본 연구는 54일 동안 관수량과 오이(‘아시아 은천 F1’)의 생 육, 줄기 수액 흐름, 광합성 특성, 수분 이용 효율에 대한 상대 습도(RH)와 광도의 영향을 평가하였다. 오이는 토양 화분에 서 재배되었으며, 토양 수분 장력계로 자동 제어(－10kPa) 하 여 EC 1.5dS m-1의 양액을 1회 주당(per plant) 265mL 공급하 였다. 처리는 세 조건으로 광도 200μmol·m-2·s-1에 가습 처리 구(HL)와 무가습의 대조구(Control), 광도 350μmol·m-2·s-1 에 가습 처리구(HH)로 설정하였다. 주간(weekly) 평균 RH는 가습 처리구에서 79.5%(VPD 2.4kPa), 무가습 처리구에서 65.5%(VPD 4.0kPa)이었고, 평균 온도는 모든 처리구에서 25℃이었다. 총관수 횟수는 대조구에서 29회, HL처리구에 서 26회, HH처리구에서 27회이었다. HH처리구에서 초장과 마디 수, 엽 생육, 줄기 직경에서 생장이 컸으며, HH처리구에 서 광합성률이 더 높았고, 대조구에서 증산률이 더 높았다. 주 간 엽온은 HH처리구에서 28℃, HL처리구에서 26℃, 대조구 가 23℃였으며, 엽기온차는 HH처리구에서 2℃, HL처리구 에서 0℃, 대조구에서 －3℃ 이였다. 모든 처리구에서 줄기 수액흐름(SFRR)은 광의 유무와 토양수분장력에 영향을 받 아 광주기 시작 전 10%(HH, Control)－30%(HL)에서 광주 기 시작 이후 60%(HH)－90%(Control)로 상승하였고, 관수 후 SFRR은 20－30% 상승폭을 나타냈다. 광 조사 동안 평균 SFRR은 대조구에서 88.5%로 가습처리구보다 높은 경향이 었다. 이상의 결과 오이 토양 포트재배에서 토양수분장력 －10kPa 관수제어시 처리구의 토양 수분장력은 차이가 없음 에도 불구하고 적정 VPD가 유지되면 오이의 생육과 암꽃발 생률이 높았고 광주기 동안 엽기온차, 관수영향은 SFRR에 영 향을 주었다.

Mangroves are distributed in intertidal zones of coastal environments or estuarine margins, playing a critical role in the global carbon cycle. However, understanding of the carbon cycle role of mangrove associates in the Republic of Korea is still limited. This research measured soil respiration and leaf gas exchange in three habitats of Hibiscus hamabo (Gimnyeong, Seongsan, and Wimi) and analyzed the impacts on sites and months. Soil respiration was measured once a month from June to October 2022 and leaf gas exchange was measured monthly from June to September 2022. Soil respiration in August (5.7±0.8 μmol CO2 m-2 s-1) was significantly higher than that in other months (p<0.001) and soil respiration increased as air temperature increased (p<0.001). In Seongsan, net photosynthesis in July (9.0±0.9 μmol m-2 s-1) was significantly higher than that in other months (p<0.001). Net photosynthesis increased as stomatal conductance and transpiration rate increased during the entire period (p<0.001). Furthermore, a weak positive linear relationship was observed between soil respiration and net photosynthesis (r2=0.12; p<0.01). The results indicated that soil respiration was influenced not only by air temperature and season but also by net photosynthesis. This study is expected to provide basic information on the carbon dynamics of mangrove associates.

During the initial cooling period of spent nuclear fuel, Cs-137 and Sr-90 constitute a large portion of the total decay heat. Therefore, separating cesium and strontium from spent nuclear fuel can significantly decrease decay heat and facilitate disposition. This study presents analytical technique based on the gas pressurized extraction chromatography (GPEC) system with cation exchange resin for the separation of Sr, Cs, and Ba. GPEC is a micro-scaled column chromatography system that allows for faster separation and reduction volume of elution solvent compared to conventional column chromatography by utilizing pressurized nitrogen gas. Here, we demonstrate the comparative study of the conventional column chromatography and the GPEC method. Cation exchange resin AG 50W-X12 (200~400 mesh size) was used. The sample was prepared at a 0.8 M hydrochloric acid solution and gradient elution was applied. In this case, we used the natural isotopes 88Sr, 133Cs, and 138Ba instead of radioactive isotopes for the preliminary test. Usually, cesium is difficult to measure with ICP-OES, because its wavelengths (455.531 nm and 459.320 nm) are less sensitive. So, we used ICP-MS to determine the identification and the recovery of eluate. In this study, optimized experimental conditions and analytical result including reproducibility of the recovery, total analysis time and volume of eluents will be discussed by comparing GPEC and conventional column chromatography.

This study was performed to evaluate the separation of Sr, Cs, Ba, La, Ce, and Nd using gas pressurized extraction chromatography (GPEC) with anion exchange resin for the quantitation of Neodymium. GPEC is a micro-scaled column chromatography system that provides a constant flow rate by utilizing nitrogen gas. It is overcome the disadvantages of conventional column chromatography by reducing the volume of elution solvent and shortening the analysis time. Here, we compared the conventional column chromatography and the GPEC method. The whole analysis time was decreased by nine times and radioactive wastes were reduced by five times using the GPEC system. Anion exchange resin 1-X4 (200~400 mesh size) was used. The sample was prepared at a 0.8 M nitric acid in methanol solution. The elution solvent was used at a 0.01 M nitric acid in methanol solution. Finally the eluate was analyzed by ICP-MS to determine the identification and recovery. In this case, we applied the natural isotopes of LREEs (139La, 140Ce, and 144Nd) and high activity nuclides (88Sr, 133Cs, and 138Ba) instead of radioactive isotopes for the preliminary test; as a result, unnecessary radioactive waste was not produced. The recoveries were 93.9%, 105.9%, 91.9%, 47.6%, 35.9%, and 79.9% of Sr, Cs, Ba, La, Ce, and Nd, respectively. The reproducibility of recoveries by GPEC were in the range 2.8%–10.9%.

The O2 and CO2 concentrations in controlled atmosphere (CA) rooms are determined by the respiration of produce like apples and the airtightness of the CA room, with gas in the CA room controlled by O2 and CO2 removal as well as respiration (CO2 increase and O2 decrease). The purpose of this study was to evaluate the validity of the gas exchange model for O2 removal, CO2 removal, the rate of O2 decrease and CO2 increase by respiration of apples, and airtightness of the CA room. It took 17.5 hours to reduce O2 concentration from 20.9% to 2.0% after loading 4.3 tons of Fuji apples into the CA room, which was 4.2 hours longer than the 13.3 hours of the model formula. After the CO2 concentration rose to 0.5% due to respiration, it took 4.7 hours to lower the CO2 concentration to 0.2%, which was 0.6 hours longer than that of the model equation. The rate of CO2 increase by respiration was 0.021%/ h, which was similar to the model equation (0.017%/h). Also after 4.7 hours, the O2 concentration decreased by 0.1% which was also in line with the model equation (0.13%/h).