• Korean Journal of Plant Resources
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• v.15 no.1
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• pp.18-25
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• 2002

These experiments were conducted to evaluate the variability of seed germination, and seedling growth of PEG priming barley. The average germination percentage(AGP) of PEG priming seed was higher than control, but those were low with extend the treatment period. The AGP of washing seed after PEG priming was higher than unwashed seed, and that of redried seed after priming was lower than control. The germination time of priming seed was short compare to control seed, and that was prolonged with extend the priming period, and that of washing seed after priming was shortening, and that of redried seed after priming was prolonging. The emergence percentage(EP) of priming seed was higher than control, and the emergence time was shortest in 50％ field moisture capacity soil. The seedling and root length of priming seed was shorter than control.

• Proceedings of the Korea Water Resources Association Conference
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• 2021.06a
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• pp.353-353
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• 2021

메가가뭄으로 인한 적응전략 수립은 국민의 물 안보 및 수자원 재해에 대한 안전 증대에 매우 중요한 핵심기술임에도 불구하고 메가가뭄의 정량적인 평가지표는 개발 중인 상황이다. 본 연구에서는 국내/외 메가가뭄 분석 및 영향평가 관련 선행연구사례를 분석하여 메가가뭄 확산 단계별 평가지표를 도출하고자 하였다. 메가가뭄을 평가하기 위해 선행연구에서는 이상 강수량과 이상기온을 함께 고려하는 방법을 지속적으로 제안해 왔다. 이상 강수량은 기상학적 가뭄과 토양수분의 저하, 수문학적 가뭄, 사회경제적 영향에 이르기까지 가뭄을 평가할 수 있는 지표로써 활용할 수 있으며, 이상 기온은 폭염 등 기온 상승으로 인한 증발산량의 증가로 토양수분 저하와 저수량 감소 등의 영향을 평가할 수 있는 지표이다. 본 연구에서는 메가가뭄의 확산을 4단계로 구분하고 확산단계별 평가지표를 개발하였다. 또한 가뭄유형을 기상, 농업, 수문, 사회경제적 가뭄으로 구분하여 메가가뭄의 발생 단계와 그에 따른 가뭄의 확산 분야별 영향 분석을 수행하도록 제시하였다. 가뭄단계는 메가가뭄의 징후기, 진입기, 확산기, 지속적인 메가가뭄으로 인한 국가적 위기 4단계로 구분하였다. 메가가뭄은 1년 주기의 분석이 아닌 Carry over되는 연속적인 사상임에 따라 본 연구에서는 메가가뭄의 단계를 각각 2년, 3년, 4년 연속적으로 지속하였을 때로 구분하였으며, 이에 따른 기상, 농업, 수문, 사회경제적 평가지표를 제시하였다. 기상학적 메가가뭄 평가지표는 누적강수량을 이용한 강수량 부족으로 인한 가뭄, 이상기온(폭염)으로 인한 폭염으로 구분하였다. 농업적 메가가뭄 평가지표는 농업용수를 공급하는 농업용 저수지와 밭작물 생육에 영향을 미치는 토양수분에 관련한 평가항목을 이용하였으며, 수문학적 메가가뭄 평가지표는 다목적댐의 저수율과 하천 갈수량을 이용한 하천건천화 지수를 이용한 평가지표를 제시하였다. 사회경제적 메가가뭄 평가지표는 국민이 실제로 체감할 수 있는 지표로써 농작물 가격과 생·공용수의 제한급수 발생 현황을 이용한 평가가 가능하도록 제시하였다.

• Korean Journal of Soil Science and Fertilizer
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• v.39 no.5
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• pp.253-258
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• 2006

An empirical model of nitrous oxide emission from agricultural soil has been applied. It is based on the relationship between $N_2O$ and three soil parameters, soil mineral N(ammonium plus nitrate) content in the topsoil(0-15cm), soil water-field pore space, and soil temperature, determined in a study on clay loam and sandy loam at the pepper field in 2004. For comparisons between estimated and observed values of $N_2O$ emissions in the pepper field, it was investigated that $N_2O$ amount in the clay loam and sandy loam were overestimated as 12.2% and less estimated as 30%, respectively. However, $N_2O$ emissions were overestimated as 27.1% in the clay loam and 14.7% in the sandy loam from $N_2O$ gas samples collected once a week at the same time analyzing soil parameters. This modelling approach, based as it is well established and widely used soil measurements, has the potential to provide flux estimates from a much wider range of agricultural sites than would be possible by direct measurement of $N_2O$ emissions.

