• Proceedings of the Korea Water Resources Association Conference
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• 2023.05a
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• pp.341-341
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• 2023

전 세계적으로 발생하고 있는 기후변화로 최근 극한의 가뭄이나 홍수가 발생하고 있으며, 이로 인한 경제·사회적으로 피해를 발생시키고 있는 실정이다. 이에 따라 기후변화에 직접적으로 영향을 주는 원인 중 하나인 온실가스에 대한 관심 높은 실정이며, 전 지구적으로 다양한 분야에서 탄소중립을 위한 정책이나 실천 방안 마련을 위한 연구가 활발히 이루어지고 있다. 우리나라에서는 2050 장기 저탄소 발전전략을 수립하였으며, 농축산부문의 온실가스 배출량을 2018년 배출량인 24.7백만톤 대비하여 2030년까지 27.1%인 약 6.7백만톤 감축을 목표로 하며 그 중 벼 논물관리를 통한 온실가스 감축 목표량은 540천톤으로 농업인의 참여가 요구된다. 이에 본 연구에서는 저탄소 논물관리를 위한 농업인 대상으로 총 3회의 교육을 실시하였다. 저탄소 논물관리 참여의식 고츼 및 탄소 중립에 대한 이해를 돕기위한 교육을 실시하였고 교육 전·후 참여 농업인 대상의 설문조사를 실시하였다. 저탄소 논물관리의 핵심인 중간 물떼기와 관련된 설문 결과, 교육 전 2주 미만 논물을 건조한다고 응답한 농업인은 51%였으나 교육 3회 실시 후 설문에서는 2주일 이상 논물을 건조한다고 응답한 농업인이 78%로 증가하였다. 또한, 출수기부터 완전 물떼기 전까지의 논물관리 방식인 걸러대기는 교육전 49%였지만 교육 실시 후 74%로 증가하여 걸러대기를 실천하는 농업인 비율이 높아졌다. 이처럼 농업분야의 온실가스 배출량 감축을 위한 정책이 현장에서 효과적으로 실천되기 위해서는 농업인의 참여가 필수적이다. 따라서 본 연구와 같이 농업인 대상의 교육이나 컨설팅 등이 함께 이루어진다면 더욱 높은 효과를 나타낼 수 있을 것으로 사료된다.

• The Journal of the Petrological Society of Korea
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• v.18 no.2
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• pp.115-135
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• 2009

We have studied general orientational characteristics of microcracks distributed in Tertiary crystalline tuff from the northeastern part of the Gyeongsang Basin. 108 sets of microcracks on horizontal surfaces of 6 rock samples from Heunghae-eup and Cheongha-myeon, Pohang-si areas were distinguished by image processing. Those microcrack sets show a distinct linear array in 38 images. Whole domain of the directional angle(${\theta}$)-frequency(N) chart for crystalline tuff can be divided into 20 domains in terms of the phases of the distribution of microcracks. From the related chart, microcrack sets show preferred orientation which are coincident with the direction of vertical common joints. Consequently, the potential for macroscopic vertical joints in a rock body can be inferred from the directional angle showing high frequency in each domain of the related chart. This joint pattern is nearly the same in Mesozoic granites from Seokmo-do, Gwanghwa-gun. From the rose diagram for orientations of microcrack in crystalline tuff, orientations of dominant sets of microcracks in terms of frequency orders reflect representative orientations of maximum principal stress acted on crystalline tuff. Meanwhile, orientations of microcracks in crystalline tuff were compared with those of open microcracks in Bulgugsa granites from the southwestern part of the Gyeongsang Basin, and vertical rift/grain planes from Mesozoic granite quarries in Korea. In regional distribution chart, the agreement of distribution pattern between above two types of microcrack sets and vertical planes suggests that microcrack systems developed in crystalline tuff probably occur regionally in Mesozoic granites in Korea.

• Journal of the Korea Academia-Industrial cooperation Society
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• v.17 no.12
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• pp.153-161
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• 2016

Urban design claiming the notion of 'Sustainability', which inevitably includes ecological complexity, is normally geared towards the reflection of environmentally-friendly technical guidelines in the existing planning process. Although physical planning should be combined with economic, social, cultural, environmental issues, and policies, it is conducted conventionally as the sum of the closed sectoral approaches of planning. To overcome this limit, Design Charrette was invented for sustainable urban design or community design, which should consider the complexity of diverse issues. This design process unveils complicated and divergent problems and a variety of stakeholders participate in the integrated design simultaneously and cooperatively. Because Design Charrette must also be a process of agreement, it is used for sustainable community design. The aim of this study was to introduce Design Charrette as an alternative of Korean sustainable urban design, which is regarded as 'making guidelines related to green principles'. For such a purposes, the definition and differentiation of Design Charrette will be explained with an analysis of the introduction background, benefit and procedure. The contents, system and process of Design Charrette will be analyzed through case studies in Canada, where this method of design is widespread. In the last part, the implementation system (the comprehensive system of organization / content and direction of planning / process and output) will be deduced after concentrated analysis of one respected case, 'Sensitive Urban Infill Charrette' of the City of Surrey. This implementation system will be a crucial reference to develop Korean Design Charrette.

