• Title/Summary/Keyword: phosphorous release flux

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Calculation of Phosphorus Release Flux from Benthic Sediments in Sookchun Lake (소옥천 호소 저서퇴적물의 인 용출률 산정)

  • Ryu, Byong-Ro
    • Journal of Korea Water Resources Association
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    • v.48 no.1
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    • pp.9-21
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    • 2015
  • This study examined pollution level of sediment in Sookchun lake, and studied dredging validity by examining phosphorous release characteristics on surface polluted soil. Total phosphorous, the principal cause of algal blooms, exceeded dredging assessment standards regarding Daechung lake (1.5 mg/g) at all points. Also at all points, total nitrogen exceeded the dredging assessment standard regarding Paldang Lake (1.1 mg/g), but fell short of the standard regarding Daechung lake (3.0 mg/g). Dredging zone was suggested in this study is Chuso water body (WS-6~WS-12) in Sookchun lake. In relation to sediment pollution levels measured at different depths, LOI tended to decrease as it became deeper. The concentrations of T-N varied depending upon the depth as well as points, but no regular pattern was observed. The depth and site did not significantly influence T-P. From the results of phosphorous release tests, it was shown that total phosphorous release flux was calculated to be $7.2{\sim}15.4mg/m^2/d$ for anaerobic condition, $0.5{\sim}2.0mg/m^2/d$ for aerobic condition and $2.0{\sim}4.1mg/m^2/d$ for facultative condition. Release flux and T-P concentration of surface sediments had positive correlation ($R^2$ 0.7871). And The corelation between release flux and DO condition in reactor had strong negative correlation ($R^2$ 0.8824).

Effects of Water Temperature, Light and Dredging on Benthic Flux from Sediment of the Uiam Lake, Korea (의암호에서 퇴적물 용출에 대한 수온, 빛과 퇴적물 제거의 영향)

  • Youn, Seok Jea;Kim, Hun Nyun;Kim, Yong Jin;Im, Jong Kwon;Lee, Eun Jeong;Yu, Soon Ju
    • Journal of Korean Society on Water Environment
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    • v.33 no.6
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    • pp.670-679
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    • 2017
  • An experiment to study the effect of temperature, light, and dredging on release of nutrients downstream from Gongjicheon in the Uiam reservoir was carried out in the laboratory using sediments from different depths. At various water temperatures, dissolved total nitrogen was not released, but the average nutrient flux of dissolved total phosphorus was increased (0.034 at $15^{\circ}C$, 0.005 at $20^{\circ}C$, 0.154 at $25^{\circ}C$, $0.592mg/m^2/d$ at $30^{\circ}C$). Dissolved total phosphorous was released in controlled darkness. In contrast, in controlled light, the concentrations of dissolved total phosphorous and dissolved total nitrogen in the overlying water steadily decreased during the study period (70 d), because they were continuously consumed by the growth of photosynthetic algae. However, there was no significant relationship between water nutrient concentration, nutrient release, and the depth of the sediment. We concluded that the dredging of sediment would not affect the nutrient release rate of the sediment, because there were no significant differences in the nutrient concentrations released from the sediment. When the sediment was removed from the surface to 20 cm in depth, the nutrients were not transferred to the water body, implying that the sediment removal had little effect on secondary pollution.

In-situ Treatment for the Attenuation of Phosphorus Release from Sediments of Lakes (호소퇴적물로부터 인 용출 저감을 위한 In-situ 처리)