• Journal of Life Science
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• v.20 no.10
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• pp.1468-1475
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• 2010

Sulfate reduction rates (SRR) using $^{35}SO_4^{-2}$, sulfide producing rates (SPR) using gas chromatography, the number of sulfate reducing bacteria (SRB) using the most probable number (MPN) method, and soil components (moisture, ammonium, total nitrogen, total organic carbon, total carbon, total inorganic phosphorus, total phosphorus, and sulfate) using standard methods in the organic/conventional rice paddy soils, cleaned/polluted reservoir soils, and cleaned/polluted foreshore soils were studied with the change of seasons. The average SRR was more related to the number of SRB and soil components (especially nitrogen and phosphorus) than sulfate concentration. SRR was also recorded to be highest in October soil samples. However, SPR was higher in foreshore soils containing a high concentration sulfate than in fresh water soils, and it was also recorded to be higher in the polluted areas than in clean areas. From these results, we can conclude that the SRR and SPR of anaerobic environments were affected by the number of SRB, soil components and temperature.

• Journal of Life Science
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• v.20 no.9
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• pp.1353-1357
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• 2010

Quantification of the ecosystem respiration is essential in understanding the carbon cycling of natural and disturbed landscapes. Soil respiration and some environmental factors which affect soil respiration were investigated in a Larix leptolepis plantation inKongju, Korea. Soil respiration was measured at midday of the $15^{th}$ and $30^{th}$ day of every month from May to December in a non-cutting area (Control) and a cutting area (Treatment) with IRGA Soil Respiration Analyzer. Throughout the study period, average soil temperature and water content were $23.3{\pm}0.5^{\circ}C$ and $27.76{\pm}7.12%$ for control, and $25.9{\pm}3.1^{\circ}C$ and $24.55{\pm}5.12%$ for treatment, respectively. There was a positive correlation ($R^2$=0.8905) between soil respiration and soil temperature in the study area. However, there was no significant correlation between soil respiration and soil moisture ($R^2$=0.4437). The seasonal soil respiration increased in the summer and decreased in the winter. In August, maximum soil respirations in the control and treatment areas were $0.82{\pm}0.13$ and $1.32{\pm}0.10$ $gCO_2{\cdot}^{-2}{\cdot}r^{-1}$, respectively. Total amounts of $CO_2$ evolution in the control and treatment areas from May to December in 2008 were 2,419.2 and 3,610.8 $CO_2g{\cdot}m^{-2}$, respectively. The amount of soil respiration in the treatment area was 49.3% greater than in the control. Increased soil respiration in the treatment area may be due to increased soil temperature, which drives increased microbial decomposition. According to our present investigation, forest cutting will increase the atmospheric $CO_2$ by increasing soil respiration.

• Magazine of the Korean Society of Agricultural Engineers
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• v.38 no.5
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• pp.47-54
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• 1996

본 연구에서는 지표면유출과 중간유출의 수문학적과정을 함께 모의발생 시키는 합성 유역모델이 제시되었다. 본 모델은 디지털지형모델과 상호 연결되도록 하였으며 지형이 복잡한 지역에서도 유출이 시간과 공간적으로 누가계산되어 이 분야의 조사연구에 필요한 정보를 제공할 수 있다. 본모델을 이용 유역의 불투수층 위에 분포해있는 토양의 중간계층과 토양수분의 계산 및 침투/용탈의 과정을 모의 발생시킬 수 있다.

• Proceedings of the KSRS Conference
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• 2006.03a
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• pp.145-148
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• 2006

새로 조성된 간척지 갯벌이 건조 수축하면 지반 침하와 더불어 토양 내로의 마이크로파의 침투 깊이가 증가한다 따라서 인공위성 DInSAR를 이용하여 지반 침하량을 구하고자 할 때, 건조 시 동시에 발생하는 마이크로파의 개펄 침투 현상을 규명하여 보정해 주어야 한다. 이를 위하여 다편광 산란계(Polarimetric Scatterometer)를 구성하여 건조 개펄에 대한 실내실험을 실시하였다. PolScat의 구성은 5.0-5.6GHz 대역의 dual-polarization square horn antenna를 사용하였으며 Agilent 8753ES 벡터 네트워크 분석기를 사용하였다. 길이 2m, 폭 2m, 높이 20cm의 개펄 샘플을 약 6주 동안 실내에서 건조시켜 위상을 측정한 결과 지반 침하와 함께 약 4mm의 마이크로파 투과현상이 발견되었다. 따라서 인공위성 DInSAR 지반침하량 계산에 있어서 반드시 토양 수분에 따른 마이크로파의 토양 침투 깊이를 보정해 주어야 함이 밝혀졌다.

