• 한국어류학회지
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• 제25권1호
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• pp.25-32
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• 2013

We studied the age and growth of striped beakperch (Oplegnathus fasciatus) in the Jeju marine ranching area using a total of 423 otoliths from August 2009 to August 2010. The surface reading method, which was etched with 5% HCl, was the best method to read ages of this fish. The monthly mean fork length ranged from 20.9 cm to 27.7 cm in the Jeju marine ranching area during from August 2009 to August 2010. The annual ring was formed in July to September once a year. Fish were principally composed of 3 to 5 years old and the oldest was 12 years old. The von Bertalanffy growth parameters of this species, which were estimated from a non-linear regression, were $L_{\infty}$=48.20 cm, $t_0$=-1.031yr, and K=0.123/yr.

• 한국수산과학회지
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• 제48권6호
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• pp.929-939
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• 2015

We studied the characteristics of age and growth of the Goldeyes rockfish Sebasetes thompsoni in the Ulleungdo and Dokdo areas by using 730 otoliths from February 2013 to February 2014. The lowest value of the marginal index was found in June once a year. The spawning period was estimated as April. Therefore, the duration from fertilization to the complete formation of the first annual growth ring is fourteen months. From the parameters calculated using the weighted average length of the year ring formation, the growth of S. thompsoni was demonstrated by the von Bertalanffy growth equation as $L_t=34.68(1-e^{-0.2113(t+0.7683)})$ for females and $L_t=29.79(1-e^{-0.2163(t+1.7964)})$ for males, $L_t=32.84(1-e^{-0.25(t+0.57)})$ for combined sex. Comparing with growth performance index(${\Phi}$) from these 4 offshore areas, parameter of S. thompsoni in Ulleungdo area was 2.4087, that of in Tong-yeong was 2.2835, that of in Aomori was 2.4077 and in Niigata was 2.3927. As a result, the value of Dokdo and Ulleungdo areas showed the highest.

• 한국농림기상학회지
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• 제18권3호
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• pp.109-119
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• 2016

본 연구는 우리나라의 대표 활엽수종 중의 하나인 신갈나무를 대상으로 기후변화에 의한 연도별 생장도일의 변화가 잠재분포 및 생장에 미치는 영향을 평가하기 위해 수행하였다. 이를 위해 신갈나무 분포 지역의 기후특성을 반영한 군집분석을 실시하였으며, 그 결과 7개의 기후군집으로 분류되었다. 각 군집에 포함된 시군에서 수집된 일평균기온 자료를 기반으로 1951년부터 2010년까지 60년 동안의 연도별 생장도일과 기온효과지수를 산출함으로써 시간 경과에 따른 신갈나무의 잠재분포 범위와 생장의 변화 추이를 평가하였다. 이와 함께 기후변화 시나리오 RCP 4.5와 RCP 8.5를 적용하여 2011년부터 2100년까지 연도별 생장도일과 온도효과지수를 산출하여, 기후변화에 의한 신갈나무의 잠재분포 범위와 생장의 변화를 예측하였다. 신갈나무가 현재 분포하고 있는 지역의 생장도일을 연도별로 산출하여 비교한 결과 위도와 해발고도가 낮은 지역은 시간이 경과함에 따라 신갈나무에 적합한 생육가능 범위를 벗어나는 것으로 분석되었다. 특히 기후변화 시나리오를 적용할 경우 지속적인 기온의 상승으로 인해 2050년 이후에는 잠재분포의 변화뿐만 아니라 생장에도 큰 지장을 주는 것으로 평가되었다.

• 한국환경복원기술학회지
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• 제22권3호
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• pp.1-14
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• 2019

