• The Korean Journal of Ecology
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• 제27권3호
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• pp.155-159
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• 2004

In order to gain a better understanding of how forests participate in the cycling of carbon, effects of nitrogen addition on soil respiration were investigated on the oak forest in Kongju, Korea. Study site was divided into control, treatment f and treatment 2 plots, with 5 replication in each plot. In each replicate of treatment 1 and treatment 2 were fertilized with ammonium nitrate (NH$_4$NO$_3$), 30 g/$m^2$ and 60 g/$m^2$, respectively. Soil respiration, soil temperature, ammonium-N and nitrate-N were measured during the experimental period. Ammonium-N and nitrate-N in Ta were higher than those in control and T$_1$. Ammonium-N and nitrate-N in top-soil and sub-soil decreased sharply in August after bi9 rainfall in July in T$_1$ and T$_2$, however, those in control plot increased. Soil respiration in T$_2$ Plot showed consistently higher than those in control and T$_1$ until the end of July. However, soil respiration was similar among the control, T$_1$ and T$_2$ in mid-August and September The amount of Co$_2$ released from soil respiration in control, T$_1$ and T$_2$ in mid-August was 8.0$\pm$0.4, 9.3$\pm$0.6 and 10.2$\pm$0.5 $\mu$mol$^{-1}$ ㆍm$^{-2}$ ㆍs$^{-1}$ , respectively. However, those in control, T$_1$ and T$_2$in mid-August was 13.0$\pm$0.4, 13.5$\pm$0.5, 13.3$\pm$0.6 $\mu$mol$^{-1}$ ㆍm$^{-2}$ ㆍ$^{-1}$ , respectively. The results suggest that nitrogen addition in this oak forest has a positive effect on soil respiration.

• 한국토양비료학회지
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• 제29권4호
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• pp.353-359
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• 1996

돈분(豚糞)에서 유래(由來)한 질소의 토양 중 행동을 구명하고자 사양토와 양토를 공시하여 무저(無低) PVC 포트(직경 20cm, 높이 100cm) 조건에서 토양침투수 채취용 ceramic cup tube를 설치하고 시험을 실시하였다. 가축분은 생돈분과 발효돈분을 공시하여 0, 50, 100톤/ha수준으로 처리하였으며 옥수수재배에 의한 질산태질소 이동에 미치는 요인분석을 위하여 양토(壤土)에 한하여 옥수수를 공시 작물로 재배하면서 나지구(裸地區)와 비교(比較)하였다. 토양깊이 90cm에서 채취한 침투수의 질산태질소 농도는 돈분시용량이 많을수록 증가하였고 토성별(土性別)로는 사양토 보다 양토에서 돈분(豚糞)의 부숙상태별로는 생돈분에 비하여 발효돈분에서 높았다. 옥수수 재배지에서 침투수의 질산태질소 농도는 동일량의 돈분이 처리된 나지구에 비하여 64.6-68.9% 가 감소되었다. 침투수에 양(陽)이온들의 농도는 돈분시용량이 많을수록 증가하였으며 옥수수 재배구에서는 침투수의 양이온 농도가 나지에 비하여 현저히 감소되었다. 침투수(浸透水)에 질산태질소(窒酸態窒素) 농도가 증가할수록 Ca, Mg, Na 농도는 증가하여 이들 양이온들이 돈분유래 질산태질소와 동반용탈(同伴溶脫)되는 경향을 보였다. 침투수(浸透水)의 질산태질소 당량에 대한 양이온들의 당량비는 돈분시용량이 많을수록 증가하였으며 사양토(砂壤土) 양토(壤土) 공히 돈분시용량이 많을수록 심토 중에 질산태질소 농도가 증가되었다.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2003년도 총회 및 춘계학술발표회
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• pp.107-110
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• 2003

Reduction of nitrate by zero valent iron (Fe$^{0}$ ) has been previously studied, but the proper treatment for the by-product of ammonium has not been reported. However, in terms of nitrogen contamination, ammonium may be regarded as another form of nitrogen contaminants since it can be oxidized to nitrate again under aerobic conditions. This study is focused on simultaneous removal of nitrate and its by-product of ammonium, with the ZanF (Zeolite anchored Fe), a product derived from zeolite modified by Fe(II) chloride followed by reduction with sodium borohydride. Batch experiments were performed without buffer at two different pH condition with ZanF, iron filing, Fe(II)-sorbed zeolite, and pure zeolite to estimate the nitrate reduction and the ammonium production. At higher pH, removal rate of nitrate was reduced in both ZanF and iron filings. ZnF removed 60 % of nitrate at initial pH of 3.3 with no production of ammonium, while iron filing showed equivalent production of ammonium to the reduced amount of nitrate. In terms of nitrogen contamination, ZanF removed about 60 % and 40 % at initial pH of 3.3 and 6, respectively, while iron filing presented negligible removal against total nitrogen including nitrate and ammonium.

