태풍 파랑과 지진을 연계한 케이슨식 방파제의 동적거동

윤현수,노병진,윤성규,강기천,Hyeonsu Yun,Byeongjin Roh,Seong-Kyu Yun,Gichun Kang 한국지반신소재학회 2024 한국지반신소재학회 논문집 Vol.23 No.1

Recently, the frequency and intensity of typhoon-induced wave loading are increasing due to changed marine environments such as climate change. In addition, frequent earthquakes are causing a lot of damage around the world, including in Japan, Chile, Haiti, China, and Indonesia. In Korea, damage from typhoons has also been increasing since the 2000s, and the frequency and intensity of earthquakes are also increasing. Korea is surrounded by sea on three sides, so typhoons can cause a lot of damage to coastal structures, and earthquakes also cause a lot of damage to coastal structures. As such, the frequency and intensity of typhoon-induced wave loading and earthquakes are increasing both domestically and internationally, but there is no research linking typhoons and earthquakes. Therefore, in this study, numerical analysis was performed for a total of four cases by linking typhoon waves and earthquakes to the caisson breakwater. Numerical analysis was performed by applying wave loads in Case 1 and seismic wave in Case 2, seismic wave after wave loads in Case 3, and wave loads after seismic wave in Case 4. As a result of the numerical analysis, it was confirmed that in Case 3 and Case 4, which linked a typhoon and earthquakes, the damage caused by each load increased compared to Case 1 and Case 2 because the load was applied while the existing ground strength was reduced. In addition, it was confirmed that the greatest damage occurred in Case 3, in which seismic wave were applied after the wave loads.

함백분지(咸白盆地) 남부지역(南部地域)에 분포(分布)하는 백악기(白堊紀) 화강암질암류(花崗岩質岩流)의 암석화학적(岩石化學的) 연구(硏究)

윤현수,Yun, Hyun Soo 대한자원환경지질학회 1986 자원환경지질 Vol.19 No.no.spc

The Geodo granodiorite intruded into the Joseon Supergroup is fine-grained at the marginal part, and medium-grained and more leucocratic at the central part. The Quartz monzonite porphyry intruded inte Precambrian granite and Geodo granodiorite has abundant plagioclase phenocryst. The Imog granite intruded into the Yulri Group and the Joseon Supergroup is mediumgrained biotite granite with partly pinkish feldspar phenocryst. The K/Ar ages obtained from the biotite of the Geodo granodiorite and Imog granite are Early ($111{\pm}1{\sim}107{\pm}1$ Ma) and Late ($93{\pm}1{\sim}92{\pm}1$ Ma) Cretaceous, respectively. The K/Ar sericite age of the quartz-sericite zone of the lower Jangsan quartzite occuring in the western area gave much younger age (about 170 Ma) than that of the Jangsan quartzite, that might be reset due to the regional metamorphism of the Daebo orogeny. The granitic rocks of the area are felsic to mafic, metaluminous to peraluminous, calc-alkalic (alkali-lime index${\fallingdotseq}$ 57) and I-type (magnetite-series) based on the chemical data_ And they appear to have been fractionated at the order of Geodo granodiorite, Quartz monzonite porphyry and Imog granite. In terms of mineralogy, geochemistry and K/Ar biotite age, a rock suite of monzodiorite, quartz monzodiorite and quartz monzonite-granodiorite in the Geodo stock was fractionally differentiated from a magmatic body from its margin to inward.

함백익지(咸白益地) 기반지역(基盤地域)에 분포(分布)하는 선(先)캠브리아 화강암질암류(花崗岩質岩類)의 암석화학적(岩石化學的) 연구(硏究)

