Nutrient fluxes and sediment oxygen demands (SOD) were measured with intact sediment cores collected from three stations in the downstream of Nagdong River. The sediments were subjected to controlled oxic and hypoxic conditions and temperature gradients (from $10^{circ}C$ to $30^{circ}C$) of the overlying waters in laboratory batch system. The effect of temperature and labile layer thickness of the sediment on SOD were examined. $PO_4;^{3-}$ and $NH_4;^+$ fluxes were elevated above $20^{circ}C$ and large mobilities were observed when they were coupled with a hypoxic and high-temperature condition. In the well oxygenated conditions, $PO_4;^{3-}$ fluxes were negative or negligible but $NH_4;^+$ fluxes ranged from 1.3 mg N $m^{-2};hr^{-1}$ to 2.3 $m^{-2};hr^{-1}$. Temperature quotients($Q_{10}$) of $PO_4;^{3-}$ fluxes were 3.7 ${sim}$ 7.3 ranges to have the most high values. $PO_4;^{3-}$ and $NH_4;^+$ fluxes had the logarithmic increase with temperature, while $NO_3;^-$ was negatively absorbed to the sediment and linearly correlated with the temperature. $SiO_2$ fluxes showed no difference among oxic and hypoxic conditions and sediment texture. The nutrient fluxes would be closely correlated with pore water chemistry of sediments and activated by the top sediment layer composition such as labile organic matters or algal detritus. The ecological implications of the nutrient fluxes were discussed in terms of sources and sinks of nutrients coupled to algal productions in the Nagdong River.