• 한국작물학회지
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• 제49권3호
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• pp.194-198
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• 2004

본 연구는 남서해안 간척지에서 토양 염농도(저염; 0.1%, 중염; 0.3∼0.4%)별로 쌀 품질 향상을 위한 적정 질소 시비량을 구명하기 위하여 시험한 결과를 요약하면 다음과 같다. 1.유추분화기의 초장은 질소 시비량이 많을수록 컸고, 토양염농도간에는 저염 토양에서 켰다. 2. 출수기는 저염 토양에서는 표준비인 N20kg/10a에 비해 N8-N16kg/10a까지는 같았으나 N24kg/10a에서는 1일 늦었고, 중염 토양에서는 N8-N16kg/10a 까지는 1일이 삘랐고 N24kg/10a에서는 같았으며, 토양 염농도간에는 저염 토양에서보다 중염 토양에서 4일 정도 늦었다. 3. 질소시비량이 많을수록 간장이 크고, 포장도복이 심했다. 4. 저염 토양에서 질소시비량이 많을수록 $\textrm{m}^2$ 당 립수는 많았으나 등숙비율이 낮아져 발 수량은 N12kg/10a이상에서는 유의차가 없었으며, N12kg/10a이하에서 현미의 완전미율이 높고 단백질 함량이 낮았다. 5.중염 토양에서는 질소시비량이 많을수록 $\textrm{m}^2$ 당 립수가 많고 등숙비율이 비슷하여 발 수량은 질소시비량이 많을수록 높았으나 N20kg/10a 이상에서는 유의차가 없었고, 현미의 완전미율과 단백질함량은 질소시비량간에 비슷하였다. 따라서 남서해안 간척지에서 쌀 수량 및 미질 등을 고려해 볼 때, 저염 토양에서는 N12kg/10a, 중염 토양에서는 N20kg/10a이 적당할 것으로 생각된다

• 한국토양비료학회지
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• 제21권4호
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• pp.443-449
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• 1988

논토양의 질소고정미생물(窒素固定微生物) flora와 그 활성(活性)에 미치는 볏짚 연용효과(連用效果)를 밝히기 위하여 일본 청삼현(靑森縣) 농업시험장내 화학비료연용구(化學肥料連用區) 및 볏짚연용구(連用區) 작토층(作土層)을 공시토양으로 하고 질소시비량(窒素施肥量)을 달리하여 질소고정미생물 flora의 변천(變遷)과 대응하는 질소고정활성의 변화정도를 조사하였다. 1. 시용(施用)볏짚의 광합성미생물(光合成微生物)에 의한 ARA는 양토양(兩土壤) 모두 질소 300ppm 첨가구에서는 3주후(週後)부터, 질소 33ppm 및 무첨가구에서는 시용초기(施用初期)부터 ARA가 현저히 증가하였다. 비광합성미생물(非光合成微生物)에 의한 ARA는 광합성미생물(光合性微生物)에 의한 ARA의 1/10에 지나지 않았다. 2. 시용(施用)볏짚에 서식(棲殖)하고 있는 질소고정미생물 flora를 조사한 결과 초기 3주간에는 양토양(兩土壤) 모두 광합성세균(光合成細菌)(Rhodopseudomonas)이 주로 증식(增殖)하였으며 균량(菌量)과 ARA는 상관관계가 인정되었다. 그후 ARA의 급격(急激)한 증가에 대응(對應)하여 heterocyst형성 염조(鹽藻)의 증식이 현저히 증가하였는데 이상과 같은 효과(效果)는 화학비료연용구(化學肥料連用區) 토양보다 볏짚연용구(連用區) 토양에서 더욱 뚜렷하였다. 3. 염조류(鹽藻類)의 증식(增殖)은 질소시비량에 따라 약간씩 달라 질소 무시용구에서는 Anabaena, Nostoc, Cylindrospermum이 주로 증식(增殖)되었으나 질소 33ppm 시용구에서는 Cylindrospermum, Calothrix, 질소 100ppm 시용구에서는 Calothrix가 왕성히 증식(增殖)되는 경향이었다.

• 상하수도학회지
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• 제11권4호
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• pp.99-109
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• 1997

To estimate the nutrients delivery characteristics of Chogang stream to Keum River, sediment and soil characteristics were analyzed in the stream and in the stream bank. Along the stream, soil samples from river sediment were collected and tested monthly for phosphorus and nitrogen concentrations. Nitrogen concentration in the sediment is much lower than that of soil in the river bank especially in summer presumably due to the high desorption characteristics of nitrogen by the increasing rainfall energy during summer. Instead, the concentrations of phosphorus were similar for the sediment and the soil in the river bank due to the strong adsorption characteristics of phosphorus. Batch tests were performed to evaluate the desorption potential of the sediments. Universal Soil Loss Equation (USLE) was applied to quantify soil erosion in each watershed due to rainfall. It was estimated that approximately 25% of total phosphorus by mass basis could be released from the sediment if the water was disturbed vigorously. The mass load of nitrogen and phosphorus into the Chogang Stream from the watershed were evaluated from the USLE and release ratio of phosphorus.

