• Title/Summary/Keyword: $[^{13}N]NH_3$

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A Study of Soil and Water Pollutions in Kyungsan Province (경산지역 토양 및 수질오염에 관한 연구)

  • 김용태;이부용;김동석;양소영;이동훈;박병윤
    • Journal of Environmental Science International
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    • v.11 no.7
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    • pp.713-720
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    • 2002
  • In order to provide the basic information on the environmental pollution of Kyungsan province, the contents of Pb, Cd, Cr, Cu, Mn and Zn in soil, stream water, aquatic sediment and groundwater were investigated, and also the values of pH, COD, $KMnO_4-C$,\;NH_3-N,\;NO_2-N,\;NO_3-N$ and $Cl^-$ of stream water and groundwater were determined. The results were as follows. The values of COD, $NH_3-N,\;NO_2-N$ and $NO_3-N$ of the stream waters were very low. The contents of Pb, Cd, Cr, Cu and Zn in the stream waters were respectively at range of $0.014~0.063 mg/{\ell},\;0.004~0.007 mg/{\ell$\mid$, 0~0.045 mg/{\ell},\;0~0.008 mg/{\ell}$\;and\;$0.001~0.175 mg/{\ell}$, and these values were much lower than those of contaminated stream water in Korea. The contents of Cd, Cr, Cu and Zn in the soils were respectively at range of 0.12~O.71 ppm, 0.88~2.65 ppm, 2.86~22.33 ppm and 3.89~26.39 ppm, and these values were much lower than those of ordinary polluted areas in Korea. The contents of Cd, Cr, Cu, As, Zn and Mn in the aquatic sediments were respectively at range of 3.05~3.81 ppm, 14.6~70.6 ppm, 13.74~61.59 ppm, 76.8~465.5 ppm, 12.56~190.83 ppm and 333.3~l188.3 ppm. The values of pH, $KMnO_4-C,\;NH_3-N$, and $NO_3-N$ of the groundwaters were respectively at range of 7.6~8.4, $0~3.95{\ell}$, 0.05~0.15 mg/{\ell}$ and 0.05~0.42 $mg/{\ell}$. The contents of Pb, Cd and Cr in the groundwaters were respectively at range of 0.015~0.061 $mg/{\ell}$, 0.O06~0.009 $mg/{\ell}$ and 0.005~0.045 $mg/{\ell}$.

Synthesis of N-doped Ethylcyclohexane Plasma Polymer Thin Films with Controlled Ammonia Flow Rate by PECVD Method

  • Seo, Hyunjin;Cho, Sang-Jin;Boo, Jin-Hyo
    • Applied Science and Convergence Technology
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    • v.23 no.1
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    • pp.44-47
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    • 2014
  • In this study, we investigated the basic properties of N-doped ethylcyclohexene plasma polymer thin films that deposited by radio frequency (13.56 MHz) plasma-enhanced chemical vapor deposition (PECVD) method with controlled ammonia flow rate. Ethylcyclohexene was used as organic precursor with hydrogen gas as the precursor bubbler gas. Additionally, ammonia ($NH_3$) gas was used as nitrogen dopant. The as-grown polymerized thin films were analyzed using ellipsometry, Fourier-transform infrared [FT-IR] spectroscopy, UV-Visible spectroscopy, and water contact angle measurement. We found that with increasing plasma power, film thickness is gradually increased while optical transmittance is drastically decreased. However, under the same plasma condition, water contact angle is decreased with increasing $NH_3$ flow rate. The FT-IR spectra showed that the N-doped ethylcyclohexene plasma polymer films were completely fragmented and polymerized from ethylcyclohexane.

Investigate Electronic Property of N-doped Plasma-Polymer Thin Films for Applied Biosensors

  • Seo, Hyeon-Jin;Hwang, Gi-Hwan;Nam, Sang-Hun;Ju, Dong-U;Lee, Jin-Su;Yu, Jeong-Hun;Bu, Jin-Hyo;Yun, Sang-Ho
    • Proceedings of the Korean Vacuum Society Conference
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    • 2013.08a
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    • pp.159-159
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    • 2013
  • In this studying, we investigated the basic properties of N-doped plasma polymer. The N-doped plasma polymer thin films were deposited by radio frequency (13.56 MHz) plasma-enhanced chemical vapor deposition method. Various carbon-source were used as organic precursor with hydrogen gas as the precursor bubbler gas. Additionally, ammonia gas [NH3] was used as nitrogen dopant. The as-grown polymerized thin films were analyzed using cyclic voltammetry, ellipsometry, Fourier-transform infrared [FT-IR] spectroscopy, Raman spectroscopy, FE-SEM, and water contact angle measurement. Electronic property of N-doped plasma thin film is changed as flow rate of the NH3 gas.

