• 제목/요약/키워드: burial age

검색결과 48건 처리시간 0.024초

개인 특성별 자연장 인식과 이용의도 간의 구조적 관계 (Structural Relationship among Personal Characteristics, Perception and Use Intention of Natural Burial)

  • 김철재
    • 한국조경학회지
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    • 제45권4호
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    • pp.45-53
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    • 2017
  • 최근 자연장에 대한 국민들이 관심과 호감이 커져가고 있지만, 이에 반해 자연장 선택하는 국민은 별로 많지 않다. 본 연구의 개인의 특성, 자연장에 대한 인식 요인, 그리고 자연장 이용의도 간에 구조적 관계를 실증적으로 분석하여 자연장 이용을 활성화할 수 있는 필요한 정보를 제공하는 데 있다. 이를 위해 대전에 거주하는 학생과 주민 430명을 대상으로 설문조사를 실시하였다. 본 연구의 결과는 다음과 같다. 첫째, 설문응답자의 연령과 종교별로 자연장 이용의도에 유의적인 차이가 있었다. 연령에서는 20대가, 종교에서는 천주교 신자의 자연장 이용의도가 가장 높게 나왔다. 둘째, '자연장 정보'에서는 연령별, 종교별로, '종교와 철학'은 연령별, '물리환경'에서는 성별, 연령별로, '보존성'에서는 성별, 연령별에서 유의적인 차이가 있었다. 전체적으로 보면 연령이 낮을수록 자연장 인식이 더 긍정적으로 나왔고, 성별의 경우, '물리환경'에서는 여자가 남자보다, '보존성'에서는 남자가 여자보다 더 긍정적으로 생각하였다. 셋째, 자연장 인식의 하위 변인인 자연장 정보, 장법, 종교와 철학, 물리환경, 보전성 모두 자연장 이용의도에 유의적인 정(+)의 영향력이 있었다. 오즈비(odds ratio)를 보면, 종교와 철학, 장법, 물리환경, 보존성, 자연장 정보의 순으로 자연장 이용의도에 미치는 영향이 큰 것으로 나타났다.

한국 방향주구묘의 일고찰 (A Study of Square-shaped moated burial precincts in Korea)

  • 이원광
    • 헤리티지:역사와 과학
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    • 제33권
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    • pp.36-67
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    • 2000
  • Square-shaped moated burial precincts(方形周溝墓) can be classified into type I that has bridges only at the comers, type II that has bridges at the comers and sides, type III that has bridges only at the sides, type IV that is surrounded by the moat without bridges, type V that has its sides less than those of type I ~ V by 1 or 2, and type VI that has the round-shaped ground. But the time differences among the types are not known yet. For the burial appliances of square-shaped moated burial precincts, there are stone coffins, pit burials and jar burials. The major burial appliances situated in the mound are stone coffins and pit burials, and jar burials are subsidiary appliances that were buried at the shoulder part of the mound or at precincts. According to the case of Gwanchang-ri KM423, grave mounds, which arc closely related with the burial appliances, were built by heaping up the earth in and around the precinct as low as only enough to protect the burial appliances. Considering the relics unearthed in the burial compartment of KM437, the time when square-shaped moated burial precincts were formed is estimated to be the age when Songguk-ri type earthenware and clay stripes earthenware co-existed. It was the early Iron Age when ironware began to sp read in this country. Emerging first in that age, square-shaped moated burial precincts were presumably formed until around the end of BC or the beginning of AD, when KM404 and KM423, which were unearthed with plain earthenware, grey earthenware and ironware, were formed. When analyzing the form of small-sized graveyards in precincts, the unearthed relics and the locations, the people who formed square-shaped moated burial precincts were considered as those who had a culture comprising clay stripes earthenware, which appears newly in the Songguk-ri type earthenware of native, and ironware, and a settled agricultural society based on paddy fields and labor forces of family units.

대청도 지두리 해안의 모래 퇴적층의 특성과 매몰연대에 대한 연구 (A Study on the Characteristics and Burial Ages of Sediment Deposits at Jiduri, Daecheong Island)

