• 아시안잔디학회지
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• 제9권1호
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• pp.81-89
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• 1995

The variations of the soil texture, $SiO_2$ /$Al_2$$O_3$ ratio, buffer action, exchangeable base, ex-changeable hydrogen, and mineral nutrients were investigated to estimate the grade of the soil fertility of the soil derived from the different parent rocks such as the granite in Kwangnung and the basalt in Chejudo. The results investigated were showed as follows : Basalt soils in Chejudo belong to sandy clay, light clay and sandy clay loam, while gramite soils in Kwangnung sandy loam. The $SiO_2$ /$AI_2$$O_3$ ratio of the grassland in Chejudo was 1.11 and that of the oak forest soils was 1.24, while granite soils in Kwangnung 1.54 and 1.46, respectively. The buffer actions of ba-salt soils against the N /10 HCI and $Ca(OH)_2$ were stronger than those of granite soils. The $SiO_2$/$Al_2$$O_3$ + $Fe_2$$O_3$ ratios of grassland and oak forest soils of basalt in Chejudo showed 1.10 and 1.24 respectively, while those of the grassland and oak forest of Kwangnung 1.44 and 1.33. The base exchange capacity of basalt soils which has higher value of exchangeable hydrogen was stronger than that of granite soils. But the base saturation of granite soils showed higher value than that of basalt soils. Water contents of basalt soils in Chejudo was lower than that of granite soils fo Kwangnung Basalt soils in Chejudo contain still more humus and total nitrogen than gran-ite soils in kwangnung, The amount of available nitrogen, available phosphorus and exchangeable calcium of granite soils were more than that of basalt soils, Therefore, estimating the soil fertility, granite soils in Kwangnung is higher than that of basalt soils in Chejudo.

• 한국토양비료학회지
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• 제36권3호
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• pp.127-133
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• 2003

토양미생물의 생태적 특성을 평가하기 위해 화강암, 석회암 및 현무암을 모재로 한 12개의 토양통의 미생물적 특성을 조사하였다. 토양미생물상은 토양화학성과 유의한 상관관계를 보였는데, 특히 토양 pH는 형광성 슈도모나스와, 토양 EC는 방선균, 사상균, 중온성 Bacillus 및 호알카리성균과 정의 관계를 보였다. 포자형성균인 Bacillus는 화강암과 현무암에 비해 석회암토양에서 높은 균수를 보였으나, 그람음성균은 모암간에 비슷한 수준을 유지하였다. 화강암유래 토양에서는 Burkholderia, Pseudomonas, Ralstonia가, 석회암토양에서는 Pseudomonas, Burkholderia, Phyllobacterium가, 현무암토양에서는 Burkholderia속이 우점적으로 분포하고 있었다.

• 한국지반환경공학회 논문집
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• 제17권9호
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• pp.29-35
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• 2016

Being mostly made up of highly permeable basalt and volcanic ash soil, Jeju Island's lithosphere characterizes its streams to be dry, flowing only when precipitation is happening. Under this condition, this research was motivated to identify the need of conservation of underground water, which is taking up most of (84% of) Jeju's water usage, and made an attempt to reduce the permeability of stream beds so that it can replace underground water and be used instead. To this end, this study suggested a simple method to make dry streams to carry water all-year-round by reducing permeability of stream floor. The experiment of permeability was performed on the porous basalt and compared it with that of same basalt with volcanic ash soil and Jumunjin sand layer added on top. The results showed a dramatic decrease in permeability of water when both volcanic ash soil and Jumunjin sand is were layered on top of porous basalt. Despite being gained in a controlled environment with a simple test, this result may provide a realistic and effective method of preserving Jeju Island's underground water which ultimately is a method of resolving water related issues.

• 한국토양비료학회지
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• 제46권6호
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• pp.519-524
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• 2013

pH buffer capacities (pHBC, $cmol_c\;kg^{-1}\;pH^{-1}$) of 6 residual Entisols derived from granite, granite-gneiss, limestone, sandstone, shale, and basalt in Korea were studied. Soil acidity may become a problem if the soil pH is reduced to critical levels when nutrient cycles are unbalanced (especially N, C and S). The relation between the pHBC and the physico-chemical properties of the 6 soils was also studied. In the A horizons of all the soils except Euiseong series developed from sandstone, the contents of clay, organic matter and cation exchange capacity (CEC) were higher than those of C horizon, but bulk density and pH were lower than C horizon. Clay content of Euiseong series decreased with soil depth, which might be caused by the elluviation. The soils developed from granite, granite-gneiss and sandstone have a higher $SiO_2$ content than those developed from basalt and limestone. The contents of $Fe_2O_3$ and MgO were high in the soils from developed from basalt, limestone and shale comparing with the soils from granite, granite-gneiss and sandstone. The soils from basalt and limestone showed higher values of ignition loss than those from the other parent rocks. The pHBC of the soils was ranged from 1.8 to 3.2 $cmol_c\;kg^{-1}\;pH^{-1}$ showing as follows : basalt, limestone > shale, granite-gneiss > granite sandstone.

