• 한국대기환경학회지
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• 제19권5호
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• pp.529-540
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• 2003

A closed chamber system was used for measuring $N_2$0 fluxes from an agriculturally managed upland soil in Kunsan during the growing season from May to July 2002. It is known that soil is one dominant source of atmospheric $N_2$O, contributing to about 57% (9 Tg y $^{-1}$ ) of the total annual global emission. Hence, its increasing emissions and concentrations are largely associated with agricultural activities. In order to elucidate characteristics of soil nitrogen emissions from intensively managed agricultural soils and to understand the roles of soil parameters (soil moisture, soil pH, soil temperature, and soil nitrogen) in the gas emission, $N_2$O soil emissions were measured at every hour during the experimental period (21 days). Soil $N_2$O fluxes were calculated based on changes of $N_2$O concentrations measured inside a closed chamber at every hour. The analysis of $N_2$O was made by using a Gas Chromatography (equipped with Electron Capture Detector). Soil parameters at sampling plots were also analyzed. Monthly averaged $N_2$O fluxes during May, June, and July were 0.14, 0.05, and 0.13 mg-$N_2$O m$^{-2}$ h$^{-1}$ , respectively. Soil temperature and soil pH did not significantly vary over the experimental period; soil temperatures ranged from 12∼$25^{\circ}C$, and soil pH ranged 4.56∼4.75. However, soil moisture varied significantly from 32% to 56% in WFPS. Relationships between soil parameters and $N_2$O fluxes exhibited positive linear relationships. Strong positive correlation ($R^2$ = 0.57, P< 0.0001) was found between $N_2$O flux and sil moisture. It suggests that soil moisture has affected strongly soil $N_2$O emissions during the experimental periods, while other parameters have remained relatively at constant levels. $N_2$O flux from agricultural soils was significant and should be taken account for the national emission inventory.

• 한국약용작물학회지
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• 제8권2호
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• pp.89-93
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• 2000

절편씨마를 이용하여 마를 재배할 경우 토성에 따른 괴경의 형태적 특성과 수량성의 차이를 단마 품종 '마1호'와 장마 품종 '안동재래종'을 공시하여 검토한 결과를 요약하면 다음과 같다. 사토에서는 괴경의 길이가 짧고 분기의 발생이 많아 괴경의 모양이 좋지 않았다. 양토와 사양토에서는 사토에 비하여 분기 발생이 적어 괴경의 모양이 양호하였으며, 괴경의 생체수량은 단마가 $21{\sim}27%$, 장마가 각 6% 증수되었고 , 상마수량은 단마가 $45{\sim}55%$, 장마가 $20{\sim}22%$ 증수되었다. 식양토에서 단마는 괴경의 분지 발생이 다소 많았으며, 장마는 괴경의 굵기가 가늘고 만곡되어 모양이 좋지 않았다.

• 한국토양비료학회지
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• 제51권1호
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• pp.61-70
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• 2018

This study was carried out to review and compare crop cultivations upon chemical properties of paddy soil and qualitative characteristics of rice in Sejong-city from a point of view of farming extension to rice farmers and to utilize the result of the study as a basic guideline for precise agricultural practice. The pH in soils of Sejong was about 6.1-6.6 and had no difference with an average pH of paddy soils in Chung-Nam with pH 6.1. However, the average of organic matter, calcium (Ca) and available silicate in Sejong was lower than the average of them in Chung-Nam. The yields of rice were higher in 2010 than in 2011 and 2012, and the protein contents of rice were the highest in 2011 while the lowest water contents of rice in 2011. The protein contents upon regions were the highest in 2011 with 6.1%, and the amylose contents were the highest in Yeondong-myun, Jeoneu-myun, and Yeonseo-myun in 2010 while Kumnam-myun and Jeondong-myun were the highest in 2012. With the increase of precipitation, the protein content level in rice was increased while the amylose content level tended to decrease. Correlations between the chemical properties of paddy soil and the quality of rice and between level of organic matter in soil and amylose contents were negative (r = -0.507), and the correlation between the moisture contents and amylose contents (r = 0.419) and between the water contents and whiteness (r = 0.485) were positive. Because the quantity and quality of rice yield is determined by the soil characteristics, the consultation to farmers for the proactive soil analysis and for the maintenance of stable level of pH, organic matter and available silicate based on historical results of analysis is highly recommended. Also, the analysis on the effect of the weather and the soil characteristics affecting the quality and quantity of rice would be another good way.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2006년도 학술발표회 논문집
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• pp.333-337
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• 2006

