丹江口水库氮磷内源释放对比

利用柱状沉积物采样器在丹江口水库采集不同点位原位柱状沉积物,通过静态培养释放实验及间隙水分子扩散模型两种方法获取沉积物-水界面N和P释放速率,分析水体N和P释放特征.结果表明,不同采样点N和P界面交换速率差异显著.静态培养条件下,5个点位NH_4~+-N和PO_4~(3-)-P释放速率分别为13. 07～24. 88 mg·(m~2·d)~(-1)和3. 06～6. 02 mg·(m~2·d)~(-1);分子扩散模型条件下,5个点位NH_4~+-N和PO_4~(3-)-P释放速率分别为2. 67～7. 25 mg·(m~2·d)~(-1)和0. 04～0. 18 mg·(m~2·d)~(-1). N和P释放速率总体呈北高南低的趋势,支流N和P最低释放速率分别是主库区最高释放速率的1. 48和1. 57倍.两种方法均表明郭家山支流N和P的释放速率最高,具有较大内源N和P释放风险.比较两种方法发现,利用Fick定律计算出的界面N和P释放速率明显小于柱样模拟方法得出的结果,N和P的R/F值分别为3. 43～4. 98和29. 67～72. 88,这表明用分子扩散模型法进行内源释放速率估算时,偏离真实情况较大,而原柱样静态模拟实验则较贴近真实情况.

Endogenous Release of Nitrogen and Phosphorus in the Danjiangkou Reservoir

In situ sediments were collected at different sites of the Danjiangkou Reservoir using a columnar sediment sampler, and the release rate of N and P at the sediment-water interface was determined through static incubation experiments and the diffusion model of interstitial water molecules. The results showed that there was a significant difference in the release rate for N and P from sediments collected at five sampling sites. The release rates of NH₄⁺-N and PO₄^3--P under static incubation conditions were 13.07-24.88 mg·(m²·d)^-1 and 3.06-6.02 mg·(m²·d)^-1, whereas those estimated by Fick''s Fist Law were 2.67-7.25 mg·(m²·d)^-1 and 0.04-0.18 mg·(m²·d)^-1, respectively. Overall, the release rates of N and P in the tributaries were 1.48 and 1.57 times higher than that in the reservoir, respectively, and they tended to decrease from the north to the south. The R/F values of NH₄⁺-N and PO₄^3--P were 3.43-4.98 and 29.67-72.88, respectively. The highest release rates of N and P were observed in the Guojiashan tributary for both methods. However, it was found that the release rates of N and P estimated by Fick''s Fist Law were significantly lower than those obtained by the simulation method, indicating that the static incubation experiment with intact sediments allowed the release rates of N and P to be closer to the actual situation compared to the interstitial water molecule diffusion model.