• Research in Community and Public Health Nursing
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• v.1 no.1
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• pp.174-175
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• 1989

본 연구는 보건진료원의 업무를 분석하기 위하여 충북에서 활동하고 있는 보건진료원 136 명을 대상으로, 설문지를 흥해 자료수집을 하였으며 백분률, 평균값, 표준편차로 자료처리를 하였다. 조사기간은 1968 년 8월 1일부터 11월 20일까지 했으며 그 결과를 요약하면 다음과 같다. 1. 보건진료원의 일반적 특성과 업무에 관련 된 배경을 살펴보면 다음과 같다. 보건진료원의 일반적 특성으로 연령 분포는 30 - 34세가 30.1 %로 가장 많았고 결혼 상태는 기혼자가 61.8 % 였다. 종교는 기독교가 42.6% 로 많았고 학력은 3 년제 간호전문대학 과정졸업 자가 78.9 %로 많았다. 현 가족과 동거상태에서 배우자와 자녀가 함께 사는 경우가 76.5% 였고, 보건진료원의 경력은 1 년 마만이 41.2 %로 가장 많았다. 보건진료원의 업무에 관련된 배경을 살펴보면, 근무지역조건은 갑지가 65.3 % 였고, 현 거주지는 보건진료소내 숙소가 대다수 였다. 보건진료소는 신축된 건물이 대다수였고, 보건진료소 시설은 '그저 그렇다'고 대답한 수가 가장 많았다. 보건진료소 운영협의회 수당은 월 $5\sim7$만원인 경우가 85.6 % 였다. 2. 보건진료원의 보건의료제공 실태는 다음과 같다. 보건진료원이 현재 담당하는 주민수는 $501\sim1,000$ 명이 35.3 % 이고, 1,500 명 이상의 주민을 담당하는 경우도 32% 였다. 보건진료소를 이용한 주만은 연평균 1,956 명이고, 보건진료소 평균 이용건수는 1,812건이다. 보건진료원의 직업만족도는 만족한다가 40.6%로 대체로 긍정적으로 나타났다. 3. 보건진료원과 보건의료 관련기관과의 관계는 다음과 같다. 지역주민의 보건의료자원 이용 정도는 보건소 진료소가 1 위로 가장 많았고, 약국, 약방, 의원, 보건지소의 순위로 나타났다. 보건의료 관련기관과의 협조가 잘 되고 있지 않다고 응답한 경우도 있는데, 보건소(19.7 %), 보건지소( 20.2%) 민간보건 의료기관(22.4 %)이며, 그 이유를 알아서 협조가 잘 이루어지도록 노력해야겠다. 원하는 감독체계는 보건소장(47.3 %), 보건간호 전문가(37.2 %)로 나타났으나 이는 현재있는 감독체제내에서 생각한 것이며 간호전문가에 의한 새로운 감독체제를 원하고 있었다. 많이 이용하는 의뢰 기관은 병원(52 %), 의원(24.4 %), 보건소(10.2 %) 순이었다. 4. 보건진료원의 업무 영역별 수행정도를 살펴보면 다음과 같다. 보건진료원의 업무 영역을 7개 영역으로 구분하여 수행평균 평점을 보면통상질환 관리가 3.70점, 사업운영 관리 및 지도가 3.44 점, 사업계획 수립이 3.19 점, 지역사회 조직 및 개발이 3.17 점, 모자보건 및 가족계획이 3.14 점, 지역사회 보건관리가 3.09 점, 보건 정보체계 개발이 3.02 점으로 나타났다. 위의 결과에서 지역사회 보건관리가 3.09점으로 통상질환 관리 3.70 점 보다 낮게 나타났는데 이는 일차보건의료 사업 정착의 과도기적인 현상으로 생각하며, 이 부분을 더 많이 수행해야 할 것으로 사려된다. 5. 보건진료원의 업무 영역별 수행 소요시간의 평균은 다음과 같다. 지역사회 조직 및 개발 3.48 시간, 사업계획 수립 3.55 시간, 지역사회보건 관리 6.74 시간, 모자보건 및 가족계획 5.55 시간, 통상잘환 관리 15.94시간, 사업운영 관리 및 지도 4.39시간, 보건정보체계 3.62 시간으로 나타났다. 보건진료원이 통상질환 관리와 더불어 예방활동을 효율적으로 할 수 있도록 적절한 행정적, 교육적 지원이 있어야 한다고 생각한다.