• 한국토양비료학회지
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• 제15권2호
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• pp.89-94
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• 1982

1. 벼수량(收量)에 미치는 인산시용효과(燐酸施用効果)가 현저(顯著)하지 않은 화강암유래(花崗岩由來) 보통답(普通畓)과 시용효과(施用効果)가 현저(顯著)한 현무암유래중점질답(玄武岩由來重粘質畓)에 있어서 담수(湛水)에 따라 용출(溶出)되는 인산염(燐酸塩)을 추정(推定)하기 위해 solubility diagram법(法)을 사용(使用)했다. 2. 토양용액중(土壤溶液中) 인산농도(燐酸濃度), 양(陽)이온농도(濃度), pH치(値)의 담수(湛水)에 따른 변화(変化)를 측정(測定)했다. 그 변화양상(変化樣相)은 어느 토양(土壤)에서도 비슷했다. 보통답(普通畓)의 인산시용구(燐酸施用区), 무시용구(無施用区)의 값은 비슷했으나 중점질답(中粘質畓)에서는 차이(差異)가 보였다. 3. 보통답(普通畓), 중점질답(重粘質畓) 공(共)히 담수(湛水)에 따라 용출(溶出)되는 인산농도(燐酸濃度)는 담수후(湛水後) 얼마동안은 시용인산(施用燐酸)과 토양중(土壤中)알루미늄인산(燐酸)에 의해 지배(支配)되고, 그후 환원발달(還元発達)에 따라 토양중(土壤中) vivianite계(系) 인산(燐酸)에 의해 지배(支配)되는 것으로 추정(推定)되었다.

• Geomechanics and Engineering
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• 제37권1호
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• pp.85-95
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• 2024

This study investigates the influence of nano-silica and basalt fiber content, curing duration, and freeze-thaw cycles on the static and dynamic properties of soil specimens. A comprehensive series of tests, including Unconfined Compressive Strength (UCS), static triaxial, and dynamic triaxial tests, were conducted. Additionally, scanning electron microscopy (SEM) analysis was employed to examine the microstructure of treated specimens. Results indicate that a combination of 1% fiber and 10% nano-silica yields optimal soil enhancement. The failure patterns of specimens varied significantly depending on the type of additive. Static triaxial tests revealed a notable reduction in the brittleness index (IB) with the inclusion of basalt fibers. Specimens containing 10% nano-silica and 1% fiber exhibited superior shear strength parameters and UCS. The highest cohesion and friction angle were obtained for treated specimens with 10% nano-silica and 1% fiber, 90 kPa and 37.8°, respectively. Furthermore, an increase in curing time led to a significant increase in UCS values for specimens containing nano-silica. Additionally, the addition of fiber resulted in a decrease in IB, while the addition of nano-silica led to an increase in IB. Increasing nano-silica content in stabilized specimens enhanced shear modulus while decreasing the damping ratio. Freeze-thaw cycles were found to decrease the cohesion of treated specimens based on the results of static triaxial tests. Specimens treated with 10% nano-silica and 1% fiber experienced a reduction in shear modulus and an increase in the damping ratio under freeze-thaw conditions. SEM analysis reveals dense microstructure in nano-silica stabilized specimens, enhanced adhesion of soil particles and fibers, and increased roughness on fiber surfaces.

• 한국토양비료학회지
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• 제4권1호
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• pp.33-40
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• 1971

Using radioactive $^{40}K$ in potassium, a study was conducted to evaluate the potassium supplying power of different soil types developed on different parent materials. A conversion factor based on two parameters namely $\frac{available\;K_{soil}}{total\;K_{soil}}$ and $\frac{K_{plant}}{K_{soil}}$ was developed and found to be closely related to plant response. According to this characterization soils derived from the various parent materials were ranked as basalt >Silla series>gneiss>porphyry>granite${\gg}$schist. From the point of view of potassium response as measured by yield as similar response pattern was observed. That is, soils derived from basalt to be most responsive as compared to the other soils. The variations among the soils may be accounted for to their potassium bearing mineralogical composition and their stability.