  • 김종연
    • 한국지형학회지
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    • 제25권1호
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    • pp.1-17
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    • 2018
  • The characteristics and burial ages of sand sediments on the Jiduri coast in Daechung-myeon, Ongjin-gun, Incheon were investigated. Daecheong Island is the area where the characteristics of the rocky coast and sand coast are shown. Various studies have been conducted on the Okjukdong sand dune that appears in the north of the island. However, there has been no study on the sandy sedimentary topography of the Jiduri and Moraewul area in the south. The sandy sedimentary terrain of Jiduri is divided into sandy beaches, sand dunes and sand deposits along the slope including climbing dune. Overall, the depth of sandy sediments in Jiduri is not deep. The characteristics of sandy sediments and burial ages were investigated at an elevation of about 23 m above sea level at the back of Jiduli Beach and 46 m above sea level at the ridge line between Jiduri and Moraewol. From the Jiduri coast to the hillside behind, the average grain size decreases and the sorting becomes better as it moves from the intertidal zone to the beach and the foredune. This indicates the selective sand transport by the wind and can be judged by the terrain formed under the current sedimentation environment. The average grain size at the upper part of the section of JD-1 (elevation of about 23m MSL) was $1.6918{\varphi}$ of medium sand. The sorting was $0.4584{\varphi}$, skewness was -1.0491 and kurtosis was -1.2411, respectively. Particularly, the average particle size of the crosssection issomewhat uniform, but the color of the constituent material changes from brown to black. In the case of JD-2 (about 46 m MSL), the mean grain size of the section was $1.7943{\varphi}$, the sorting was 0.4931, the skewness was -1.1163, and the kurtosis was 1.2133. On the other hand, the brown and black layers of JD-1 exhibited a burial age of $0.1{\pm}0.0ka$ and the JD-2 had a burial age of $0.7{\pm}0.0ka$.

해남 북평면 퇴적층의 특성과 매몰 연대에 대한 연구 (A Study on the Characteristics and Burial Age of Sediment Layers at Bukpyeong myeon, Haenam gun)

  • 신원정;양동윤;김종연
    • 한국지형학회지
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    • 제23권3호
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    • pp.41-55
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    • 2016
  • The granulometric characteristics and chemical composition of the samples from the Bukpyeong myeon, Hainam gun, Jeollanam do were analyzed in this study. The samples were collected from the outcrop of coastal area where the height is about 30m. The burial age of the sediments also estimated by OSL(Optically Stimulated Luminescence) method. The origin and forming processes of the samples are not clear in this stage as limited number of evidences can be found. However it is suggested that the samples are not aeolian deposits originated from chinese loess by the chemical analysis. The mean diameter of samples were $5{\sim}6{\varphi}(silt)$ and are increased slightly downwards. The samples also well sorted. The samples have been heavily weathered by the chemical alteration index. The value of CIA increase downward rapidly at the upper part of outcrop, then stabilized afterwards. The vertical concentration changes ratio of cations varies; Si increases downwards while Fe, Ti, K and Mg decrease. There are fluctuation in concentration ratio of Na and Ca with increasing depth. The burial age of sample from upper part are estimated as $104.52{\pm}4.45ka\;BP$, while that of lower part are $136.10{\pm}6.52ka\;BP$, and they fall in to last part of MS6. The deposition rate for this site is found about 0.017mm/year. The uplift rate of the site is supposed to be 0.24~0.26m/ka with assumption of palaeo-sea level of +6m. However the origin of the sediment deposits should be explored and cleared.

"정조국장도감의궤"를 중심으로 한 염습의대 고찰 (Study on Burial Dressing of King based on "Jeong-jo Gukjang Dogam Euigwe")

  • 고영
    • 복식
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    • 제61권5호
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    • pp.147-163
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    • 2011
  • King Jeong-jo (正祖) was the 22nd king of Joseon dynasty (朝鮮王朝), who led the golden age of Korean culture during his ruling. This study is on the burial dressing of King Jeong-jo based on the publications during his ruling; such as "Gukjo Sangrye Bopyeon (國朝喪禮補編)", "Chungwan Tonggo (春官通考)", Jeong-jo "Gukjang Dogam Euigwe (國葬都監儀軌)", "Jeongjo Binjeon Honjeon Dogam Euigwe (正祖殯殿魂殿都監儀軌)" and "Jeong-jo Sillok (正祖實錄)", "Gukjo Sangrye Bopyeon (國朝喪禮補編)" was published in 1758. It compiled the funeral protocols of royal court, complementing the shortcomings of protocol documents published till then. "Chungwan Tonggo" was published in 1788, compiling all the protocols and customs practiced during Joseon dynasty in an organized manner. "Jeong-jo Gukjang Dogam Euigwe" and "Jeongjo Binjeon Honjeon Dogam Euigwe", record the burial dressing and the state funeral of King Jeong-jo in detail based on the contents of above protocol publications. In addition, the 'Daeryeom Euidae ', 'Soryeom Euidae', 'Seup Euidae' and 'Mokyok Euidae' that had been actually practiced were studied in detail based on the records in June/July, 1800 in Book 54 'Jeong-jo' of The Annals of the Joseon Dynasty. The timing of King Jeong-jo's state funeral was when the most elaborated and complete protocol books of Joseon dynasty had been published. Therefore, it was possible to explore the solemn and magnificent funeral culture and King's burial dressing in late Joseon dynasty by way of King Jeong-jo's burial dressing.

