광주 선교 스테이션은 의료활동을 통해서 복음의 접촉점을 가졌을 뿐만 아니라, 당시 열악한 위생상태와 질병을 통하여 죽어가는 사람들을 치료해 주었다. 특히 광주 선교스테이션의 한센병과 폐결핵환자에 대한 치료는 헌신적이었다. 많은 사람들이 치료를 받고 새로운 삶을 살아가게 되었고, 그리스도의 사랑을 실천함으로 이를 통하여 주님께 돌아오는 이들이 많았다. 환자들을 찾아가기도 했다. 의사가 없는 지역에 순회진료를 했고, 그리고 농어촌 의료봉사, 보건예방교육 등을 통하여 국민건강 증진과 위생에 대한 인식을 변화시켰다. 의료활동은 광주지역을 넘어서 여수와 순천으로 그리고 남부지역으로 확대되었다. 또한 치료와 회복 그리고 재활 프로그램을 통하여 사회의 소중한 일원으로 살아가게 했고, 의료인재를 양성해서 장차 선교한국으로의 토대를 마련했다.

최근 내수면양식장의 BFT 양식 배출수의 도시농업용 활용에 관한 연구가 활발하게 본 연구진에 의해 진행되어지고 있다. 하지만 도시농 업용으로 한정된 연구에서 비료가 다량으로 사용되어 지고 있는 과수에의 활용에 대한 연구 필요성이 대두되어 누구나 가정에서도 재배가 가능한 블루베리에서 BFT 배출수의 효과를 구명하여 보고자 본 연구를 수행하였다. BFT 배출수는 내수면양식연구센터 틸라피아를 양식 하고 있는 양식조의 물을 채취하여 무처리, 농장 관행법, 배출수 원액, 배출수 1/2희석액, 배출수 1/4 희석액 시비 등 5처리로 실험하여 다음 과 같은 결론을 얻었다. 블루베리의 총생산량과 과립당 무게는 처리간 유의성이 없어 배출수가 기존의 비료를 대체하여도 블루베리 열매 의 생육에 영향을 주지 않아 비료로서의 이용가능성이 있었음을 확인하였다. 그리고 과실내 무기성분의 변화에서는 나트륨과 철의 함량이 높게 나와 이를 줄일 수 있는 배출수 비료화의 또 다른 연구 점을 보여주고 있다. 블루베리의 고유 기능성 물질인 안토시아닌의 함량 결과에 서는 처리에 따른 일관성을 보이고 있지 않아 기능성물질의 변화에도 배출수의 처리가 나쁜 영향을 보이지 않음을 알 수 있어 블루베리의 재배에 있어서도 배출수의 비료활용도는 가능성이 있다는 결론을 얻을 수 있었다. 하지만 비료로서의 사용가능성을 더 높이기 위해서는 보다 정제된 배출수의 사용과 효과를 얻기 위해서는 배출수의 가공적 연구가 더욱 필요하다고 판단된다.

본 연구는 국제적으로 해양투기의 기준이 엄격해지고 있는 현재의 실정에 맞추어 양식장에서 배출되는 배출수를 자원의 선순환의 개념으로 이를 토마토 재배에 적용하여 도시농업용 비료로서의 이용가치를 구명하고자 수행하였다. 시험용 작물로는 완숙형 토마토‘슈퍼 선로드’를 사용하였으며, BFT 배출수는 내수면양식연구센터 틸라피아를 양식하고 있는 양식조의 물을 채취하여 무처리, 상업용 하이포넥스500배 희 석액, 배출수 원액을 매일 관주, 배출수 원액을 1주에 1회 관주, 완효성 고체비료 시비 등 5처리로 실험하여 다음과 같은 결론을 얻었다. 배출 수원액을 매일 처리하는 구가 T/R율과 엽록소함량이 제일 높은 결과를 보였으며, 과실의 당도도 제일 높은 결과를 보였다. 또한 토마토의 기 능성 물질은 리코펜함량의 결과에서도 하이포넥스와 관행의 재배방법보다 3배가 많은 함량의 결과를 보였다. 하지만 토마토 체내의 무기성 분의 함량결과 질소가 다른 처리구에 비해 제일 많은 결과를 보여 비료사용으로서의 보완점을 연구해야하는 문제점도 보였다. 하지만 생육 과 기능성 물질의 함량결과등을 고려하여 본다면 BFT 양식 배출수의 비료효과에 대한 가능성은 매우 높은 것으로 나타났다.

