• 농약과학회지
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• 제11권1호
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• pp.32-37
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• 2007

항공방제시 비표적생물에 대한 안전거리를 설정하고자 벼의 주요 병해충인 도열병, 잎집무늬마름병, 벼멸구 및 나방류를 동시에 방제할수 있는 훼림존 트리싸이클라졸 액상수화제+비피유제+바리신액제와 헥사코나졸유제+이소란유제+파프유제의 3종 혼용농약을 항공 살포한 후 논물중 농약 잔류량과 수서생물 및 꿀벌에 미치는 영향을 조사하였다. 항공방제시 대상지역 이외의 포장으로 분무입자가 비산하는 정도는 바람부는 방향으로는 30 m, 반대방향으로는 20 m 이내로 비교적 비산 정도가 낮았다. 항공살포 후 살포지역내 논물중 농약의 잔류량을 조사한 결과 항공방제 6일후에는 논물 중에서는 농약이 검출되지 않았다. 항공방제 지역의 수서생물에 미치는 영향을 조사한 결과, 송사리와 미꾸라지는 방제지역 내외를 막론하고 모든 지점에서 치사되지 않았다. 물벼룩은 항공방제지역으로부터 10 m 지점 이내에 노출된 경우 48시간후 모두 치사되었으나 30 m 이상 지점에서는 영향이 없었다. 꿀벌은 바람부는 방향으로 50 m와 반대방향으로 20 m까지 $7{\sim}100%$ 치사하여 항공 방제시 안전거리는 수서생물의 경우 50 m, 꿀벌의 경우는 100 m로 설정하였다.

• 한국지구과학회지
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• 제39권6호
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• pp.555-567
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• 2018

본 연구에서는 서해 연안에서의 실측-위성 해수면온도 차이를 규명하고 그 특성을 분석하기 위해 GCOM-W1/AMSR2 마이크로파 해수면온도 자료와 서해 연안에 위치한 덕적도, 칠발도, 외연도 해양기상 부이의 실측 수온 자료를 활용하여 2012년 7월부터 2017년 12월까지 총 6,457개의 일치점 자료를 생산하였다. 5년 이상의 덕적도, 칠발도, 외연도 해양 부이 수온 자료와 AMSR2 해수면온도를 비교하여 정확도를 제시하였다. 마이크로파 위성 해수면온도와 현장 관측 부이 해수면온도 간의 차이는 풍속과 수온 등 환경 요인에 대한 의존성을 가지는 것으로 나타났다. 낮시간 풍속이 약할 때 ($<6ms^{-1}$) AMSR2 해수면온도는 실측 해수면온도보다 높게 산출되며, 밤시간에 대해서는 풍속이 커질수록 양의 편차가 증가함을 밝혔다. 또한 AMSR2 해수면온도와 실측 해양부이 수온 간의 차이가 증가하는 경향은 낮은 온도에서 마이크로파 센서의 민감도의 저하와 육지에 의한 자료오염과 관련이 있는 것으로 나타났다. 실측-위성 해수면온도 차이를 월별로 도시해본 결과, 마이크로파 위성 해수면온도의 편차는 강한 바람이 부는 겨울철에 가장 커진다고 알려져 있던 기존의 경향성과는 달리 덕적도, 칠발도 부이에서는 여름철 가장 큰 해수면온도 편차값이 나타났다. 이러한 차이는 부이의 위치에 따른 조석 혼합의 공간적 차등에 기인한 것으로 사료된다. 본 연구는 인공위성 합성장에 기여도가 높은 마이크로파 위성 해수면온도를 사용할 때 한반도 서해안에서 발생할 수 있는 문제점과 제한점을 제시하였다.

