• 한국제4기학회지
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• 제9권1호
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• pp.43-60
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• 1995

The Kanweoldo Deposit in the Cheonsoo Bay western coast of Korean Peninsula is considered to be influenced by severe freezing condition under cold humid environment of the last glacial age. The evidence of severe freezing in the some upper part of the fine-grained Kanweoldo Deposit is characteristically irregular wavy la-mellar structure with the interval of 2∼8mm. In particular lamina show very compacted fabrics composed of rounded or spheroidal discrete aggregates covered by silt caps. Such laminar structure and associated micro-fabrics might owe to soil freezing such as ice segregation in lens form cryophoresis pressure from growing ice and disturbance by frost-creep. Furthermore pedogenesis of cold-humid type such as gleyzation or peseudo-gleyzation also might af-fect the kanweoldo Deposit in the priod of severe cold-humid cli-mate of the Wrm. The Kanweoldo sediment and organic remnant(16,708 B.P. with error limit of 250 years) affected by severe cryogenic activities sug-gest that the paleoclimate of Late Wrm in Korea might be so cold and humid as to engender the cryogenic structure in subaerial silty and sandy silt deposits.

• Journal of the korean society of oceanography
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• 제32권3호
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• pp.120-127
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• 1997

Depositional environment off the Shihwa Dam has been studied to investigate the change of sedimentation process and the pollution. In order to understand how the sediments are distributed, polluted and modified, depositional factors have been analyzed and compared with the previous data. Study area, located off the Shihwa Dam, was surveyed to collect 25 bottom samples and 2 cores in 1996 and echo-sounding in 1997. These sediments were analyzed for the study of the global characteristics of sediment such as grain size and organic matter. Among these samples, the selected twenty surface sediments were analyzed for the comparison with their contents of metallic elements (Al, Mn, Fe, V, Cr, Co, Ni, Cu, Zn, Cd, Pb, As). According to field and lab analysis of sediments, three sedimentological zones have been generally identified around study area; near the dam (sandy Silt), near the dike (Sand) and offshore (silty Sand) zones. Textural parameters show that the content of silt and clay is dominant near the dam excepting the dike zone of LNG Storage Base and offshore (Palmido). The total concentration of Mn, Ni, Fe, Zn and Cd in bulk sediments was increased after the construction of the dam, while the content of Mn and Cr were higher near tidal channel than in the offshore area. Meanwhile, the annual increasing pattern of some heavy metal has appeared in this area. Based on this primary study, modification of the depositional environment may be caused by the construction of the dam and LNG Storage Base. Additionally, environmental evaluation on organic/inorganic factors has been suggested for interpreting environmental changes caused by coastal development in the nearshore such as the Shihwa coastal area.

• 광물과 암석
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• 제33권3호
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• pp.153-163
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• 2020

우리나라 제4기 고환경 변화 특성 규명을 위하여 수원시의 편마암 및 화강암 풍화대를 피복하는 적갈색 점토-실트 퇴적물 2개 단면(~3.5 m)에 대하여 광물 및 지화학 분석을 실시하였다. 퇴적층은 광물조성과 화학조성의 수직 변화를 기준으로 4개의 퇴적층(Unit 1-4)으로 구분되었다. 최하부 Unit 1은 K-장석 함량이 높은 사질 퇴적물로서 기반암 풍화물의 기여도가 높다. Unit 2는 전이층이며, Unit 3은 적갈색 점토-실트질 퇴적물로서 총점토 함량이 평균 58%이며, 주요 점토광물은 일라이트-스멕타이트 혼합층 광물과 수산기삽입질석/스멕타이트이다. Unit 3에는 사장석이 거의 함유되어 있지 않은 반면에, 그 풍화물인 고령토 광물의 함량이 다른 층들보다 높다. Unit 4는 전반적 광물조성과 화학적 특성이 Unit 3과 유사하나, 사장석과 녹니석의 함량이 더 높고 고령토 광물의 함량은 더 낮다. 단면내 화학성분 변화를 국내 타지역 적갈색 점토-실트층과 비교한 결과, Unit 3과 4는 풍성퇴적물의 범위에 포함되었다. 이 지역 퇴적 단면에서 고환경변화는 다음과 같이 해석된다. 기반암인 편마암과 화강암 풍화물이 침식되어 주변부에 사질 퇴적물로 퇴적되어 하부층(Unit 1, 2)을 이루고, 그 위에 빙하기의 점토-실트질 풍성퇴적물층(Unit 3)이 퇴적되었다. Unit 3은 간빙기의 풍화작용으로 풍화되어 전체적으로 적갈색 토양화되었다. 그 후 다시 빙하기로 접어들면서 최상부에 풍성퇴적물층(Unit 4)이 퇴적되었다.

