• Fisheries and Aquatic Sciences
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• 제11권2호
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• pp.103-112
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• 2008

Compressional sound velocities of shelf sediments in the South Sea of Korea, were measured in situ and in the laboratory for six cores. In situ sound velocity was measured using the Acoustic Lance (frequency of 7.5-15 kHz), while laboratory velocity was measured by the pulse transmission technique (frequency of 1MHz). Physical properties were relatively uniform with sediment depth, suggesting little effect of sediment compaction and/or consolidation. Average in situ velocity at each core site ranged from 1,457 to 1,488 m/s, which was less than the laboratory velocity of 1,503 and 1,604m/s. In muddy sediments the laboratory velocity was 39-47 m/s higher than in situ velocity. In sandy sediments, the difference was greater by an average of 116 m/s. Although the velocity data were corrected by the velocity ratio method based on bottom water temperature, the laboratory velocity was still higher than the in situ velocity (11-21 m/s in muddy sediments and 91 m/s in sandy sediments). This discrepancy may be caused by sediment disturbance during core collection and/or by the pressure of Acoustic Lance insertion, but it was most likely due to the frequency difference between in situ and laboratory measurement systems. Thus, when correcting laboratory velocity to in situ velocity, it is important to consider both temperature and frequency.

• 미생물학회지
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• 제21권2호
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• pp.79-85
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• 1983

Ammonia oxidation activity of polluted water samples in Jinhae Bay and isolated strain from the seawater was investigated, and effects of environmental factors such as temperature, salinity, substrate concentration to the ammonia oxidation were also investigated. The ammonia oxidation activities of sediments, 0.01-0.04mg eq. $NO_2-N/l/h$, were exceptionally higher than that of sea water, $0.5{\sim}1{\mu}g$ eq. $NO_2-N/l/h$. the activities of muddy sediments at station 4 and 2 were 0.03~0.04mg eq. $NO_2-N/l/h$ and that of sandy sediment at station 3 was 0.002mg eq. $NO_2-N/l/h$. In the case of sea water, the activity of polluted area, station 1, was 2 times higher than that of offshore, station 4. The isolated strain reached log phase after 30days culturs and its oxidation activity was $2{\sim}3{\mu}g$ eq. $NO_2-N/day$. The maximum oxidation of ammonia by IA 13 strain occured at 30mg/l oxidation increased with the salinity rising up to 100% seawater concentraion. And temperature for maximum oxidation of ammonia was $35^{\circ}C$. the oxidation increased with the salinity rising up to 100% seawater concentration.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2023년도 학술발표회
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• pp.399-399
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• 2023

한강상류 비점오염원관리지역은 장기간 나지로 방치되고 있는 고랭지밭이 집중 분포하고 있어, 강우시 다량의 흙탕물 발생으로 인해 하천 환경오염 및 상·하류 지역사회간 갈등 문제가 지속적으로 발생하고 있다. 이러한 강우시 흙탕물로 인해 하류지역 주민들은 심각한 피해를 호소하므로 상·하류 지역간 갈등을 해소하기 위해서라도 상류지역에서 발생한 흙탕물이 어디까지 도달하는지에 대한 과학적 평가가 요구된다. 하지만, 상류부터 하류 사이에는 많은 유입 지류하천이 존재하고 있어, 실측을 통해 흙탕물의 거동을 파악하기에는 한계가 있다. 이러한 한계를 극복하고 유사거동을 파악하기 위해서는 강우시 실측 모니터링과 수질 모델링을 통한 흙탕물 거동 특성 평가가 필요하다. 현재, 자운지구에서 발생한 흙탕물은 내린천을 거쳐 소양호까지 영향을 미치고 있으나, 실제 상류유역에서 발생한 흙탕물이 하류 유역에 미치는 영향을 정량적으로 평가하고 흙탕물의 거동특성을 파악한 연구는 전무하다. 이에 본 연구에서는 자운지구를 포함한 내린천유역을 대상으로 강우시 실측 모니터링을 수행하고 수질 모델링을 통해 흙탕물의 거동특성을 평가하였다. 강우시 실측 모니터링 자료와 SWAT 모형을 활용하여 흙탕물 거동특성을 분석한 결과, 상류유역에 해당하는 자운지구에서 발생한 유사가 하류지역인 내린천까지 이동하고 있는 것으로 모의가 되었으며, 내린천의 유사 이동량은 448,986 ton으로 이중 자운지구에서 발생한 유사량은 9.7%의 기여도를 가지는 것으로 분석되었다.

