일반적으로 배사에 비해서 준설은 경제적 부담이 크기 때문에 배사를 효율적으로 운영하는 것이 중요하다. 본 연구에서는 2차원 하상변동 모형 인 Nays2DH를 이용하여 홍수기 운영수위에 따른 배사효율을 낙동강에 위치한 달성보를 중심으로 분석하였다. 분석결과, 가동보의 수 만큼 배사 수로가 형성되었으며, 배사수로 상류에는 퇴적이 발생하는 것으로 나타났다. 또한, 홍수기 운영수위를 EL. 14.5 m로 운영하는 것이 EL. 14.0 m로 운영하는 것에 비해서 배사효율이 약 4.6% 증가하여 퇴사가 약 4.5% 감소하는 것으로 나타났다. 본 연구에서 분석한 홍수기 운영수위에 따른 배 사효율의 변화를 고려한다면, 저수지 퇴사 저감 및 준설주기의 장기화가 가능할 것으로 판단된
In this study, before and after sunset carbon dioxide concentration and air temperature were observed in two points of atmosphere (lower observation point of the GL + 0.1 m, the upper observation point of GL + 1.0 m) on the foreshore at located in Suncheon Bay and their variations were analyzed. Observation was performed on the foreshore on 2~4 August 2010. Instrument (VAISALA, GMP343) was set two hours before sunset and then observation was made continuously for six hours. In three days, observed carbon dioxide concentration was 375~419 ppm, and the air temperature was in the range of 28.7~32. 5℃. The average concentration of carbon dioxide was 388~399 ppm in the upper observation point and 386~396 ppm in the lower observation point. It was higher in the upper observation point and its fluctuations were similar in two observation points. Correlation coefficients between carbon dioxide concentration and air temperature in the upper observation point were in the range of –0.64~–0.88, and were calculated –0.65 to -0.90 in the lower observation point. For the carbon dioxide concentration, correlation coefficients between the upper part and the lower part were very high as 0.98 in three times. For the air temperature, correlation coefficients between the upper part and the lower part were very high as 0.97 and 0.99. In the same observation time, the slope of the linear regression function as carbon dioxide concentration in the lower observation point for the upper observation point was in the range of 0.97~1.01. Carbon dioxide concentration was slightly higher in the upper observation point. Because carbon dioxide in the lower observation point was closer on the surface of the foreshore and absorbed from atmosphere to the foreshore. In this study, it was showed that the vertical variation of carbon dioxide concentration was insignificant in the several meter scale of atmosphere on the surface of the foreshore.
열대지역에 적응하는 온대 자포니카 벼 품종 개발을 위한 이삭형질 개선의 육종 방향을 제시하고자 한국과 필리핀 우기재배에서의 이삭형질 변이 및 특성에 대해서 조사하였다. 이삭형질의 변이는 2차 지경 착생립수가 차이가 가장 많이 나는 형질이었고 1차 지경 평균립수가 가장 적게 나는 형질이었다. 2차 지경 관련 형질이 1차 지경 관련 형질보다 수당립수와의 상관관계가 높았다. 지역간 차이가 많이 난 형질은 2차 지경 립수, 2차 지경수, 수당립수, 총지경수 순
In order to monitor the impact of high temperature which is seen frequently with climate change, we investigated the monthly change in globe temperature, air temperature, mean radiant temperature and effective radiant heat flow, because the four well reflect thermal radiation from bio-meteorological aspect. Both globe temperature and air temperature showed an increasing trend every month. Compared to air temperature, globe temperature had a wider range of temperature change and was more influenced by meteorological element such as precipitation. Diurnal trends of air temperature, globe temperature and the difference between their temperature had the lowest value before the sunrise and the highest around 1300~1500 LST, showing the typical diurnal trends. Globe temperature and the difference between their temperature had a sharp increase around 1000~1100 LST, maintained high value until 1700 LST and then reclined, though varied by month. The difference between globe temperature and air temperature was highly dependent on the amount of precipitation and clouds. The duration in which globe temperature was higher than air temperature was the lowest in July. Therefore the amount of precipitation was the most affecting, followed by the amount of clouds and wind. In order to find out the diurnal trends of temperature in city center and city outskirts, we assumed the roof of a concrete building as a city center, and the grass-covered observatory of the Gimhae International Airport as city outskirts. The diurnal trends of temperature in the two sites showed a strong correlation. The highest and lowest temperature also had the same trend.
출수기와 성숙기가 다양한 계통포장에서 저 Amylose, 고단백계통을 선발하고자 할때 그 기준을 세우기 위한 한 방법으로 재배시기에 따른 Amylose 및 단백질함량의 계통간 변이양상을 구명하고자 포장과 온실에서 수차 또는 수년간 재배된 시료의 Amylose와 단백질함량의 계통간 변이를 검토하였다. 그 결과를 요약하면 다음과 같다. 1. 조생계통을 동일한 비료수준에서 시기를 다르게하여 포장에서 재배할 경우 단백질함량은 생육기간과 부의 상관이 있었고, 조기<보통기<만기재배 순으로 증가되었다. 2. 포장에서 재배시기가 다를 경우 Amylose 함량은 출수기가 늦어질수록 높아졌으나 생육기간과는 직접적인 관계가 없었다. 3. 온실내에서의 수확시기에 따른 단백질함량의 변이는 품종에 따라 달랐으나 3월부터 10월까지는 품종간 차이가 컸다. 4. 온실내에서 저 Amylose품종의 Amylose함량은 수확시기에 따라 변이가 컸고, 7월에 가장 낮았다. 고 Amylose계통은 수확시기에 따른 변이가 적었다. 5. 년차에 따라서 단백질함량은 변이가 적었다. Amylose함량은 저 Amylose계통에서는 고온인 해에 낮았으나, 고 Amylose계통에서는 년차에 따른 변이가 적었다.