• 제목/요약/키워드: Lower Terrace

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Long-Term Investigation of Regional Topographic Effects on Soil Chemical Properties and Heavy Metal Concentrations in Paddy Fields

  • Ahn, Byung-Koo;Kang, Seong-Soo;Shin, Jae-Yeon;Lee, Jin-Ho
    • 한국토양비료학회지
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    • 제45권5호
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    • pp.738-743
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    • 2012
  • Topographic conditions of agricultural fields work as a important factor to identify different soil properties. This study was conducted to investigate the selected soil chemical properties and the concentrations of heavy metals, Cd, Cr, Pb, Cu, Ni, and Zn, in the paddy fields of different topographic areas at four year intervals from 1999 to 2011. Three-hundred soil sampling sites in the paddy fields were selected from the different topographic areas that were local valley and fans, fluvio-marine deposits, alluvial plains, and diluvial terraces. The mean values of soil pH ranged 5.7~5.8 that were within optimal range for rice cultivation. The mean values of other properties such as soil organic matter (SOM) content, the concentrations of exchangeable cations, $K^+$, $Ca^{2+}$, and $Mg^{2+}$, and available silicate concentration were lower or close to the optimal values, but the mean concentrations of available phosphorus were exceeded the range of optimal value, $80{\sim}120mg\;kg^{-1}$, in many paddy fields. In particular, The concentrations of available phosphorus in the paddy fields of local valley and fans, alluvial plains, and fluvio-marine plains were mostly declined. However, in diluvial terrace areas, the phosphorus concentrations unexpectedly increased; furthermore, they were significantly higher than those in other topographic areas. The mean concentrations of 0.1 M HCl-extractable heavy metals, Cd, Cr, Pb, Cu, Ni, and Zn, in the paddy fields were slightly and gradually declined during the study years, but the Pb concentrations were not statistically changed. In addition, the concentrations of heavy metals were widely ranged depending on the different sampling sites. Nevertheless, the concentrations of heavy metals were significantly lower than the levels of Soil Contamination Warning Standard (SCWS) for agricultural lands (1-region) presented in Soil Environment Conservation Law (SECL).

한강 퇴적토의 식재 토양 활용에 관한 기초연구 (A Preliminary Study on Application of Alluvial Deposit in the Han River for Planting Soil)

  • 조용현;김갑수
    • 한국환경복원기술학회지
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    • 제3권4호
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    • pp.60-73
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    • 2000
  • The purpose of the study was to analyze the feasibility of the alluvial deposit deposited on upper terrace in Han River as a substitute for conventional plant soil. For this purpose, the soil characteristics were analyzed, and germination and growth rate of pansy and marigold for 75 days were investigated. Soil contamination level of all the samples, except mineral oil, was analysed under the legal contamination level, while some mineral oil was detected in almost samples at 2.0~32mg/kg. The measures of the soil texture (sandy loam or loam), organic matter (2.5~5.5%), available phosphate (22~98mg/kg), exchangeable cation of K (0.5~1.1cmol/kg), Ca (0.9~9.6cmol/kg), Mg (0.1~0.7cmol/kg), Na (0.7~3.1cmol/kg), CEC (3.1~24.3cmol/kg) were identified as not worse than those of conventional planting soil. But the pH (5.1~5.3) was detected slightly lower than the range (5.5~6.9) of average domestic field soil. The germination rate of pansy in alluvial deposit was lower than that of fertile field or paddy field soil, while the growth rate of pansy for 75 days in alluvial deposit was as good as that of the compared fertile soils. But the germination rate and growth rate of marigold in alluvial deposit were much poorer than those of marigold in compared fertile soils. Consequently, the feasibility of alluvial deposit as a substitute for planting soil was evaluated to be high.

