi basin to the Haseo basin. The rocks in the Changgi basin are dated to be from $19.92{\pm}0.47$ to $22.05{\pm}0.67Ma$. With exception of only one locality in the Geumgwangdong they all formed before 20 Ma B.P. The Eoil basalt by Tateiwa in the Eoil basin are dated to be from $20.44{\pm}0.47$ to $18.35{\pm}0.62Ma$ and they are younger than those in the Changgi basin by 2~4 Ma. Specifically, basaltic rocks in the sedimentary and voncanic sequences of the Eoil basin can be well compared to the sequence of associated sedimentary rocks. Generally they become younger to the stratigraphically upper part. Among the basin, the Haseo basin is characterized by the youngest volcanic rocks. The basalt (911214-7) which crops out in Jeongja-ri, Gangdong-myon, Ulsan-gun is $16.22{\pm}0.75Ma$ and the other one (911214-9) in coastal area, Jujon-dong, Ulsan is $14.64{\pm}0.66Ma$ old. The radiometric data are positively collaborated with the results of paleomagnetic study, pull-apart basin model and East Sea spreading theory. Especially, the successively changing age of Eoil basalts are in accordance with successively changing degree of rotation. In detail, following results are discussed. Firstly, the porphyritic rocks previously known as Cretaceous basement (911213-2, 911214-1) show the age of $43.73{\pm}1.05$ 및 $49.58{\pm}1.13Ma$(Eocene) confirms the results of Jin et al. (1988). This means sequential volcanic activity from Cretaceous up to Lower Tertiary. Secondly, intrusive andesitic rocks in the Pohang basin, which are dated to be $21.8{\pm}2.8Ma$ (Jin et al., 1988) are found out to be 15 Ma old in coincindence with the age of host strata of 16.5 Ma. Thirdly, The Quaternary basalt (911213-5 and 911213-6) of Tateiwa(1924) is not homogeneous regarding formation age and petrological characteristics. The basalt in the Changgi basin show the age of $19.92{\pm}0.47$ and $22.05{\pm}0.67$ (Miocene). The basalt (911213-8) in Sangjond-ri, which intruded Nultaeri Trachytic Tuff is dated to be $20.55{\pm}0.50Ma$, which means Changgi Group is older than this age. The Yeonil Basalt, which Tateiwa described as Quaternary one shows different age ranging from Lower Miocene to Upper Miocene(cf. Jin et al., 1988: sample no. 93-33: $10.20{\pm}0.30Ma$). Therefore, the Yeonil Quarterary basalt should be revised and divided into different geologic epochs. Fourthly, Yeonil basalt of Tateiwa (1926) in the Eoil basin is correlated to the Yeonil basalt in the Changgi basin. Yoon (1989) intergrated both basalts as Eoil basaltic andesitic volcanic rocks or Eoil basalt (Yoon et al., 1991), and placed uppermost unit of the Changgi Group. As mentioned above the so-called Quarternary basalt in the Eoil basin are not extruded or intruaed simultaneously, but differentiatedly (14 Ma~25 Ma) so that they can not be classified as one unit. Fifthly, the Yongdong-ri formation of the Pomgogri Group is intruded by the Eoil basalt (911214-3) of 18.35~0.62 Ma age. Therefore, the deposition of the Pomgogri Group is completed before this age. Referring petrological characteristics, occurences, paleomagnetic data, and relationship to other Eoil basalts, it is most provable that this basalt is younger than two others. That means the Pomgogri Group is underlain by the Changgi Group. Sixthly, mineral composition of the basalts and andesitic rocks from the 4 basins show different ground mass and phenocryst. In volcanic rocks in the Pohang basin, phenocrysts are pyroxene and a small amount of biotite. Those of the Changgi basin is predominant by Labradorite, in the Eoil by bytownite-anorthite and a small amount pyroxene.

