• Title/Summary/Keyword: river-table

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Protective Effect of BOEC Co-Culture System against Nitric Oxide on Development of Bovine IVM/IVF Embryos

  • Jang, Hyun-Yong;Jung, Yu-Sung;Li, Zheng-Yi;Yoon, Hyoung-Jong;Cheong, Hee-Tae;Kim, Jong-Taek;Park, Choon-Keun;Yang, Boo-Keun
    • Reproductive and Developmental Biology
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    • v.32 no.3
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    • pp.167-173
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    • 2008
  • Somatic cells such as oviduct epithelial cell, uterine epithelial cell, cumulus-granulosa cell and buffalo rat river cell has been used to establish an effective culture system for bovine embryos produced in in vitro. But nitric oxide (NO) metabolites secreted from somatic cells were largely arrested the development of bovine in vitro matured/ in vitro fertilized (IVM/IVF) embryos, suggesting that NO was induced the embryonic toxic substance into culture medium. The objective of this study was to investigate whether BOEC co-culture system can ameliorate the NO-mediated oxidative stress in the culture of bovine IVM/IVF embryos. Therefore, we evaluated the developmental rate of bovine IVM/IVF embryos under BOEC co-culture system in the presence or absence of sodium nitroprusside (SNP), as a NO donor, and also detected the expression of growth factor (TGF-$\beta$, EGF and IGFBP) and apoptosis (Caspase-3, Bax and Bcl-2) genes. The supplement of SNP over 5 uM was strongly inhibited blastocyst development of bovine IVM/IVF embryos than in control and 1 uM SNP group (Table 2). The developmental rates beyond morulae stages of bovine IVM/IVF embryos co-cultured with BOEC regardless of SNP supplement (40.4% in 5 uM SNP+ BOEC group and 65.1% in BOEC group) were significantly increased than those of control (35.0%) and SNP single treatment group (23.3%, p<0.05: Table 3). The transcripts of Bax and Caspase-3 genes were detected in all experiment groups (1:Isolated fresh cell (IFC), 2:Primary culture cell (PCC), 3:PCC after using the embryo culture, 4: PCC containing 5 uM SNP and 5: PCC containing 5 uM SNP after using the embryo culture), but Bcl-2 gene was not detected in IFC and PCC (Fig. 1). In the expression of growth factor genes, TGF-$\beta$ gene was found in all experimental groups, and EGF and IGFBP genes were not found in IFC and PCC (Fig. 2). These results indicate that BOEC co-culture system can increase the development beyond morula stages of bovine IVM/IVF embryos, possibly suggesting the alleviation of embryonic toxic substance like nitric oxide.

Method of Estimating Groundwater Recharge with Spatial-Temporal Variability (시공간적 변동성을 고려한 지하수 함양량의 추정 방안)

  • Kim, Nam-Won;Chung, Il-Moon;Won, Yoo-Seung
    • Journal of Korea Water Resources Association
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    • v.38 no.7 s.156
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    • pp.517-526
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    • 2005
  • In Korea, the methods of estimating groundwater recharge can categorized into two groups. One is baseflow separation method by means of groundurater recession curve, the other is water level fluctuation method by using the data from groundwater monitoring wells. Baseflow separation method is based on annual recharge and lumped concept, and water-table fluctuation method is largely dependent on monitoring wells rather than water budget in watershed. However, groundwater recharge rate shows the spatial-temporal variability due to climatic condition, land use and hydrogeological heterogeneity, these methods have various limits to deal with these characteristics. For this purpose, the method of estimating daily recharge rate with spatial variability based on distributed rainfall-runoff model is suggested in this study. Instead of representative recharge rate of large watershed, the subdivided recharge rate with heterogeneous characteristics can be computed in daily base. The estimated daily recharge rate is an advanced quantity reflecting the heterogeneity of hydrogeology, climatic condition, land use as well as physical behaviour of water in soil layers. Therefore, the newly suggested method could be expected to enhance existing methods.

