• 한국물환경학회지
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• 제34권5호
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• pp.487-493
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• 2018

Urban stormwater runoff is the one of the most extensive causes of deterioration of water quality in streams in urban areas. Especially, in the Suyeong River watershed, non-point sources from urban-residential areas are the most common cause of water pollution. Also, it has been ascertained that BOD and COD as indexes of organic matter, have limitation on management of Suyeong River's water quality. In this study, changes of organic matter properties of Suyeong River from inflow of non-point source during rainfall were investigated. Fractions of organic matters were analyzed using water samples collected at two sites (Suyeong River and Oncheon Stream) during a rain event. Variations of dissolved organic carbon (DOC) concentration by rainfall were similar to flow rate change in the river. Distribution of organic matter fraction according to change of rain duration revealed that while hydrophilic component increased at initial rainfall, the hydrophobic component was similar to change in dissolved organic carbon (DOC) concentration. Also, the relative proportion of hydrophilic components in organic matter in river water increased, due to rainfall. Results of biodegradation of organic matters revealed that decomposition rate of organic matters during rainfall was higher than that of during a non-rainfall event.

• 한국대기환경학회지
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• 제3권2호
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• pp.53-61
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• 1987

Automatic and manual rain smaplers wre installed at the roof of National Institute of Environmental Research (NIER), and the rain sampling and measurement were conducted during the period April to August 31, 1987. The rain sampling and measurement were carried out in the following manners: The 1st : Acidity and conductivity were measured entirely by automatic rain sampler (continuous measurement) The 2nd : Acidity and conductivity wrer measured in the laboratory with the sample that was taken out of automatic rain sampler. The 3rd : Acidity and conductivity were measured in the laboratory with the sample that was taken out of manual rain sampler. Afterwards, those different measurement values were compared each other and the following conclusions were obtained: 1) The pH of the continous measurement by the automatic sampler was lower than that of the laboratory measurement, and it was reversed in case of the conductivity. 2) The significance was recognized at 5% risk ratio for the population mean of difference of the measurement values of the pH and conductivity from both samples. 3) The significance was not recognized at 5% risk ratio by the analysis of variance by one way layout for the pH and conductivity. 4) The significance was recognized at 5% risk ratio by the analysis of variance by two way layouts for the pH conductivity. 5) The significance was recognized at 5% rrisk ratio for the differences of the pH values obtained by oboth samplers, and no significance was recognized for conductivity. 6) In comparison of the measurement values from the two samplers were shown a good correlation for pH; correlation coefficient (r) = 0.63, and regression equation Y = 0.53X + 2.78. For conductivity, the correlation was also excellent; correlation coefficient (r) = 0.53 and regression equation Y = 0.63X + 5.65.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2005년도 학술발표회(1)
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• pp.95-96
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• 2005

• 보존과학회지
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• 제11권1호
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• pp.15-27
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• 2002

군위 삼존석굴은 주로 반상 흑운모 화강암으로 구성되며 그 내부가 기계적, 화학적 및 생물적 풍화작용에 의해 훼손되었다. 이 풍화작용의 근본요인은 빗물에 의해 일어나며 이 빗물은 절리를 따라 스며들어 석굴내부로 누수된다. 그러므로 누수를 일으키는 절리를 조사하고 누수 경로를 추적하여 차수대책을 강구하였다. 석굴 주위의 반상 흑운모 화강암은 북동동과 북서서 절리조를 규칙적으로 발달시키며, 그 중에 북동동 절리조가 훨씬 뚜렷하게 나타난다. 북동동 절리조는 4개 절리대를 형성하며 이중에 $J_m$과 $J_3$, 절리대가 누수의 직접적인 원인이 되며 석굴훼손에 큰 영향을 미친다. 석굴 안쪽의 인장절리는 $J_m$ 절리대로 통하며, 이 경로는 작은 빗물이 석굴내부까지 누수되지는 않겠지만 큰비는 누수를 일으키며 상당히 오래 지속될 것으로 생각된다 석굴입구 천장의 절리와 균열들은 $J_m$ 절리대로 연장되며 10mm 이내의 작은 비에도 빗물이 쉽게 석굴내부로 스며든다. 차수대책은 누수부위보다 L: -9m에서 L: +10m까지 범위의 $J_m$ 절리대와, 반경 5m 원 상반부의 J3 절리대의 빗물 유입부를 차단하는 방안이 가장 바람직하다. 처리제는 충진제와 발수경화제를 사용하여 절리와 열극의 틈을 일일이 막아야만 하며, 점도를 높이기 위해 경화제와 속결제를 혼합하여 사용하는 것이 좋다.

