• Journal of Plant Biology
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• 제12권4호
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• pp.19-29
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• 1969

This study investigated the vertical distribution of the vegetation in Mt. Hanla of Quelpart Island from 1967 to 1969. According to the physiognomy and life form of plants, the following plant communities are observed and arranged tentatively from the foot to the top. A. North-facing slope. (1) Grass land(0∼600m) (2) Deciduous broad-leaved forest(600∼1200m) (3) Mixed forest(broad and needle leaved forest : 1200∼1300m) (4) Evergreen coniferous forest(1300∼1700m) (5) Scrub communities(1700∼1950m) B. South-facing slope. (1) Grass land(0∼700) (2) Deciduous broad-leaved forest(700∼1300m) (3) Mixed forest(1300∼1550m) (4) Evergreen coniferous forest (1550∼850m) (5) Scrub communities(1850∼1950m) D. West-facing slope. (1) Grass land(0∼650) (2) Deciduous brod-leaved forest(650∼1400m) (3) Mixed forest(1400∼1500m) (4) Evergreen coniferous forest(1500∼1750m) (5) Scrub communities(1750∼1950m) The relation of the geological map and vegetation are as follows: (1) In the region of lava of Mt. Hanla are mainly distribut4ed deciduous broad-leaved forest. (2) In the region of Mt. Hanla are mainly distributed scrub. (3) In the region of lava of Gogun-san are involved deciduous broad-leaved forest, scrub and grass land of Gaimi-Dung.

• The Korean Journal of Ecology
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• 제27권4호
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• pp.217-224
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• 2004

The purpose of this study is to clarify the effects of the conversion of the forest management type from a natural deciduous broad-leaved forest to an artificial evergreen coniferous forest based on organic matter dynamics. We investigated the amounts and carbon contents of the forest floor and the litterfall, soil chemical characteristics and cellulose decomposition rates in the natural deciduous broad-leaved forest and adjacent artificial evergreen coniferous forest. In the artificial evergreen coniferous forest were planted Japanese cypress (Chamaecyparis obtusa) on the upper slope and Japanese cedar (Cryptomeria japonica) on the lower slope. The soil carbon and nitrogen contents, CEC and microbial activity had decreased due to the conversion of the forest management type from a natural deciduous broad-leaved forest to an artificial Japanese cypress forest, and were almost the same for the conversion to a Japanese cedar forest. Under the same conditions, it is considered that the soil fertility was different by planting specific tree species because the organic matter dynamics were changed by them.

• 한국환경생태학회지
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• 제12권4호
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• pp.317-330
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• 1999

한려해상국립공원의 통영지구와 욕지도에서 현존식생과 식생구조를 파악하기 위하여 1998년 7월에 37개의 조사구를 설치하여 조사하였다. 조사대상지의 식생은 지리적 격리와 인위적 교란에 의해 지역간 식생구조가 상이하였다. 대상지의 식생은 곰솔림, 곰솔 - 소나무와 낙엽활엽수가 경쟁하는 혼효림, 낙엽활엽수림, 곰솔 - 소나무와 상록활엽수가 경쟁하는 혼효림, 상록활엽수림으로 총 5개 그룹으로 대별되었다. 조사대상지 대부분의 현존 식생은 곰솔림으로 이루어졌으며, 상록활엽수림은 추봉도, 용초도, 비진도, 욕지도, 유재도에 작은 면적으로 분포하였다. 통영지구와 욕지도의 식생구조는 소나무, 곰솔, 낙엽활엽수에서 구실잣밤나무 등을 거쳐 참식나무, 후박나무, 생달나무로 식생천이가 예상된다.

• 한국산림과학회지
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• 제90권6호
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• pp.756-766
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• 2001