Floating Photovoltaic Plant Location Analysis using GIS (GIS를 활용한 수상 태양광 발전소 입지 분석)

  • Lee, Ki Rim;Lee, Won Hee
    • Journal of Korean Society for Geospatial Information Science
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    • v.24 no.1
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    • pp.51-59
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    • 2016
  • Global consumption of fossil fuels continues to increase. As developing countries use fossil fuel as much as the existing fossil fuel using countries, the total amount of fossil fuel consumed has risen. The finite fossil energy depletion insecurity have become serious. In addition, fossil energy is caused by environmental pollution, economic and social problems remain in assignments that need to be addressed. Although solar power is clean and has many benefits, there are several problems in the process of installing a solar power plant. To solve these problems, floating photovoltaic plants has emerged as an alternative. This floating photovoltaic plants location analysis has not been made yet. In this study, the conditions of the floating photovoltaic plants location is analyzed with the Analytic Hierarchy Process using the terrain and climate factors. The score is assigned to the attribute information of each factor by the classification table. After multiplied by the weight the result is analyzed by visualization of the score. As the result, the score of the northen part of Gyeongsangbuk-do province is higher than the southern part of Gyeongsangbuk-do province. Especially Andongho lake in Andong City and the reservoir in Yeongyang-Gun are extracted as the optimal location. The score of the river boundary is low not the center of the river stream. It is expected that this study would be a more accurate floating solar power plant location analysis.

The Estimation of Groundwater Recharge with Spatial-Temporal Variability at the Musimcheon Catchment (시공간적 변동성을 고려한 무심천 유역의 지하수 함양량 추정)

  • Kim Nam-Won;Chung Il-Moon;Won Yoo-Seung;Lee Jeong-Woo;Lee Byung-Ju
    • Journal of Soil and Groundwater Environment
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    • v.11 no.5
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    • pp.9-19
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    • 2006
  • The accurate estimation of groundwater recharge is important for the proper management of groundwater systems. The widely used techniques of groundwater recharge estimation include water table fluctuation method, baseflow separation method, and annual water balance method. However, these methods can not represent the temporal-spatial variability of recharge resulting from climatic condition, land use, soil storage and hydrogeological heterogeneity because the methods are all based on the lumped concept and local scale problems. Therefore, the objective of this paper is to present an effective method for estimating groundwater recharge with spatial-temporal variability using the SWAT model which can represent the heterogeneity of the watershed. The SWAT model can simulate daily surface runoff, evapotranspiration, soil storage, recharge, and groundwater flow within the watershed. The model was applied to the Musimcheon watershed located in the upstream of Mihocheon watershed. Hydrological components were determined during the period from 2001 to 2004, and the validity of the results was tested by comparing the estimated runoff with the observed runoff at the outlet of the catchment. The results of temporal and spatial variations of groundwater recharge were presented here. This study suggests that variations in recharge can be significantly affected by subbasin slope as well as land use.

Evaluating Village-based Resources for Conserving Nakdong-Jeongmaek (낙동정맥 보전을 위한 마을기반 자원평가)

  • Kim, Tae-Su;Hwang, Shin-Hee;Cho, Ki Hwan;Kim, Su-Jin;Jang, Gab-Sue
    • Journal of the Korean Society of Environmental Restoration Technology
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    • v.23 no.4
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    • pp.47-58
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    • 2020
  • This study was done to evaluate resources distributed around the Nakdong-Jeongmaek which is the eastern ridge line of the Nakdong-river basin with 437km in length. Here we found and/or searched for thousands of resources within each of 210 villages around the ridge, which were divided into six categories including landscape, natural park, protected area, history, tourism and biodiversity. An inventory was also created using an attribute table in a shape file for identifying the spatial location and property for every resource existing in each village. Each of fields for six-typed resources has 210 records representing each village and resources within it. If a resource exists in a village, '1' is assigned for its existence in its corresponding record. Otherwise, '0' is assigned for its non-existence in the record. The number of '1' on six records for a village is meaning the number of resources contained within a village, which can be a barometer to decide the properties of each village. In this study, we found five core villages containing all kind of resources in it, while 52 villages were found having only a single type of resources within it. The other villages were known to have multiple resources like having two or more ones.

Analysis of Groundwater Recharge Change using Water Table Fluctuation Method by Subbasins in Geum, Yeongsan, Seomjin River Watersheds (지하수위 변동법을 활용한 금강 및 영산·섬진강 권역 표준유역 별 지하수 함양량 변동 분석)

