• 제목/요약/키워드: forest floor

검색결과 191건 처리시간 0.053초

지리산 개서어나무림에서의 12년간 지역기후의 변화에 따른 연간 종자생산량의 변동 (Twelve Years Changes in Local climate Factors and Annual fluctuations of Seed Production of the Carpinus tschonoskii Forest in Mt. jiri in Southern Korea)

  • 임영득;홍선기
    • The Korean Journal of Ecology
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    • 제21권6호
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    • pp.809-814
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    • 1998
  • Changes of annual seed production related to climate change were studied for 12 years in Piagol, a riparian valley in Mt. Jiri. Sixty-four seed traps (sized 0.5 ${\times}$ 0.5 $m^{2}$) were set up on the forest floor of surveyed area. Seeds were collected from these traps at an interval of 15 days from September to November since 1984. Vegetation of the study area was mainly consisted of the naturally regenerated Carpinus tschonoskii in the tree layer. Acer mono, Quercus serrata, Carpinus laxiflora and Symplocos chinensis also appeared in the same layer. Maximum production occurred in 1984 and 1994. As a result of comparing seed production with local climate factors for 12 years, seed productivity and the year of maximum production of Carpinus forest were merely related with precipitation, air temperature and duration of sunshine among local climate factors. Duration of sunshine was, however, not contributed to periodically high productivity of seed of riparian valley carpinus forest.

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월악산 소나무림의 낙엽생산과 낙엽을 통한 영양염류 이입량 (Litterfall and Nutrient Input via Litterfall in Pinus densiflora Forest at Mt. Worak National Park)

  • 남궁정;문형태
    • 환경생물
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    • 제27권3호
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    • pp.261-265
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    • 2009
  • 월악산 국립공원 내의 소나무군락에서 2005년 5월부터 2008년 4월까지 3년 동안 월별 낙엽의 생산량과 낙엽을 통해 임상에 이입되는 영양염류의 양을 조사하였다. 2005, 2006, 2007년의 낙엽생산량은 각각 3.070, 3.066, 3.099 ton $ha^{-1}yr^{-1}$이었으며, 3년 동안의 평균 낙엽생산량은 $3.078{\pm}0.018\;ton\;ha^{-1}yr^{-1}$이었다. 낙엽 구성원 중 침엽, 가지 및 수피, 생식기관 그리고 기타가 차지하는 비율은 각각 61.9, 10.4, 5.2, 22.5%으로 침엽이 차지하는 비율이 가장 컷다. 조사지소에서 3년 동안 낙엽을 통해 임상에 이입되는 질소, 인, 칼륨, 칼슘 그리고 마그네슘의 평균 양은 18.014, 0.878, 4.240, 7.349 그리고 2.172 kg $ha^{-1}yr^{-1}$이었다.

대기 산성 강하물: 토양과 삼림 생태계의 반응 (Atmospheric Acidic Deposition: Response to Soils and Forest Ecosystems)

  • 김준호
    • The Korean Journal of Ecology
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    • 제28권6호
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    • pp.417-431
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    • 2005
  • 한국에서 산성 강하물에 의하여 대부분의 토양은 교환성 양이온, 특히 $K^+$, $Mg^{2+}$$Ca^{2+}$가 세탈되어 유럽과 북미의 삼림 쇠퇴 지역의 토양과 버금가는 수준이고, 염기성 양이온/알루미늄이온$(BC/Al^{3+})$의 몰 비가 낮아서 식물의 정상 생장의 임계 부하수준으로 낮아졌다. 광릉 삼림의 수관은 산성 강하물 중에서 $NO_3^-$$NH_4^+$을 흡수하여 수용원(sink)으로, $K^+$을 세탈하여 공급원(source)으로 작용하지만 산성 강하 물량이 많은 관악산의 삼림은 그러한 기능이 저하되었다 침엽수림과 활엽수림 분수계 생태계는 총수관 통과수의 $K^+$, $NH_4^+$, $Cl^-$, $NO_3^-$$SO_4^{2-}$를 임상토양에 보유하고, $Na^+$, $Mg^{2+}$$Ca^{2+}$을 임상토양에서 계류수로 세탈하고 있어 산성 강하물에 대한 삼림의 반작용이 큼을 보이고 있다.

