• 제목/요약/키워드: cold temperature dry

검색결과 166건 처리시간 0.027초

동결 온도에서 다짐효과에 관한 실험적 연구 (An Experimental Study on the Effectiveness of Soil Compaction at Below-Freezing Temperatures)

  • 황범식;채덕호;김영석;조완제
    • 한국지반환경공학회 논문집
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    • 제16권1호
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    • pp.37-43
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    • 2015
  • 우리나라는 사계절이 뚜렷하며 여름에는 고온다습한 무더운 날씨를 보이고 겨울에는 혹한의 날씨가 지속된다. 이러한 계절적 특성을 고려하여 국내 토공 분야에서는 많은 연구들이 있었으나 대부분의 연구가 지반의 동결 융해에 초점을 맞추어 이루어졌다. 이러한 연구들은 시공 당시의 기온에 따른 지반특성을 반영하지 못하였으며 상온에서 다져진 지반을 대상으로 실시되었다. 그러나 동절기 다짐의 경우 상온에서의 다짐과는 다른 지반상태를 나타낼 것으로 예상되며, 그에 따른 동결 융해로 인한 강도 및 변형 특성 또한 다르게 나타날 것으로 판단되나 이를 고려한 연구는 아직까지 전무한 상황이다. 따라서 본 연구에서는 $-3^{\circ}C$$-8^{\circ}C$에서 주문진 표준사에 카올리나이트를 0%, 5%, 10%, 15%의 중량비로 혼합하여 다짐시험을 실시하였으며, 상온($18^{\circ}C$)에서의 다짐곡선과 비교하여 온도 및 세립분 함량에 따른 다짐 효과를 살펴보았다. 시험 결과, 동결 온도에서 다짐 시 최대건조단위중량이 감소하는 경향을 보였으며, $-8^{\circ}C$ 이하에서 다짐 시공 시 시방서의 다짐기준을 만족하지 못하는 것으로 나타났다.

북서태평양에서 난수성(Pleuromamma sp.)과 냉수성(Neocalanus plumchrus) 요각류의 지방 함량 및 구성 분석을 통한 생리/생태 비교 (The Physiological and Ecological Comparisons between Warm (Pleuromamma sp.) and Cold Water Copepod Species (Neocalanus plumchrus) in the Northwestern Pacific Ocean Using Lipid Contents and Compositions)

  • 고아라;주세종;이창래
    • Ocean and Polar Research
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    • 제31권1호
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    • pp.121-131
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    • 2009
  • In an effort to better understand the physiological and ecological differences between warm and cold water copepod species in Korean waters using lipid contents and compositions, two species of copepods (Pleuromamma sp. as a warm water species and Neocalanus plumchrus as a cold water species) were collected from the Northwest Pacific and East Sea/Sea of Japan, respectively. The cold water species showed two fold higher lipid contents than the warm water species (11% vs. 5% of dry weight). Wax esters, known as one of the major storage lipid classes, were found to be the dominant lipid class (accounting for 64% of total lipids) in the cold water species, whereas, in the warm water species, phospholipids, which are known as membrane components, were the dominant lipid class (accounting for 43% of total lipids),with a trace amount of the storage lipids as a form of triacylglycerols (${\leq}1%$ of total lipids). With regard to the fatty acid compositions, saturated fatty acids (SAFA), especially 16:0 (about 30% of total fatty acids), were most abundant in the warm water species, whereas the polyunsaturated fatty acids (PUFA), particularly eicosapentaenoic acid (EPA : 20:5(n-3)) (${\geq}16%$ of total fatty acids), were most abundant in the cold water species. Among the neutral fraction of lipids, phytol, originating from the side chain of chlorophyll and indicative of active feeding on phytoplankton, was detected only in the warm water species. Significant quantities of fatty alcohols were detected in cold water species, particularly long-chain monounsaturated fatty alcohols (i.e. 20:1(n-9) and 22:1(n-11)), which are well known to abound in cold water herbivorous copepods. However, only trace amounts of short-chain fatty alcohols were detected in the warm water species. Twelve different kinds of sterols were detected in these copepod species, with cholest-5-en-$3{\beta}$-ol (cholesterol) and cholesta-5, 24-dien-$3{\beta}$-ol (desmosterol) dominating in cold and warm water species, respectively. In addition, for the warm water species (Pleuromamma sp.), we assessed the latitudinal gradients of lipid contents and compositions using samples from three different latitudinal regions (Philippine EEZ, Japan EEZ, and the East China Sea). Although no latitudinal gradients of lipid contents were detected, the lipid compositions, particularly dietary fatty acid markers, varied significantly with the latitude. The findings of this study confirm that the distribution of lipid contents and compositions in copepods may not only indicate their nutritional condition and diet history, but may also provide insights into their living strategies under different environmental conditions (i.e., water temperature, food availability).