• 한국작물학회지
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• 제46권3호
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• pp.215-220
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• 2001

본 연구는 혀의 분얼최성기의 관수스트레스 시 탁도(청수, 반탁수, 탁수) 및 관수시간에 따라 반응하는 단백질, 지방산 조성 및 지질과산화(malodialdehyde)를 정량하여 관수에 따른 생육장해 및 그 작용기작을 구명하여, 관수에 따른 생화학적 대사의 기초자료를 제공하고자 실시되었다. 관수스트레스에 의해 가용성단백질은 약 20%가 감소하였다. 특히 탁도가 높고 관수시간이 경과할수록 급격히 감소하였으며, 관수 36시간부터 감소량이 크게 나타났다. 단백질 전기영 동패턴은 관수스트레스에 따라 생성이나 소멸한 펩타이드는 없었으나 약 53Kd부위의 폴리펩타이드는 관수초기부터 함량이 증가하였고, 약 28Kd는 48시간, 54시간에서만 함량이 증가하였다. 관수스트레스에 의한 지질의 과산화정도는 약 150%가 증가하였고, 탁도처리에서 청수와 반탁수간의 차이는 작은 경향이었지만, 관수 60시간에서 약 160-180%가 증가하였다. 그러나 탁수에서는 관수초기부터 malondialdehyde함량이 높았고, 36시간이후부터는 약 190-200%로 급격히 증가하였다. Catalase는 탁도가 높고 처리시간이 경과할수록 활성은 급격히 증가하였다. 관수 48시간을 기준으로 catalase 활성변화가 크게 나타났다. 지방산조성의 변화는 포화지방산의 조성비율은 증가하고 불포화지방산은 감소하였다. 특히 불포화지방산 중 monounsaturated은 증가하였고 polyunsaturated의 상대적인 조성비율은 감소하였다. Double bond index는 탁도가 높을수록 관수기간이 경과할수록 감소폭은 커서 불포화정도가 떨어짐을 나타냈다.

• 한국작물학회:학술대회논문집
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• 한국작물학회 2017년도 9th Asian Crop Science Association conference
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• pp.227-227
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• 2017

This study was conducted to analyze the reduction of quality and ripening rate of rice due to submergence during ripening stage and identify the physiological cause. Korean japonica type rice cultivars, Nampyeong was used in the experiment. The following 7, 14 day after heading, they were then moved into submergence treatment facility and we conducted the tests under three different submergence conditions - T1(clear water and overhead submergence), T2(Muddy water and exposure of Flag leaf end ), T3(Muddy water and overhead submergence), and the treatment lasted for 4days. The decrease of ripening rate was most severe in T3 treatment at 7days after heading, and the decrease of head rice ratio was most severe in T3 treatment at 14days after heading. Meanwhile the starch synthesis was inhibited, as the supply of assimilation products was inhibited in grain during the submergence treatment. And in stem, sucrose content was increased because the soluble carbohydrates accumulated before heading were decomposed. These changes may be due to the consumption of respiratory substrate in anaerobic conditions and the inhibition of the production of photosynthetic products by light interception. In order to see what kind of reaction occurs at the molecular level, we examined the degree of RNA expression in grain, stem and leaf. First, the expression of rna associated with starch synthesis in grain was decreased in all submergence treatment. and especially Ospul(DBE) was more decreased in 14days after heading treatment than 7days after heading treatment. This difference can explain the result that the decrease of head rice ratio was more severe at 14days after heading. And in stem, the expression of rna associated with the supply of assimilation products was decreased in submergence treatment. Finally in leaf, the expression of rna(ADH, ALDH) associated with anaerobic respiration was increased, while the expression of rna associated with photosynthesis was decreased. These results of physiological analysis can used to develop the cultivation technique and to offer the information for breeding the cultivars with tolerant characteristics to submergence stress during ripening stage in rice.

