• 한국작물학회지
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• 제44권2호
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• pp.134-137
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• 1999

An experiment was carried out to determine the effects of priming and growth regulator treatment of seeds on the emergence and seedling growth of rice, Oryza sativa L. (cv. 'Ilpumbyeo'). Normal seeds were primed in a -0.6 MPa polyethylene glycol solution at 15$^{\circ}C$ for four days with air-bubbling. Then both primed and non-primed seeds were soaked in water, 100 ppm GA$_3$, 2 ppm ABA, and 10 ppm kinetin solutions for 24 hours. The seeds were planted in soil at 3 and 5 cm depths and allowed to germinate in a growth cabinet at 2$0^{\circ}C$. Generally, the emergence rate at the 3 cm seeding depth was higher and emerged faster compared with the 5 cm seeding depth. The emergence rate of primed seeds was higher and emerged faster compared to non-primed seeds. GA$_3$ and kinetin treatments were the most effective to improve the emergence rate of non-primed seeds. Coleoptile length at the 5 cm seeding depth was longer than that at the 3 cm seeding depth. Leaf number, plant height, and root length of primed seedlings were higher compared with non-primed seeds. GA$_3$ promoted the elongation of plant height and mesocotyle length.

• 농업과학연구
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• 제47권4호
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• pp.1097-1107
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• 2020

Assessment of soil carbon stock is essential for climate change mitigation and soil fertility. The digital soil mapping (DSM) is well known as a general technique to estimate the soil carbon stocks and upgrade previous soil maps. The aim of this study is to calculate the soil carbon stock in the top soil layer (0 to 30 cm) in Jeolla Province of South Korea using the DSM technique. To predict spatial carbon stock, we used Cubist, which a data-mining algorithm model base on tree regression. Soil samples (130 in total) were collected from three depths (0 to 10 cm, 10 to 20 cm, 20 to 30 cm) considering spatial distribution in Jeolla Province. These data were randomly divided into two sets for model calibration (70%) and validation (30%). The results showed that clay content, topographic wetness index (TWI), and digital elevation model (DEM) were the most important environmental covariate predictors of soil carbon stock. The predicted average soil carbon density was 3.88 kg·m-2. The R2 value representing the model's performance was 0.6, which was relatively high compared to a previous study. The total soil carbon stocks at a depth of 0 to 30 cm in Jeolla Province were estimated to be about 81 megatons.

• 한국토양비료학회지
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• 제37권3호
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• pp.131-135
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• 2004

본 연구는 일반 기상 측정에서 에너지 수지를 구할 때 이용되는 지중열류 값과 토양 내 10 cm 깊이에서 측정한 토양온도를 활용하여 태양 복사에너지와 지표면 복사 에너지의 도달과 분배에 중요한 역할을 하는 토양표면의 온도를 예측하고자 수행하였다. 2003년 6월 10일부터 6월 24일까지 측정한 지중열류와 토양온도 그래프에서 토양온도나 지중열류는 주기성을 나타내며 일중 최저 지중열류와 최고 토양온도 사이에는 위상편차가 존재한다. 토심 5 cm에서 측정하여 시간별로 평균한 토양온도와 지중열류 사이에는 2시간의 시간지연이 존재하며 토양온도와 시 공간상에서의 지중열류는 정의 상관관계를 보였다. 이는 단위체적 당 열용량과 깊이에 따른 열량의 변화율이 태양에너지와 지표면 복사를 통한 지중열류에 비례한다는 것을 의미한다. 예측된 토양 표면온도는 시간별로 평균하였을 때 그 평균온도가 $20^{\circ}C$를 넘어 여름철의 기온을 반영하였으며 모양도 주기함수 형태를 보였다. 진폭은 $4.5^{\circ}C$로서 10 cm 깊이에서의 진폭인 $3.4^{\circ}C$보다 $1.1^{\circ}C$ 높았으며 최저온도가 나타난 시간은 토양표면의 경우는 오전 8시, 10 cm 깊이에서는 오전 9시였으며 최고온도가 나타난 시간은 토양표면은 16시, 10 cm 깊이는 19시이었다. 시간별로 평균하지 않았을 때의 최고와 최저온도는 각각 33.2, $16.5^{\circ}C$ 였으며, 토양표면온도 분포는 $15-20^{\circ}C$가 5.3%, $20-25^{\circ}C$가 65.6%, $25-30^{\circ}C$가 28.1%, $30-35^{\circ}C$가 1%로 대부분의 온도는 $20-25^{\circ}C$ 범위의 값을 나타냈다. 예측된 토양표면온도의 검증을 위해 토양표면 온도와 10 cm 깊이의 토양온도를 가지고 계산한 산술 평균과 토심 5 cm에서 측정한 토양온도를 비교하였다. 또한, 그 과정을 통해 얻어진 추정회귀모형은 P값이 0.001보다 작아 유의성이 인정 되었다. 회귀모형의 결정계수는 0.968이었고 표준오차는 0.38로 예측된 토양표면온도는 추정 회귀모형에 의해 실제 값에 가깝게 추정할 수 있을 것이다.