• 농업과학연구
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• 제50권2호
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• pp.181-192
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• 2023

Appropriate fertilization methods are required according to species to supply necessary nutrients to plants and prevent soil environmental contamination in nurseries. In this study, the effects of nitrogen and phosphorus fertilization on the growth of Liriodendron tulipifera and soil characteristics were investigated. After 16 fertilization treatments (4 levels of nitrogen × 4 levels of phosphorus) were applied to one-year-old L. tulipifera seedlings at the Yongmun Nursery Station of the Korea Forest Service, height, root collar diameter (RCD), biomass, leaf nutrients, and soil characteristics were investigated. The height increased as the amount of nitrogen and phosphorus fertilization increased, and the RCD was the highest in the ×2 treatment. Biomass growth was on average 40.0% higher for the treatment with high nitrogen fertilization compared to the low nitrogen treatment. The seedling quality index was the highest with nitrogen and phosphorus ×2 treatment. Leaf phosphorus and magnesium concentrations decreased when nitrogen fertilization was applied, and leaf potassium concentrations decreased as nitrogen fertilization increased. Soil pH and exchangeable potassium decreased as the amount of phosphorus application increased, and exchangeable magnesium decreased as the amount of nitrogen application increased and increased as the amount of phosphorus application increased. Considering the growth of L. tulipifera seedlings and changes in the soil characteristics at the nursery stage, twice the standard fertilization amount is the appropriate fertilization amount for nursery of the Yongmun Nursery Station. It is expected that this study will contribute to improving nursery soil fertilization management technology for healthy seedling production.

• The Korean Journal of Ecology
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• 제18권3호
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• pp.385-395
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• 1995

Species effects on soil nitrogen mineralization and nitrification in the top 15 cm of soil were evaluated using the buried-bag incubation method in three coniferous plantations in the Kwangneung Experimental Forest, Kyonggi Province. The plantations were established on a similar soil in 1927, and included Larix decidua, Pinus strobus, and Thuja occidentalis. Ten soil samples within each plantation were taken during an entire growing season (May 2~Oct. 30, 1994). Mean daily nitrogen mineralization rates during 45-day in situ soil incubations were significantly different among species and incubation dates. Growing season nitrogen mineralization also differed significantly among species and ranged from 47.7 mg N/kg soil for Larix decidua to 21.5 ma N/kg soil for Thuja occidentalis. Growing season nitrification differed significantly among species and comprised from 93% to 100% of the total growing season nitrogen mineralized. We speculated that organic matter contents and quality might control nitrogen mineralization and nitrification in these soils.

• 한국작물학회지
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• 제46권2호
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• pp.145-149
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• 2001

This study was performed to evaluate the growth and nodulation characters of hypernodulating soy-bean mutant, SS2-2, and to know the growth and yield performance of the mutant in infertile soil. Soil fertility was adjusted by mixing the different ratios of soil components including clay, river sand, and horticultural bed, which resulted in fertile and infertile soil. Dry weight, nitrogen concentration, and leaf nitrate reductase of each plant were measured around V6 stage (47 days after planting) and around R3 stage (82 days after planting). There were significant effects of soil fertility and soybean genotype on the total dry weights including root, nodule, stem, leaf, and pod dry weight at V6 and R3 stages. Total dry weight of hypernodulating mutant, SS2-2, was clearly less than that of its wild type, Sinpaldalkong 2. However, nodule development on the roots of SS2-2 was much greater than that of Sinpaldalkong 2, regardless of soil fertility. Though SS2-2 was smaller in plant size than Sinpaldalkong 2, genotypic difference in total nitrogen content was not significant at both V6 and R3 stages because SS2-2 fixed more nitrogen biologically than its wild type in the root nodule. The SS2-2 mutant showed lower plant yield in both infertile and fertile soil. The SS2-2 contained more crude seed protein than Sinpaldalkong 2, and was characterized with reduced top and root growth.

• 한국환경농학회지
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• 제38권4호
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• pp.262-268
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• 2019