본 연구에서는 원격탐사와 GIS 기술을 이용하여 지형특성을 분석하고 효과적인 토양보존계획 및 관리를 위해 검토되어야 할 토사유실 원인지역을 선정하기 위한 전략적 접근방법을 제시하였다. 이를 위해 지형학적으로 인접되어 있지만 저수지의 탁도에는 매우 큰 차이를 보이고 있는 안동과 임하호 유역을 선정하였다. 각 유역에 대한 효과적인 토양보존계획 및 관리를 위해서는 강우발생에 따른 토사유실의 전반적인 거동을 파악하는 것이 중요하다. 또한 토양보존 프로그램의 효용성을 증가시키기 위해서는 각 유역을 구성하고 있는 소유역별 토사유실 잠재성을 심도 있게 분석해야 한다. 특히 본 연구에서는 안동호와 임하호 유역을 상류, 중류, 하류로 구분하여 토양침식인자, 지형인자, 식생피복인자 그리고 토사유실량의 거동을 분석하였다. 여기서 제시된 접근방법은 토양보존계획을 위해 검토되고 관리되어야 할 우선지역 선정을 위한 가이드라인을 제공 할 것이다.

• 한국토양비료학회지
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• 제49권6호
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• pp.705-711
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• 2016

Crimson clover, a legume crop, is a landscape crop and green manure crop that can be sowing in spring and autumn. Its red flower blooms in May, and serves various roles such as landscape composition, weeds suppressing, prevention of soil loss and nutrient on sloping land and supplying nitrogen and organic matter in soil. Thus, in order to utilize this crop in agriculture land, we evaluated the growth characteristics of crimson clover cultivated in four different soil textures; sand, sandy loam, loam, and clay loam. The nitrogen content of crimson clover was $15.8g\;kg^{-1}$ and C/N ratio was 20.3. Its plant height was 42.5 cm in sandy loam and 49.5 cm in loamy, respectively, approximately 20 cm longer than the sand and clay loam. The crimson clover in sandy loam and loam bloomed about seven days earlier than those in sand and clay loam. Regarding number of flower per hill and flower length, there were no difference among the soil textures. Dry weight of crimson clover for sandy loam and loam was $2.5Mg\;ha^{-1}$ and $2.3Mg\;ha^{-1}$, respectively, $0.8{\sim}1.1Mg\;ha^{-1}$ higher than that of sand and sandy loam. Plant height and dry weight of crimson clover increased with delaying harvest time. Nitrogen contribution in loam and clay loam was $51.3kg\;ha^{-1}$ and $53.5kg\;ha^{-1}$, respectively. Therefore, in terms of flowering properties and dry weight, the proper soil texture for the growth and development of crimson clover was sandy loam and loam.

• 한국지진공학회논문집
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• 제1권3호
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• pp.1-10
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• 1997

구조물 동적거동이 지반과 기초 특성에 따라 영향을 받는다는 것은 인식되었지만, 구조물 내진설계를 위한 설계규준이 지반의 본질적인 복잡성과 기초-지반체계에 대한 체계적인 연구부족으로 지반특성을 부분적으로만 반영하고 있어 불안전하거나 너무 안전한 결과를 초래한다. 이 연구에서는 전단파속도, 지반깊이, 기초 근입깊이 및 말뚝기초의 영향을 평가하여 구조물 내진해석을 위한 기초-지반체계의 운동학적 상호작용 영향을 고찰하였으며, 지반과 기초 특성을 고려한 합리적 내진해석을 위해 지반체계에 대한 수정된 분류기준을 제안하였다. 말뚝기초를 포함한 중형이나 대형 묻힌기초의 경우, 지초-지반체계의 운동학적 상호작용 영향을 고려하기 위해서는 기토밑 지반깊이를 최소한 60m 까지 고려해야하고, 말뚝유무에 관계없이 기초-지반체계의 회전운동도 구조물 내진해석에 포함되어야 한다.

• 한국지반환경공학회 논문집
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• 제13권3호
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• pp.71-76
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• 2012

자연상태의 퇴적물과 준설과정을 거친 준설토 사이에는 퇴적물이 안정상태에서 교란되기 때문에 수질의 탁도가 좋지 않으며, 다시 침강 시 체적변화가 발생한다. 이에 수질의 탁도를 좋게하고 준설토의 부유물질의 침강을 촉진하기 위하여 투입되는 응결제 및 응집제의 양에 따라 준설토는 다양한 특징을 보인다. 본 연구에서는 자연상태의 습윤준설토와 노건조준설토에 약품회사 A, B, C사의 약품투입량에 따른 준설토의 부유물질(SS)측정, 체적변화 및 침강속도의 특성분석을 파악하고자 연구를 수행하였다. 실험 결과 습윤준설토와 노건조준설토의 약품량이 많을수록 부유물질(SS)측정은 낮아지고, 체적변화율은 증가하는 경향을 보이고 있으며, 침강속도는 빨라지는 경향을 보였다. 또한 습윤준설토와 노건조준설토의 약품량의 차이는 노건조준설토 경우 $100{\pm}5^{\circ}C$에서 건조시키기 때문에 유기물 및 미생물이 소멸하여 적은 양으로도 약품에 민감한 반응을 보이는 것으로 판단된다.