With a view to developing a database of death years of Korean firs (Abies koreana) at Yeongsil in Mt. Halla and investigating their abrupt inter-annual growth reduction tree-ring analysis was employed. To this end, 10 living trees (YSL) were selected to establish a master chronology and 20 dead trees were used to date their dead years. To investigate the difference in death years by death types, 10 trees, which remained standing (YSSD) out of the 20 dead trees were selected. The rest 10 dead trees were already fallen (YSFD). Two increment cores per tree at breast height were extracted in contour direction using an increment borer. A 106-year master chronology (1911-2016) was successfully established from the 10 YSLs. Through cross-dating between individual YSSD time series and the master chronology, it was verified that 1 YSSD was dead in summer 1978, 1 YSSD between autumn 1999 and spring 2000, 2 YSSDs in summer 2007, 1 YSSD in summer 2010, 1 YSSD in summer 2012, and 1 YSSD in summer 2013. The youngest tree rings of 2 YSSDs having no bark were in 1977 and 2002. For the YSFDs, it was verified that 1 YSFD was dead between autumn 1997 and spring 1998, 1 YSFD between autumn 2001 and spring 2002, 2 YSFDs between autumn 2009 and spring 2010, 1 YSFD in summer 2010, and 2 YSFDs between autumn 2012 and spring 2013, while the youngest tree rings of 2 YSFDs having no bark were in 1989 and 2004. To note, the death years of two trees, one from each death type (YSSD and YSFD), could not be verified due to poor cross-dating with the master chronology. The inter-annual growth reductions of YSSD and YSFD occurred more frequently and intensively than YSL. Typically, the YSFD showed the most frequent and intensive inter-annual growth reduction. On comparing the inter-annual growth reductions with the corresponding records of typhoons however we could not find any reliable relationship. Finally, from prior reports and results of the current study it can be concluded that the death and abrupt growth reduction of korean fir at Yeongsil in Mt. Halla are not caused by only a certain environmental factor but various factors.

• 한국환경생태학회지
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• 제33권5호
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• pp.565-577
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• 2019

설악산 분비나무 개체군의 쇠퇴징후에 대한 요인과 군락의 변화 양상을 파악하기 위하여 귀때기청봉, 관모능선, 설악폭포지역에 고정조사구를 설치하였으며, 군락구조, 개체군동태, 비대생장 및 활력도 등을 2009년부터 모니터링 하였다. 설악폭포지를 제외한 3개 조사지는 아교목층이 수관층을 형성하는 3층구조를 보였다. 목본수종의 중요치에서는 분비나무, 눈측백, 신갈나무, 사스래나무, 당단풍나무 등이 주요 종으로 분포하였으며, 설악폭포지에 분포하는 분비나무의 중요치는 2009년 45.3%에서 2018년 36.8%로 가장 크게 감소하였다. 생육목의 개체수($DBH{\geq}5cm$)는 귀때기청봉2와 관모능선에서 각각 1,800개체/ha와 1,700개체/ha로 가장 많았으며, 지난 10년 동안 고사율은 귀때기청봉1과 설악폭포지에서 각각 38.3%와 35.3%로 매우 높게 나타났다. 분비나무 개체군의 흉고직경급 분포에서는 귀때기청봉1 지역에서 가장 안정적인 역 J자형의 분포를 보였다. 분비나무의 연평균 비대생장은 0.96~1.73mm/year 였으며, 활력도가 감소 추세를 보인 귀때기청봉2, 관모능선, 설악폭포 지역에서 비대생장은 대체로 생장이 저하되는 추세를 나타내었다. 향후 모니터링 과정이 지속적으로 이루어진다면, 아고산 식생의 보전과 관리를 위한 기초자료 확보가 가능할 것으로 생각된다.

• 한국기후변화학회지
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• 제9권3호
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• pp.293-302
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• 2018

This study was carried out to provide basic information on efficient preservation and management of an Abies koreana forest through analyzing the ecological characteristics by slope in Seseok, Mt. Jirisan. Soil moisture content at southern and northern slopes was 29.9% and 21.7%, respectively, and there was no significant difference among soil properties between southern and northern slopes. The importance value of A. koreana in the southern and northern slopes was high for tree and subtree layers, respectively. It is noteworthy that many seedling and saplings of A. koreana were present on the southern slope. The species diversity was 0.413 for the tree layer, 0.632 for the subtree layer, and 0.609 for the shrub layer on the southern slope and 0.396 for the tree layer, 0.783 for the subtree layer, and 1.215 for the shrub layer on the northern slope. Evenness and dominance ranged from 0.371 to 0.609 and 0.629 to 0.391 on the southern slope and from 0.380 to 0.968 and 0.620 to 0.032 on the northern slope, respectively. The mortality of A. koreana was 9.6% on the southern slope and 24.4% on the northern slope, a distinct difference between the slopes. The mortality type at two slopes was the highest proportion of standing dead. Annual mean tree ring growth of A. koreana on the southern slope (1.76 mm/yr) was higher than that on the northern slope (1.64 mm/yr).

