군락 광합성 모델의 도출을 위하여 생육 챔버가 필요하며, 이를 위한 광합성의 효율적인 측정 방법이 필요하다. 본 연구의 목적은 내부 환경 제어가 가능한 생육 챔버를 이용하여 광도 및 이산화탄소 농도 변수를 갖는 로메인 상추(Lactuca sativa L.)의 군락 광합성 곡선을 도출하는 방법을 확립하는 것이다. 실험에 사용한 상추는 식물공장 모듈에서 재배되었으며, 군락 광합성을 측정하기 위하여 아크릴로 제작된 생육 챔버(1.0x0.8x0.5m)를 이용하였다. 첫 번째로, 다음의 두 방법을 적용하여 측정된 군락 광합성 속도를 통해 각 방법의 시정수를 계산하여 비교하였다. 즉, 1) CO2 농도를 고정(1,000μmol·mol-1) 하고 광도를 변화(340, 270, 200, and 130μmol·m-2·s-1) 시키거나, 2) 광도를 고정(200μmol·m-2·s-1)하고 CO2 농도를 변화(600, 1,000, 1,400, and 1,800μmol·mol-1) 시켰다. 두 번째로, 1)과 2)의 방식을 적용하여 군락 광합성을 측정했을 때, 특정 광도(200μmol·m-2·s-1)와 특정 CO2 농도(1,000μmol·mol-1)에서 측정된 군락 광합성 속도 값을 비교하였다. 실험 결과 CO2 농도를 변화시키는 방식의 시정수는 광도를 변화시키는 방식에 비해 3.2배 큰 값을 나타내었다. 광도를 변화시키며 측정할 때 군락 광합성 속도는 1분 이내에 안정되었고, CO2 농도를 변화시킬 경우에는 6분 이상의 시간이 소요되었다. 따라서 광도를 변화시키는 측정 방식이 생육 챔버를 이용하여 작물의 군락 광합성 속도를 측정할 때 적합한 방식임을 확인하였다.

The carbon capture and storage (CCS) technology from industrial flue-gas is an important environmental issue these days. Membrane process can be competitive technology for its relatively small footprint and eco-friendly system. Many membrane modules with high selectivity and excellent flux have been developed so far. However, the high purity and recovery for CO2 capture can be achieved by optimization of operating conditions such as membrane area, feed/permeate pressure ratio and humidity of flue gas as well as membrane permeance or selectivity. In this study, we discuss the effect of operating parameters for high CO2 purity and recovery at permeate side. Using polymeric hollow fiber membrane, the single membrane process was tested to figure out the effect of feed flow rate, pressure ratio, membrane area and moisture content.

This study has two objectives. One is developing the runoff model for Hoe-Dong Reservoir basin located at the upstream of Su-Young River in Pusan. To develop the runoff model, basic hydrological parameters - curve number to find effective rainfall, and storage coefficient, etc. - should be estimated. In this study, the effective rainfall was calculated by the SCS method, and the storage coefficient used in the Clark watershed routing was cited from the report of P.E.B. The other is the derivation of transfer function for Hoe-Doug Reservoir basin. The linear, discrete, input-output model which contained six parameters was selected, and the parameters were estimated by the least square method and the correlation function method, respectively. Throughout this study, rainfall and flood discharge data were based on the field observation in 1981.8.22 - 8.23 (typhoon Gladys). It was observed that the Clark watershed routing regenerated the flood hydrograph of typhoon Gladys very well, and this fact showed that the estimated hydrological parameters were relatively correct. Also, the calculated hydrograph by the linear, discrete, input-output model showed good agreement with the regenerated hydrograph at Hoe-Dong Dam site, so this model can be applicable to other small urban areas.