• 한국지리정보학회지
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• 제8권3호
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• pp.65-73
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• 2005

임하호 유역의 지질은 점토질 및 셰일층으로 구성되어 있기 때문에 강우발생시 흙탕물의 형태로 많은 토립자가 호소로 유입되므로 호소내 탁도관측자료는 유역내 토사유실을 평가하는 간접지표가 될 수 있다. 본 연구에서는 GIS 기반토사유실모델을 활용하여 연토사유실량을 평가하였으며 월별로 토사유실량을 배분하기 위해 시우량자료를 이용한 강우가중치 기법을 적용하였다. 2003년도 탁도자료를 볼때, 강우가중치에 의한 월별토사유실량 방법이 강우량자료에 의한 월별토사유실량 보다 더 효과적임을 알 수 있었다.

• The Korean Journal of Ceramics
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• 제2권4호
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• pp.212-215
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• 1996

This paper focuses the strength and wear resistance of CVD diamond films. The strength of free-standing CVD diamond films synthesized by microwave plasm CVD, DC plasma CVD, RF plasma CVD and arc discharge plasma jet CVD has been measured by three-point bending test. The wear resistance of CVD diamod films has been evaluated by the pin-on-disk type testing. diamond films coated on the base of sintered tungsten carbide pin by hot filament CVD have been rubbed with a sintered diamond disk in muddy water. Volume removed wear of CVD diamond has been compared with stellite, WC alloy and bearing steel.

• Animal Systematics, Evolution and Diversity
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• 제36권3호
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• pp.264-267
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• 2020

Thaumatometra tenuis (A. H. Clark, 1907), an unstalked crinoid that lives on the muddy bottoms of the deep sea, is re-described with images in this study. This species distributes in the cold water zone of the northwestern Pacific and had been reported at the end of 1800s from South Korea but had not been found thereafter. So we thought that this species was no longer living in Korea. In March 2019, a large number of T. tenuis were found near the Sokcho-si, Gangwon-do, Korea. So the presence of T. tenuis in Korea is reconfirmed. This species, markedly fragile overall, is characterized by long segments of cirri and pinnules, and P₁ composed of 35 segments.

• 한국지구과학회지
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• 제44권4호
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• pp.264-274
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• 2023

The Korea Strait comprises a continental shelf in a shallow sea that experienced glacio-eustastic sea-level changes during the Quaternary period. A long core of 76.6 m in length was acquired at the South Sea Drilling Project site (SSDP-101; 34°19.666'E and 128°16.335'N) with a 60 m water deep. The uppermost massive sand beds were interpreted as sandy sediments of the nearshore marine sand ridge in the shallow sea during the transgression of sea level, whereas the lower parts of alternating sandy and muddy beds were interpreted as deposits in marsh, estuary, and tidal flat environments. A three-layered geoacoustic model was reconstructed for the sedimentary succession in the high-resolution seismic profile based on a 140-grain size and sediment type of core SSDP-101. For the actual underwater simulation and experiments, the in-situ P-wave speeds were calculated using the sound speed ratio of the Hamilton method.

• Ocean and Polar Research
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• 제24권1호
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• pp.55-61
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• 2002

Eelgrass, Zostera marina L. widely spreads throughout all the coastal areas of the Korean Peninsula. However, some previously reported eelgrass populations disappeared. The disappearance was probably caused by anthropogenic disturbance such as reclamation and pollutant or exceeded nutrient release. Eelgrass beds occurred from the intertidal to the subtidal zone, mainly in lagoon, estuaries, ports, barrier reef and bays. Eelgrass beds were also found at the intertidal mud and sand flats, subtidal mud and sandbank in more exposed areas. Habitat characteristics of eelgrass beds distributed on the coasts of the Korean Peninsula varied among coast areas. Eelgrass distributed constantly throughout the southern coast of Korea, while the distribution was limited at lagoon, bay, port, or barrier reef on the eastern coast, because of steep water depth and high wave energy in that coast. On the western coast, eelgrass mainly appeared at the intertidal and subtidal zones in islands. Sediment characteristics of the Z. marina beds varied with locality, tidal current and water motion. Sediments of Z. marina beds were composed of sand, muddy sand, sandy mud and mud. Mean grain size ranged from 1.5 to 4.1 phi.