Preliminary Study of the Ecological Impact of Forest Fires in G. Massigit, G. Gede-Pangrango National Park, West Java

  • Abdulhadi, Rochadi;Adhikerana, A.S.;Ubaidillah, R.;Suharna, N.
    • The Korean Journal of Ecology
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    • 제23권2호
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    • pp.125-129
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    • 2000
  • Gunung Gede Pangrango National Park is one of the Long-term Ecological Research Site in Indonesia. In the late 1997, the fires have burnt and destroyed nearly 300 ha forest in this park. and G. Masigit was the largest burnt area (250 ha) of nine locations of hot spot recognized. Undergrowth vegetation got the most severe impacts. Almost undergrowth vegetation in various location were totally burnt. However, within three months following burning new seedlings such as Omalanthus populneus, Macaranga, Trema orientalis and Eupatorium appeared in the forest floor- The number of mycoflora recorded in burnt forest was interestingly increased in post forest fires site. Forest fires in G. Masigit had also affected the wild life population and diversity. For example, the number of bird species and the number of soil insects in burnt forest was significantly reduced. The forest fires had also great impact on soil. such as on soil organic contents, bulk density, colour, consistency, permeability and the activity of soil microorganisms.

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The Change in Fuel Moisture Contents on the Forest Floor after Rainfall

  • Songhee Han;Heemun Chae
    • Journal of Forest and Environmental Science
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    • 제39권4호
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    • pp.235-245
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    • 2023
  • Forest fuel moisture content is a crucial factor influencing the combustion rate and fuel consumption during forest fires, significantly impacting the occurrence and spread of wildfires. In this study, meteorological data were gathered using a meteorological measuring device (HOBO data logger) installed in the south and north slopes of Kangwon National University Forest, as well as on bare land outside the forest, from November 1, 2021, to October 31, 2022. The objective was to analyze the relationship between meteorological data and fuel moisture content. Fuel moisture content from the ground cover on the south and north slopes was collected. Fallen leaves on the ground were utilized, with a focus on broad-leaved trees (Prunus serrulata, Quercus dentata, Quercus mongolica, and Castanea crenata) and coniferous trees (Pinus densiflora and Pinus koraiensis), categorized by species. Additionally, correlation analysis with fuel moisture content was conducted using temperature (average, maximum, and minimum), humidity (average, minimum), illuminance (average, maximum, and minimum), and wind speed (average, maximum, and minimum) data collected by meteorological measuring devices in the study area. The results indicated a significant correlation between meteorological factors such as temperature, humidity, illuminance, and wind speed, and the moisture content of fuels. Notably, exceptions were observed for the moisture content of the on the north slope and that of the ground cover of Prunus serrulata and Castanea crenata.

Changes in Forest Disturbance Patterns from 1976 to 2005 in South Korea

  • Park, Pil Sun;Lee, Kyu Hwa;Jung, Mun Ho;Shin, Hanna;Jang, Woongsoon;Bae, Kikang;Lee, Jongkoo;Lee, Don Koo
    • 한국산림과학회지
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    • 제98권5호
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    • pp.593-601
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    • 2009
  • Forest disturbances including forest fire, insect pests and diseases, landslides, and forest conversion from 1976 to 2005 were investigated to trace the changes of major forest disturbance agents and their characteristics over time in accordance with changes in natural and social environment in South Korea. While the damaged area by insect pests and diseases continuously decreased for the past 30 years, damaged areas by forest fire and landslide were fluctuating through years. The interval of large forest fires has become shorter with increased tree volume. The precipitation between January and April were significantly correlated with large fire occurrences as Pearson's correlation coefficient -0.400 (P=0.029). The composition of major insect pests and diseases damaging Korean forests has been changed continuously, and become more diversified. While damages by pine caterpillar (Dendrolimus spectabilis) and pine needle gall midge (Thecodiplosis japonensis) decreased, damage by introduced pests has been more serious recently. The change of precipitation pattern that brought more localized heavy rain or powerful typhoon resulted in the recent increase in landslide areas. The major land uses to induce forest conversion have been changed, reflecting the changes in industrial structure in South Korea as agriculture and mining in 1970s, mining and golf ranges classified in pasture in 1980s, and road and housing construction in 1990s and 2000s. Changes in forest disturbance patterns in South Korea show that a country's industrial development is jointly working with global warming on forest stand dynamics. Altering energy structure and land use pattern induced by industrial development accumulates forest volume and reforms microenvironments on forest floor, interacting with climate change, inducing shorter interval of large forest fire and changes in major species composition of forest insect pests and diseases.

