• Journal of Korea Soil Environment Society
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• v.2 no.3
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• pp.59-67
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• 1997

To investigate the effects of organic matter and soil depth on soil water flow in a multi-layered soil, the saturated hydraulic conductivities(Ksat) were measured from the single- and multi-layered soil columns, that the soils were mixed with the oven-dried cow manure compost(CMC) at 4 different ratios such as 0, 2, 4, and 6% on a weight basis. The measured hydraulic conductivities(Ksat) were compared with theoretical hydraulic conductivity (Keff calculated by Jury's equation of effective hydraulic conductivity. In the single layered soil column saturated hydraulic conductivities(Ksat) were significantly decreased with increasing the application rate of compost. In the multi-layered the soil columns Ksat was also decreased with increasing rate of compost and soil depth. Calculated Keff showed the similar results of Ksat as obtained from the measured Ksat, whereas steadily increased with increasing soil depth. Therefore, modification of Jury's equation should be required to adapt theoretical Keff for Held application.

• Journal of the Korean Geographical Society
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• v.35 no.2
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• pp.159-176
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• 2000

본 연구는 남한강 상류의 소지류인 쌍천 유역에 발달한 하성단구의 퇴적물을 모재로 발달한 토양 특성을 조사.분석하였다. 중위 단구의 A1층은 갈색(10YR 4/3)의 미사질토양이고 발달도가 낮은 입상구조이며 B1층은 황갈색(10YR 5/8)의 사질식양토로 아각괴상구조이다. 고위단구의 A1층은 옅은 적갈색(5YR 4/3)의 미사질양토 내지 황갈색(10YR 5/8)의 미사질식토로 발달도가 낮은 아각괴상구조이다. B1층은 적색(2.5YR 3/6)의 사질식토 내지 밝은 적갈색(2.5YR 4/6)의 식양토로 발달도가 양호한 아각괴상구조이다. 고위단구 퇴적층을 모재로 발달한 토양의 구조는 중정도의아각괴상구조이고 조직이 치밀하다. 토양은 A1층, B1층,B2층으로 되어 있으며 또한 B층은 점토가 집적되어 있고 점토 피막이 나타난다. 쌍천의 중위단구상에 발달한 토양은 황갈색토이고 고위 단구상의 토양은 적색토이다. 고위단구 퇴적물을 모재로 발달한 본 적색토는 생성시가가 민델-리스 간빙기의 이전에 생성된 것으로 현재보다 온난한 생물-기후 조건하에서 탈규산화를 동반하는 적색토화작용에 의해 형성된 것으로 추정된다. 고위단구에 발달한 적색토는 토양단면의 형태적 및 물리 화학적인 특성등으로 보아 고적색토로 분류된다.

• Journal of Soil and Groundwater Environment
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• v.13 no.2
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• pp.12-20
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• 2008

This study was conducted to investigate the spatial distributions of chromated copper arsenate (CCA) metals in soils around three log structures and a sound barrier, all built with CCA-treated wood. Sixty-six surface and 35 profile soil samples were collected around the wood structures in addition to 13 background soil samples. The concentrations of chromium, copper, and arsenic in the soil samples collected in the vicinity of the structures were higher than those in the background samples, except in the case of one structure. The concentrations in the surface soils adjacent to the 3-year-old structures seemed to be higher than those in the soils adjacent to the 8-year-old ones. Although the lateral distributions of the metals varied with the structures, chromium and arsenic appeared to show concentration gradients within 20-60 cm and 40-100 cm, respectively. Copper seemed to be the least mobile, displaying concentration gradients only within 20 cm. Even though there were no explicit vertical concentration gradients for any of the metals according to the profile soil sample analysis, chromium and copper seemed to show concentration gradients only up to 5 and 10 cm, respectively, whereas arsenic showed gradients up to 35 cm. At study sites, it was evident that heavy metals leached into soil from CCA-treated wood were confined to neighboring areas both laterally and vertically, and that any plausible ecological impact may occur only within a small range.

