• Proceedings of the Korean Society for Bio-Environment Control Conference
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• 1998.10a
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• pp.151-155
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• 1998

본 실험은 무등산수박과 달고나수박으로 98년 4월 2일에 파종하여 4월 24일 토양과 펄라이트＋코코피트 혼합배지에 각각 정식하였다. 무등산수박과 달고나수박의 재배방법에 따른 생장결과를 보면 엽수는 달고나수박이 많은 반면 총엽면적은 무등산수박이 높게 나타났다. 생체중 및 건물중에 있어서도 달고나수박보다 무등산수박이 더 높게 나타났으며 토양재배보다 양액재배 수박이 더 월등한 생장차이를 나타내었다. 당도는 달고나 수박이 무등산수박보다 훨씬 더 높은 반면 과실무게는 무등산수박이 더 높게 나타났다. 엽병내 질소흡수량은 생육초기에는 26,000-30,000prm 정도이었고 수분후 33일에는 38,000-44,000ppm 정도로 상승하였다. 인산은 생육초기 4,000-8,800ppm 정도에서 수확기에 이르면 480-l,600ppm 정도로 감소하였다. 칼륨은 생육초기에 10,000-26,000ppm 정도였으나 수분기부터는 8,000-14,000ppm 범위로 흡수되었다. 칼슘의 흡수는 생육초기에는 앙액재배 수박이 52,000-5,700ppm 범위로 토양재배 수박의 2,700-3,900ppm 범위보다 약간 많은 것으로 나타났지만 생육이 진전됨에 따라 토양재배 수박의 흡수량이 양액재배 수박의 흡수량보다 많아지는 경향이었다. 마그네슘의 흡수는 생육초기에 토경에서 훨씬 더 용이하게 흡수되는 경향이었으나 수분기부터는 200-700ppm 범위로 일정하였다.

• Proceedings of the Korea Water Resources Association Conference
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• 2022.05a
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• pp.323-323
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• 2022

증발산은 지표면과 식물의 엽면적에서 액체가 기체로 기화되는 현상으로 수자원적 측면에서는 지표의 이용 가능한 물이 대기 중으로 손실됨을 의미하며, 증발산 요소는 온도, 습도, 바람의 영향에 의한 변동이 크며 특히 토양수분의 가용성에 큰 영향을 미친다. 국내의 피복 환경은 주로 산지 사면으로 이루어져 있어 증발산량의 특성이 대체적으로 지면의 증발보다 식물의 뿌리로부터 흡수되어 잎의 기공으로 발생하는 증산작용이 지배적이다. 증산작용이 발생하는 메커니즘은 기공을 열어 광합성에 필요한 이산화탄소가 흡수하는 과정에서 물의 손실이 발생하는데 대기 중 이산화탄소의 농도가 높으면 기공이 빠르게 닫혀 증산량도 줄어들어 대기 중으로 물 손실이 줄어드는 현상이 관측된다. 따라서 본 연구에서는 국내 설마천 소유역에서 유출량, 강우량, 토양수분, 증발산량 등과 같은 수문 요소가 이산화탄소 플럭스와 상관성을 분석해보고자 한다.

• Korean Journal of Soil Science and Fertilizer
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• v.13 no.2
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• pp.71-76
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• 1980

Effect of soil moisture on growth of 2 year old Pan ax ginseng was investigated by pot culture using clay loam and sandy loam soils. In clay loam soil emergence rate of new shoot and stem growth were greatly decreased below 40% of field capacity. In sandy loam soil the growth of stem and leaf were greatly affected below 40% moisture. Root yield showed maximum at 60% moisture and significantly coorelated with stem diameter and root length. Rotten root rate and die back rate of top were least at 60% and gradually increased with either increase or decrease of soil moisture.

• Korean Journal of Soil Science and Fertilizer
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• v.26 no.4
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• pp.284-288
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• 1993

Tow Kinds of Soils, vertisol and alfisol, were selected and analyzed pore space distribution(PSD) by mercury intrusion method and soil water potential after freeze-drying from different water conditions, such as 0.033MPa, 1.5MPa and ovendry. The PSD values measured by mercury intrusion method were higher in large pores than the values from soil water potential. Also, there were big differences of PSD by the changes of the water content befor freeze-drying.

• Korean Journal of Soil Science and Fertilizer
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• v.13 no.4
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• pp.115-118
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• 1981

Effect of water potential of culture solution on photosynthesis, transpiration and water uptake was investigated using polyethylene glycol 6000. 1. Even at -0.5 bar of culture solution phothosynthesis was decreased by 20% within 1 hour. Plant in control showed 3.26% loss of initial water for 13 hours suggesting very sensitive in water uptake. 2. Relation between water potential of culture solution (${\psi}$) and water uptake amount (W) 2-year root was ${\psi}=-2.890/e^{2.796W}$ indicating that permanent wilting point will be greater than -2.89 bar. 3. Transpiration considerably decreased with the decrease of water potential and thus by 23.9% at -0.5 bar after 4 hours. 4. From the above results ginseng plant appears to have high root water potential at permanent wilting point and thus very week to water stress due to drought or high salt content in soils.