• 환경영향평가
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• 제31권1호
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• pp.1-10
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• 2022

본 연구는 비점오염원 저감시설인 차집시설을 대상으로 다양한 강우조건에 따라 초기우수 유출수의 수질특성을 파악하고, 용존성 오염물질의 기원을 파악하기 위하여 수행되었다. 본 연구는 도시지역 내 위치한 G-배수구역의 10개 차집시설 중 비강우시에도 불명수가 유입되는 것으로 조사된 차집시설 #1, #5, #8, #9 및 #10 등 5개 지점에서 수질분석을 통하여 차집시설에서 비점오염물질의 유출특성을 파악하였다. 연구결과로써 강우량에 따라 차집시설에서 우수유출수의 수질특성에 영향을 받는 것으로 판단되었다. 비강우시 EC, BOD, TOC, TN의 평균농도는 강우시에 비하여 높은 것으로 조사되었으며, DO의 평균농도는 강우시에 비하여 낮은 것으로 조사되었다. 또한, 차집시설에서 유출수의 용존성 유기물은 주로 내부에서 생성된 유기물로 구성된 것으로 판단되었다. 우수유출수는 주변 환경에서 유입되는 오염물질의 영향을 많이 받으며, 강우로 인하여 차집시설의 외부로부터 유입되는 난분해성 휴믹계 물질이 많아진 것으로 판단된다.

• 한국물환경학회지
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• 제26권4호
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• pp.648-653
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• 2010

Discharged pollution load for the management of Total Maximum Daily Loads (TMDLs) is calculated on the basis of rainfall data for reference year. Rainfall has an influence on discharged pollution load in unit watershed with combined sewer system. This study reviewed the status of discharged pollution load and rainfall conditions. We also investigated rainfall effects on discharged pollution load by analyzing change of the load in accordance with increase of rainfall. The change ratio of discharged pollution load was 18.6% while inflow load only 5.8% for 5 years from 2004 to 2008 in Daejeon district. The greatest rainfall and rain days were over 2 times than the least during the period. This change in rainfall could have great effect on discharged pollution load. The analysis showed that discharged pollution load increased 2.1 times in case rainfall increased 2 times and 1.2 times in case rain days increased 2 times. Rainfall effects, therefore, should be considered to make resonable evaluation of discharged pollution load in the assessment of annual performances.

• 자원환경지질
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• 제13권4호
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• pp.229-239
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• 1980

A various kinds of harmful gases in the gallery and the increasing quantity of in-flow water are the important factors causing mainly the decline in production. In this thesis, the increase and decrease of in-flow water which effects the out put have been investigated and analysed in the statistical method. Through the results obtained together with the stastistical data some typical interreation formula between the quantity of in-flow water and production have been induced and the productive percentage in season was examined with special reference to Changsung Coal Mine. The formulas are as fallows: (1) Underground in-flow water to production; $Y=-5.74x^2+108.9x+6,346.6$ where, Y: production(tons/day): x:in-flow water($m^3/min$), (2) Rain and Snow fall to production; P=6.555-1.591 R+1.282S where, P;production(tons/day); R:rain fall(mm); S : snowfall(cm), (3) Productivity ratio in season compared with the average annual production; 1st quarter of year:100.1%, 2nd quarter of year: 100.3%, 3rd quarter of year: 97.2%, 4th quarter of year: 102.4%.

• 한국암석학회:학술대회논문집
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• 한국암석학회.한국광물학회 2000년도 공동학술발표회 논문집
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• pp.3-11
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• 2000

The earth environment consists of four spheres : geosphere, hydrosphere, atmosphere and biosphere. The geosphere consists mostly of minerals. It, however, contains some water and air in its shallow depth. Although hydrosphere and atmosphere consist predominantly of water and air, respectively, both contain some minerals. The biosphere consisting of various organisms is present in the interfaces of geosphere, hydrosphere and atmosphere. The natural environment of the earth is continuously changing by the interaction of four spheres. It suggests that out relevant environmental problems can not be revolved without understanding the natural relationship of these four spheres. Minerals in our environment are very important because they are the main constituent materials of the earth and they control our environment. The roles of minerals in our environment have not been understood even in the scientific society. Thus their roles have been neglected. Review of studies on the environmental mineralogy so far made at our laboratory and others show that minerals control the environment in various ways. Minerals neutralize the acid water as well as acid rain. Minerals in soils and rocks are major neutralizer of the acid rain. Salinization of sea water is attributed to the ionic substitution between minerals and sea water. Some minerals control the humidity of the air. Corals, the products of biomineralization, are the main carbon controller of the air. Minerals also adsorb heavy metals, organic pollutants and radioactive nuclides. Such remarkable functions for controlling the environment come from the mineral-water reaction and biomineralization. All these phenomena are subjects of the environmental mineralogy, a new field of earth science.