• Proceedings of the Korean Society of Applied Pharmacology
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• 1994.04a
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• pp.179-179
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• 1994

새로운 항생물질을 개발하기 위하여 토양으로부터 분리한 균주를 액체 및 고체배지에서 배양하여 여러 검정균에 대하여 종이디스크법으로 항균효력을 조사하였다. 그 결과 (+), G(-), fungi 등에 강한 항균 효력을 보인 토양균 SNUS 8810-43과 Mycobacterium, fungi에 항균력을 보인 토양균 SNUS 8810-129를 선택하여 각각의 배양액에서 항생물질을 분리하고, 분리한 항생물질의 구조를 규명하고자 하였다. 토양균 SNUS 8810-43의 배양액으로부터 항생물질을 분리하기 위하여 양이온 교환 수지 관 크로마토그래피와 셀룰로오스 관 크로마토그래피를 수행하여 시료 JJH-II-46-43을 얻었다. 시료 JJH-II-46-43의 IR, $^1$H-NMR, $^{13}$C-NMR, $^1$H-$^1$H COSY, $^1$H-$^{13}$C COSY, FAB-MS 스펙트럼을 얻어 분리한 항생물질의 구조를 분석하여 이 항생물질의 구조가 N-methylstreptothricin과 동일하다는 것을 확인하였다. Mycobacterium smegmatis에 강한 활성을 나타내는 물질을 토양균 SNUS 8810-129로 부터 분리하였다. 토양균 SNUS 8810-129를 배양한 V-8 아가판을 메탄올로 추출하여 이를 실리카겔 관 크로마토그래피와 preparative TLC로 시료 LCH-IV-17B, LCH-III-387을 얻었다. 시료LCH-IV-l7B, LCH-III-387의 $^1$H-NMR, $^{13}$C-NMR, FAB-MS, CI-MS, IR등의 스펙트럼을 얻어 분리한 항생물질의 구조를 분석하여 이 항생물질이 glycolipid계 항생물질이라는 것을 알았다. $^{13}$C-NMR 상의 자료와 화학적인 방법으로 구성당을 조사한 결과 이 항생물질을 이루고있는 당은 rhamnose 임을 알았다. 또 이 항생물질을 구성하는 지방산은 화학적인 방법과 MS 스펙트럼, $^{13}$C-NMR 스펙트럼으로부터 hydroxydecanoic acid인 것으로 확인되었다. 항생물질 LCH-III-387와 항생물질 LCH-IV-l7B는 각각 rhamnose를 1, 2개 포함하고 있는 것으로 확인되었다. 그리고 동일한 탄소수의 지방산을 가지고 있는 것으로 생각되었다. 이들 항생물질을 이루는 구성당과 지방산간의 정확한 연결및 구조, 생리활성에 관한 연구는 계속 수행중에 있다.

• Proceedings of the KGS Conference
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• 2003.11a
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• pp.89-92
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• 2003

한반도에서는 장마전선이나 태풍으로 인하여 발생된 산사태가 큰 재해의 원인 중에 하나이다. 그러므로 산사태에 대하여 재해를 예측하거나 예방하기 위해서는 그 산사태 발생원인이 밝혀져야 한다. 그러나 산사태 발생원인을 수문학적으로 밝히려고 한 연구 사례는 국내에서는 거의 없다. 그래서 본 연구에서는 산사태를 발생시키는 주요한 영력인 산지유역사면에서 물의 움직임을 알아보기를 위해서 강우유출특성을 밝혔으며 그 특성의 차이에 미치는 토양구조의 영향을 나타냈다. (중략)

• Proceedings of the Korea Water Resources Association Conference
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• 2008.05a
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• pp.1244-1248
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• 2008

지표수-지하수 통합모형인 SWAT-MODLFOW는 토양수가 침루과정을 거쳐 지하수로 유입되는 일방향 구조를 갖고 있어 지하수위 상승 및 하강에 따른 토양수량, 침루량, 중간유출량 등 수문성분량의 변화를 고려할 수 없다. 따라서 본 연구에서는 지하수위 변화에 따른 토양수의 분포양상 변화를 고려할 수 있도록 토양수-지하수간의 연결 구조를 양방향으로 개선하여 두 영역간의 연결성을 강화하였다. 지하수위가 상승할 경우 토양대와 지하수대간의 중첩 영역이 생기게 되는데, 이 중첩 영역을 지하수대로 간주하여 영역 내 흐름거동이 지하수 유동 메커니즘을 따르는 토양수-지하수 결합루틴을 새롭게 제시하였다. 이 결합루틴은 지하수 상승, 하강에 따라 토양수대의 두께가 변하는 가변 토양층 방식(variable soil layer method)으로 계산을 수행할 수 있도록 코드를 구성하였다. 개선된 SWAT-MODLFOW 모형을 무심천 유역에 적용하여 토양수와 지하수간의 상호작용을 해석하고 하천저지대와 같이 지하수위 상승지역에서의 수문성분량의 분포를 보다 현실적으로 구현할 수 있음을 입증하였다.

