대청도 지두리 해안의 모래 퇴적층의 특성과 매몰연대에 대한 연구
A Study on the Characteristics and Burial Ages of Sediment Deposits at Jiduri, Daecheong Island
0
조회
0
다운로드
4
인용
0
참고문헌
키워드
초록
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 1.6918φ of medium sand. The sorting was 0.4584φ, skewness was -1.0491 and kurtosis was -1.2411, respectively. Particularly, the average particle size of the cross section is somewhat 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 1.7943φ, 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 ± 0.0 ka and the JD-2 had a burial age of 0.7 ± 0.0 ka.
Abstract
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 1.6918φ of medium sand. The sorting was 0.4584φ, skewness was -1.0491 and kurtosis was -1.2411, respectively. Particularly, the average particle size of the cross section is somewhat 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 1.7943φ, 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 ± 0.0 ka and the JD-2 had a burial age of 0.7 ± 0.0 ka.
참고문헌 (18)
- Bachyn, T.E., "Reactivation of supply-limited dune fields from blowouts: A conceptual framework for state characterization", Geomorphology, 201, pp.172~182 (2013)
- Chen, T., "Characteristics and genesis of meghemitite in Chinese loess and paleosols: Mechanism for magnetic susceptibility enhencement in paleosols", Earth and Planetary Science Letters, 240, pp.790~802 (2005)
- Chough, S,K., "Sedimentology" (1995), Woosung
- Clarke, M.L., "Effects of storminess, sand supply and the North Atlantic Oscillation on sand invasion and coastal dune accretion in western Portugal", The Holocene, 16(3), pp.341~355 (2006)
- Cunningham, A. C., "Extracting storm-surge data from coastal dunes for improved assessment of flood risk", Geology, 39(11), pp.1065~1066 (2011)
- Dearing, J., "Environmental magnetic susceptibility-Using the Bartington MS2 system" (1999), Bartington Instruments
- Gilbertson, D. D., "Sand drift and soil formation along an exposed North Atlantic coastline:14,000 years od diverse geomorphological, climatic and human impacts", Journal of Archaeological Science, 26, pp.439~469 (1999)
- Kim, H.J., "Analysis for making process of coastal sand dune at Daecheongdo", The Journal of Applied Geography, 28, pp.91~109 (2009)
- Korea Geological Society, "Geology of Korea" (1999), Sigma Press
- Lewis, D., "Coastal dune:geomorphology, ecology and management for conservation", pp.463~473 (1992), Balkme
- 박천영, "대청도 옥죽동 해안사구의 지형특징 및 발달과정에 관한 고찰", 한국지형학회지, 16(1), pp.101~111 (2009), 한국지형학회
- Explanatory note of Jeju (Baekado, Jinnampo) sheet (1:250000), "Park, K.H.", Korean Institute of Mining Geology, ~ (2000)
- 박경문, "인천광역시 연안 해안사구 보전현황 평가 연구: 중구, 옹진군을 중심으로", 대한지리학회지, 51(3), pp.345~365 (2016), 대한지리학회
- Park, Y.A., "Study of the Cheonripo intertidal beach sands and coastal dune sands, Cheonripo, the west coast of Korea", The Korean Journal of Quaternary Research, 7(1), pp.93~102 (1993)
- Phantuwongraj, S., "Coastal geomorphic conditions and styles of storm surge washover deposits from Southern Thailand", Geomorphology, 192, pp.43~58 (2013)
- 신원정, "영광 하사리 해안 퇴적층 내의 연안 범람 증거", 한국지형학회지, 24(3), pp.83~103 (2017), 한국지형학회
- Sun, J., "Multiple origins and interpretations of the magnetic susceptibility signal in Chinese wind-blown sediments", Earth Planetary Science Letters, 180, pp.287~296 (2000)
- Xiao, J., "Grain size of quartz as an indicator of winter monsoon strength of the Loess Plateau of Central China during the last 130,000 Yr", Quaternary Research, 43, pp.22~29 (1995)