• Journal of Ginseng Research
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• 제6권2호
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• pp.168-203
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• 1982

Effects of soil moisture on growth of Panax ginseng, of various factors on soil moisture, and of moisture on nutrition, quality, physiological disorder, diseases and insect damage were reviewed. Optimum soil moisture was 32% of field capacity with sand during seed dehiscence, and 55-65% for plant growth in the fields. Optimum soil moisture content for growth was higher for aerial part than for root and higher for width than for length. Soil factors for high yield in ginseng fields appeared to be organic matter, silt, clay, agreggation, and porosity that contributed more to water holding capacity than rain fall did, and to drainage. Most practices for field preparation aimed to control soil moisture rather than nutrients and pathogens. Light intensity was a primary factor affecting soil moisture content through evaporation. Straw mulching was best for the increase of soil moisture especially in rear side of bed. Translocation to aerial part was inhibited by water stress in order of Mg, p, Ca, N an Mn while accelerated in order of Fe, Zn and K. Most physiological disorders(leaf yellowing, early leaf fall, papery leaf spot, root reddening, root scab, root cracking, root dormancy) and quality factors were mainly related to water stress. Most critical diseases were due to stress, excess and variation of soil water, and heavy rain fall. The role of water should be studied in multidiciplinary, especially in physiology and pathology.

• 생태와환경
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• 제40권2호
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• pp.234-243
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• 2007

청계천 복원이후 하천수질의 생태학적 평가를 하기 위하여 청계천을 비롯한 인접수역 중랑천 및 한강 본류를 대상으로 강우 전후 조류 및 수질변화와 현장수에 대한 조류성장잠재력(AGP)을 조사하였다. 조사는 청계천(정점 1, 2), 중량천(정점 3), 두 하천의 합류부(정점 4), 한강 본류의 상류(정점 5)및 하류(정점 6)등 총 6개 정점을 선정하여 2006년 하계(강우 이 전 7월 25일, 강우 이 후 8월 28일)에 각각 1회씩 실시하였다. 한편, AGP조사를 위해 각 정점에서 채수한 현장수를 공시종 남조 Microcystis aeruginosa 배양계에 1/6, 2/6, 3/6씩 각각 첨가하고, 온도 $25^{\circ}C$, 광조건 100 ${\mu}mol$ photons $m^{-2}s^{-1}$ (14h : 10h LD cycle)에서 11일간 배양하였다. 조사결과, 총질소는 중랑천과 청계천의 합류부에서 높았는데, 특히 후자는 강우 전후 각각 14.4, 18.5 mg $L^{-1}$를 기록하며 가장 높았다. 총인 역시 중랑천과 청계천의 합류부에서 높았는데, 총질소의 경우와 같이 정점 4의 총인은 강우 전후 각각 1.1, 1.3 mg $L^{-1}$를 기록하며 가장 높았다. 엽록소-${\alpha}$는 강우 후에는 중랑하수처리장 방류지점을 포함하고 있는 청계천과 중랑천의 합류부인 정점 4에서 매우 높았으며 가장 우점한 조류는 Cyclotella sp.로 조사되었다. 현장수에 대한 AGP조사결과, 강우 전에는 대조구에 비해 모든 정점에서 높은 성장을 보였으나, 강우 후에는 대조구에 비해 전반적으로 낮은 성장을 나타냈다. 다만, 강우 후에는 현장수 첨가량이 증가함에 따라 대조구와 큰 차이를 보이지 않았는데 이는 강우에 의한 영양물질의 증가가 원인인 것으로 판단되었다. 따라서 청계천을 포함한 조사하천들은 평상시에는 비교적 안정된 생태계를 유지하고 있으나 집중강우시 영양물질 유입으로 인한 하류의 조류번식 가능성이 우려되며, 특히 중량천의 수질개선이 시급한 것으로 판단되었다.