The objective of this study is to find a useful method of utilizing effluent water from the BFT inland water culture. Recently Sludge and effluent water have been noted to cause water pollution. Therefore, this progressive study of recycling method will replace the use of chemical fertilization. Effluent water from inland water culture contains many fertilization ingredients. This study used different using methods of fertilization. As a result, effluent water that isn't matured and diluted had positive effects on the growth of lettuce. Effluent water of undiluted involved many mineral elements and proper pH concentration for plants growth but which are involved many concentrations of Na + ion. High concentrations of Na + ions are harmful for the growth of plants. This experiment did not show plants adversely affected by Na + ions. Potentially Na + ions can cause physiological disturbances of the plant. Effluent water smells because effluent waters using is need to additional pre-treatment for removal its high concentration Na + ions and bad smell.

Recently, increasing interest in environmental pollution problems that can be discharged emerging from inland water cultures, problems in the processing of effluents are recognized as environmental pollution sources are difficult accordingly. As a result, in this study, the effluent water as such a source of environmental pollution carried examine the availability of as organic fertilizer to be used for cultivation of crops. The study tested using 3 types of crops, As a method of using as a fertilizer in a particular solution that was created and practices to liquid fertilizer solution used to the concentration of the effluent. After you grow crops in a certain amount of irrigation once every week for each processing it was analyzed for the differences of content of the functional substance and growth of crops. As a result a certain amount of the effluent water in the stock solution, the content of functional materials and growth of crops were found to be superior to other processes in irrigation which was treated weekly. In conclusion, according to these results the effluent water from BFT inland water culture has been found to give a positive effects on the contents of the functional materials and growth of crops. Studies on a method for utilizing the effluent water as a fertilizer is considered further required.

Ozone concentrations in water and air, and resulting disinfective properties, were measured following generation by either an ozone generator or a low-temperature dielectric barrier discharge plasma generator. In freshwater, ozone concentrations of 0.81 and 0.48 mg/L O3 were observed after the ozone and plasma generators had been operated for five minutes, respectively. Higher levels of dissolved O3 were attained more easily with the ozone generator. In seawater, both systems were capable of creating concentrations greater than 3.00 mg/L O3 after 5minutes of operation. Higher ozone levels were attained more easily in seawater than in freshwater. Rates of bacterial sterilization in seawater after three minutes were 96% and 88%, using the plasma and ozone generators, respectively. In freshwater, higher concentrations of ozone were released into the atmosphere by the ozone generator than by the plasma generator. In creating equivalent levels of dissolved ozone in freshwater, the plasma generator released 4.5 times more ozone into the atmosphere than did the ozone generator. This shows that ozone generators are more effective than plasma generators for creating ozonated water. For the same concentration of dissolved ozone in seawater, more ozone was released into the atmosphere using the ozone generator than using the plasma generator. Therefore, with regard to air pollution, plasma generators seem to be less expensive than ozone generators.

We studied the ozone concentrations generated by low-temperature dielectric barrier discharge plasma reactor after adding air and phytoplankton to control the ozone concentrations in seawater. We also examined the numbers of bacteria and Vibrio spp. after treatment using the plasma reactor. As the airflow rate was increased, more ozone was removed. Although marked variation in the ozone decrease was observed with and without airflow, the rate of ozone removal did not increase proportionately with the airflow rates. The ozone concentration decreased with increasing organic matter and time. The amount of organic matter seems to be an important factor decreasing the dissolved ozone concentration in liquid. The ozone concentration was 0.07, 0.32, 1.28, and 2.3 mg/L when operating the plasma reactor for 30, 60, 180, and 300 s, respectively; i.e., the ozone concentration increased with the reactor operating time. The initial numbers of bacteria and Vibrio spp. were 800 and 480 CFU/mL, respectively. After operating the plasma reactor at a flow rate of 6 L/min for 30 s, no bacteria or Vibrio spp. were detected. The disinfection effect of this plasma reactor seems to be superior to that of a conventional ozone generator.

