This study shows that the vertical migration speed of sound scattering layers (SSLs), which is distributed in near Funka Bay, were measured by 3D velocity components acquired from a bottom moorng ADCP. While the bottom mooring type has a problem to measure the velocity vectors of sound scattering layer distributed near to surface, both the continuous vertical migration patterns and variability of backscatterers were routinely investigated as well. In addition, the velocity vectors were compared with the vertical migration velocity estimated from echograms of Mean Volume Backscattering Strength, and estimated to produce observational bias due to SSLs which is composed of backscatterers such as euphausiids, nekton, and fishes have swimming ability.

토양중 유기물 함량 차이에 따른 토양내에서 carbofuran과 ethoprophos의 약효 변화, 수직 이동성 및 잔효성에 미치는 영향을 조사하기 위하여 고구마뿌리혹선충 (Meloidogyne incognita)을 공시하여 실험하였다. 두 약제 모구 토양중 유기물 함량이 많을수록 약효는 감소였다. 약제의 수직이동성은 토양 표면에서 0~2cm층에서는 유기물의 함량에 관계없이 두 약제 모두 80%이상의 높은 방제가를 보였으나, 2~4cm층에서는 유기물의 함량에 관계없이 두 약제 모두 80%이상의 높은 방제가를 보였으나, 2~4cm 층에서는 두 약제의 방제가가 다르게 나타났다. Carbofuran의 경우 유기물 함량에 따라 10~30%의 방제가를 나타냈으나, ethoprophos는 0.4% 유기물 토양에서만 약 30%의 방제가를 나타냈으며, 나머지 유기물 토양에서는 효과가 거의 없었다. 또한 4cm 이하의 토양에서는 carbofuran은 대부분의 토야에서 5~20%의 내외의 약효를 나타냈으나, ethoprophos은 거의 나타내지 않았다. 따라서 , 두 약제 중에서 토양중 이동성은 carbofuran이 더 큰 것으로 나타났다. 토양중 유기물 함량은 두 약제의 잔효지속기간에 큰 영향을 주었으며, 유기물 함량이 증가함에 따라 약효지속기간이 감소하였다. 약효의 반감기는 carbofuran의 경우 유기물 함량이 0.4%인 토양에서는 2~3주로 나타났으나, 0.8%, 1.6% 토양에서는 1주 정도였다. 한편, ethoprophos의 경우 0.4%, 0.8%의 토양에서는 3~4주, 1.6%인 토양에서는 1~2주로 나타났다. 그러나 두 약제 모두 3.2%의 유기물함량 토양에서 약제의 효과가 거의 나타나지 않았다.

The speed of vertical migration and the volume backscattering strength of the scattering layers during the evening and morning transitions between day and night were measured in November 1990-1992 in thermally stratified waters of the East China Sea. Acoustical measurements were carried out using a scientific echo-sounder operating at t재 frequencies of 25 and 100kHz, and using an echo-integration system connected with a micro-computer. Biological sampling was accomplished by bottom trawling to identify fish species recorded on the echo sounder, and the species and length compositions were determined. The values of scattering strength were allocated to group of fishes according to the fish traces on the echo recording paper and the species composition of trawl catches. The vertical velocities of migration derived from the changes in the depths and the values of peak scattering strength of the dense layer vertically migrating toward the bottom or toward the surface. The trawl data suggest that snailfish and fishing frog were the most abundant fishes in all research stations. As sunrise approached, the fish formed a strong concentration just above the thermocline. The the highest values of scattering strength in the entire water column appeared in the depth strata above the thermocline just before the begining of downward migration. As soon as the fish began to migrate downwards across the thermocline, the values of the scattering strength in the depth strata above the thermocline rapidly decreased, while the values for the scattering layer moving slowly toward the bottom gradually increased. During the 1992 surveys, the speed of the vertical migration was estimated to be 0.38m/min in the upward migration and 0.32m/min in the downward migration, respectively. That is the rate of vertical migration was slightly higher at dusk than at dawn. Similar migration patterns were observed on different stations and under different weather conditions during the surveys in 1990.