  • Kim, Seog-Ku;Lee, Mi-Kyung;Ahn, Jae-Hwan;Kang, Sung-Won;Kim, Young-Im
    • Journal of Korean Society of Environmental Engineers
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    • v.28 no.5
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    • pp.563-572
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    • 2006
  • In order to propose optimum in-situ treatment for reducing phosphorous release from sediment of stationary lakes, a series of column tests were performed. The sediment used in experiment was very fine clay with a mean grain site $7.7{\phi}$ and high $C_{org}$ contents(2.4%). Phosphorous releases were evaluated in two ways : in lake water(with microbial effect) and in distilled water(without microbial effect). As in-situ capping material, sand and loess were used while Fe-Gypsum and $SiO_2$-Gypsum were used for in-situ chemical treatment. In case of lake water considering the effect of microorganism, phosphorous concentration rapidly decreased in the early stage of experiment but it was gradually increased after 10 days. Flux of phosphorous release for control was $3.0mg/m^2{\cdot}d$. Whereas, those for sand layer capping(5 cm) and loess layer capping(5 cm) were $2.5mg/m^2{\cdot}d\;and\;1.8mg/m^2{\cdot}d$, respectively because the latter two were not consolidated sufficiently. For Fe-gypsum and $SiO_2$-gypsum the fluxes were $1.4mg/m^2{\cdot}d$ which meant that reduction efficiency of phosphorous release was more than 40% higher than that of control. The case capping with complex layer was $1.0mg/m^2{\cdot}d$, which showed high reduction efficiency over 60%. The addition of gypsum($CaSO_4{\cdot}2H_2O$) into the sediment reduced release of Phosphorus from the sediments. Gypsum acted as a slow-releasing source of sulphate in sediment, which enhanced the activity of SRB(sulfate reducing bacteria) and improved the overall mineralization rate of organic matter.

Estimation of Nutrients Released from Sediments of Deukryang Bay (득량만 퇴적물로부터 영양염 용출 평가)

  • 김도희;박청길
    • Journal of Environmental Science International
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    • v.7 no.4
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    • pp.425-432
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    • 1998
  • The purpose of the present study is to estimate the release of dissolved Inorganic nitrogen and photophorous from sediments of Deukryang Bay. One method used In this study is to calculate nutrients released from a concentration gradient between sediment porewaters and the overlying water based on periments. The calculated and measured ammonium released from the sediments were 8.93mg-atN/$m^2$ hr and 60.4mg/atN/$m^2$ hr, respectively In July. 8.57mg-atN/$m^2$. hr and 32.9mg/atN/$m^2$ hr, respectively in October. The ammonium was released more highly in truly than in October, and the measured ammonium flux was higher than the calculated one. The calculated nitrate plus nitrite released from the sediments were 0.31mg/atN/$m^2$. hr in July and 0.84mg/atN/$m^2$. hr in October. The measured nitrate plus nitrite released from the sediments was 282mg/atN/$m^2$. hr in October. The calcuated was lower than the measured because the content of the nutrients in the sediments was always much more than in the overlying waters, and it has shown a differently seasonal pattern compared to the ammonium flux. The calculated phosphorous released from the sediments were 0.97mP/atN/$m^2$ hr and measured negative fluxed -6.50mP/atN/$m^3$ hr In truly, and alculated 0.18mg/atP/$m^2$. hr and measured 24.6mg/atP/$m^2$. hr, respectively in October.

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A Study on Water Quality after Construction of the Weirs in the Middle Area in Nakdong River (낙동강 중류수계의 인공보 설치에 따른 보 내 수질특성에 관한 연구)

  • Lee, Sun-Hwa;Kim, Bo-Ram;Lee, Hye-Won
    • Journal of Korean Society of Environmental Engineers
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    • v.36 no.4
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    • pp.258-264
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    • 2014
  • This study is to investigate water quality changes of nitrogen (N) and phosphorous (P) at Gangjung-Goryeong Weir and Dalseong weir, in 2012-2013. Concentration of COD, TOC, T-N, T-P showed 3.5~6.8 mg/L, 3.4~6.5 mg/L, 1.8~4.0 mg/L, 0.08~0.12 mg/L respectively, in the Nakdong river main stream. Water quality of Dalseong weir showed lower level of contamination than that of Gangjung-Goryeong weir. Because of input loading of nutrients and organic matters from tributaries. At the analysis of sediments at each weirs, sedimentation fluxes of the hypolimnion represented 1.6~2.4 times higher than epilimnion fluxes. Sinking rate (%/d) of SS, N and P of the hypolimion showed in the range of 1.68 %/d~2.42 %/d. It is implied that the suspended matters seem to be floating in the water body. In the result of nutrients release experiment, release flux of nutrients in July showed 3~4 times higher than April. The reason was considered that nutrients is easily released in the anaerobic condition and at high water temperature.