• Title/Summary/Keyword: broad-leaved deciduous forest

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Community Distribution on Mountain Forest Vegetation of the Geumsusan and Doraksan Area in the Worak National Park, Korea (월악산국립공원 금수산 및 도락산 일대 삼림식생의 군락분포에 관한 연구)

  • Lee, Jung-Yun;Oh, Jang-Geun;Jung, Se-Hoon;Kim, Ha-Song
    • Korean Journal of Ecology and Environment
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    • v.48 no.2
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    • pp.129-138
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    • 2015
  • Forest vegetation of Geumsusan (1,016.0 m) and Doraksan (964.4 m) in Woraksan National Park is classified into mountain forest vegetation. Mountain forest vegetation is subdivided into deciduous broad-leaved forest, mountain valley forest, coniferous forest, riparian forest, afforestation and other vegetation. Including 77 communities of mountain forest vegetation and 5 communities of other vegetation, the total of 82 communities were researched; mountain forest vegetation classified by physiognomy classification are 37 communities deciduous broad-leaved forest, 16 communities of mountain valley forest, 8 communities of coniferous forests, 1 community of riparian forest, 15 afforestation and 5 other vegetation. As for the distribution rate for surveyed main communities, Quercus variabilis and Quercus mongolica communities account for 33.031 percent of deciduous broadleaved forest, Cornus controversa community takes up 29.142 percent of mountain valley forest, Pinus densiflora community holds 64.477 percent of mountain coniferous forest holds. In conclusion, minority species consisting of Quercus variabilis, Quercus mongolica, Pinus densiflora, Quercus serrata and Cornus controversa are distributed as dominant species of the uppermost part in a forest vegetation region in Woraksan National Park. In addition, because of vegetation succession and climate factors, numerous colonies formed by the two species are expected to be replaced by Quercus variabilis, Quercus mongolica, Cornus controversa and Fraxinus mandshurica which are climax species in the area.

Disturbance Regime of the Pinus densiflora Forest in Korea (한국 소나무림에서의 교란체제)

  • Lee, Chang-Seok
    • The Korean Journal of Ecology
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    • v.18 no.1
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    • pp.179-188
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    • 1995
  • Death patterns of gap-makers and changes of environmental factors in gaps formed by disturbance were studied in Pinus densiflora forests of Youngwol, Mt, Mansu, Mt. Songni, Uljin, and Mt, Obong in Korea. Death pattern of gap-makers showed that standing deat type was the most frequent in all the study areas. Longevity of Pinus densiflora was about 140 years, which was about half of that of the temperate deciduous broad-leaved trees. size of gaps were distributed from $20m^2$ to $235m^2$, more than 80% of those were gaps created by death of two or more trees. Relative light intensity and water content of soil in gap area were higher than those in non-gap area and those in the central part of gap were the highest.

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Planting Structure and Ecological Characteristics of Green Spaces at the Dangjin Steam Power Plant (당진화력발전소 녹지공간의 식재현황 및 생태적 특성 분석)

  • Kang Hyun-Kyung;Lee Soo-Dong;Han Bong-Ho
    • Journal of the Korean Institute of Landscape Architecture
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    • v.33 no.6 s.113
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    • pp.78-89
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    • 2006
  • This study was conducted to analyze the planting structure and ecological characteristics of greon spaces on the grounds of e Dangjin steam power plant. To achieve these goals, we surveyed existing vegetation, plant community structure, Plant volume and growth rate. Based on e vegetation analysis, existing vegetation was classified into six types: herbaceous species $(70.54\%)$, evergreen coniferous trees $(21.17\%)$, deciduous broad-leaved trees $(5.10\%)$, deciduous coniferous trees $(1.47\%)$, shrubs $(0.12\%)$, and other types $(1.59\%)$. The coal storage, office, and playground areas were community is the natural forest area where a Pinus thunbergii / Pinus densiflora community is distributed in terms of vegetation structure, species diversity, plant volume, and growth rate. The artificial green spaces(near the coal storage, office, playground areas) had a single-layer structure. Species diversity indices of the artificial green areas were $0.1655\~0.4807$ compared to 0.8628 in the natural forest, which presented a good growth environment. Also, the plant volume in the artificial green space was lower than that of the natural green space. Therefore, it would be desirable to develope a multi-layer structure similar to that of the vegetation in the natural green space in order to improve the amount of plant volume. The plant-damage ratio of Pinus thunbergii was $52.48\%$ in the coal storage area, and $8.48\~ 11.52\%$, in the other survey areas. Also, the vitality of Pinus thunbergii was $15.45k{\Omega}$ in the coal storage areas, which indicates bad growing conditions. This suggests that soil characteristics and dust have a bad impact on growth. The investigation into deciduous tres' growth status showed that appropriate plants would be Albizzia julibrissin, Acer palmatum var. sanguineum, Acer palmatum, Malus spp., Prunus sargentii.