• Journal of the Korean Geotechnical Society
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• v.34 no.9
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• pp.5-17
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• 2018

A magnitude 5.4 earthquake struck the city of Pohang, North Gyeongsang Province, South Korea on November 15, 2017. Many sand volcanoes were observed on paddy fields, parks and roads. This phenomenon was the first to be observed as a sign of soil liquefaction in South Korea. In this study, two different kinds of ejected Pohang sands were collected from a liquefied paddy field. Those sands were reconstituted into loose and dense conditions and then a series of cyclic simple shear tests were conducted under confining stresses of 100 and 200 kPa. A real earthquake motion was also repetitively applied to the specimen. As a result of constant shear stress tests, the cyclic resistance ratio (CRR) of loose sand was 0.12-0.14, while the CRR value of dense sand was 0.17-0.21. It was shown that the relative density was more influencing factor on liquefaction resistance than the sand types and initial confining stress. When a real Pohang earthquake motion was repetitively applied to the specimen, a loose sand was liquefied at the second earthquake motion but the dense sand at the third earthquake motion.

• The Korean Journal of Petroleum Geology
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• v.2 no.2 s.3
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• pp.91-99
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• 1994

In the Heunghae area, genetic relationships among sedimentary facies, lithology, stratigraphy and diagenetic mineral facies of the Yeonil Group, are discussed. Conglomerate and sandstone of lower to middle parts of the Yeonil Group contain considerable amounts of volcaniclastic sediments, which were derived from the Tertiary volcanics exposed in the western margins of the sedimentary basin. A new stratigraphic division of the Yeonil Group into the Chunbuk and Pohang Formations is proposed on the basis of sedimentary facies, lithologic characteristics including volcaniclastic feature, and the presence of a key bed of siliceous mudstone overlying the Chunbuk Formation. Diagenetic mineral facies largely depend on the lithology and composition of sediments. Heulandite, smectite, calcite, and opal-CT are commonly found as diagenetic minerals in the Yeonil Group. Among these authigenic minerals, heulandite occurs as the coarse- grained main cement in conglomerates and sandstones of the Chunbuk Formation. Formation of the zeolite cement is favored by partial volcaniclastic lithology of the Chunbuk Formation. Smectite composition and diagenetic mineral facies such as heulandite and opal-CT may reflect that the Yeoil Group has undergone a shallow rial temperature ranging $40{\~}60^{\circ}C$.

• Korean Journal of Heritage: History & Science
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• v.43 no.3
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• pp.122-143
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• 2010

The Shilla Stone Monument in Jungseongri was found during the road-construction in Pohang. It has approximately two hundreds of letters inscribed on the surface of one side, and it is estimated to be older than Shilla Stone Monument in Naengsuri which had been known for the oldest stele in Shilla Period. This monument is made of fine to medium-grained biotite granite, while the Shilla Stone Monument in Naengsuri is made of fine-grained granodioritic porphyry bearing feldspar and amphibole phenocrysts. Both rock types of the monuments are interpreted to be cognate with biotite granite in Shinkwangmyeon, and with granodioritic porphyry in Gigyemyeon. They are characterized by xenolith and miarolitic cavity. Damage aspects in both monuments are discoloring, cracking and breaking. These damages do not cause structural instability of the monuments, but attenuate aesthetic value. Black and brown discoloring contaminants on the surface of the Jungseongri Monument contain a high amount of manganese and iron. As a result of ultrasonic test, both monuments were evaluated to be medium-weathered (MW), although the velocity of the Shilla Monument in Jungseongri was slightly lower than the Shilla Monument in Naengsuri. This is because the Monument in Juengseongri had been exposed to outdoor environment for long time until the discovery. It is necessary for Shilla Monuments to be protected by appropriately environmental control and management.