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Characteristics of Water Quantity and Quality of the Anyangcheon using SWAT Model and Calculation Result of EMC (SWAT 모형과 EMC 산정결과를 이용한 안양천의 수량 및 수질 특성)

  • Chung, Eun-Sung;Lee, Kil Seong;Shin, Mun-Joo
    • Journal of Korean Society on Water Environment
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    • v.22 no.4
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    • pp.648-657
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    • 2006
  • Characteristics of water quantity and quality of the Anyangcheon were analyzed through many field measurements and the distributed hydrologic simulation model, Soil and Water Assessment Tool (SWAT). Event mean concentrations (EMCs) and baseflow mean concentrations were calculated from the data and the daily runoff were simulated by SWAT. The runoff was divided into the direct runoff and the baseflow. Using those values and quantity and quality data of release from the wastewater treatment plant (WWPT), unit loads of BOD, COD, SS, $NO_2-N$, $NO_3-N$, $NH_3-N$, and Dis-P were derived. EMCs of BOD and SS were even higher than the baseflow mean concentrations. The total runoff from October to April (7 months) of 2004 was just 13.5%, since the rainfall usually is concentrated in summer season. Futhermore BOD and SS were loaded during the event by 50.9% and 70.9%, respectively and over three quarters of total COD, $NO_2-N$, $NO_3-N$, $NH_3-N$, and Dis-P were flowed into the Anyangcheon during the remaining period. Therefore, the efficiency of WWPT for COD, $NO_2-N$, $NO_3-N$, $NH_3-N$, and Dis-P should be intensified from Oct. to Apr. and the runoff quality management of BOD and SS should be planned during the summer season.

Mineralization of organic materials applied to Korean ginseng (고려인삼(高麗人蔘) 유기질비료(有機質肥料)의 무기화(無機化))

  • Hong, Jung-Kook;Park, Hoon;Park-Lee, Quihee
    • Korean Journal of Soil Science and Fertilizer
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    • v.13 no.1
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    • pp.13-19
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    • 1980
  • 1. Ginseng field and virgin soils, to which Yakto, washed Yakto, litters (deciduous and coniferous trees) and bone meal were applied, were incubated at 60% of field capacity of the soils to shed light on the production of $NH_4-N$ and $NO_3-N$ through mineralization of the organic materials being the nitrogen sources for Korean ginseng. 2. Total nitrogen content mineralized in the soils, to which the following organic materials were applied, was:bone meal>Yakto${\gg}$litter (deciduous trees)> washed Yakto, litter (coniferous trees). The content increased with incubation time in all the virgin and ginseng field soils excepting only the virgin soils applied with washed Yakto and litters of which the contents decreased. A large part of nitrogen mineralized in the virgin and ginseng field soils to which Yakto was applied was nitrate form, while a half ginseng field soils and a considerable part in the other virgin soils was ammonium form in the other treatments. 3. $NH_4-N$ content produced in the virgin and ginseng field soils applied with bone meal increased with the time, while it decreased in the other treatments. And the content in the soils applied with bone meal was very high. 4. $NO_3-N$ content showed a continuous increase during the incubation time in all treatments of ginseng field soils and only in the virgin soil to which Yakto was applied, wherease it showed almost no change in the other treatments of virgin soils. And the content in the soils applied with Yakto was very high. 5. Yakto was expected to supply nitrate enough to meet amounts of nitrogen required by ginseng with different ages and also expected to increase in soil fertility, while bone meal was expected only to supply much nitrogen of which a considerable part was ammonium form.

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Environmental Studies in the Lower Part of the Han River Vl. The Statistical Analysis of Eutrophication Factors (한강 하류의 환경학적 연구 Vl. 부영양 요인의 통계적 해석)