• Korean Journal of Medicinal Crop Science
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• v.5 no.1
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• pp.1-6
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• 1997

The experiment was conducted to investigate the effect of water stress on yield and quality of Ligusticum chuanxiong Hort. The water stress treatment was imposed artificially on seedling, flowering and rhizome enlargement stage of the plant. The root yield rate decreased to 19.1%, 18.2% and by the water stress treatment at rhizome enlargement, seedling and flowering stage, respectively. Portion of the products having commercial quality grade (above 20g of rhizome weight) was 93.4% at control plot, while it was 85%, 81.7% and 78.3% when stressed for water at seedling, flowering and root enlargement stage, respectively. Content of extract was the higher in the order of control, water stressed at rhizome enlargement, flowering and the seedling stage. Postive correlationship was found between yield of rhizome and rootlet yield or economic production ratio, and between dry weight of stem and rootlet yield.

• Korean Journal of Soil Science and Fertilizer
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• v.12 no.2
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• pp.77-82
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• 1979

Wilting and transpiration charactistics of Panax ginseng leaves were investigated at two temperature levels. Water potential and water absorption characteristics of leaf segments were also observed. Soybean leaves were compared. 1. Ginseng leaves were thiner, higher in water content and lower in dehydration rate. But time required to reach permanent wilting point (pwp) was less than half of that of soybean leaves because water content at pwp was about two times higher (80% of initial water for ginseng and 50% for soybean leaves). The time was shorter under high air temperature. 2. Transpiration rate was about a quater of soybean leaves and lower at $33^{\circ}C$ than $23^{\circ}C$, indicating that ginseng leaves are less tolorant to high air temperature. 3. Ginseng leaf segment showed smaller water free space but greater water deficit and little difference in was absorption rate. 4. Water potential of leaves measured by liquid immersion method was lower than that of soybean leaves. 5. Above results strongly suggest that ginseng plants are more susceptible to water stress. Thus greater light intensity during leaf growing stage (April to June) is recommendable to increase stomate frequency resulting greater transpiration rate and high temperature tolerance during July and August. Abundant water around roots seems to be beneficial as long as oxygen is not limited in rhizosphere.

• Korean Journal of Soil Science and Fertilizer
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• v.34 no.5
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• pp.350-357
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• 2001

This study was performed to evaluate an effect of soil water retention and chinese cabbage growth on application of super water absorbent(CPAM-AS-hyd). In seedling experiments, the CPAM-AS-hyd application rates were 0, 5 and 10kg/10a in bed soil of experimental field. The emergence percentage of chinese cabbage was increased by 9% with application of CPAM-AS-hyd otherwise emergence rates was delayed by 1 day. Water content in soil with CPAM-AS-hyd(10kg/10a) was 27.6%(v/v) at 10days after irrigation and that of control was 20.7%. The CPAM-AS-hyd application caused to alleviate wilting point by 5 days. The content of NO3-N in bed soil was increased with CPAM-AS-hyd application. In the field experiments, as the CPAM-AS-hyd application rates were 5kg/10a and 10kg $10a^{-1}$, the irrigation amounts applied during the growth periods were 1.87 ton, 1.65 ton and 1.53 ton at-0.2bar irrigation frequence and 1.38 ton, 1.25 ton and 1.15 ton at -0.5bar for growth period control, in the CPAM-AS-hyd of 5kg $10a^{-1}$ and CPAM-AS-hyd of 10kg $10a^{-1}$ plot, respectively. The CPAM-AS-hyd application caused to increase yield of chinese cabbage by 9~34% as compared to the control. The contents of $NH_4-N$ and $NO_3-N$ in soil were decreased with the CPAM-AS-hyd application in 10 days after transplanting of chinese cabbage, but the contents of those in soil were increased with the CPAM-AS-hyd application as compared to the control in 20 days after transplanting. The T-N, CaO, MgO and $K_2O$ contents in chinese cabbage increased due to the CPAM-AS-hyd application however $P_2O_5$ content was similar to the control.