• The Journal of Engineering Geology
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• v.32 no.4
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• pp.559-569
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• 2022

This study investigated the acidification and mixing with seawater of groundwater, stream water, and reservoir water in the Hunghae area of Pohang City, as well as the source of water expelled to the stream by liquefaction induced by the Pohang earthquake on 15 November 2017. Geologically, the area consists of Tertiary sedimentary rocks. We collected six samples of groundwater, five of reservoir water, four of stream water, two of liquefaction water, and one of seawater to analyze the chemical composition and stable isotopes (𝛿D and 𝛿¹⁸O). Gogkang Stream flows eastward through the central part of the study area into the East Sea. The groundwater and reservoir water in the lower part of the stream are acidic (pH < 4), have a Ca(Mg)-SO₄ composition, and high concentrations of Al, Fe, and Mn, likely due to the oxidation of pyrite in Tertiary rocks. The groundwater in the upper part of the stream have a Ca(Na)-HCO₃(Cl) composition, indicating the mixing of seawater with the stream water. The 𝛿D and 𝛿¹⁸O isotope data indicate the isotopic enrichment of reservoir water by evaporation. Based on the chemical and isotopic data, it is inferred that the two samples of liquefaction water originated from alluvium water in a transition zone with stream water, and from deep and shallow groundwaters that has been infiltrated by seawater, respectively.

• The Journal of the Petrological Society of Korea
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• v.18 no.4
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• pp.315-336
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• 2009

We have studied the orientational characteristics of microcrack frequency, it's length and density in Tertiary crystalline tuff from the northeastern part of the Gyeongsang Basin. 134 sets of microcracks on horizontal surfaces of 3 rock samples from Heunghae-eup were distinguished by enlarged photomicrographs of the thin sections. The variability in patterns among microcrack length-frequency histograms for three rock samples from different altitudes were derived. The pattern of histograms changes progressively from negative exponential form to log-normal form in proportion to altitude. The distribution pattern for rock sample no.1 from lower altitude shows the broad length distribution characterized by higher mean and median, and higher standard deviation. Meanwhile, this distribution pattern corresponds with characteristics of joint length distribution in sedimentary rocks of the lower part of the Gyeongsang Supergroup. The occurrence frequency of shorter microcracks increases toward both NW and NE directions from the $N0{\sim}10^{\circ}W$, with the dominant direction of $N80{\sim}90^{\circ}W$ and $N80{\sim}90^{\circ}E$, respectively. This distribution pattern represents the relative differences in formation timing among microcrack sets and the result of the new initiation of shorter microcracks. Meanwhile, the longest microcracks within $N60{\sim}70^{\circ}W$($L_{max}$:1.18 mm) and $N0{\sim}10^{\circ}W$($L_{max}$:0.80 mm) directions are seen, but this kind of microcracks are very limited in number. Whole domain of the directional angle($\theta$)-frequency(N), length(L) and density($\rho$) chart can be divided into five sections in terms of phases of the distribution of related curves. From the distribution chart, density curve shows five distinct peaks in the WNW-ESE($N70{\sim}80^{\circ}W$), NS~NNE-SSW($N0{\sim}10^{\circ}W$, $N10{\sim}20^{\circ}E$), ENE-WSW($N50{\sim}60^{\circ}E$), and nearly EW($N80{\sim}90^{\circ}E$) directions, respectively. Especially, main directions of faults correspond with the directional angle showing high density. Consequently, these distribution patterns of density curve reflect the representative maximum principal stress orientations suggested in previous studies.

• Geophysics and Geophysical Exploration
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• v.8 no.2
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• pp.145-155
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• 2005

A two-dimensional (2-D) interpretation of MT data has been performed for the purpose of fracture detection for geothermal development. Remote stations have been operated in Kyushu, Japan (480 km apart) as well as in Korea (60 km and 165 km apart in 2002 and 2003 data set, respectively). Apparent resistivity and phase curves calculated by remote processing with the Japan remote data showed enough quality for 2-D inversion for the whole frequency range. Remote reference processing with Korea remote reference data also showed quite good continuity in apparent resistivity and phase curves except some noisy frequency bands; around the power frequency, 60 Hz, and around the dead band $10^{-1}Hz\;Hz\;\~1\;Hz$, where the natural EM signal is known to be very weak. Even though the subsurface showed severe three-dimensional (3-D) characteristics in the survey area so that 2-D inversion by itself could not give enough information for deep geological structures, the 2-D inversion for the 5 survey lines showed several common features. The conductive semi-consolidate mudstone layer is dipping from north to south (about 500 m depth on the south and 200 m on the north most part of the survey area). The boundary between the low (L-2) and high (H-2) resistivity anomalies can be thought as a major fault with strike $N15^{\circ}E$, passing through the sites 206, 112 and 414. The shallow (< 1 km) conductive anomalies (L-4) seem to be fracture zones having strike E-W (at site 105) and $N60^{\circ}W$ (at site 434). And there exists a conductive layer in the western and west-southern part of the survey area in the depth below $2\~3\;km$, for which further investigation is to be needed.