• 한국해양학회지:바다
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• 제10권1호
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• pp.100-112
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• 2005

갯벌의 온도구조와 열적 특성변화를 조사하기 위해 서해안 공소만 갯벌조간대에서 고도가 다른 3개 지점을 설정하여 40 cm깊이까지 계절별로 1개월간의 온도관측을 수행하였다. 표층에서 평균온도는 하계에 아래층보다 높고 동계에는 낮아져 표층가열과 냉각에 의한 온도구조와 변화 형태를 보여주었으며 표준편차는 아래층으로 갈수록 감소하였다. 주기성이 뚜렷한 일사량과 조위 변화가 주로 단기적 온도변화를 야기하였고, 간헐적으로는 강우와 강한 풍속도 영향을 주었다. 시계열분석에 의하면 24시간, 12시간 그리고 8시간 주기 성분에 강한 에너지 첨두(peak)를 보였으며, 24시간 주기성분이 가장 큰 에너지를 보였다. 24시간 주기 성분은 일사량변화, 12시간 주기는 반일주조 조위변화 그리고 8시간 주기성분은 일사량과 조위변화의 상호작용에 의한 온도파동으로 해석되었다. EOF분석에서 제 1모드와 제 2모드가 수직온도구조 변화의 96%를 차지하였다 제 1모드는 갯벌 표층에서의 가열과 냉각에 의한 현상으로, 제 2모드는 갯벌내부의 열 전파과정에서 발생하는 지연효과로 해석되었다. 교차스펙트럼 분석에서 24시간 주기성분 온도파동에 의한 열전달위상은 깊이에 따라 선형적으로 증가하는 평균위상 차이를 보였고, 표층에서 10 cm, 20 cm, 40 cm 깊이까지의 위상 차이에 의한 지연시간은 각각 3.2시간, 6.5시간 9.8시간이었다. 일차원적 열확산모델에서 산출된 24시간 주기성분 온도파동의 수직 확산계수는 깊이와 계절에 걸쳐 평균하였을 때 중부조간대 정점에서는 $0.70{\times}10^{-6}m^2/s$, 하부조간대 정점에서는 $0.57{\times}10^{-6}m^2/s$의 값을 보였다. 깊이 평균된 확산계수는 봄철에 크고 여름철에 작았고, 계절 평균된 확산계수는 2cm부터 10cm깊이까지 증가하고 10cin부터 40cm깊이까지는 감소하는 수직구조를 보였다. 평균 열확산계수를 사용하여 구한 온도전파 확산속도는 2 cm 깊이로부터 10 cm, 20cm, 40cm까지 각각 $8.75{\times}10^{-4}cm/s,\;3.8{\times}10{-4}cm/s,\;1.7{\times}10^{-4}cm/s$정도의 값이 되어 표층에서 깊어질수록 작아졌다.

• 한국농공학회지
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• 제22권4호
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• pp.82-95
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• 1980