• Korean Journal of Agricultural and Forest Meteorology
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• v.6 no.1
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• pp.18-23
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• 2004

This study was conducted to provide a national forest management method for natural Pinus densiflora forest stands in central South Korea based on growth characteristics and water relations. Average stand volume per hectare was 259.3㎥ in the pine study site. Basal area, volume, annual mean increment and periodic annual increment of DBH for 10 years at each slope aspect appeared to decrease as the aspect shifts from north to south. Stems per hectare showed the lowest value at the northern aspect. Maximum water potentials measured between 12 and 14 o'clock were analyzed by aspect and elevation. Water potential of pine decreased as the aspect changed from north to south, and water potential increased at lower elevations. Soil water content for the pine stands tended to decrease as the aspect shifted from north to south. Water potential and soil moisture content were highly correlated. Soil water deficits indicate that pines have a higher moisture requirement on the ridge and the southern aspect.

• Magazine of the Korean Society of Agricultural Engineers
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• v.38 no.4
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• pp.53-62
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• 1996

작물의 최대 수확을 위한 관개계획은 작물의 수분장력 스트래스와 삼투스트래스를 최소화 시킬 수 있도록 언제 얼마의 물을 어떤 속도로 공급해 줄 것인가를 결정하는 것이다. 이는 토양, 작물 및 대기의 여러 가지 요소를 측정하여 결정할 수 있다. 관개속도는 주로 토양의 투수계수에 의하여 결정되지만 관개시간과 양은 토양함수량과 경우에 따라서는 토양염도에 의하여 결정된다. Time Domain Reflectometry (TDR)는 한 개의 탐침으로 토양 함수량과 토양염도를 동시에 측정하는 새로운 기법이다. TDR의 측정원리와 상업용 TDR장비에 대하여 자세히 설명하였다. TDR 탐침의 간격, 직경 및 길이의 제한요소를 토양함수량과 전기전도도의 함수로 나타내었다. 토양 columm 및 현장에서의 TDR 전극 삽입과 케이블테스터의 신속한 분리기법과 토양층에 TDR 탐침을 영구히 설치하는 기법에 대하여 자세히 설명하였다.

• Korean Journal of Agricultural and Forest Meteorology
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• v.21 no.4
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• pp.297-306
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• 2019

Soil moisture monitoring is an important task to cope with climate change, and soil water prediction can provide large-scale soil moisture information. Therefore, this study was conducted to evaluate the relationship between the measured and predicted soil water content, and to estimate the correlation between the soil characteristics and soil water content. The selected sites in soil moisture monitoring network were 76, and the soil with high sand content (sand, loamy sand, and sandy loam in soil texture) accounted for 77% of the total. Organic matter and bulk density were 0.03 to 3.50% and 1.01 to 1.69 Mg m^-3, respectively. Predicting values of field capacity and wilting point were lower than the measured soil water content, and the correlation coefficient between the measured and predicted values were low as 0.548 to 0.748. However, a significantly high positive correlation (p<0.01) found between the measured and predicted soil water content. Soil water (field water capacity and wilting point) content was highly positively correlated with silt, clay, and organic matter (p<0.01) and highly negatively correlated with sand (p<0.01).

• KSCE Journal of Civil and Environmental Engineering Research
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• v.31 no.3B
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• pp.211-220
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• 2011

In this study a conceptual soil water model is proposed to simulate water balance at catchment scale. The model is based on the sequential separation of daily precipitation into surface runoff, wetting, vaporization, and percolation. The proposed model is calibrated by using three observation sets: empirically estimated annual vaporization, monthly wetting estimated by NRCS-CN method, and both of them. The model performance is evaluated to understand which hydrologic components for calibrating the model are needed. It is shown that both of annual vaporization and monthly wetting are indispensable hydrologic components to simulate reasonably precipitation partitioning.

• Journal of Korea Water Resources Association
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• v.35 no.1
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• pp.65-75
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• 2002

The objectives of this study are to analyse model-based soil moisture variations depending on model parameters m and $T_0$ and to evaluate the model performance for the simulation of soil moisture variations by the comparison of observed groundwater levels and model-driven soil moisture amounts and observed and simulated river discharges at the basin outlet. The selected study area is the Pyungchang IHP river basin with outlet at Sanganmi station and the summer flooding events during '94-'98 are used for the analysis. As a result, soil moisture holding capacity is increased according to increase the parameter m that represents effective groundwater depth. This phenomenon is especially dominant when higher m and $T_0$ values are used. The qualitative comparison of computed base flow and observed groundwater level shows that the base flow peaks are reasonably simulated and the decreasing limbs of hydrograph are mainly caused by base flows. It is concluded that TOPMODEL can be used effectively for simulating basin-averaged soil moisture variations in addition to river flow generations.