광승리 연안의 연안범람기원퇴적층 형성과 변화 과정에 대한 연구 - 퇴적물의 매몰연대와 화학분석을 기반으로 - (A Study on the Forming and Evolution of Coastal Flood Origin Deposits at Gwangseungri Coast - Based on Burial Age and Chemical Analysis -)

  • 신원정;양동윤;김종연
    • 한국지형학회지
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    • 제25권3호
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    • pp.71-87
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    • 2018
  • As part of further study on Gwangseungri coastal deposits which occurred at 10 ~ 15m above sea level and was analyzed as palaeo-coastal flood-type sediments, six burial ages of six additional samples from the two cross sections (KST1 and, KST2) near to the points of the past study were estimated and the geochemical analysis was performed. Further investigation on the cross section KST1 revealed a reversal of the burial age at the bottom of the section which was identified as palaeo-flooding sediments and supposed to have been buried about 350 years ago. At the lower part of the KST1, the burial age of the sediment layer was estimated to be 3,800 years. The lower part of KST2 sediments was identified as sediments that was formed about 6,600 years ago and about 20,000 years ago. Considering the inclination of the sediment layers, the coastal flooding sedimentsreported to have formed 700 years ago in the previousstudy are located at the top and the KST1 section analyzed in thisstudy seemed to be connected to the lower part. The chemical analysis showed that the relationship between these layers was not continuous but had a discontinuous characteristic influenced by a specific event, and the chemical composition also showed a rapid change. If we judge these together, the lowest part of Gwangseungrisediment layerseemed to have formed during the last glacial period but it was hard to find its origins clearly. On top of this layer, a fine sediment layer containing gravels was also formed.Itseemed thatsedimentation did not occur continuously, but was affected by temporary events in such a way that after a sediment layer was formed, it stopped. Since then, a coastal flooding event occurred about 700 years ago, and part of flooded sediments accumulated in the rear slope. After that, when a flood layer including additional granular materials about 350 years ago was formed, sedimentation along the slope seemed to have occurred.

네스티드로짓모형을 활용한 사회경제적 특성에 따른 장사유형 선호 분석 (A Analysis on Preference of Funeral Type by Socioeconomic Characteristics using Nested Logit Model)

  • 주호상;최열
    • 대한토목학회논문집
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    • 제39권6호
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    • pp.933-943
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    • 2019
  • 본 연구의 목적은 사회경제적 특성에 따른 장사유형 선호의 결정요인을 도출하는 것이다. 우리나라는 '장사 등에 관한 법률'에 의하여 장사유형은 매장, 봉안, 자연장으로 구분하고 있다. 본 연구는 사람들이 3가지 장사유형을 선택함에 있어 그들이 가진 어떠한 사회경제적 특성이 영향을 미치는지 실증분석하였다. 이를 위하여 2017년 사회조사 자료와 전국의 장사시설 자료를 수집하였다. 그리고 매장과 화장을 상위 계층으로 하고, 화장의 하위 계층에 봉안과 자연장이 반영된 위계 구조를 구성하여 분석용 자료를 구축하였다. 구축된 자료를 바탕으로 네스티드로짓모형을 활용한 실증분석을 실시하였다. 실증분석 결과, 장사유형의 선호에 통계적으로 유의한 영향을 미치는 사회경제적 특성은 성별, 연령, 가구주 여부, 혼인상태, 전반적인 생활에 대한 만족도, 사회경제적 지위에 대한 계층의식, 월평균 가구소득, 주택 유형, 주택 점유형태, 도시 거주 여부로 추정되었다. 네스티드로짓모형의 결과는 직접 탄력성과 교차 탄력성을 산출하여 변수별 탄력성 계수를 근거로 해석하여야 한다. 따라서 본 연구는 통계적으로 유의한 변수들의 직접 탄력성 및 교차 탄력성 계수를 산출하였다. 산출한 직접 탄력성은 통계적으로 유의한 변수가 변화할 때, 각 장사유형의 선택 확률을 해석하는데 활용하였다. 그리고 교차 탄력성은 특정 장사유형을 선택하는 경우, 나머지 장사유형을 선택하는 확률이 어떻게 변화하는지 해석하는데 활용하였다. 실증분석 결과 중 주목해야하는 점은 자연장과 관련된 사항이다. 자연장에 대한 수요를 충족하기 위한 자연장지의 공급을 활성화하고, 자연장에 대한 인식 제고를 위한 노력을 기울일 필요가 있다. 이를 통하여 국토 공간을 효율적으로 이용하여야 할 것이다.