This paper complies the results of the studies so far made on the subsoil improvement of subsurface drainage systems for wet paddy fields (those were located in the Gum-Ho area in Kyung Buk province) which had poor permeability and a high water table. In general, a drainage problem is an excess of water on the ground surface which can effect the productivity and bearing capacity of the soil. With drain pipe systems, (According to their depths and spacing) it may be possible to correct that problem. The experimentation consisted of three test plots, two of which included drain pipe systems with varing depths and width spacing of the pipes. The third plot (C) was an ordinary plot being exempt of a drain pipe system. In detail, the depth of plot A was 80 cm, and the width spacings began at 2. Om and increased by 2. Om up to 10. 0m. The depth of plot B was 60cm and the width spacing was the same as plot A. These tests were performed to research specific details; such as crop yeild, bearing capacity of the soil, the amount of underdrainage, surface cracks, root distribution, the water table level, the consumptive water depth and the soil moisture content. The test period lasted three years, from 1977 thru 1979. The results obtained were as follows: 1. During the test period, the weather conditions for the area tested were in accordance with the annual average for that area. Furthermore the precipitation factor during the spring cultivation season, the intermediate drainage period and the harvest drainage period was of optimum conditions for controling surface cracks, because of less precipitation than evaporation. 2. The difference in the level of the ground water table in plots A and B was hardly noticable, but the difference in the test plots and the ord. plot was greatly noticable. The test plots (A, B) were 30 to 40cm lower than the ordinary plot. On the whole, the ground water table of the ord. plot always stayed at a level of 15-20cm beneath the surface of the soil, the ground water table of the test plot A showed The difference in the depth of the pipe lower than the test plot B, while the test plots showed a remarkable descending effect. 3. The soil temperature in plot A was slightly core than in plot B with a difference of 0. 47$^{\circ}$C, but plot A was 1. 6$^{\circ}$C higher than the ord. plot during the flooding period, but after drainage the temperature difference climed to 2. 0$^{\circ}$C. 4. During the 3rd test year, the values of the cracks were recorded with the values of 59cm in plot A, 42cm in plot B and 15cm in the ordinary plot. Plots A and B had increased 2.5 times the value of the first year while the ordinary plot had remained the same. 5. The root weight of the rice was measured at a value of 77.2 gr. for plot A, 73.5 gr. for plot B and 65.3 gr. for the ord. plot. Therefore, the root growths in plots A and B were much more energetic than in the ord. plot. 6. The consumptive water depth measured during the 3rd year resulted in the values of 26. 0mm per day for plot A, and 24.9 mm per day for plot B, respectively. Therefore, both plot A and plot B maintained the optimum consumptive water depths, but the ordinary plot only obtained the value of 12.3 mm per day, which clearly showed less than the optimum consumptive water depth which is 20 to 30 mm/day. 7. The soil moisture content is in direct relationship to the ground water level. During drainage, test plot A decreased in its ground water level much more rapidly than the other two plots. Therefore, plot A had a much less soil moisture content. But this decreased water level could be directly effected by the weather conditions. 8. The relationship between the bearing capacity and the soil moisture content were directly inversely proportional. It can be assumed that the occurence of soil creaks is limited by the soil moisture content. Therefore, the greater the progress of the surface creaks resulted in a greater bearing capacity. So, tast plot A with a greater amount of surface cracks than the other test plots resulted in a greater bearing capacity. But, the bearing capacity at the harvest season could be effected by the drainage during the intermediate drainage period and by the weather conditions. 9. Comparing the production of the test plots to the ord. plot; there was an increased value of 840kg for plot A, 755kg for plot B and 695kg for the ord. plot in the rough rice. Therefore, plot A had an increase of 20% over the ordinary plot. The possibility of producing double crops was investigated. The effects on barley production in the test plots showed a value of 367kg per 10 acres, which substantiated the possibility of double crops because that value showed an increased value over the average yearly yield for those uplands. 10. So as a result, it can be recommended that by including a drain pipe system with the optimum conditions of an (80cm centimeter) depth and a (l0m) spacing will have a definite positive effect on the over all production capacity and quality of wetpaddy fields.

• Journal of Ecology and Environment
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• 제30권2호
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• pp.151-159
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• 2007

We studied the optimal ranges of water and soil characteristics for wetland plants, particularly Scirpus tabernaemontani (softstem bulrush) and Typha latifolia (broadleaf cattail), which are dominant species with potential for restoration of Korean wetlands. We observed vegetation in S. tabernaemontani and T. latifolia communities from the mid to late June, 2005, and measured characteristics of water environments such as water depth (WD), temperature (WT), conductivity (WC), and concentration of several ions $(NO_3{^-}-N,\;Ca^{2+},\;Na^+,\;Mg^{2+},\;and\;K^+)$, and characteristics of soil environments such as soil texture, organic matter (loss on ignition, LOI), conductivity, and pH. The S. tabernaemontani community was accompanied by Zizania latifolia (Manchurian wildrice), Persicaria thunbergii (Korean persicary), Actinostemma lobatum (lobed actinostemma), and Beckmannia syzigachne (American slough grass), while the T. latifolia community was accompanied by P. thunbergii, T. angustifolia (narrowleaf cattail), and Glycine soja (wild soybean). We defined the optimal range for distribution (ORD) as the range that each plant was crowded. The optimal range of water characteristics for the S. tabernaemontani community was a $WD\;10{\sim}50cm,\;WT\;24.0{\sim}32.0^{\circ}C,\;WC\;100{\sim}500{\mu}S/cm,\;{NO_3}{^-}-N\;0{\sim}60ppb,\;K^+\;0.00{\sim}1.50ppm,\;Ca^{2+}\;7.50{\sim}17.50ppm,\; Na^+\;2.50{\sim}12.50ppm,\;and\;Mg^{2+}\;3.00{\sim}7.00ppm$. In addition, the optimal range of soil characteristics for the S. tabernaemontani community was a soil texture of loam, silty loam, and loamy sand, $LOI\;8.0{\sim}16.0%,\;pH\;5.25{\sim}6.25$, and conductivity $10{\sim}70{\mu}S/cm$. The optimal range of water characteristics for the T. latifolia community was a $WD\;10{\sim}30cm,\;WT\;22.5{\sim}27.5^{\circ}C,\;WC\;100{\sim}400{\mu}S/cm,\;{NO_3}{^-}-N\;0{\sim}60ppb,\;K^+\;0.00{\sim}1.50ppm,\;Ca^{2+}\;0.00{\sim}17.50ppm,\;Na^+\;0.00{\sim}12.50ppm,\;and\;Mg^{2+}\;0.00{\sim}5.00ppm$, and the optimal range of soil characteristics for the T. fatifolia community was a soil texture of loam, sandy loam, and silty loam, LOI $3.0{\sim}9.0%,\;pH\;5.25{\sim}7.25$, and conductivity $0{\sim}70{\mu}S/cm$.

