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RISS 인기검색어
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- 저자 : 이동섭(Lee, Dong-Seop) (검색결과 287 건)
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이동섭,Lee, Tong-Sup 한국해양학회 1999 바다 Vol.4 No.4
여름과 겨울철 남해의 해수에 포함되어 있는 영양염의 분포 특성을 수온, 염분, 겉보기 산소 소모량, pH 등의 환경 인자들과의 상관도를 통해 파악하고자 하였다. 여름철에 영양염의 분포는 염분보다는 수온과 양호한 상관도를 보였으며 생물 활동과 관련이 갚은 pH, 겉보기 산소 소모량과 유의한 상관관계를 보였다. 이로 보아 여름철에 형성되는 염전선역에서 일차생산자에 의한 영양염 소비가 활발하여 염분과 영양염과의 상관성을 강력하게 변형시키는 것으로 판단된다. 겨울철에는 수온이 영양염과 가장 유의한 상관관계를 나타내어 수직 혼합된 냉수와 북상하는 난류의 세력이 만나는 열전선의 위치가 영양염 분포에 가장 중요한 요인으로 분석되었다. 여름철에 가장 우수한 상관도를 보였던 ($R^2$ >0.6) pH의 경우 겨울철에 생물 활동이 미약하여 상관도가 크게 낮아졌다($R^2$ <0.5). 수심에 대해 적분한 질산염+아질산염 인산염 규산염의 값은 각기 여름철에는 321 $mmol{\cdot}m^{-2}$, 23 $mmol{\cdot}m^{-2}$, 637 $mmol{\cdot}m^{-2}$이었고 겨울철에는 261 $mmol{\cdot}m^{-2}$, 31 $mmol{\cdot}m^{-2}$, 742 $mmol{\cdot}m^{-2}$로 계산되었다. 영양염의 질소 대 인의 비는 여름철에는 인이 상대적으로 부족한 반면 겨울철에는 이와 반대로 질소가 결핍되어 우기에 강우와 하천을 통한 질소의 유입이 남해 생태계 유지에 중요한 역할을 하는 것으로 판단된다. This paper presents the results of recent nutrients measurement and analysis in relation to other environmental parameters such as temperature, salinity, AOU and pH in the South Sea, Korea. In summer, temperature showed stronger correlation with nutrients than salinity and also did the parameters related to biological activities such as pH and AOU. Implications of above results exemplify that primary producers in the vicinity of salt front actively consumed nutrients so that nutrients-salinity correlation is strongly modified in the salt front. Nutrient in winter showed significant correlation only with temperature. Nutrient distribution seems governed by the location of thermal front between vertically mixed cold water in northern area and warm waters flowing north. Due to weak biological activity in winter pH-nutrients correlation, which was strongest in summer ($R^2$ >0.6) dropped sharply in winter ($R^2$ <0.5). Depth integrated nitrate+nitrite, phosphate and silicate values are 321 $mmol{\cdot}m^{-2}$, 23 $mmol{\cdot}m^{-2}$, 637 $mmol{\cdot}m^{-2}$ in summer and 261 $mmol{\cdot}m^{-2}$, 31 $mmol{\cdot}m^{-2}$, 742 $mmol{\cdot}m^{-2}$ in winter, respectively. NIP values in summer exhibit phosphorus deficiency, however, winter situation is reversed for nitrogen. Nitrogen input via precipitation and riverine discharge in wet season seems potentially critical for maintaining the South Sea ecosystem.
