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  * 구축 학술지 : 한국해양학회지, Journal of the Korean Society of Oceanography, 한국해양학회지, 바다, Ocean Science Journal


Fig. 6. The distribution of harmonic constants of various mean sea levels
[논문정보] 한국연안의 월평균해면의 변화에 대하여
Table 5. Positions and reference levels at each oceanographic stations
[논문정보] 한국연안의 월평균해면의 변화에 대하여
Fig. 7. Correlations between monthly means of observed mean sea levels (ΔH') and steric sea levels. (ΔH'.)
[논문정보] 한국연안의 월평균해면의 변화에 대하여
Table 6. Harmonic constants of Sa and Ssa tides
[논문정보] 한국연안의 월평균해면의 변화에 대하여
Fig. 1. Stations de l'hydrologie et de peches de plancton effectuees en fevriermars 1967 dans la mer coreenne. Croix: Hydrologie, cercles: plancton
[논문정보] 동계 한국근해의 수괴지표성 모악류
Fig. 2. Isothermes(trait plein)et isohalines(trait interrompu)de surface dans la mer coreenne en fevrier-mars 1967
[논문정보] 동계 한국근해의 수괴지표성 모악류
Fig. 3. Repartition de Sagitta elegans recolte par filet NORPAC en vartical par rapport au tracedes isothermes dans la mer coreenne en fevrier-mars 1967. Trait, plein: courant chaud, trait. Interrompu: courant froid.
[논문정보] 동계 한국근해의 수괴지표성 모악류
Fig. 4. Repartition de Sagitta bedoti et de quotre Chaetognathes (lignes 315 et 316) recolte par filet NORPAC en vertical par rapport au trace des Isothermes (50m) dan la mer coreenne. Trait. Plein: courant chaud, trait: interompu: courant froid.
[논문정보] 동계 한국근해의 수괴지표성 모악류
Fig. 5. Distribution geographique de quatre especes des Chaetognathes a la mer coreenne en hiver, 1967. D. Sagitta minima, E. S. enflate, F. S. serratodentata, G. Pterosagitta draco
[논문정보] 동계 한국근해의 수괴지표성 모악류
Fig. 6. Repartition de Sagitta recolte par filet NORPAC en vertical par rapport au trace des isohalines (50m) dans la mer Coreenne. Trait. Plein: courant chaud, trait. Interrompu: courant froid, double trait: courant cotier ouest Correen
[논문정보] 동계 한국근해의 수괴지표성 모악류
Fig. 1. Vertical profiles of pH, oxygen, temperature, salinity, total alkalinity/salinity ratio at 53˚46'N, 158˚36'W on 7 July 1966 (Hydrographic station AKH-16 of YALOC-66 cruise on R/V YAQUINA)
[논문정보] The Processes Contributing To The Vertical Distribution Of Apparent pH In The Northeastern Pacific Ocean The Processes Contributing To The Vertical Distribution Of Apparent pH In The Northeastern Pacific Ocean
Fig. 2. Apparent oxygen utilization (AOU) vs. pH for the hydrographic station AKH-16. Apparent pH was measured aboard R/V YAQUINA under one atmosphere at 25℃. Calculated slope of -0.50 is from equation (9): Upper slope follows deep water of the depth greater than 1,250 m and the lower slope for the water shallower than 250 m. Negative AOU is observable near the surface
[논문정보] The Processes Contributing To The Vertical Distribution Of Apparent pH In The Northeastern Pacific Ocean The Processes Contributing To The Vertical Distribution Of Apparent pH In The Northeastern Pacific Ocean
Fig. 3. Comparison of the vertical profiles of AOU and pH in the upper 1,800 m. Note the almost constant AOU between the depths of 250 and 1,250 m. The increase in apparent pH in the same depths (shown by the shaded area) is mainly due to the carbonate dissolution
[논문정보] The Processes Contributing To The Vertical Distribution Of Apparent pH In The Northeastern Pacific Ocean The Processes Contributing To The Vertical Distribution Of Apparent pH In The Northeastern Pacific Ocean
Fig. 4. Total alkalinity/ salinity ratio vs. pH for the hydrographic station AKH-16. The calculated slope of 0.025 is from equations (11) and (12). The field data agree with the slope in the depth range of 250 m to 1,250 m where AOU is essentially invariant.
[논문정보] The Processes Contributing To The Vertical Distribution Of Apparent pH In The Northeastern Pacific Ocean The Processes Contributing To The Vertical Distribution Of Apparent pH In The Northeastern Pacific Ocean
Fig. 5. Vertical profiles of the AOU effect (left), the carbonate dissolution effect (right) and the net effect on pH for the hydrographic station AKH-16. The net effect is obtained by summing both the AOU and carbonate dissolution effects. The dots are pH I measured at 25℃.
[논문정보] The Processes Contributing To The Vertical Distribution Of Apparent pH In The Northeastern Pacific Ocean The Processes Contributing To The Vertical Distribution Of Apparent pH In The Northeastern Pacific Ocean
Fig. 1. Isolate #271 in type growth. An arthrospore is shown at 'A' and normal transverse fission is shown at 'B'
[논문정보] Polymorphism Of A Deep Marine Benthic Bacterium From The Gulf Of Mexico Polymorphism Of A Deep Marine Benthic Bacterium From The Gulf Of Mexico
Fig. 2. Isolate #271 in its typical myceloid form. Four myceloid filaments can be seen attached to the hold-fast organelle at 'A'. Active release of the medium length rods from a filament is shown at 'B' and a thin section of empty sheath is shown at 'C'. Septa can be seen at 'D'
[논문정보] Polymorphism Of A Deep Marine Benthic Bacterium From The Gulf Of Mexico Polymorphism Of A Deep Marine Benthic Bacterium From The Gulf Of Mexico
Fig. 3. An artist's conception of typical myceloid growth based on the microscopic field photographed in Fig. 2. This sketch clearly illustrates the process of cell release from the myceloid filaments as it has been observed microscopically. (Phelps Brown, artist)
[논문정보] Polymorphism Of A Deep Marine Benthic Bacterium From The Gulf Of Mexico Polymorphism Of A Deep Marine Benthic Bacterium From The Gulf Of Mexico
Fig. 4. The production of a cystite at the terminal end of a myceloid filament.
[논문정보] Polymorphism Of A Deep Marine Benthic Bacterium From The Gulf Of Mexico Polymorphism Of A Deep Marine Benthic Bacterium From The Gulf Of Mexico
TABLE 1. Cytochemical and biochemical properties of isolate #271
[논문정보] Polymorphism Of A Deep Marine Benthic Bacterium From The Gulf Of Mexico Polymorphism Of A Deep Marine Benthic Bacterium From The Gulf Of Mexico
TABLE 1. Continued. Cytochemical and biochemical properties of isolate #271
[논문정보] Polymorphism Of A Deep Marine Benthic Bacterium From The Gulf Of Mexico Polymorphism Of A Deep Marine Benthic Bacterium From The Gulf Of Mexico
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