• 한국생물공학회:학술대회논문집
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• 한국생물공학회 2002년도 생물공학의 동향 (X)
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• pp.390-393
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• 2002

BTEX가 함유된 groundwater에 에탄올이 첨가된 경우 토양 미생물에 의한 BTEX의 분해는 에탄올이 존재하지 않는 경우에 비해 크게 낮아짐을 알 수 있었다. 이는 토양내 미생물이 에탄올을 우선 이용하며, 따라서 토양내 산소와 mineral의 결핍을 야기하여 BTEX의 분해가 느려짐에 기인한다. 전자수용체로 Fe(III), nitrate, sulfate를 groundwater에 첨가한 경우, BTEX의 분해도는 크게 증가하였으며, sulfate의 효과가 가장 높았다.

• 자원환경지질
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• 제31권5호
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• pp.425-430
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• 1998

The results of radon $(^{222}Rn)$ concentrations and working levels (WL) for forty rooms in Kwanak Campus, Seoul National University on granite bedrock of Jurassic age showed that radon concentration have mean value of 3.0 pCi/L and 0.011 for working level. A number of rooms where these values exceed the EPA's action level are five (13%). It was also suggested that indoor basement rooms in poor ventilation condition can be classified as extremely high radon risk zone having more than 4 pCi/L and 0.020 WL. It was proved that inflow of soil-gas was a primary factor that governs indoor radon level by comparison of soil-gas radon concentrations with indoor radon concentrations.

• 한국유가공학회:학술대회논문집
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• 한국유가공기술과학회 2006년도 제62회 춘계 심포지움 - 친환경유제품 개발과 소비 전망
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• pp.47-56
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• 2006

유기농 제품이 아기에게 더 안전하다는 인식은 유기농 제품에 특별히 영양소가 더 많이 들어 있다는 의미는 아니다. 일부 미네랄 함량은 토양 질에 따라 달라지기 때문에 화학 비료를 많이 사용해서 토양이 오염된 경우 미네랄 함량이 영향을 받을 수 있다. 그러나 비타민, 당질, 단백질, 지질 등 기본적인 영양소는 크게 달라지지 않는다. 그보다 아기의 건강을 위협하는 화학 농약의피해로부터 벗어날 수 있다는 것이 유기농 제품의 가장 큰 장점일 것이다. 이와 같이 소비자들이 바라는 유기농 식품은 안전하고, 믿을 수 있고, 품질이 좋고 건강에 도움이 되며 나아가 환경과 생태계에 도움이 되는 식품일 것이다.

• Journal of Ginseng Research
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• 제7권1호
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• pp.74-79
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• 1983

Effect of soil moisture on content and partition of mineral nutients in panax ginseng (2 years old) was investigated. Similarity was found between N and p, Ca and Mg, K and Fe. Mn and Zn were quite different each other and from others. Nutrient partition was affected more by nutrient content than by dry matter. Under suboptimal moisture condition partition to shoot was inhibited in order of Mg, Zn, Ca, Mg, N and P while accelerated in odor of Fe. K and Mn. Under supraoptimal moisture condition Partition to shoot was inhibited in order of Zn, Fe, K, and Ca, while accelerated in order of Mg, N, Mn and p.

• 아시안잔디학회지
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• 제11권4호
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• pp.281-288
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• 1997

This study was performed to find out the mineral cycles of sulphur in dynamic grassland ecosystems in a steady state condition at the northwest side on Mt. Kwanak. The experimental results may be summarized on the communities of a Zoysia japonica and a Miscanthus sinensis as follows. As compared with some properties of the surface soils among two semi-natural grasslands, sulphur war greater quantity in a Miscanthus sinensis than in a Zoysia japonica on Mt. Kwanak . For the case of steady production and release, the raion of annual mineral production to the amount accumulated on the top of mineral soil in a steady state provides the estimates of release constant k. The release constants on sulphur of the litter were 0.54 in a Zoysia japonica and 0.36 in a Miscanthus sinensis grassland. The half times of S required for the release or accumulation of the litter on the grassland were 1.28 years in a Zoysia japonica and 1.93 years in a Miscauthus sinensis The amounts of annual cycles for sulphur in the grassland ecosystem under the steady-state conditions were 20.65g /$m^2$ in a Zoysia japonica and 26.28g /$m^2$ in a Miacanthus sinensis grassland. Key words: Zoysia japonica Miscanthus sinensis Mt. Kwanak, Sulphur, Mineral cycles.