• 한국토양비료학회지
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• 제25권2호
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• pp.168-174
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• 1992

밭토양(土壤)의 심층(深層)에 용탈집적(溶脫集積)되어 있는 nitrate를 작물(作物)이 이용(利用)할 때 이의 흡수(吸收)를 저해(沮害)하는 토양성분(土壤成分)을 찾고 그 요인(要因)을 구명(究明)하기 위하여 먼저 토양심도별(土壤深度別)로 nitrate와 chloride를 비롯한 몇가지 토양성분(土壤成分)들의 분포(分布)를 조사(調査)하였다. 1. 토심(土深) 150cm까지 몇가지 토양성분(土壤成分)들의 분포(分布)를 조사(調査)한 결과(結果) T-N함량(含量)은 표토(表土)에서 많았다가 하층(下層)으로 갈수록 적어졌고, nitrate의 함량(含量)은 아래로 갈수록 적어지다가 토심(土深)110cm부터는 다시 증가(增加)하여 nitrate의 용탈(溶脫) 집적현상(集積現象)을 보였다. 2. $^{15}N$의 천연함량비율(天然含量比率)인 T-N과 nitrate의 ${\delta}a^{15}N$ 값은 하층(下層)으로 갈수록 높아졌고 다른 보문(報文)의 토양(土壤)들에 비(比)하여 높은 편이었다. 그러나 조사포장내(調査圃場內)에서 이들의 변이(變異)는 크지 않았다. 3. chloride함량(含量)과 EC값은 nitrate가 집적(集積)된 하층(下層)으로 갈수록 급격(急激)히 높아져 chloride와 염기(鹽基)들이 용탈집적(溶脫集積)되었음을 알 수 있었고 이들 간(間)에는 고도(高度)의 정(正)의 상관(相關)이 있었다.

• 한국지하수토양환경학회지:지하수토양환경
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• 제29권1호
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• pp.18-27
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• 2024

In this study, the pump and fertilize (PAF) was applied to reduce nitrogen infiltration into groundwater at three corn cultivation sites over a three-year period, and its effectiveness was evaluated. PAF involves pumping nitrate-contaminated groundwater and using it for irrigation, thereby replacing the need for chemical fertilizers. This method not only substitutes chemical fertilization, but also reduces nitrogen infiltration into groundwater through root zone consumption. To confirm PAF's effectiveness, an equal amount of nitrogen was applied in each cultivation plot, either through chemical fertilizer or irrigation with nitrate-contaminated groundwater. Regular monitoring of infiltrating pore water and groundwater was conducted in each cultivation plot. The linear regression slope for nitrate concentration in the pore water after repeated application of PAF ranged from -3.527 to -8.3485 mg-N/L/yr, confirming that PAF can reduce nitrate concentration in the pore water. With an increasing proportion of PAF, the infiltrating nitrate mass in pore water was reduced by 42% compared to plots fertilized with chemical fertilizer. Additionally, the linear regression slope of nitrate concentration in groundwater was calculated as -2.2999 and -9.2456 mg-N/L/yr. Therefore, continuous application of PAF in rural areas is expected to significantly contribute to reducing nitrate concentration in groundwater.

• 한국토양비료학회지
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• 제45권6호
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• pp.943-948
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• 2012