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이동섭,정영관 ( Dong Sup Lee,Young Gwan Chung ) 한국산림과학회 1986 한국산림과학회지 Vol.75 No.1
This study was initiated to estimate productivity of Quereus variabilis stand. However the practical objective of this study was to provide some information to establish the basis of selecting the suitable site for Quercus variabilis. The productivity measured in terms of DBH, height, basal area and stem volume was hypothesized, respectively, to be a function of a group of factors. This study considered 32 factors, 20 of which were related to the forest environmental factors such as tree age, latitude, percent slope, etc. and the rest of which were related to soil factors such as soil moisture, total nitrogen, available P₂O_5, etc. The data on 4 productivity measurements of Quercus variabilis growth and related factors cited were collected from 99 sample plots in Kyeongbook and chungbook provinces. Some factors considered were, in nature, discrete variables and the others continuous variables. Each kind of factor was classified into 3 or 4 categories and total numbers of such categories were eventually amounted to 110. Then each category was treated as an independent variable. This is amounted to saying that individual variable was treated a dummy variable and assigned a value 1 or 0. However the first category of each factor was deleted from the normal equation for statistical consideration. First of all, each of 4 productivity measurements of Quercus variabilis growth was regressed and, at the same time, those 110 categories. Secondly, the partial correlation coefficients were measured between each pair of 4 productivity measurements and 32 individual foctors. Finally, the relative scores were estimated in order to derive the category ranges. The result of these statistical analyses could be summarized as follows: 1) Growth measurement in terms of height seems to be a more significant criterion for estimation of productivity of Quercus variabilis. 2) Productivity of forest on stocked land may better be estimated Sn terms of forest environmental factors, on the other hand, that of unstocked land may be estimated in terms of physio-chemical factors of soil. 3) The factors that a strongly positive relation to all growth factors of tree are age group, effective soil, soil moisture, etc. This implies that these factors might effectively be used for criteria for selecting the suitable site for Quercus vdriabilis. 4) Patent rock, latitude, total nitrogen, age group, effective soil depth, soil moisture, organic matter, etc., had more significant category range for tree growth. Therefore, the. suitable site for Quercus variabilis may be selected, based on this information. In conclusion, the above results obtained by the rnultivsriable analysis can be not only the important criteria for estimating the growth of Quercus variabilis but also the useful guidance for selecting the suitable sites and performing the rational of Quercus variabilis forest.
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이동섭,김일남,강동진,김동선,Lee, Tong-Sup,Kim, Il-Nam,Kang, Dong-Jin,Kim, Dong-Seon 한국해양학회 2007 바다 Vol.12 No.3
울릉분지의 일부 저층수에서 아질산염의 존재가 확인된 것은 용존산소가 매우 풍부한 환경에서 예상되지 않던 결과로서 괄목할만한 사실이었지만 과학적으로 설명되지 않았다. 오캄의 제안에 따르면 가능한 몇 가지 설명 가운데 대륙사면 표층 퇴적물 안에서 일어나는 탈질산화의 중간산물로써 해수로 유출되는 것이 제반 여건과 가장 잘 부합된다. 그런데 울릉분지에서는 이런 탈질산화에 따른 무기질소의 손실을 보상하는 특별한 방법이 존재하지 않은 것으로 보이며 이는 현재 심해수의 낮은 질소: 인의 비와 일맥상통한다. 여기에 열염순환을 약화시키는 온난화의 효과가 가중될 경우 현재의 생물펌프가 위축될지 또는 현재 식물플랑크톤 군집을 대체하는 새로운 군집으로 바뀌게 될지도 모른다. 그 경우 이는 동해 생태계가 직면하게 될 심각한 도전이 될 것이다. 한편으로는 수중에 산화제가 풍부함에도 불구하고 표층 퇴적물의 유기탄소함량이 아주 높게 나타나서 울릉분지에서 질소(유기물)의 순환에 대해 풀리지 않는 문제가 여전히 남아있다. Presence of bottom water nitrite in the Ulleung Basin was remarkable because it is totally unexpected phenomenon at such an oxygen-rich environment. Yet no scientific explanation was set forward. Of several plausible explanations, following the Ockham's suggestion, a leaching of nitrite as an intermediate product of denitrification in the top sediment at the slope is most agreeable to given environmental settings. There seems no complementary process to make up the loss of N in the Ulleung Basin, which seems contribute to the characteristically low N:P ratio in the deep waters. If warming proceeds that weakens the thermohaline circulation, a current biological pump may stall and the phytoplankton assemblage might replaced drastically. If so this will pause an utmost challenge to the ecosystem of the East/Japan Sea. Still there remains a contradictory sedimentary signature that requests further explanation regarding the N (or organic C)-cycle such as extraordinarily high organic carbon content despite abundant oxidants in the overlying waters.