Plant Community Structure of Abies holophylla Community from Sinseongam to Jungdaesa in Odaesan National Park (오대산국립공원 신성암~중대사 전나무림 식물군집구조 특성)

  • Kim, Dong-Wook;Han, Bong-Ho;Kim, Jong-Yup;Yeum, Jung-Hun
    • Korean Journal of Environment and Ecology
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    • v.29 no.6
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    • pp.895-906
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    • 2015
  • This study was carried out to the structure of plant community from Sinseongam to Jungdaesa in Odaesan National Park, furthermore, it seeks to curate the basic data for planning of the Abies holophylla's forest management in Odaesan National Park. In order to identify the current ecological environment, this study explored the actual vegetation as primary research and set to twenty plots(i.e. $400m^2$) for analysing detailed structure of plant communities. The research methodology was qualitative analysis, therefore it used TWINSPAN and DCA analysis tools. Especially, TWINSPAN performed well in several comparisons of classification techniques, DCA is one of the ordination technique showed that the plant communities. The plant community was analysed classification and ordination by TWINSPAN and DCA, moreover it was analysed the structure of plant community such as importance percentage of woody species, DBH class distribution, the index of diversity and rate of sample tree growth. The main vegetation was A. holophylla-Quercus mongolica forest and Deciduous broad-leaved forest in the communities where located in low altitude and valley, whereas main vegetation where located in high altitude and slope was Q. mongolica forest. The research site's plant communities were classified four groups. In all of communities, A. holophylla was dominant species in main canopy layer, furthermore, the three communities (community I, II, III) are growing up next generation of A. holophylla excluding community IV. The communities (community I, II, III) can be sustained current status which dominates the A. holophylla communities, simultaneously, there might be expanded the Deciduous broad-leaved communities by Carpinus cordata, Betula schmidtii and so on. While, it showed that the community IV tended to be weaken the forces of A. holophylla, therefore the community IV can be transferred to C. cordata-Deciduous broad-leaved communities in the future. The age of sample trees was 79~128(i.e. A. holophylla), 75~87(i.e. Pinus koraiensis) and 190 years(i.e. Ulmus davidiana var. japonica). The index of Shannon's Species diversity (H') were ranged from 0.3889 to 1.3332 in the communities.

Palynological Study of Moojechi Bog (무제치늪의 화분분석 연구)

  • 최기룡
    • The Korean Journal of Quaternary Research
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    • v.15 no.1
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    • pp.13-20
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    • 2001
  • The Pollen analyses and the $^{14}C$-dating of the sediments of Moojechi bog were performed in order to study the vegetation history and the environmental changes of the southeasterm montane zone of Korea. These results show that the local pollen assemblage of the montane zone changed from lower upward cool-temperate northern/altimontane forest(MI) into cool-temperate central/montane forest(M II a) and cool-temperate souther $n_montane forest(M II b). Furthermore, In the case of the present cool temperature deciduous broad-leaved forests, its distribution would begin to be expanded from 8,000yr B.P., and its regional differentiation would be developed from 6,700yr B.P..P.