• Journal of Animal Science and Technology
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• 제45권6호
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• pp.975-986
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• 2003

가을철에 태어난 한우 암송아지 36두를 방목전 . 후의 농후사료 급여수준에 따라 4개 처리(T1: 체중의 0.5%, T2: 체중의 1.0%, T3: 체중의 1.5%, T4 : 체중의 2.0%)를 두어 방목기 195일을 포함한 426일간 사양 시험한 결과를 요약하면 다음과 같다. 1) 전기간의 일당증체량은 T4, T3, T2 및 T1이 각각 0.501, 0.450, 0.403 및 0.348kg으로 방목전 . 후 사사기의 농후사료 급여수준이 증가할수록 높았으며, 방목기의 일당증체량은 방목전 육성기의 농후사료 급여수준이 체중의 1.0%일 때가 가장 높았다. 2) 공시기간 동안 kg 증체에 소요된 TDN량은 8.50${\sim}$8.70kg(평균 8.61kg)이었고, T3, T4, T1, 및 T2의 순으로 사료이용성이 높았으며, 방목기간의 kg 증체에 소요된 TDN량은 7.99${\sim}$10.96kg(평균 9.22kg)으로 방목전의 농후사료 급여수준이 증가할수록 높았다. 그리고 전기간동안 농후사료에 대한 조사료 비율은 49.6${\sim}$68.2%(평균 58.5%)이었다. 3) 체중 225kg에 도달되는 시기는 14.1${\sim}$16.1개월령(평균 15.1개월령), 그리고 체중 250kg에 도달되는 시기는 16.4${\sim}$19.0개월령(평균 17.6개월령)으로 사사기의 배합사료 급여수준이 체중 대비 0.5% 증가함에 따라 초임시기가 약 0.9개월씩 단축되었다. 첫 종부는 평균 19.5개월령, 272.2kg에 실시되었고 임신율은 52.8%였지만, 사사기 농후사료 급여수준이 1.5% 이상일 때는 임신율이 66.6%로 증가하였다. 이상과 같은 결과들을 종합해 볼 때 가을에 태어난 한우 암송아지를 축사에서 볏짚 위주로 사육할 때의 농후사료 급여수준은 체중의 1.8% 그리고 개량초지에서 방목사육 할 때에는 체중의 1.5%가 적정수준인 것으로 판단된다.

• 한국안광학회지
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• 제17권3호
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• pp.265-272
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• 2012

목적: 약도의 근시를 가진 아동과 중등도 이상의 근시를 가진 아동을 대상으로 역기하렌즈를 착용시키고 난 후의 근시교정효과를 비교하여 알아보고자 한다. 방법: 7세에서 15세 사이의 -2.00 D이하 근시안 19안(Group 1)과 -2.25 D이상에서 -4.00 D이하의 근시안 28안(Group 2), -4.25 D이상에서 근시안 15안(Group 3), 총 31명(62안)을 대상으로 역기하렌즈 착용 전, 착용 후 1주일, 1개월, 3개월, 6개월 후의 나안시력과 각막지형도상의 굴절력 변화를 근시의 정도에 따라 3그룹으로 나눠 교정효과를 알아보고 이에 대한 추적 결과의 통계적 유의성을 검증하고자 하였다. 결과: 역기하렌즈를 착용하고 난 후 Group 1은 착용 후 1주일에 시력이 0.45 에서 0.95 로 0.50 향상되었으며 1개월째 0.91, 3개월째 1.02 로 향상되었으나 6개월째 0.95 로 다시 감소하였다. Group 2는 착용 후 1주일에 시력이 0.34 에서 0.77 로 0.43 향상되었으며, 1개월째 0.91 로 증가되었으며, 3개월째 0.97 시력까지 향상되어 6개월까지 통계적으로 지속되었다. Group 3은 착용 후 1주일에 시력이 0.15 에서 0.70 로 0.55 향상되었으며, 1개월째 0.87, 3개월에는 0.91 로 향상되었으나 6개월째 0.86 으로 다시 감소되었다. 각막지형도상 평균 Sim K(simulated keratometry reading)값은 Group 1이 $42.84{\pm}1.17D$에서 착용 후 1주일에 $41.48{\pm}0.98D$로 감소하였으며 3개월까지 감소하다가 6개월에는 증가하였다. Group 2는 $42.91{\pm}1.57D$에서 착용 후 1주일에 $41.78{\pm}1.58D$로, 3개월까지는 감소하다가 6개월에 증가하였다. Group 3은 $42.64{\pm}1.64D$에서 $40.77{\pm}1.20D$로 착용 후 1주일에는 감소하였고 1개월 후에 다시 증가하였다가 3개월에 감소하여 6개월까지 감소하였다. 결론: 본 연구 결과 역기하렌즈의 착용 후 1주일부터 근시교정효과가 있었으며 근시정도에 따라 그 효과 발생 시기는 차이가 있었으나 모든 그룹에서 근시교정효과가 나타났음을 알 수 있었다.