산화가 초본층의 발샐 및 토양의 화학적 특성에 미친 영향 (Effects of Forest Eire on Herb Layer Development and Chemical Properties of Soil)

  • 박관수;이미정;송호경
    • 한국환경생태학회지
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    • 제16권2호
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    • pp.141-148
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    • 2002
  • 본 연구는 산화가 초본층의 발생 및 토양의 화학적 특성에 미친 영향을 조사하기 위해 2000년 4월 대전의 계족산에서 발생한 산화지를 대상으로 실시되었다. 식생조사는 곰솔우점림 (침엽수림)과 아까시나무우점림(활엽수림)에서 10m$\times$10m의 방형구를 설치하여 실시하였고, 초본층의 발생조사는 7월 21일 Dierssen의 우점도법을 적용하여 실시되었다. 초본층의 피도는 침\ulcorner활엽수지역 모두에서 산화지가 비산화지보다 높았으며, 출현종수는 산화지와 비산화지의 차이보다 침\ulcorner활엽수 간에 차이가 더 높았다 토양 시료는 비산화지, 그리고 산화지에서 산화 3일 후 그리고 산화 8개월 후에 0~10cm와 10~20cm 토양깊이에서 채취되었다. 토양 유기물층은 비산화지에서는 깊이가 약 1.5cm이었으나 산화지에서는 유기물층이 없었다. 산화 발생 3일 후 산화지와 비산화지 간의 토양 유기물, 전질소, 유기인산, 치환성 양이온함량, pH및 CEC는 유의적인 차이가 없는 것으로 나타났다. 또한 산화지에서 산화 3일 후와 약 8개월 후의 토양의 화학적 특성들은 일부를 제외하고는 유의적인 차이가 없었다.

횡성지역 천연 소나무와 참나무류 순림 및 혼효임분의 탄소 저장량 추정 (Carbon Storage of Natural Pine and Oak Pure and Mixed Forests in Hoengseong, Kangwon)

  • 이수경;손요환;노남진;허수진;윤태경;이아름;;이우균
    • 한국산림과학회지
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    • 제98권6호
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    • pp.772-779
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    • 2009
  • 산림 생태계 내 탄소 수지에 관한 기초자료를 확보하기 위해 소나무와 참나무류의 순림 및 이들의 혼효임분에 대한 탄소 저장량을 추정하였다. 연구대상지는 강원도 횡성군 둔내면 일대로 임분별로 흉고직경 5 cm 이상 임목에 대한 흉고단면적($m^2/ha$)을 기준으로 소나무:참나무류의 비율이 95:5인 소나무 순림과 0:100인 참나무류 순림, 그리고 20:80-70:30인 혼효림을 선정하였다. 각각의 임분 내 식생, 낙엽층, 고사목의 생체량과 탄소 농도를 분석하고, 0-30 cm 깊이까지의 토양 탄소 농도를 분석하였다. 식생(상층 임목과 하층 식생)의 탄소 저장량은 참나무류 순림에서 147.6 Mg C/ha, 소나무 순림에서 141.4 Mg C/ha, 혼효림에서 115.8 Mg C/ha 등으로 통계적으로 유의한 차이는 없었다. 낙엽층 내 탄소 저장량은 소나무 순림에서 12.7 Mg C/ha, 참나무류 순림에서 9.9 Mg C/ha와 혼효림에서 8.4 Mg C/ha 등이었으며, 고사목 내 탄소 저장량은 혼효림에서 2.2 Mg/ha, 참나무류 순림에서 1.7 Mg/ha 와 소나무 순림에서 1.1 Mg/ha 등으로 낙엽층의 탄소량은 임분간 유의한 차이가 있었으나(p<0.05), 고사목의 탄소 저장량은 임분간 유의한 차이가 없었다(p>0.05). 지표로부터 30 cm 깊이까지의 토양 탄소 저장량은 소나무 순림에서 44.4 Mg C/ha이고, 혼효림에서 41.6 Mg C/ha과 참나무류 순림에서 33.3 Mg C/ha 등의 분포를 보였으나 임분간 유의한 차이는 없었다. 생태계 내 총 탄소 저장량은 소나무 순림에서 199.6 Mg C/ha, 참나무류 순림에서 192.5 Mg C/ha, 혼효림에서 169.1 Mg C/ha 등으로 임분별로 통계적으로 유의한 차이는 없었다. 탄소 저장량이 혼효림에서 순림보다 낮은 것은 탄소 저장량의 대부분을 차지하는 식생의 탄소 저장량이 혼효림에서 더 낮기 때문이었다. 혼효림의 식생은 소나무와 참나무류의 종간경쟁으로 참나무류의 직경생장이 둔화되고 임분 밀도가 높아 참나무류 임목간의 경쟁이 심하게 되어 순림보다 낮은 생체량을 보이는 것으로 추정된다. 혼효임분에서 탄소 저장량을 증가시키기 위해서는 간벌과 같은 적절한 임분관리를 통한 임분의 종내 및 종간경쟁을 완화시킬 필요가 있는 것으로 사료된다.

