• Proceedings of the Korean Environmental Sciences Society Conference
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• 2005.05a
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• pp.45-49
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• 2005

최근 해안송림에 대한 관심이 높아지고 있고, 이를 효과적으로 보전, 활용해야한다는 목소리가 높지만, 국내에서는 이러한 해안송림이 어떻게 변천되고 지역에 어떻게 기능해 왔는지 아직 알려지고 있지 않다. 본고는 해안송림의 기초연구로서, 하동송림을 대상으로 이러한 해안송림의 사회적인 기능과 관리문제를 검토한 것에 있다. 하동송림을 사례로 조사한 결과, 해안송림은 송림이 지역과 밀착함으로써 주민의 레크레이션기능은 물론 외부관광객을 끌어들일 수 있는 지역발전의 중요한 소재가 될 수 있는 것으로 나타났다. 또한 해안 송림이 지역주민의 일상생활과 밀접히 연관되고 지역발전의 한 축으로서 기능하면서, 송림에 대한 관리 및 주체의식이 높아지는 것으로 나타났다. 이러한 지역발전의 실질적 기능 및 자연스러운 관리의식의 고양은 일반 공원이나 원거리 해안림 등에서는 쉽게 나타나지 않는 것으로서, 마을 숲(해안송림 등)이 갖고 있는 하나의 중요한 잠재력이 아닌가 생각된다. 그러나 관리측면에서는 하천오염이 해결되지 않고, 송림확장계획이 중지되고, 소나무재선충 방지책에 의문에 제기되는 등 적지 않은 문제가 나타나고 있다. 또한 이러한 문제발생의 원인으로는 해안송림에 대한 기본적인 인식의 부족, 책임 있는 관리주체의 부재, 구체적인 연구의 부족 등이 검토된다. 해안송림의 기능과 식생은 고정되어 있는 것이 아니라 지역 환경에 따라 끊임없이 변화되는 것에 있어, 변화에 대응하는 개발논리가 필요하다. 따라서 이러한 특수성을 일반적 임업관리나, 시설보수 차원에서의 접근은 소중한 지역의 자산과 발전기회를 잃은 거와 다르지 않다. 소중한 지역자원의 가치를 빛내고, 보다 효과적인 활용을 위해서는, 보다 체계적이고 파지티브한 관리 및 활용 정책이 요구되는 것에 있고, 이를 위해서는 책임 있는 관리주체를 조직하는 것과 함께, 토지사병에 기초한 송림의 이용 및 식생 변화에 대한 연구가 필요한 것으로 판단된다.

• Journal of Korean Society of Forest Science
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• v.102 no.3
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• pp.315-322
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• 2013

This study was carried out to establish a management program and soil restoration plan through analysis of soil properties and visitor questionnaires in Songrim in Hadong, Korea. Soil bulk density in Songrim was slightly higher in the closed-woodlands ($1.31g/cm^3$) than in the open-woodlands ($1.39g/cm^3$). Soil bulk density in the closed-woodlands was higher in walking trails ($1.74g/cm^3$) than in forest areas ($1.39g/cm^3$), while the rates of pore space were lower in walking trails (42.6%) than in forest areas (50.5%). The soil porosity were lower in the closed-woodlands (34.6%) than in the open-woodlands (42.6%). Soil strength in surface soil was slightly lower in the open-woodlands ($8.5kgf/cm^2$) than in the closed-woodlands ($10.5kgf/cm^2$). The content of organic matter, total nitrogen and exchangeable cations of the woodlands was low compared with the optimum nutrient content for tree growth in Korea forest soil. According to the survey, the objective of visiting in Songrim was to enjoy recreation and landscape views. To conserve pine forest ecosystems in Songrim, the respondents said that it needs to the implement of closed-woodland periods, the establishment of smoking free zone, and the prohibition of garbage throwing and alcohol including disciplinary rules and education. Also the respondents said that pine forest ecosystem in Songrim is relatively sound, but the woodlands require the intensive management to the ecosystem and the introduction of native understory vegetation, such as grasses under pine forest ecosystem. It is recommended to designate the rest-year forest for a proper period in all woodlands to restore the Songrim soil rather than the alternation application between the rest-year for three years or non-rest-year trails, and to open partially the walking trails across the woodlands after the period. In addition, the forest within the woodland is need to designate a long-term rest-year.