• 한국환경과학회지
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• 제19권4호
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• pp.415-425
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• 2010

The purpose of the present study was to analyze the vegetation structure and distributional characteristics of Abies koreana forests in Mt. Halla, and to provide basicdata for an ecological study on Abies koreana in Mt. Halla. The results of the analysis showed that the mean importance percentage(M.I.P,) of Abies koreana in the Youngsil and Bangaeoreum and the Azalea field were 28.3%, 23.6%, and 46.4%, respectively. The ratios of DBH (diameter at breast height) to height were similar in all region, except in the Azalea field, where Abies koreana of various ages, both young and old, were found. The species diversity (H) of the upper and lower layers in the Youngsil and Bangaeoreum and in the Azalea field were 0.625 and 0.810, 0.731 and 0.848, and 0.342 and 0.757, respectively. A total of 52 community were distributed at locations higher than 1,300m above sea level. The proportions of each community in the whole Abies koreana forest were 56.5%(Azalea field), 11.0% (Youngsil trail at 1,550-1,650 m above sea level), and 8.1%(Janggumok and Kundurewat region). The total area of the Abies koreana forest was calculated to be 795.3ha by combining all the areas of each community. An Abies koreana forest with the largest area was found at locations 1,500-1,600 m above sea level, taking up 38.8% of the total Abies koreana forest area. For the slopes of the distributional area of Abies koreana, 46.1%(highest proportion) of the total area was $10\sim25^{\circ}$, and for the azimuth of the distributional area, 17.4%(the highest proportion) of the total area was $0-45^{\circ}$. The vegetation structure showed large differences between areas. It was found, however, that the distribution was mostly in the areas with a relatively gentle slope. It is suggested that research be done to forecast the possible changes in the differences in the vegetation structures between different areas caused by climate changes. In addition, there is a need to monitor the Abies koreana and alpine plants in the subalpine zones of Mt. Halla, which are sensitive to climate change, to obtain the basic data that are necessary for the protection and maintenance of the ecosystem.

• The Korean Journal of Physiology
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• 제8권2호
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• pp.19-31
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• 1974