• 대한기계학회논문집
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• 제18권5호
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• pp.1322-1329
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• 1994

The effect of thermal stratification on the stratified flow past a circular cylinder was examined in a wind tunnel. Turbulent intensities, the rms values of temperature and turbulent convective heat flux as well as the velocity and temperature profiles in the cylinder wake with a strong thermal gradient of $200^{\circ}C/m$ were measured by using a hot-wire and cold-wire combination probe. It is found that the temperature field affects as an active contaminant, so that the vertical growth of vortical structure is suppressed and the strouhal number decreases with increasing the extent of stratification. And also, the wake structure can not sustain their symmetricity about the wake centerline and vertical turbulent motion dissipates faster than that of the neutral case when such a strong thermal gradient is superimposed. It is evident that the turbulent mixing in the upper half section is stronger than that of the lower of the wake in a stably stratified flow because the turbulent intensities and convective heat flux in the upper half section are larger than those of the lower half of the wake.

• 한국해양학회지
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• 제20권1호
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• pp.12-21
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• 1985

하계 동지나해에서 가장 중요한 해양학적 현상들을 재검토하였다. 계절적 수 온약층 상부 표층수는 태양가열과 주로 양자강으로 부터의 담수의 유입 그리고 하 계 계절풍에 의해 지대한 영향을 받고 있다. 수온약층 하부층에는 여러가지 해양역 학적 작용에 대한 질량장의 조정에 의해서 몇가지 분명히 구별되는 수괴들 즉 쿠로 시오 표층수, 서북태평양 중앙수, 황해저층 냉수등이 잠입되고 있다. 잠입된 황해저 층 냉수와 서북태평양 중앙수와의 전선역 혼합이 제주 남방 대륙붕상의 저층에서 일어난다. 이 혼합수는 제주 주변과 한국 남해안 중저층의 해수 특성에 커다란 영 향을 미칠 것으로 보인다.

• 한국대기환경학회지
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• 제10권1호
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• pp.41-48
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• 1994

A monitoring system for atmospheric CFC-12 and CFC-11 has been established at Mt. Kwan-Ak, Seoul National University (SNU) since July, 1991. The concentrations showed quite a large variation ranging from 495 to 37600 pptv (pptv=part per trillion, 10$^{-12}$ , v/v) for CFC-12 and from 233 to 12100 pptv for CFC-11 due to many local sources. However, monthly medians show rather limited ranges ; 553~765 pptv for CFC-12 and 301~431 pptv for CFC-11. Furthermore minimum concentrations could be defined relatively well during the whole period of observation. The regional background concentrations in 1993 near SNU wer estimated as 533 pptv for CFC-12 and 293 pptv for CFC-11. These values are very comparable to global averages in Northern Hemisphere, 523 pptv for CFC-12 and 287 pptv for CFC-11, reflecting the fast atmospheric mixing processes within the hemisphere. Examinations with meteorological parameters such as wind speed and direction suggest the possible measurement-window at SNU, appropriate for regional monitoring. Studies for improving the monitoring capability of the SNU station such as automation of the analysis system along with correlation with other meteorological parameters, are in progress at the present time.

• 환경영향평가
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• 제21권5호
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• pp.665-681
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• 2012

This study investigates the influence of anthropogenic heat (AH) release on urban boundary layer in the Gyeong-In region using the Weather Research and Forecasting model that includes the Seoul National University Urban Canopy Model (SNUUCM). The gridded AH emission data, which is estimated in the Gyeong-In region in 2002 based on the energy consumption statistics data, are implemented into the SNUUCM. The simulated air temperature and wind speed show good agreement with the observed ones particularly in terms of phase for 11 urban sites, but they are overestimated in the nighttime. It is found that the influence of AH release on air temperature is larger in the nighttime than in the daytime even though the AH intensity is larger in the daytime. As compared with the results with AH release and without AH release, the contribution of AH release on urban heat island intensity is large in the nighttime and in the morning. As the AH intensity increases, the water vapor mixing ratio decreases in the daytime but increases in the nighttime. The atmospheric boundary layer height increases greatly in the morning (0800 - 1100 LST) and midnight (0000 LST). These results indicate that AH release can have an impact on weather and air quality in urban areas.