• Proceedings of the Korean Environmental Sciences Society Conference
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• 2003.11b
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• pp.77-81
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• 2003

1)일본에서 해안림은 강풍, 비사로부터 경작지를 보호하기 위해 조성되었고. 그의 기능은 해안방풍림.입회림 $\rightarrow$레크레이션임 $\rightarrow$생활환경림으로 변화하고 있다. 그리고 관리문제는 초기 입회의 권리문제로부터 이용의 제어문제로, 그리고 최근에는 쓰레기, 방화, 청소년범죄 등의 사회문제로, 그의 중심이 이동하고 있다. 2)이러한 입회적 이용과 해안흑송림의 식생변화(광엽수화)와는 그의 관련성이 높다는 의문이 제기되어온 것에 있으나, 본 연구를 통해 입회적 이용이 소멸(부영양화)되는 것에 따라 해안흑송림의 천이가 발생되고 있는 것이 입증된다. 3)그리고, 현재 문제시되고 있는 쓰레기, 화제, 범죄 등의 관리문제는 이러한 식생변화와 매우 큰 관련성(밀폐된 산림구조에서 관리문제가 큼)을 갖고 있는 것으로 나타난다. 4)이상에서 보면, 전체적으로는 해안흑송림의 변용에는, 이용의 변화가 산림의 식생변화를 부르고, 다시 이러한 밀폐된 산림구조가 새로운 관리문제(쓰레기. 범죄, 방화 등)를 발생시키는 메커니즘이 자리 잡고 있는 것을 알 수 있다.

• The Journal of the Petrological Society of Korea
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• v.21 no.2
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• pp.151-171
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• 2012

The Permo-Triassic Songrim orogeny in the Korean peninsula was a major tectonic event involving complicated continental collisions at the eastern margin of Eurasia. Based on the previous studies on the metamorphic and deformations features of the Songrim orogeny, this paper presents metamorphic and structural characteristics and timing of the Songrim orogeny in the Taebaeksan basin, and discuss about correlation of the tectono-metamorphic evolution of the Taebaeksan basin with the Okcheon basin and the Imjingang belt with a combined analysis of bulk crustal shortening direction, metamorphic P-T and T-t (time) paths. The metapelites in the Pyeongan Supergroup in the northeastern margin of the Taebaeksan basin have experienced lower-temperature/medium-pressure (LT/MP) regional metamorphism followed by high-temperature contact metamorphism due to the Jurassic granite intrusion. The earlier LT/MP regional metamorphism produced two loops of clockwise P-T-d (deformation) paths combined with four deformation events ($D_1-D_4$). The first loop concomitant with $D_1$ and $D_2$ occurred at $400-500^{\circ}C$, 1.5-3.0 kbar, and related with growth of syn-$D_1$ chloritoid and andalusite, post-$D_1$ margarite, Ca-rich syn-$D_2$ or post-$D_2$ plagioclase. The second loop accompanying $D_3$ and $D_4$ occurred at $520-580^{\circ}C$, 2.0-6.0 kbar, and associated with the growth of syn-$D_3$ garnet and staurolite, and syn-$D_4$ and/or post-$D_4$ andalusite porphyroblasts. Furthermore the syn-$D_1$ chloritoid and andalusite porphyroblasts grew during E-W bulk crustal shortening, whereas the syn-$D_3$ garnet and staurolite, and the syn-$D_4$ and/or post-$D_4$ andalusite porphyroblasts have grown under N-S bulk crustal shortening. The similarity in the characteristics and timing of the metamorphism and bulk crustal shortening directions between the Okcheon and Imjingang belts suggest that the peak metamorphic conditions tend to increase toward the western part (Imjingang belt and southwestern part of the Gyeonggi Massif) from the eastern part (Taebaeksan basin). The E-W bulk crustal shortening influenced the eastern part of the Okcheon belt, whereas the N-S bulk crustal shortening resulted in strong deformation in the Imjingang and Okcheon belts. Consequently, the Permo-Triassic Songrim orogeny in the Korean peninsula is probably not only related to collision of the North and South China blocks, but also to the amalgamation of terrane fragments at the eastern Eurasia margin (e.g., collision of the Sino-Korean continent and the Hida-Oki terrane).