In oder to study the correlation between daily urinary output of sodium chloride and blood pressure, twenty four hour urine samples were collected from 224 cases (70 male and 154 female) of healthy Koreans whose age varied from 18 to 70 years old. The volume and concentration of sodium, chloride and potassium and total nitrogen were measured, along with the resting blood pressure. Results obtained are summarized as follows; 1. Daily urinary output was increased as a function of age. However, daily urinary output per unit sulface area was maintained at approximately 800 to 900 $ml/m^2$ in all age groups of male and it increased as a function of age in female groups. There was no significant difference between male and female. 2. The daily urinary sodium concentration was decreased gradually acceding to age in both sexes. Daily excretion of sodium was constant regardless of age in both sexes but especially high in 25-39 year female age group, which was slightly greater in males than in females. 3. The daily urinary chloride concentration was at approximately 250 meq/L in all age groups of male and which decreased as a function of age in females. 4. Hence the daily urinary output of sodium chloride was constant in all age groups of males which increased as a function of age in female groups. However, daily excretion of sodium chloride per unit sulface area was maintained at approximately 11 $gm/m^2$ in males and which increased as a function of age in females. 5. The daily urinary excretion of potassium was constant regardless of age in both sexes. 6. Urinary K/Na ratio was maintained at approximately 0.27 in males and 0.33 in females. 7. The daily urinary output of total nitrogen amount was approximately $8{\sim}10$ gm in males and $7{\sim}9$ gm in females. However, daily urinary output of nitrogen per unit sulface area was constant regardless of age in both sexes. 8. The systolic blood pressure was increased gradually according to the age in both sexes and was higher for males than females under 40 years of age. However, there was no significant difference between both sexes in ages over 40 years. 9. Quantitative comparisons indicated that daily urinary output and sodium chloride excretion are higher while daily potassium output, nitrogen excretion and urinary K/Na ratio are significantly lower among Koreans than a among Occidentals. These findings suggest that average Koreans live on low-protein and high-salt diet throughout their livers. Statistical result obtained may he summarized as follows; 10. The relation between blood pressure and sodium concentration of urine. The correlation between systolic blood pressure and sodium concentration was negatively associated for both sexes and the correlation coefficient was significant for females $({\gamma}_1=-.19<-{\gamma}_{152},\;_{0.05}=-0.159)$ and it was not significant for males $({\gamma}_1=-.19>-{\gamma}_{68},\;_{0.05}=-0.232)$ tut may be due to the sample size for males. The correlation between diastolic blood Pressure and sodium concentration was negatively associated for both sexes and the correlation coefficient was significant for males $({\gamma}_1=-.37<-{\gamma}_{68},\;0.05=-0.232)$ and the relation was not significant for females $({\gamma}_1=-.11>-{\gamma}_{152},\;_{0.05}=-0.159)$. 11. The relation between blood pressure and daily urinary sodium chloride excretion. The association between systolic blood pressure and sodium chloride excretion was positively correlated for both sexes and the relation was significant for females $({\gamma}_1=.20>{\gamma}_{152},\;_{0.05}= 0.159)$ and it was insignificant for males $({\gamma}_1=.09<{\gamma}_{68},\;_{0.05}=0.232)$, The relation between diastolic blood pressure and sodium chloride excretion was positively associated and insignificant for both sexes males $({\gamma}_1=.17<{\gamma}_{68},\;_{0.05}=0.232)$ and females $({\gamma}_1=.09<{\gamma}_{152},\;_{0.05}=0. 159)$. 12. The relation between daily urinary nitrogen excretion and sodium chloride excretion. The association between daily nitrogen excretion and sodium chloride excretion was positively significant for both sexes, males $({\gamma}_1=.31>{\gamma}\;_{68},\;_{0.05}=0.232)$ and females $({\gamma}_1=.36>{\gamma}_{-152},\;_{0.05}=0.159)$.

• Journal of Nutrition and Health
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• 제13권1호
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• pp.27-36
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• 1980

A dietary survey of 100 children, aged 5 to 6, of Y.C. Kindergarten located in Yowido apartment compound of Seoul, was conducted July 18 to August 21, 1979. The results are summarized as follows: General family environment: Ninety four percent of the subjects were from families having two to three children, without grandparents in the home. One hundred percent of fathers were educated at or above the college level, while 83.9% of mothers had completed college. Mothers' ages ranged from 30 to 40 years, with 58% in the $31{\sim}35$ age bracket. Nearly 60% of the fathers were office and government employees, 10% were professors and teachers, 30% were engaged in businesses and other work, while 91.3% of mothers were unemployed. Anthropometric measurements: Mean values of standing height, body weight, girth of head and girth of chest, ranged from the 75th to the 90th percentile of Korean standards. None of the subjects had anthropometric indicators below the 5th percentile, representing the malnutrition borderline, of the Korean standards; while 12%, 24%, 17% and 14% of subjects supposed the 97th percentile in standing height, body weight, girth of head, and girth of chest, respectively. Furthermore, 58% of subjects exceeded Jelliffe's standard in arm circumferences; 60%, in triceps skinfold thickness; and 14.5% of subjects exceeded 120% of the latter standard. From this data, a certain number of these children were judged to he rather overweight. Dietary intake: Mean intake per day of energy and of nutrients, excluding iron, reached or exceeded Korean recommended dietary allowances. The energy input ratio of carbohydrate: protein: fat was 61.4 : 13.2 : 25.4, showing lower dependance on carbohydrates and higher dependance on fat for energy needs, compared with the average for Korean children of the same age group. Mean FAO-protein score of each subject's diet was shown to be as high as 90.6. Energy intake was divided among breakfast, lunch, and evening meal, on the average, in a ratio of 19.6 : 24.1 : 23.0. Approximately 33.3% of the daily caloric intake came from the snacks. Nutrition Knowledge of mothers: Nutrition knowledge of mothers was highly scored. Mothers' self-evaluations of their knowledge of nutrition was highly correlated with attitudes toward nutrition behavior.