• 한국산업융합학회 논문집
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• 제20권5호
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• pp.395-404
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• 2017

Cultivating soybeans in rice paddy field reduces labor costs and increases the yield. Soybeans, however, are highly susceptible to excessive soil water in paddy field. Controlled drainage system can adjust groundwater level (GWL) and control soil moisture content, resulting in improvement soil environments for optimum crop growth. The objective of this study was to fit the soybean growth data (canopy height and stem diameter) using Gompertz model and Logistic model at different GWL and validate those models. The soybean, Daewon cultivar, was grown on the lysimeters controlled GWL (20cm and 40cm). The soil textures were silt loam and sandy loam. The canopy height and stem diameter were measured from the 20th days after seeding until harvest. The Gompertz and Logistic models were fitted with the growth data and each growth rate and maximum growth value was estimated. At the canopy height, the $R_2$ and RMSE were 0.99 and 1.58 in Gompertz model and 0.99 and 1.33 in Logistic model, respectively. The large discrepancy was shown in full maturity stage (R8), where plants have shed substantial amount of leaves. Regardless of soil texture, the maximum growth values at 40cm GWL were greater than the value at 20cm GWL. The growth rates were larger at silt loam. At the stem diameter, the $R_2$ and RMSE were 0.96 and 0.27 in Gompertz model and 0.96 and 0.26 in Logistic model, respectively. Unlike the canopy height, the stem diameter in R8 stage didn't decrease significantly. At both GWLs, the maximum growth values and the growth rates at silt loam were all larger than the values at sandy loam. In conclusion, Gompertz model and Logistic model both well fit the canopy heights and stem diameters of soybeans. These growth models can provide invaluable information for the development of precision water management system.

• 한국습지학회지
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• 제13권2호
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• pp.243-263
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• 2011

시화호 형도 근처 조간대(帶, intertidal zone) 지역 갯벌의 퇴적환경을 알아보기 위해 10개 정점 표층 및 2개 정점 주상퇴적물에 대한 입도, 함수율, 휘발성산화합물(Acid Volatile Sulfide; AVS), 총유기탄소(Total Organic Carbon; TOC) 및 중금속(Al, Fe, Mn, Cu, As, Pb, Zn, Ni, Cd 및 Cr) 항목에 대해 분석 하였다. 표층 퇴적물은 대체로 분급이 불량(분급도, 0.60~2.31${\phi}$)한 sandy Silt, slightly gravelly muddy Sand, silty Sand 및 Sand 등의 퇴적상으로 구분되며, 평균입도는 2.95~6.00${\phi}$로 극조립 실트(Silt)에 해당한다. 표층 퇴적물의 Al 함량은 1.54%, Fe은 1.75%, Cu는 9.1ppm, As는 1.1ppm, Pb은 18.8ppm, Ni은 11.0ppm, Cd은 0.02ppm 그리고 Cr은 30.1ppm으로 측정되었으며, 주상 퇴적물 또한 미국해양대기청(National Oceanic and Atmospheric Administration; NOAA) 기준의 ERL(Effective Range Low, 저서생물에 독성을 보이는 초기 10% 농도)을 초과하지 않았다. 주상퇴적물의 과잉 방사능 납($^{210}Pbex$)의 분포를 통해 퇴적률을 추정한 결과, 급격한 퇴적물의 다량유입에 의해 수직적으로 방사능(activity)이 유사한 값을 나타내고 있어 정확한 퇴적률(apparent sedimentation rate)은 추정할 수 없었다. 그러나 2개 코어 상부 35cm 에서 퇴적물의 급격한 유입 및 환경적 영향등으로 금속 농축계수(Enrichment factors; EF) 계산값은 비교적 높게 나타났다.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2003년도 총회 및 춘계학술발표회
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• pp.418-421
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• 2003