오이 시설재배지에서 질소 시비량 절감에 대한 호밀 환원 효과와 수량과 토양용액 중 질산태질소와의 관계를 평가하였다. 시험 처리구는 토양검정시비구 (NPK), 호밀을 $42.3Mg\;ha^{-1}$ 환원하여 질소비료 199 kg N $ha^{-1}$의 0, 50, 75, 100%의 4 수준으로 시비하여 시설재배지에서 오이 수량과 토양용액의 질산태질소 농도를 조사하였다. NPK의 오이수량은 $68.8Mg\;ha^{-1}$이었고, 호밀의 투입은 토양검정 질소시비량의 25-50%를 절감할 수 있었다. 오이재배 기간 중 NPK 토양용액의 평균 $NO_3$-N 농도는 $32.4mg\;L^{-1}$ 이었고, 호밀처리구의 0, 50, 75, 100%에서는 각각 26.0, 30.1, 41.4, $58.5mg\;L^{-1}$으로 질소시비량이 증가함에 따라 높아졌다. 이때 시설재배 오이수량과 토양용액 중 평균 $NO_3$-N 농도와의 수식 ($Y=49.3+0.63X-0.0034X^2$, $R^2=0.778^{**}$)은 유의성을 나타내었다. 따라서 오이 재배 중 토양용액 분석으로 질소 웃거름 시비량 결정이 가능할 것으로 판단되었다. 그러나 오이수량과 토양용액 $NO_3$-N 농도와의 관계에 대한 추가적인 실증연구가 필요할 것으로 사료된다.

• 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.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2002년도 총회 및 춘계학술발표회
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• pp.254-257
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• 2002

The purposes of this research are to identify the source and to analyze the pathway of nitrate contamination in "cultural village", Jeungpyeong. In order to examine recharge processes and flow pattern that closely related to the influent of nitrate contaminant, the flow field was simulated and the oxygen and hydrogen stable isotopes were analyzed. The nitrogen isotope was used to delineate contaminant sources. The shallow groundwater was mainly composed of precipitation, but leakage of domestic water and sewage contributed to the recharge. Nitrate contaminants were possibly from the leakage of sewage and animal waste. The nitrate concentration decreased due to dilution by low concentration water.ion water.

• 한국토양비료학회지
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• 제44권6호
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• pp.1112-1117
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• 2011

재배기간이 긴 잎들깨 시설 촉성재배 조건에서 질소시비 수준별 시험을 통하여 토양의 질산태질소 함량에 따른 질소 웃거름시비량 결정기준을 설정하였다. 잎들깨 주산단지인 금산과 밀양 두 지역에서 각각 1개의 시설하우스에서 질소시비량 5수준과 관행구를 난괴법 3반복과 4반복으로 각각 실시하였다. 생육시기별로 매달 건물중과 질소흡수량, 마디생장량을 조사하였고, 토양질산태질소를 분석하였다. 금산포장의 마디당 질소 요구량은 $2.2kg\;10a^{-1}$, 밀양포장은 $3.5kg\;10a^{-1}$로 조사되었다. 토양질산태질소의 하한기준은 금산포장과 밀양포장 모두 $NO_3$-N $10mg\;kg^{-1}$로 설정하였다. 상한기준 설정은 토심 15 cm, 용적밀도 $1.2Mg\;m^{-3}$, 토양 중 질산태질소의 이용율 70%를 적용하여 잎들깨 1마디에 필요한 질소요구량을 충족하는 수준으로 결정하여 금산포장과 밀양포장 각각 $30mg\;kg^{-1}$과 $40mg\;kg^{-1}$로 설정하였다. 따라서 금산지역은 Y=-0.157X + 4.71에 의해, 밀양지역은 식 Y=-0.1667X + 6.6667에 의해 잎들깨 1마디 생육에 필요한 질소 웃거름 시비량을 결정할 수 있었다.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 2003년도 총회 및 춘계학술발표회
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• pp.63-66
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• 2003

This study applied a hydrogeological field survey and isotope investigation to identify source locations and delineate pathways of groundwater contamination by nitrogen compounds. The infiltration and recharge processes were analyzed with groundwater-level fluctuation data and oxygen-hydrogen stable isotope data. The groundwater flow pattern was investigated through groundwater flow modeling and spatial and temporal variation of oxygen isotope data. Based on the flow analysis and nitrogen isotope data, source types of nitrate contamination in groundwater are identified. Groundwater recharge largely occurs in spring and summer due to precipitation or irrigation water in rice fields. Based on oxygen isotope data and cross-correlation between precipitation and groundwater level changes, groundwater recharge was found to be mainly caused by irrigation in spring and by precipitation at other times. The groundwater flow velocity calculated by a time series of spatial correlations, 231 m/yr, is in good accordance with the linear velocity estimated from hydrogeologic data. Nitrate contamination sources are natural and fertilized soils as non-point sources, and septic and animal wastes as point sources. Seasonal loading and spatial distribution of nitrate sources are estimated by using oxygen and nitrogen isotopic data.