윤현수,이대성,Yun, Hyun Sao,Lee, Dai Sung 대한자원환경지질학회 1986 자원환경지질 Vol.19 No.1

The area of this study is located in the Sang dong district, Youngwol Gun, Kangwon Do, where the Ogcheon fold belt comes into contact with the Ryongnam massif. The area is covered by the Precambrian metasedimentary rocks of Yulri Group in the south from the line of Ungyosan-Maebongsan-Jansan-Taebaegsan Mountains and by the Cambro-Ordovician sedimentary rocks of Choseon Supergroup in the north. The Choseon Supergroup unconformably overlies the Yulri group. Several granitic intrusives occur in the Precambrian and Cambro-Ordovician terrain. The purpose of this study is to clarify the geochronology, mineralogical composition, geochemical characteristics, petrogenesis and tectonic settings of the Precambrian granitic rocks, and to evaluate the P.T. conditions of granitic intrusions. The K/Ar ages obtained from the muscovite of Nonggeori Granite, Naedeogri granite and pegmatite intruded into the Yulri Group are Early Proterozoic ($1805{\pm}18Ma$ to $1642{\pm}23Ma$), and those from the migmatitic pegmatite are Late Carboniferous ($305{\pm}4Ma$), respectively. The Precambrian granitic rocks are characterized by the presence of muscovite, tourmaline and grey feldspar with faint lineation of mafic minerals. In terms of mineralogical and chemical composition, the granitic rocks are felsic, calc-alkalic, peraluminous and S-type (ilmenite-series). The geochemical characteristics of major and trace elements indicate that the granitic rocks belong to syn-collision setting at the compressional plate margin. They were formed by progressive melting of relatively homogeneous crustal materials under 1~3kb and $670^{\circ}{\sim}720^{\circ}C$ in aqueous fluid conditions, and the Naedeogri granite was more fractionated than the Nonggeori granite. During the Taebaeg disturbance, Nonggeori granite, Naedeogri granite and pegmatite were intruded and emplaced into the Yulri Group. Migmatitic pegmatite occurring in the southwestern area, however, gave much younger muscovite age than the pegmatite intruded into the Yulri Group in rest of the area did, that might be due to the regional metamorphism of the Post-Choseon disturbance. The Geodo granitic mass and the Imog granite were intruded during the Bulgugsa disturbance.

문경남부일대(聞慶南部一帶)에 분포(分布)하는 백악기(白堊紀) 화강암류(花崗岩類)의 미량원소(微量元素) 및 광물화학(鑛物化學)

윤현수,Yun, Hyun Soo 대한자원환경지질학회 1991 자원환경지질 Vol.24 No.4

The studied Cretaceous granties are widely distributed at the southern Mungyeong area in the southwestern part of Ogcheon Fold Belt. From the mineralogical and geochemical compositions, it is suggested that they show the characteristics of I-type and magnetite-series and formed under the conditions of high oxygen fugacity. The mineral chemistry of plagioclase, alkali feldspar and biotite in the granites by EMPA, was revealed as albite to oligoclase, microcline to microcline perthite and orthoclase perthite, and annite compositions, respectively. The granites have the distribution patterns of enriched LREE and depleted HREE, and show Eu negative anomalies suggesting mainly due to the feldspar fractionation in the residual magma. The geochemical data of Eu, EU/$^*Eu$, Sm and Gd suggest that the granites of the area have more abundant alkali feldspar crystallization than plagioclase. From the geochemical characteristics of Sr/Ba, La/Sm vs. Ce/Yb and other trace element evidences, the granites were the late stage products of differentiation and fractionated from a homogeneous parental granitic magma.

상동지역(上東地域) 선캠브리아 화강암류(花崗巖類)의 K-Ar 백운모(白雲母) 연령측정(年齡測定)

윤현수,Yun, Hyun Soo 대한자원환경지질학회 1991 자원환경지질 Vol.24 No.1

The studied Nonggeori and Naedeogri granites in the Sangdong area intruded into the Precambrian metasedimentary rocks of the Yulri Group. The Cambro-Ordovician Choseon Supergroup overlied unconformably upon the Yulri Group. Pegmatitic dykes injected into the Yulri Group and the granites, but not in the Choseon Supergroup. Field relationships suggest approximate ages of the intrusive rocks in the studied area belong to the Precambrian. Extremely pure concentrates of muscovites(40-80#) were obtained from the granites by conventional isodynamic magnetic separators. The contents of K and 40Ar in the muscovites show 8.60-8.78% and 98.52-99.11%, respectively. From the potassium contents of the muscovites and the approximate ages, the sample amounts for argon analyses are average of 0.00371gr. The K-Ar ages on the muscovites were revealed as Proterozoic ($1673{\pm}22{\sim}1802.5{\pm}17.5Ma$).

