• Journal of Ocean Engineering and Technology
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• v.32 no.5
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• pp.361-366
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• 2018

The present study analyzed the variation factors in inducing a salinity change using the existing observation network in the section between the Nakdong River Estuary Barrage and Changnyeong-Haman Weir, and also examined the seasonal changes in precipitation, salinity, and discharge. Furthermore, this study analyzed the causes of a salinity increase by collecting observational data during a period when abnormal salinity occurred, and further investigated the salinity transfer time in a section of approximately 5.3 km from the Nakdong River Estuary Barrage to Nakdong River Bridge to understand the behavioral characteristics of the salinity moving upstream. The study results would make it possible to control the increase in salinity and block salt water from moving upstream by understanding the salinity variation characteristics according to the discharge amount. This will provide stability in collecting water from various residential, agricultural, and industrial sources through water intake facilities scattered near the Nakdong River Estuary Barrage.

• The Journal of the Petrological Society of Korea
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• v.9 no.1
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• pp.1-12
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• 2000

The Cretaceous basaltic rocks in Gyeongsang Basin are temporally and spatially dispersed widely in thick sedimentary piles: Chilgog basaltic rock (CGB) and Cheongyongsa basaltic rock (CSB) in the Shindong Group, and Hakbong basaltic rocks (HBB), Osibbong basalt (OSB), Secheondong basaltic rocks (SCB), Haman basaltic rocks (HAB), Hama basaltic rocks (HMB), and Chaeyaksan basaltic rocks (CYB) in the Hayang Group, upwardly in their stratigraphy. Chilgog basaltic rock is merely identified as pebbles in the Shilla Conglomerate and its provenance has not been found, and it is characteristics that the volcanics except Osibbong basalt and Chaeyaksan basaltic rocks are very small in both of their thickness and extension. Petrochemical diversity of the basaltic rocks are revealed; OSB and SCB distributed in the Yeongyang Minor Basin preserve the calc-alkaline natures in major and immobile minor element geochemistry, but CGB, HBB, HAB, and CYB reflect that they might be originated from calc-alkaline basaltic magma of volcanic arc in continental margin area by trace elements and altered to alkaline suites in the viewpoint of their major element geochemistry. Major and trace element geochemistry of CSB and HMB suggests that they may be derived from within -plate alkaline magma contaminated by the upper continental crust, especially in the case of the former.

• Korean Journal of Heritage: History & Science
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• v.55 no.3
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• pp.152-176
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• 2022

This paper, a basic study on the restoration of arrow quivers during the Three Kingdoms Period, aimed to contribute details to the existing plan to restore the arrow quivers. The arrow quivers of the Three Kingdoms Period consist of a pouch for holding arrows and a backpiece. However, the two parts do not remain, and only metal parts have been excavated. The excavated arrow quivers were classified into three types for restoration. Centered on the pouch, the quivers were classified into type 1 made up of a W-shaped part and ㄷ-shaped part, and type 2 with only the band-shaped piece identified. Type 3 is similar to type 2, but it is assumed to be a separate type where an iron band extending from the hanging piece(吊手金具) is connected to a band-shaped piece. Before proposing a restoration plan for the three types of arrow quivers, the location of the hanging piece (吊手金具) and the observation of organic matter were reflected. In addition, such details as the location of the hanging piece (吊手金具), which cannot be identified by the excavation status alone, were derived from the ways of wearing the arrow quivers observed in the Joseon Dynasty, Shosoin (正倉院), and Haniwa (埴輪) in Japan. Referring to the existing record on the transformation of arrow quivers based on the hanging piece (吊手金具), the arrow quivers change from type 1 to types 2 and 3 in this paper. However, some of types 2 and 3 maintain the ways of wearing of type 1, and there were cases where the old-fashioned parts were kept. In particular, in Haman (咸安), it was confirmed that the typical type 1 was buried up until late periods.