• Environmental Analysis Health and Toxicology
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• 제22권2호통권57호
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• pp.129-135
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• 2007

Polycyclic aromatic hydrocarbons(PAHs) have been analyzed to assess vertical distribution of them with different land uses. The soils were collected from three layers; surface $(0{\sim}5cm)$, intermediate $(6{\sim}10cm)$, and deep $(11{\sim}15cm)$ layer, respectively considering land use; paddy, upland, and mountain in each site. Total 89 samples of soil from 10 sites were analyzed. Overall mean of ${\sum}PAHs$ were 137 (range $8.87{\sim}625{\mu}g\;kg^{-1}$), 203 (range $16.5{\sim}645{\mu}g\;kg^{-1}$), and $83.4{\mu}g\;kg^{-1}$ (range $6.65{\sim}667{\mu}g\;kg^{-1}$) for paddy, upland, and mountain soil, respectively. The dominant PAHs were fluoroanthene/benzo(b)fluoroanthene>pyrene>indeno(1, 2, 3-cd) pyrene in paddy, fluoroanthene/pyrene>benzo(b)fluoroanthene>chrysene in upland, and benzo(b)fluoroanthene>pyrene>chrysene in mountain soil, whereas the profile was quite similar for each other except that indeno(1, 2, 3-cd)pyrene and benzo(ghi)perylene are relatively higher in the paddy soils. Although the concentration gradient by depth was not observed in the paddy and upland soils because perturbation of soil layer by tillage, significant decrease was in the deep layer relative to the surface and intermediate layer. However, the concentration gradient of PAHs by soil depth was clearly shown in mountain soil without experiencing disturbance of tillage.

• Journal of Biosystems Engineering
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• 제27권1호
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• pp.39-44
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• 2002

In order to obtain the information of bio-environment control, the thermal characteristics of soil in the greenhouse heated by the heat pump and latent heat storage system were experimentally analyzed. The experimental systems were composed of the greenhouse with a heat pump and a latent heat storage system (system I), the greenhouse with a heat pump (system II), the greenhouse with a latent heat storage system (system III), and the greenhouse without auxiliary heating system (system IV). The thermal characteristics experimentally analyzed in each system were temperature of soil layers, soil heat storage and release, soil heat capacity and soil heat storage ratio. The results could be summarized as follows. 1. Time to reach the highest temperature at 20cm deep in soil layers of the crop routs in case of system I was shown to be delayed by 6 hours in comparison to the time of the highest temperature at the soil surface. 2. In the clear winter days, the stored heat capacity values fur the system I and the system II were shown to be 22.3% and 11.0% higher than the released heat capacity respectively, and the stored heat capacity values for the system III and the system IV were shown to be 6.2% and 29.6% lower than the released heat capacity respectively This confirms that the system I provided the best heat storage effect. j. The heat quantity values stored or released were shown to be highest at 5 cm depth of soil layers. And it was reduced with increasing of depth of soil layers until 20 cm and was not changed under the soil layer of 20 cm depth. 4. The heat absorption rates of soil, the ratio between supplied and stored heat energy, fur both the system I and system II were lower than 23%.