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진천분지 뢰스-고토양 연속층의 형성과 퇴적 환경 (Formation and sedimentary environment of loess-paleosolsequence in the Jincheon Basin, Chungbuk Province, Korea)

  • 윤순옥;박충선;황상일
    • 한국지형학회지
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    • 제20권3호
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    • pp.1-14
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    • 2013
  • 진천분지 하안단구면 상부에 퇴적되어 있는 뢰스-고토양 연속층인 진천단면을 대상으로 형성시기 및 입도조성과 기후변화 등 퇴적환경을 밝혔다. 진천단면은 상부에서 하부로 표층, 뢰스-고토양 연속층, 점이층 I, 점이층 II 그리고 하안단구 자갈층으로 이루어져 있다. OSL 연대측정 결과 뢰스-고토양 연속층은 MIS 6~4에 퇴적된 것으로 판단된다. 연속층은 대자율 변화에 기초하여 4개의 층준으로 구분된다. 입도분석 결과, 진천단면 뢰스-고토양 연속층은 지금까지 한국에서 보고된 뢰스 퇴적층과 입도조성이 유사하다. 특히 Y값은 중국 뢰스고원의 뢰스 및 고토양 층준보다는 작고, Red Clay 또는 양쯔강 하류의 Xiashu 뢰스와 유사하다. 이는 원거리 기원 또는 퇴적 이후 한반도에서 강한 풍화작용을 경험한데 기인한 것으로 생각된다.

지우천 유역의 퇴적지형 연구 (Depositional Landforms in Jiwoo Drainage Basin)

  • 오인순
    • 한국지역지리학회지
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    • 제15권2호
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    • pp.192-203
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    • 2009
  • 본 연구에서는 남강 최상류부의 지우천 유역을 대상으로 침식분지 내 퇴적지형의 형성과정을 고찰하였다. 퇴적 지형의 형태적 특성과 퇴적상 분석을 통하여 밝혀진 형성과정을 요약하면 다음과 같다. 첫째, 사평, 응암, 내동뒷들 지점의 고위퇴적지는 최종빙기 동안의 한랭한 주빙하 환경하에서 젤리플럭션 작용으로 퇴적되었으며, 상류에서 하류방향으로 하상비고가 낮아진다. 고위퇴적지의 범위는 지우천과 남강이 합류하는 곳에서 하류방향 약 1km지점인 것으로 추정된다. 둘째, 장승불들 지점에 분포하는 완경사면의 퇴적물은 심층풍화된 기반암이 완만한 사면을 형성한 이후 최종 빙기 동안 젤리플럭션 작용으로 운반된 것이다. 셋째, 사평, 용추사, 등방들 지점의 저위퇴적지는 후빙기의 온난습윤한 환경하에서 고위퇴적지가 개석되는 동안 퇴적물의 일부가 하상에 남겨지고, 이후 고위퇴적지의 개석이 완료됨에 따라 하천의 저항(퇴적물양)보다 하천의 운반력이 초과함으로써 하상이 다시 침식되어 형성된 것으로 사료된다.

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三陟 五十川 중.하류부의 河岸段丘 지형발달 (The Geomorphic Development of River Terraces along the Middle and the Lower Parts of the Osip-cheon River in Samchok City)

  • 윤순옥;황상일;정석교
    • 대한지리학회지
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    • 제37권3호
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    • pp.222-236
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    • 2002
  • 태백산맥 동사면을 흘러 직접 동해로 유입하는 삼척 오십천의 중.하류부 하안단구는 기후단구와 해면변동단구로 구분된다. 기후단구는 5단이 확인되며, 해면변동단구는 해발고도 145-150m까지 7단의 지형면이 20-30m 간격으로 분포한다. 이와 같은 해면변동단구의 수직적 분포특징은 지반의 지속적인 융기와 기후변화에 의한 빙기와 간빙기의 해면승강작용의 결과이다. 해면변동단구 고고위면은 한반도에서 현재까지 보고된 가장 높은 해안단구보다 해발고도가 더 높다. 해발고도 40m에 분포하는 해면변동단구는 marine oxygen isotope stage 7, 해발고도 70m인 해면변동단구는 stage 9, 해발고도 90m인 해면변동단구는 stage 11, 해발고도 110m 지형면은 stage 13, 해발고도 150m 지형면은 stage 15의 간빙기에 형성된 것으로 추정된다. 중위면, 고위면과 고고위면에는 doline와 함께 uvala와 같은 카르스트지형이 발달하고 있으므로 토지이용과 지형경관이 특징적이다.