토양에서 유기자원의 무기화 특성을 구명하기 위하여 질소함량별로 볏짚, 우분퇴비, 균배양체, 유박, 아미노볼 등 총 5가지를 각각 처리하여 128일 동안 실내 항온배양실험을 실시하였으며, 이 분석결과를 질소 무기화 모형에 적용하여 유기자원의 질소 무기화 양상을 구명하였다. 항온배양 기간 동안 유기자원의 질소 순 무기화율은 질소함량이 가장 높은 아미노볼에서 가장 높았고, 질소함량이 가장 낮은 볏짚에서 가장 낮았다.잠재적 질소 무기화율은 전질소 함량과는 양의 상관관계(0.96)가 인정되었다. 무기화 속도상수 k는 유기자원의 유기물(-0.96) 및 탄소함량(-0.97)과 음의 상관관계가 인정되었다. 모형에 의해 추정된 1작기 동안의 질소 무기화율은 볏짚 6.6%, 우분퇴비 11.6%, 균배양체 30.9%, 유박 70.7%이었으며 아미노볼은 81.0%를 나타냈다. 질소 무기화율은 유기자원의 종류 또는 질소함량에 따라 다르게 나타나 질소 무기화율을 유기자원의 질소 공급 특성을 결정하는 지표로 사용할 수 있다. 질소함량이낮거나 발효과정을 거치는 퇴비 등의 유기자원은 퇴비화 과정에서 유기태 질소가 안정화되어 질소의 무기화율이 무발효 유기자원보다 낮으므로 시비량 결정시 양분공급의 목적보다는 토양 물리성 개량을 목적으로 사용하는 것이 바람직하다.

• The Korean Journal of Ecology
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• 제19권2호
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• pp.179-189
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• 1996

Growth and nitrogen retention of Persicaria thunbergii were investigated in the wetland microcosms which contained the plants growing on soil bed. Nitrogen solution was supplied to the microcosms with the same amount of $NH_4^{+}-N\; and\; NO_3^{-}-N$ at the rates of 0.00, 0.78, 1.57, 3.14g $N{\cdot}m^{-2}{\cdor}wk^{-1}$ from May 1 to August 31, 1995. The solution was detained for 5 days to react with soil and plant and then allowed to leach. The contents of NH_4^{+}-N\;and\; NO_3^{-}-N$ in the leachate, total Kjeldahl nitrogen, plant biomass, and soil characteristics were determined. Nitrogen retained by plant was estimated as the increment of TKN in plant biomass. The addition of 0.78 and 1.57g $N{\cdot}m^{-2}{\cdot}wk^{-1}$ resulted in significant increase of plant biomass. However, plant growth was inhibited when nitrogen was added at the rate of 3.14g $N{\cdot}m^{-2}{\cdot}wk^{-1}$. Overall, the plant biomass was positively correlated with the amount of nitrogen retained by plant and soil system. The amounts of $NO_3^{-}-N$ leached from the microcosms were 5~10 times higher than those of $NH_4^{+}-N$. While total nitrogen added ranged from 143.2 to 576.5g $N/m^2$, total leaching loss of inorganic nitrogen and nitrogen retained by plant was as little as 1.04~22.71g $N/m^2$, and 5.46~12.91g $N/m^2$, respectively. Then, the plant seemed to contribute to KDICical and microbial immobilization of nitrogen in the soil. Finally, it is suggested that a large portion of nitrogen added was lost into the air by denitrification and volatilizaton, and / or leached in organic forms.

• 한국작물학회지
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• 제44권1호
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• pp.1-3
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• 1999

This study was carried out to determine the effects on rice growth, yields and soil improvement under the different nitrogen levels in machine-transplanted rice after plowing at the fruiting stage of milk vetch. The fresh weight of milk vetch at plowing time was 20.95 ton/ha. In dry weight, T-N and C/N were 1.58%, 21.8%, respectively. Organic matter, total nitrogen and exchangeable calcium of soil after the experiment in the plot of milk vetch were higher than those before the experiment. Leaf area and dry weight of rice plants at heading date increased as nitrogen level increased. The number of panicle and spikelets per $\textrm{m}^2$were not different except for the 110 kg/ha nitrogen level plot with milk vetch. Brown rice yield ranged from 5.45 to 6.08 ton/ha, in creasing with increased nitrogen level. So the yield increased by 1% at 77 kg/ha nitrogen level, 7% at 110 kg/ha nitrogen level plot with milk vetch compared with conventional level (rice straw 5.4 ton/ha and nitrogen 110 kg/ha).

• 한국환경농학회지
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• 제37권3호
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• pp.166-171
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• 2018

중량식 라이시미터를 활용하여 배추 재배 중 식양토와 사양토의 질소 용탈과 질소 수지를 평가하였다. 생육 초기인 9월 초 강우로 인해 식양토와 사양토 모두 토심 150 cm 이하로 배수가 있었다. 식양토는 점토의 수축 및 작물 뿌리 등에 의해 형성된 대공극을 통해 일시적으로 배수량이 증가하였으나, 사양토는 식양토와 달리 강우량에 따라 일정하게 배수량이 증가하고, 감소하였다. 토성별로 질소 용탈량을 분석한 결과, 식양토에서는 비료의 용탈이 거의 없는 반면, 사양토에서는 식양토에 비해 5배 많은 질소 용탈이 있었다. 질소수지에서 작물 흡수량에 비해 질소 용탈량이 차지하는 비율은 적었으나 식양토에 비해 사양토에서의 용탈량이 많아 질소 수지 산정에 토성에 따른 용탈특성을 고려할 필요가 있다.