• 한국산림과학회지
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• 제52권1호
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• pp.72-78
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• 1981

1979년(年) 8월(月) 25일(日) 태풍(颱風) Judy 호(号)의 영향으로 진해지구(鎭海地区)는 일강우량(日降雨量) 465mm의 집중호우(集中豪雨)로 많은 산사태(山沙汰)가 발생하여 38명(名)의 인명사망(人命死亡)과 가옥(家屋), 농경지(農耕地)에 막대한 재산피해(財産被害)를 냈다. 기왕(既往)의 조사(調査)에 의하면 일강우량(日降雨量) 300mm 이상(以上)일때 산사태발생(山沙汰発生)의 위험이 있다고 하였으나 진해지구(鎭海地区)는 과거 27년간(年間)에 일강우량(日降雨量) 300mm 이상(以上)이 5회(回) 있었음에도 불구하고 한번도 산사태(山沙汰)가 발생(発生)한 기록(記錄)이 없었다. 이것은 이 지구(地区)에 있어서 산사태발생(山沙汰発生)에 관계(関係)되는 각인자(各因子)(강우(降雨), 지질(地質), 지형(地形), 삼림(森林))의 과거(過去)와 현재(現在)의 질적변화(質的変化)에 기인(基因)한다고 생각됨으로 이들의 인자(因子)와 산사태발생(山沙汰発生)의 관계(関係)를 알기 위하여 조사(調査)한 결과(結果)는 다음과 같다. 1. 산사태개수(山沙汰個数)는 71개(個), 면적(面積)은 15.3ha 이다. 2. 지질(地質)에 있어서는 산사태개수중(山沙汰個数中) 안산암(安山岩) 및 화강암(花崗巖)에서 각각(各各) 89%, 11% 이며 면적(面積)은 안산암(安山岩) 및 화강암(花崗巖)에서 각각(各各) 45%, 55%가 발생하였다. 3. 경사(傾斜) $26^{\circ}{\sim}35^{\circ}$ 범위에서 산사태개수(山沙汰個数)는 44%, 면적(面積)은 55% 발생하여 가장 많고 9% 이하(以下) $41^{\circ}$ 이하(以下)에서는 발생하지 않았다. 사면형(斜面形)에서 보면 산사태개수(山沙汰個数)는 하강사면(下降斜面) 및 복합사면(複合斜面)에서 각각(各各) 52%, 46% 발생하여 타(他) 사면형(斜面形) 보다 많았다. 4. 임령(林令) 5~15년(年)에서 산사태개수(山沙汰個数)(2.19개(個)/100ha)및 면적(面積)(0.47ha/100ha)이 가장 많았고 임령(林令) 26년(年) 이상(以上)에서는 발생하지 않았다. 5. 산사태발생인자중(山沙汰発生因子中)(강우(降雨), 지질(地質), 지형(地形), 삼림(森林)) 인력(人力)으로서 그 형질(形質)을 변화(変化)시킬 수 있는 것은 삼림인자(森林因子)뿐이다. 5. 진해지구(鎭海地区)는 과거(過去) 많은 집중호우(集中豪雨)가 있었음에도 불구(不拘)하고 이번 처음 산사태(山沙汰)가 일어난 것은 과거와 현재의 삼림인자(森林因子)의 질적변화(質的変化)에 기인(起因)된다고 생각된다.

• Journal of Preventive Medicine and Public Health
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• 제27권3호
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• pp.447-463
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• 1994