• 한국토양비료학회지
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• 제25권3호
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• pp.220-230
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• 1992

우리나라에서 토양(土壤) 온도(溫度)를 정규적으로 관측(觀測)하고 있는 기상청(氣象廳) 산하(傘下) 기상대(氣象臺) 및 관측소(觀測所) 관측(觀測) 노장(露長)의 토양시료(土壤試料)를 채취(採取)하여 토양(土壤)의 열전도(熱傳度) 특성(特性)과 관련이 깊은 토양(土壤)의 용적밀도(容積密度), 토성(土性), 유기물(有機物) 함량(含量) 등 물리적(物理的) 특질(特質)을 분석(分析)하였으며, 토양(土壤)의 열확산(熱擴散) 계수(係數)를 산출(算出)하였다. 기상청(氣象廳) 산하(傘下) 기상대(氣象臺) 및 관측소(觀測所) 토양(土壤)의 물리적(物理的) 특성(特性)을 조사한 결과(結果) 0-10cm의 표토(表土)는 52%가 사양토(砂壤土)였으며, 양토(壤土)와 미사질양토(微砂質壤土)가 38%, 그리고 식양토(埴壤土) 및 미사질식토(微砂質埴土)가 10%이었다. 이들 토양(土壤)의 열특성(熱特性)과 관계가 깊은 용적밀도(容積密度)는 사토(砂土)가 $1.41g/cm^3$, 양토(壤土)와 미사질양토(微砂質壤土)가 $1.33g/cm^3$, 그리고 식양토9埴壤土) 및 미사질식토(微砂質埴土)가 $1.21g/cm^3$로 토성(土性)이 미세할수록 낮은 값을 보였다. 열확산(熱擴散) 계수(係數)는 평균(平均) $3.53{\times}10^{-3}cm^3/sec$이었으며, $1.159-8.401{\times}10^{-3}cm^3/sec$의 범위에 있었다. 특히 유기물(有機物) 함량(含量)이 높고 용적밀도(容積密度)가 낮은 제주도(濟州道) 토양(土壤)의 열확산(熱擴散) 계수(係數)는 표토(表土)에서 $2{\times}10^{-3}cm^3/sec$으로 다른 지역의 토양(土壤)보다 현저히 낮았다. 토심(土深) 30cm 이하(以下) 토양(土壤)의 열확산(熱擴散) 계수(係數)는 평균(平均) $6.81{\times}10^{-3}cm^3/sec$로 $1.54-16.12{\times}10^{-3}cm^3/sec$의 범위를 보여 표토(表土)보다 높았다. 열확산(熱擴散) 계수(係數)로부터 계산(計算)된 표토(表土)의 일주간(日週期) 불역심(不易深)(damping depth)은 5.92-13.65cm였으며, 깊이 30cm이하의 연주기(年週期) 불역심(不易深)은 124-342cm이었다. 한편, 실험실내(實驗室內)에서 열선막대법에 의하여 측정(測定)된 열확산9熱擴散) 계수(係數)와 용적밀도(容積密度) 및 토양수분함량(土壤水分含量)과의 관계로부터 열확산(熱擴散) 계수(係數)를 추정(推定)할 수 있는 중회귀(重回歸) 모델을 이용하면 토양온도(土壤溫度)가 부족한 지점(地點)의 열확산(熱擴散) 계수(係數)를 추정(推定)할 수 있게 되었다.

• 한국토양비료학회지
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• 제40권2호
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• pp.109-113
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• 2007

계화간척지의 간척지구별 숙답화에 따른 토양특성을 구명하여 시비 및 토양관리계획을 수립하고자 논토양 100필지의 토양특성과 177농가에 대한 영농설문을 조사 분석한 결과 유효토심은 17.8 cm로 적정값(50 cm 이상)에 비하여 크게 미달되었으며 특히 심토의 경우 토양경도 $12.40kg\;cm^{-2}$, 용적밀도 $1.59g\;cm^{-3}$ 로 매우 높아 토양의 물리성이 불량하였다. 토양의 염농도는 0.03~0.12%로 거의 제염이 되었으며, 작토의 pH는 6.0, 유기물함량은 $8.6g\;kg^{-1}$, 유효 인산 및 규산은 각각 58과 $85mg\;kg^{-1}$, CEC는 $7.4cmol\;kg^{-1}$, ESP는 10.3%로 나타나 토양 중 양분의 불균형 현상이 나타났다. 또한 계화간척지 논에서 벼재배시 농가의 시비량($N-P_2O_5-K_2O$, kg $ha^{-1}$)은 200-54-61이었으며 경운시기는 84%가 춘경을 하였으며 벼 재배 시 볏짚을 매년 시용하는 농가는 14%에 불과하였다.