문경(聞慶) 남부일대(南部一帶)에 분포(分布)하는 백악기(白惡紀) 화남암류(花南岩類)의 암석학(岩石學) 및 암석화학(岩石化學)

윤현수,김선억,Yun, Hyun Soo,Kim, Seon Eok 대한자원환경지질학회 1990 자원환경지질 Vol.23 No.3

The Cretaceous granites are widely distributed in the studied area, Mungyeong-Sangju, which belongs to the southwestern part of the Ogcheon Folded Belt. The granites are characterized by medium-coarse grained, spotted miaroles, partly flow textures of biotite, aplitic dykes and pegmatitic pockets with druse. From the major compositions, the granites indicate peraluminous, calc-alkaline, salic and late stage products of differentiation. In the view of normative compositions of Qz-Ab-Or and perthitic alkali feldspar, they were formed under 1-4kb and $426^{\circ}-456^{\circ}C$ in acqueous conditions. The K/ Ar biotite age shows $72{\pm}1$ Ma for this grante, corresponding to the igneous activity of the Bulgugsa Disturbance periods in the area. The above results represent that these granite bodies are differentiated from a single magma.

저에너지건축물 설계를 위한 건축물 단열성능의 효과적 조정과 야간외기 도입에 따른 에너지 시뮬레이션 연구

윤현수(Hyun-Su Yun),이태규(Tae-Kyu Lee),김정욱(Jeong-Uk Kim) 한국산학기술학회 2018 한국산학기술학회논문지 Vol.19 No.10

본 연구는 최근 자원고갈 문제에 따른 에너지 절감을 바탕으로 총 에너지 수요에서 높은 비중을 차지하고 있는 건축물 에너지의 수요 감축에 목적을 두었고 국내에서 에너지절약형 건축물 설계를 위해 고시한 단열기준을 보다 효과적으로 조정하기 위한 보완점을 제시하고 에너지절약형 고단열, 고기밀 건축물의 쾌적성 유지의 한계점을 추가 보완하고자 야간외기 환기시스템을 도입하며 종합하여 최종 저에너지건축물 설계모델을 제시하였다. 먼저, 단열성능의 효과적 조정 모델은 건축물의 각 경사면별로 다르게 조정하여 각각의 수요 민감도를 충분히 고려할 수 있는 방법을 제시하고, 야간외기 도입 모델의 경우 건축물의 에너지 성능을 최대로 할 수 있는 모델을 선정하였다. 두 가지 모델을 결합한 최종 저에너지건축물 모델은 결과적으로 대상 건축물의 남, 북의 경사면 단열을 강화한 모델과 야간외기를 통한 환기 시스템을 단시간 운전한 모델이었으며 국내 단열기준에 의거한 Base 모델과 비교할 때 약 6~7%의 절감효과를 보였다. 따라서, 본 연구에서 제시하는 효과적 단열조정법과 야간외기 도입은 저에너지건축물 모델 설계에 있어 수요 민감도 분석 선행의 필요성을 환기시키는 점에서 시사점이 높고 대상 건축물의 건물에너지 수요를 저감할 수 있는 설계모델로 활용도가 높을 것이다. This study was done to reduce total energy demand based on resource shortage problems and to provide improvement points for more efficient adjustment of the high insulation standards for saving energy in Korea. The demand sensitivity was fully considered by varying the slope of each building. The energy performance of the building was maximized by the introduction of outdoor air at night. A final low-energy building model was developed with the two measures combined, and the short-term operation of the night-fuzzy ventilation system was simulated. The result showed a reduction of about 6 to 7 percent compared to the base model. The results could have many implications in terms of the need to conduct demand sensitivity analyses in architectural design.