영하에서의 다짐에너지에 따른 다짐 효과 평가 (Evaluations on the Compaction Energy Effects on the Soil Compaction at Sub-Zero Temperature)

  • 이정협;황범식;채덕호;조완제
    • 한국지반환경공학회 논문집
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    • 제16권8호
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    • pp.13-20
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    • 2015
  • 인구가 증가하고 자원이 고갈되면서 새로운 자원개발을 위한 대안으로 극한지 개발이 떠오르고 있다. 전 세계 육지 면적 중 14%가 극한지 지역에 해당되며, 이 지역들의 개발을 위한 해외극지 건설시장이 많이 확대되었다. 이미 선진국들은 극한지 연구의 필요성을 인식하고 기술 개발에 많은 투자를 하고 있는 반면, 우리나라의 경우 극한지 개발을 위한 기술이 선진국에 비해 매우 낮으며 관련 연구 또한 미약한 실정이다. 국내의 동절기 시공의 경우 지반동결에 의한 강도 및 변형특성에 대한 명확한 기준이 마련되어있지 않으며 현장에서의 간단한 지침을 통해서만 관리되고 있다. 따라서 본 연구에서는 상온($18^{\circ}C$), $-3^{\circ}C$, $-8^{\circ}C$에서 세립분 함량을 0%, 5%, 10%, 15%로 변화하면서 D 다짐 시험을 실시하여 영하온도에서의 다짐특성에 대해 살펴보았으며, 기존의 문헌연구와 비교를 통해 영하온도에서의 다짐에너지에 따른 다짐 효과에 대해 평가하였다. 시험 결과 영하온도에서 다짐에너지가 클수록 최대건조단위중량은 증가하는 것으로 나타났으며, $-3^{\circ}C$에서의 D다짐 시험결과는 상온의 결과와 크게 다르지 않으나 $-8^{\circ}C$ 이하에서의 다짐시공 시 다짐성능의 저하가 상당한 것으로 나타났다.

Climate Change Impacts in Natural Resources and Livestock in Mongolia Climate

  • Batima, P.;Natsagdorj, L.;Bayarbaatar, L..;Bolortsetseg, B.;Natsagsuren, N.;Erdenetsetseg, B.
    • 한국제4기학회지
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    • 제18권2호통권23호
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    • pp.103-104
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    • 2004
  • This paper discuss some results of observed changes of meteorological elements as temperature, precipitation and some extreme indexes in Mongolia. Mongolia is one of the largest landlocked countries in the world. The climate is characterized by a long lasting cold winter, dry and hot summer, low precipitation, high temperature fluctuation and relatively high number of sunny days per year. During last 60 years the annual mean air temperature has risen $1.66^{\circ}C$. Intensive warming of > $2^{\circ}C$ was observed at higher altitudes of high mountains when warming of < $1^{\circ}C$ was observed the Domod steppe and the Gobi Desert. Heat Wave Duration have statistically significant risen trend with increaded number of days by 8-18 at significance level of 95-99.9% depending on geography and Cold Wave Duration have shortened by 13.3 days significance level of 95-99%. In general, by the amount of precipitation, Mongolia falls in semi-arid and arid region. It is 300-350 mm in the high mountain regions while it is only 50-150 mm in Gobi Desert regions. The changes of annual precipitation have very localized character i.e.decreasing at one site and increasing at a sit nearby. Annual precipitation decreased by 30-90 mm in the northern-central region and increased by 2-60 mm in the western and eastern region. The magnitude of alteration changes in precipitation regardless increasing or decreasing is 5-25%. A trends, significant at the level of 90%, found where changes are more than 40 mm or more than 15% of annual mean value. Moreover, the soil moisture resources was decreased in the last 40 years. Specially, moisture contents of the top soil have decreased 2 times(N. Natsagsuren, 2002). Months of June and July in Mongolia is the year that moisture is not inhibiting vegetation growth. Unfortunately, its also found that moisture in this time tends to decrease. Increased temperature, decreased precipitation and soil moisture are most likely resulted in occurences of more intense drought spells that have taken place during the recent years. Intimately, these changes have considerable impact on livestock in Mongolia.