  • Jae Beom Lee;Jeong-Seok Yang;Amos Agossou;Yeong Jin Jeong;Min Seong Ha
    • Proceedings of the Korea Water Resources Association Conference
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    • 2023.05a
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    • pp.377-377
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    • 2023
  • 기후변화로 인한 국내 수문기상 환경의 변화는 기존의 강수 패턴의 변화를 야기하고, 이는 수문학적 측면에서 유역 내 지하수 함양량의 변화를 야기할 수 있다. 상시 취수가 가능한 대규모 하천 인근 지역 외의 지역은 가용 수량의 확보를 위하여 생·농·공 용수 확보를 위하여 지하수를 적극적으로 이용하고 있다. 유역의 수자원 관리를 위하여 하천, 저수지, 댐 등으로 대표되는 지표수자원의 관리와 함께 지하수자원 관리의 중요성이 대두되고 있다. 지하수자원의 관리를 위해서는 기존 지하수 이용시설의 지하수 이용량에 대한 정확한 정보를 수집하는 것이 중요하지만 지하수 함양량을 정량적으로 평가하는 것 또한 매우 중요하다. 지하수 함양량을 산정하기 위한 방법으로는 물수지 분석, MIKE, SWAT 등 모형을 이용한 분석 등 다양한 평가 방법이 있으나 유역의 지하수 함양에 영향을 줄수 있는 수문환경에 대한 정확한 정보가 있어야 하기 때문에 권역 내 표준유역 전반에 대한 지하수 함양량을 산정하기 어려운 단점이 있다. 본 연구에서는 지하수위 관측자료와 강수량 관측자료를 이용한 지하수위 변동법을 적용하여 표준유역 별 지하수 함양량을 산정하였다. 최근 5년간의 자료를 이용하여 표준유역 별 지하수 함양량 산정 결과를 제안함으로써 표준유역 단위 수자원 관리에 기여하고자 하였다. 본 연구 결과는 표준 유역 별 가뭄 대응 방안을 도출하는데 기초 자료로써 활용 될 수 있을 것으로 기대된다

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Temporal-Spatial Location of Dwelling Site in Asan Bay in the Neolithic Age (아산만지역(牙山灣地域) 신석기시대(新石器時代) 집자리의 시공적(時空的) 위치(位置))

  • Koo, Ja Jin
    • Korean Journal of Heritage: History & Science
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    • v.42 no.3
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    • pp.26-47
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    • 2009
  • This study examined dwelling site from among the sites of the Neolithic age found in the Asan Bay(牙山灣) area, and the temporal-spatial location and meaning of the dwelling site (settlement). The majority of the settlements in the area are of a square style but some coexist with rectangular-style settlements, which is noteworthy. The dwelling sites of the Neolithic age found in Asan Bay area are mostly located in a ridge of hilly areas, divided into gentle, low areas (20~50 meters above sea level) and relatively high areas (50~80 meters above the sea level). Although location strongly corresponded to the residents' subsistence and the technical levels within the culture, it likely was greatly affected by natural environment where they lived, as well. In examining radiocarbon dating results and the excavated artifacts, the settlements found in Asan Bay were determined to belong to the period II(3,500~3,000 B.C.) stated in the Relative Chronological table of Dwelling sites in the Neolithic age, written by the author. Said Dwelling sites are proven to have a close relationship with those found on the coast of Gyeonggi Province(京畿道) and in the Geum River(錦江) valley. This is deemed to be the result of expansion and interchange between Gyeonggi Province(京畿道) group and Geum River(錦江) valley group, who constituted the large settlements. Additionally, the Daecheon-ri type dwelling sites in the Geum River valley were verified to be the result of exchange, and spread to the Asan Bay area in the same era. Two forms of Dwelling sites coexisted dynamically in the Asan Bay area around 3,500 B.C. Such a phenomenon resulted primarily from the expansion of the dwelling site due to the introduction of primitive agriculture, as well as environmental (temperature), biological and social changes at those times.

Numerical Modeling of Water Transfer among Precipitation, Surface Water, Soil Moisture and Groundwater