Ground seawater quality was investigated, and the algal growth potential (AGP) tests were performed along the Tongyeong coast to examine the inflow of materials, which is needed for the red tide species Cochlodinium polykrikoides to grow. The study was conducted to determine the mechanism for C. polykrikoidesred tides. Water temperature, salinity, pH, and dissolved oxygen (DO) ranged from 16.05 to 20.74°C, 18.20 to 32.11 psu, 6.00 to 7.61, and 3.41 to 7.91 mg/L (41.4– 96.1%), respectively. No seasonal variation was observed in water temperature. The salinity, pH, and DO saturations at most stations were lower than those of coastal seawater at Tongyeong. The NH4 +-N, NO2+3 --N, PO4 3--P concentrations ranged from 0.43 to 16.00μM, 1.50 to 132.38μM, and 1.30 to 6.29μM, respectively; the values at some stations were much higher than observed in Tongyeong coast seawater. Using seawater from station B, C. polykrikoides grew consistently, with a high growth rate, similar to the red tide in nature. This seawater appeared to contain materials needed by C. polykrikoides to grow. Therefore, C. polykrikoides red tides seem to occur wherever the ground sea water contains materials that are needed for its growth.

The environmental changes related to hypoxic water mass were investigated at Gamak bay in summer times, June, July and August 2006. The hypoxic water mass was found, in first, at the northern area of Gamak bay on 27 June. This water mass has been sustained until the end of August and disappear on 13 September. In Gamak bay, the hypoxic water mass was closely related to geography. During the formation of oxygen deficiency, changes in dissolved nutrients was studied and found that on surface layer and lower layer, DIN were 0.80 μM~19.8 μM(6.03 μM) and 1.13 μM～60.83 μM(10.66 μM), and DIP were 0.01 μM～0.92 μM(0.24 μM), and 0.01 μM～3.57 μM(0.49 μM), respectively, far higher distribution on lower layer of the water where hypoxic water mass was occurred. The configuration of phosphorus was analyzed to figure out the possibility of release of phosphorus from sediments. It was found that the Labile-Phosphorus, which is capable of easy move to water layer by following environmental change was found more than 70%. Therefore, in Gamak bay, it was found that the possibility of large amount of release of soluble P into the water, while hypoxic water mass was occurred in deep layer was higher. It is suggested that DIP in the northern sea of Gamak bay mainly sourced from the soluble P from lower layer of the waters where hypoxic water mass was created more than that from basin. However, existence form of phosphorus in sediments during normal times, not during creation of hypoxic water mass, needs further study.

We examined the horizontal distribution of salinity and the concentrations of DIN and DIP after heavy rainfall events in coastal areas of South Korea from Yeoja Bay to Narodo and from Gwangyang Bay to Geomodo to determine whether fresh water actually flows into areas of Cochlodinium polykrikoides red tides and to observe its effect on the growth of this organism after heavy rainfall. Following heavy rainfall (155 mm) in the Yeosu and Suncheon regions, the average salinity was 21 and 29 psu at Yeoja Bay and in the coastal waters of Narodo, respectively. After 126 mm of rainfall, the values were 19 and 25 psu in the coastal waters of Yeosu and Geomodo, respectively. This may have been caused by an influx of fresh water, after the rainfall event, into the open sea coastal areas around Narodo and Geomodo from the Dong and Seomjin Rivers, which are about 3540 km away. After the rainfall, the concentrations of NH4-N, NO2-N, and PO4-P were slightly increased; however, the concentration of NO3-N was greatly increased and diffused throughout the coastal areas of Narodo and Geomodo, which frequently experience C. polykrikoides blooms. The influence of NH4-N, NO2-N, and PO4-P on the occurrence of C. polykrikoidesred tides in coastal areas around Narodo and Geomodo after heavy rainfall does not appear to be great. Instead, the occurrence C. polykrikoides red tides in the coastal areas of Narodo and Geomodo seems to be facilitated by NO3-N.