Despite the public health importance of injury and poisoning in terms of its high mortality and incidence, epidemiologic information to be utilized are scarce in Korea. This study was carried out in 1990 on a representative sample population (about 55,000 persons) along with the 6th National Tuberculosis Prevalence Survey in order to estimate the magnitude of injury and poisoning occurrence and to identify its epidemiologic characteristics which can be aided for establishing preventive strategy. Pre-tested and structured Questionnaire was used by trained interviewer to collect data including general information of the person, various information on the injury and poisoning during the past one year such as time and place of its occurrence, its nature and external causes, type of medical institute attended, duration of treatment and outcome of the accident occured. In analysis of the data collected incidence rates per 1000 persons by sex, age group and its nature as well as external causes, and relative frequencies were calculated. The result obtained are as followings; 1. The incidence rate per 1000 was 30 for both sexes, 39 for male and 22 for female, male being 1.8 times more frequent than female. Age adjusted incidences were not much different from the crude rates. Age group specific rate curve showed bimodal shape in both sexes, small peaks in preschool children and higher peaks in older ages. The incidence rate per 1000 people by area was highest in Jeon-bug province (57/1000) and the lowest in Daegu city(11/1000). 2. The place where the injuries occured were road in 46%, within the boundary of house in 25%, and working place in 12% The injuries and poisoning had occured more frequently during the months from March to August of the year than other months. 3. The relatively frequent injuries by its nature were contusion with intact skin surface (19%), fracture of upper limb (13%), open wound of head, neck and trunk (12%) and fracture of lower limb (11%) among males; contusion with intact skin surface (28%), sprains and strains of joints and adjacent muscle (14%), fracture of upper limb (10%) and fracture of lower limb (9%) among females. Higher incidence rate among males than females were fracture of skull (4.5 times), open wound and fractures of limbs ($2{\sim}3$ times). Age specific rate of injuries and poisoning by its nature showed increasing pattern by age in fractures of upper and lower limbs and sprains & strains of joints whereas the age group of 30's showed highest incidence in open wounds of upper limb. Fractures of radius and ulna in upper limb, fractures of tibia & fibula and ankle in lower limb were most frequent among fractures of upper and lower limbs. The frequent injuries among sprains and strains of joints and adjacent muscles were that of ankle, foot and back, and among open wound were that of head and fingers. 4. Relative frequency of injuries and poisoning by external causes showed following order : other accidents (25%), accidental falls (23%), motor vehicle accident (22%) and other road vehicle accident (14%) among males and accidental falls (37%), motor vehicle accident (24%) and other accident (18%) among females. The external causes revealing higher incidences among males than females, were other road vehicle accident (4.8 times), vehicle accident not elsewhere classifiable (4.4 times), accidental poisoning (4.4 times), accidents due to natural and environmental factors (2.8 times), and sucide & self-inflicted injuries (2.8 times). Age specific incidence by external causes for frequent injuries showed that incidence of other accident steadily increased from 10's till age 50's; motor vehicle traffic accident increased from age 20's and dropped after age 60's; on the other hand accidental fall increased strikingly by age. The most frequent external causes among motor vehicle traffic accidents was motor vehicle traffic accident involving collision with pedstrain (69%), pedal cycle accident (30%) and other road vehicle accident (71%) among other road vehicle accidents; falls on same level from slipping, tripping or standing (44%) and other falls from one level to another among accidental falls; accidents caused by machinary (32%) for male and striking against or struck accidentally by objects or person for female among other accidents. 5. Seventy nine percent of the injuries and poisonings were treated in general hospital or hospital/clinic. The duration of treatment ranged from a few days to 123 weeks; the majority(52%) took under 2 weeks, 36% for $3{\sim}8$ weeks and 4% over 21 weeks. 6. The accident resulted in full recovery of normal healthy state in 62%, residual functional defects in 21% and on process of treatment in 16%.

• 환경정책연구
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• 제11권3호
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• pp.25-47
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• 2012