• Economic and Environmental Geology
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• v.52 no.5
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• pp.367-379
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• 2019

Pyeongan Supergroup (PS) in the Taebaeksan basin preserves key geological evidences to understand the tectonometamorphic evolution of the Songrim orogeny that affected the formation of the Korean Peninsula during the late Paleozoic to early Mesozoic. The aims of this paper therefore are to investigate the characteristics of the Songrim orogeny based on the previous results of metamorphism and deformations of the PS, and then to review geological significance and research necessity of the PS. Age distributions and Th/U ratio of detrital zircon in the PS indicate that sedimentary environment of the Taebaeksan basin during the late Paleozoic was arc-related foreland basin and retro-arc foreland basin at the active continental margin. In addition, the main magmatic activities occurred in the early Pennsylvanian and Middle Permian, thus sedimentation and magmatic activities occurred simultaneously. The PS was affected by lower temperature-medium pressure (M1) and medium temperature and pressure (M2) regional metamorphism during the Songrim orogeny. During M1, slate and phyllite containing chloritoid, andalusite, kyanite porphyroblasts intensively deformed by E-W bulk crustal shortening combined with folding and shearing. And garnet and staurolite porphyroblasts were formed during the N-S bulk crustal shortening accompained by M2. Such regional metamorphism of the PS is interpreted to occur in an area where high strain zone is localized during ca. 220-270 Ma. In order to elucidate the evolution of the Taebaeksan basin and tectonic features of the Songrim orogeny, it is expected that the study will be carried out such as the regional distribution of metamorphic zones developed in the PS, characteristics and timing of deformations, and late Paleozoic paleo-geography of the Taebaeksan basin.

• Journal of Korean Society of Forest Science
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• v.86 no.2
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• pp.200-207
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• 1997

The throughfall, stemflow and precipitation interception during the period of May to November 1995 were compared between three stands of Pinus koraiensis, Larix leptolepis and Quercus species stand growing at Kwangju-Gun, Kyunggi-Do. The total amount of precipitation during the period in the study area was 1,821mm, higher than average precipitation. The amount of interception showed 21.8% of the total precipitation in Quercus stand, whereas 15.7 and 19.4 in P. koraiensis and L. leptolepis stands, respectively. Precipitation leached on forest floor was occupied mainly by throughfall for all the stands, and it was specially higher in P. koraiensis stand. The amount of stemflow was appeared higher in Quercus stand(5.0%) than P. koraiensis stand(1.1%) or L. leptolepis stand(1.1%). The relationship between throughfall or stemflow and total precipitation in all the stands were highly significant.

• Conservation Science in Museum
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• v.3
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• pp.1-7
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• 2001

The gilded bronze Sarria reliquary(National Treasure No. 325-1) excavated from a five story tower in Songlim Temple is considered as a very important Sarria reliquary of Unified Silla Dynasty Kingdom along with glass Sarria containers excavated in package. It was found that this Sarria container was in a very weak condition in the conservation dept. of National Museum of Korea due to the wearing of the inside wood and the decay of the gilded bronze, so a conservation treatment was conducted by focusing on the prevention of further decay and wearing. Also because there is little information about Sarria reliquary, detailed investigation by means of precision actual measurements, microscopic examination and X-ray photography was carried out.

• Proceedings of the Mineralogical Society of Korea Conference
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• 2001.06a
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• pp.96-99
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• 2001

• Proceedings of the Zoological Society Korea Conference
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• 2001.10a
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• pp.195.3-196
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• 2001

• Social Workers
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• no.1 s.33
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• pp.16-17
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• 2005