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이동섭,김준모,우경인,장혜란,Dong Sub Lee,Joon Mo Kim,Kyung In Woo,Hae Ran Chang 대한안과학회 2006 대한안과학회지 Vol.47 No.9
Purpose: To determine postoperative astigmatic changes after surgery for congenital ptosis and the astigmatic changes depending on surgical method and to discern cases of postoperatively developed anisometropia or amblyopia. Methods: Fifty-one patients who underwent surgery due to congenital ptosis were reviewed. Refraction or cycloplegic refraction was conducted preoperatively and 3 to 6 months after surgery to measure astigmatic changes. Astigmatic changes in operated eyes were compared to control eyes. Astigmatic changes were compared depending on surgical method. Results: The mean astigmatism was 1.33±1.29D preoperatively and 1.48±1.13D postoperatively (P=0.10) and the mean astigmatic change in the ptotic and control eye was an increase in cylinder +0.56±0.55D and +0.68±0.72D (P=0.37). The mean astigmatic change of patients receiving frontalis sling was +0.57±0.67D which was similar to those who received levator resection (+0.56±0.50D). Newly developed anisometropia was found in three patients postoperatively due to an increase in astigmatism, but newly developed amblyopia was not found. Conclusions: The increase of astigmatism by ptosis surgery was not statistically significant and there was no statistically significant difference when accounting for surgical method. However, it is necessary to monitor refractive error carefully in younger patients to prevent amblyopia because postoperative increase of astigmatism can cause anisometropia.
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동해 난수역의 일차생산에 대한 대한해협 유입 영양염의 기여
이동섭,노태근,Lee, Tongsup,Rho, Taekeun 한국해양학회 2013 바다 Vol.18 No.2
대륙주변해인 동해의 일차생산력은 조사하기 쉬운 듯하지만 해황의 역동적 변동성 때문에 현장 관측으로 파악하기 매우 어렵다. 이 연구에서는 난수역의 평균적인(총)일차생산 배경값을 생지화학적 가설에 기반하여 추정하였다. 계산에 사용된 비혼합-부상 가설은 일단 일차생산이 오로지 대한해협을 통해 수송된 영양염에 의해서만 일어난다고 가정했을 경우로서, 결과($209\;gC\;m^{-2}\;y^{-1}$)는 발표된 위성기반 순일차생산력과 대등한 것으로 나타났다. 그런데 일차생산이 100% 신생산에 의존한다고 가정했었기 때문에 이 구속을 풀어 신생산지표를 0.6이라 가정하면 일차생산력은 40% 가량 높아진다. 결과는 오로지 대한해협을 통해 유입되는 영양염만으로도 기존에 알려진 일차생산을 지지하고도 남음을 말해준다. 그런데 배경값을 구하기 위해 배제시켰던 여러 가지 변동 요인들, 예컨대 용승, 지하수 유입, 대기 유입, 해양 투기, 태풍 등 배경에 더 해지는 교란은 모두 일차생산을 추가로 부양하는 요인이고, 여기에 아직 정량화 되지 못한 초미소남세균의 광합성에 대한 기여까지 고려하게 되면 실제 일차생산력은 배경값의 두 배 이상도 가능할 것으로 추정된다. 이 경우에 일차생산력은 신생산지표가 0.6으로 알려진 페루 용승역과 비등한 규모가 된다. In situ measurement of a primary production in East Sea, a marginal sea with a fair accessibility, is nonetheless an arduous task because of dynamic variability. In this study, we estimated the mean value of background (gross) primary production over the warm region of the East Sea based on a biogeochemical hypothesis. We propose an immiscible-shoaling hypothesis for the estimation of primary production, which assumes that primary production in the warm region occurred only by the nutrient supply through the Korea Strait. Annual primary production thus estimated is $209\;gC\;m^{-2}\;y^{-1}$, which is comparable to the satellite-based estimates of net primary production in the region. However, since this hypothesis assumes that primary production is based on only the new nutrients supplied to the system, primary production would increase by 40% if we release the assumption, and assume f = 0.6. This suggests that nutrient influx through the Korea Strait alone is more than enough to support primary production previously reported. Primary production may increase as much as two times if we considered other external perturbations excluded intentionally to estimate the background level of primary production, such as coastal upwelling, submerged ground water discharge, aeolian input, ocean dumping, and mixing by typhoons as well as the contribution of cyanobacteria that has not been quantified in the region. This implies the primary production in the warm region of the East Sea would be comparable to that of the Peru upwelling region with f = 0.6.
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