자연적으로 분포하고 있는 백운봉지역 상록활엽수림의 산림군락구조를 파악하기 위하여 총 31개의 조사구($300m^2$)를 설치하여 식생조사를 실시하였다. 조사구내에서 출현된 54개의 수종에 대한 평균중요치를 변수로 Cluster 분석한 결과 붉가시나무군락(Quercus acuta community), 붉가시나무-동백나무군락(Quercus acuta-Camellia japonica community), 붉가시나무-낙엽활엽수군락(Quercus acuta-Deciduous broad-leaved tree species community), 붉가시나무-상록 낙엽활엽수군락(Quercus acuta-Evergreen Deciduous broad-leaved tree species community), 붉가시나무-개서어나무군락(Quercus acuta-Carpinus tschonoskii community) 등 5개의 유형으로 구분되었다. 교목상층과 교목하층의 식피율은 각각 평균 88%, 53%였고, 출현빈도가 높은 식물은 붉가시나무, 동백나무, 때죽나무, 사스레피나무, 광나무, 생달나무, 사람주나무, 당단풍 순이었다. 조사지 내 주요 우점 수종은 붉가시나무 외에 때죽나무, 산벚나무, 서어나무, 졸참나무, 개서어나무가 우점하였으며, 교목하층은 붉가시나무, 동백나무, 사스레피나무, 광나무, 생달나무, 사람주나무 순으로 우점하였다. 산정 주변지역을 제외하고는 교목상층 및 교목하층에서 우세한 붉가시나무림이 지속적으로 유지될 것으로 추정되었다. 각 군락에 대한 종다양도는 붉가시나무군락이 0.687, 붉가시나무-동백나무군락이 0.866, 붉가시나무-낙엽활엽수군락이 0.933, 붉가시나무-상록 낙엽활엽수군락이 0.966, 붉가시나무-개서어나무군락이 1.018로 나타났다. 각 군락에 대한 우점도는 0.206~0.416으로 나타났다.

• 한국환경과학회지
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• 제23권11호
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• pp.1863-1879
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• 2014

This study aims at classifying and interpreting on the shrine forest vegetation located in Jirisan national park affiliated to an ecotone in southern part of Korea, foreseeing a vegetation change based on composition species and dominant species on canopy, and proposing the direction of vegetation management. The shrine forests were classified into the 7 community units as Chamaecyparis obtusa-Cryptomeria japonica afforestation, Pinus densiflora community, Pinus rigida afforestation, Quercus variabilis-Quercus serrata community, Zelkova serrata-Kerria japonica for. japonica community, Phyllostachys bambusoides forest, Camellia japonica community. This research is also expatiated on the analogous results of ordination analysis with phytosociological analysis. The constituents of deciduous broad-leaved forest in the warm temperate zone were appeared in the most vegetations. It emerged less that the constituents of evergreen broad-leaved forest in the warm-temperate zone and deciduous broad-leaved forest in the cold-temperature zone. The life form analyses were made use with the two ways: appearance species in total communities and each community. The species diversity of shrine forests is declined because the high dominances of Sasa borealis and Pseudosasa japonica emerged in the shrub and herb layers. These shrine forests will be succession to Q. variabilis-Q. serrata community as the representative vegetation of deciduous broad-leaved forest in the warm-temperate zone, owing to the temperature rise by global warming, and an evergreen broad-leaved forest will be able to be also formed if a temperate rise will be continued. The one of the artificial management of shrine forests is to consider the introduction of the constituents of evergreen broad-leaved forest in the warm-temperate zone.

• Journal of Ecology and Environment
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• 제34권3호
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• pp.259-267
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• 2011

A pollen analytical study of sediment sequences collected from Yongneup moor (sampling point: $38^{\circ}$12'57.4" N, $120^{\circ}$7'30.2" E) was conducted to understand the vegetation history in the mountainous region of the central Korean peninsula. Carbon dating was carried out to measure five successive samples obtained from the bottom at a depth of 180 cm to the surface. The Yongneup moor sediment revealed four main local pollen zones; that is, four past vegetation phases as follows: Local pollen zone I: Quercus-Pinus zone; estimated age, 5,900-4,800 calibrated years (cal) before present (BP); vegetation type, cool-temperate central/montane deciduous broad-leaved forest. Local pollen zone II: Pinus-Abies-Quercus zone; estimated age, 4,800-3,400 cal BP; vegetation type, cool-temperate northern/alti-montane mixed coniferous and deciduous broad-leaved forest. Local pollen zone III: Quercus-Pinus-Abies zone; estimated age, 3,400-400 cal BP; vegetation type: cool-temperate central/montane deciduous broad-leaved forest. Local pollen zone IV: Pinus-Quercus zone; estimated age, 400-present cal BP; vegetation type, cool-temperate central/montane mixed deciduous broad-leaved and coniferous forest. It was confirmed that subalpine coniferous forests had expanded to the mountainous region of the central Korean peninsula during the period from 4,800-3,400 cal BP and thereafter deciduous forests dominated by Q. mongolica were established. Notably, secondary forests dominated by P. densiflora developed in the lower part of the mountainous region of the central Korean peninsula about 400 cal BP due to human interference.