송이생산을 고려한 소나무비오톱유형화 및 지도 작성을 통한 송이생산지의 생태적 관리방안을 제시하고자 하였다. 연구대상지는 동서고속도로 신설구간 중 송이가 다량 생산되는 양양군구간을 대상으로 도로노선중앙에서 좌우 700m씩 범위내 총 $19.79km^2$을 설정하였다. 연구의 내용은 4단계로 구분하였으며 첫째, 양양군 송이관련특성, 둘째, 송이관련 선행연구 고찰, 셋째, 송이생산을 고려한 소나무비오톱유형화 기준 및 프로세스 정립, 넷째, 송이생산을 고려한 소나무비오톱지도화 등이다. 송이생산에 적합한 경사도 $30{\sim}40^{\circ}C$ 지역은 24.77%, 남향계열은 17.44%이었고 식생구조는 소나무군락 26.00%, 평균수령, $38{\pm}8.34$ 년생, 교목층 평균식생밀도 $9.55{\pm}4.98$ 주/$100m^2$ 등으로 송이생산에 최적 식생구조였다. 토양산도(pH)는 5.0~5.6(47.96%) > 5.6~7.0(42.90%) > 4.0~5.0(9.14%)로서 송이발생에 적합한 약산성 토양인 pH 4.0~5.6의 면적은 57.10%였다. A0층의 깊이는 평균 $3.39{\pm}2.14cm$이며 4~6cm(78.03%) > 0~2cm(18.10%) > 2~4cm(3.87%)였다. 선행연구와 현장조사 결과를 바탕으로 현존식생(소나무우점비율), 지형(지형특성 및 경사도), 수령, 토양특성(토양산도와 A0층 깊이), 식생밀도를 유형화 기준으로 설정하여 총 6개 송이생산을 고려한 소나무비오톱유형으로 구분하였다. 유형별 분포면적은 송이생산잠재(II)소나무비오톱유형(32.86%) > 송이생산 부적합 소나무비오톱유형(22.17%) > 송이생산적합(II)소나무비오톱유형(17.79%) > 송이생산적합(I)소나무비오톱유형(14.86%) > 송이생산잠재(I)소나무비오톱유형(9.77%) > 송이생산소나무비오톱유형(2.55%) 등의 순이었다.

• 대한핵의학회지
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• 제36권3호
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• pp.166-176
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• 2002

목적: 이 연구의 목적은 시각 활성 자극에 의한 뇌 활성영역을 확인하고 국소 뇌 혈류량을 정량적으로 분석하는데 그 목적이 있다. $^8F-fluoro-2-deoxy\;glucose\;(FDG)\;PET$과 $^{15}O-water\;PET$에서 시각 자극을 가하는 동안 시각피질에서의 기전이 확인되었으며 PET에 비해 적은 비용으로 널리 사용되고 있는 $^{99m}Tc-HMPAO$ Brain SPECT를 이용하여 시각자극을 주었을 때 대뇌 후두엽의 일차시각피질과 시각 연합 피질에서의 국소 뇌 혈류 변화율을 정량적으로 분석하고자 하였다. 대상 및 방법: 오른손을 주로 사용하는 25세에서 33세의 나이 분포를 갖는 남자 3, 여자 3명(평균나이 26.7세)의 정상인을 대상으로 $^{99m}Tc-HMPAO$ Brain SPECT (925 MBq)를 시행하였고 8 Hz의 발광다이오드를 이용하여 $4{\sim}5$분 동안 시각활성 자극을 주었을 때와 대조군으로 자극을 가하지 않은 비 활성상태에서의 경우로 나누어 스캔하고 해부학적 기준정보를 제공하기 위해 MR 영상과 융합하였으며 관심영역을 설정하여 혈류량을 정량적으로 분석하였다. 결과: 정량적인 분석을 위해 대뇌의 전체 용적과 계수율을 계산하고 관심 영역을 설정하여 관심영역에 대한 복셀 당 평균 계수율을 측정하여 각 대상의 시각 활성자극을 가한 영상에서 정상 상태의 영상을 픽셀 당 픽셀로 감산하여 통계적 파라미터를 이용한 뇌 지도를 구성하였으며 뇌 활성이 Brodmann 영역의 시각피질(Ba 17)과 시각연합피질(Ba 18,19)에서 활성화되어 있음을 Talairach 좌표를 통해 확인하였고 regional index를 계산하여 국소 뇌혈류 변화율을 측정하였다. 결론: $^{99m}Tc-HMPAO$ Brain SPECT에서 8 Hz의 발광 다이오드로 시각 자극을 주었을 때 후두엽의 일차 시각피질과 시각 연합 피질에서 뇌 활성화를 확인하였고 통계적 파라미터를 이용한 SPM99에서 뇌 지도를 작성하여 시각자극에 의한 활성영역을 Talairach 좌표와 Brodmann 분류에 의해 확인하여 T1 강조 MR 영상에 융합하였다. 후두엽의 일차시각피질에서 시각 활성자극에 의해 국소 뇌 혈류량이 $32.50{\pm}5.67%$ 증가하고 있음을 정량적으로 분석하였다.