한탄강(漢灘江) 일대(一帶)의 지표기복(地表起伏)에 관한 정보(情報) (A Study on the Information of Landforms in the vicinity of the Hantan River)

  • 김주환
    • 동굴
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    • 제72호
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    • pp.19-30
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    • 2006
  • 본 연구의 목적은 한탄강유역의 지질 및 지형정보를 제공하려는 것이다. 추가령 열곡과 관련이 있는 이 지역에는 선지형, 원지형, 차지형으로 구분하는 것이 가능하다. 또한 단구의 분포도 연구지역을 통하여 잘 나타난다. 결론적으로 보면 한탄강 유역에는 화산활동에 의해 용암대지가 형성되었으며 이 지역에 나타나는 백의리층은 용암층 밑의 하상 역을 의미한다. 하계패턴의 발달은 불안정하며, 분기율, 하천길이비율 등은 다른 하천에 비해 낮다. 단구의 높이는 $5{\sim}25m$ 정도이고 대부분이 충적단구이다. 직탕폭포지역은 기반암인 화강암위에 용암대지가 덮혀있다 구침식면지역은 수평용암대지 보다 경사가 급하나 고석정 지역의 지형은 직탕폭포 부근과는 다르다. 기반암이 화강암인 것은 직탕폭포 주변과 동일하나 하천의 횡단면이 비대칭적인 것이 특징이다.

해남 북평면 퇴적층의 특성과 매몰 연대에 대한 연구 (A Study on the Characteristics and Burial Age of Sediment Layers at Bukpyeong myeon, Haenam gun)

  • 신원정;양동윤;김종연
    • 한국지형학회지
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    • 제23권3호
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    • pp.41-55
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    • 2016
  • The granulometric characteristics and chemical composition of the samples from the Bukpyeong myeon, Hainam gun, Jeollanam do were analyzed in this study. The samples were collected from the outcrop of coastal area where the height is about 30m. The burial age of the sediments also estimated by OSL(Optically Stimulated Luminescence) method. The origin and forming processes of the samples are not clear in this stage as limited number of evidences can be found. However it is suggested that the samples are not aeolian deposits originated from chinese loess by the chemical analysis. The mean diameter of samples were $5{\sim}6{\varphi}(silt)$ and are increased slightly downwards. The samples also well sorted. The samples have been heavily weathered by the chemical alteration index. The value of CIA increase downward rapidly at the upper part of outcrop, then stabilized afterwards. The vertical concentration changes ratio of cations varies; Si increases downwards while Fe, Ti, K and Mg decrease. There are fluctuation in concentration ratio of Na and Ca with increasing depth. The burial age of sample from upper part are estimated as $104.52{\pm}4.45ka\;BP$, while that of lower part are $136.10{\pm}6.52ka\;BP$, and they fall in to last part of MS6. The deposition rate for this site is found about 0.017mm/year. The uplift rate of the site is supposed to be 0.24~0.26m/ka with assumption of palaeo-sea level of +6m. However the origin of the sediment deposits should be explored and cleared.

복원된 양재천에서 복원 효과 평가 및 평가 결과에 기초한 개선방안 (An Evaluation on Restoration Effect in the Restored Yangjae Stream and the Improvement Plan Based on the Result)