• 한국연소학회지
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• 제4권2호
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• pp.23-33
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• 1999

A turbulent non-premixed ethylene flame, which was set up in a vertical wind tunnel, was examined to understand the effect of turbulent mixing on formations of soot and gaseous species in the flames. Temperature and velocity profiles were measured using uncoated thermocouples and LDV system. Gaseous samples were withdrawn by using a water cooled stainless iso-kinetic gas sampling probe. The samples for inorganic compounds and light hydrocarbons were collected with sampling bottles and were analyzed by a gas chromatography. The samples for aromatic hydrocarbons were collected on a sorbent tube and were analyzed on a GC/MS system. Some of main results were followed. CO and $CO_2$ were measured relatively in early part of flame and the concentration of CO was greater than that of $CO_2$ all over the early flame region due to the scavenging of the oxidizing species OH by soot particles. Aromatic hydrocarbons were measured at x/D=122 along the radial direction and main important species were benzene, xylene, toluene, styrene, indene, naphthalene. The peak points of these compounds occurred at r/D=0.8 apart from the center of flame, around in which the concentration of $C_2H_2$ decayed relatively rapidly from the maximum value.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2006년도 Proceedings of ISRS 2006 PORSEC Volume I
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• pp.118-121
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• 2006

Variations in the extent and dispersal of river plume are important in the study of coastal environment. The objectives of this study are to examine relationship between satellite detected plume area and river discharge and to clarify the temporal and spatial dynamic of plume from Tokachi River, Hokaido, Japan. We used 1.1 km spatial resolution of SeaWiFS normalized water-leaving radiance (nLw) images from 1998 to 2002. Supervised maximum likelihood classification was implemented to define classes of surface water optical properties. Satellite observed plume area was correlated to the amount of river discharge from April to October. First mode (44% of variance) of EOF analysis shows the turbid plume distribution resulting from re-suspension by strong wind mixing along the coast during winter. This mode also shows plume distribution along-shelf direction in spring and late summer. Second mode (17% of variance) shows spring pattern across-shelf direction due to strong discharge of snow melting water.

• Journal of Mechanical Science and Technology
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• 제15권7호
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• pp.895-905
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• 2001

This paper presents vector fields, three dimensional mean velocities, turbulent intensities, turbulent kinetic energy and Reynolds shear stresses measured in the X-Y plane of the gas swirl burner with a cone type baffle plate by using an X-type hot-wire probe. This experiment is carried out at the flow rates of 350 and 450ℓ/min which are equivalent to the combustion air flow rate necessary to release 15,000 kcal/hr in a gas furnace. The results show that the maximum axial mean velocity component exists around the narrow slits situated radially on the edge of a burner. Therefore, there is some entrainment of ambient air in the outer region of a burner. The maximum values of turbulent intensities occur around the narrow slits and in front of a burner up to X/R=1.5. Moreover, the turbulent intensity components show a relatively large value in the inner region due to the flow diffusion and mixing processes between the inclined baffle plate and the swirl vane. Consequently, the combustion reaction is expected to occur actively near these regions.

• 대한기계학회논문집
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• 제19권5호
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• pp.1340-1350
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• 1995

The effects of thermal stratification on the flow past a heated circular cylinder with various heating rates were examined in a wind tunnel. Turbulent intensities, r.m.s.values of temperature and turbulent convective heat flux distributions in the cylinder wakes with and without thermal stratification were measured by using a hot-wire and cold-wire combination probe. The phase averaging method was also used to estimate coherent contributions to the turbulent flow field in the near wake. The results show that the scalar mixing process is very different according to the mean temperature fields especially in the upper part of the wake. The coherent structure of the temperature field makes a large contribution to the time mean value like velocity components. However, the coherency of the temperature fluctuation is very different with the change of mean temperature fields, though the velocity coherent motions are quite similar in all experimental conditions.