• Journal of the Korean Society of Food Science and Nutrition
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• v.33 no.1
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• pp.140-145
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• 2004

This study was performed to compare and investigate major quality characteristics of traditional dried persimmons from various regions (Sangju, Haman, Youngdong and Dongsang) The moisture contents of dried persimmons were highest contained on 38.20％ at Sangju and crude protein contents were range from 1.41％ to 2.40% and crude fat contents were 0.11% to 0.20% and crude ash contents were 0.99% to 1.27%. Water activity (Aw) of dried Persimmons was 0.781 in Sangju and Brix was 55.1% in Sangju. In case of Hunter's value, ‘L’ value of dried persimmons was bright color value in Sangju (34.05) and Youngdong (33.06). ‘a’ value of dried persimmons was more red value in Youngdong (8.15) and Sangju (6.91), atso ‘b’ value of dried persimmons was more yellow value in Youngdong (16.72) and Sangju (15.80). At the texture of dried persimmons, hardness was highest in Dongsang (6818.80) and lowest in Sangju (1221.20), fracturability was highest in Youngdong (5630.10) and lowest in Sangju (3.82), adhesiveness was highest in Youngdong (425.67), springiness and coke-siveness were highest in Haman (2.67) and Sangju (0.46), gumminess and chewiness were highest in Youngdong (4641.29 and 6060.68). In the microfloral states of dried persimmons, cell counts of bacteria was highest number in 3000 cfu/g at Dongsang, lactic acid bacteria was highest number in 2600 cfu/g at Dongsang, yeast was highest number in 1000 cfu/g at Youngdong, mold was highest number in 320 cfu/g at Dongsang. Sensory score of dried persimmons, color and sweetness were highest in Youngdong (3.91 and 4.55), lowest astringency in Sangju (1.91), highest texture in Sangju and Haman (3.36 and ,3.36), highest overall acceptance in Sangju (3.64).

• Korean journal of applied entomology
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• v.22 no.1 s.54
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• pp.1-6
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• 1983

The survey on the occurrence and distribution of barley stripe disease was conducted in the farmer's field of 19 gun (county) throughout Yeongmm area in May of 1982, in order to obtain a basic information on the breeding of resistant varieties, and for control of the disease. The percent of infected culms of barley stripe disease in Gyeongnam province (Southern Yeongnam) was higher $(13.7\%)$ them in Gyeong-bug $(6.9\%)$, northern Yeongnam, and especially, Ham-an, Milyang, Eui-chang and Weol-seong were severly occurred. The cultivar of Millyang 6 was slightly infected while the cultivars Olbori and Oweolbori were severely infected by the disease. Among soil conditions, the barley plant grown in the loam, clay and clay loam texture which have more availble moisture, and that of the plant cultivated in the poorly drained soils were shown to have severe infection. The barley plant grown in the soils in local valley $(18.8\%)$ where is frequently over saturated with water showed the more infection the barley plant grown in plains $(9.5\%)$. Generally, the poorer the soil drainage the more severeinfection occurred. Among cultivation conditions, the earlier the sowing dates of the barley, the less the percent of infected culms was observed. The heavier or lighter application of N fertilizer than the optimum to barley plant seemed to cause more infection.

• Economic and Environmental Geology
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• v.18 no.2
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• pp.107-124
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• 1985

More than fifty copper veins are emplaced around late Cretaceous granitoid stock in Haman-Gunbuk district, southernmost part of Korea. These veins cut both late Cretaceous granitoids and hornfels of Jindong formation which is intruded by the granitoids. The paragenesis of veins is nearly the same, consisting of (1) an early vein stage in which most iron oxide minerals, tourmaline and other silitcate minerals were deposited, (2) a calcite and quartz with base·metal sulfide stage and (3) late vein lets of barren calcite stage. Fluid inclusion studies reveal highly systematic trends of salinity and temperature during mineralization. Ore fluids of early vein stage were complex NaCl-KCl rich brines. Salinities of polyphase inclusions in quartz and scapolite in thie stage reached up to 72 wt.% and gradually decreased to 10.5wt. % in closing stage. Homogenization temperatures of inclusions in the beginning of this stage were up to $490^{\circ}C$ and then declined steadly to $290^{\circ}C$ in the late stage. Salinities of fluid inclusions in quartz and calcite of base·metal sulfide stage were 37.4~5.7wt. % and homogenization temperatures range from $373^{\circ}C$ to $170^{\circ}C$. Intermittent boiling of early vein fluid is indicated by fluid inclusions in quartz. Potassic alteration of granodiorite adjacent to early vein seems to be related to early saline vein fluid. Fluid inclusion data of base-metal sulfide stage of this area reveal nearly the same range as those of Koseong copper mining district about 30km apart from this area.

• Korean Journal of Fisheries and Aquatic Sciences
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• v.35 no.6
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• pp.589-594
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• 2002

Natural clonal stock of triploid crucian carp, Carassius aurahs was identified and its cytogenetic, molecular genetic and morphological traits were studied. Cytogenetic analysis of the clonal crucian carp revealed that they were natural triploidy, evidenced by 1.5-fold increases of cell size, DNA content, and chromosome number. Multi-locus DNA fingerprinting using $(GATA)_4$ probe showed that they had an identical fingerprint profile, indicating the clonal propagation of the population. External morphology and morphometric characteristics of triploid individuals were much uniform compared to those of diploids. Natural triploid crucian carp was proven to be all-female in this study.

