중부지방 3백만 주민의 상수원으로 이용되는 대청호는 부영양화가 심화되어 적절한 수질관리가 없으면 상수원수의 최저등급인 3급수를 만족할 수 없는 상태에 이르고 있다. 그래서 2002년 1월에 금강수계 물관리 및 주민지원 등에 관한 법률이 제정되었는 바, 오염총량제와 수변구역의 지정을 통한 수질보전 등을 주요한 내용으로 포함하고 있다. 오염총량제를 실천하기 위해서는 대청호의 환경용량을 추정하는 것이 필수 불가결하다. 환경용량의 추정은 장래 대청호 수질영향권역에서 개발사업이 이뤄질 때 환경영향평가 특히 누적영향평가를 위해 필요하다. 대청호의 환경용량을 추정하기 위해 오염부하량과 유량의 변화가 대청호의 총질소와 총인농도에 미치는 영향을 WASF5모형으로 분석하였다. 총질소 부하량이 50%증가한다고 가정했을때 갈수기. 명수기, 홍수기에 각각 0.14-0.29 mg/l, 0.12-0.16 mg/l and 0.03-0.05 mg/l 정도의 농도 변화가 예측되었다. 총질소 부하량이 지금의 반이하로 감소하더라도 총질소농도 5급수기준 (1.0-1.5 mg/l)을 달성할 수가 없다. 대청호의 환경용량을 상수원수 3급수기준으로 산정한다면, 그것은 현재의 총질소 부하량의 반보다 훨씬 적다고 추정할 수 있으며 따라서 총질소 부하량은 지금의 반이하로 줄어들어야 할 것이다. 총인 부하량이 50%증가한다고 가정했을 때 갈수기, 평수기, 홍수기에 각각 0.005-0.011 mg/l, 0.004-0.006 mg/l and 0.001-0.002 mg/l 정도의 농도 변화가 예측되었다. 총인 부하량이 지금의 반이하로 감소하더라도 총인 농도 4급수기준 (0.05-0.1 mg/l)을 간신히 달성할 수 있다. 따라서 대청호의 환경용량은 지금의 총인 부하량의 반정도로 추정할 수 있으며 총인 부하량은 지금의 반이하로 줄어들어야 할 것이다. 오염부하량을 줄이기 위한 방안을 정오염원과 비정오염원으로 나눠 제시하였고 오염총량제 실현방안을 제시하였다.

본 연구에서는 침출수를 비롯한 매립지의 각종 오염물질 배출로 수자원이 오염되어 피폭체의 피해가 빈발하는 문제를 해결하기 위해서, 매립지의 상대적 유해성을 평가하여 한정된 환경관리 예산의 합리적 배분을 위한 우선순위를 결정할 수 있는 의사결정 지원도구로서 LHR(Landfill Site Hazard Ranking)모형을 개발했다. LHR모형은 다요소의사결정(多要素意思決) 기법에 정성적 위해성(危害性) 평가기법을 접맥시켜 주관적 가중치를 모형에 반영한 가치내재화(價値內在化) 모형이다. LHR모형은 피폭체의 주요 피폭경로를 지하수 이동경로와 지표수 이동경로로 보았으며, 각 이동경로별로 누출 가능성, 폐기물 특성 및 피폭체 특성으로 요소범주를 3종류로 구분하여 폐기물의 독성이나 매립량같은 특성이 매립지의 수리지질학적 요소 및 자연지리적 요소에 의해 결정되는 오염물질의 누출 가능성을 통해 매립지 주변의 지역주민과 취약한 수생태계 같은 피폭체에 끼치는 매립지의 유해성을 상대적으로 평가했다. 그리고 LHR모형에서는 매립지 유해성을 공기 이동경로 및 사회경제적 측면에서도 평가하기 위해 매립지 이격거리별 토지이용 형태의 유해성을 평가했다. 그리고 각 평가요소별 가중치는 위계분석과정(位階分析過程)의 쌍대비교법(雙對比較法)에 의하여 할당했으며, 민감도 분석으로 LHR모형을 검증했다.

The purpose of this study is to assess the environmental carrying capacity of Chongju City for the environmental management and the urban growth management. The urban environmental carrying capacity assessment of the city by the index of ecological footprint(EF), shows that the ecosystem of the city has been overloaded and most of the deficiencies has come from outside of the city. The EF index, the area of land per capita required for production and consumption in the city, was 1.731 ha per capita in 1989 and 1.901 ha per capita in 1999. On the other side, the ecologically productive land is 0.0175 ha per capita. It means that every citizen owes 1.88 ha per capita to the ecosystem in 1999. The land consumption of the city has increased by 0.1705 ha per capita during the last 10 years. The capacity of infrastructure and the service supply estimated by the Onishi model does not exceed the demand of the city in 1999. But the rapidly increasing population and fast urban growth need the expansion of the capacity. The water supply capacity of the city appears to be sufficient in 1999, but the water supply demand will increase in the future. The capacity of sewage treatment facilities seems to be sufficient, but the higher level of sewage treatment facilities should be adopted for the improvement of water quality as the generation of sewage will increase and its characteristics will also make the wastewater treatment difficult. Due to the decrease of solid waste generated, the land fill capacity for solid waste disposal is not insufficient at present, but the capacity will be saturated in the near future. Therefore, the scientific management system of solid wastes should be introduced. The air quality of the city meets both the national air quality standard and WHO recommendation standard, but the strong regulation and control of automobile emission gas such as CO, $CO_2$, NOx and HC is required for clean air.

The opinionnaire was given to two groups; residents and public officials working at environmental administrative section. Based on the result of questionnaire, perceptional differences between these groups toward environmental NGOs were comparatively anaIyzed. The results were classified into following four items; Firstly, numbers of residents who recognize the existences of environmental NGOs in Kyonggi-Do were lower than those who didn't. Secondly, in both groups, more than 80% of respondents acknowledged that residents should be involved in decisions and developments of environmental projects. Thirdly, respondents belonging to both groups overwhelmingly selected the item "being improved" as the answer for the question asking whether NGOs' environmental activities contribute to improve of environmental conditions. This indicated that public officials also acknowledged the positive role of NGOs in environmental issues. Lastly, the answer of "intensive upbringing is necessary" was ranked as the first place for the question asking "necessity of raising environmental NGOs". However, it was hard to tell which opinion was superior in the matter of financial support necessity for NGOs judging from the answers by respondents of public officials.

The purpose of this study is to analyze the geomorphological environment changes of tidal flat in the Cheonsu Bay. Especially, it centers on the changes in the sedimentary environment using remote sensing data. Multi-temporal Landsat data and topographic maps were used in this study. The results are summarized as follows: the tidal flat of Cheonsu Bay changes in many ways depending on the direction of the tidal current. In the neighborhood of Ganwoldo, the scale of the tidal flat has continuously been expanded due to the superiority of sedimentation after a tide embankment was built. When we analyzed the grain size of sediments and implemented in-situ field survey, it was found that the innermost part of the bay consists of a mud flat, with the midway part mixed flat, and the nearest part to the sea sand flat. On the other hand, in the neighborhood of Seomot isle and its beach, sedimentation is superior in the eastern part whereas erosion is superior in the western part. In other words, the western coast of the beach is contacted with the open seas and under much influence of ocean wave. The eastern coast is placed at the entrance of the bay and has sand bar and tidal flat developed due to submarine deposits that are accumulated on the sea floor by the tidal current. In conclusions, remote sensing methods can be effectively applied for quantitative analysis of geomorphological changes in tidal flat, and it is expected that the proposed schemes can be applied to another geomorphological environments such as beach, sand dune, and sand wave.