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Forest Vegetation of Mt. Pal-Gong (팔공산(八公山) 삼림식생(森林植生))

  • Hong, Sung Cheon;Cho, Hyun Je;Yun, Yong Whal;Kim, Je Hak
    • Journal of Korean Society of Forest Science
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    • v.70 no.1
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    • pp.17-27
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    • 1985
  • Through the study of the physiognomical vegetation, the vertical distribution, the distribution of forest community and the flora of the woody plants on the south facing slope of Mt. Pal-Gong, the results obtained were summarized as follows. The forest of Pinus densiflora was dominant in the region of below 750m above the sea level, the mixed forest of conifer and broad-leaved trees in the region of 750m to 950m and the pure forest of deciduous broad-leaved trees in the region of above 950m. Pinus densiflora and Quercus mongolica were dominant for the upper-story trees, Acer pseudo-sieboldianum and Carpinus laxiflora for the mid-story trees, Lespedeza maximowiczii, Sasa purpurascens, Rhododendron mucronulatum and Rhododendron schlippenbachii for the under-story trees. Among seventeen forest communities, Cephalotaxus koreana, Populus davidiana and Alnus hirsuta var. sibirica were considered remarkable communities on the south facing slope of Mt. Pal-Gong. The woody plants growing on Mt. Pal-Gong are composed of 59 families, 7 subfamilies, 122 genera, 178 species, 29 varieties and 10 formae. Populus davidiana, Alnus hirsuta var. sibirica and Rubus phoenicolasius were collected newly in this study.

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Vegetation History of Wangdeungjae Moor, Mt. Jiri in Korean Peninsula (지리산 왕등재늪의 식생변천사 연구)

  • Jang, Byeang-O;Sin, Seang-Uk;Choi, Kee-Ryang
    • Journal of Ecology and Environment
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    • v.29 no.3
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    • pp.287-293
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    • 2006
  • We carried out pollen analysis and radiocarbon dating from sediments of Wangdeungjae moor (960 m a.s.l.) to clarify vegetation history of temperate broad-leaved deciduous forest zone of Mt. Jiri. Three local pollen zones and two sub-zones were recognized on the basis of variation in the palynofloral assemblage: I. Quercus zone (150-114 cm), II. Quercus-Pinus zone (114-43 cm): IIa. Quercus-Pinus subzone (114-83 cm), IIb. Quercus-Pinus-Herbs subzone (83-43 cm), III. Pinus-Quercus zone (43-27 cm). Radiocarbon date from sediment depth 111-116 cm was estimated $1,160{\pm}40yr$ B.P. From these results, overall vegetation around of Wangdeungjae moor and Mt. Jiri have changed from Q. mongolica dominant to steady decrease of Q. mongolica whereas steady increase of P. densiflora, finally abrupt increase of P. densiflora. 'Medieval Warm Period (MWP)' and 'Little Ice Age (LIA)' have not had an effect on change of vegetation around, at least, Mt. Jiri. But at maximum period of LIA, extension of grassland and steady increase of Pinus were recognized around the moor. After then, an abrupt increase of Pinus is supposed that vegetation change is reflected in human impact surging around foothills.

Postglacial Vegetation History of the Central Western Region of the Korean Peninsula (한반도 중서부 지역의 후빙기 식생 변천사)

  • Jang, Byeong-O;Yang, Dong-Yoon;Kim, Ju-Yong;Choi, Kee-Ryong
    • Journal of Ecology and Environment
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    • v.29 no.6
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    • pp.573-580
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    • 2006
  • A sediment core from the Cheollipo arboretum ($36^{\circ}$ 47' 57'N, $126^{\circ}$ 09' 04') was studied for pollen analysis in order to reconstruct postglacial vegetational change and environmental changes around the central western region of the Korean Peninsula. The record shows four pollen assemblage zones: Zone CHL-I, Quercus stage (ca. 9,300$\sim$6,200 yr BP): zone CHL-II, Quercus-Pinus stage (ca. 6,200$\sim$4,600 yr BP); zone CHL- III, Pinus-Quercus stage (ca. 4,600$\sim$1,160 yr BP): zone CHL-IV and Pinus stage (ca. 1,160 yr BP-present). During the 9,300$\sim$8,500 yr BP, the early Holocene, researchers have guessed a piece of cool-temperate norihern/altimontane mixed coniferous and deciduous broad-leaved forest. Between 8,500$\sim$4,600 yr BP the Quercus dominated the landscape of study area and the established dates of this typical cool-temperate central/montane deciduous broad-leaved forest vegetation might be ca. 6500 yr BP, and then the Pinus developed around the site at ca. 5,700 yr BP. The abrupt increase of Pinus and NAP (non-arboreal pollen) after ca. 1,100 yr BP indicates the vegetation changes due to human activities. From the dynamics of the Chenopodiaceae pollen indicating salt marsh and freshwater pollen flora such as Typha, Trapa, Nymphoides and so forth, we suggest that the tidal flat was altered into freshwater lake around 6,500 yr BP.