해남과 거제도의 상록활엽수림에 있어서 낙엽의 생산과 분해에 관한 연구 (A Study on the Production and Decomposition of Litters of Evergreen Broadleaved Forests in Haenam and Koje-Do)

  • Chang, Nam-Kee
    • The Korean Journal of Ecology
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    • 제8권3호
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    • pp.163-169
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    • 1985
  • The composition rates of litters were studied at Camellia japonica forests in Koje-Do and Haenam, and at Quercus acuta, Quercus acutissima, Cryptomeria japonica, and Chamaecyparis abtusa forests in Haenam. Total amounts of nitrogen, phosphorus, potassium, calcium, and sodium in litter samples were measured and the relation between these amounts and decomposition rate was studied. Annual litter production were rarely different at each forest in Haenam. The amount of accumulated organic matter was about 4 times greater at C. japonica forest in Koje-Do than at the C. japonica forest in Haenam. These amounts were 5, 282.1 $\pm$ 1, 026.03g/m2 in Koje-Do and 1, 420.7 $\pm$ 384.77g/$m^2$ in haenam. The decomposition rate were rarely differnet at each forest in Haenam, but the rates showed great difference at C. japonica foreests in Koje-Do and Haenam. The rates were 0.093 and 0.313 at C. japonica forests in Koje-Do and in Haenam respectively. The sodium contents were 0.472% and 0.229% on L layer and on Css layer of C. japonica forest in Koje-Do, while they were 0.034% and 0.043% on L layer, and on Css layer of C. jpaonica forest in Haenam. It is sugested that much difference in the salt contents in the forest floor was present from the results of sodium content measured at each site, and that the decomposition rate was affected by the much concentration of salt in Koje-Do.

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남한의 산림생태계에 있어서의 낙엽의 분해모델 (A Model for Litter Decomposition of the Forest Ecosystem in South Korea)

  • Park, Bong Kyu;In Sook Lee
    • The Korean Journal of Ecology
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    • 제4권1_2호
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    • pp.38-51
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    • 1981
  • The present investigation was estimated the effect of temperature, precipitatiion, and time on the decomposition of litters with litter bags of Pinus densiffora and Quercus mongolica at Gure where elevation in 50m, and at Nogodan where elevation in 1300m on Mt. Jiri. As the above results, decomposition model was proposed to relation of the environmental conditions. And was investigated the production and decomposition of litters from the stands of various forest communities in Kwangneung, Mt. Jiri and Mt. Halla. The results are as follows; The models for the decay of organic carbon (C) was as follows: $C=Coe^{-Kt}$ (limiting factor;time) $C=Coe^{-K'te}$ (limiting factor;tempedrature) $C=Coe^{-KnP}$ (limiting factor:precipitation) As observed in litter bag method, the decomposition rate of litter in Pinus densiflora was slower than that of Quercus mongolica. The higher elevation, the slower decomposition rate. The decomposition of litters at Gure where elevation in 50m was equally influenced by temperature and precipitation. But at Nogodan where elevation in 1300m was much inflenced by precipitation. The decay constant of litters was larger in hardwood forest than in coniferous forest. In the same species, the more elevatiion, the less decomposition constant. The time required for the decay of 50%, 95^, 99% of the accumulated litters in the forest floor were faster in hardwood forest than in coniferous forest. In the same species, the higher elevatiion, the longer time required.

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