낭산일대에 분포하는 화강섬록암 암석자원의 열극체계 및 물리적 특성

윤현수(Hyun Soo Yun),홍세선(Sei Sun Hong),박덕원(Deok Won Park) 한국암석학회 2007 암석학회지 Vol.16 No.3

낭산지역 일대의 쥬라기 흑운모 화강섬록암은 담회색, 치밀조직을 이루는 중립질암이다. 암체에 대한 광역적인 열극체계 분석결과는 다음과 같다. 열극의 주향은 빈도등급에 의하여 크게 세 방향으로 분류가 가능하다. 이들 열극은 빈도등급에 의하여 (1) N80°~90°E (1st-order) > (2) N70°~80°E (2nd-order) > (3) NS~N10°E (3rd-order)의 순으로 나타난다. 특히 이들 열극의 간격은 200 cm 미만의 것들이 대부분을 차지한다. 따라서 분석된 열극체계 및 간격으로 미루어 낭산일대에서는 규격석보다 비규격석의 산출이 훨씬 많아 쇄석자원의 잠재성이 더 클 것으로 해석된다. 특히 밀집하는 기존 석산의 수직상 채석면의 방향도 빈도등급에 의하여 두 그룹으로 분류되어, (1) N14°W~N16°E (1st-order)와 (2) N78°E~N88°E (2nd-order)에서 뚜렷이 우세하다. 상기한 두 그룹의 수직상 채석면의 방향은 광역적 열극체계와는 다소 차이가 있다. 이와 같은 현상은 단위 석산에서 발달하는 미세균열의 배향성과 크게 관련되는 것으로 볼 수 있다. 낭산지역의 물성 중에서 비중, 흡수율, 공극률, 압축강도, 인장강도와 마모경도는 각각 2.65, 0.28%, 0.73%, 1,628 ㎏/㎠, 100 ㎏/㎠ 및 31의 평균값을 가진다. 공극률의 경우와는 달리, 낭산 및 속리산지역의 화강암류는 상호 유사한 마모경도를 가진다. 이는 마모저항의 지표로 간주되는 석영과 알칼리장석의 모우드 값의 차이로 설명될 수 있다. 한편 낭산지역의 연구를 통하여 규명된 수직상 채석면의 방향 및 각종 물성특성의 전반적인 이해는 차후 이 지역의 암석자원 활용 시 주요 정보로 활용될 것으로 기대된다. The studied Nangsan area is widely covered by the Jurassic biotite granodiorite, which is mainly light grey in color and medium-grained in texture. Results of the regional fracture pattern analysis for the granodiorite body are as follows. Strike directions of fractures show three dominant sets in terms of frequency order. The sets are in an order of a (1) N80°~90°E (1st-order) > (2) N70°~80°E (2nd-order) > (3) NS~N10°E (3rd-order). Spacings of the fractures are mostly predominant in less than 200 cm. Therefore, the granodiorite of the area has more potential for non-dimensional stones than dimension ones. And orientations of vertical quarrying planes can be also divided into two groups in terms of frequency: (1) N14°W~N16°E (1st-order) and (2) N78°E~N88°E (2nd-order). The orientations of the two groups are more or less different from those of the regional fracture patterns. These can be mainly attributed to the preferred orientations of microcrack developed in the quarries. Of physical properties, specific gravity, absorption ratio, porosity, compressive strength, tensile strength and abrasive hardness are 2.65, 0.28%, 0.73%, 1,628 ㎏/㎠, 100 ㎏/㎠ and 31, respectively. Contrary to the porosity, both granites of the Nangsan and Sogrisan areas show almost similar values of the abrasive hardness. These can be explained by the differences of Qz + Af modes, which can be regarded as an index for abrasive resistance. Meanwhile, it is anticipated that comprehensive understanding of the orientations of vertical quarrying planes and characteristics of various physical properties will be utilized as an important information for stone resources.

경기북부 갈말-영북일대 백악기 홍색 각섬석흑운모화강암의 암석화학

윤현수(Hyun Soo Yun),홍세선(Sei Sun Hong),김정민(Jeongmin Kim) 한국암석학회 2006 암석학회지 Vol.15 No.4