  • 김아름;김동욱;임봉순;설재원;이창석
    • 생태와환경
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    • 제53권4호
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    • pp.390-407
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    • 2020
  • This study was carried out to evaluate the restoration effect in the restored Yangjae stream and to draw up an adaptive management plan based on the results. As the result of evaluation on the restoration effect, the restored Yangjae stream was evaluated with low naturalness in both terms of the morphology of the stream and the composition and spatial distribution of vegetation. The diverse functional groups were introduced in the vegetation restoration, but the flooding regime, which is significant in the spatial distribution of riparian vegetation, were not correctly reflected. Exotic species or species that were not ecologically suitable for the location were introduced on the embankment and thus a measure to improve those problems is required. As the ecological principle was not reflected in the restoration plan, the stream was constructed as the double terrace structure. Therefore, the width of the waterway was narrowed further, and the waterfront was not designed to accommodate changes from flooding disturbance, making the micro-topography of the stream simpler and the naturalness lower. The adaptive management plan was prepared to improve those problems, and a plan for creating an ecological network was recommended to enhance the restoration effect.

중층형 생활한옥 모델시안 연구 - 청주 서운동의 사례를 중심으로 - (The Tentative Plans of Middle-rise Traditional Houses (Han-ok) Located on Seoun-dong in Urban Area of Cheongju, Korea)

  • 김찬구;김태영
    • 한국농촌건축학회논문집
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    • 제24권2호
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    • pp.21-28
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    • 2022
  • Focusing on the creation of a new han ok, especially a mid-rise hybrid-structured Han-ok, this study proposes a middle-rise (four-story) Han-ok on one and two lots located in Seoun-dong, the existing Han-ok intensive housing site in downtown Cheongju. 1) In terms of layout and function, according to the existing L-shaped Han-ok corresponding to the road and the direction, the parking lots and shops on the 1st floor, the business facility on the 2nd floor, the Han-ok on the 3rd and 4th floors are placed. There are yards, open roof yards, and semi-open Daecheong(大廳, main hall), which can be shared by residents. 2) In terms of structure and form, one or two floors (some 3 floors) are 5.4m square and 5.4×6.6m modules of the RC(Reinforced Concrete) group, and the upper floor reflects the 2.7m module, size and shape of the existing Han-ok. By extending the outer wall of the RC group in the lower floors (1st to 3rd floors) to the wooden exterior of the upper floors (2nd to 4th floors), it is attempted to avoid the awkward appearance of the RC group being exposed to wooden structures. And it is also attempted to reflect the wooden shape and design elements through the elevation elements such as horizontal windows, corner windows, picture frames, and vertical slits. 3) In environmental control and facilities, it is attempted to smooth the ventilation of the building by forming a vertical upward airflow from the dark space of the low floor to the positive of the upper floor. This doubles the effect through a vertical rise of cold air generated in a narrow alleyway, piloti parking lot, and the various voids. In addition to the Daecheong and Numaru(loft) of Han ok, the rooftop yard, the terrace, and the balcony, horizontal natural ventilation is generated through divided doors and transom windows.

소백산맥 북부 지역 하천의 하각률 분포 (Incision Rate Distribution of Streams on the Northern Part of the Sobaek Mountain Range)

  • 이광률;박충선
    • 한국지형학회지
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    • 제27권3호
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    • pp.41-51
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    • 2020
  • This study tried to reveal incision rate distribution of streams on the northern part of the Sobaek Mountain Range with OSL age dating and geomorphic analysis, and factors influencing on the distribution were also discussed. With results from the previous studies, a total of 10 sites from 7 streams in the study area showed the rates ranging from 0.220 m/ka to 0.297 m/ka. Namhan-gang and Geum-cheon indicated the highest and lowest rates, respectively. Both sides in the northern section in the study area showed similar rates, while the western side in the middle section and the eastern side in the southern section showed higher rates than the other sides. Higher rates were also found from the eastern and northern sides where the Range runs N-S and E-W directions, respectively. Certain relationships with altitude and distance from the divide can be recognized from the rates and may be attributed to active incision with altitude and location of the uplift axis near the present divide. The rates on granite and sedimentary rock were higher than those on metamorphic rock, indicating that bedrock type is one of the important factors influencing on stream incision. Tectonic movement seemed to play some roles in the rates, because areas with lineaments showed lower rates. This study suggests that incision rate distribution of streams on the northern part of the Sobaek Mountain Range reflects various local geomorphic and geologic conditions.