  • Chen, Xi;Zhang, Zhicai;Chen, Yongqin
    • Proceedings of the Korea Water Resources Association Conference
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    • 2006.05a
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    • pp.2-11
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    • 2006
  • In the processes of hydrological cycle, when precipitation reaches the ground surface, water may become surface runoff or infiltrate into soil and then possibly further percolate into groundwater aquifer. A part of the water is returned to the atmosphere through evaporation and transpiration. Soil moisture dynamics driven climate fluctuations plays a key role in the simulation of water transfer among ground surface, unsaturated zone and aquifer. In this study, a one-layer canopy and a four-layer soil representation is used for a coupled soil-vegetation modeling scheme. A non-zero hydraulic diffusivity between the deepest soil layer modeled and groundwater table is used to couple the numerical equations of soil moisture and groundwater dynamics. Simulation of runoff generation is based on the mechanism of both infiltration excess overland flow and saturation overland flow nested in a numerical model of soil moisture dynamics. Thus, a comprehensive hydrological model integrating canopy, soil zone and aquifer has been developed to evaluate water resources in the plain region of Huaihe River basin in East China and simulate water transfer among precipitation, surface water, soil moisture and groundwater. The newly developed model is capable of calculating hydrological components of surface runoff, evapotranpiration from soil and aquifer, and groundwater recharge from precipitation and discharge into rivers. Regional parameterization is made by using two approaches. One is to determine most parameters representing specific physical values on the basis of characterization of soil properties in unsaturated zone and aquifer, and vegetations. The other is to calibrate the remaining few parameters on the basis of comparison between measured and simulated streamflow and groundwater tables. The integrated modeling system was successfully used in the Linhuanji catchment of Huaihe plain region. Study results demonstrate that (1) on the average 14.2% of precipitation becomes surface runoff and baseflow during a ten-year period from 1986 to 1995 and this figure fluctuates between only 3.0% in drought years of 1986, 1988, 1993 and 1994 to 24.0% in wet year of 1991; (2) groundwater directly deriving from precipitation recharge is about 15.0% t of the precipitation amount, and (3) about half of the groundwater recharge flows into rivers and loses through evaporation.

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Spatial Characteristics of Vegetation Development and Groundwater Level in Sand Dunes on a Natural Beach (해안사구의 지하수위와 식생 발달의 공간적 특성 연구)

  • Park, JungHyun;Yoon, Han-sam;Jeon, Yong-Ho
    • Journal of the Korean Society for Marine Environment & Energy
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    • v.19 no.3
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    • pp.218-226
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    • 2016
  • Field observations were used to study the characteristics and influence of groundwater level fluctuations on vegetation development on the natural beach of a sandy barrier island, in the Nakdong River estuary. The spatial/temporal fluctuations of the groundwater level and the interactions with the external forces (weather, ocean wave and tide) were analyzed. The results indicated that when it rains the groundwater level rises. During summer, when precipitation intensity is greater than 20 mm/hour, it rose rapidly over 20 cm. Subsequently, it fell gradually during periods of no precipitation. Seasonal characteristics indicated that the groundwater level was high during the summer rainy season and tended to fall in the winter dry season. The time-averaged groundwater level, observed from the four observations over 3 years (2012-2014), was about 1.47 m, higher than mean sea level (M.S.L.). It was shown that the average annual groundwater level rises toward the land rather than showing intertidal patterns observation. Differences in the presence or absence of a coastal sand dunes affected the progress of vegetation. In other words, in environments of saltwater intrusion where the groundwater level varies, dependent on the distance from the shoreline and bottom slope, sand dunes can be provided to affect soil conditions and groundwater, so that vegetation can be grown reliably.

Adina rubella Phytocoena in Jeju Island, Korea (제주도 하천의 중대가리나무 식생)

  • Choi, Byoung-Ki;Ryu, Tae-Bok;Kim, Jong-Won
    • Korean Journal of Ecology and Environment
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    • v.48 no.1
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    • pp.68-76
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    • 2015
  • There is no willow riparian vegetation in Jeju Island, Korea. Instead, a genetically-isolated population of Adina rubella is found in some parts of the riparian system. We describe its syntaxonomy and synecology. A total of 27 phytosociological relev$\acute{e}$s were collected, 11 relev$\acute{e}$s from 91 sites and 16 relev$\acute{e}$s from the previously published relevant materials. Data were analyzed by traditional Braun-Blanquet method and multivariate PCoA (Principal coordinates analysis). New syntaxa are distinguished, Adinion rubellae all. nov. and its type association Tripogono-Adinetum rubellae ass. nov. with two subassociations, typicum and rhododendretosum poukhanensae. Adino-Rhododendretum poukhanensae Itow et al. 1993 was discarded owing to mismatch of syntaxonomy and syngeography of Adina and Rhododendron phytocoena. The alliance Adinion is Jeju's regional and partly ombrotrophic vegetation occurring in pothole and rock crevice where are independent on ground-water table. We also suggest a revised alliance, Rhododendrion poukhanensae Lee 2004 ex. hoc loco in Korean peninsula, as a corresponding syntaxon to Adinion, which completely differs from Phragmito-Salicion. Finally we pointed out that Adina phytocoena requiring an absolutely monitoring has been threatened by river maintenance project of local government.