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극한 기후변수가 농업에 미친 경제적 효과 추정 -강원도의 사례- (Estimating the Economic Impacts of Extreme Climate Events on Agriculture: the Case of Gangwon-do)

  • 정준호;이승호
    • 대한지리학회지
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    • 제47권3호
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    • pp.459-470
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    • 2012
  • 본 연구는 강원도 농업을 사례로 1993-2010년 기간 동안 11개 시군별 기후, 지리 및 토양, 사회 경제적 변수들에 대한 패널자료를 구축하고 리카디언 방법을 사용하여 극한기후 변수들이 논과 밭 경작유형별로 토지가치에 미친 경제적 효과를 추정하고자 시도한다. 추정결과에 따르면, 호우 관련 극한기후 변수는 논과 밭의 토지가치와 부정적인 관계가 있다. 여름철 관련 극한기온 변수들은 토지가치에 음(-)의 영향을 미치고 있지만, 한파를 제외한 겨울철 관련 극한기온 변수들은 토지가치와 정(+)의 관계를 보여주고 있다.

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수도작의 미기상과 생산성 (Microclimate and Rice Production)

  • Uchijima, Zenbei
    • 한국작물학회지
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    • 제27권4호
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    • pp.314-339
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    • 1982
  • Fluctuating climate is still most important environmental constrain, although improved modem agricultural technology has succeeded to increase crop production in the world. To stabilize the food production under fluctuating weather conditions, it is very needed to obain the quantitative information of interactions between crops and climate. The main purpose of this paper is three hold. Using the JIBP-data, the dry matter accumulation of rice crops is studied in relation to weather indexes (\SigmaTa and \SigmaSt). Temperature dependence of the yield index of rice is analyzed as to air temperature and water temperature. \SigmaT$_{10}$ -fluctuations are studied using meteorological data at various stations. The possible shift of \SigmaT$_{10}$ -isopleths due to climate fluctuation is evaluated. The second interest is in the plant climate of rice crops. Using results of canopy photosynthesis, it is pointed that the canopy structure has most important implication in plant climate. Leaf-air, stomatal, and mesophyll resistances of rice crops are described in relation to weather conditions. The change in light condition and aerodynamical property of rice crops with the growth is illustrated. The energy partition is also studied at different growing stages. Third point is to show in more detail effective countermeasures against cold irrigation water and cool summer. Heat balance of warming pond and polyethylene tube as a heat exchanger is studied to make nomo-grams for evaluating the necessary area and necessary length. Effects of windbreak net on rice crops are illustrated by using experimental and simulation results.lts.

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Effect of Salicylic Acid on Growth and Chilling Tolerance of Cucumber Seedlings

  • Lee, Gui-Soon;Hong, Jung-Hee
    • 한국환경과학회지
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    • 제11권11호
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    • pp.1173-1181
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    • 2002
  • The present study was undertaken to investigate the effect of low temperature and salicylic acid(SA) on the chilling tolerance of acclimated and nonacclimated cucumber(Cucurmis sativus L.) seedlings. The acclimation phenomenon was characterized in chilling-sensitive cucumber seedlings and found to have a significant effect on the survival and shoot dry weights. The injuries experienced by the acclimated seedlings in the third leaf stage were on average smaller by half than those experienced by the nonacclimated seedlings. Chilling also caused a large increase in the free proline levels, regardless of the acclimation status. Exogenous treatment with SA(0.5mM) resulted in improved growth and survival of the nonacclimated chilled seedlings, indicating that SA induced chilling tolerance and SA and acclimation had common effects. The application of cycloheximide in the presence of SA restored the acclimation-induced chilling tolerance. The elevated proline level observed in the cold-treated and SA-treated plants was more pronounced in the light than in the dark at a chilled temperature, indicating that endogenous proline may play a role in chilling tolerance by stabilizing the water status in response to chilling. From these results it is suggested that SA provided protection against low-temperature stress by increasing the proline accumulation, and pre-treatment with SA may induce antioxidant enzymes leading to increased chilling tolerance.