Surfactant enhanced in-situ soil flushing was peformed to remediate the soil and groundwater at an oil contaminated site, and the effluent solution was treated by the chemical treatment process including DAF(Dissolved Air Flotation). A section from the contaminated site(4.5m$\times$4.5m$\times$6.0m) was selected for the research, which was composed of heterogeneous sandy and silt-sandy soils with average Hydraulic conductivity of 2.0$\times$10$^{-4}$ cm/sec. Two percent of sorbitan monooleate(POE 20) and 0.07% of iso-prophyl alcohol were mixed for the surfactant solution and 3 pore volumes of surfactant solution were injected to remove oil from the contaminant section. Four injection wells and two extraction wells were built in the section to flush surfactant solution. Water samples taken from extraction wells and the storage tank were analyzed by GC(gas-chromatography) for TPH concentration with different time. Five pore volumes of solution were extracted while TPH concentration in soil and groundwater at the section were below the Waste Water Discharge Limit(WWDL). Total 18.5kg of oil (TPH) was removed from the section. The concentration of heavy metals in the effluent solution also increased with the increase of TPH concentration, suggesting that the surfactant enhanced in-situ flushing be available to remove not only oil but heavy metals from contaminated sites. Results suggest that in-situ soil flushing and chemical treatment process including DAF could be a successful process to remediate contaminated sites distributed in Korea.

• Geomechanics and Engineering
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• 제16권5호
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• pp.547-558
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• 2018

Studies of soil dynamic properties in Malaysia are still very limited. This study aims to investigate the dynamic properties of two selected tropical residual soils (i.e., Sandy Clay and Sandy Silt) and a sand mining trail (Silty Sand) in Peninsular Malaysia using 1g shaking table test. The use of 1g shaking table test for soil dynamic testing is often constrained to large strain level and small confining pressure only. Three new experimental setups, namely large laminar shear box test (LLSBT), small chamber test with positive air pressure (SCT), and small sample test with suction (SSTS) are attempted with the aims of these experimental setups are capable of evaluating the dynamic properties of soils covering a wider range of shear strain and confining pressure. The details of each experimental setup are described explicitly in this paper. Experimental results show that the combined use of the LLSBT and SCT is capable of rendering soil dynamic properties covering a strain range of 0.017%-1.48% under confining pressures of 5-100 kPa. The studied tropical residual soils in Malaysia behaved neither as pure sand nor clay, but show a relatively good agreement with the dynamic properties of residual soils in Singapore. Effects of confining pressure and plasticity index on the studied tropical residual soils are found to be insignificant in this particular study.

• Geomechanics and Engineering
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• 제32권4호
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• pp.445-452
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• 2023

Temperature is one of the important factors affecting the permeability of water in the soil. In the present study, the impact of water temperature on hydraulic conductivity (k) with and without coarse aggregations by considering six types of soils was analyzed. Moreover, the effect of sand and gravel presence in the soil was investigated through the infiltration based on constant and inconstant water head experiments. Results indicated that by increasing the water temperature, adding gravel to sandy soil caused the hydraulic conductivity to raise. It is supposed that the gravel decreased the contact surface between the water and the soil aggregates. It is deduced that due to decreasing kinetic energy, k tends to have lower values. Furthermore, adding the sand to sandy silt-clay soil showed that the sand did not have a marginal effect on the variation of k since the added sand cannot increase the contact surface like gravel. Finally, increasing the main diameter of the soil will increase the effect of the water temperature on hydraulic conductivity.