• 농업과학연구
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• 제49권2호
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• pp.215-226
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• 2022

This study aims to investigate the soil environment characteristics of the Abies koreana community, which is currently showing a continuous decline in its size, in order to provide fundamental data for the management and creation of a conservation plan for the Abies koreana communities at the Korean national parks of Sobaeksan, Deogyusan, and Jirisan. Soil depth investigations were conducted at depths deeper than 40 cm into the B horizon at most study sites, except for the Dwaejipyeongjeon and Byeoksoryeong sites. The soil water content exceeded 30% on average, and these soils showed low bulk density levels. The soil texture was found to be the loamy or silty loam type at most study sites. It was also found in a chemical characteristic assessment that the soil samples contained more than 10% organic matter at most study sites. The cation exchange capacity (C.E.C.) and total N concentration levels were also high at most study sites. However, the soil showed low exchangeable K⁺, Na⁺, Ca²⁺, and Mg²⁺ levels at most study sites. Finally, the pH values were 4.90, 4.53, and 4.60 at soil depths of 10 cm at the Sobaeksan, Deogyusan and Jirisan sites, respectively, outcomes that are notably lower than the average levels in soil from Korean forests according to the literature. This appears to be due to the cold and wet climate of these subalpine regions given the reduced leaf-litter decomposition rate and accumulation of organic acids.

• 분석과학
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• 제19권1호
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• pp.18-30
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• 2006

This paper describes the cumulative deposition of fallout Pu in soil and lichen at the present time and give the characteristics of fallout Pu deposits in the soil. In the soil of the forest, the accumulated depositions of $^{239,240}Pu$ were estimated to be in the range of 34.0 to $101.2Bq\;m^{-2}$ with an average value of $65.3{\pm}21.6Bq\;m^{-2}$. The average inventory of $^{239,240}Pu$ in the forest was calculated to be two times higher than that in the hill. Also, the deposited activities of $^{239,240}Pu$ in cultivated soil were significantly lower than those in the hill or forest. However, the cumulative depositions of fallout Pu in the volcanic ash soil on Cheju Island were much higher than those in the forest and hill soils. The measured activity concentrations of Pu isotopes in lichens and mosses showed large variations, due to characteristics of species and life span of lichen and moss colonies. From depth profiles, it was found that most of the fallout Pu has been accumulated in upper 10 cm layer of soil. Except for a few cases, the concentrations of $^{239,240}Pu$ in soil tended to decrease exponentially with increasing soil depth. Among parameters affecting the cumulative deposition of fallout Pu, organic substances and rainfall play an important role in the retention and relative mobility of fallout Pu in the soil. However, pH showed a weak correlation with the deposition of fallout Pu in the soil. From sequential leaching experiments, Pu was found to be associated predominantly with the "organic" and "oxy-hydroxy" fractions. Both the activity ratios of $^{238}Pu/^{239,240}Pu$ and $^{241}Pu/^{239,240}Pu$ in soils, lichens and mosses and the atomic ratios of $^{240}Pu/^{239}Pu$ in soils are close to those observed in the cumulative deposit global fallout from nuclear weapon testings. The results obtained from this research make it possible to interpret and predict the behavior of fallout Pu under natural conditions.

• 한국자원식물학회지
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• 제33권6호
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• pp.651-658
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• 2020

The aim of this study was to investigate the comparative growth characteristics and ginenoside contents of wild-simulated ginseng on different years (7 and 13-year-old) by monitoring soil properties of cultivation regions. Plant and soil samples were collected from 6 different cultivation regions. Soil organic matter (OM), total nitrogen (TN) and cation exchangeable capacity (CEC) were significantly higher in 13-year-old wild-simulated ginseng cultivation regions compared to 7-year-old wild-simulated ginseng cultivation regions. Growth characteristics of wild-simulated ginseng had shown significantly higher in 13-year-old wild-simulated ginseng compared to 7-year-old wild-simulated ginseng. Ginsenoside G-Rb1, Rb2, Rc, Rd, Re, Rf, Rg1 were significantly higher in 13-year-old wild-simulated ginseng than 7-year-old wild-simulated ginseng. According to the results of correlation analysis, soil OM, TN and CEC of the cultivated regions were positively correlated with the growth of wild-simulated ginseng. In addition, the root length of wild-simulated ginseng showed positive correlation with ginsenoside content. Hence, this study was able to investigate the correlation between growth and ginsenoside content of wild-simulated ginseng based on soil characteristics of the cultivation regions.