Changed Relationship between Snowfall over the Yeongdong region of the Korean Peninsula and Large-scale Factors

  • Cho, Keon-Hee;Chang, Eun-Chul
    • 한국지구과학회지
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    • 제38권3호
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    • pp.182-193
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    • 2017
  • A typical snowfall pattern occurs over the east coastal region of the Korean Peninsula, known as the Yeongdong region. The precipitation over the Yeongdong region is influenced by the cold and dry northeasterly wind which advects over warm and moist sea surface of the East Sea of Korea. This study reveals the influence of large-scale factors, affecting local to remote areas, on the mesoscale snowfall system over the Yeongdong region. The National Centers for Environmental Prediction-Department of Energy reanalysis dataset, Extended Reconstructed sea surface temperature, and observed snowfall data are analyzed to reveal the relationship between February snowfall and large-scale factors from 1981 to 2014. The Yeongdong snowfall is associated with the sea level pressure patterns over the Gaema Plateau and North Pacific near the Bering Sea, which is remotely associated to the sea surface temperature (SST) variability over the North Pacific. It is presented that the relationship between the Yeongdong snowfall and large-scale factors is strengthened after 1999 when the central north Pacific has warm anomalous SST. These enhanced relationships explain the atmospheric patterns of recent strong snowfall years (2010, 2011, and 2014). It is suggested that the newly defined index in this study based on related SST variability can be used for a seasonal predictor of the Yeongdong snowfall with 2-month leading.

냉각탑 성능 예측을 위한 프로그램 개발 (Program Development for the Prediction of Cooling Tower Performance)

  • 정재형;정재현;최영기
    • 설비공학논문집
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    • 제26권3호
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    • pp.130-136
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    • 2014
  • The present study is performed to set up the framework of cooling tower performance predictions. The performance of mechanical forced draft cooling tower is directly related to the state of a nuclear power plant system, such as the condenser and evaporator. The main parameters related to the state of systems are as follows : wet bulb temperature, dry bulb temperature and absolute humidity. The performance evaluation of cooling tower must be considered at the power plant design. In this study, the toolkit developed by the American Cooling Tower Industry association (CTI) has been used for the framework construction. In order to validate the framework, it is being applied to the cooling tower constructed for the U.S. Nuclear Power Plant. The test results have shown good agreements with the cold water temperature on the cooling tower performance curves provided by manufacturers.

하계 동중국해 북부 해역에서 저층 냉수괴의 거동 (Movement of Cold Water Mass in the Northern East China Sea in Summer)

  • 장성태;이재학;김철호;장찬주;장영석
    • 한국해양학회지:바다
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    • 제16권1호
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    • pp.1-13
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    • 2011
  • 황해저층냉수는 지난 동계의 차고 건조한 바람에 의해 생성되어, 하계에 황해 중앙골을 따라 남하하는 것으로 알려져 있다. 동중국해 북부해역에서 황해저층냉수의 특성과 거동을 파악하기 위해 2003년부터 2009년까지 하계에 관측한 자료를 분석하였다. 수괴분석을 통해 본 연구해역에 영향을 미치는 황해저층냉수를 새롭게 정의하여 북서저층냉수라고 명명하였고, 수온 $13.2^{\circ}C$ 이하, 염분 32.6~33.7 psu와 밀도 $24.7{\sim}25.5\;{\sigma}_t$로 특성지었다. 지형류 계산에 의해 연구해역에서 북서저층냉수는 약 2 cm/s 이하의 속도로 남하하는 것으로 추정하였다. 정의한 북서저층냉수는 수온의 범위와 자지하고 있는 영역에서 연간 변동을 보이며, 이러한 변동은 이전 해 동계 황동중국해의 표층수온의 변화와 밀접한 관련이 있었고, 동계 표층수온의 변화는 동계 기온에 의한 영향이 지배적임을 확인하였다. 동계 동중국해 표층수온은 북극진동 지수와 높은 상관성을 보이며, 동계의 북극진동이 음일 때 동중국해 표층수온이 하강하였고, 이러한 영향으로 북서저층냉수 세력이 동중국해 북부 해역까지 저수온을 보이면서 확장하였다. 동 연구는 동계의 북극진동지수, 황동중국해 겨울철 표층수온, 동중국해 북부의 북서저층냉수가 역학적으로 관련이 있음을 보였고, 이를 바탕으로 하계 동중국해 북부해역에서 저층냉수의 거동을 유추할 수 있을 것으로 사료된다.