• Proceedings of the Korea Water Resources Association Conference
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• 2019.05a
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• pp.261-261
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• 2019

최근 기후변화의 영향으로 인한 국지성 돌발호우 및 태풍 규모의 증가로 홍수에 의한 피해가 증가할 것으로 예상되는바 피해를 저감할 수 있는 대비책 마련과 피해의 정확한 분석을 위한 툴의 개발이 필수적이다. 이를 위하여 선진국에서는 하천과 연계된 홍수범람 해석모형인 HEC-RAS(USACE), Mike Flood(DHI) 등을 개발 및 배포하고 있는 반면에 국내에서 개발된 모형들은 연구목적으로 활용되는 수준에 그치고 있다. 따라서, 본 연구에서는 수공구조물의 운영을 고려한 1차원 하천흐름해석모형(K-RIVER) 및 제방 또는 댐으로부터의 범람모의를 수행할 수 있는 2차원 홍수범람해석모형(K-FLOOD)을 이용하여 하천으로부터의 홍수범람현상을 하천과 범람원 사이의 양방향 흐름을 고려하여 연계해석 할 수 있는 모형을 개발하였다. 개발된 모형을 경상남도 함안국 법수면 백산리에 위치하고 있는 벽산제를 대상으로 2002년 8월 6일 홍수사상에 의한 홍수범람현상의 재현을 통하여 적용성 검토를 수행하였다. 또한, 국내에서 주로 활용되고 있는 방법인 HEC-RAS와 FLUMEN을 이용한 결과 및 HEC-RAS 1D/2D연계모의결과와 비교를 통하여 결과의 적정성을 검토하였다. K-RIVER와 K-FLOOD를 연계모의한 결과는 HEC-RAS 1D/2D의 결과와 유사한 결과를 보였다. 그러나 HEC-RAS와 FLUMEN을 이용하는 경우 하천과 범람원의 수위에 따라 양방향으로 생성되는 흐름에 대한 모의가 불가능하여 하천의 수위저하시 범람원에서 하천으로의 유입을 고려할 수 없어 범람면적이 감소되는 현상을 모의할 수 없음에 따라 침수심 및 침수시간을 정확히 모의하는 것에는 한계가 있는 것으로 나타났다.

• Journal of the Korean Geophysical Society
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• v.4 no.1
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• pp.11-20
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• 2001

Seismic refraction and electrical resistivity surveys were conducted in Bangeosan Maaebul site located in Haman, Kyungnam, in order to present geophysical safety analysis method for masonry cultural properties. Seismic refraction exploration revealed that the ground was composed of three layers in term of seismic wave velocity; the upper, medium, and lower layers. The low velocity ranging from 308 to 366 m/sec in upper layer suggests weathered soil, the intermediate velocity from 1906 to 2090 m/sec in the medium layer indicates weathered rocks, and the high velocity from 5061 to 5650 m/sec in the lower layer implies extremely hard rocks. Our seismic result suggests that the upper and medium layer around the Maaebul should be reinforced to support the construct. The result of electric resistivity survey shows that there exists a low resistivity zone, ranging from 131 to 226 Ohm-m, at the right side of the Maaebul with the direction of NE-NNE. This area is the weakness zone as it plays role of the underground water passage in rainy season.

• Korean Journal of Soil Science and Fertilizer
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• v.43 no.5
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• pp.572-577
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• 2010

Field monitoring was performed to evaluate the soil chemical properties of 31 sweet persimmon orchard soil samples every two months from April to October in 2008 at Gyeongnam Province. Soil chemical properties such as pH, organic matter, available phosphate, exchangeable potassium, exchangeable calcium, exchangeable magnesium, exchangeable sodium, ammonium nitrogen, and nitrate nitrogen were analyzed. The soil chemical properties of both top soil, and subsoil showed that soil pH was significantly increased whereas ammonium nitrogen, and nitrate nitrogen were significantly decreased. The insufficient levels of nutrients in top soil, and subsoil were higher in 69.4%, and 84.7% for pH, 63.7%, and 84.7% for organic matter compared to optimum range. Meanwhile, the excessive levels of available phosphate showed 70.2% in top soil, and 46.8% in subsoil compared to optimum range. The experimental results showed that the optimum fertilization based on soil testing was the most important thing in soil nutrients management for sweet persimmon.