• 한국해양학회지
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• 제28권3호
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• pp.241-258
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• 1993

우리 나라 서남해안의 임자도와 낙월도 주변해역은 해안선의 굴복이 매우 복잡하 며 북동-남서 방향으로 대상의 사퇴가 잘 발달되어 있어 이 해역에 분포하는 표층퇴적 물의 특성과 퇴적환경을 규명하기 위해 총 40개소에 걸쳐 채니기 등으로 시료를 채취 하여 퇴적학적 및 미고생물학적 연구를 수행하였다. 연구해역은 퇴적물의 입도 분포상 니질 사 역 퇴적상, 사 퇴적상, 실트질 사 퇴적상, 사질 실트 퇴적상, 실트 퇴적상의 5개 퇴적상으로 분류되었으며, 표층퇴적물의 입도분석 결과 평균입도, 분급도, 왜도 및 첨도 등은 광역적으로 산포되는 경향을 보였지만 그 입도특성은 일반적으로 천해퇴 적상이 지니는 특징에 해당되는 것으로 나타났다. 연구해역의 퇴적물 중 사질퇴적상을 보이는 부분에서 산출된 석영립들을 전자현미경으로 관찰한 결과 이들은 대체로 고에 너지 환경에서 생성되었으며 한때는 대기 중에 노출되었을 가능성 등이 시사되며 전체 적으로 연구해역에 분포하는 퇴적물 중에는 다양한 기원의 쇄설성 입자들이 혼재된 것 으로 해석된다. 연구해역에서 산출된 규편모류와 mammoplankton은 각각 1속 6종과 5속 5종이 산출되었는데 이들 미생물 유해들의 군집 분석 결과 연구해역의 퇴적물들은 온 난수괴의 영향아래 퇴적물의 재동현상이 비교적 활발히 일어나고 있는 것으로 추정된 다. 또한 유기물 및 탄산염의 함량과는 뚜렷한 상관관계를 설정하기는 어려웠다.

• 한국토양비료학회지
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• 제48권4호
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• pp.240-245
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• 2015

The monitoring of soil fertility changes in orchard is very important for agricultural sustainability. Field monitoring was performed to evaluate the soil chemical properties of 140 orchard (23 sites for sandy loam, 88 sites for loam, 28 sites for silt loam, and 1 site for loamy fine sand) in Gyeongnam province every 4 years from 2002 to 2014. Soil chemical properties such as pH, electrical conductivity, amount of organic matter (OM), available phosphate ($P_2O_5$), lime requirement (LR), exchangeable potassium (K), calcium (Ca), magnesium (Mg), and sodium were analyzed. The amount of OM, exchangeable K, Ca, and Mg were significantly increased as cultivation year increases. The frequency distribution within optimum range of subsoil chemical properties in 2014 was 34.3% for pH, 35.0% for OM, 17.1% for available $P_2O_5$, 22.9% for exchangeable K, 15.7% for exchangeable Ca, and 22.1% for exchangeable Mg. In addition, the available $P_2O_5$ and exchangeable calcium were excess level with portions of 69.3% and 48.6%, respectively. The soil chemical properties in the topsoil and subsoil showed that soil pH was significantly higher in sandy loam soil than those from the loam and silt loam soils. The OM, exchangeable K, Mg, and LR of loam soil were higher than those from the sandy loam soil. These results indicated that a balanced management of soil chemical properties as affected by soil texture can improve the amount of fertilizer applied for sustainable agriculture in orchard field.