한반도 남동부 해안 해성단구의 분류와 편년에 있어서 본 연구에서 도출된 OSL 연대 적용의 한계성 검토 (The Examination of the Limitations of Using the OSL Dates Derived from this Study in the Correlation of MIS 5 Marine Terraces Distributed in the Southeastern Coast of the Korean Peninsula)

  • 최성길;타무라 토시카즈;미야우치 타카히로;츠카모토 스미코
    • 한국지형학회지
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    • 제25권4호
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    • pp.63-75
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    • 2018
  • The lower marine terrace 1 and 2 surfaces distributed between Ulsan and Pohang coast in the southeastern coast of the Korean penninsula have been correlated with MIS 5e and 5a (or 5c) by amino acid dates, 14C dates, wide-spread tephra correlation and pollen analysis respectively. In this study, to test the reliability of the OSL method for the estimation of the numerical burial age of marine sediment deposits, we analyzed the samples from the marine terraces which have been known as typical marine terraces formed during MIS 5e and MIS 5a in the above-mentioned coast. The burial ages of the marine deposit of the lower marine terrace 1 and 2, with paleoshoreline altitudes of 18m to 19m and 10m to 11m respectively, both showed about the same age of 60 ka BP. The lower marine terraces 1 and 2, however, were divided into two terrace surfaces by a clear terrace cliff. Besides, the OSL dates of the lower and upper parts of the lower marine terrace 2 of the Bonggil coast showed the reversed burial ages. In the lower marine terrace 1 of the Sanhari coast, almost the same burial ages were derived from both the lower part (marine rounded gravel layer) and the upper part (terrestrial angular gravel layer) of the terrace deposit. Therefore, at the present time, judging from only the OSL dates measured in this study, it could be argued that the OSL method is not the best for the estimation of forming periods of the lower marine terraces 1 and 2 and their classification.

영광군 백수읍 하사리 일대의 사질 퇴적층 특성과 매몰 연대에 대한 연구 (A Study on Characteristics and Burial Ages of Sand Deposits at Hasari, Baeksoo, Yeonggwang)

  • 신원정;양동윤;김종연
    • 한국지형학회지
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    • 제24권1호
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    • pp.25-38
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    • 2017
  • To investigate the characteristics of sand sediment topography in the Yeonggwang coastal area of Chonnam and to collect evidence of the past extreme events causing coastal flooding, three sites were surveyed among the sediments of Baeksoo-eup Hassari. In this study, the changes of particle characteristics, chemical composition, and the age of deposition of sediments were investigated. The sediments near Baeksoonam Elementary School at the elevation of 10m near the paleo-coastline are estimated to have been deposited at about 3,400 years ago and the grain size of the upper part of the sandy layer is in the range of $2.47-2.11{\varphi}$. The burial age of the sediment layer at Sadeung junction(BSN-B) was about 100 years. Considering the distance from the current coastline, the sands forming the dune are estimated to have been moved or deposited from the nearby area or the other dune on the front side. The mean grain size is observed to be fining upward. Especially, the mean of the upper part is about $2.3{\varphi}$, which is similar to other survey points. The averaged grain size of the lower part of the BSNC (Hasari-1 Gu) was $2.196{\varphi}$ and the upper part was $2.16{\varphi}$. The sorting showed that the upper part was slightly poorer than the lower, and it was difficult to specify the change of the environment. The burial age of the lower layer, which contains shells, was about 300 years. Considering previous studies, this shell layer is presumed to have formed by coastal flooding, such as a storm surge.

낙동강 남부지역의 상례문화 실태 조사 - 부산의 교사집단을 중심으로 - (Customary Funeral Rites of Teachers in the Southern Nak-dong River Area)

  • 이기숙
    • 가정과삶의질연구
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    • 제22권5호
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    • pp.133-147
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    • 2004
  • Korean funeral customs are an important part of the mourning process in Korea. A survey was conducted in the southern part by the Nak-dong river, centered around the city of Busan to examine Korean funeral rites. This study was conducted with survey research. The target population included 234 teachers and experienced the death of a family member within the last three years. Results showed that they presented their condolences 5 to 6 times on average per year. Funeral rites were performed usually at a hospital funeral hall. The preference of burial to cremation was about the same. According to the survey, funeral expenses averaged 9,570,000 won and donations received for funeral expenses, 12,630,000 won. Problems the respondents expressed about the process included large funeral expenses, the decision whether to bury or cremate, and fatigue from staying up all night. When classified according to the demographic characteristics, there were significant differences in the variables. Frequency of attending funerals depended on gender, age, and health status. Condolence style depended on religion. The type of funeral (burial or cremation) depended on family income. The type of reception depended on gender. Funeral expenses depended on the age Second, in the process of preparing for a family member's death, they thought it was important to prepare a funeral ceremony portrait of the deceased and a scroll by themselves, and the preparation