• Korean Journal of Soil Science and Fertilizer
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• v.16 no.2
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• pp.168-178
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• 1983

Influence of several dehydration treatments on original structure and water behavior in the process of drying were investigated employing three hawaiian volcanic ash soils and four synthetic minerals. These three soils were developed under different rainfall condition and contained three different amount of amorphous materials in them. Measurement of water losses by oven drying at $105^{\circ}C$, $P_2O_5$ drying, freeze drying, and critical point drying revealed that more water losses were noted by oven drying than by three other drying techniques and the differences of water losses between oven and $P_2O_5$-drying were closely related to amoun: of amorphous materials in them, showing the order of Kaiwiki > Hilo > Kawaihae. This indicates that dehydration of amorphous materials by elevated temperature ($105^{\circ}C$) excluded water beyond that in the adsorbed (hygroscopic) state. The effect of dehydration treatments on initial structure was visualized by scanning electron microscopy. The micrographs showed that oven-and $P_2O_5$-dried samples formed into large mass of sub-angular blocky, dense, and closed crumbs, while the freeze dried and critical point dried samples resulted in less shrinkage, and small, fluffy and open spongy structure. However, critical point drying technique produced bulkier, softer, and greater open structure samples than even freeze drying. Additional Index Words: original structure, synthetic minerals, critical point drying, $P_2O_5$ drying. 1. This is a part of author's Ph.D. dissertation submitted to the University of Hawaii, Honolulu, Hawaii 96822 in 1979. 2. Professor of Agricultural Chemistry, Korea University.

• Journal of Korea Soil Environment Society
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• v.4 no.3
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• pp.17-24
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• 1999

The effects of hydrophobic chain length and its structure of nonionic surfactants on surfactant adsorption and contaminated diesel removal were studied in kaolin soil. Hydrocarbon chain length and double bond in hydrophobic tail group of nonionic surfactants affected surfactant adsorption and diesel removal efficiency from kaolin soil. The degrees of surfactant adsorption and diesel removal were closely related each other. Among nonionic surfactants we studied, surfactants with shorter hydrophobic chain length and higher HLB value showed lower degree of adsorption and higher efficiency of diesel removal. The existence of unsaturated carbons in the structure of hydrophobic chain enhanced diesel removal by reducing surfactant adsorption to kaolin soil. The best diesel removal was obtained after adsorption saturation was reached. If surfactant concentration was higher than a critical value, diesel removal was reduced probably because of precipitation. liquid crystal formation, or coacervation of surfactants at high concentration.

• The Journal of Engineering Geology
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• v.33 no.1
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• pp.69-83
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• 2023

Forest fires increase the risk of subsequent soil erosion and mass movement in burned areas, even under rainfall conditions below landslide alert thresholds, by destroying plants and vegetation and causing changes to soil properties. These effects of forest fires can alter runoff in burned areas by altering soil composition, component minerals, soil water repellency, soil mass stability, and soil fabric. Heat from forest fires not only burns shallow organic matter and plants but also spreads below the surface, affecting soil constituents including minerals. This study analyzed X-ray diffraction and physical properties of topsoil and subsoil obtained from both burned and non-burned areas to identify the composition and distribution of clay minerals in the soil. Small amounts of mullite, analcite, and hematite were identified in burned soils. Vermiculite and mixed-layer illite/vermiculite (I/V) were found in topsoil samples from burned areas but not in those from non-burned areas. These findings show changes in soil mineral composition caused by forest fires. Expansive clay minerals increase the volume of soil during rainfall, degrading the structural stability of slopes. Clay minerals generated in soil in burned areas are therefore likely to affect the long-term stability of slopes in mountainous areas.

• Korean Journal of Microbiology
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• v.51 no.1
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• pp.21-30
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• 2015

The goal of this study was to identify relationships between the composition of sulfate reducing bacterial assemblages and terminal restriction fragment length polymorphism (T-RFLP) patterns in rice paddy and dry farming soils. Samples of organic farming soils, conventional farming soils, and dry field farming soils were collected in August and November. Analyses of the soil chemical composition revealed similar total nitrogen, total carbon and total inorganic phosphorus levels; however, the moisture content and total carbon were higher than in the other soils in both August and November, respectively. Sulfate reducing bacteria utilizing lactic acid were more widely distributed than those that used acetic acid, and the number of sulfate reducing bacteria in organic farming soil was most abundant. Phylogenetic analysis based on 181 clones revealed that most showed low similarity with cultured sulfate reducing bacteria, but more than 90% similarity with an uncultured sulfate reducing bacteria isolated from the environment. T-RFLP analysis revealed that fragments of 91, 357, 395, and 474 bp were most common, and the community structure of sulfate reducing bacteria changed seasonally.