• 한국토양비료학회지
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• 제34권6호
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• pp.373-379
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• 2001

우리 나라 산지토양의 주요 모암에서 발달된 잔적층 암쇄를 대상으로 토양의 단면 특성, 이화학적 특성 X-선 형광분석 (XRF)을 통하여 모재에 따른 토양의 화학조성 변화와 주요한 구성원소의 풍화량을 토양층위 및 모암별로 비교하였다. 모암에 관계없이 토양의 C층에 비하여 A층에서 점토함량, 양이온 치환용량 (CEC), 유기물 함량은 높았으며, 용적밀도 ($kg\;m^{-3}$)와 pH는 낮은 경향을 보였다. 그러나 사암모재의 의성통에서는 점토함량이 감소하였는데 이는 토양과 함께 유실 되었거나 하부로 이동한 것으로 보였다. 토양 중 $SiO_2$함량은 화강암, 화강편마암, 석회암, 혈암 유래 토양에서, $Fe_2O_3$와 MgO는 현무암, 석회암, 혈암 유래 토양에서, CaO는 석회암 유래 토양에서 각각 높았다. 현무암 모재의 구좌통과 석회암 모재의 장성통 토양에서 작열감량(Igniton loss)이 크게 나타났다. 토양 화학성분별 풍화 정도는 공시 토양의 모암에 관계없이 염기이온(K, Ca, Mg, Na)들의 풍화량이 Si, Al, Fe 보다 크게 나타났다. C층과 비교하여 A층의 $TiO_2$의 함량비가 클수록 화학성분의 풍화정도가 큰 토양으로 나타났으며, 이는 $TiO_2$가 다른 원소보다 풍화에 상대적으로 안정된 광물이기 때문인 것으로 보인다. 각 원소의 절대적 함량비를 고려할 때 화강암, 화강편마암, 사암, 혈암, 현무암 유래 토양에서는 Si, Al의 유실이 심했으나 석회암 유래 토양에서는 탄산염의 빠른 풍화로 Ca, Mg이온의 풍화량이 많았다. 화학 성분의 풍회가 큰 토양은 사암 유래 의 성통과 화강암 유래 도산통 >> 혈암 유래 음성통과 석회암 유래 장성통 > 화강편마암 유래 덕산통 > 현무암 유래의 구좌통 순이었다.

• The Korean Journal of Ecology
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• 제7권2호
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• pp.67-73
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• 1983

Jeju-Do is a volcanic island of which climate is very warm and humid, but Opuntia lanceolata Haw, showing CAM metabolism is growing at Wolyung-Ri, Hanrim-Eup, Jeju-Do. Annual productivity of Opuntia was 696.47g/m2/yr and 533.47g/m2/yr at two populations on the seashore respectively and 414.92g/m2/yr on the basalt wall of a village. Stem area index was 13.74, 6.93, and 9.30 at each population which are higher values than average range of leaf area index. The standing crop was the highest at the second cladode from the cladode showed little difference at most chemical properties of P, K, Ca and Na. Total nitrogen contents were the most at the youngest cladode and the lest at the oldest one. Soils were infertile of which organic contents were 1.5% and 5.0% on the seaside and the basalt wall respectively. The soil on the basalt wall contained little water whose water contents were 0.9% and at seashore population 15.12% of water contents were. Furthermore high exchangeable Na contents in soil added waer deficiency.

• 한국토양비료학회지
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• 제5권1호
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• pp.17-23
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• 1972

밭 토양 특히 신 개간지 토양에서 결핍되기 쉬운 무기성분을 종합적으로 함유하는 종합 무기성분 거름을 제조하여 그 비효를 조사하기 위하여 우리나라 주로 모임별 토양을 공시하여 시험한 결과 1. 자실수량은 산성모암인 화강암을 모재로한 토양에서 그도의 종수 효과를 보였으나 염기성 모암인 현무암 및 혈암을 모재로한 토양에서는 그 시용효과가 없었다. 2. 화강암을 모재로한 토양에서는 C.M.F시용량에 비례하여 자실수량이 증가하였으나 현무암 및 혈암토양에서는 C.M.F. 1수준(118.5kg/10a)에서는 약간 증수하는 경향이었으나 2수준(237.0kg/10a)에서는 오히려 감수하는 경향이였다. 3. C.M.F 시용에 따른 식물체중 양분함량변화는 점소는 염기성모암을 모재로한 토야에서는 별 차이가 없으나 산성모암을 모재로한 토양에서는 감소하는 경향이었으며 칼슘함량은 이와 반대의 경향을 보였으며 인산, 마그네슘 및 붕소는 각 토양에서 공히 증가하였고 가리는 화강암을 모재로한 숙전토양에서는 약간 감소하였으며 그외 토양에서는 모두 증가하였다. 또한 이들 양분의 식물체중 흡수량은 C.M.F. 시용으로 각 성분 공히 증가하는 경향이었으며 자실수량과의 관계는 1~5%의 정의 상관관계를 보였다. 4. C.M.F시용에 따른 작물 수확후 토양중 잔류양분함량 변화를 보면 질소 및 치환성 망강 함량은 감소하였으나 pH, C.E.C., $Av-P_2O_5$, Ex-CaO, Ex-MgO 및 수용성 붕소 함량은 현저히 증가하였다. 또한 토양중 잔류된 무기양분 함량과 자실수량과의 관계를 보면 Ex-CaO. 및 Ex-MgO 함량과는 1%수준의 정상관관계를 치환성 망강량과는 1%수준의 부상관관계를 보였다.