• 한국산림과학회지
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• 제69권1호
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• pp.6-12
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• 1985

수간석해(樹幹析解)를 위한 계산시간(計算時間)을 크게 단축(短縮)시키면서 정확(正確)한 계산결과(計算結果)를 얻을 수 있는 전산화(電算化)프로그램을 BASIC어(語)로 개발(開發)하였다. 원판측정자료(圓板測定資料) 등은 사용자(使用者) 자신이 전산기(電算機)에 직접 입력(入力)시킬 수 있도록 하였으며, 자료목록(資料目錄), 단면적(斷面績), 령급별(齡級別) 수고(樹高), 각종 성장량(成長量)과 성장률(成長率) 등이 출력(出力)되도록 하였다. 이 때, 통나무 재적(材積)은 Huber식(式)에 의하여 계산(計算)하였으며 성장률(成長率)은 Pressler식(式)에 의하여 계산(計算)하였다. 본(本) 프로그램의 목록(目錄)은 부록(附錄) I과 같다.

• 대한화학회지
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• 제15권6호
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• pp.370-377
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• 1971

The Carbon-14 content in surface air at Seoul, Korea, was measured from February 1970 to August 1971 and a Larix Leptolepis, Gordon tree (Ip-Gal Namu) grown at Kwang-Nung, Kyunggi-Do, Korea, having 37 growth rings, was assayde for $^{14}C$. From the results of the surface air study, it was calculated that during the above period the inventory of excess $^{14}C$ in the atmosphere decreased with a half-time of 4.6 years. The overall yearly decrease was also checked. The tree-ring study showed that the tree's atmosphere was affected by $^{14}C$ from nuclear tests after 1956. In one study, atmospheric $CO^2$ samples were collected bi-monthly by the absorption of $CO^2$ in alkaline hydroxide solution. In the other, 5 year annual growth rings were assayed for radiocarbon. For the radioactivity measurement, carbon atoms in samples were converted to carbon atoms of benzene. The resulting benzene was taken as primary solvent for liquid scintillation counting.

• The Korean Journal of Ecology
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• 제21권2호
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• pp.125-131
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• 1998

Histological damage and growth inhibition of Pinus densiflora were analysed in different areas around the Metropolitan area of Seoul urban (heavily polluted), suburban (lightly polluted), and rural(unpolluted) areas. Soil properties of each area were also investigated. Contact angles of water droplet on needle leaves growing in polluted areas were lower than that in unpolluted area. Transpiration rates of needle leaves growing in polluted areas were more rapid than that in unpolluted area. These results represented that needle leaves growing in polluted areas were more susceptible to water deficit than that growing in unpolluted area was. Growths of annual ring of Pinus densiflora growing in polluted areas were lower than that in unpolluted area. On the other hand, soil pH in polluted areas was lower than that in unpolluted area. That is, the former was more acidified than that the latter was. Ca and Mg contents in polluted areas were lower than that in unpolluted area, while Al contents in polluted areas were higher than that in unpolluted area. These soil properties revealed that the effects of acid precipitates in urban and suburban areas were severer than that in rural area.

• 수산해양기술연구
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• 제49권3호
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• pp.261-269
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• 2013

The age and growth of the Pacific cod, Gadus macrocephalus were investigated using left sagittal otoliths of 682 individuals collected in the West Sea of Korea from January to December 2007. The seasonal changes in the ratio of an opaque zone to interval between annular rings revealed that the narrow translucent parts of the otolith were annual growth rings formed between February and March once a year. The spawning period was December to January and therefore the duration from fertilization to the complete formation of the opaque zone became thirteen months. From the parameters calculated using the average length when the year ring was formed, the estimated von Bertalanffy growth equations were $L_t=100.0(1-e^{-0.1640(t+0.5247)})$ for females and $L_t=64.6(1-e^{-0.3335 (t+0.3342)})$ for males when is total length in age t.