• 한국토양비료학회지
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• 제43권3호
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• pp.322-328
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• 2010

This study was initiated to investigate the physical and chemical properties of the clay mineral illite and its effect on the growth of cherry tomato (Hongjak) as affected by the forms and concentrations of illite using the bed soil in the glass house. The composition of illite was analyzed by SEM(scanning electron microscope). The cherry tomato was cultivated in the bed soil in the glass house at Chungbuk National University for 10 weeks of total duration. The application rates of illite used as particulate and powder forms were standard 1:20 (w/w), two times 1:10 (w/w), four times 1:5 (w/w) of standard application, respectively. The surface of illite used in the study appeared to be hexagonal sheet and it included K and the variety of other elements. The growth lengths of cherry tomato were 11-23% greater in the pots treated than in the untreated pots. Based on the analyses of the major cations, K, Ca, and Mg from the cherry tomato the amounts of K taken in the leaf and stem of the cherry tomato were 8-45% and 3-30% greater than untreated pots, respectively. The amount of Ca in the leaf and stem taken up by the cherry tomato were 6-39% and 11-40% greater than untreated pots, respectively. The amounts of Mg in the leaf and stem taken up by the cherry tomato were 17-62% and 19-54% greater than untreated pots, respectively. Based on the analysis for the amount of cations, such as K, Ca, and Mg taken up by cherry tomato in treated and untreated bed soil, it appears that the illite treatment enhanced the early growth of cherry tomato.

• 한국환경농학회지
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• 제32권2호
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• pp.102-107
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• 2013

BACKGROUND: Pithy pear fruit are not distinguished externally from sound fruit and thus often cause unexpected economic losses. To find out the cause of pithiness, the pithiness incidence and characteristics of Japanese pear (Pyrus pyrifolia cv. Niitaka) fruit picked from a spot frequently produced pithy fruit in an orchard were compared with those of fruit picked from another spot produced sound fruit every year. And the soil chemical properties of the two spots and mineral contents in fruit, shoots, and leaves of Japanese pear trees cultivated in the two spots were also examined. METHODS AND RESULTS: The pithiness incidence was 0, 8.8, and 11.3% at 7 days before and 0 and 7 days after optimal harvest date, respectively, in the spot frequently produced pithy fruit. Flesh firmness was significantly lower in pithy fruit than in sound fruit, while soluble solids content was slightly higher in pithy fruit than in sound fruit. Unlike other mineral contents, Ca content was significantly lower in pithy fruit than in sound fruit. These results indicate that Ca deficiency in fruit is closely associated with decrease in flesh firmness and thus pithiness development. Ca content in soil of the spot frequently produced pithy fruit was also significantly lower than that in soil of the spot produced sound fruit. However, shoots or leaves did not exhibit significant difference in Ca and/or other mineral contents between the two spots, indicating that Ca deficiency in fruit is dependent on the translocation of Ca within a plant rather than soil Ca status. Although total-N, available $P_2O_5$, K, and Ca contents were significantly lower in soil of the spot frequently produced pithy fruit than in soil of the spot produced sound fruit, Mg and Na contents and pH were not different between the soil conditions. CONCLUSION(S): Fruit maturity and Ca level in fruit are closely related to the incidence of pithiness in 'Niitaka' Japanese pear.

• 한국토양비료학회지
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• 제36권5호
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• pp.311-322
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• 2003

공생균근은 식물 뿌리에 의한 인산 등 무기염류의 흡수를 촉진시키지만 토양의 인산 농도 가 너무 낮거나 높으면 공생균근 형성이 억제되는 것으로 알려져 있다. 본 연구는 화산회토양에서 감귤 뿌리의 공생균근 형성에 적합한 유효인산 수준을 구명하기 위하여 수행하였다. 중과석을 인 공급원으로 하여 인산 시용량을 $0-1000mg\;kg^{-1}$으로 달리한 토양에서 공생균근균 접종과 비접종 처리로 나누어 탱자 유묘를 화분에 심어 유리온실에서 5개월 동안 재배하였다. 탱자 유묘의 공생균근 형성율은 인산 무시용구(유효인산 함량 $0.73mg\;kg^{-1}$)에서 33%이었는데, $50mg\;kg^{-1}$ 시용구(유효인산 함량 $2.6mg\;kg^{-1}$)에서 43%로 증가되었지만 $200mg\;kg^{-1}$ 시용구(유효인산 함량 $8.3mg\;kg^{-1}$)에서는 34%로 무시용구와 비슷하였고 그 이상 인산 시용량이 증가함에 따라 형성율은 오히려 감소하였다. 공생균근균의 접종으로 초장, 생체중 및 건물중 등으로 측정된 탱자 유묘의 생장은 비접종 처리구와 비교하여 모든 인산 처리 수준에서 증가되었으며, 그 증가량은 공생균근 형성율에 비례하였다. 그리고 탱자 유묘의 인산을 비롯한 무기양분 흡수량도 모든 인산 처리 수준에서 공생균근 형성율과 높은 정의 상관관계를 보였다.