Spread and distribution characteristics of ecosystem-disturbing plant Alliaria petiolata(M. Bieb.) Cavara & Grande in Korea (생태계교란식물 마늘냉이의 확산과 분포 특성)

  • Yeon-Ji Lee;Bo-Ram Hong;Kyu-Song Lee
    • Korean Journal of Environmental Biology
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    • v.42 no.1
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    • pp.62-79
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    • 2024
  • Garlic mustard (Alliaria petiolata) is a species that has devastated the United States and Canada. It is known to play a role in destroying the ecosystem. In this study, the domestic distribution of garlic mustard was confirmed and a detailed distribution map was created for the Samcheok region, where the largest population has been established in South Korea. This study investigated the growth environment, life cycle, and population dynamics of the species in the Samcheok region. Garlic mustard was found in a total of 301 locations in Samcheok, with a total distribution area of 2,957 square meters. Annual plants germinated in mid-April, overwintered in rosette form, underwent vegetative growth from April 10 to April 24 the following year, and flowered from April 24 to May 7. Individuals producing seeds began to die off from June. Both annual and biennial individuals showed a trend of increasing and then decreasing in number around April 27 (118 days). Garlic mustard grew well under favorable light conditions in early spring. They showed less growth on leaf litter, short distance from roads, lower altitude, deciduous broad-leaved forest of middle and lower parts of the slope and forest edge. Without proper control measures in the Samcheok region, it is likely to spread more rapidly in deciduous broad-leaved forests along hiking trails in the Galyasan Mountains. In particular, it is more likely to extend to oak community where light enters the site during flowering than to pine community where there is less light in the site.

The Late Quaternary Pollen Analysis of Gokgyo River Basin in Asan-City, Korea - Focused on Vegetation and Climate Environment between the Last Glacial Maximum and the Late Glacial - (충남 아산 곡교천 유역의 제4기 후기 화분분석 - 최종빙기 최성기~만빙기 식생 및 기후환경에 주목하여 -)

  • PARK, Ji-Hoon;KIM, Sung-Tae
    • Journal of The Geomorphological Association of Korea
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    • v.20 no.1
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    • pp.11-20
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    • 2013
  • The pollen analysis was performed targeting the valley plain alluvium of Jangjae-ri, Asan area in order to clarify the climate and vegetation environment of the Last glacial maximum and the Late glacial in terms of Gokgyo River Watershed In Asan-City, Korea. The sample collection point gets included in the current deciduous broadleaf forest zone (south cool temperate zone). The results are as follows. (1) The vegetation environment of about 19,300-14,100yrB.P. at the investigation area is mainly classified into YJ-I period and YJ-II period while YJ-Ia period is classified once again into YJ-Ia period and YJ-Ib period. YJ-Ia period (19,300-17,500yrB.P.) is correlated with the Last Glacial Maximum while the vegetation at the time has relatively a little wide distribution area of grassland compared to the forest and the forest vegetation of this time period is the mixed conifer and deciduous broad-leaved forest. YJ-Ib period (15,400-14,750yrB.P.) is correlated with the Late glacial (or the Last Glacial Maximum) and the distribution area of grassland became wider compared to the forest. While the forest vegetation of this time period is the mixed conifer and deciduous broad-leaved forest, a difference exists in terms of the dominant tree species. YJ-II period (about 14,650-14,100yrB.P.) is correlated with the Last glacial while the distribution area of grassland became even wider than the forest compared to the YJ-Ib in case of the vegetation at the time and the forest vegetation of this time period is the coniferous forest. (2) Both YJ-I period and YJ-II period were relatively cold and dry compared the End of Late Glacial (about 12,000-10,000yrB.P.)~Early Holocene (10,000-8,500yrB.P.), Also, YJ-II period was relatively colder than the YJ-I period and the YJ-Ib period was relatively more humid than the YJ-Ia period.