  • Jung, Seung-Won;Hue, Hoi-Kwon;Lee, Jin-Hwan
    • Korean Journal of Ecology and Environment
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    • v.37 no.1 s.106
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    • pp.78-86
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    • 2004
  • In order to reveal the relationship between the concentration of chlorophyll- a and the environmental factors affecting eutrophication, the present study was biweekly conducted at G stations in the lower part of the Han river during the period from Feb. 24,2001 to Feb. 9,2002. Water temperature was changed from $0.5^{\circ}C$ to $26.4^{\circ}C$, pH was 5.77${\sim}$8.99, DO 3.15${\sim}$14,36 mg $L^{-1}$, BOD 0.90${\sim}$7.45 mg $L^{-1}$, and COD 1.16${\sim}$9.13 mg $L^{-1}$. TN and TP were ranged from 1.68${\sim}$20.96 mg $L^{-1}$, and 0.02 ${\sim}$ 1.17 mg $L^{-1}$, respectively. $NH_4\;^+$-N, $NO_3\;^-$-N, and $PO_4\;^{3-}$-P were ranged from 0.56${\sim}$3.60 mg $L^{-1}$, 0.03${\sim}$7.29 mg $L^{-1}$, and 0.002${\sim}$0.754 mg $L^{-1}$. Chlorophyll- a was extensively changed from 2.29 ${\mu}g\;L^{-1}$ to 136.28 ${\mu}g\;L^{-1}$ by month and stations. Results of nutrients indicated the eutrophic level in this area and water quality was the gradual worsening in the lower stations than those of upper stations during the period studied. The Pearson correlation analysis between the concentration of chlorophyll- a and the environmental factors indicated that BOD, COD, pH, $NH_4\;^+$-N, TP, TN, conductivity and $PO_4\;^{3-}$-P were positive correlation, but $NO_3\;^-$-N was negative. The environmental factors investigated using the principal component method could be triparted. The first factor group included conductivity, BOD, COD, TN, TP, $NH_4\;^+$-N, $PO_4\;^{3-}$-P and SS, the second WT and DO, and the third pH and $NO_3\;^-$-N. Using the stepwise regression analysis, chlorophyll- a was under the influence of conductivity, $PO_4\;^{3-}$-P, $>NO_3\;^-$-N and $NH_4\;^+$-N Chlorophyll-a = 0.3661 ${\times}$ (Conductivity) - 0.3592 ${\times}$ ($PO_4\;^{3-}$-P) - 0.3449 ${\times}$ ($NO_3\;^-$-N)+0.4362 ${\times}$ ($NH_4\;^+$-N.

Determination of the Origin in both Dissolved Inorganic Nitrogen and Phytoplankton at the Lake Paldang using Stable Isotope Ratios (δ13C, δ15N, δ15N-NO3 and δ15N-NH4) (질산염 및 식물플랑크톤의 안정동위원소비를 이용한 팔당호 수계내의 질소원 기원 연구)

  • Kim, Min-Seob;Lee, Eun-Jeong;Yoon, Suk-Hee;Lim, Bo-La;Park, Jaeseon;Park, Hyunwoo;Chung, Hyen-Mi;Choi, Jong-Woo
    • Korean Journal of Ecology and Environment
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    • v.50 no.4
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    • pp.452-458
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    • 2017
  • The nitrogen isotope value in both ammonium and nitrate ion were determined at 9 stations during both June and August 2016, in order to understand the origin of DIN at the Han river. ${\delta}^{15}N-NO_3$ and ${\delta}^{15}N-NH_4$ values in 8 stations (CP, SB, MHC, P4, SJ, SBC, P2, SC) were no significant variation. However ${\delta}^{15}N-NO_3$ and ${\delta}^{15}N-NH_4$ values in KK (Kyeongan stream) showed significant different in comparison with 8 stations, with an apparent increase of nitrogen isotope values. These results indicate that antropogenic nitrogen source influence on KK station. Also the ${\delta}^{13}C$ and ${\delta}^{15}N$ isotope ratio of phytoplankton (Diatom and Cyanobacteria) in KK (Kyeongan stream) showed heavier values, compared to other study stations. These results indicate that nitrogen isotope value in phytoplankton effects by different nitrogen source in study sites. These results suggest that the analysis of stable isotope ratios is a simple but useful tool for the identification of dissolved inorganic nitrogen origin in aquatic environments.

Sanitary Chemical Conditions of Farmwaters in Choongcheongnam and Kangwon Province According to Spring and Summer (충청남도 및 강원도 목장지역 목장용수의 춘하절간 위생화학적 변화)

  • 이강문;박석기;이용욱
    • Journal of Food Hygiene and Safety
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    • v.9 no.4
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    • pp.229-235
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    • 1994
  • It is very important to investigate the sanitary chemical conditions of farmwaters used for cattle breeding in the dairy farms. For this purpose we examined pH, KMnO4 consumption, total hardness, chloride, sulfate, NH3-N, NO3-N, fluoride, lead, iron, manganese, cadmium, copper, zinc and chrome in the farmwaters sampled 2 times(spring and summer)in Choongcheongnam and Kangwon Province. The pH of farmwaters in Choongcheongnam and Kangwon Province was 6.49$\pm$0.09, 6.70$\pm$0.06, total hardness 90.21$\pm$7.07, 64.53$\pm$6.38 mg/ι, consumption of KMnO4 4.13$\pm$0.62, 4.34$\pm$0.26mg/ι, NO3-N 6.51$\pm$0.55, 3.61$\pm$0.58 mg/ι, chloride ion 20.51$\pm$1.99, 5.41$\pm$1.36 mg/ι and sulfate ion 6.61$\pm$1.02, 7.28$\pm$1.30 mg/ι, respectively. But NH3-N was scarcely detected. Fluoride, iron, lead, cadmium, zinc, manganese and chrome were not detected from the tested farmwaters. There was high significance between each other in total hardness, NO3-N, chloride ion and sulfate ion. There was regional and seasonal significance in only NO3-N but only regional significance in total hardness and chloride ion.