• 한국환경생태학회지
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• 제35권2호
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• pp.204-219
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• 2021

본 연구는 남해안에 분포하는 양호한 산림 식생의 복원과 관리뿐만 아니라 장기적인 측면에서 기후변화에 따른 변화 경향을 파악하고자 가라산과 노자산 서사면에 분포하는 식생의 식물군집구조 특성을 조사·분석하였다. 86개 조사구를 대상으로 군락을 분류한 결과, 저지대를 중심으로 분포하는 곰솔-굴피나무군락, 곰솔-소나무군락, 계곡부 및 전석지대를 중심으로 출현하는 개서어나무-낙엽활엽수군락, 때죽나무-낙엽활엽수군락, 고로쇠나무-낙엽활엽수군락, 낙엽활엽수군락, 느티나무군락, 상대적으로 해발고가 높고 급경사 사면에 분포하는 졸참나무군락, 졸참나무-때죽나무군락, 때죽나무-소사나무군락, 참회나무군락으로 유형화되었다. 천이경향상 상록침엽수는 낙엽활엽수로의 천이가 진행될 것이나 수령이 약 50년인 개서어나무, 느티나무, 고로쇠나무 등 낙엽활엽교목림은 층위구조가 발달되었을 뿐만 아니라 생태적으로 안정되어 현재의 상태를 유지할 것으로 판단되었다. 환경요인으로는 표고, pH, 점토와 실트의 함량, Mg⁺⁺, Ca⁺⁺ 등이 식물 군락 분포에 직간접적으로 영향을 미치는 것으로 분석되었다.

• The Korean Journal of Ecology
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• 제16권4호
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• pp.459-476
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• 1993

내륙지역(두륜산, 불갑산)과 서남해 섬지역(홍도, 진도)의 상록활엽수림과 주변 낙엽활엽수림을 대상으로 식생구조와 식생천이 계열을 분석, 추정하였다. 4개 지역의 상록활엽수림은 대부분 50여 년생 미만의 영급구조로서 처닝도중상의 군집구조를 나타내고 있었으며, 교목층에서의 우점종은 구실잣밤나무, 후박나무, 붉가시나무, 참식나무, 종가시나무, 참가시나무 등이었다. 상록활엽수림대의 식생은 낙엽활엽수종에서 상록활엽수종으로 식생천이가 진행중이었으며, 교목층에서는 후박나무, 참식나무 및 황칠나무가, 아교목층 및 관목층에서는 식나무와 센달나무가 극상단계의 수종으로 추정되었다.

• 한국환경생태학회지
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• 제9권1호
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• pp.30-41
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• 1995

불갑산지역의 상록활엽수림에 대한 식생구조를 분석하기 위하여 40개 조사구에 대한 TWINSPAN과 DCA Ordination 기법을 적용한 결과 5개 식물군집유형 즉 푸조나무군집, 참식나무-푸조나무-비자나무군집, 낙엽활엽수혼효림군, 갈참나무군집. 굴참나무-갈참나무군집으로 분리되었다. 그러나 불갑산 식생은 천이도중상의 불안정한 식생구조라고 판단된다. 상록활엽수림대에서 극상수종으로 판단되는 참식나무는 푸조나무와 정의 상관관계를, 개서어나무, 굴참나무, 갈참나무와 부의 상관관계를 나타냈다.

• Journal of Forest and Environmental Science
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• 제32권2호
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• pp.196-204
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• 2016

In this study, vegetation succession and the rate of consequent topsoil development were investigated in shallow landslide scars of sedimentary rock slopes covered by volcanic ashes and pumice in Kagoshima prefecture, Japan. Seven shallow landslide scars of different ages were selected as study areas. In the initial period after the occurrence of a shallow landslide, deciduous broad-leaved trees such as Mallotus japonicus or Callicarpa mollis were occupied in the areas. Approximately 30 years after the landslide, evergreen broad-leaved trees such as Cinnamomum japonicum invaded in the areas, already existed present deciduous broad-leaved trees. After 50 years, the summit of the canopy comprised evergreen broad-leaved trees such as Castanopsis cuspidata var. sieboldii and Machilus thunbergii. Moreover, the diversity of vegetation invading the site reached the maximum after 15 years, followed by a decrease and stability in the number of trees. The total basal areas under vegetation increased with time. It was concluded that the vegetation community reaches the climax stage approximately 50 years after the occurrence of a shallow landslide in the study areas, in terms of the Fisher-Williams index of diversity (${\alpha}$) and the prevalence of evergreen broad-leaved trees. Moreover, according to the results of topsoil measurement in the study areas, the topsoil was formed at the rate of 0.31 cm/year. The development of topsoil usually functions to improve the multi-faceted functions of a forest. However, when the increased depth of topsoil exceeds the stability threshold, the conditions for a shallow landslide occurrence are satisfied. Therefore, we indicated to control the depth of topsoil and strengthen its resistance by forest management in order to restrain the occurrence of shallow landslides.