To analyze the water characteristics in the dry and wet seasons, the data for temperature, salinity, nutrients and chl-a were used, which were observed in the south coastal area of Korea during April to October 2000. At Yeosu in the south coast of Korea, the higher values of 35.0 psu in salinity were shown in March and April, the lower values of 23.0 psu in salinity were shown in August and September. The annual range of salinity was 12.0 psu. The total amount of precipitation in the wet season (July to October) was occupied 68% (about 846 mm) during 2000. The precipitation of the dry season (November to June) was occupied 32% (about 394 mm) in the year. In the coastal area, the salinity variation is distinct in the period of July to October. Based on this result, we divided the season into two parts: the dry season during April to June and the wet season during July to October. Factor analysis was shown that temperature has strong negative relation and nutrients show positive relations in the dry season by the factor 1, which explains the total variance of 50.6% at the surface water. In the wet season, salinity has negative relation and nutrients show positive relation by the factor 2, which explains the total variance of 33.5%. The bottom layer also showed similar to those of surface water in the results of factor analysis. These mean that nutrients become rich due to the freshwater inflow in the wet season. The low saline water is shown not only in the south coast but also in the overall region in the South Sea of Korea. It is suggested that the South Sea of Korea may call a ROFI (Region of Freshwater Influence) system in summer.

An algal assay procedure using an indigenous phytoplankton assemblage was tested to estimate the propagation of red tide phytoplankton species and determine the optimal time interval at which to measure growth yield in eutrophic marine waters where red tides frequently occur. Various red tide phytoplankton species were propagated on a large scale by adding nitrogen or phosphorous. This procedure was useful for estimating the limiting nutrient, elucidating the mechanisms underlying red tides, and determining the levels of increases in organic matter in eutrophic coastal waters. The algal assay using indigenous C. polykrikoides showed that this species did not always propagate, apparently because of very low concentrations of trigger elements that are necessary for its growth, rather than as a result of other environmental characteristics, e.g., water temperature or stress from sampling. In the winter, when water temperatures are lower than in spring, summer, or autumn, maximum propagation and the limiting nutrient could be estimated by measuring phytoplankton biomass at 2–3-day intervals. However, in the other seasons, when water temperatures are higher, phytoplankton biomass should be measured at 2-day intervals. In particular, daily monitoring will be required to determine precise growth yields in warm seasons.

In order to study the temporal variations of nutrients and chlorophyll-a in the Bottol Bada, three field observations were carried out on 20, 23 and 26 July, 2004. The low N:P values exhibit nitrogen deficiency during the periods of observation. This result is not representative of typical summer environment in the southern coast of Korea. The possible mechanisms are as follows: 1) The freshwater inflow was not sufficient for the supply of nitrogen because the total precipitation was 11.9 mm in July, 2004. This amount is no more than 5% in normal precipitation in July. 2) There was an inflow of oceanic water under the subsurface into the Bottol Bada. Even though the oceanic water comprises more nutrients, it produces the stratification between the surface and the subsurface water and seems to prevent the supply of nutrinets to the surface layer. 3) The high chlorophyll-a concentration of 1.2 μg/L was shown near the narrow channel between Gae-do and Geumo-do. This seems to be resulted from the inflow of water from Gamak Bay.

Based on the observation on 20, 23 and 26 July 2004, the distributions of temperature, salinity and stratification was investigated in relation to ebb, turn of tide and flood. The results are as follows: 1) The high temperature and low saline water with 23.5～24.0℃ and 32.4～33.0psu existed at Naro Island. 2) The cold surface water below 21.0℃ and 33.0～33.4psu appeared in the area near Gae Island and Geumo Island. 3) The cold and saline water, below 24.0℃ at the surface and 17.0℃ near the bottom, 32.8～33.8psu at the surface and 33.8～34.0psu near the bottom, existed in Sori Island. These waters were more saline compared to the South Sea Coastal Water with about 31.8psu. This suggests that the oceanic saline water intruded into the Bottol Bada through the area near Sori Island. The stratification appeared during all the observation periods due to a high solar radiation of 22MJ/m2, and a weak wind speed of 2.9m/s on the average while the mean speed of wind in July is around 3.9 m/s. It qualitatively suggested that the stratification was maintained during the observation periods because of a high solar radiation, a weak wind speed and intrusion of saline oceanic water.