갈말-영북일대의 화강암류는 암상에 의하여 회색 각섬석흑운모화강암(JHBG), 흑운모화강암(JBG)과 홍색 각섬석흑운모화강암(CHBG)으로 분대될 수 있다. 전지는 북부에 소규모로 분포하는 중립질암으로서 미립 질 스펜을 함유하며, JBG는 북부-동부일대에 주로 분포하는 담회색-회색의 중립질암이다. 주연구대상인 후자는 대부분 북부-남동부일대에 넓게 발달하는 중-조립질암으로 뚜렷한 홍색을 띠며, 국부적으로 미세 공동구조와 정동구조의 포켓상 페그마타이트질부가 발달된다. 광물연령(K-Ar 법)으로 미루어 JHBG와 JBG는 시기를 달리하는 쥬라기 대보조산운동기의, CHBG는 백악기 불국사변동기의 화성활동산물이다. 이는 야외산상 및 지질 선후관계 해석과도 잘 일치한다. CHBG는 석영, 사장석, 알칼리장석, 흑운모, 각섬석, 갈렴석, 인회석, 져어콘, 일부 방해석과 불투명광물 등으로 구성된다. 이 중에서 알칼리장석은 대부분 퍼다이트질 정장석이며, 드물게 수반되는 방해석은 미세공동의 이차적 충전광물로 보인다. 모우드 분석 및 QAP 삼각도에서 모두 화강암영역에 속하며, 대부분 섬장화강암과 몬조화강암의 경계부에 도시된다. 주원소 변화경향, A/CNK 몰비, SiO₂ 대 K₂O 그리고 AMF 관계 등으로 미루어, 이 암은 단일한 화강암질 마그마에서 생성된 산성암, 고-칼륨의 캘크-알카린계열 그리고 과알루미나암질의 분화말기 산물이다. Ba 대 Sr 관계에서도 분화경향을 뚜렷이 이루며, CaO 대 Sr 그리고 K₂O 대 Sr 관계로 미루어 Sr이 알칼리장석보다 사장석의 분별결정작용에 더 관여하였다. 희토류원소 표준화도에서 경희토류원소에서 중희토류원소로 갈수록 점진적으로 뚜렷이 결핍되는 양상을 이룬다. 그리고 Eu의 부 이상과 표준화값 등으로 미루어 사장석의 분별결정작용이 이 화강암 전체에 걸쳐 미약하게 일어난 것으로 보인다. Division of granites in the Galmal-Yeonbug area, northern Gyeonggi, can be grey hornblende biotite granite (JHBG), biotite granite (JBG) and pink hornblende biotite granite (CHBG) by lithofacies. JHBG of small stock occurs as medium-grained with grey color and minute sphene. JBG occurs as medium-grained and light grey to grey in the north-east part of the area. The main study target CHBG covers in the north-southeast part of the area, and occurs medium- to coarse-grained with pink color. CHBG shows partly minute miaroles, and pegmatitic pocket with druse texture. From the mineral age data (K-Ar method), JHBG and 180, and CHBG are the igneous activity products of Daebo orogeny with different Jurassic and Bulgugsa disturbance of Cretaceous, respectively. And the age data also agree with geologic occurrences and interpretations of the granites in the field. CHBG consists of quartz, plagioclase, alkali-feldspar, biotite, hornblende, allanite, apatite, zircon, some calcite and opaques. Among them, alkali-feldspar and calcite occur characteristically in mostly perthitic orthoclase and secondary filling of minutely miarolitic cavity, respectively. In modal analysis and QAP diagram, CHBG plots in granite field, and especially boundary of monzo- and syeno-granite fields. From the major oxide variations, molar A/CNK, SiO₂ vs K₂O, AMF and so on, CHBG belongs to the acidic, peraluminous and high-K calc-alkaline, and was late differentiation product of single granitic magma. Barium and strontium have also dominantly differentiation trend, and in CaO vs Sr and K₂O vs Sr, Sr was more participitated in the fractionation of plagioclase than that of alkali-feldspar. Normalized REE concentrations to chondrite value have parallel and gradual LREE enrichment and HREE depletion patterns, and weak Eu negative anomalies and narrow ranges of normalized Eu can suggest that plagioclase fractionations occurred mildly in the whole CHBG.

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윤현수 ( Hyun Soo Yun ),오세진 ( Se Jin Oh ),이상필 ( Sang Phil Lee ),오승민 ( Seung Min Oh ),김록영 ( Rok Young Kim ),김성철 ( Sung Chul Kim ),양재의 ( Jae E. Yang ) 한국토양비료학회 2012 한국토양비료학회 학술발표회 Vol.2012 No.-