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Changes of water Quality During the Seed Production Period of Dark-banded Rockfish Sebastes inermis in Large Scale Tanks (대형 수조에서 볼락 종묘 생산에 따른 수질 환경의 변화)

  • Oh, Sung-Yong;Noh, Choong-Hwan
    • Journal of Aquaculture
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    • v.19 no.1
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    • pp.25-32
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    • 2006
  • An experiment was carried out to investigate changing of water quality during the seed production of dark-banded rockfish Sebastes inermis in large scale tanks. Ten broodstock of dark-banded rockfish were held in three circular tanks (diameter 6.5 m; depth 2 m; water volume 50 ton) each (stocking density $0.061kg/m^3$). During the experiment the temperature ranged from 14.2 to $16.1^{\circ}C$. The fingerlings were 134 with rotifers only during 1 to 9 days after parturition, rotifers with Artemia nauplii during 10 to 20 days after parturition, Artemia nauplii only during 21 to 35 days after parturition, Artemia nauplii with commercial diet during 36 to 80 days after parturition and commercial diet only during 81 to 85 days after parturition. Water quality (dissolved oxygen, pH, $NH_4^+-N,\;NO_2^--N,\;NO_3^--N\;and\;PO_4^{3-}-P$) in rearing tanks measured every 5 days in long term monitoring investigation or every 2 hours in diurnal monitoring investigation. In 85 days after parturition, the body weight of fish grew up to 0.88 f and specific growth rate was 8.0%/day in body weight. In long term monitoring investigation, with the increase of the amount of supplied commercial diet, the concentration of dissolved oxygen (DO) and pH decreased, but the concentration of $NH_4^+-N\;(4.5\;to\;76.3{\mu}M),\;NO_2^--N\;(0.02\;to\;0.06{\mu}M),\;NO_3^--N\;(3.0\;to\;5.9{\mu}M)$, and $PO_4^{3-}-P\;(0.41\;to\;0.59{\mu}M)$ increased. In the diurnal monitoring investigation, the concentration of $NH_4^+-N$ showed great fluctuation and ranged from 3.0 to $9.1{\mu}M$ when fed rotifers, 16.3 to $45.8{\mu}M$ when fed Artemia nauplii and 36.5 to $120.1{\mu}M$ when fed commercial diet. After daily feeding with each of feed, the amount of dissolved inorganic nitrogen (DIN) and phosphorus (P) wastage were 7.0 g and 0.7 g when fed rotifers, 24.7 g and 0.7 g when fed Artemia nauplii and 140.9 g and 2.2 g when 134 commercial diet. The amount of DIN and phosphorous wastage during 134 commercial diet was significantly higher than that of fed rotifer and Artemia nauplii (P<0.05). Results will provide valuable information far water quality management and culture of dark-banded rockfish in commercial seed production systems.

Assessment on Environmental Stabilization of Used Open Dumping Landfill - A Case Study of Kamkok Landfill - (사용종료 비위생 매립지의 환경 안정성 평가 - 감곡 매립지 사례 연구 -)

  • Park, Sangchan;Cho, Byeongreal;Jeong, Jihye;Lee, Minhee;Kim, Taeyoung;Park, Jongho
    • Journal of the Korean GEO-environmental Society
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    • v.9 no.6
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    • pp.13-19
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    • 2008
  • The objectives of this paper are to investigate states of these open dumping landfills for managing, utilizing and stabilization of a municipal solid waste landfill site in environmentally secure conditions. The result of the physical analysis of the landfill showed that it is composed of between 29.72-63.84% organic matter, 32.88% vinyl plastic. The environmental assessment of the landfill site confirmed that the landfill is at a maturation phase due to 0.18 of $BOD_5$/CODcr of leachate. VS and FS of TS Was respectively 30.37%, 32.34% and C/N ratio was 21.8. Surface water around landfill was BOD 10.7 mg/g, SS 37.8 mg/g, E-Coli 31,157(MPN/$100m{\ell}$) and Ground water was $COD_{Mn}$ 1.13-1.38 mg/g, $NO_3-N$ 1.025-4.075 mg/g. Leachat indicated T-P 0.002-0.028 mg/g, $NH_3-N$ 4.0-21.0 mg/g. The soil contamination of around landfill didn't appear as below of the regulation of Soil Environment Conservation Act. The Landfill Gas was $CH_4$ 13.25%, $CO_2$ 6.17%, H2S and CO was not detected. Also Surface Water was not detected $CO_2$, $CH_4$, $H_2S$, CO.

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