• 자원환경지질
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• 제32권6호
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• pp.611-631
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• 1999

Enviromental geochemisty and heary metal contamination at the Kongjueil mine creek were underaken on the basis of physicohemical properties and mineralogy for various kinds of water (surface, mine and ground water),soil, precipitate and sediment collected of April and December in 1998. Hydrgeochemical composition of the water samples are characterized by relatively significant enricant of Ca+Na, alkiali ions $NO_3$ and Cl inground and surfore water, wheras the mine waters are relatively eneripheral water of the mining creek have the characteristics of the (Ca+Mg)-$(HCO_3+SO_4)$type. The pH of the mine water is high acidity (3.24)and high EC (613$\mu$S/cm)compared with those of surface and ground water. The range of $\delta$D and $\delta^{18}O$ values (relative to SMOW) in the waters are shpwn in -50.2 to -61.6% and -7.0 to -8.6$\textperthousand$(d value=5.8 to 8.7). Using computer program, saturation index of albite, calcite, dolomite in mine water are nearly saturated. The gibbiste, kaolinite and smectite are superaturated in the surface and ground water, respectively. Calculated water-mineral reaction and stabilities suggest that weathing of silicate minerals may be stable kaolinite owing to the continuous water-rock reaction. Geochemical modeling showed that mostly toxic heavy metals may exist larfely in the from of metal-sulfate $(MSO_4\;^2)$and free metal $(M^{2+})$ in nmine water. These metals in the ground and surface water could be formed of $CO_3$ and OH complex ions. The average enrichment indices of water samples are 2.72 of the groundwater, 2.26 of the surface water and 14.15 of the acid mine water, normalizing by surface water composition at the non-mining creek, repectively. Characteristics of some major, minor and rate earth elements (Al/Na, K/Na, V/Ni, Cr/V, Ni/Co, La/Ce, Th/Yb, $La_N/Yb_N$, Co/Th, La/Sc and Sc/Th) in soil and sediment are revealed a narrow range and homogeneous compositions may be explained by acidic to intermediate igneous rocks. And these suggested that sediment source of host granitic gneiss colud be due to rocks of high grade metamorphism originated by sedimentary rocks. Maximum concentrations of environmentally toxic elements in sediment and soil are Fe=53.80 wt.% As=660, Cd=4, Cr=175, Cu=158, Mn=1010, Pb=2933, Sb=4 and Zn=3740 ppm, and extremely high concentrations are found are found in the subsurface soil near the ore dump and precipitates. Normalizing by composition of host granitic gneiss, the average enerichment indices are 3.72 of the sediments, 3.48 of the soils, 10.40 of the precipitates of acid mine drainage and 6.25 of the soils near the main adit. The level of enerichment was very severe in mining drainage sediments, while it was not so great in the soils. mineral composition of soil and sediment near the mining area were partly variable being composed of quartz, mica, feldspar, chlorite, vermiculite, bethierin and clay minerals. reddish variable being composed of quartz, mica, feldspar, chlorite, vermiculite, bethierin and clay minerals. Reddish brown precipitation mineral in the acid mine drainage identifies by schwertmanite. From the separated mineralgy, soil and sediment are composed of some pyrite, arsenopyite, chalcopyrite, sphalerite, galena, malachite, goethite and various kinds of hydroxied minerals.

• 지질공학
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• 제32권2호
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• pp.209-219
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• 2022

본 연구에서는 강우에 따른 사면 내 지반특성 변화와 사면붕괴 형상을 실험적으로 규명하기 위하여 인공강우장치와 모형토조를 이용한 실내모형실험을 수행하였다. 이를 위하여 균질한 모래를 대상으로 모형 실험을 수행하였으며, 계측장치를 이용하여 강우침투에 의한 사면 내 포화양상을 조사하였다. 모형사면은 30°의 경사면에 35°의 사면경사로 조성하였고 강우강도는 50 mm/hr를 적용하였다. 토층의 깊이는 모형토조의 크기를 고려하여 35 cm로 선정하고 TDR센서는 깊이별로 설치하여 시간에 따른 지반특성 변화를 고찰하였다. 실험결과 강우 시 모형사면은 강우침투로 인하여 지표에서 지중으로, 선단부에서 정상부로 포화가 진행됨을 알 수 있다. 즉, 강우의 침투로 인하여 사면의 선단부가 먼저 포화되고 이후 지속적인 강우로 인하여 포화의 영역이 사면의 선단부로부터 정상부로 확대됨을 알 수 있다. 모형사면의 붕괴는 사면의 선단부에서부터 붕괴가 시작되어 이후 사면의 정상부로 확장되는 진행성 사면붕괴가 발생되었으며, 최종 사면붕괴시점에서 붕괴면적이 급격하게 증가하였다. 또한 활동면은 원호활동의 형태로 발생되었다. 한편, 사면 내 모관흡수력이 흙-함수특성곡선(SWCC)에서 산정된 공기함입치(AEV)에 이르게 되면 사면붕괴가 발생되는 것으로 나타났다.